#: locale=en ## Tour ### Description ### Title tour.name = Geology Virtual Field Experience ## Skin ### Button Button_01F2D9B2_E3F5_80AD_41EA_F572E945B3D5.label = 4.1.7 - Rock description and classification Button_01F2D9B2_E3F5_80AD_41EA_F572E945B3D5_mobile.label = 4.1.7 - Rock description and classification Button_04E5E3A7_E3CA_80B3_41E2_D21BE35BE96E.label = 4.1.8 - Field relationships among rack units Button_04E5E3A7_E3CA_80B3_41E2_D21BE35BE96E_mobile.label = 4.1.8 - Field relationships among rack units Button_04FF3AEB_EC06_D8A9_41EB_DF43484EBF61.label = 5.2.7 - Measuring structures Button_04FF3AEB_EC06_D8A9_41EB_DF43484EBF61_mobile.label = 5.2.7 - Measuring structures Button_05504F71_E3CD_81AF_41D4_57DA9B2D3A18.label = 4.2.1 - Interpreting how rock units formed Button_05504F71_E3CD_81AF_41D4_57DA9B2D3A18_mobile.label = 4.2.1 - Interpreting how rock units formed Button_06F7CED3_EC06_B8F9_41D3_562D89BB26E0.label = 5.3.1 - Old mine workings Button_06F7CED3_EC06_B8F9_41D3_562D89BB26E0_mobile.label = 5.3.1 - Old mine workings Button_073A9FA3_EC01_5959_41E6_81B5679222E1.label = 5.2.8 - Structural data to download and plot Button_073A9FA3_EC01_5959_41E6_81B5679222E1_mobile.label = 5.2.8 - Structural data to download and plot Button_08120645_EC03_4BD9_41D2_735E6907D165.label = 5.3.2 - Describing fold elements in the field Button_08120645_EC03_4BD9_41D2_735E6907D165_mobile.label = 5.3.2 - Describing fold elements in the field Button_089B93A1_E3CA_80AF_41E9_4B74505FA0FE.label = 4.3.3 - Petrographic description and interpretation Button_089B93A1_E3CA_80AF_41E9_4B74505FA0FE_mobile.label = 4.3.3 - Petrographic description and interpretation Button_08FFD819_E3CA_8F9F_41E1_94A1B094D732.label = 4.2.3 - Interpreting how rock units formed Button_08FFD819_E3CA_8F9F_41E1_94A1B094D732_mobile.label = 4.2.3 - Interpreting how rock units formed Button_0932DBF9_E3CA_809F_41DC_9A1A8E0D1522.label = 4.3.4 - Interpret geochemistry data in context of field relationships Button_0932DBF9_E3CA_809F_41DC_9A1A8E0D1522_mobile.label = 4.3.4 - Interpret geochemistry data Button_093E0C5F_EC07_BFE9_41ED_705E790A5EFC.label = 5.2.9 - Making a map Button_093E0C5F_EC07_BFE9_41ED_705E790A5EFC_mobile.label = 5.2.9 - Making a map Button_098A5F4A_E3CA_81FD_41D6_474E534A221F.label = 4.2.4 - Interpreting how rock units formed Button_098A5F4A_E3CA_81FD_41D6_474E534A221F_mobile.label = 4.2.4 - Interpreting how rock units formed Button_0A03B46C_E3CA_87B5_4195_60D5065E1E07.label = 4.2.2 - Interpreting how rock units formed Button_0A03B46C_E3CA_87B5_4195_60D5065E1E07_mobile.label = 4.2.2 - Interpreting how rock units formed Button_0A0D98CB_EC03_58E9_41E2_50842E8CF6CC.label = 5.2.1 - Measuring elements of a fold video Button_0A0D98CB_EC03_58E9_41E2_50842E8CF6CC_mobile.label = 5.2.1 - Measuring elements of a fold video Button_0A3A312E_EC03_C9AB_41EC_5EA855C81755.label = 5.3.4 - Interpretation of formation Button_0A3A312E_EC03_C9AB_41EC_5EA855C81755_mobile.label = 5.3.4 - Interpretation of formation Button_0AE6E8DD_E3CD_8097_41E2_6CC36E1E9637.label = 4.3.1 - 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Structural data to download and plot Button_0DF2F6DA_EC0F_48EB_41D6_5E604FB2C82D.label = 5.0.1 - Introduction video A Button_0DF2F6DA_EC0F_48EB_41D6_5E604FB2C82D_mobile.label = 5.0.1 - Introduction video A Button_0E3F2C12_E3CB_876D_41E8_95A2D2AA926C.label = 4.2.5 - Plotting structural data to download and plot Button_0E3F2C12_E3CB_876D_41E8_95A2D2AA926C_mobile.label = 4.2.5 - Plotting structural data to download Button_0E87E14A_EC01_49EB_41E1_FF823B8D56EB.label = 5.2.6 - Structural data to download and plot Button_0E87E14A_EC01_49EB_41E1_FF823B8D56EB_mobile.label = 5.2.6 - Structural data to download and plot Button_0ECB26B6_DCEB_5D0C_41DE_32C40D6F6F4E.label = 2.0 - Introduction video Button_0ECB26B6_DCEB_5D0C_41DE_32C40D6F6F4E_mobile.label = 2.0 - Introduction video Button_0F2194CB_DCEB_7D04_41CF_2A2CC94F427A.label = 2.0 - Introduction video Button_0F2194CB_DCEB_7D04_41CF_2A2CC94F427A_mobile.label = 2.0 - Introduction video Button_0F8C32FD_EC01_48A9_41EC_00DBD5C57F12.label = 5.2.5 - Measuring and classifying folds Button_0F8C32FD_EC01_48A9_41EC_00DBD5C57F12_mobile.label = 5.2.5 - Measuring and classifying folds Button_1E7760BF_9EC2_9DC0_4196_E45552463920.label = Locality 1 – BaseMap StrongColours Button_240A1478_EC07_CFB7_41E7_FEAC23313B64.label = 1.0 - introduction Button_240A6477_EC07_CFB9_41E1_E080611E8EF0.label = 1.0 - introduction Button_240A6478_EC07_CFB7_41E9_704845CD789C.label = 1.0 - introduction Button_240AD479_EC07_CFA9_41D7_161CCC073E42.label = 1.0 - introduction Button_240B046B_EC07_CFA9_41DF_1AD798D21F44.label = 1.0 - introduction Button_240B0472_EC07_CFBB_41D2_A3B80E870B8F.label = 1.0 - introduction Button_240B3475_EC07_CFB9_41E6_B9872A8A6DD1.label = 1.0 - introduction Button_240B4469_EC07_CFA9_41E8_D8DDE6AE4AD9.label = 1.0 - introduction Button_240B4470_EC07_CFB7_41CE_12E2575E76FE.label = 1.0 - introduction Button_240B4472_EC07_CFBB_41DA_927E65F0AFC7.label = 1.0 - introduction Button_240B4473_EC07_CFB9_41E5_877ACE51D564.label = 1.0 - introduction Button_240B546A_EC07_CFAB_41C2_61B34AB94682.label = 1.0 - introduction Button_240B547A_EC07_CFAB_41DD_5E9667B1B642.label = 1.0 - introduction Button_240B8474_EC07_CFB8_41D0_5EC3B6A588C6.label = 1.0 - introduction Button_240BA477_EC07_CFB9_41A4_19A0F3A29D6B.label = 1.0 - introduction Button_240BB476_EC07_CFBB_41E4_FD2992EF66C6.label = 1.0 - introduction Button_240BF476_EC07_CFBB_41C0_7F385B9CCED9.label = 1.0 - introduction Button_2434146D_EC07_CFA8_41DA_0E032420033A.label = 1.0 - introduction Button_2434146F_EC07_CFA9_41C3_1A88C998779B.label = 1.0 - introduction Button_24342466_EC07_CFDB_41D5_5D24B9EEC2CC.label = 1.0 - introduction Button_24343465_EC07_CFD9_41E1_646F72E4C9A3.label = 1.0 - introduction Button_24346466_EC07_CFDB_41DC_2A8612356298.label = 1.0 - introduction Button_2434646D_EC07_CFA9_41CC_FBF473D001A0.label = 1.0 - introduction Button_24348470_EC07_CFB7_41D1_5C24DFAF7A11.label = 1.0 - introduction Button_24349467_EC07_CFD9_41E6_D5CA7059B4E2.label = 1.0 - introduction Button_24349469_EC07_CFA9_41D3_C5CAD6AB108C.label = 1.0 - introduction Button_2434946A_EC07_CFAB_41EA_FA5480F1E7DF.label = 1.0 - introduction Button_24349471_EC07_CFB9_41EB_47F11A5794D6.label = 1.0 - introduction Button_2434A47A_EC07_CFAB_41E9_6302D731BFA9.label = 1.0 - introduction Button_2434C46F_EC07_CFA9_41DD_203FE3F12AC0.label = 1.0 - introduction Button_2434D468_EC07_CFD7_41D6_1256FA35C8D2.label = 1.0 - introduction Button_2434D46E_EC07_CFAB_41E0_FD3A4AF94A82.label = 1.0 - introduction Button_2434E467_EC07_CFD9_41C8_D6EE33DD3AF6.label = 1.0 - introduction Button_2437A462_EC07_CFDB_41C4_290285C6041C.label = Explore location 5 Button_2437A463_EC07_CFD9_41D9_AB87CA68C858.label = Show report Button_2437D461_EC07_CFD9_41D0_0ED819C7B2FA.label = Download button Button_24D989D2_EC01_D8FB_41DD_8A6564B1A099.label = 8.0 - Introduction video Button_24D989D2_EC01_D8FB_41DD_8A6564B1A099_mobile.label = 8.0 - Introduction video Button_24D9B9D3_EC01_D8F9_41E7_BF547D78CBF4.label = 8.1.1 - Describing rocks using various criteria Button_24D9B9D3_EC01_D8F9_41E7_BF547D78CBF4_mobile.label = 8.1.1 - Describing rocks using various criteria Button_24D9B9DC_EC01_D8EF_41E6_238AC1575BA3.label = 8.2.2 - Showing geological relationships using appropriate map symbols Button_24D9B9DC_EC01_D8EF_41E6_238AC1575BA3_mobile.label = 8.2.2 - Showing geological relationships using map symbols Button_24DA79D4_EC01_D8FF_41E4_2D3B311C0CF0.label = 8.1.2 - Describing rocks using various criteria Button_24DA79D4_EC01_D8FF_41E4_2D3B311C0CF0_mobile.label = 8.1.2 - Describing rocks using various criteria Button_24DB19E4_EC01_D8DF_41DD_ED2273733D4D.label = 8.3.1 - Interpret geochemistry data in context of field relationships Button_24DB19E4_EC01_D8DF_41DD_ED2273733D4D_mobile.label = 8.3.1 - Interpret geochemistry data in context of field relationships Button_24DB89DC_EC01_D8EF_41E9_235E11935159.label = 8.2.1 - Interpreting how rocks units are formed Button_24DB89DC_EC01_D8EF_41E9_235E11935159_mobile.label = 8.2.1 - Interpreting how rocks units are formed Button_24DF69CF_EC01_D8E9_41CB_AFFA1419C9D7.label = Download button Button_24DF69CF_EC01_D8E9_41CB_AFFA1419C9D7_mobile.label = Download button Button_24DFA9D1_EC01_D8F9_41E0_B5AA5EE80965.label = Show report Button_24DFA9D1_EC01_D8F9_41E0_B5AA5EE80965_mobile.label = Show report Button_24DFC9D0_EC01_D8F7_41B3_7B0AAE787FE4.label = Explore location 8 Button_24DFC9D0_EC01_D8F7_41B3_7B0AAE787FE4_mobile.label = Explore location 8 Button_2688EA21_EC06_DB59_41E2_D8857FEFBE11.label = 6.3.2 - 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Introduction video Button_26B50A10_EC06_DB77_41E7_DE5820727049_mobile.label = 6.0 - Introduction video Button_26B5FA0D_EC06_DB69_41C8_741F9DADB86B.label = Explore location 6 Button_26B5FA0D_EC06_DB69_41C8_741F9DADB86B_mobile.label = Explore location 6 Button_26B5FA0E_EC06_DB6B_41EB_2AD16903B67C.label = Show report Button_26B5FA0E_EC06_DB6B_41EB_2AD16903B67C_mobile.label = Show report Button_27C103F9_EC06_C8A9_41C9_5983D60D10BC.label = 7.0 - Introduction video Button_27C103F9_EC06_C8A9_41C9_5983D60D10BC_mobile.label = 7.0 - Introduction video Button_27C11403_EC06_CF59_41D6_01C1F7E68F7C.label = 7.2.2 - Interpreting relationships from a field map Button_27C11403_EC06_CF59_41D6_01C1F7E68F7C_mobile.label = 7.2.2 - Interpreting relationships from a field map Button_27C153FB_EC06_C8A9_41E1_A608157138B7.label = 7.1.3 - Identify and classifying rocks based on descriptions Button_27C153FB_EC06_C8A9_41E1_A608157138B7_mobile.label = 7.1.3 - Identify and classifying rocks based on descriptions Button_27C15402_EC06_CF5B_41CC_6182AC0C9E80.label = 7.2.1 - Geological history from field observation Button_27C15402_EC06_CF5B_41CC_6182AC0C9E80_mobile.label = 7.2.1 - Geological history from field observation Button_27C193FA_EC06_C8AB_41DD_119118870821.label = 7.1.1 - Identify and classifying rocks based on descriptions Button_27C193FA_EC06_C8AB_41DD_119118870821_mobile.label = 7.1.1 - Identify and classifying rocks based on descriptions Button_27C3A3F7_EC06_C8B9_41E7_85DE5DD0F7EC.label = Explore location 7 Button_27C3A3F7_EC06_C8B9_41E7_85DE5DD0F7EC_mobile.label = Explore location 7 Button_27C3A3F8_EC06_C8B7_41BD_91AEC3E06B86.label = Show report Button_27C3A3F8_EC06_C8B7_41BD_91AEC3E06B86_mobile.label = Show report Button_27C7740A_EC06_CF6B_41EC_1E83EB6E89A1.label = 7.3.2 - Incorporating micro-scope-scale observation Button_27C7740A_EC06_CF6B_41EC_1E83EB6E89A1_mobile.label = 7.3.2 - Incorporating micro-scope-scale observation Button_27C7B409_EC06_CF69_41A9_F48A9701164F.label = 7.3.1 - Incorporating micro-scope-scale observation Button_27C7B409_EC06_CF69_41A9_F48A9701164F_mobile.label = 7.3.1 - 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Interpreting how rock units formed Button_FD045A20_9FC2_8CC0_41DD_B8FF587AF91D_mobile.label = 1.2.4 - Interpreting how rock units formed Button_FF7F4ADC_9FFD_8D40_41D5_9F9F25EB472B.label = 1.3.3 - Integrating geochronology Button_FF7F4ADC_9FFD_8D40_41D5_9F9F25EB472B_mobile.label = 1.3.3 - Integrating geochronology ### Multiline Text HTMLText_0C8CE044_E3D6_7FF5_41E7_F1D5FDB0D1DD.html =
Instructions for locality 5


Click the explore location 5 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_0C8CE044_E3D6_7FF5_41E7_F1D5FDB0D1DD_mobile.html =
Instructions for locality 5


Click the explore location 5 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_2437C461_EC07_CFD9_41D4_CA730ACEBC38.html =
Instructions for locality 5


Click the explore location 5 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_24DEB9CE_EC01_D8EB_41A9_BDBB3D8E9D63.html =
Instructions for locality 8


Click the explore location 8 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_24DEB9CE_EC01_D8EB_41A9_BDBB3D8E9D63_mobile.html =
Instructions for locality 8


Click the explore location 8 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_26B45A0B_EC06_DB69_414D_A8515E9C7A25.html =
Instructions for locality 6


Click the explore location 5 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_26B45A0B_EC06_DB69_414D_A8515E9C7A25_mobile.html =
Instructions for locality 6


Click the explore location 5 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_27CC73F5_EC06_C8B9_4187_81F5A0FABC66.html =
Instructions for locality 7


Click the explore location 7 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_27CC73F5_EC06_C8B9_4187_81F5A0FABC66_mobile.html =
Instructions for locality 7


Click the explore location 7 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_2D0E0406_E3BA_8775_41DA_34D51E89F129.html =
Instructions for locality 4


Click the explore location 4 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_2D0E0406_E3BA_8775_41DA_34D51E89F129_mobile.html =
Instructions for locality 4


Click the explore location 4 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_2DC6B1BE_ABAC_BA27_41B7_556847B19CC4.html =
Instructions


Structural data and plot


Download the spreadsheet of the structural data and plot them on the base map Locality 2.
HTMLText_37A0F4D7_7CBA_1C59_41DA_7CD790D28F50.html =
Header 1


Header 2 [Youtube]


[Dev note: this is an embedded YouTube movie with the suggested videos disabled and autoplay. Autoplay will only work on Desktop computers not on mobile devices]
Mauris aliquet neque quis libero consequat vestibulum. Donec lacinia consequat dolor viverra sagittis. Praesent consequat porttitor risus, eu condimentum nunc. Proin et velit ac sapien luctus efficitur egestas ac augue. Nunc dictum, augue eget eleifend interdum, quam libero imperdiet lectus, vel scelerisque turpis lectus vel ligula. Duis a porta sem. Maecenas sollicitudin nunc id risus fringilla, a pharetra orci iaculis. Aliquam turpis ligula, tincidunt sit amet consequat ac, imperdiet non dolor.


Integer gravida dui quis euismod placerat. Maecenas quis accumsan ipsum. Aliquam gravida velit at dolor mollis, quis luctus mauris vulputate. Proin condimentum id nunc sed sollicitudin.


Header 2


• Nisl nec mi sollicitudin facilisis
• Nam sed faucibus est.
• Ut eget lorem sed leo.
• Sollicitudin tempor sit amet non urna.
• Aliquam feugiat mauris sit amet.
HTMLText_3D37CA66_B970_948F_41D7_CD7BF922FA64.html =
Instructions



Structural data to download and plot


Download the spreadsheet of the structural data and plot them on the base map Locality 3.
HTMLText_3E117F91_B890_8B85_41D5_62822A5F8D95.html =
Instructions


Structural data to download and plot


Download the spreadsheet of the structural data and plot them on the base map locality 3.
HTMLText_40C275FC_BB70_9F83_41E4_38705AD01538.html =
Instructions


Plotting structural data to download and plot


Download the spreadsheet of structural data and plot them on the base map for Locality 4 and a stereonet.
HTMLText_4DEA72B8_7CB6_F4D7_41C5_487BEBE0F389.html =
Location


Mount Hunt


Yikari WA 6430







HTMLText_4F3AC8B5_AC15_29B0_41D9_DD87B90C6EA5.html =
Instructions for locality 2


Click the explore location 2 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_4F3AC8B5_AC15_29B0_41D9_DD87B90C6EA5_mobile.html =
Instructions for locality 2


Click the explore location 2 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_5097FF0B_7854_6576_41B6_663C329C8376.html =
Instructions for locality 1


Click the explore location 1 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_537A0F4A_7C5E_0C4B_41DA_ACE856FB7CBE.html =
Credits



Nick Timms (Curtin EPS) – mastermind and overlord and acknowledges support from a Curtin Media Grant


Madelon Heperi (Curtin FLET) – programming, graphic design and teaching and learning design


Martin Towner (Curtin EPS) – drone pilot, cameraman, sound guy, field model, drone mosaic data processing


Aaron Cavosie (Curtin EPS) – geochemistry data and petrology wizard


Katy Evans (Curtin EPS) – teaching and learning design and acknowledges support from a Curtin Media Grant


Diana Taylor (Curtin FLET) – teaching and learning design


David Mole (CSRIO at the time) – whole geochemistry and sample collector and acknowledges support from the Science Plus Leader program of CSIRO


Chris Kirkland (Curtin EPS) – geochronology data collection and processing


Sean Makin (Curtin EPS) – drone pilot and data processing


Andrea Rajšic (Curtin EPS) – 360 camera operator, structural data collection and field model


Dave Belton (Curtin EPS) – areal 360 drone pilot and data processing


Tony Snow (Curtin EPS) – areal 360 drone co-pilot and assistant


Denis Fougerouse (Curtin EPS) – field model


Timmons Erickson (Curtin EPS, now at NASA) – sample collector


Steve Reddy (Curtin EPS) – sample collector
HTMLText_5D448817_78DC_EB9E_41D6_4EC2EE7CA496.html =
Credits


Nick Timms (Curtin EPS) – mastermind, overlord and acknowledges support from a Curtin Media Grant


Madelon Heperi (Curtin FLET) – programming, graphic design and teaching and learning design


Martin Towner (Curtin EPS) – drone pilot, cameraman, sound guy, field model, drone mosaic data processing


Aaron Cavosie (Curtin EPS) – geochemistry data and petrology wizard


Katy Evans (Curtin EPS) – teaching and learning design and acknowledges support from a Curtin Media Grant


Diana Taylor (Curtin FLET) – teaching and learning design


David Mole (CSRIO at the time) – whole geochemistry and sample collector and acknowledges support from the Science Plus Leader program of CSIRO


Chris Kirkland (Curtin EPS) – geochronology data collection and processing


Sean Makin (Curtin EPS) – drone pilot and data processing


Andrea Rajšic (Curtin EPS) – 360 camera operator, structural data collection and field model


Dave Belton (Curtin EPS) – areal 360 drone pilot and data processing


Tony Snow (Curtin EPS) – areal 360 drone co-pilot and assistant


Denis Fougerouse (Curtin EPS) – field model


Timmons Erickson (Curtin EPS, now at NASA) – sample collector


Steve Reddy (Curtin EPS) – sample collector
HTMLText_5FEA5D79_78CC_6592_41DD_90B3E8A37249.html =


Location


Mount Hunt


Yikari WA 6430
HTMLText_668B71CB_7834_1CF6_41AE_E80D9955201C.html =


Aerial views
HTMLText_668B71CB_7834_1CF6_41AE_E80D9955201C_mobile.html =


Aerial views
HTMLText_74BBD1CC_7834_3CF2_41D7_0CB75B8ACF12.html =
Header 1


Header 2 [Youtube]


[Dev note: this is an embedded YouTube movie with the suggested videos disabled and autoplay. Autoplay will only work on Desktop computers not on mobile devices]
Mauris aliquet neque quis libero consequat vestibulum. Donec lacinia consequat dolor viverra sagittis. Praesent consequat porttitor risus, eu condimentum nunc. Proin et velit ac sapien luctus efficitur egestas ac augue. Nunc dictum, augue eget eleifend interdum, quam libero imperdiet lectus, vel scelerisque turpis lectus vel ligula. Duis a porta sem. Maecenas sollicitudin nunc id risus fringilla, a pharetra orci iaculis. Aliquam turpis ligula, tincidunt sit amet consequat ac, imperdiet non dolor.


Integer gravida dui quis euismod placerat. Maecenas quis accumsan ipsum. Aliquam gravida velit at dolor mollis, quis luctus mauris vulputate. Proin condimentum id nunc sed sollicitudin.


Header 2


• Nisl nec mi sollicitudin facilisis
• Nam sed faucibus est.
• Ut eget lorem sed leo.
• Sollicitudin tempor sit amet non urna.
• Aliquam feugiat mauris sit amet.
HTMLText_79D330ED_0151_BCF4_4156_F01FB64A5F57.html =
Credits


Nick Timms (Curtin EPS) – mastermind, overlord and acknowledges support from a Curtin Media Grant


Madelon Heperi (Curtin FLET) – programming, graphic design and teaching and learning design


Martin Towner (Curtin EPS) – drone pilot, cameraman, sound guy, field model, drone mosaic data processing


Aaron Cavosie (Curtin EPS) – geochemistry data and petrology wizard


Katy Evans (Curtin EPS) – teaching and learning design and acknowledges support from a Curtin Media Grant


Diana Taylor (Curtin FLET) – teaching and learning design


David Mole (CSRIO at the time) – whole geochemistry and sample collector and acknowledges support from the Science Plus Leader program of CSIRO


Chris Kirkland (Curtin EPS) – geochronology data collection and processing


Sean Makin (Curtin EPS) – drone pilot and data processing


Andrea Rajšic (Curtin EPS) – 360 camera operator, structural data collection and field model


Dave Belton (Curtin EPS) – areal 360 drone pilot and data processing


Tony Snow (Curtin EPS) – areal 360 drone co-pilot and assistant


Denis Fougerouse (Curtin EPS) – field model


Timmons Erickson (Curtin EPS, now at NASA) – sample collector


Steve Reddy (Curtin EPS) – sample collector
HTMLText_7EDFE906_0151_AD34_4160_FA5048301482.html =
Credits



Nick Timms (Curtin EPS) – mastermind and overlord and acknowledges support from a Curtin Media Grant


Madelon Heperi (Curtin FLET) – programming, graphic design and teaching and learning design


Martin Towner (Curtin EPS) – drone pilot, cameraman, sound guy, field model, drone mosaic data processing


Aaron Cavosie (Curtin EPS) – geochemistry data and petrology wizard


Katy Evans (Curtin EPS) – teaching and learning design and acknowledges support from a Curtin Media Grant


Diana Taylor (Curtin FLET) – teaching and learning design


David Mole (CSRIO at the time) – whole geochemistry and sample collector and acknowledges support from the Science Plus Leader program of CSIRO


Chris Kirkland (Curtin EPS) – geochronology data collection and processing


Sean Makin (Curtin EPS) – drone pilot and data processing


Andrea Rajšic (Curtin EPS) – 360 camera operator, structural data collection and field model


Dave Belton (Curtin EPS) – areal 360 drone pilot and data processing


Tony Snow (Curtin EPS) – areal 360 drone co-pilot and assistant


Denis Fougerouse (Curtin EPS) – field model


Timmons Erickson (Curtin EPS, now at NASA) – sample collector


Steve Reddy (Curtin EPS) – sample collector
HTMLText_80703397_C35B_5579_41D1_33A43CF1C780.html =
Instructions


Bedding data


Download the spreadsheet of structural data and plot them on the base map for Locality 5.


HTMLText_80DE42D9_C35B_54E9_41D1_B133CE8CFF6C.html =
Instructions


Bedding data


Download the spreadsheet of structural data and plot them on the base map for Locality 5.


HTMLText_80DEC2E0_C35B_54D7_41B1_2143A941D645.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_83B4FBC9_CD7C_EFFC_41E6_3E3510160080.html =
Instructions


subtitle


Mauris aliquet neque quis libero consequat vestibulum. Donec lacinia consequat dolor viverra sagittis. Praesent consequat porttitor risus, eu condimentum nunc. Proin et velit ac sapien luctus efficitur egestas ac augue. Nunc dictum, augue eget eleifend interdum, quam libero imperdiet lectus, vel scelerisque turpis lectus vel ligula. Duis a porta sem. Maecenas sollicitudin nunc id risus fringilla, a pharetra orci iaculis. Aliquam turpis ligula, tincidunt sit amet consequat ac, imperdiet non dolor.


Donec feugiat:


• Nisl nec mi sollicitudin facilisis
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• Ut eget lorem sed leo.
• Sollicitudin tempor sit amet non
• Aliquam feugiat mauris sit amet.
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Instructions


Interpreting how rock are formed


Download the image and make an interpretive sketch of the pillows at this location, making particular note of domes and keels.


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Photo Album or image


This is a photo album / image template with download buttons.









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LOREM IPSUM


Mauris aliquet neque quis libero consequat vestibulum. Donec lacinia consequat dolor viverra sagittis. Praesent consequat porttitor risus, eu condimentum nunc. Proin et velit ac sapien luctus efficitur egestas ac augue. Nunc dictum, augue eget eleifend interdum, quam libero imperdiet lectus, vel scelerisque turpis lectus vel ligula. Duis a porta sem. Maecenas sollicitudin nunc id risus fringilla, a pharetra orci iaculis. Aliquam turpis ligula, tincidunt sit amet consequat ac, imperdiet non dolor.


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Instructions


Interpretation of formation environment


Download the sedimentary log and complete an interpretation of the environment of formation of the beds.
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360 VR Geological


This Virtual Geological Fieldtrip takes you to selected geological landmarks over two square kilometres of dry and harsh climate of Kalgoorlie Boulder, Western Australia.


With 360-degree panoramas, 3D photogrammetry, drone footage, microscopic images and datasheets this resource provides you with an array data required to carry out geological.


In the acitivy panoramas, select the level you would like to explore.


Credits


Curtin University
Faculty of Science and Engineering
Office of the Dean Teaching and Learning





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Instructions


Structural data and plot


Download the spreadsheet of the structural data and plot them on the base map Locality 2.
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Instructions


Download the spreadsheet of the structural data and plot them on the base map Locality 2.
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Instructions


Foliation data


Download the spreadsheet of structural data and plot them on the base map for Locality 5.


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Instructions


Foliation data


Download the spreadsheet of structural data and plot them on the base map for Locality 5.


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Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_96E241F0_B990_F783_41DC_60FD28B9E304.html =
Instructions



Interpretation of formation environment


Download the sedimentary log and complete an interpretation of the environment of formation of the beds.
HTMLText_9883C170_B8B0_9483_41BC_887D82714F78.html =
Instructions



Interpretation of formation environment


Download the sedimentary log and complete an interpretation of the environment of formation of the beds.
HTMLText_9A2B2EEB_B8B0_8D85_41DA_C3FA31A99E0E.html =
Instructions



Interpretation of formation environment


Download the sedimentary log and complete an interpretation of the environment of formation of the beds.
HTMLText_9A481CCE_CDB7_A9F4_41BA_ABEEF518AC1D.html =
Instructions


Step 1
Download the base map files for locality 8.


Step 2
Print the subdued colour base map to fit to an A3 page.


Step 3
Carefully trace the margins of as many pillows as you can observe at this locality. Tip – use the strong colour base map on a screen to zoom in to see the image in detail. Add line symbols to your legend.


Step 4
Use keel and dome shapes of mapped pillows to annotate your map with younging symbols in appropriate orientations, and add to the legend.


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Instructions


Step 1
Download the Base map files for locality 5.


Step 2
Find the data spreadsheets and plot data on the geology map.


Step 3
Infer bedrock geology boundaries through cover (scree and colluvium) on the geology map


Step 4
Infer any faults and large scale folds
HTMLText_A44D01C0_CD8C_7BEC_41E8_FC0E37626C56.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
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Instructions


Foliation data


Download the image and make an interpretive sketch of the pillows at this location, making particular note of domes and keels.


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Instructions for locality 1


Click the explore location 1 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
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Instructions for locality 1


Click the explore location 1 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_ADB0EFAC_CDFC_67B4_41DB_08D05E8D89CD.html =
Instructions


Download the spreadsheet of the structural data and plot them on the base map Locality 2.
HTMLText_AFD88AF3_CD95_A9AC_41E6_D965F41069E9.html =
Instructions


Interpreting how rock units formed


Download the image and make an interpretive sketch of the pillows at this location, making particular note of domes and keels.


HTMLText_AFDA1AF9_CD95_A99C_41D8_C7A890004229.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_B5A58B32_8030_A3D0_41DF_E338580D79AD.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality


HTMLText_BB3CB7DB_C2EF_5CE9_41AC_7F3655EACF18.html =
Instructions


Step 1
Download the Base map files for locality 5.


Step 2
Find the data spreadsheets and plot data on the geology map.


Step 3
Infer bedrock geology boundaries through cover (scree and colluvium) on the geology map


Step 4
Infer any faults and large scale folds











HTMLText_BD74265C_8073_E250_41D4_5A5FBABD0659.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_BE801F19_BB70_8C85_41D3_54AC77537042.html =
Instructions


Plotting structural data to download and plot


Download the spreadsheet of structural data and plot them on the base map for Locality 4 and a stereonet.
HTMLText_BE94C485_B891_FD8D_41C8_B7202B320F9A.html =
Instructions


These optical photomicrographs are from samples within 50m of this location.


Step 1
In a notebook, make petrographic descriptions of each sample, including mineralogy and texture, and identify rock types.


Step 2
Make interpretations about magmatic history, noting any possible petrogenetic links between the samples.


Step 3
Map the rock types on to the base map for this locality
HTMLText_BF307766_B990_9C8F_41B5_F2B8CDBC5E08.html =
Instructions


Structural data and plot


Download the spreadsheet of structural data and plot them on the base map for Locality 5.


HTMLText_BF3B0444_B990_7C83_41E3_338855844A47.html =
Instructions


Structural data and plot


Download the spreadsheet of structural data and plot them on the base map for Locality 5.


HTMLText_BF3B044B_B990_7C85_41D1_C006B0925AB7.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_C8133AC5_FD36_4C29_41D8_6A46CE980A97.html =
Instructions


These optical photomicrographs are from samples within 50m of this location.


Step 1
In a notebook, make petrographic descriptions of each sample, including mineralogy and texture, and identify rock types.


Step 2
Make interpretations about magmatic history, noting any possible petrogenetic links between the samples.


Step 3
Map the rock types on to the base map for this locality
HTMLText_CAB39B89_FD33_CC39_41E4_4A1DC4BABFF6.html =
Instructions


These optical photomicrographs are from samples within 50m of this location.


Step 1
In a notebook, make petrographic descriptions of each sample, including mineralogy and texture, and identify rock types.


Step 2
Make interpretations about magmatic history, noting any possible petrogenetic links between the samples.


Step 3
Map the rock types on to the base map for this locality
HTMLText_CDDD44E9_C48D_99BC_41E1_4DA778ED326B.html =
Instructions


Step 1
Download the base map files for locality 8.


Step 2
Print the subdued colour base map to fit to an A3 page.


Step 3
Carefully trace the margins of as many pillows as you can observe at this locality. Tip – use the strong colour base map on a screen to zoom in to see the image in detail. Add line symbols to your legend.


Step 4
Use keel and dome shapes of mapped pillows to annotate your map with younging symbols in appropriate orientations, and add to the legend.


HTMLText_CDE2203E_C4B7_9894_41D3_A68A4D26A3EE.html =
Instructions


Step 1
Download the base map files for locality 8.


Step 2
Print the subdued colour base map to fit to an A3 page.


Step 3
Carefully trace the margins of as many pillows as you can observe at this locality. Tip – use the strong colour base map on a screen to zoom in to see the image in detail. Add line symbols to your legend.


Step 4
Use keel and dome shapes of mapped pillows to annotate your map with younging symbols in appropriate orientations, and add to the legend.
HTMLText_CE17884C_FD32_4C3F_41E9_395E36FE252C.html =
Instructions



These optical photomicrographs are from samples within 50m of this location.


Step 1
In a notebook, make petrographic descriptions of each sample, including mineralogy and texture, and identify rock types.


Step 2
Make interpretations about magmatic history, noting any possible petrogenetic links between the samples.


Step 3
Map the rock types on to the base map for this locality.
HTMLText_DE3723A8_95E8_3EF7_41E2_120BC0DE0F67.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality


HTMLText_E2DAE97B_9EC2_8F40_41C5_956C80CFE2F6.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_E38766EF_9F7E_8540_41DB_FFEEA381D07B.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_E65110A3_9F43_9DC0_41D0_D96707610F81.html =
Instructions


Download the spreadsheets of structural data and plot them on the base map for locality 1.


HTMLText_E6C11502_9F42_84C0_41DD_7A529B6B5935.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_E6C344FC_9F42_8540_41DE_3B222EAAF757.html =
Instructions


Download the spreadsheets of structural data and plot them on the base map for locality 1.


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Localities


There are eight localities of interest with various tasks and activities covering a range of skill levels.


Select the locality below that you want to explore than select the skill set relevant to that locality.
HTMLText_E8057D40_80D0_67B0_41CA_3A38E159CD84_mobile.html =
Localities


There are eight localities of interest with various tasks and activities covering a range of skill levels.


Select the locality below that you want to explore than select the skill set relevant to that locality.
HTMLText_EA98A712_FD1E_D0D5_41E9_12CFAF9CC35E.html =
Instructions



These optical photomicrographs are from samples within 50m of this location.


Step 1
In a notebook, make petrographic descriptions of each sample, including mineralogy and texture, and identify rock types.


Step 2
Make interpretations about magmatic history, noting any possible petrogenetic links between the samples.


Step 3
Map the rock types on to the base map for this locality.
HTMLText_F43A2056_E1BE_7F95_41C8_545F3A3A6D5D.html =
Instructions for locality 3


Click the explore location 3 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_F43A2056_E1BE_7F95_41C8_545F3A3A6D5D_mobile.html =
Instructions for locality 3


Click the explore location 3 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
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A and C are correct.
This is consistent with observations and can be tested by field mapping.
htmlText_072670F6_0668_8C7C_4158_0E53EFE107EC.html =
Incorrect. A chilled margin of a pyroxenite should also be ultramafic.
htmlText_0726B0AA_0669_8C94_4196_F8C3CD0C48FA.html =
A and C are correct.
This is consistent with observations and can be tested by field mapping.
htmlText_0726EB11_0669_9DB4_4189_94AFAAF1D2A3.html =
While feasible, this would require a period of erosion before a basalt flow and is not the simplest explanation.
htmlText_07649F27_06E9_B59C_4177_F15E48181063.html =
A, B and C are correct.
htmlText_076506B6_06E8_94FC_4194_D1E1F5034190.html =
A, B and C are correct.
htmlText_07652CAC_06E8_94EC_417B_74A2E6DA2577.html =
A, B and C are correct.
htmlText_07656B28_06E8_9D94_417B_0E1BA83FE3EF.html =
Incorrect.
htmlText_0ABC2941_A1C2_8F40_41BB_2F1FAEDF49A7.html =
Incorrect, these rocks plot in dacite and trachyte fields, and across the trends for both sub-alkaline and alkaline series.
htmlText_0ABCC93F_A1C2_8CC0_41E2_8B83C661E677.html =
Correct, these rocks plot in dacite and trachyte fields, and across the trends for both sub-alkaline and alkaline series.
htmlText_0ABD0934_A1C2_8CC0_41BD_A5D8B06C9039.html =
Incorrect, extraction of melt from a garnet-rich source region leads to the depleted heavy REE in the melt when the garnet remains in the source region.
htmlText_0ABD193C_A1C2_8CC0_41E0_30FB8F5A78AC.html =
Correct, the answer is strongly light-REE enriched.
htmlText_0ABD793D_A1C2_8CC0_41CE_F2759397506A.html =
Incorrect, the answer is strongly light-REE enriched.
htmlText_0ABDA93A_A1C2_8CC0_41B9_94FD08FE4606.html =
Incorrect, the answer is strongly light-REE enriched.
htmlText_0ABDD933_A1C2_8CC0_41E2_229E47015FE6.html =
Correct, extraction of melt from a garnet-rich source region leads to the depleted heavy REE in the melt when the garnet remains in the source region.
htmlText_0ABDF942_A1C2_8F40_41D5_1184D7F1A3EE.html =
Incorrect, these rocks plot in dacite and trachyte fields, and across the trends for both sub-alkaline and alkaline series.
htmlText_0ABE192F_A1C2_8CC0_41DD_B63E6C641F28.html =
Incorrect, light REE become enriched in the melt by fractional crystallization because they are incompatible in most magmatic silicate phases.
htmlText_0ABE4938_A1C2_8CC0_41CF_6C1A618654F9.html =
Incorrect, the answer is strongly light-REE enriched.
htmlText_0ABE7931_A1C2_8CC0_41D6_62315A6070A0.html =
Incorrect, extraction of melt from a garnet-rich source region leads to the depleted heavy REE in the melt when the garnet remains in the source region.
htmlText_0ABED92D_A1C2_8CC0_41E0_5DEF318F99DB.html =
Incorrect, light REE become enriched in the melt by fractional crystallization because they are incompatible in most magmatic silicate phases.
htmlText_0ABEF936_A1C2_8CC0_41DB_4A786ED2EFE3.html =
Incorrect, extraction of melt from a garnet-rich source region leads to the depleted heavy REE in the melt when the garnet remains in the source region.
htmlText_0ABF692B_A1C2_8CC0_41D9_F8CB5E302DE5.html =
Correct, light REE become enriched in the melt by fractional crystallization because they are incompatible in most magmatic silicate phases.
htmlText_0ABFE929_A1C2_8CC0_41B4_9857A6029239.html =
Incorrect, light REE become enriched in the melt by fractional crystallization because they are incompatible in most magmatic silicate phases.
htmlText_0C842B91_A1C2_83C0_41D2_C6D887FC8A59.html =
Incorrect, even though the data indicate the zircon grains have lost Pb (recent) and have common Pb contamination (all to be expected in the Yilgarn Craton), the seven most concordant points yield ~2673 Ma, which is the best estimate of magmatic.
htmlText_0C844B90_A1C2_83C0_41CA_53BBC27D1B93.html =
Correct, even though the data indicate the zircon grains have lost Pb (recent) and have common Pb contamination (all to be expected in the Yilgarn Craton), the seven most concordant points yield ~2673 Ma, which is the best estimate of magmatic.
htmlText_0C852B8E_A1C2_83C0_41CE_E47576A97A16.html =
Incorrect, even though the data indicate the zircon grains have lost Pb (recent) and have common Pb contamination (all to be expected in the Yilgarn Craton), the seven most concordant points yield ~2673 Ma, which is the best estimate of magmatic.
htmlText_0C88CBA9_A1C2_83C0_41D1_AD33E2D27034.html =
Incorrect, recent Pb-loss causes data points to shift to the right, and contamination of common Pb shifts data points towards the common Pb isotopic composition in the top left. Data distribution indicated that zircon from this rock have been variable affected by both of these processes.
htmlText_0C896BA8_A1C2_83C0_41CE_1E0C5970C5FB.html =
Correct, recent Pb-loss causes data points to shift to the right, and contamination of common Pb shifts data points towards the common Pb isotopic composition in the top left. Data distribution indicated that zircon from this rock have been variable affected by both of these processes.
htmlText_0C89EBA6_A1C2_83C0_41D6_7A89601090DA.html =
Incorrect, recent Pb-loss causes data points to shift to the right, and contamination of common Pb shifts data points towards the common Pb isotopic composition in the top left. Data distribution indicated that zircon from this rock have been variable affected by both of these processes.
htmlText_0C8AAB9B_A1C2_83C0_41D5_EAFDBCC395D2.html =
Incorrect, ideally weighed mean ages have a MSWD = 1 and p = 1. The values of 0.65 and 0.69 are acceptable close to 1.
htmlText_0C8AEB99_A1C2_83C0_41CE_6A5F59E63587.html =
Correct, ideally weighed mean ages have a MSWD = 1 and p = 1. The values of 0.65 and 0.69 are acceptable close to 1.
htmlText_0C8B2BA1_A1C2_83C0_41C8_7FC662111E3C.html =
Correct, U/Pb has less precision than Pb/Pb for this range and also is susceptible to recent Pb loss. Therefore, Pb/Pb is better to use to calculate an age in this case.
htmlText_0C8B4B9F_A1C2_83C0_41D3_F89767B9F11C.html =
Incorrect, U/Pb has less precision than Pb/Pb for this range and also is susceptible to recent Pb loss. Therefore, Pb/Pb is better to use to calculate an age in this case.
htmlText_0C8B5B97_A1C2_83C0_41D6_36FAFD167D7F.html =
Incorrect, ideally weighed mean ages have a MSWD = 1 and p = 1. The values of 0.65 and 0.69 are acceptable close to 1.
htmlText_0F682FCB_BB90_8B85_41BC_2A9B68E317E3.html =
Incorrect, the answer is plagioclase
htmlText_0F685FC9_BB90_8B85_41C6_2A0BFB02780E.html =
Correct, the answer is plagioclase.
htmlText_0F688FCD_BB90_8B9D_41E6_A422EC7916B1.html =
Incorrect, the answer is plagioclase.
htmlText_0F69CFC8_BB90_8B83_41D6_391C6FB51D20.html =
Incorrect, the answer is plagioclase.
htmlText_166CA345_8031_E3B0_41D4_35050265D69C.html =
Correct, the dyke on the opposite side has moved to the left, which is a sinistral, or left lateral displacement” or for the incorrect answer.
htmlText_166CD344_8031_E3B0_41DB_0B22B5F0231D.html =
Incorrect, the dyke on the opposite side has moved to the left, which is sinistral, or left lateral displacement.
htmlText_166E1340_8031_E3B0_41C1_6F63371D74AB.html =
Correct, the dyke segments are discontinuous and separated from one another, i.e., sharply truncated and offset.
htmlText_166E2341_8031_E3B0_41A2_0233A9D5E54A.html =
Incorrect, the dyke segments are discontinuous and separated from one another, i.e., sharply truncated and offset.
htmlText_1BB97477_9EC6_8540_41E2_B4AB5C5AA50C.html =
Incorrect, for strike slip faults, sigma 2 is vertical, and sigma 1 and sigma 3 are oriented obliquely to the fault plane.
htmlText_1BB9A472_9EC6_8540_41D6_1E9979D21004.html =
Incorrect, for strike slip faults, sigma 2 is vertical, and sigma 1 and sigma 3 are oriented obliquely to the fault plane.
htmlText_1BB9D475_9EC6_8540_41E0_2587DBEA5AEE.html =
Correct, for strike slip faults, sigma 2 is vertical, and sigma 1 and sigma 3 are oriented obliquely to the fault plane.
htmlText_1D5A5763_8030_A270_41DB_EE51D928B10E.html =
Incorrect, red weathering typically indicates that the original rock was Fe-rich.
htmlText_1D5BF762_8030_A270_41DD_9DD33874BFF1.html =
This is correct, the answer is mafic.
htmlText_1FCC7ABE_8030_E2D0_41B5_A4EF303FFF04.html =
Correct, the answer is pyrite.
htmlText_1FCCBAC0_8030_E2B0_41DE_A1B4001F5037.html =
That is correct, the crystals forms are cube-shaped, and are therefore cubic.
htmlText_1FCD4AB5_8030_E2D0_41D7_67DD05138FE4.html =
Incorrect, the answer is pyrite.
htmlText_1FCDFAB7_8030_E2D0_41CE_0A6557B5865D.html =
Incorrect, the answer is pyrite.
htmlText_1FCE2AB3_8030_E2D0_41DC_38CEF0F8B5FD.html =
Incorrect, the answer is pyrite.
htmlText_1FD27AC1_8030_E2B0_41DD_F565C2E0E669.html =
Incorrect, the crystals forms are cube-shaped, and are therefore cubic.
htmlText_1FD34AC3_8030_E2B0_41C0_82E6D84A6B75.html =
Incorrect, the crystals forms are cube-shaped, and are therefore cubic.
htmlText_1FD3EAC5_8030_E2B0_41D4_69E404335564.html =
Incorrect, the crystals forms are cube-shaped, and are therefore cubic.
htmlText_21F7D5F9_B88F_9F85_41E4_4D345C6A4951.html =
Not correct, the answer is clinopyroxene.
htmlText_21F855F8_B88F_9F83_41E0_B6A9B77B51DD.html =
Correct, the answer is clinopyroxene.
htmlText_21F8C5F6_B88F_9F8F_41C4_70DF8DCB32B0.html =
Not correct, the answer is clinopyroxene.
htmlText_21F955F5_B88F_9F8D_41DF_AEC245805CC4.html =
Not correct, the answer is clinopyroxene.
htmlText_21F9C5F0_B88F_9F83_41E5_A9EA7EAD7CC8.html =
Not correct, the answer is orthopyroxene.
htmlText_21FA35EF_B88F_9F9D_41D6_808CAF865C22.html =
Not correct, the answer is orthopyroxene.
htmlText_21FA65F3_B88F_9F85_41E2_774AB4AC4CD2.html =
Correct, the answer is orthopyroxene.
htmlText_21FA95ED_B88F_9F9D_41E4_E33ED3FE9FA2.html =
Incorrect, the answer is porphyritic.
htmlText_21FAD5F2_B88F_9F87_41DE_D4F92C197B68.html =
Not correct, the answer is orthopyroxene.
htmlText_21FB05EC_B88F_9F83_41C0_93EE37D2BFC9.html =
Incorrect, the answer is porphyritic.
htmlText_21FBD5EB_B88F_9F85_41A0_471CC91DE26E.html =
Correct, the answer is porphyritic.
htmlText_21FC75E6_B88F_9F8F_41D0_0CC3012F05E7.html =
Incorrect, the answer is ultramafic.
htmlText_21FCE5E5_B88F_9F8D_41A4_2BCCA23C64E2.html =
Incorrect, the answer is ultramafic.
htmlText_21FCE5E9_B88F_9F85_41E2_E5DFE93B9F55.html =
Incorrect, the answer is porphyritic.
htmlText_21FD45E8_B88F_9F83_41DA_6266441CD611.html =
Correct, the answer is ultramafic.
htmlText_21FD75E4_B88F_9F83_41B2_9E391178652A.html =
Incorrect, the answer is ultramafic.
htmlText_21FDE5E2_B88F_9F87_41B1_3C8E37B80BFF.html =
Correct, the answer is porphyritic pyroxenite.
htmlText_21FE65E1_B88F_9F85_41B2_150CCECB0C61.html =
Not correct, the answer is porphyritic pyroxenite.
htmlText_21FEE5E0_B88F_9F83_41DE_0FD08208CB6E.html =
Not correct, the answer is porphyritic pyroxenite.
htmlText_21FF15DF_B88F_9FBD_41D3_78F78ABB1289.html =
Not correct, the answer is porphyritic pyroxenite.
htmlText_29552D81_C4F4_A86C_41D2_015013D09CF4.html =
Incorrect. The data do not plot on the volcanic arc array.
htmlText_295A7D80_C4F4_A86C_41DB_380656ADE410.html =
Correct. The data plot along a trend from N-MORB, suggesting some crustal contamination.
htmlText_295ACD7F_C4F4_A894_41E8_52AB22FB8C02.html =
Incorrect. The data plot along a trend from N-MORB, suggesting some crustal contamination.
htmlText_295ADD7D_C4F4_A894_41E1_1BE52FBCF5EF.html =
Incorrect. The data plot away from an OIB source.
htmlText_2CE44D5D_C4F4_6894_41C4_C551051F831A.html =
Correct.
htmlText_2CE46D5C_C4F4_6894_41C2_09FF16A8C8EA.html =
Incorrect. Pillows in this location are 30-60 cm across.
htmlText_2CE7BD5E_C4F4_6894_41DA_F201E20357C4.html =
Incorrect. Pillows in this location are 30-60 cm across.
htmlText_2CE7CD5D_C4F4_6894_41D8_0E90D380A968.html =
Incorrect. Pillows in this location are 30-60 cm across.
htmlText_2E805C25_C4F7_A8B4_41C9_93E4C7545326.html =
Incorrect. Pillow lavas are most commonly associated with subaqueous extrusion.
htmlText_2E82EC22_C4F7_A8AC_41C2_AF5E936ED503.html =
A is correct. Pillow lavas are most commonly associated with subaqueous extrusion.
htmlText_2E833C24_C4F7_A8B4_41AB_EAA5CF825F96.html =
Incorrect. Pillow lavas are most commonly associated with subaqueous extrusion.
htmlText_2E836C23_C4F7_A8AC_41D1_5A2DEDE9350B.html =
A is correct. Pillow lavas are most commonly associated with subaqueous extrusion.
B is correct, but less common than a subaqueous extrusion origin.
htmlText_2FCACBFF_C4F7_AF94_41E5_C7E58B21C503.html =
Incorrect. Pillows young towards the west.
htmlText_2FCAFC00_C4F7_A86C_418D_F681D7BFB780.html =
Incorrect. Pillows young towards the west.
htmlText_2FCB7C01_C4F7_A86C_41DA_757C5F2BEB1B.html =
Incorrect. Pillows young towards the west.
htmlText_2FCB9C02_C4F7_A86C_41B7_B14322E4808A.html =
Correct.
htmlText_48BA1AA6_BB91_958F_41DD_EE7252972F9D.html =
Not correct, the answer is: was extruded as lava that cooled rapidly.
htmlText_48BA1AA9_BB91_9585_41CD_B765992296B0.html =
Not correct, the answer is: was extruded as lava that cooled rapidly.
htmlText_48BB2AA8_BB91_9583_41C8_A94F29B5691B.html =
Not correct, the answer is: was extruded as lava that cooled rapidly.
htmlText_48BBEAA7_BB91_958D_41E6_945BFC42474E.html =
Correct, the answer is: was extruded as lava that cooled rapidly.
htmlText_49659C58_BB90_8C83_41C5_5BFCF2FAC322.html =
Not correct, the answer was extruded as lava that was supercooled from high temperatures.
htmlText_4965FC56_BB90_8C8F_41D0_D12E5106E54C.html =
Not correct, the answer was extruded as lava that was supercooled from high temperatures.
htmlText_49661C54_BB90_8C83_41CC_A33F8E1A2F57.html =
Correct, the answer was extruded as lava that was supercooled from high temperatures.
htmlText_4966BC5A_BB90_8C87_41E6_C050AC1C388C.html =
Not correct, the answer was extruded as lava that was supercooled from high temperatures.
htmlText_4A4C64DE_BB90_7DBF_41E7_6CC053DBF14A.html =
Not correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A4D24DB_BB90_7D85_41A1_E845AB78AEF1.html =
Not correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A4D64DD_BB90_7DBD_41E5_439AEB9D83BF.html =
Correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A4DB4DA_BB90_7D87_41D6_62F777DAE914.html =
Not correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A96599C_BB91_9783_41E6_FF57FCF1952A.html =
Not correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A97599B_BB91_9785_41DF_FA4EB1818E27.html =
Correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A978997_BB91_978D_41D9_33368C7FBD4D.html =
Not correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A97E999_BB91_9785_41E6_C33883D76C36.html =
Not correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4AFC1C31_BBF0_8C85_41E5_3FB6157A94A8.html =
Not correct, the answer is observed.
htmlText_4B383A51_BB91_B485_41CE_E16C7CC5482A.html =
Correct, is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4B38AA4F_BB91_B49D_41D8_2E90B8C56C18.html =
Not correct, is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4B3B0A4E_BB91_B49F_41D4_EC7079B5414A.html =
Not correct, is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4B3BDA52_BB91_B487_41C8_4E5D1B068203.html =
Not correct, is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4E7898F0_BB93_9583_41C1_D72279BCEF9A.html =
Not correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4E7938EF_BB93_959D_41E0_C9A6F97CA73B.html =
Correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4E7958EE_BB93_959F_41DA_79D821115275.html =
Not correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4E79E8ED_BB93_959D_41E2_A48DB701FE60.html =
Not correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_517671EC_BB90_B783_41A9_7CE1094B15D4.html =
Incorrect, the answer is a hyperbyssal intrusion.
htmlText_5176F1ED_BB90_B79D_41D8_85E4BA03BA80.html =
Correct, the answer is a hyperbyssal intrusion.
htmlText_517951EE_BB90_B79F_41BD_1994B6C338AE.html =
Incorrect, the answer is a hyperbyssal intrusion.
htmlText_517981EA_BB90_B787_41DB_726F90AB737D.html =
Incorrect, the answer is a hyperbyssal intrusion.
htmlText_53003052_BBF3_9484_41E6_F199F8F00851.html =
Not correct, the answer is observed.
htmlText_573820F2_BBF1_F584_41C1_CF4CCB8DB6A2.html =
Correct, the answer is observed.
htmlText_58B03D19_BBB1_8C85_41B6_463B5FC2AE9C.html =
Not correct, the answer is felsic porphyry.
htmlText_58B15D1B_BBB1_8C85_41D7_4863E5B85429.html =
Not correct, the answer is felsic porphyry.
htmlText_58B22D23_BBB1_8C85_41E7_AEA451F1D22D.html =
Not correct, the answer is it is felsic to intermediate in composition.
htmlText_58B24D1F_BBB1_8CBD_41D7_746922373B9E.html =
Not correct, the answer is porphyritic.
htmlText_58B29D1D_BBB1_8CBD_41E2_43CCFB7D2918.html =
Not correct, the answer is felsic porphyry.
htmlText_58B2CD1C_BBB1_8C83_41D6_9F1756F09C39.html =
Correct, the answer is felsic porphyry.
htmlText_58B34D2F_BBB1_8C9D_41BD_D343613F8EAD.html =
Correct, the answer is plagioclase.
htmlText_58B36D25_BBB1_8C8D_41E6_5711F04200A4.html =
Correct, the answer is it is felsic to intermediate in composition.
htmlText_58B37D21_BBB1_8C85_41BF_2730C6132BDA.html =
Not correct, the answer is porphyritic.
htmlText_58B39D24_BBB1_8C83_41E1_E13F562E368C.html =
Not correct, the answer is it is felsic to intermediate in composition.
htmlText_58B3AD20_BBB1_8C83_41D8_EAD45C581D0E.html =
Correct, the answer is porphyritic.
htmlText_58B47D2D_BBB1_8C9D_41DB_E4C0E4160570.html =
Not correct, the answer is plagioclase.
htmlText_58B4AD27_BBB1_8C8D_41C7_75C0B8742A19.html =
Not correct, the answer is plagioclase.
htmlText_58B4DD22_BBB1_8C87_41A2_6E342C9F53FC.html =
Not correct, the answer is porphyritic.
htmlText_58B5FD2E_BBB1_8C9F_41E4_E8E475A8DB97.html =
Not correct, the answer is plagioclase.
htmlText_5977A3D1_BBF0_7B85_41C7_5651A4E7B3C1.html =
Not correct, the answer is observed.
htmlText_60A718BB_BB8F_9585_41E2_09A3B94AC459.html =
Incorrect, the answer is N-S.
htmlText_60A7B8BA_BB8F_9587_41D6_FA52597F57F3.html =
Correct, the answer is N-S.
htmlText_60A848B8_BB8F_9583_41D9_7FA95AB8421A.html =
Incorrect, the answer is N-S.
htmlText_60A8A8B7_BB8F_958D_41CD_B21389C33BA0.html =
Incorrect, the answer is N-S.
htmlText_617115F5_BB8F_9F8D_41D4_9F22894CE63F.html =
Not correct, the answer is spinifex.
htmlText_6171B5F1_BB8F_9F85_41CB_259C8F1FE243.html =
Correct, the answer is spinifex.
htmlText_6171E5F3_BB8F_9F85_41DB_63092C25CEF8.html =
Not correct, the answer is spinifex.
htmlText_617275EA_BB8F_9F87_41D9_5878B880D18A.html =
Incorrect, the answer is spinifex basalt.
htmlText_617285EE_BB8F_9F9F_41DF_654E5CA00167.html =
Correct, the answer is spinifex basalt.
htmlText_6172D5E8_BB8F_9F83_41A0_0EA1AD25FA8A.html =
Incorrect, the answer is spinifex basalt.
htmlText_6172D5F0_BB8F_9F83_41C4_B29BF259FF2B.html =
Not correct, the answer is spinifex.
htmlText_617335EC_BB8F_9F83_41D8_7B48A33F25E9.html =
Incorrect, the answer is spinifex basalt.
htmlText_62A46AF0_BB91_9583_41E3_C59FA3D223F2.html =
Not correct, the answer is basalt.
htmlText_62A46AF2_BB91_9587_41A9_F85067E575D4.html =
Not correct, the answer is basalt.
htmlText_62A4FAEF_BB91_959D_41C1_4F3566346544.html =
Correct, the answer is basalt.
htmlText_62A7DAEE_BB91_959F_41C3_601410DCD533.html =
Not correct, the answer is basalt.
htmlText_63000B93_BB90_8B85_4191_D561A4DD8A45.html =
Correct, the answer is dolerite.
htmlText_63005B91_BB90_8B85_41DD_F11FBFB0CF41.html =
Not correct, the answer is dolerite.
htmlText_63012B90_BB90_8B83_41E6_91967EAFF62A.html =
Not correct, the answer is dolerite.
htmlText_63017B8E_BB90_8B9F_41B9_5F154D904873.html =
Not correct, the answer is dolerite.
htmlText_88307B11_C329_3579_41E6_81A2F80BE0D6.html =
Incorrect, the answer is: NW - SE.
htmlText_8830EB12_C329_357B_41DA_233CD0081044.html =
Correct, the answer is: NW - SE.
htmlText_88313B0E_C329_356B_41C1_E00F8657E018.html =
Incorrect, the answer is: NW - SE.
htmlText_8831BB0F_C329_3569_41E0_4AAC4AFCBCE0.html =
Incorrect, the answer is: NW - SE.
htmlText_8927F518_9B61_D797_417F_9183DBEAB30A.html =
Instructions:
These photos of several felsic dykes exposed within 300 m of this location.
Step 1
In a notebook, describe the mineralogy and texture of each sample, particularly the phenocryst, noting any similarities and/or differences.
Step 2
Make interpretations about the cooling history of these rocks.
htmlText_94A558D0_A994_EA7B_41B5_96350236D0A3.html =
Incorrect, the answer is felsic.
htmlText_94A5D8CE_A994_EA67_41C6_F7661FB9AE1B.html =
Correct, the answer is felsic
htmlText_94A628DB_A994_EA6D_41E4_7689D230ABEF.html =
Correct, the answer is quartz.
htmlText_94A6A8DA_A994_EA6F_41BB_9522282B227E.html =
Incorrect, the answer is quartz.
htmlText_94A6C8D1_A994_EA7D_41E1_0B660BB964A5.html =
Incorrect, the answer is felsic.
htmlText_94A6E8D8_A994_EA6B_41C6_E647747DB8B7.html =
Incorrect, the answer is quartz.
htmlText_94A758DD_A994_EA65_41DD_09048A3869CB.html =
Incorrect, the answer is quartz.
htmlText_94A778D7_A994_EA65_41D6_61BDE9366D49.html =
Incorrect, the answer is quartz.
htmlText_94A7C8D6_A994_EA67_41E0_18969319A1E6.html =
Incorrect, the answer is quartz.
htmlText_94A7D8D4_A994_EA7B_41E4_DDC34368D34D.html =
Correct, the answer is quartz
htmlText_94A7D8DC_A994_EA6B_41CF_E01F9979A202.html =
Incorrect, the answer is quartz.
htmlText_9E0215E7_A9B5_DA25_41C0_1DC7C97CE890.html =
Incorrect, they are felsic.
htmlText_9E0385E6_A9B5_DA24_41E5_169C17175B8F.html =
Correct, they are felsic.
htmlText_9E0425EC_A9B5_DA2B_41A2_208B138B2AF8.html =
Incorrect, the answer is thinly bedded.
htmlText_9E0445F0_A9B5_DA3B_41B6_37B8C95BD766.html =
Correct, the answer is finely laminated.
htmlText_9E0455EB_A9B5_DA2D_41B8_08102B9253F4.html =
Incorrect, the answer is thinly bedded.
htmlText_9E04A5ED_A9B5_DA25_41B1_72EA39BD2781.html =
Correct, the answer is thinly bedded.
htmlText_9E04C5F1_A9B5_DA3D_41CB_F170FB915B6E.html =
Incorrect, the answer is finely laminated.
htmlText_9E0505EE_A9B5_DA27_41DE_9B955114B73C.html =
Incorrect, the answer is finely laminated.
htmlText_9E0585EF_A9B5_DA25_41CC_4D97F07F0BB7.html =
Incorrect, the answer is finely laminated.
htmlText_9E05D5EA_A9B5_DA2F_41E3_F87710819BE5.html =
Incorrect, the answer is thinly bedded.
htmlText_9EC36034_B970_F483_41D7_E1137A034E28.html =
Correct, it requires flow to form an erosive base.
htmlText_9EC39036_B970_F48F_41DF_B78EEE6A7D09.html =
Incorrect, it requires flow to form an erosive base.
htmlText_9EC3F035_B970_F48D_41B6_94631E8DC909.html =
Incorrect, it requires flow to form an erosive base.
htmlText_9ECC2030_B970_F483_41D4_0EFF8A069C87.html =
Correct.
htmlText_9ECD902F_B970_F49D_41A7_B94E304DD1D7.html =
Incorrect, the answer is the blue symbol.
htmlText_A282235A_CD94_F89C_41DB_47C8793FCB78.html =
Incorrect. An igneous rock with this grain size is pegmatitic.
htmlText_A282235F_CD94_F894_41E5_823D0244BE53.html =
Incorrect. Intermediate rocks contain much less mafic materials.
htmlText_A282335E_CD94_F894_41C3_2186018FA612.html =
Incorrect. Felsic rocks contain much less mafic materials.
htmlText_A282735B_CD94_F89C_41D9_6FA10A7E74AB.html =
Incorrect. An igneous rock with this grain size is pegmatitic.
htmlText_A282F359_CD94_F89C_41DC_BD629BB09BDB.html =
Correct.
htmlText_A2838361_CD94_F8AC_41C3_8026F36B322A.html =
Incorrect. Ultramafic rocks contain much less plagioclase.
htmlText_A283A360_CD94_F8AC_41DD_369187A4EE86.html =
Correct.
htmlText_A283D35C_CD94_F894_41D5_721615633A28.html =
Incorrect. An igneous rock with this grain size is pegmatitic.
htmlText_A28D0356_CD94_F894_41DB_A3F493E8235D.html =
Incorrect. Dolerite is a medium grained mafic rock.
htmlText_A28D635D_CD94_F894_41D3_BCB7500B503B.html =
Correct.
htmlText_A28D7358_CD94_F89C_41E6_7853380A0A26.html =
Incorrect. This rock is gabbro, but pegmatitic gabbro is more suitable.
htmlText_A28D9355_CD94_F894_41D8_58104E232106.html =
Incorrect. Basalt is a fine grained mafic rock.
htmlText_A2BC00E0_CD94_99AC_41D6_A5C47FA6897B.html =
Incorrect. Gabbro also contains plagioclase feldspar.
htmlText_A2BC00E1_CD94_99AC_41E2_BBF2F85609D4.html =
Correct.
htmlText_A2BC80DF_CD94_9994_41D2_1081F9E2798C.html =
Incorrect. Peridotite also contains olivine.
htmlText_A2BD90E3_CD94_99AC_41DC_5F561BB7BB2B.html =
Incorrect. Dunite contains over 90% olivine.
htmlText_A2FC4CFF_CD94_A994_41D5_1755F8F3CA07.html =
Incorrect. The fracture surface is smooth and conchoidal.
htmlText_A2FCED02_CD94_A86C_41D6_3C4502250AAC.html =
Incorrect. The fracture surface is smooth and conchoidal.
htmlText_A2FCFD03_CD94_A86C_41D4_341C7A0C4CEC.html =
Incorrect. This rock type is darker than rhyolite.
htmlText_A2FD5D05_CD94_A874_41CD_212F94016E46.html =
Correct.
htmlText_A2FD8D04_CD94_A874_41DE_CA96F0069F6F.html =
Incorrect. This rock type is darker than dacite.
htmlText_A2FDCD00_CD94_A86C_41DC_C9D84E022C72.html =
Incorrect. The fracture surface is smooth and conchoidal.
htmlText_A2FDCD05_CD94_A874_41E5_9F816284D644.html =
Incorrect. This rock type is fine grained.
htmlText_A2FF6D01_CD94_A86C_41E3_DD5709C03D5A.html =
Correct. The fracture surface is smooth and conchoidal.
htmlText_A3844DB3_C56F_ECB9_41D0_3776CB541E9D.html =
Incorrect, the answer is younging to the west.
htmlText_A3848DB1_C56F_ECB9_41D8_7C034EE2DE82.html =
Incorrect, the answer is younging to the west.
htmlText_A384DDB2_C56F_ECBB_41E0_E04C052ABB11.html =
Incorrect, the answer is younging to the west.
htmlText_A3BB0DB0_C56F_ECB7_41E6_3941F2E77A6A.html =
Correct, the answer is younging to the west.
htmlText_A3C32EBD_C56F_2CA9_41BE_CC54B72BAF3B.html =
Incorrect. This doesn’t explain why all slides of pillows are laminated
htmlText_A3CC1EBB_C56F_2CA9_418A_8FA6D86AF0D9.html =
Incorrect. Tectonic deformation should cut across pillows, but laminations are always parallel to their margins.
htmlText_A3CC1EC1_C56F_2CD9_41DC_A6EE3C39B770.html =
Not correct, the answer is dark green, laminated.
htmlText_A3CC5EBC_C56F_2CAF_41CC_2C20A75EAB07.html =
Correct. Inflation of pillows causes quenching of a layered glassy skin when in contact with water.
htmlText_A3CC6EC2_C56F_2CDB_41DB_17EC8CA33F8A.html =
Correct, the answer is dark green, laminated.
htmlText_A3CC9EC0_C56F_2CD7_41C5_CE9EA7188FD6.html =
Not correct, the answer is dark green, laminated.
htmlText_A3CDFEC4_C56F_2CDF_41D5_F19952619F7C.html =
Not correct, the answer is dark green, laminated.
htmlText_A41A26DD_CD95_F994_41B3_45D8B3374AD5.html =
Incorrect. MH58 has a similar total alkali content.
htmlText_A41B46DC_CD95_F994_41E4_929B18A8FCA5.html =
Incorrect. MH58 has a similar SiO2 content.
htmlText_A41B56DB_CD95_F99C_41B7_2696D5B6D251.html =
Correct.
htmlText_A42426D8_CD95_F99C_41E4_B8223881547B.html =
Incorrect. MH58 is slightly enriched LREE and a negative Nb+Ta anomaly.
htmlText_A42486DA_CD95_F99C_41E3_87099CA157D7.html =
Incorrect. MH58 is slightly enriched LREE and a negative Nb+Ta anomaly.
htmlText_A42496D9_CD95_F99C_41B4_8F70C4DAB05F.html =
Correct.
htmlText_A424F6DE_CD95_F994_41D8_956E46BE8FA8.html =
Incorrect. MH58 has a similar silica and total alkali content.
htmlText_A425C6D7_CD95_F994_41E0_E4DF7921224D.html =
Incorrect. MH58 is slightly enriched LREE and a negative Nb+Ta anomaly.
htmlText_A450659D_CD95_9B94_41D2_A2843C2AB5B2.html =
Incorrect. Bladed and/or acicular is more appropriate.
htmlText_A451859C_CD95_9B94_41DC_68831FB61DAE.html =
Incorrect. Bladed and/or acicular is more appropriate.
htmlText_A451A59B_CD95_9B9C_41BD_A447F72DC1B6.html =
Correct. The answer is bladed, acicular.
htmlText_A4521598_CD95_9B9C_41E3_3659D8B9F841.html =
Correct. The answer is clinopyroxene.
htmlText_A4523597_CD95_9B94_4181_B32A6743D0A1.html =
Incorrect. Olivine does not form twins and has second order interference colours.
htmlText_A452C59E_CD95_9B94_41B0_4023728D1044.html =
Incorrect. Bladed and/or acicular is more appropriate.
htmlText_A452E599_CD95_9B9C_41E8_F05D5B462696.html =
Incorrect. Chlorite does not have third order interference colours.
htmlText_A452F59A_CD95_9B9C_41BC_8FE35662C0D3.html =
Incorrect. Chlorite does not have third order interference colours.
htmlText_A5989154_CD95_B894_41CE_B593E279D80B.html =
Correct. The answer is cumulate.
htmlText_A5991150_CD95_B8EC_41C6_6519CDA657EF.html =
Incorrect. The texture is not indicative of this process.
htmlText_A5992151_CD95_B8EC_41E8_38F8390EFB12.html =
Incorrect. The former pyroxene grains form a cumulate texture.
htmlText_A599A152_CD95_B8EC_41D3_9309AE08233E.html =
Incorrect. The former pyroxene grains form a cumulate texture.
htmlText_A599F153_CD95_B8EC_41D0_359B2035D389.html =
Incorrect. The former pyroxene grains form a cumulate texture.
htmlText_A59A2149_CD95_B8FC_41CB_CFC79D5EA965.html =
Incorrect. Quartz has first order interference colours.
htmlText_A59A214A_CD95_B8FC_41C5_BC9CB5B65F20.html =
Incorrect. Plagioclase has first order interference colours.
htmlText_A59A414E_CD95_B8F4_41D2_1E79C13DEE71.html =
Incorrect. The pyroxene crystals are distinct and have not intergrown.
htmlText_A59A914F_CD95_B8F4_41DB_E8032924F95C.html =
Incorrect. The crystals are too coarse grained for a rapidly quenched lava.
htmlText_A59AF14B_CD95_B8FC_41D6_BC2F67370C00.html =
Correct. Chlorite has anomalous interference colours and is a common greenschist facies metamorphic mineral in mafic rocks.
htmlText_A59B714C_CD95_B8F4_41E0_B9D8FE43078B.html =
Incorrect. Actinolite has second order interference colours.
htmlText_A59BC14D_CD95_B8F4_41A2_D226576A9AD6.html =
Correct. Solid pyroxene crystals precipitated from a fractioning magma sank and accumulated.
htmlText_A5E055F0_CD94_7BAC_41E6_96DA9DAEF50C.html =
Incorrect. These rock types do not define conformable layers.
htmlText_A5E185F2_CD94_7BAC_41C8_FC0518AE8671.html =
Incorrect. Basalt occurs bodies that are tens meters across that is not always in contact with pyroxenite.
htmlText_A5E1C5F1_CD94_7BAC_41E6_E951C9C36865.html =
Correct. Pyroxenite and gabbro both cross cut basalt.
htmlText_A5E6D5F3_CD94_7BAC_41E6_A0DBC390247D.html =
Incorrect. Basalt is cross cut pyroxenite, indicating that basalt is older than the pyroxenite.
htmlText_AC5891F2_C56F_54BB_41A3_4213426143F5.html =
Not correct, the answer is 60%.
htmlText_AC5911F6_C56F_54BB_41D1_36B5C21D90B5.html =
Not correct, the answer is 60%.
htmlText_AC59B1F5_C56F_54B9_41DF_24D9DF92A471.html =
Correct, the answer is 60%.
htmlText_AC59F1F3_C56F_54B9_41AF_A16AC48D7467.html =
Not correct, the answer is 60%.
htmlText_AC5E21E9_C56F_54A9_41D0_AD8C8EB58DD9.html =
Correct.They predominantly contain more feldspar and less mafic minerals.
htmlText_AC5F61EF_C56F_54A9_41C6_6A30750BFAA3.html =
Incorrect.They predominantly contain more feldspar and less mafic minerals.
htmlText_AC5FB1EB_C56F_54A9_41C7_012796F5D373.html =
Incorrect.They predominantly contain more feldspar and less mafic minerals.
htmlText_ACC013A6_C56E_D55B_41E4_1F6B0ECA213A.html =
Incorrect. Varioles could be globules and spherules felsic immiscible liquid. However, quenched immiscible liquid droplets should have sharp margins.
htmlText_ACC093A7_C56E_D559_41A0_417FB06A61F8.html =
Correct. Radiating crystals and indistinct margins are consistent with devitrification of volcanic glass
htmlText_ACC0D3A9_C56E_D4A9_41D0_F3D3B9D2EE9D.html =
Correct. Each variole has a radiating pattern of crystals, indicating radial growth from the variole cores.
htmlText_ACC0D3AE_C56E_D4AB_41C8_D4A2AEB95981.html =
Incorrect. Their irregular and indistinct margins suggest they formed by alteration rather than as primary objects.
htmlText_ACC173A3_C56E_D559_41CD_5A8E90C08763.html =
Incorrect. Varioles could be globules and spherules felsic immiscible liquid. However, quenched immiscible liquid droplets should have sharp margins.
htmlText_ACC1F3A4_C56E_D55F_41DA_A9BE35E95550.html =
Incorrect. Varioles could be globules and spherules felsic immiscible liquid. However, quenched immiscible liquid droplets should have sharp margins.
htmlText_ACC203B7_C56E_D4B9_41B2_C065E51D56C4.html =
Incorrect, they contain a microscopic spinifex texture that indicates supercooling of melt.
htmlText_ACC293B3_C56E_D4B9_41D6_A92EB2706C4C.html =
Incorrect, they contain a microscopic spinifex texture that indicates supercooling of melt.
htmlText_ACC2A3B4_C56E_D4BF_41E3_0AADE4E0D2F5.html =
Correct, they contain a microscopic spinifex texture that indicates supercooling of melt.
htmlText_ACC333B0_C56E_D4B7_41D9_05AC0F5017F2.html =
Correct. Their irregular and indistinct margins suggest they were formed by alteration rather than as primary objects.
htmlText_ACC363AA_C56E_D4AB_41E8_6D4E52D74534.html =
Incorrect. Each variole has a radiating pattern of crystals, indicating radial growth from the variole cores.
htmlText_ACCD53B5_C56E_D4B9_41C5_78AD058C947E.html =
Incorrect, they contain a microscopic spinifex texture that indicates supercooling of melt.
htmlText_AD66182F_C56E_F3A9_41A8_CD17DF7A54C7.html =
Incorrect. Felsic dykes are more enriched in LREE and depleted HREE than the variolitic sample.
htmlText_AD668831_C56E_F3B9_41DB_1F63C86F998F.html =
Incorrect. Plagiogranite are more enriched in all trace elements relative to the variolitic sample.
htmlText_AD67382D_C56E_F3A9_4191_DC64D5639500.html =
Incorrect. Ultramafics tend to be more depleted than the variolitic sample.
htmlText_AD67B82E_C56E_F3AB_41D7_BE5DABA642A8.html =
Correct. The variolitic sample has a similar trace element distribution to other mafic rocks in the area.
htmlText_AE6988F9_B890_9585_41E7_08789708AF10.html =
Incorrect, the answer is flattening due to compaction in a hot volcanic ash flow.
htmlText_AE6A1900_B890_9483_419A_A36C77EE9360.html =
Incorrect, the answer is fine grained felsic.
htmlText_AE6AF8FA_B890_9587_41CA_B35C3E79FDFB.html =
Incorrect, the answer is flattening due to compaction in a hot volcanic ash flow.
htmlText_AE6AF8FB_B890_9585_41C3_F914EF13BA16.html =
Correct, the answer is flattening due to compaction in a hot volcanic ash flow.
htmlText_AE6B28FE_B890_957F_41BE_FDF66B65C8FC.html =
Incorrect, the answer is fine grained felsic.
htmlText_AE6B7901_B890_9485_41B4_E81950D0A9E8.html =
Correct, the answer is fine grained felsic.
htmlText_AE6B98FF_B890_957D_41E4_8F2142AE25C9.html =
Incorrect, the answer is fine grained felsic.
htmlText_BDF72EB5_A995_6625_41AB_E027634895EF.html =
Instructions
These optical photomicrographs are from several porphyritic felsic dykes exposed within 300 m of this location.
Step 1
In a notebook, make petrographic descriptions of each sample, including mineralogy and texture of the groundmass and phenocrysts.
Step 2
Make interpretations about magnetic history, noting any possible petrogenetic links between the dykes.
htmlText_BE9FC433_B88F_FC85_41E7_68E740BFB3B0.html =
Correct, the answer is garnet.
htmlText_BE9FC435_B88F_FC8D_41E6_0953992BA3B8.html =
Incorrect, the answer is garnet.
htmlText_BE9FC437_B88F_FC8D_41D9_5F66CBD61C22.html =
Incorrect, the answer is garnet.
htmlText_BE9FC439_B88F_FC85_41D7_14668FCFC366.html =
Incorrect, the answer is garnet.
htmlText_BE9FC43B_B88F_FC85_41AA_7ECAD73C5522.html =
Correct, the answer is MH55 has significantly depleted HREE and a stronger negative NB+Ta anomaly.
htmlText_BE9FC43D_B88F_FCFD_41C3_DC00A06BA37D.html =
Incorrect, the answer is MH55 has significantly depleted HREE and a stronger negative NB+Ta anomaly.
htmlText_BE9FC43E_B88F_FCFF_41E7_A47ECA518437.html =
Incorrect, the answer is MH55 has significantly depleted HREE and a stronger negative NB+Ta anomaly.
htmlText_BE9FC440_B88F_FC83_41E2_648EEE977C2D.html =
Incorrect, the answer is MH55 has significantly depleted HREE and a stronger negative NB+Ta anomaly.
htmlText_BE9FC442_B88F_FC87_41E5_8671EE23250C.html =
Incorrect, the answer is: MH15, MH14, MH20, MH55, MH56
htmlText_BE9FC444_B88F_FC83_41DD_2FAFA933F4F1.html =
Correct, the answer is: MH15, MH14, MH20, MH55, MH56
htmlText_BE9FC446_B88F_FC8F_41DB_B7A66BF80951.html =
Incorrect, the answer is: MH15, MH14, MH20, MH55, MH56
htmlText_BE9FC447_B88F_FC8D_41E5_FA636E26A2C1.html =
Incorrect, the answer is: MH15, MH14, MH20, MH55, MH56
htmlText_BEA1F33A_B8B3_9487_41C7_149E8F3C9B25.html =
Not correct, the correct answer is: MH15, MH14, MH20, MH55, MH56.
htmlText_BEA1F33B_B8B3_9485_41C8_D921E59534E7.html =
Correct, the correct answer is: MH15, MH14, MH20, MH55, MH56.
htmlText_BEA1F33D_B8B3_94FD_41AF_F6D4AC2944A9.html =
Not correct, the correct answer is: MH15, MH14, MH20, MH55, MH56.
htmlText_BEA1F33E_B8B3_94FF_41D5_64456D9A6098.html =
Not correct, the correct answer is: MH15, MH14, MH20, MH55, MH56.
htmlText_BEA1F340_B8B3_9483_41DA_51867C7E4210.html =
Not correct, the answer is they do not contain alkali-bearing minerals.
htmlText_BEA1F341_B8B3_9485_4198_E7DC0C6AAE82.html =
Correct, the answer is they do not contain alkali-bearing minerals.
htmlText_BEA1F343_B8B3_9485_41E1_0D18352020F8.html =
Not correct, the answer is they do not contain alkali-bearing minerals.
htmlText_BEA1F344_B8B3_9483_41E6_13411A84DAAF.html =
Not correct, the answer is they do not contain alkali-bearing minerals.
htmlText_BEE2D25A_B8B1_9487_41E0_35AE1EDBE835.html =
Correct, therefore the dyke is younger than the tectonic foliation.
htmlText_BEE2D25B_B8B1_9485_41CF_182811CA139F.html =
Not correct.
htmlText_BEE2D25F_B8B1_94BD_41C3_FB21EB8DD4AA.html =
Not correct, the answer is: Striking E-W, dipping steeply N.
htmlText_BEE2D260_B8B1_9483_41DB_3C877067B432.html =
Not correct, the answer is: Striking E-W, dipping steeply N.
htmlText_BEE2D261_B8B1_9485_41C6_15EB0866E3F8.html =
Correct, the answer is: Striking E-W, dipping steeply N.
htmlText_BEE2D263_B8B1_9485_41E3_6345FE8AD78B.html =
Not correct, the answer is: Striking E-W, dipping steeply N.
htmlText_BEE50F84_B8B0_8B83_41E1_39791A333FF9.html =
Not correct, the answer is steeply dipping W.
htmlText_BEE50F86_B8B0_8B8F_41D5_D678CF496DC1.html =
Not correct, the answer is steeply dipping W.
htmlText_BEE50F87_B8B0_8B8D_41E0_FA46E1BAE1C6.html =
Not correct, the answer is steeply dipping W.
htmlText_BEE50F89_B8B0_8B85_41E2_CF0B7CBB4EC3.html =
Correct, the answer is steeply dipping W.
htmlText_BF09034E_B970_749F_41D6_F86DA80E2EB9.html =
Incorrect, the correct answer is sub-vertical.
htmlText_BF09034F_B970_749D_41E1_4AC0F4F29822.html =
Correct, the answer is sub-vertical.
htmlText_BF090350_B970_7483_41CF_E3467E13D6B7.html =
Incorrect, the correct answer is sub-vertical.
htmlText_BF090352_B970_7487_41B7_6661C531C6C7.html =
Incorrect, the correct answer is sub-vertical.
htmlText_BF090353_B970_7485_41B3_4B452F641D94.html =
Not correct. The answer is foliated.
htmlText_BF090354_B970_7483_4162_6EDDF958FA09.html =
Not correct. The answer is foliated.
htmlText_BF090356_B970_748F_41E5_F5B76DAC0B02.html =
Not correct. The answer is foliated.
htmlText_BF090357_B970_748D_41D2_A6611CFD7169.html =
Correct. The answer is foliated.
htmlText_BF1A1E33_B990_8C85_41BE_38122BAA9117.html =
Incorrect, the answer is close.
htmlText_BF1A1E36_B990_8C8F_4195_F423829BECBA.html =
Incorrect, the answer is close.
htmlText_BF1A1E38_B990_8C83_41DB_5A2BC3047540.html =
Correct, the answer is close.
htmlText_BF1A1E39_B990_8C85_41E0_854BD29054CC.html =
Incorrect, the answer is close.
htmlText_BF1A1E3C_B990_8C83_41DA_048C84EAB3CD.html =
Incorrect, the answer is vertical.
htmlText_BF1A1E3D_B990_8CFD_41B9_362B6F0CEB12.html =
Incorrect, the answer is vertical.
htmlText_BF1A1E3F_B990_8CFD_41D9_40450BE2EAE7.html =
Incorrect, the answer is vertical.
htmlText_BF1A1E41_B990_8C85_41E5_37542D83A3DC.html =
Correct, the answer is vertical.
htmlText_BF1A1E43_B990_8C85_41E6_0D539C83AAAF.html =
Incorrect, the answer is vertical.
htmlText_BF1A1E45_B990_8C8D_41D5_7CE1A38AFB01.html =
Incorrect, the answer is vertical.
htmlText_BF1A1E47_B990_8C8D_41CA_EA61EFF1E11D.html =
Incorrect, the answer is vertical.
htmlText_BF1A1E48_B990_8C83_41DC_DB43B3D22E59.html =
Correct, the answer is vertical.
htmlText_BF1A1E4A_B990_8C87_4180_854E3CD29B90.html =
Correct, the answer is NW-SE.
htmlText_BF1A1E4C_B990_8C83_41C9_488BD9B8DA84.html =
Not correct, the answer is NW-SE.
htmlText_BF1A1E4E_B990_8C9F_41DA_E399A94C1153.html =
Not correct, the answer is NW-SE.
htmlText_BF1A1E50_B990_8C83_41E0_5FC05DDE747A.html =
Not correct, the answer is NW-SE.
htmlText_BF1A3ECB_B990_8D85_41CB_D58C4886C39D.html =
Incorrect, the answer is: NW-SE.
htmlText_BF1A3ECD_B990_8D9D_41E3_BFE933755875.html =
Incorrect, the answer is: NW-SE.
htmlText_BF1A3ECF_B990_8D9D_41E0_80966F5CEAE0.html =
Incorrect, the answer is: NW-SE.
htmlText_BF1A3ED0_B990_8D83_41D3_33493B8A1E38.html =
Correct, the answer is: NW-SE.
htmlText_BF1A3ED2_B990_8D87_41D6_06E832C61203.html =
Not correct, the answer is spaced axial planar cleavage.
htmlText_BF1A3ED4_B990_8D83_41D2_6635EB6C8CDC.html =
Correct, the answer is spaced axial planar cleavage.
htmlText_BF1A3ED6_B990_8D8F_4171_A8BEFD87C12B.html =
Not correct, the answer is spaced axial planar cleavage.
htmlText_BF1A3ED7_B990_8D8D_41C3_D5BB6157D61F.html =
Not correct, the answer is spaced axial planar cleavage.
htmlText_BF1A567B_B990_9C85_41B8_107765DF193C.html =
Not correct, the answer is tight.
htmlText_BF1A567D_B990_9D7D_41E1_D276998888AB.html =
Not correct, the answer is tight.
htmlText_BF1A567F_B990_9D7D_41E2_00F23A246BED.html =
Not correct, the answer is tight.
htmlText_BF1A5681_B990_9D85_41D0_6CACFE99E55D.html =
Correct, the answer is tight.
htmlText_BF1A5683_B990_9D85_41E6_A6EE5997DD90.html =
Not correct, the correct answer is 15 degrees.
htmlText_BF1A5685_B990_9D8D_41AB_9C791035FBFC.html =
Not correct, the correct answer is 15 degrees.
htmlText_BF1A5687_B990_9D8D_41E7_DB79819DEC6E.html =
Not correct, the correct answer is 15 degrees.
htmlText_BF1A5688_B990_9D83_41C0_16F691DC2E45.html =
Correct, the answer is 15 degrees.
htmlText_BF1A568A_B990_9D87_41D9_1D3434FD5F94.html =
Incorrect, the answer is NW - SE.
htmlText_BF1A568C_B990_9D83_41BE_FE0D6A3EB42C.html =
Incorrect, the answer is NW - SE.
htmlText_BF1A568E_B990_9D9F_41C0_35F4ECD6F732.html =
Incorrect, the answer is NW - SE.
htmlText_BF1A5690_B990_9D83_41D6_C144FE17C99E.html =
Correct, the answer is NW - SE.
htmlText_C0B06514_AB6D_FBFB_41E3_36F3EE1DEB9C.html =
Incorrect, the correct answer is cross bedding.
htmlText_C0B09515_AB6D_FBE5_41B7_6C9B23D6D205.html =
Correct, the correct answer is cross bedding.
htmlText_C0B09516_AB6D_FBE7_41C2_FA569028465F.html =
Incorrect, the correct answer is cross bedding.
htmlText_C0B1E512_AB6D_FBFF_4189_85BF62C4711F.html =
Incorrect, the correct answer is cross bedding.
htmlText_C0B3B519_AB6D_FBED_41E0_056D25269D1C.html =
Correct, the correct answer is the blue symbol.
htmlText_C0B3F518_AB6D_FBEB_41C6_856F8227C243.html =
Incorrect, the correct answer is the blue symbol.
htmlText_C1C14825_AA93_EA25_41E1_9AA07AC4B7DC.html =
Incorrect, the answer is a fault.
htmlText_C1C18836_AA93_EA27_41DC_888D320F336E.html =
Correct, the answer is NW-SE.
htmlText_C1C1A82E_AA93_EA27_41E4_B962856321D5.html =
Incorrect, the answer is a fault.
htmlText_C1C1C82A_AA93_EA2F_41E4_C5AB57B625A1.html =
Incorrect, the answer is a fault.
htmlText_C1C1E82C_AA93_EA2B_41D7_4CFDE36FE41A.html =
Correct, the answer is a fault.
htmlText_C1C21830_AA93_EA3B_41B9_87039663E230.html =
Incorrect, the answer is NW-SE.
htmlText_C1C2B833_AA93_EA3D_41E2_65C472C3C9D6.html =
Incorrect, the answer is NW-SE.
htmlText_C1C2D831_AA93_EA3D_41DE_AF4181EFF356.html =
Incorrect, the answer is NW-SE.
htmlText_C540E745_B991_BC8D_41C3_91E015608BAB.html =
Correct, the answer is tectonic deformation.
htmlText_C541A746_B991_BC8F_41E6_F3657F15F596.html =
Not correct, the answer is tectonic deformation.
htmlText_C5477744_B991_BC83_41E1_45E55DD1D987.html =
Not correct, the answer is tectonic deformation.
htmlText_C5477747_B991_BC8D_41E3_B299433EB941.html =
Not correct, the answer is tectonic deformation.
htmlText_CC4E7F12_B9B0_8C87_41CB_E6E3BFC4634F.html =
Not correct, the answer is 43 degrees NE.
htmlText_D43796E3_B9B0_7D85_41DA_713F005E7EB6.html =
Correct, the answer is 43 degrees NE.
htmlText_D45C3710_B990_7C83_41DB_FF8E2DA8B3FC.html =
Incorrect, the correct answer is 029.
htmlText_D45C6711_B990_7C85_41DD_D741BC11B737.html =
Incorrect, the correct answer is 7cm.
htmlText_D45C8714_B990_7C83_41AA_189D23212186.html =
Incorrect, the correct answer is 7cm.
htmlText_D45CB70E_B990_7C9F_41D0_45FD85CD5280.html =
Incorrect, the correct answer is 029.
htmlText_D45D670D_B990_7C9D_41E0_53D532DF1B1A.html =
Correct, the correct answer is 029.
htmlText_D45D970C_B990_7C83_41CA_6193C092F17B.html =
Incorrect, the correct answer is 029.
htmlText_D45DF713_B990_7C85_41DC_31F1714F80B4.html =
Correct, the correct answer is 7cm.
htmlText_D5448445_B9B0_9C8D_41E2_0EF2E0E9447E.html =
Not correct, the answer is 43 degrees NE.
htmlText_D69328AC_B9B1_9583_41DA_E758291FA058.html =
Not correct, the answer is 43 degrees NE.
htmlText_DD283E1B_C3E9_2F69_41E0_4CCD3DECB15C.html =
Correct, the correct answer is N-S.
htmlText_DD288E1C_C3E9_2F6F_41E0_EEA7F8E57948.html =
Incorrect, the correct answer is N-S.
htmlText_DD289E1D_C3E9_2F69_41D8_178B08FF9578.html =
Incorrect, the correct answer is N-S.
htmlText_DD28BE16_C3E9_2F7B_41E3_136DC487B936.html =
Incorrect, the answer is folding involved layer-parallel shearing.
htmlText_DD28EE18_C3E9_2F77_41E4_5B094272C749.html =
Correct, the answer is folding involved layer-parallel shearing.
htmlText_DD29DE1A_C3E9_2F6B_4197_8123D6D19949.html =
Incorrect, the answer is folding involved layer-parallel shearing.
htmlText_DD364E21_C3E9_2F59_41C2_03DE992321E1.html =
Correct, the answer is box folds.
htmlText_DD36DE22_C3E9_2F5B_41E1_88A82DA4B16D.html =
Not correct, the answer is box folds.
htmlText_DD374E19_C3E9_2F69_41D6_6C0A5E398E5C.html =
Incorrect, the answer is folding involved layer-parallel shearing.
htmlText_DD375E1F_C3E9_2F69_41E2_0552EEE72471.html =
Not correct, the answer is box folds.
htmlText_DD376E1E_C3E9_2F6B_41DE_DEAC5A30A2B4.html =
Incorrect, the correct answer is N-S.
htmlText_DD37DE20_C3E9_2F57_41E2_785975DBD4B6.html =
Not correct, the answer is box folds.
htmlText_DD40DC93_C3E9_7379_41E5_D79C1AEF8B0F.html =
Incorrect, the answer is: focus on mapping rock types, ductile and brittle structures, and alteration, especially near known old workings.
htmlText_DD461C98_C3E9_7377_41BF_46626466B7F7.html =
Incorrect.
All answers are correct.
Check historical records with the shire and/or Department of Mines Industry Regulation and safety
Make a detailed geological field map of the area to develop and test the hypotheses
Take samples from old workings and analyse them in the laboratory
Read academic literature on gold mineralization in the region
htmlText_DD474C95_C3E9_7379_41E2_CE1D24557F9B.html =
Incorrect, the answer is: focus on mapping rock types, ductile and brittle structures, and alteration, especially near known old workings.
htmlText_DD475C94_C3E9_737F_41CB_2049DF739CCA.html =
Incorrect, the answer is: focus on mapping rock types, ductile and brittle structures, and alteration, especially near known old workings.
htmlText_DD475C99_C3E9_7369_41DC_520373F47FA5.html =
ncorrect.
All answers are correct.
Check historical records with the shire and/or Department of Mines Industry Regulation and safety
Make a detailed geological field map of the area to develop and test the hypotheses
Take samples from old workings and analyse them in the laboratory
Read academic literature on gold mineralization in the region
htmlText_DD477C9A_C3E9_736B_41D1_10B330A04525.html =
Incorrect.
All answers are correct.
Check historical records with the shire and/or Department of Mines Industry Regulation and safety
Make a detailed geological field map of the area to develop and test the hypotheses
Take samples from old workings and analyse them in the laboratory
Read academic literature on gold mineralization in the region
htmlText_DD479C97_C3E9_7379_41E1_B736CF8E530A.html =
Incorrect.
All answers are correct.
Check historical records with the shire and/or Department of Mines Industry Regulation and safety
Make a detailed geological field map of the area to develop and test the hypotheses
Take samples from old workings and analyse them in the laboratory
Read academic literature on gold mineralization in the region
htmlText_DD47FC96_C3E9_737B_41D5_C3769B9E6918.html =
Correct, the answer is: focus on mapping rock types, ductile and brittle structures, and alteration, especially near known old workings.
htmlText_DDE46039_C3E9_53A9_41C6_D7446C6BA45E.html =
Incorrect, the answer is sedimentary layers deposited, then folded and foliated, then intruded by a felsic dyke.
htmlText_DDE4803A_C3E9_53AB_41AC_0EDECBCBD9A3.html =
Correct, the answer is sedimentary layers deposited, then folded and foliated, then intruded by a felsic dyke.
htmlText_E34CE914_B9F0_B483_41E5_27E21A1BDB2D.html =
Correct, the correct answer is: ‘z’ folds.
htmlText_E34D9916_B9F0_B48F_41DC_04AD4CC7B1E4.html =
Incorrect, the correct answer is: ‘z’ folds.
htmlText_E34DC917_B9F0_B48D_41D6_F88B378D7431.html =
Incorrect, the correct answer is: ‘z’ folds.
htmlText_E34DD91E_B9F0_B4BF_415D_BF40CADC23F6.html =
Not correct, the answer is NW-SE.
htmlText_E34EE91A_B9F0_B487_41E1_2BEC6C05FCBE.html =
Not correct, the answer is NW-SE.
htmlText_E34EE91C_B9F0_B483_41C1_A8A3D6E99FB1.html =
Not correct, the answer is NW-SE.
htmlText_E34F491D_B9F0_B4BD_41C2_BB9FA89FF82C.html =
Correct, the answer is NW-SE.
htmlText_E470CC4D_B9F1_8C9D_41D4_6175AE6EF922.html =
Incorrect, the correct answer is the red symbol.
htmlText_E47F4C4B_B9F1_8C85_41E4_10957F6791DF.html =
The red symbol is the correct answer.
htmlText_E79039E0_B9F0_F783_41E6_9A0F84F597C3.html =
Incorrect, the answer is NW-SE.
htmlText_E790B9E2_B9F0_F787_41D0_22F6A7EC6986.html =
Correct, the answer is NW-SE.
htmlText_E79199DE_B9F0_F7BF_41BE_D8FC6E7E3B33.html =
Incorrect, the answer is NW-SE.
htmlText_E791B9E4_B9F0_F783_41DC_98878D1840C2.html =
Incorrect, the answer is NW-SE.
htmlText_EA841517_A41B_3870_41C9_A37241C74E5E.html =
Incorrect, the dyke discontinues into aligned segments arranged in an overlapping stepwise manner known as ‘an echelon’. Each segment is narrows to a tip.
htmlText_EA841518_A41B_3870_41D5_DF98DB1640D2.html =
Correct, the dyke discontinues into aligned segments arranged in an overlapping stepwise manner known as ‘an echelon’. Each segment is narrows to a tip.
htmlText_EA84E516_A41B_3870_41D0_0E82C9A3BE82.html =
Incorrect, the dyke discontinues into aligned segments arranged in an overlapping stepwise manner known as ‘an echelon’. Each segment is narrows to a tip.
htmlText_EA86E63D_C32B_3FA9_4196_14ADA96EECDD.html =
Correct!
All answers are correct.
Check historical records with the shire and/or Department of Mines Industry Regulation and safety
Make a detailed geological field map of the area to develop and test the hypotheses
Take samples from old workings and analyse them in the laboratory
Read academic literature on gold mineralization in the region
htmlText_EA8A2288_A41B_5850_41C2_39D7F5167080.html =
Incorrect, dykes open parallel to the least compressive stress (sigma 3) direction. Here, sigma 3 much be ESE-WNW – perpendicular to the dyke margin.
htmlText_EA8A6287_A41B_5850_41A4_17C5B647AC2B.html =
Incorrect, dykes open parallel to the least compressive stress (sigma 3) direction. Here, sigma 3 much be ESE-WNW – perpendicular to the dyke margin.
htmlText_EA8B1285_A41B_5850_41D4_A9526617E6F1.html =
Correct, dykes open parallel to the least compressive stress (sigma 3) direction. Here, sigma 3 much be ESE-WNW – perpendicular to the dyke margin.
htmlText_EA8D0542_A41B_38D0_41A6_228771AF56B8.html =
Incorrect, the contact is sharp.
htmlText_EA8D2540_A41B_38D0_41E4_2F2B330ACB08.html =
Correct, well done.
htmlText_EA8E353E_A41B_38B0_41B9_48E6325BF2F5.html =
Incorrect, the contact is sharp.
htmlText_EA8EA53F_A41B_38B0_41D9_9886FE6EE0FF.html =
Incorrect, the contact is sharp.
htmlText_EA906545_A41B_38D0_41E1_7C0ECD6D5409.html =
Incorrect, the dyke discontinues into aligned segments arranged in an overlapping stepwise manner known as ‘an echelon’. Each segment is narrows to a tip.
htmlText_EA906546_A41B_38D0_41DA_6E943FE7997B.html =
Although slightly variable, overall, the contract trends NE-SW.
htmlText_EA90D548_A41B_38D0_41E0_43E3B748E48A.html =
Although slightly variable, overall, the contract trends NE-SW.
htmlText_EA91F544_A41B_38D0_41E3_B6C078DCB9A6.html =
Although slightly variable, overall, the contract trends NE-SW.
htmlText_EB9AAF19_AAAC_E7ED_41E4_AAEAD354ECF3.html =
Incorrect, the answer is 87 degrees northeast.
htmlText_EB9C0F14_AAAC_E7FB_41D1_8B3F43650319.html =
Incorrect, the answer is 156 or 336.
htmlText_EB9C0F15_AAAC_E7E5_41D7_AB1BE778C0B5.html =
Incorrect, the answer is 156 or 336.
htmlText_EB9C2F1B_AAAC_E7ED_41DE_B2817D7FBC1C.html =
Incorrect, the answer is 87 degrees northeast.
htmlText_EB9CDF13_AAAC_E7FD_41B1_4615CBCC02F0.html =
Incorrect, the answer is 156 or 336.
htmlText_EB9D3F18_AAAC_E7EB_41C4_A3F9599B7233.html =
Incorrect, the answer is 87 degrees northeast.
htmlText_EB9D6F17_AAAC_E7E5_41BC_229DE1DFFB2A.html =
Correct, the answer is 87 degrees northeast.
htmlText_EB9FAF11_AAAC_E7FD_41E0_7C7A6601F90A.html =
Correct, the answer is 156 or 336.
htmlText_F12DB84A_F403_47EB_41E1_8B287A9FE485.html =
Incorrect, the answer is porphyritic dolerite.
htmlText_F12E3496_F401_4F7B_41E9_4B7FA79B538D.html =
Incorrect, the answer is porphyritic dolerite.
htmlText_F12E5539_F401_C9A9_41D1_CB0682C11645.html =
Correct, the answer is porphyritic dolerite.
htmlText_F12E78DD_F401_B8E9_41D8_10146550897F.html =
Incorrect, the answer is porphyritic dolerite.
htmlText_F2227949_F401_B9E9_41D8_E541A33BE110.html =
Possibly. To test this hypothesis, other geochemical signatures of sedimentary input could be examined.
htmlText_F224F267_F402_CBD9_41D2_CDAAF0D7C05F.html =
Possibly. To test this hypothesis, other geochemical signatures of sedimentary input could be examined.
htmlText_F2252C10_F403_5F77_41E9_75BD29A5DD33.html =
Possibly. To test this hypothesis, other geochemical signatures of sedimentary input could be examined.
htmlText_F22566B9_F403_C8A9_41EB_7986CE82802F.html =
Possible but unlikely. Hydrothermal alteration by SiO2 would make the rock strong and resistant in the field, which is not observed.
htmlText_F5F9F41A_C369_336B_41C4_080774824A48.html =
Incorrect, the answer is the rock is rich in magnesium.
htmlText_F5FA0419_C369_3369_41B0_1E2C83E610D0.html =
Incorrect, the answer is the rock is rich in magnesium.
htmlText_F5FA9418_C369_3377_41E8_2D78E6381902.html =
Incorrect, the answer is the rock is rich in magnesium.
htmlText_F5FB2416_C369_337B_41D1_7A5071525DD0.html =
Correct, the answer is the rock is rich in magnesium.
htmlText_FB030746_EC02_C9DB_41D9_D9C6DCDF7353.html =
Incorrect. The answer is massive, crystalline, medium grained, porphyritic.
htmlText_FB040755_EC02_C9F9_41DF_DEFA4A6D45FB.html =
Not correct, the answer is clinopyroxene.
htmlText_FB04274A_EC02_C9EB_41D0_6E99AE7EF45E.html =
Correct. The answer is massive, crystalline, medium grained, porphyritic.
htmlText_FB042750_EC02_C9F7_41E3_08092C9E1145.html =
Incorrect, the answer is interstitial.
htmlText_FB042751_EC02_C9F9_41D5_8B016FF38D0E.html =
Correct, the answer is interstitial.
htmlText_FB042756_EC02_C9FB_41B0_5C3F9EC8C4FB.html =
Correct, the answer is clinopyroxene.
htmlText_FB04874D_EC02_C9E9_41E9_D735CB915D5B.html =
Incorrect. The correct answer is mafic.
htmlText_FB04874E_EC02_C9EB_41E4_5425D590A0AA.html =
Incorrect. The correct answer is mafic.
htmlText_FB04A749_EC02_C9E9_41E6_82D9772BA1D2.html =
Incorrect. The answer is massive, crystalline, medium grained, porphyritic.
htmlText_FB04B747_EC02_C9D9_41C2_2B3F427C4C22.html =
Incorrect. The answer is massive, crystalline, medium grained, porphyritic.
htmlText_FB05474C_EC02_C9EF_41BE_9D794BC27025.html =
Incorrect. The correct answer is mafic.
htmlText_FB054758_EC02_C9F7_41C3_E95E5921422D.html =
Not correct, the answer is orthopyroxene.
htmlText_FB055752_EC02_C9FB_41E6_9200BE0AFA31.html =
Incorrect, the answer is interstitial.
htmlText_FB055753_EC02_C9F9_41BD_A4B6FB3921F7.html =
Incorrect, the answer is interstitial.
htmlText_FB05A757_EC02_C9F9_41E1_D90CD1F6C888.html =
Not correct, the answer is clinopyroxene.
htmlText_FB05C74B_EC02_C9E9_41C3_E188EE20632C.html =
Correct. The answer is mafic.
htmlText_FB06675B_EC02_C9E9_41EB_9A8413F13CAC.html =
Correct, the answer is orthopyroxene.
htmlText_FB06C759_EC02_C9E9_41EB_0A08B9C65EB9.html =
Not correct, the answer is orthopyroxene.
htmlText_FB06F754_EC02_C9FF_41E4_5FA3DE098423.html =
Not correct, the answer is clinopyroxene.
htmlText_FB06F75A_EC02_C9EB_41D4_31F1B67FC801.html =
Not correct, the answer is orthopyroxene.
## Hotspot ### Tooltip HotspotPanoramaOverlayArea_0972F36D_A1C3_8340_41A7_4F6178987520.toolTip = 1.3.1 - Petrographic description and interpretation HotspotPanoramaOverlayArea_0AB82927_A1C2_8CC0_41E1_C78375BFD789.toolTip = 1.3.2 - Integrating geochemistry HotspotPanoramaOverlayArea_0C85AB8C_A1C2_83C0_41DE_E52C968E0B60.toolTip = 1.3.3 - Integrating geochronology HotspotPanoramaOverlayArea_0F6C2FA7_BB90_8B8D_41E3_A853994D378A.toolTip = 4.1.3 - Rock description HotspotPanoramaOverlayArea_15B37B1B_83CF_E3D0_41C9_10329F402660.toolTip = 1.1.4 - Describing rocks HotspotPanoramaOverlayArea_165D1334_8031_E3D0_41B9_466975928317.toolTip = 1.1.3 - Interpreting field relationship HotspotPanoramaOverlayArea_1A739F66_9EC3_8340_41D2_2D947E199AEC.toolTip = 1.2.2 - Making a field map HotspotPanoramaOverlayArea_1BB83470_9EC6_8540_41B5_F89DACFABEDB.toolTip = 1.2.1 - Interpreting how rocks formed HotspotPanoramaOverlayArea_1C0F57DD_9EC5_8340_41DC_3AF9FC9E912A.toolTip = 1.2.3 - Plotting structural data onto a map HotspotPanoramaOverlayArea_1D568756_8030_A250_41D6_4000BBFF5074.toolTip = 1.1.1 - Identifying and classifying rocks HotspotPanoramaOverlayArea_1FCAEA9E_8030_E2D0_41D9_FFC558A6097D.toolTip = 1.1.2 - Describing rocks HotspotPanoramaOverlayArea_29564D6E_C4F4_A8B4_41E6_11BEDDE2D731.toolTip = 8.3.1 - Interpret geochemistry data in context of field relationships HotspotPanoramaOverlayArea_2CD60D48_C4F4_68FC_4168_A84D49EE55E4.toolTip = 8.1.1 - Describing rocks using various criteria HotspotPanoramaOverlayArea_2E0985DD_B88F_9FBD_4198_3E55F0269557.toolTip = 4.1.1 - Rock description and classification HotspotPanoramaOverlayArea_2E13F7ED_C4F4_67B4_41D6_C561EE5A6B77.toolTip = 8.2.2 - Showing geological relationships using appropriate map symbols HotspotPanoramaOverlayArea_2EFF9C15_C4F7_A894_41E4_2C41CC537616.toolTip = 8.2.1 - Interpreting how rocks units are formed HotspotPanoramaOverlayArea_2FC7CBEB_C4F7_AFBC_41D9_E444FAB71A1A.toolTip = 8.1.2 - Describing rocks using various criteria HotspotPanoramaOverlayArea_3EDCB5AF_B88F_BF9D_41A3_7C493516BD47.toolTip = Introduction video HotspotPanoramaOverlayArea_48586CC7_BB91_8D8D_41B4_D622C35972ED.toolTip = 4.2.5 - Plotting structural data to download and plot HotspotPanoramaOverlayArea_4885DA99_BB91_9585_41E4_83C9DED533F6.toolTip = 4.2.6 - Interpreting how rock units formed HotspotPanoramaOverlayArea_496A1C32_BB90_8C87_41C1_8C390A828CE6.toolTip = 4.2.8 - Interpreting how rock units formed HotspotPanoramaOverlayArea_4A496499_BB90_7D85_41E4_90CBE3FBDDA1.toolTip = 4.2.2 - Interpreting how rock units formed HotspotPanoramaOverlayArea_4A93B980_BB91_9783_41E4_6D629BB46C72.toolTip = 4.2.3 - Interpreting how rock units formed HotspotPanoramaOverlayArea_4B072A39_BB91_B485_41CA_C4B6198A75E0.toolTip = 4.2.4 - Interpreting how rock units formed HotspotPanoramaOverlayArea_4E4B38DF_BB93_95BD_41E4_F1127FF25207.toolTip = 4.2.1 - Interpreting how rock units formed HotspotPanoramaOverlayArea_514451D7_BB90_B78D_41E6_FE5972A788C6.toolTip = 4.2.7 - Interpreting how rock units formed HotspotPanoramaOverlayArea_58AD9D18_BBB1_8C83_41C0_A331E0EF9F86.toolTip = 4.1.4 - Rock description and classification HotspotPanoramaOverlayArea_5A3EB64F_BB93_9C9D_41E7_9A0EEA8D163C.toolTip = 4.1.5 - Boundary identification HotspotPanoramaOverlayArea_60ABE897_BB8F_958D_41B6_42ECBD3AA77E.toolTip = 4.1.8 - Field relationships among rack units HotspotPanoramaOverlayArea_617655CE_BB8F_9F9F_41D6_79A957ACD43A.toolTip = 4.1.9 - Rock description and classification HotspotPanoramaOverlayArea_62AB2AEC_BB91_9583_41D7_680040B06DF4.toolTip = 4.1.6 - Rock description and classification HotspotPanoramaOverlayArea_630F8B6E_BB90_949F_41E2_CD23D8B934AA.toolTip = 4.1.7 - Rock description and classification HotspotPanoramaOverlayArea_6A59EFC5_EC03_78D9_41E0_65C971F8F1E1.toolTip = Go to location 5 HotspotPanoramaOverlayArea_72C25AE7_EC01_F8D9_41E3_5AB298EE01B3.toolTip = Go to location 3 HotspotPanoramaOverlayArea_82E5340B_A42D_7850_41D9_1812B0B0E8B9.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_833EF918_A42D_2870_41A7_15228A1A6924.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_83B968C3_C359_74D9_41D5_ABED339FC6D5.toolTip = 5.2.9 - Making a map HotspotPanoramaOverlayArea_8806BAFD_C329_34A9_41D6_617504F2C225.toolTip = 5.2.7 - Measuring structures HotspotPanoramaOverlayArea_8991A1D3_A9F4_BA7D_41E0_629ED58A5661.toolTip = Introduction video HotspotPanoramaOverlayArea_9078F7EE_A4ED_67D0_41D0_FF29DEA248ED.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_90A3D881_A4EB_2850_41DE_EA5ACE5FDB87.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_910BD8C3_EC06_D8D9_41DC_DB9307C60F67.toolTip = Go to location 7 HotspotPanoramaOverlayArea_914E0CD1_A4F5_29F0_41DE_31396389D48E.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_92F46192_EC01_C97B_41ED_186E85A09822.toolTip = Go to location 4 HotspotPanoramaOverlayArea_94AAD8CC_A994_EA6B_41D8_D16A5A0714AB.toolTip = 2.1.2 - Rock description HotspotPanoramaOverlayArea_9798E99A_A4ED_6870_41CA_2AADFFFBD4FA.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_97BA2C62_A4EC_E8D0_41C4_1A48A0895895.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_97E38CFB_A4ED_29B0_41D8_402F02AFF149.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_9E1685E5_A9B5_DA25_41D9_F13E0DA91B0B.toolTip = 2.1.1 - Rock description HotspotPanoramaOverlayArea_9EB11024_B970_F483_41D6_02CB84702980.toolTip = 2.3.4 - Rock description HotspotPanoramaOverlayArea_9EBB6A9D_B970_95BD_4193_22F16A927ADA.toolTip = 2.3.3 - Download the sedimentary log C - D HotspotPanoramaOverlayArea_A2025CF0_CD94_A9AC_41DB_C37032C0AD9B.toolTip = 7.1.1 - Identify and classifying rocks based on descriptions HotspotPanoramaOverlayArea_A28F9349_CD94_F8FC_41DC_2D4F16741916.toolTip = 7.1.3 - Identify and classifying rocks based on descriptions HotspotPanoramaOverlayArea_A2B990CA_CD94_99FC_41CD_D8F9A97701D7.toolTip = 7.1.2 - Identify and classifying rocks based on descriptions \ HotspotPanoramaOverlayArea_A2E516AE_B8B0_7D9F_41E4_E49212D02950.toolTip = 2.3.2 - Download the sedimentary log A - B HotspotPanoramaOverlayArea_A3B5CD97_C56F_ED79_41D4_08E4A73D6F05.toolTip = 6.1.1 - Making geological sketches of rocks and their relationships HotspotPanoramaOverlayArea_A3C12EA9_C56F_2CA9_41B2_F6EA6A046CB2.toolTip = 6.1.2 - Interpreting how rock units formed \ HotspotPanoramaOverlayArea_A427F6CD_CD95_F9F4_41DB_CA3052A1F3A6.toolTip = 7.3.3 - Interpret geochemistry data in context of field relationships HotspotPanoramaOverlayArea_A45C358D_CD95_9874_419B_F9142DFC1B2A.toolTip = 7.3.2 - Incorporating micro-scope-scale observation HotspotPanoramaOverlayArea_A5252253_CD94_98EC_41B2_297448044036.toolTip = 7.2.1 - Geological history from field observations HotspotPanoramaOverlayArea_A5A41144_CD95_B8F4_41CB_35A01D25EAFA.toolTip = 7.3.1 - Incorporating micro-scope-scale observation HotspotPanoramaOverlayArea_A5EDC5DD_CD94_7B94_41E8_C450BA5C134E.toolTip = 7.2.2 - Interpreting relationships from a field map HotspotPanoramaOverlayArea_AC5C11D8_C56F_54E8_41A1_B3D77D22FD94.toolTip = 6.2.1 - Interpreting how rock units formed HotspotPanoramaOverlayArea_ACC6C3A2_C56E_D55B_41D5_018063B9F424.toolTip = 6.3.1 - Incorporating micro-scope-scale observation HotspotPanoramaOverlayArea_AD1B181B_C56E_F369_41D8_F1397F603736.toolTip = 6.3.2 - Interpret geochemistry data in context of field relationships HotspotPanoramaOverlayArea_AE6048EC_B890_9583_41DB_F39BF554AA7C.toolTip = 2.3.1 - Rock description HotspotPanoramaOverlayArea_B2B5CD6D_A9EC_AA25_41D2_E3B502DDDBD0.toolTip = Introduction video HotspotPanoramaOverlayArea_BE9E8571_B890_7C85_41D1_2B914EFCFF0A.toolTip = Introduction video HotspotPanoramaOverlayArea_BE9F5FB6_B890_8B8F_41E3_7B82BECD8FF8.toolTip = 4.3.3 - Petrographic description and interpretation HotspotPanoramaOverlayArea_BE9FC428_B88F_FC83_41CC_C1BF81D13D4D.toolTip = 4.3.4 - Interpret geochemistry data in context of field relationships HotspotPanoramaOverlayArea_BEA193F9_B8B3_9B85_41E4_61B4B301E4BE.toolTip = 4.3.1 - Petrographic description and interpretation HotspotPanoramaOverlayArea_BEA1F328_B8B3_9483_41B8_48587C26AA46.toolTip = 4.3.2 - Interpret geochemistry data in context of field relationships HotspotPanoramaOverlayArea_BED01C0D_B890_8C9D_41DE_E0F90EC63DFC.toolTip = Introduction video HotspotPanoramaOverlayArea_BED09134_B891_9483_41D9_9A755B971E0F.toolTip = Introduction video HotspotPanoramaOverlayArea_BED0A944_B891_B483_41E4_6C671922CAC7.toolTip = Introduction video HotspotPanoramaOverlayArea_BED167E4_B890_BB83_41D2_471B9C23B73D.toolTip = Introduction video HotspotPanoramaOverlayArea_BED1801E_B890_74BF_41E1_DA647E6A54A9.toolTip = Introduction video HotspotPanoramaOverlayArea_BEE2D240_B8B1_9483_41E5_5FDF782056B5.toolTip = 5.1.1 - Relative timing HotspotPanoramaOverlayArea_BEE2EA76_B8B1_B48F_41A3_185CFF76E7A9.toolTip = 5.1.2 - Rock description video HotspotPanoramaOverlayArea_BEE50F5F_B8B0_8CBD_41CB_38BBF05464CC.toolTip = 5.1.3 - Structural measurements HotspotPanoramaOverlayArea_BF09033B_B970_7485_41E3_22FC80EC646B.toolTip = 5.1.4 -Describing structures HotspotPanoramaOverlayArea_BF1A04B0_B990_7D83_41D1_B327353CF677.toolTip = 5.2.1 - Measuring elements of a fold video HotspotPanoramaOverlayArea_BF1A1E32_B990_8C87_41D4_4A49C76BE87C.toolTip = 5.2.2 - Describing fold elements in the field HotspotPanoramaOverlayArea_BF1A2CD7_B990_8D8D_41E0_EE3F98D6450B.toolTip = 5.2.3 - Structural data to download and plot HotspotPanoramaOverlayArea_BF1A3EB2_B990_8D87_41D2_A12C7E051767.toolTip = 5.2.4 - Measuring structures HotspotPanoramaOverlayArea_BF1A5671_B990_9C85_41E3_589501C247C0.toolTip = 5.2.5 - Measuring and classifying folds HotspotPanoramaOverlayArea_C03B3938_AB6F_6A2B_41D6_AB1C941B2E4F.toolTip = 2.2.4 -Download structural data HotspotPanoramaOverlayArea_C0BC3511_AB6D_FBFD_41D6_D9EB6B4E65A1.toolTip = 2.2.1 - Rock description HotspotPanoramaOverlayArea_C12FF623_AA93_B9DD_41C8_DF3CF6C5D755.toolTip = 2.2.2 - Rock description HotspotPanoramaOverlayArea_C1C0D823_AA93_E9DD_41C0_F1FE7BAA5270.toolTip = 2.2.3 - Structural identification HotspotPanoramaOverlayArea_C37CE49B_E1CA_8093_41D4_3A50014EF883.toolTip = 3.3.2 - Structural data to download and plot HotspotPanoramaOverlayArea_C55AB737_B991_BC8D_41B1_8B34193194AF.toolTip = 3.3.1 - Rock description HotspotPanoramaOverlayArea_CB40D08E_AA9D_BAE7_41E4_0E081AE47C88.toolTip = Introduction video HotspotPanoramaOverlayArea_D5AE5709_B990_7C85_41C1_6B62A783B26F.toolTip = 3.2.1 - Structural measurement HotspotPanoramaOverlayArea_DD186029_C3E9_53A9_41E5_E349F15745D8.toolTip = 5.3.3 - Measuring elements of a fold HotspotPanoramaOverlayArea_DD24AE10_C3E9_2F77_41E5_3641DF23BB80.toolTip = 5.3.2 - Describing fold elements in the field HotspotPanoramaOverlayArea_DD7A9C89_C3E9_7369_41C8_1128DE997378.toolTip = 5.3.1 - Old mine workings HotspotPanoramaOverlayArea_E0B2D912_B9F0_B487_41B4_A1E2C57BED68.toolTip = 3.1.1 - Rock description HotspotPanoramaOverlayArea_E47DBC3B_B9F1_8C85_41E3_91F0B6557EB2.toolTip = 3.1.2 - Rock description HotspotPanoramaOverlayArea_E79CA9D3_B9F0_F785_41B8_492F941AF7D4.toolTip = 3.1.3 - Rock description HotspotPanoramaOverlayArea_E8116132_EE4A_81AD_41DF_1A71A1732D08.toolTip = Go to location 2 HotspotPanoramaOverlayArea_E81FB42E_EE75_87B5_41D3_A6579694984B.toolTip = Go to location 8 HotspotPanoramaOverlayArea_E820F011_EE4B_9F6F_41E8_DE985078E440.toolTip = Go to location 1 HotspotPanoramaOverlayArea_EA2D3038_B9F0_9483_41DD_E79D4123B160.toolTip = Introduction video HotspotPanoramaOverlayArea_EA73CE1F_A417_2870_41E3_ABDCB71E1125.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_EA73CF85_B9F3_8B8D_41DB_9C0260FC82BB.toolTip = Introduction video HotspotPanoramaOverlayArea_EA82E53C_A41B_38B0_41E3_C47A04D5334A.toolTip = 1.1.5 - Relative timing relationships HotspotPanoramaOverlayArea_EA89CBAE_A41B_2850_41C8_92AA4390ACF7.toolTip = 1.2.5 - Plotting and interpreting structural data on stereonets HotspotPanoramaOverlayArea_EAE235A9_A415_D850_41D2_2D813D386512.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_EAF81283_A41B_5850_41DF_7A2FF3E62D21.toolTip = 1.2.4 - Interpreting how rock units formed HotspotPanoramaOverlayArea_EAF89514_A41B_3870_41E0_92432192A29A.toolTip = 1.1.6 - Interpreting field relationships HotspotPanoramaOverlayArea_EB88FF0F_AAAC_E7E5_41E4_DFF5217360F8.toolTip = 2.1.3 - Structural measurement HotspotPanoramaOverlayArea_EECFE5F3_CBFC_7BAC_41E8_5A2C74699F11.toolTip = 6.1.1 - download: drone photography of pillow basalt HotspotPanoramaOverlayArea_EF0EE8F9_AA94_AA2D_41E1_9642580CB62F.toolTip = Introduction video HotspotPanoramaOverlayArea_EF813D68_AAAF_EA2B_41D5_90CC61CA487A.toolTip = 2.1.4 - Rock description HotspotPanoramaOverlayArea_F29D04A4_F403_4F5F_41EC_4C1E6BEA67A3.toolTip = Go to location 6 HotspotPanoramaOverlayArea_F58F0414_C369_337F_41E5_F0B0BAB2F131.toolTip = 5.3.4 - Interpretation of formation HotspotPanoramaOverlayArea_FB1A3743_EC02_C9D9_41E7_159550180282.toolTip = 4.1.2 - Interpreting how rock units formed HotspotPanoramaOverlayArea_FC9043A8_C366_D557_41D6_A65FEE9E47F0.toolTip = 5.2.8 - Structural data to download and plot HotspotPanoramaOverlayArea_FCF50BD7_C36A_D4F9_41CD_D1BFD5911A0E.toolTip = 5.2.6 - Structural data to download and plot ## Action ### PDF PopupPDFBehaviour_C80EDAC7_FD36_4C29_41E5_453F4B0F515E.url = files/Locality04_BaseMap_2021_en.pdf PopupPDFBehaviour_CAB1CB8A_FD33_CC3B_41E1_D17BFE64ED2F.url = files/Locality04_BaseMap_2021_en.pdf PopupPDFBehaviour_E7AEFC14_E257_8795_41E5_C7A10CADBD8D.url = files/Locality01_basemap_subdued_en.pdf PopupPDFBehaviour_E7AF3F34_E256_8195_41B4_9E95DE5E62EE.url = files/Locality01_basemap_strong_en.pdf 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//www.youtube.com/embed/GOnqki5v1RI?rel=0&autoplay=1 PopupWebFrameBehaviour_E8BD37B2_EFBA_80AD_41C9_5C681F46057B.url = //www.youtube.com/embed/QFUOHWzwQwM?rel=0&autoplay=1 PopupWebFrameBehaviour_E8C10CA6_EFCA_80B5_41EC_96E510CB0523.url = //www.youtube.com/embed/Ewvk7dMMRrg?rel=0&autoplay=1 PopupWebFrameBehaviour_EA3B4039_B9F0_9485_41D4_67A7600886FF.url = //www.youtube.com/embed/m_3K4Vd-Tfg?rel=0&autoplay=1 PopupWebFrameBehaviour_EA7D9F86_B9F3_8B8F_41E2_8BFEC98C8E67.url = //www.youtube.com/embed/m_3K4Vd-Tfg?rel=0&autoplay=1 PopupWebFrameBehaviour_EA89F1E7_A96C_DA25_41CD_455CE5C281FF.url = //www.youtube.com/embed/yacQ3mbhYlE?rel=0&autoplay=1 PopupWebFrameBehaviour_EBBF3A99_AAAD_AEED_41E0_8022B5F0EDB9.url = //www.youtube.com/embed/3bHTB86_eUQ?rel=0&autoplay=1 PopupWebFrameBehaviour_EC307A2D_AAB7_AE25_418B_CE3528890A67.url = //www.youtube.com/embed/plYgMbmSZbo?rel=0&autoplay=1 PopupWebFrameBehaviour_EDDEA7F2_EC01_48BB_41E7_7000D7B86679.url = //www.youtube.com/embed/9WyDPK9BeWg?rel=0&autoplay=1 PopupWebFrameBehaviour_F1B9BDB7_F402_B8B9_41C2_1AA95FBEB551.url = //www.youtube.com/embed/d4gzp0qBJmM?rel=0&autoplay=1 PopupWebFrameBehaviour_F1D114C8_F403_48D7_41BF_3D6C70869B54.url = //www.youtube.com/embed/JpDBVv09mt8?rel=0&autoplay=1 PopupWebFrameBehaviour_F1F13409_F403_4F69_41E9_D4B1260FCB59.url = //www.youtube.com/embed/4VTasX3W-hM?rel=0&autoplay=1 PopupWebFrameBehaviour_F1F3FC5E_F406_BFEB_41D2_17D2EC13C21E.url = //www.youtube.com/embed/1WTrs7sN9GM?rel=0&autoplay=1 PopupWebFrameBehaviour_F1FBB525_F407_4959_41D9_961612436421.url = //www.youtube.com/embed/d4gzp0qBJmM?rel=0&autoplay=1 PopupWebFrameBehaviour_F21DB74A_F403_49EB_41DF_D184CF0088AF.url = //www.youtube.com/embed/s_dm6K7sPuA?rel=0&autoplay=1 PopupWebFrameBehaviour_F63069BB_CC97_EB9C_41DC_78670362663B.url = //www.youtube.com/embed/BYRqww1ZKPs?rel=0&autoplay=1 ## E-Learning ### Answer questionOption_0AB87928_A1C2_8CC0_41E1_8C0B1B0D48F1.text = assimilation of continental crust questionOption_0ABC0940_A1C2_8F40_41D4_A0D1DD8924D5.text = alkaline questionOption_0ABC7941_A1C2_8F40_41D2_1AFD96638754.text = ultra-alkaline questionOption_0ABCA93E_A1C2_8CC0_41DD_00AE84BB3A58.text = sub-alkaline and transitional sub-alkaline to alkaline questionOption_0ABD293C_A1C2_8CC0_41CB_12DD2528AAD2.text = chondritic questionOption_0ABD5935_A1C2_8CC0_41E2_B3AA2284ACE9.text = mixing of two magmas questionOption_0ABD9939_A1C2_8CC0_41B2_AF3484CCE919.text = heavy-REE enriched questionOption_0ABDE933_A1C2_8CC0_41D1_D827F3F116E0.text = fractional crystallization questionOption_0ABDF93A_A1C2_8CC0_41BC_ADE3BBC8C14A.text = strongly light-REE enriched questionOption_0ABE0930_A1C2_8CC0_41C3_DF850F281DBF.text = melting of depleted mantle at shallow depths questionOption_0ABE3937_A1C2_8CC0_41D5_4CA91B6472FC.text = weakly light-REE enriched questionOption_0ABE7931_A1C2_8CC0_41E1_23F60C981D32.text = melt extracted from of a garnet-bearing source region questionOption_0ABEB92E_A1C2_8CC0_41A7_DBB9D22AA8CF.text = hydrothermal alteration questionOption_0ABF392A_A1C2_8CC0_41A9_7384165E80BD.text = fractional crystallization questionOption_0ABF792C_A1C2_8CC0_41AD_CF18DDA8EAD9.text = cumulate questionOption_0C84BB90_A1C2_83C0_41CC_3CF143891FAB.text = is the age when the dyke was exposed at the land surface questionOption_0C84DB8E_A1C2_83C0_41C1_C26FBB0119EF.text = is the best estimate of magmatic crystallization of the dyke questionOption_0C854B8C_A1C2_83C0_41C7_1E3261B9FC7C.text = is the age of metamorphism of the dyke questionOption_0C891BA8_A1C2_83C0_41CD_F0EDFBE2069F.text = inherited grains, Pb loss, and magmatic crystallization questionOption_0C899BA6_A1C2_83C0_41DE_C95070B15C58.text = magnetic crystallization, common Pb, and Pb loss questionOption_0C8A2BA5_A1C2_83C0_41E3_8337429D325A.text = common Pb, Pb loss and inherited grains questionOption_0C8ACB9A_A1C2_83C0_41C0_C4798F1FEC8F.text = the data points are tightly in agreement yielding a robust and precise mean age questionOption_0C8B4B9F_A1C2_83C0_41A7_72A1E5E7F74D.text = Pb/Pb questionOption_0C8B6B98_A1C2_83C0_41D7_F5B48D9FD1EE.text = the data points are reasonable consistent within analytical precision, and the age is acceptable.C: the data questionOption_0C8B8B96_A1C2_83C0_41E1_C81466C3AAEE.text = the data points are wildly different and indicating the mean age is not acceptable questionOption_0C8BCB9E_A1C2_83C0_41C5_E4DCD26D51A5.text = U/Pb questionOption_0F680FCA_BB90_8B87_41E3_1562E5FCC50D.text = olivine questionOption_0F68DFCC_BB90_8B83_41E6_CE8A6AD602A3.text = orthopyroxene questionOption_0F699FC9_BB90_8B85_41D2_5C4B0E8AA8E9.text = plagioclase questionOption_0F69CFC7_BB90_8B8D_41C4_7E38D4072CA6.text = quartz questionOption_166CC345_8031_E3B0_41D6_B9F0BFBBBF10.text = left lateral (sinistral) questionOption_166E433F_8031_E3D0_41DE_6DB25B2C8B66.text = sharply truncated and offset questionOption_166F0344_8031_E3B0_41DC_2FD15A00B43A.text = right lateral (dextral) questionOption_166FD340_8031_E3B0_41CA_2D6848C82D09.text = continuous and sheared questionOption_1BB80470_9EC6_8540_41D5_28F4C3E04DC3.text = Sigma 1 =vertical, sigma 2 and 3 = horizontal questionOption_1BB91475_9EC6_8540_41E3_DF531E994D80.text = Sigma 3 = vertical, sigma 1 and 2 = horizontal questionOption_1BB9E473_9EC6_8540_41CB_F287E7B8F969.text = Sigma 2 = vertical, sigma 1 and 3 = horizontal questionOption_1D5A3763_8030_A270_41D2_400474B7161C.text = felsic questionOption_1D5B4762_8030_A270_41D3_FAB300D863E0.text = mafic questionOption_1FCC0ABE_8030_E2D0_41C5_C1693D33DD28.text = Cubic questionOption_1FCD6AB5_8030_E2D0_41D7_080A0955B631.text = Quartz questionOption_1FCDEAB7_8030_E2D0_41D1_067A36BA96E8.text = Pyrite questionOption_1FCECAB4_8030_E2D0_419B_335487AA9D96.text = Olivine questionOption_1FCFAAB2_8030_E2D0_41DB_87FDC3A4AC4E.text = Fieldspar questionOption_1FD20AC2_8030_E2B0_41C4_2AC4E78E51D8.text = Spherical questionOption_1FD33AC4_8030_E2B0_41C1_A5429EDFA772.text = Prismatic questionOption_1FD37AC0_8030_E2B0_41B3_566E26EA16CE.text = Tetrahedral questionOption_21F795F8_B88F_9F83_41E4_C02A8D9A355C.text = orthopyroxene questionOption_21F815F7_B88F_9F8D_41DB_D3AF017F7104.text = clinopyroxene questionOption_21F885F6_B88F_9F8F_41D2_D599E68B553A.text = hornblende questionOption_21F925F1_B88F_9F85_41B1_4191A5141401.text = clinopyroxene questionOption_21F985F0_B88F_9F83_41DF_6F2BBCBCE46B.text = hornblende questionOption_21F9E5F4_B88F_9F83_41E2_E3B85FC8325C.text = olivine questionOption_21FA55F3_B88F_9F85_41E4_FDDEB6ED66BC.text = orthopyroxene questionOption_21FAE5EE_B88F_9F9F_41B2_473DF9CB064B.text = olivine questionOption_21FB05EB_B88F_9F85_41E4_84F35548CECC.text = vesicular questionOption_21FB65ED_B88F_9F9D_41C4_C19E892F66F4.text = poikilitic questionOption_21FC05E6_B88F_9F8F_41E6_B15DF58D2172.text = mafic questionOption_21FC65EA_B88F_9F87_41DD_ABD794D9B925.text = porphyritic questionOption_21FC85E9_B88F_9F85_41E0_F6DCBC298C01.text = amygdaloidal questionOption_21FCD5E4_B88F_9F83_41DB_8D998D831440.text = intermediate questionOption_21FD15E7_B88F_9F8D_41D7_258D36FAA49B.text = ultramafic questionOption_21FD35E3_B88F_9F85_4198_1D5FC35CD31F.text = granitic / felsic questionOption_21FDC5E2_B88F_9F87_41E1_156F99FAA91C.text = porphyritic pyroxenite questionOption_21FE45E1_B88F_9F85_41CC_B118FCDC0599.text = porphyritic dolerite questionOption_21FED5E0_B88F_9F83_41DC_65993DF05A74.text = porphyritic granite questionOption_29557D7D_C4F4_A894_41DC_7E7A0C595E77.text = ocean island basalt (OIB) with progressive fractional crystallisation questionOption_2955CD80_C4F4_A86C_41C8_3D8FACF4B7FA.text = volcanic arc (slab melting) questionOption_295A1D7F_C4F4_A894_41D1_3EBED5B6F254.text = normal mid-ocean ridge basalt (N-MORB) with a component of assimilation of felsic Archaean crust questionOption_295A9D7E_C4F4_A894_41E1_F049D44AF3CD.text = enriched mid-ocean ridge basalt (E-MORB) with a component of assimilation of felsic Archaean crust questionOption_2CE43D5D_C4F4_6894_4143_AA37DDBF2169.text = 1-2 m across questionOption_2CE4BD5C_C4F4_6894_41E2_38337CB45296.text = 30-60 cm across questionOption_2CE4DD5B_C4F4_689C_41E8_235426069FFC.text = <30 cm across questionOption_2CE7ED5E_C4F4_6894_41DD_F71829AFB498.text = >2 m across questionOption_2E0945DF_B88F_9FBD_41D2_D0E97C040C8F.text = porphyritic andesite questionOption_2E821C21_C4F7_A8AC_41DD_884BD5BF1EEB.text = continent-continent collision boundary questionOption_2E827C20_C4F7_A8AC_41BD_7D66426E982E.text = plume-related ocean island volcanism questionOption_2E828C22_C4F7_A8AC_41E9_25A2D05A6B6D.text = extrusion of lava into water (subaqueous) questionOption_2E82BC23_C4F7_A8AC_41C5_08455FECFA6C.text = extrusion of lava over land (subaerial) questionOption_2E835C24_C4F7_A8B4_41DE_ADA14799B7C0.text = explosive eruption of lava as a hot ash flow questionOption_2E83EC25_C4F7_A8B4_41B0_CA3C9C112DF4.text = slow cooling causing polygonal cooling joints questionOption_2EFD0C1E_C4F7_A894_41B0_FE97808D6150.text = a mid ocean ridge at a divergent plate boundary questionOption_2EFDCC1F_C4F7_A894_41C7_AF7595F589D1.text = a back-arc basin questionOption_2FCA7BFF_C4F7_AF94_41E7_18F34F0F9173.text = young towards the north questionOption_2FCB0C00_C4F7_A86C_41D7_5D0D30D1C7DC.text = young towards the east questionOption_2FCB0C01_C4F7_A86C_41C9_742666708EF9.text = young towards the south questionOption_2FCB2C02_C4F7_A86C_41E0_83292FF06250.text = young towards the west questionOption_48BA4AA6_BB91_958F_41AC_F4B6FEC2E981.text = was extruded as lava as lava that was supercooled from high temperatures questionOption_48BA4AA9_BB91_9585_41A6_3EA41A4E4B70.text = was extruded in a subaqueous environment questionOption_48BB6AA8_BB91_9583_41E2_E1B5910D1D23.text = is a hyperbyssal intrusion questionOption_48BBDAA7_BB91_958D_41D3_E41AD3D4EFB4.text = was extruded as lava that cooled rapidly questionOption_49640C59_BB90_8C85_41D2_35617D18BC46.text = was extruded in a subaqueous environment questionOption_49658C57_BB90_8C8D_41B0_C2FC9C7F2BE5.text = is a hyperbyssal intrusion questionOption_49664C53_BB90_8C85_41E6_90473F2119F6.text = was extruded as lava that was supercooled from high temperatures questionOption_49668C55_BB90_8C8D_41BF_D11F7E8B2B1D.text = was extruded as lava that cooled rapidly questionOption_4A4C24DE_BB90_7DBF_41C4_F90D44EEFBF6.text = was extruded in a subaqueous environment questionOption_4A4D44DC_BB90_7D83_41E3_FDDE84D5140A.text = is a hyperbyssal intrusion with a two-stage cooling history questionOption_4A4D84D9_BB90_7D85_41B4_5EA4C9DEC1E7.text = is a hyperbyssal intrusion cooled very slowly questionOption_4A4DF4DB_BB90_7D85_41C5_74743FD53DA0.text = was extruded as lava that cooled rapidly questionOption_4A96199C_BB91_9783_41D4_8D0D8396FD27.text = was extruded in a subaqueous environment questionOption_4A964996_BB91_978F_41D0_E343048498B1.text = is a hyperbyssal intrusion cooled very slowly questionOption_4A97399A_BB91_9787_41DC_C1E666B73F00.text = is a hyperbyssal intrusion with a two-stage cooling history questionOption_4A97C997_BB91_978D_41CD_74456A28AD8D.text = was extruded as lava that cooled rapidly questionOption_4B388A4E_BB91_B49F_41E4_A3779FD12E04.text = was extruded as lava that cooled rapidly questionOption_4B38CA50_BB91_B483_41CF_E268240CE421.text = is a hyperbyssal intrusion with a two-stage cooling history questionOption_4B39BA51_BB91_B485_41E5_F0C14C9F7105.text = was extruded in a subaqueous environment questionOption_4B3B0A4D_BB91_B49D_415B_9AB36255638C.text = is a hyperbyssal intrusion cooled very slowly questionOption_4E4608ED_BB93_959D_41B7_53001695051E.text = is a hyperbyssal intrusion cooled very slowly questionOption_4E78B8F0_BB93_9583_41C3_FEE2C4DBC63B.text = was extruded in a subaqueous environment questionOption_4E7958EF_BB93_959D_41DB_F361885FA2CF.text = is a hyperbyssal intrusion with a two-stage cooling history questionOption_4E7978EE_BB93_959F_41D3_18E674442371.text = was extruded as lava that cooled rapidly questionOption_517611ED_BB90_B79D_41DD_EA9A9528384C.text = is a hyperbyssal intrusion questionOption_517971EE_BB90_B79F_41D6_08582F9E689A.text = was extruded in a subaqueous environment questionOption_517991EC_BB90_B783_41E2_A999F3FF33B9.text = was extruded as lava that cooled rapidly questionOption_5179A1EA_BB90_B787_41E0_7A5B1BCA495C.text = was extruded as lava that was supercooled from high temperatures questionOption_54D7BABD_BBF0_F5FD_41CD_0F5765FC23B1.text = drift questionOption_56064DCD_BBF1_8F9D_41D4_309019E55DB9.text = inferred questionOption_57FAB722_BBF0_BC87_41D9_3C4449993A5C.text = observed questionOption_58AE9D19_BBB1_8C85_41DD_192B58FB4714.text = granite questionOption_58B17D1B_BBB1_8C85_41DD_D71EC19B052C.text = dolerite questionOption_58B25D23_BBB1_8C85_41BA_AC6B1D3326FC.text = it is mafic in composition questionOption_58B26D1E_BBB1_8CBF_41E1_CC1959119242.text = amygdaloidal questionOption_58B2BD1D_BBB1_8CBD_41E2_5AFCF2A5EBF6.text = pyroxenite questionOption_58B2FD1C_BBB1_8C83_419A_68525FCFA3C5.text = felsic porphyry questionOption_58B37D2F_BBB1_8C9D_41CA_4A50434D2095.text = plagioclase questionOption_58B38D25_BBB1_8C8D_41D6_A8730A88D558.text = it is felsic to intermediate in composition questionOption_58B39D20_BBB1_8C83_41DB_E47D1C2D6BA2.text = vesicular questionOption_58B3BD24_BBB1_8C83_41D5_06DC73B5EFF2.text = it is ultramafic in composition questionOption_58B3DD1F_BBB1_8CBD_41C3_172B193CFD92.text = porphyritic questionOption_58B41D2E_BBB1_8C9F_41DA_A467D04EE66C.text = orthopyroxene questionOption_58B49D2D_BBB1_8C9D_41E6_4527796AA40E.text = quartz questionOption_58B4ED27_BBB1_8C8D_41E1_1215B96A84AA.text = hornblende questionOption_58B4FD21_BBB1_8C85_41CC_9C6120DDD78C.text = poikilitic questionOption_5918685B_BBF1_F485_41A6_7DC443DD9CE2.text = gradational questionOption_60A7D8BB_BB8F_9585_41E4_C735F5A8431C.text = E-W questionOption_60A838B8_BB8F_9583_41E4_023444E44C0D.text = NW-SE questionOption_60A868B9_BB8F_9585_41CD_606AB47072B8.text = N-S questionOption_60A8C8B6_BB8F_958F_41D5_9EEAE6F87684.text = NE-SW questionOption_617135F4_BB8F_9F83_41E0_D52CD4673B08.text = poikilitic questionOption_617185EB_BB8F_9F85_41D3_D06EC62730C3.text = poikilitic basalt questionOption_617185F2_BB8F_9F87_41E6_9FBE6BA9FB69.text = ophitic questionOption_617265E9_BB8F_9F85_41DF_03CD6BEB1905.text = vesicular basalt questionOption_617265F1_BB8F_9F85_41A8_7961D3BB9D19.text = spinifex questionOption_6172A5ED_BB8F_9F9D_41E7_80F3ECA0102A.text = spinifex basalt questionOption_6172C5EF_BB8F_9F9D_41DC_A1CAA775DC98.text = amygdaloidal questionOption_6172D5E7_BB8F_9F8D_41E6_D35526E761E1.text = amygdaloidal basalt questionOption_62A48AF0_BB91_9583_41E6_1160AD056DC6.text = sandstone questionOption_62A48AF2_BB91_9587_41E0_5A7695953F76.text = dolerite questionOption_62A71AEF_BB91_959D_41BF_675CC860FD0F.text = basalt questionOption_62A91AED_BB91_959D_41D4_6984BFE49D21.text = granite questionOption_63006B92_BB90_8B87_41CC_F210684DB210.text = dolerite questionOption_63016B8E_BB90_8B9F_41DA_E14F4D057FE2.text = granite questionOption_63018B91_BB90_8B85_41DA_F578BF3566B2.text = sandstone questionOption_6301CB8F_BB90_8B9D_41E3_E1AF42B0C64F.text = basalt questionOption_88303B11_C329_3579_41C5_55F2EBF7BA35.text = NW - SE questionOption_88310B0F_C329_3569_41B2_DCD0313D03BC.text = NE - SW questionOption_8831DB10_C329_3577_41D9_657D2B4D0F5D.text = E - W questionOption_88329B0E_C329_356B_417A_F07506658542.text = N - S questionOption_94A538D8_A994_EA6B_41C2_9E34129092C8.text = pyroxene questionOption_94A568D1_A994_EA7D_41E3_39FDDD8D6637.text = ultramafic questionOption_94A5A8CF_A994_EA65_41E1_7D01FF4994C8.text = mafic questionOption_94A618D5_A994_EA65_41CF_85725A081265.text = olivine questionOption_94A658D9_A994_EA6D_41C5_EB84497ACB94.text = feldspar questionOption_94A668D4_A994_EA7B_41B6_3DD2234F16A0.text = quartz questionOption_94A678DA_A994_EA6F_41E0_873DFD45C19A.text = quartz questionOption_94A798D6_A994_EA67_41E2_822DF8AB6EC9.text = pyrite questionOption_94A7E8DD_A994_EA65_41D4_623A379135B0.text = apatite questionOption_94A7F8DC_A994_EA6B_41A7_B1A7E3535ADC.text = hornblende questionOption_94ABB8CD_A994_EA65_41C0_164FF8800F75.text = felsic questionOption_9E0205E7_A9B5_DA25_41DC_03627F35D9EB.text = they are mafic questionOption_9E0405EC_A9B5_DA2B_41E0_0DB4C4CD6D8E.text = finely laminated questionOption_9E0415EC_A9B5_DA2B_41CC_64A0027143AB.text = thinly bedded questionOption_9E0435F1_A9B5_DA3D_41D6_EEC839D01016.text = thinly bedded questionOption_9E0565EE_A9B5_DA27_41D6_16FAA20EC3A7.text = cross bedded questionOption_9E0585EB_A9B5_DA2D_41DA_3DEAF69F4818.text = massive questionOption_9E05A5EF_A9B5_DA25_41D9_E6E2B65FD806.text = finely laminated questionOption_9E05B5EA_A9B5_DA2F_41CF_89B581A550BD.text = cross bedded questionOption_9E05F5EE_A9B5_DA27_41B0_7FA611DEE6D1.text = massive questionOption_9E1825E6_A9B5_DA27_41C1_309D0E2CFDF8.text = they are felsic questionOption_9EC34034_B970_F483_41D7_47EA7A507EDE.text = requires flow to form an erosive base questionOption_9EC3802F_B970_F49D_41E5_03BCA4FA94EB.text = red symbol questionOption_9EC3D035_B970_F48D_41E7_19510BA776A5.text = it is strictly a marine only environment questionOption_9EC3F036_B970_F48F_41DB_50113AEABD4A.text = it is a sedimentary structure found only is aeolain (wind-blown) deposits questionOption_9ECC0030_B970_F483_41DA_2DD5C970E5A8.text = blue symbol questionOption_A282435B_CD94_F89C_41E3_4330E2BA50DA.text = coarse grained questionOption_A2825360_CD94_F8AC_41D4_9728FE3B9FD6.text = ultramafic questionOption_A282735A_CD94_F89C_4190_C02CFF2D3783.text = medium grained questionOption_A282735E_CD94_F894_41E8_EC243D847CF6.text = intermediate questionOption_A282735F_CD94_F894_41DD_C4CF49584E0D.text = mafic questionOption_A282A359_CD94_F89C_41D3_4DBFE2CB32AE.text = fine grained questionOption_A282A35D_CD94_F894_41D5_516520EF1573.text = felsic questionOption_A283235C_CD94_F894_41C0_A3FF8C90D04D.text = pegmatitic questionOption_A28D4358_CD94_F89C_41E3_FB90B1FCCBA9.text = pegmatitic gabbro questionOption_A28D5357_CD94_F894_41CD_D0B62F332744.text = gabbro questionOption_A28DD356_CD94_F894_41D6_5E4050C30050.text = dolerite questionOption_A28DF355_CD94_F894_41B3_539DB3698E0A.text = basalt questionOption_A2BC40E2_CD94_99AC_41CE_2C8F8588F6EF.text = dunite questionOption_A2BC90DF_CD94_9994_41DC_E1D49FA20F46.text = peridotite questionOption_A2BCF0E0_CD94_99AC_41E3_C4FA47866166.text = gabbro questionOption_A2BCF0E1_CD94_99AC_41DE_51C47834D5AC.text = pyroxene questionOption_A2FC3D03_CD94_A86C_41D7_3F9737194946.text = dacite questionOption_A2FC5CFE_CD94_A994_41DF_CF22914050FD.text = hackled questionOption_A2FC7CFF_CD94_A994_41E5_8E04923828EA.text = irregular questionOption_A2FC7D04_CD94_A874_41E9_1AB3D6681E3C.text = dolerite questionOption_A2FC9D01_CD94_A86C_41E3_B34ED8A48974.text = stepped questionOption_A2FCAD02_CD94_A86C_41E6_FD2CE97645FB.text = rhyolite questionOption_A2FD0D00_CD94_A86C_41E0_C66A4093D47E.text = conchoidal questionOption_A2FD0D05_CD94_A874_41E4_B14D71FA76E0.text = basalt questionOption_A3841DB3_C56F_ECB9_41DA_12FBAD284F7E.text = younging to the south questionOption_A3BA6DAF_C56F_ECA9_41E5_CFA2C0E2394C.text = younging to the west questionOption_A3BB5DB0_C56F_ECB7_419F_FDD75D645F00.text = younging to the east questionOption_A3BB6DB1_C56F_ECB9_41E0_3484096BE64B.text = younging to the north questionOption_A3CC0EBC_C56F_2CAF_41E0_E373CEE07748.text = layers of quenched glass formed as pillows inflate questionOption_A3CCCEC1_C56F_2CD9_41E2_89A5F2AA0D1A.text = pale green, laminated questionOption_A3CCDEC2_C56F_2CDB_41E2_5F34AD665E3D.text = dark green, laminated questionOption_A3CCEEBA_C56F_2CAB_41B3_A1BC6D10EE2D.text = tectonic deformation localising shearing of pillows questionOption_A3CCEEBF_C56F_2CA9_41E8_4BB9DD0CD233.text = pale green, spotted questionOption_A3CD8EBD_C56F_2CA9_41D6_8CDA74B237BF.text = trapped shale deposited on pillow surfaces questionOption_A3CDAEC3_C56F_2CD9_41C3_74A1C9445757.text = pale, green, massive questionOption_A41B16DB_CD95_F99C_41B2_2D1A03F55E7E.text = MH58 is significantly more silicious questionOption_A41B86DC_CD95_F994_41E2_166E1BC516A5.text = MH58 is significantly more enriched in total alkalis questionOption_A42406D7_CD95_F994_41C8_949A7D513740.text = strongly negative Ti and Nb+Ta anomalies questionOption_A42456DD_CD95_F994_41E6_3BA5F6DD43C4.text = MH50 is relatively depleted in silica and total alkalis questionOption_A42476D8_CD95_F99C_41DA_4B6D458D51BC.text = slightly enriched LREE and a negative Nb+Ta anomaly questionOption_A424C6DA_CD95_F99C_41CE_7647BF76C28E.text = They are not significantly distinguishable questionOption_A424E6D9_CD95_F99C_41B9_3354F8A41704.text = strongly enriched in HREE and depleted LREE questionOption_A425B6D6_CD95_F994_41E4_83A49A78080D.text = highly enriched LREE and depleted HREE questionOption_A451259A_CD95_9B9C_41E0_62A0E90BF6FC.text = actinolite questionOption_A451359B_CD95_9B9C_41A4_02647451CF47.text = bladed, acicular questionOption_A451759C_CD95_9B94_41CE_F0C4DE2B61F1.text = tabular, prismatic questionOption_A451F59D_CD95_9B94_419A_F6DB26065FA7.text = spheroidal, nodular questionOption_A4524599_CD95_9B9C_41D7_1D869451039D.text = chlorite questionOption_A4527598_CD95_9B9C_41E4_220C2B586B02.text = clinopyroxene questionOption_A452B59E_CD95_9B94_41DF_08B43A602BAD.text = dendritic questionOption_A4539597_CD95_9B94_41DE_13B79428874D.text = olivine questionOption_A5182261_CD94_98AC_41D9_0FCD9E1F751F.text = Basalt forms a chilled margin of a pyroxenite intrusion questionOption_A5185260_CD94_98AC_41D2_6A3DBE83DD1D.text = Pyroxenite and gabbro and intruded an earlier basalt flow questionOption_A518D263_CD94_98AC_41B9_06B38072D336.text = Basalt lava flow was extruded over pyroxenite questionOption_A5199262_CD94_98AC_41DE_09A82AB376C2.text = Basalt, pyroxenite and gabbro are different parts of a differentiated flow questionOption_A5982153_CD95_B8EC_41DE_6E78C407E896.text = cumulate questionOption_A5995150_CD95_B8EC_41E8_96409664E9A9.text = graphic questionOption_A5997151_CD95_B8EC_41C2_1ECAD9810804.text = ophitic questionOption_A5999152_CD95_B8EC_41E0_1F377BF78CB6.text = porphyritic questionOption_A59A114D_CD95_B8F4_41E6_07FFEC37140F.text = slow crystallization and intergrowth in a magma chamber questionOption_A59A614A_CD95_B8FC_41E8_3CF03CD2FFF3.text = chlorite questionOption_A59A7149_CD95_B8FC_41D8_5832702C9A06.text = plagioclase questionOption_A59A914E_CD95_B8F4_41D7_E9F21FDE3AE0.text = rapid quenching of a lava questionOption_A59AA14F_CD95_B8F4_41E4_D3B8BA351B24.text = extrusion into an aqueous body questionOption_A59B014B_CD95_B8FC_41E5_E71F73572215.text = actinolite questionOption_A59BA14C_CD95_B8F4_41BB_36A05CBC1553.text = settling of crystals at the base of a magma chamber questionOption_A59BC148_CD95_B8FC_41E0_B16AB29A183F.text = quartz questionOption_A5E015F1_CD94_7BAC_41D9_54804FDAC6FA.text = Pyroxenite and gabbro and intruded an earlier basalt flow questionOption_A5E0B5EF_CD94_7BB4_41B5_F824255AD8CD.text = Basalt, pyroxenite and gabbro are different parts of a differentiated flow questionOption_A5E145F3_CD94_7BAC_41E4_1EEB80DE64A4.text = Basalt lava flow was extruded over pyroxenite questionOption_A5E1E5F2_CD94_7BAC_41DB_1C1E70480D16.text = Basalt forms a chilled margin of a pyroxenite intrusion questionOption_AC5811F4_C56F_54BF_41DB_D2CAD0FFF9B3.text = 60% questionOption_AC5841F3_C56F_54B9_41D1_7B6EF7F71C73.text = 10% questionOption_AC5971F5_C56F_54B9_41C0_D107A9EBEC0F.text = 90% questionOption_AC5E11EA_C56F_54AB_41DC_BED560437BE8.text = They are more fine grained than the host rock questionOption_AC5E31E9_C56F_54A9_41E7_7AA3187039C0.text = They are more felsic than the host rock questionOption_AC5F31F2_C56F_54BB_41E8_18B93D19B87A.text = 2% questionOption_AC5F71EB_C56F_54A9_41B1_2CE0B65FE5FA.text = They are more mafic than the host rock questionOption_ACC043A5_C56E_D559_41E5_8699DA7FBBB5.text = quenched droplets of immiscible liquid in a lava questionOption_ACC043A7_C56E_D559_41BB_A8BA0A5828AB.text = devitrification of volcanic glass – alteration of unstable glass by growth of crystals questionOption_ACC073AE_C56E_D4AB_41DE_D5F955C4C546.text = discrete and sharp questionOption_ACC0D3A8_C56E_D557_41D8_02F05ADA1672.text = radiating crystals questionOption_ACC113A2_C56E_D55B_41E8_33355FFBC3DE.text = amygdales – vesicles that have been later cemented by calcite questionOption_ACC1A3A4_C56E_D55F_41E6_A55902744FB5.text = ocelli – spherulitic crystallization within a magma chamber questionOption_ACC233B3_C56E_D4B9_41E6_3D348BC89087.text = single crystal of quartz questionOption_ACC253B4_C56E_D4BF_41DC_22B026087B18.text = concentric domains with microscopic spinifex texture questionOption_ACC2E3B5_C56E_D4B9_41E4_0DE1132995CF.text = drusy cement infill questionOption_ACC303A9_C56E_D4A9_41C0_C1175C3C9C0C.text = concentric shells of crystals questionOption_ACC343AF_C56E_D4A9_41D8_DE6E52CD14DB.text = irregular and indistinct questionOption_ACC3A3B6_C56E_D4BB_41E7_533D2135F5E2.text = pore space questionOption_AD64182A_C56E_F3AB_41AC_AA553A4B80F7.text = fractional crystallization of mafic magma questionOption_AD64482B_C56E_F3A9_41CA_41EA9A919752.text = hydrothermal silicification questionOption_AD64B82D_C56E_F3A9_41E3_1FA2EA03FAE7.text = ultramafics questionOption_AD652827_C56E_F359_41D1_C466F26CBC15.text = magma mixing with coexisting silicious melts questionOption_AD657829_C56E_F3A9_41D2_32588E3CB6F8.text = contamination by assimilation of silicious sediments into the magma questionOption_AD665830_C56E_F3B7_41BD_254D96FA9AB4.text = plagiogranite questionOption_AD67482E_C56E_F3AB_41D8_2D15A9E14D74.text = mafic rocks questionOption_AD67882F_C56E_F3A9_41C6_DCABC608F07B.text = felsic dykes questionOption_AE6A18FA_B890_9587_41E2_F8A7517AC964.text = erosion in a fluvial environment questionOption_AE6A18FB_B890_9585_41BA_DAB13848AEC4.text = flattening due to compaction in a hot volcanic ash flow questionOption_AE6A38F8_B890_9583_41D8_196EC26919BB.text = flattening due to tectonic deformation questionOption_AE6A3900_B890_9483_41A4_5AD55EADA4C8.text = shale questionOption_AE6A9901_B890_9485_41A7_1265CEDC9CBF.text = fine grained felsic questionOption_AE6B48FD_B890_957D_41C8_1CB5F5779342.text = gabbro questionOption_AE6BB8FE_B890_957F_41DE_50A0FC6889DF.text = basalt questionOption_BE9FC432_B88F_FC87_41A5_C080F79558F0.text = garnet questionOption_BE9FC434_B88F_FC83_41E7_9296B3D214F6.text = plagioclase questionOption_BE9FC436_B88F_FC8F_41E4_40D935B68159.text = rutile questionOption_BE9FC438_B88F_FC83_41DF_C76940029534.text = olivine questionOption_BE9FC43A_B88F_FC87_41DF_26A1DF868A06.text = MH55 has significantly depleted HREE and a stronger negative NB+Ta anomaly questionOption_BE9FC43C_B88F_FC83_41A7_6D62A1004A7B.text = MH55 has a significantly higher Th abundance questionOption_BE9FC43E_B88F_FCFF_41D5_9D17B8C3A649.text = MH55 and MH56 have positive and negative Ti anomalies, respectively questionOption_BE9FC43F_B88F_FCFD_41D8_E8ED5E37F8AE.text = MH55 has MORB-like abundances of REE questionOption_BE9FC441_B88F_FC85_41BF_00665127F844.text = MH56, MH55, MH20, MH14, MH15 questionOption_BE9FC443_B88F_FC85_41DF_19A14099AE96.text = MH15, MH14, MH20, MH55, MH56 questionOption_BE9FC445_B88F_FC8D_41DB_2464A507C8DB.text = MH56, MH20, MH55, MH15, MH14 questionOption_BE9FC447_B88F_FC8D_41C5_7E31C518E472.text = MH14, MH15, MH20, MH55, MH56 questionOption_BEA1F339_B8B3_9485_41E5_890DD63E9445.text = MH56, MH55, MH20, MH14, MH15 questionOption_BEA1F33B_B8B3_9485_41C5_FA946B11D636.text = MH15, MH14, MH20, MH55, MH56 questionOption_BEA1F33C_B8B3_9483_41DF_2D8DF282EF8E.text = MH56, MH20, MH55, MH15, MH14 questionOption_BEA1F33E_B8B3_94FF_419B_AA3E4E75E5D3.text = MH14, MH15, MH20, MH55, MH56 questionOption_BEA1F33F_B8B3_94FD_41E3_EDDD283187B0.text = they do not contain quartz questionOption_BEA1F341_B8B3_9485_41DB_4D2112B96FA2.text = they do not contain alkali-bearing minerals questionOption_BEA1F342_B8B3_9487_41DF_8525EB289575.text = they have been contaminated by felsic crustal material questionOption_BEA1F344_B8B3_9483_41E5_838FA986B3E5.text = they have been crystallized from highly evolved magma questionOption_BEE2D25A_B8B1_9487_41BD_3586DE5C4AB2.text = yes questionOption_BEE2D25B_B8B1_9485_41C5_8EA4D7F92A97.text = no questionOption_BEE2D25F_B8B1_94BD_41E1_71D8E1B9AFD8.text = Striking E-W, dipping steeply N questionOption_BEE2D260_B8B1_9483_41E6_4723F9B70A0E.text = Striking N-S, dipping steeply W questionOption_BEE2D261_B8B1_9485_41E4_642A606FCA58.text = Striking E-W, dipping steeply N questionOption_BEE2D262_B8B1_9487_41E0_60B40833CECE.text = Striking N-S, dipping steeply E questionOption_BEE50F83_B8B0_8B85_41BF_45AB66DAEB9D.text = gently dipping E questionOption_BEE50F85_B8B0_8B8D_41E2_95DCFB77CE8A.text = vertical questionOption_BEE50F87_B8B0_8B8D_41E6_B6E0836251DD.text = steeply dipping NNW questionOption_BEE50F88_B8B0_8B83_41E4_A16BA611C91A.text = steeply dipping W questionOption_BF09034E_B970_749F_41BF_72C35C35F44A.text = gently dipping E questionOption_BF09034F_B970_749D_41E0_09629241EE13.text = sub-vertical questionOption_BF090350_B970_7483_41B2_CEA02D595B84.text = steeply dipping NNW questionOption_BF090352_B970_7487_41C8_E8B88FC32DF9.text = moderately dipping ENE questionOption_BF090353_B970_7485_41E1_A32E1F8113F7.text = banded questionOption_BF090354_B970_7483_41E6_A57B3BFEF217.text = massive questionOption_BF090355_B970_748D_41E7_1A9D6BEB168B.text = bedded questionOption_BF090357_B970_748D_41CB_B0AEA75C720C.text = foliated questionOption_BF1A1E32_B990_8C87_41D7_3A3EA5A96733.text = gentle questionOption_BF1A1E34_B990_8C83_41E2_342B2634CC2C.text = open questionOption_BF1A1E36_B990_8C8C_41D4_0F72916EB459.text = close questionOption_BF1A1E38_B990_8C83_41CF_5DC9C127D939.text = tight questionOption_BF1A1E3B_B990_8C85_419B_0C151E5F2189.text = horizontal questionOption_BF1A1E3C_B990_8C83_41D6_70DC84051B35.text = gently plunging questionOption_BF1A1E3E_B990_8CFF_41E6_0508AD1BEDBD.text = steeply plunging questionOption_BF1A1E40_B990_8C83_41E3_8F32EEBE8565.text = vertical questionOption_BF1A1E42_B990_8C87_41E1_8EC93491AC7F.text = horizontal questionOption_BF1A1E44_B990_8C83_41B7_70E49E3267BA.text = gently plunging questionOption_BF1A1E46_B990_8C8F_41D6_2ADCE550CB4A.text = steeply plunging questionOption_BF1A1E48_B990_8C83_41E2_58A9E837D753.text = vertical questionOption_BF1A1E4A_B990_8C87_41D0_6C2350AF40CB.text = N-S questionOption_BF1A1E4B_B990_8C85_41D1_488DA7C98F19.text = NE-SW questionOption_BF1A1E4D_B990_8C9D_41DE_D1193300AA6E.text = E-W questionOption_BF1A1E4F_B990_8C9D_41E5_D6E02270CB8F.text = NW-SE questionOption_BF1A3ECA_B990_8D87_41D9_FF42F695F6F5.text = N-S questionOption_BF1A3ECC_B990_8D83_41D0_6345D88FB950.text = NE-SW questionOption_BF1A3ECE_B990_8D9F_41D4_562E86FAD769.text = E-W questionOption_BF1A3ECF_B990_8D9D_417A_EE87762CB961.text = NW-SE questionOption_BF1A3ED1_B990_8D85_41D0_FA815419BFB8.text = shear bands questionOption_BF1A3ED3_B990_8D85_41E5_D69495C3AD08.text = spaced axial planar cleavage questionOption_BF1A3ED5_B990_8D8D_41E7_05D46E697FE2.text = stretching lineation questionOption_BF1A3ED6_B990_8D8F_4198_842BF9FF8661.text = pervasive schistosity questionOption_BF1A567A_B990_9C87_41E2_4595550276EE.text = gentle questionOption_BF1A567C_B990_9C83_41D4_17BF4776662D.text = open questionOption_BF1A567E_B990_9D7F_41A9_5C0D562F93BB.text = close questionOption_BF1A5680_B990_9D83_41DF_87F6DF8CF0AA.text = tight questionOption_BF1A5682_B990_9D87_41E5_90341458796C.text = >150 degrees questionOption_BF1A5684_B990_9D83_419C_17A72C43627E.text = 90 degrees questionOption_BF1A5686_B990_9D8F_41B2_49B54FED8B2D.text = 50 degrees questionOption_BF1A5688_B990_9D83_41E7_769DCF7D8B12.text = 15 degrees questionOption_BF1A568A_B990_9D87_41C3_3704EFC147FF.text = N - S questionOption_BF1A568B_B990_9D85_41E3_AEB1BEAC0F99.text = NE - SW questionOption_BF1A568D_B990_9D9D_41CA_3C48A1919714.text = E - W questionOption_BF1A568F_B990_9D9D_41AC_4B5B68F6A72D.text = NW - SE questionOption_C0B03514_AB6D_FBFB_41B1_000ECBF67817.text = cross bedding questionOption_C0B07513_AB6D_FBFD_41D9_C9115E4FF513.text = graded bedding questionOption_C0B0A516_AB6D_FBE7_41DA_DDCCB5EA367E.text = massive questionOption_C0B31517_AB6D_FBE5_41DC_06875633F288.text = red symbol questionOption_C0B3C518_AB6D_FBEB_41B7_1AF424468DED.text = blue symbol questionOption_C0BE4511_AB6D_FBFD_41DE_F1ED341AEBAF.text = planar laminations questionOption_C1C0F824_AA93_E9DB_41E2_04D061960105.text = a fold questionOption_C1C1082B_AA93_EA2D_41E3_4138EE3AC95B.text = a fault questionOption_C1C17829_AA93_EA2D_41C6_74553005A8B1.text = erosive channel questionOption_C1C1982C_AA93_EA2B_41A7_79F6EB5473D8.text = a dyke questionOption_C1C1B82F_AA93_EA25_41E1_DA522FF7B0E5.text = N-S questionOption_C1C28832_AA93_EA3F_41D4_6CD63B3F909A.text = E-W questionOption_C1C2C830_AA93_EA3B_41D6_B3FB4F5A50E8.text = NE-SW questionOption_C1C30835_AA93_EA25_41DB_572F67FE4200.text = NW-SE questionOption_C5406746_B991_BC8F_41E7_1CE82656741E.text = soft sediment deformation questionOption_C540B745_B991_BC8D_41BC_47B68C156D63.text = tectonic deformation questionOption_C5470744_B991_BC83_41D4_CB4A2E5FE704.text = compaction due to burial questionOption_C5470747_B991_BC8D_41C3_8A6551F2CE74.text = deformation in a hot volcanic flow questionOption_D45C170F_B990_7C9D_41E3_6D6CE83788CE.text = 220 questionOption_D45C4711_B990_7C85_41D4_1DF2BD986D6A.text = 2 cm questionOption_D45C970E_B990_7C9F_41D1_38CF0579ADEB.text = 330 questionOption_D45D470D_B990_7C9D_41D3_28FCAADD108E.text = 029 questionOption_D45D6713_B990_7C84_41E3_D27951CE4B4B.text = 20 cm questionOption_D45DD712_B990_7C87_41E5_9FFEBA0EF809.text = 7 cm questionOption_D5A3070B_B990_7C85_41DC_CBD21B0DD592.text = 0 degrees questionOption_D5A3270B_B990_7C85_41DC_42196943D98D.text = 180 questionOption_D5A3B70A_B990_7C87_41D5_F7E11EFC85A8.text = 43 degrees NE questionOption_D5A3D70A_B990_7C87_41D2_7CE000699039.text = 33 degrees NE questionOption_D5A3F70A_B990_7C87_41E5_C8BF2FE434B0.text = 50 degrees NE questionOption_DD280E16_C3E9_2F7B_41E7_F929A4AF5620.text = folding was very rapid questionOption_DD281E1B_C3E9_2F69_41D1_5719D62E1FEE.text = N-S questionOption_DD285E17_C3E9_2F79_41CC_9E4597F6B3F3.text = folding involved layer-parallel shearing questionOption_DD287E1C_C3E9_2F6F_41C7_79B4DC5D1178.text = NE-SW questionOption_DD28CE1E_C3E9_2F6B_41C2_F35226C9A9A8.text = NW-SE questionOption_DD28DE18_C3E9_2F77_41B0_87FC991B150E.text = the folds formed by an axial slip mechanism questionOption_DD28FE1D_C3E9_2F69_4162_C0B89AAA8E93.text = E-W questionOption_DD29BE19_C3E9_2F69_41E0_AA81AD538AB3.text = folds formed in response to folding questionOption_DD362E21_C3E9_2F59_41E2_9CA2DB931361.text = box folds questionOption_DD368E22_C3E9_2F5B_41B3_C4ABBF4E4CA9.text = polyharmonic questionOption_DD373E1F_C3E9_2F69_41BD_45B9BE2BE640.text = chevron questionOption_DD378E20_C3E9_2F57_41B2_BD2CE38344AD.text = ptygmatic questionOption_DD40EC94_C3E9_737F_41E7_46468D56DE29.text = focus on mapping regolith and alluvial cover questionOption_DD40FC93_C3E9_7379_41CD_3564AA765AED.text = focus on mapping metamorphic mineral assemblages to establish isograds questionOption_DD40FC99_C3E9_7369_41E7_70298C074840.text = take samples from old workings and analyse them in the laboratory questionOption_DD471C96_C3E9_737B_41C8_83CE7D341664.text = focus on mapping rock types, ductile and brittle structures, and alteration, especially near known old workings questionOption_DD471C9A_C3E9_736B_41DD_8FEA7B51A4E8.text = read academic literature on gold mineralization in the region questionOption_DD473C97_C3E9_7379_41E2_26597D07BE90.text = check historical records with the shire and/or Department of Mines Industry Regulation and safety questionOption_DD476C95_C3E9_7379_41DE_A4E2EF904970.text = focus on mapping rock textures that indicate primary depositional environments questionOption_DD47AC98_C3E9_7377_41E6_FD53775F879D.text = make a detailed geological field map of the area to develop and test the hypotheses questionOption_DDE43039_C3E9_53A9_41E1_A93406FD321B.text = sedimentary layers deposited, then folded and foliated, then intruded by a felsic dyke questionOption_DDE58038_C3E9_53B7_41D5_72F5E192EC8C.text = sedimentary layers deposited, then intruded by a felsic dyke, then folded, then foliated questionOption_E0B3A913_B9F0_B485_41DE_0AC6F1843BB9.text = ‘z’ folds questionOption_E34DB915_B9F0_B48D_41CB_361EBC7E11F8.text = ‘s’ folds questionOption_E34DE917_B9F0_B48D_41CB_CEB6F2D4BA9E.text = m’ folds questionOption_E34DF91E_B9F0_B4BF_41D3_C825450EA3BE.text = E-W questionOption_E34E891A_B9F0_B487_41D3_8BD298AE677C.text = N-S questionOption_E34E891B_B9F0_B485_41C1_4A9516AC83ED.text = NE-SW questionOption_E34F691D_B9F0_B4BD_41C1_D4904A0F9688.text = NW-SE questionOption_E470CC4C_B9F1_8C83_41A6_E52211BAC606.text = blue symbol questionOption_E47F6C4A_B9F1_8C87_41D5_AE54CC0597A3.text = red symbol questionOption_E790C9DF_B9F0_F7BD_41DA_4E1D01CC4B52.text = NE-SW questionOption_E790F9E1_B9F0_F785_41DB_35B4B911BBF7.text = NW-SE questionOption_E79199DD_B9F0_F7BD_41DF_DB7CE67BC390.text = N-S questionOption_E791F9E3_B9F0_F785_41E0_20357602E680.text = E-W questionOption_EA80D53C_A41B_38B0_41AF_77CC81B098F1.text = gradational questionOption_EA847516_A41B_3870_41E0_A5C17D485D89.text = smoothly-curved and folded questionOption_EA8A5287_A41B_5850_41C7_998AFF9138D5.text = Sigma 3 = vertical questionOption_EA8B8286_A41B_5850_41BA_69FB56BD932E.text = Sigma 3 = NNE-SSW questionOption_EA8BE518_A41B_3870_41BC_C40F5E3A2495.text = discontinuous and echelon tip zones questionOption_EA8D6541_A41B_38D0_41B6_CA70657BC553.text = stepped questionOption_EA8D7540_A41B_38D0_41D7_B7DE31D81D87.text = sharp and curved questionOption_EA8EC53E_A41B_38B0_41B0_F149E78BF4AE.text = sharp and straight questionOption_EA903546_A41B_38D0_41C7_523166CB8504.text = NE-SW questionOption_EA903547_A41B_38D0_41D9_D18DC3075451.text = E-W questionOption_EA91C545_A41B_38D0_41E4_0E423A3BE507.text = NW-SE questionOption_EA91F543_A41B_38D0_41E3_A856B55DB799.text = N-S questionOption_EAFE2284_A41B_5850_41D1_9C6AB6F59E70.text = Sigma 3 = ESE-WNW questionOption_EAFE8514_A41B_3870_41D3_993CA5E02DB4.text = truncational and faulted questionOption_EB890F10_AAAC_E7FB_41D5_F75607F5EB7E.text = 156 or 336 questionOption_EB90B616_C329_3F7B_41E5_38DA0186595E.text = all of the above questionOption_EB9ACF19_AAAC_E7ED_41C3_137515345370.text = 80 degrees northwest questionOption_EB9C7F1A_AAAC_E7EF_41CC_B2CFBE820696.text = 87 degrees northeast questionOption_EB9CAF13_AAAC_E7FD_41E4_8CD80FFFD808.text = 030 or 210 questionOption_EB9D4F18_AAAC_E7EB_41CA_E61584D54012.text = 20 degrees southwest questionOption_EB9DBF16_AAAC_E7E7_41D9_A00F0C9D38F8.text = 20 degrees northeast questionOption_EB9DDF15_AAAC_E7E5_41DD_5B0537C528BC.text = 220 or 040 questionOption_EB9F3F12_AAAC_E7FF_41E4_BA3397DFE160.text = 080 or 260 questionOption_F1283E30_F401_BBB7_41ED_635704B924DB.text = porphyritic andesite questionOption_F12845F8_F401_C8B7_41CB_BE6C79406D04.text = porphyritic granite questionOption_F1284C49_F401_DFE9_41B0_43678FE620D2.text = porphyritic dolerite questionOption_F12CA49E_F401_4F6B_41CC_9C9F8C5F8208.text = porphyritic pyroxenite questionOption_F58CD415_C369_3379_41E1_6AB6E94682E8.text = the rock is rich in magnesium questionOption_F5FA4419_C369_3369_41E2_BBE8C9B0D201.text = the rock was cooled rapidly questionOption_F5FA6418_C369_3377_41C9_5509987DCCB8.text = the rock was an intrusive igneous rock questionOption_F5FAE417_C369_3379_41C3_789091DA0567.text = the rock was originally deposited on the ocean floor questionOption_FB03274D_EC02_C9E9_41EB_F652312F1987.text = mafic questionOption_FB04174B_EC02_C9E9_41D4_6B2276AECC4C.text = granitic / felsic questionOption_FB04474F_EC02_C9E9_41BC_917A3F4668C3.text = poikilitic questionOption_FB04574E_EC02_C9EB_41DE_ED70C252C1E1.text = ultramafic questionOption_FB045755_EC02_C9F9_41E0_118C6BEBCF1F.text = plagioclase questionOption_FB047748_EC02_C9D7_41ED_864382E1F33E.text = massive, crystalline, coarse grained questionOption_FB047749_EC02_C9E9_41D6_0B1CB6CC9416.text = massive, crystalline, medium grained, porphyritic questionOption_FB04C747_EC02_C9D9_41EA_2D84E2F2384F.text = massive, crystalline, fine grained, aphyric questionOption_FB05075A_EC02_C9EB_41D5_2E9B7DB05485.text = clinopyroxene questionOption_FB051754_EC02_C9FF_41E8_61A7F3FD0D6A.text = olivine questionOption_FB051759_EC02_C9E9_41E9_F65160EBD64D.text = plagioclase questionOption_FB056752_EC02_C9FB_41B6_C9D27729032A.text = ophitic questionOption_FB056758_EC02_C9F7_41EA_C7191CD1CB4D.text = olivine questionOption_FB05974C_EC02_C9EF_41BB_FF66BDCF1BDA.text = intermediate questionOption_FB05D756_EC02_C9FB_41E9_3C27B2577FC9.text = clinopyroxene questionOption_FB05F750_EC02_C9F7_41D3_D1DAD1CB226A.text = interstitial questionOption_FB05F751_EC02_C9F9_41EC_83982FAC4DE2.text = phenocryst questionOption_FB05F757_EC02_C9F9_41D8_425B164EDF3F.text = orthopyroxene questionOption_FB06B75B_EC02_C9E9_41D4_7F99E4296B4E.text = orthopyroxene questionOption_FB1B3745_EC02_C9D9_41C8_CDDE765C8D72.text = massive, crystalline, medium grained ### Score Name score1.label = Score 1 ### Question question_0AB85928_A1C2_8CC0_41DD_53CC9CF593FD.title = Q 4/4 - Which process can lead to this kind of LREE pattern? question_0ABCB93E_A1C2_8CC0_41DA_6E2C9B62B3C8.title = Q 1/4 - This TAS diagram shows whole-rock geochemistry of several other porphyritic felsic dykes exposed within 300 m of this locality. In terms of igneous series, how are these rocks classified? question_0ABE0937_A1C2_8CC0_41E3_A77D2556F828.title = Q 2/4 - Which best describes the chondrite-normalised rare earth elements (REE) patterns preserved by these rocks? question_0ABE492F_A1C2_8CC0_41D0_FA8B9B363518.title = Q 3/4 - Which process can lead to this kind of HREE pattern? question_0C85BB8C_A1C2_83C0_41D9_A29F196C5D75.title = Q 4/4 - What inference can you make from this zircon Pb/Pb age? question_0C8A0BA5_A1C2_83C0_41C9_97DCE5A416B2.title = Q 1/4 - Study the Tera-Wasserburg diagram of zircon U-Pb data from felsic dyke sample MH35. Many data points are discordant. What reason can cause data to be spread in the direction of arrows, A, B and C. question_0C8B8B9D_A1C2_83C0_41D7_AB7275E46DF6.title = Q 2/4 -The Tera-Wassenburg diagram shows the most concordant zircon U-Pb data from felsic dyke sample MH35. Which isotype system would be most suitable for calculating an age for this rock? question_0C8BFB96_A1C2_83C0_41E0_376EC05C4F96.title = Q 3/4 - The weighted mean zircon Pb-Pb age from felsic dyke sample MH35 has been calculated from the 7 most concordant data points as 2673 +/- 8 Ma. What does the MSWD and P values tell you about the statistical validity of this age. question_0F692FC7_BB90_8B8D_41CE_5FBB4AC0E34A.title = Q 1/1 - This coarse grained, crystalline rock predominantly contains large (up to 2 cm long) lath-shaped milky-white crystals with visible twins. Identify the mineral. question_166EB33F_8031_E3D0_41BD_79857E1EFFD7.title = Q 2/2 - How would you describe the nature of the offset dyke segments? question_166F7344_8031_E3B0_41DF_04F82E2C3785.title = Q 1/2 - What is the apparent offset of the dyke in this locality? question_1BB82470_9EC6_8540_41C7_FFFA1D2DE68C.title = Q 1/1 - Using the concept of Anderson’s theory of faulting, your mapped orientation of faults, and assuming displacement is predominantly strike-slip, infer the orientation of the principal stresses (sigmas 1, 2 and 3) during faulting. question_1D5BF762_8030_A270_4198_6E8E50F5C34B.title = Q 1/1 – The image shows a dark red-weathering rock fragment inclusion – a xenolith. \ Based on its weathering colour, what was likely to be its original composition? question_1FCC1ABE_8030_E2D0_41D5_998C2A704CF0.title = Q 1/2 – What is the form of the small black crystals seen in the image? question_1FCE4AB2_8030_E2D0_41E0_040C0F2A64F4.title = Q 2/2 – These crystals have been oxidised in the weathered zone. What mineral could these have been? question_21F9F5F4_B88F_9F83_41DE_971D28103FF8.title = Q 1/5 - This rock type is green on a fresh surface and predominantly comprises medium grained stubby prismatic green crystals. Identify this mineral. question_21FAF5EE_B88F_9F9F_41B5_2E8F4479B616.title = Q 2/5 - This rock contains ~5% larger prismatic pale green crystals up to 1 cm long with two visible cleavages at ~90 degrees. Identify this mineral. question_21FC95E9_B88F_9F85_41DF_6C43D81856AE.title = Q 3/5 - What textural term is used to describe a rock with larger crystals in a crystalline groundmass? question_21FD15E3_B88F_9F85_41D3_55FF18DFB4A1.title = Q 4/5 - Classify this rock type. question_29554D7D_C4F4_A894_41C7_1DE071658053.title = Q 1/1 - From the trace element geochemistry data of Smithies et al. (2018), what were likely magmatic source(s) of rocks from the Kalgoorlie-Kambalda greenstone belt? question_2CE4CD5B_C4F4_689C_41E1_EBD2B6D0E5AF.title = Q 1/1 - Approximately how large are the pillows in this location? question_2E0955DE_B88F_9FBF_41D2_9F105BF7CBBC.title = Q 5/5 - Which name best classifies this rock type? question_2E829C22_C4F7_A8AC_41E6_FF4717B0009C.title = Q 1/2 - What environment can be interpreted from the presence of pillow structures? question_2EFD1C1E_C4F7_A894_41E3_530E20C06464.title = Q 2/2 - What tectonic environment would be compatible with the presence of pillow lava? question_2FCA4BFF_C4F7_AF94_41D8_3D138CA06827.title = Q 1/1 - Pillows have domed tops and pinched bases (keels). Using the compass and the shape of the pillows, decipher the younging direction. question_48BA5AA6_BB91_958F_416E_621F1F0A5288.title = Q 1/1 - What inference can be made about the formation of this rock? question_49665C53_BB90_8C85_41C1_574719CD05AE.title = Q 1/1 - What inferences can you make from the presence of spinifex texture? question_4A4C74D9_BB90_7D85_41E0_6FC305CB6CAB.title = Q 1/1 - What inference can be made about the formation of this rock type? question_4A965996_BB91_978F_41E4_C6091B66AAD6.title = Q 1/1 - What inference can be made about the formation of this rock type from its texture? question_4B3B3A4D_BB91_B49D_41C3_D4CF91F480BB.title = Q 1/1 - This rock is <1 m wide and cross cuts the speckled rock type. What inference can you make about the formation of this rock type from its texture, composition, and field relationship? question_4E7998ED_BB93_959D_41B2_CD22559E47C0.title = Q 1/1 - What inference can be made about the formation of this rock? \ \ question_5179D1EA_BB90_B787_41DC_758483DFF1E8.title = Q 1/1 - What inference can be made about the formation of this rock? question_53F6B188_BBF7_9783_41C9_0F886F01C0B1.title = Q 2/2 - Given that the boundary can be constrained to within 10 cm here, what type of boundary symbol should be shown when mapping at a 1:2000 scale? question_58AEAD19_BBB1_8C85_41E7_69FD00F086CE.title = Q 4/4 - Which field term best fits this rock type? question_58B26D23_BBB1_8C85_41E1_D4BE23A0FC40.title = Q 2/4 - What can be inferred from the pale colour of the groundmass of this fine grained, massive, crystalline rock type? question_58B3FD1E_BBB1_8CBF_41C7_2A54B878074B.title = Q 3/4 - What textural term is used to describe a rock with larger crystals in a crystalline groundmass? question_58B4FD27_BBB1_8C8D_41C6_F6E501D879D4.title = Q 1/4 - This rock type contains <5% milky-white weathering prismatic crystals up to 3mm long. question_60A8D8B6_BB8F_958F_41DD_32CDD00A9084.title = Q 1/2 - Using the compass, what is the approximate trend of the contact between the rock types? question_6172D5EF_BB8F_9F9D_41CF_820B65CDEF7A.title = Q 1/2 – This green, fine-grained crystalline rock contains abundant large (up to 5cm long), needle-shaped (acicular) crystals arranged distinctively in a random and interlocking way. Which term best describes this texture? question_6172F5E7_BB8F_9F8D_41CB_41507FF8308D.title = Q 2/2 – Which field name best for this rock? question_62A95AED_BB91_959D_41CA_E49196EC74E8.title = Q 1/1 - This rock is fine grained, grey green on a fresh surface, massive, crystalline, and aphyric. Identify this rock type. question_63017B8E_BB90_8B9F_41D0_8272D5580D8E.title = Q 1/1 - This rock is medium grained, massive, crystalline, and ~50% plagioclase and ~50% mafic minerals. Identify this rock type. question_88312B0E_C329_356B_41C8_CA06F0FC53A5.title = Q 1/1 - Using the compass, estimate the approximate trend of the foliation. question_94A648D3_A994_EA7D_41DD_A64E58B749A7.title = Q 2/3 - Identify the mineral clast under the hand lens. question_94A6A8D9_A994_EA6D_41E3_FC2C3CBCAC66.title = Q 3/3 - The translucent grey mineral clast has a hexagonal shape and is resistant to weathering. Identify the mineral. question_94ABF8CD_A994_EA65_41E1_642C8A2E2D18.title = Q 1/3 - Classify the pale pebble clasts in this domain. question_9E0295EE_A9B5_DA27_41E3_A8BDD8C64A76.title = Q 3/3 - What best describes the sedimentary structures? question_9E05D5EA_A9B5_DA2F_41CD_B6D27DD47405.title = Q 2/3 - What best describes the sedimentary structures? question_9E1865E6_A9B5_DA27_41DF_AFB7D167378E.title = Q 1/3 - What do the pale colours of the rock layers imply? question_9EC3F02F_B970_F49D_41CD_0C7532704B05.title = Q 2/2 - Which younging symbol is correct to indicate way-up from the channel bedform? question_9ECCB034_B970_F483_41E2_E55B622FDDB9.title = Q1/2 - To the left of the compass is a small channel bedform. What does this imply about the environment of deposition? question_A282B359_CD94_F89C_41CA_A5109ADDE8DB.title = Q 2/3 - This igneous rock contains crystals up to 10 cm long in a groundmass of ~0.5cm crystals. What term best classifies this texture? question_A282B35D_CD94_F894_41CD_69B0A4E30CCC.title = Q 1/3 - This igneous rock type contains ~50% plagioclase and ~50% pyroxene. How is it classified? question_A28D8355_CD94_F894_41D1_98507CC73E74.title = Q 3/3 - Which is the most suitable field name for this rock type? question_A2BC80DC_CD94_9994_41D8_D7D5281C7D66.title = Q 1/1 - This igneous rock type comprises entirely blocky green crystal of pyroxene. Which term best classifies this rock type? question_A2FC1D02_CD94_A86C_41C4_281A99723208.title = Q 1/2 - Give a field name for this igneous rock which is fine grained, aphyric, green-grey, and weathers into smooth rounded boulders. question_A2FC4CFE_CD94_A994_41B8_A2653EE4540C.title = Q 2/2 - What term describes curved fracture surfaces preserved by this rock type? question_A3BBFDAF_C56F_ECA9_41D8_B3C1F3A5A71E.title = Q 1/1 - The shapes of the pillows define domes (convex pillow tops) and keels (pinched pillow bases). Using your interpretive sketch, interpret the way up from the pillow forms. question_A3CC9EBA_C56F_2CAB_41D4_58FE4C783E9E.title = Q 2/2 - What is the most likely cause of the laminations at pillow margins? question_A3CC9EBF_C56F_2CA9_41DD_81B9BB018BFB.title = Q 1/2 – Which is the best description of the rinds of the pillows? question_A424D6DA_CD95_F99C_41E8_6EF2C4ADB92F.title = Q 1/2 - How does the silica and total alkali composition of pegmatitic gabbro sample MH58 compare to other mafic rocks in the area? question_A42546D6_CD95_F994_41B6_A3D18737F6B7.title = Q 2/2 - Which description best fits the trace element distribution relative to MORB for pegmatitic gabbro sample HM58? question_A451259B_CD95_9B9C_41D1_2507F1E17507.title = Q 1/2 - What terms best describe the form of pale green minerals? question_A4538597_CD95_9B94_41D0_22E52A4FD4D5.title = Q 2/2 - Identify the bladed crystals with simple twins and third order interference colours. question_A5184260_CD94_98AC_41D8_762F12061F78.title = Q 1/1 - Which interpretations are consistent with your findings from the three rock types at this locality? question_A5992150_CD95_B8EC_41CB_048B0FE9FC53.title = Q 1/3 - Which term describes the texture defined by the shapes of pseudomorphed primary pyroxene grains in this location? question_A59BB14C_CD95_B8F4_41E2_39186C6B3069.title = Q 2/3 - What process of formation can be inferred from this texture? question_A59BD148_CD95_B8FC_41CE_6E9077F9FD7B.title = Q 3/3 - What mineral has replaced (pseudomorphed) primary clinopyroxene grains? question_A5E045EF_CD94_7BB4_41C9_5490ECBA0820.title = Q 1/1 - What interpretations can be made from field relationships among rock types shown on the map of location 7? question_AC58A1F1_C56F_54B9_41E3_5EBEA7CE6ED9.title = Q 1/2 - Varioles are pale green spherulitic, dumb-bell, and globular forms. Estimate the proportion of this rock comprised of varioles. question_AC5E21E8_C56F_54D7_41D2_D8439E65E7DA.title = Q 2/2 - Varioles are paler than the surrounding rock. What can be inferred from this? question_ACC053AD_C56E_D4A9_41E0_9DF5D21248BF.title = Q 2/4 - At this scale, describe the margins of the varioles. \ \ question_ACC0C3A8_C56E_D557_41DD_6F9BC3C9BA10.title = Q 3/4 - What texture is visible in the varioles in cross polarized light? question_ACC103A2_C56E_D55B_41DA_F365B6BC5CF0.title = Q 4/4 - What is the best interpretation of varioles and how they formed? \ \ question_ACC223B2_C56E_D4BB_41DB_0455BFC38384.title = Q 1/4 - From the optical photomicrograph of the variolitic basalt, how would you describe the texture of the varioles? question_AD64C82C_C56E_F3AF_41D9_1F0911D2A670.title = Q 1/2 - With which group of rocks does a variolitic sample from this locality (MH30) have the closest affinity on the trace element diagram. question_AD653827_C56E_F359_41E7_A66190D7AE48.title = Q 2/2 - The variolitic sample MH30 is enriched in silica relative to other basaltic rocks in the area. What could be reason for this? question_AE6A48F8_B890_9583_41A5_F54262E2EB65.title = Q 2/2 - What process could have made the clasts be elongate like this? question_AE6B58FD_B890_957D_41C5_9D37129A7FF8.title = Q 1/2 - Identify the elongate clasts in this image. question_BE9FC432_B88F_FC87_41D2_DC86C4286B08.title = Q 3/3 - Depletion of heavy rare earth elements (HREE) is attributed to melt extraction from a source containing what mineral? question_BE9FC43A_B88F_FC87_41A0_CD49FAD764E0.title = Q 2/3 - How is MH55 distinguishable from MH56 based on trace elements? question_BE9FC441_B88F_FC85_41D9_2B7210A45E76.title = Q 1/3 - Sequence the samples from the least evolved to the most evolved. question_BEA1F339_B8B3_9485_41E5_8DA917E47F50.title = Q 2/2 - Sequence the samples from the least evolved to the most evolved. question_BEA1F33F_B8B3_94FD_41E0_15DE20766BD6.title = Q 1/2 - Why do pyroxenites plot along the x-axis? question_BEE2D25A_B8B1_9487_417A_F865CE796D9E.title = Q 2/2 - Does the felsic dyke cross cut the foliation? question_BEE2D25F_B8B1_94BD_41D8_47AF8A09BA83.title = Q 1/2 - This felsic dyke has extruded metasedimentary rocks. Using the compass what is the approximate orientation of the foliations in the lower left of the image? question_BEE50F83_B8B0_8B85_41E2_184DEE5440C5.title = Q 1/1 - Which best describes the orientation of bedding in these metasedimentary rocks? question_BF09034E_B970_749F_41C3_D7F0C86D724A.title = Q 2/2 - Which best describes the orientation of the foliation in this ferruginised basalt? question_BF090353_B970_7485_4199_497441799472.title = Q 1/2 - Which best describes the texture of the rock type on the right? question_BF1A1E32_B990_8C87_41D6_13F3B4A3744F.title = Q 4/4 - Classify the fold based on its interlimb angle. question_BF1A1E3B_B990_8C85_41D6_44021C07F6F0.title = Q 3/4 -Given that the surface with the compass is horizontal, and the fold hinge is exposed in the foreground, classify this fold based on the plunge of its hinge. question_BF1A1E42_B990_8C87_41D7_9F1FC5003135.title = Q 2/4 - Given that the surface with the compass is horizontal, and the fold hinge is exposed in the foreground, classify this fold based on the plunge of its hinge. question_BF1A1E4A_B990_8C87_41DD_36EA26667863.title = Q 1/4 - Using the compass, what is the approximate trend of the axial surface of this fold? question_BF1A3ECA_B990_8D87_41DE_5C91112FCD4A.title = Q 2/2 - Using the compass, what is the approximate trend of this foliation? question_BF1A3ED1_B990_8D85_41CA_2B3486E8C69C.title = Q 1/2 - A foliation can be seen in the hinge zone of this fold layered metasedimentary rock. What best describes this foliation? question_BF1A567A_B990_9C87_41D9_9E0E37D1ADAB.title = Q 3/3 - Classify the fold adjacent the compass based on its interlimb angle. question_BF1A5682_B990_9D87_41DF_3DDE05BD4C4F.title = Q 2/3 - What is the approximate interlimb angle of the fold adjacent the compass? question_BF1A5689_B990_9D85_41DA_6D8459BA5D7A.title = Q 1/3 - Several fold hinges are preserved at this outcrop. What is the approximate trend of the axial surfaces? question_C0B36517_AB6D_FBE5_41E0_A5880BDBF2AA.title = Q 2/2 - Which younging symbol is correct? question_C0BF8511_AB6D_FBFD_41E4_C88DE037ADDD.title = Q 1/2 - What structures are present in the layer between the white arrows? question_C1C0E823_AA93_E9DD_41E0_486D968DAB27.title = Q 1/2 - Identify the structure that is responsible for truncating layers in this location? question_C1C2682E_AA93_EA27_41B7_1AD931057C10.title = Q 2/2 - Use the compass to measure the trend of this structure. question_C5473744_B991_BC83_41CA_B2F6055E2EB9.title = Q 1/1 - Layers have been pulled apart to form lozenge-shaped blocks. What process could do this? question_D45C3711_B990_7C85_41E5_4E75A4ADC112.title = Q 1/3 - Approximately how thick is the in situ quartz vein? question_D5A3170B_B990_7C85_41E3_5CFD045E0E50.title = Q 2/3 – Use the compass to measure the strike of this quartz vein \ \ question_D5A3A70A_B990_7C87_41DE_85E9E4555A69.title = Q 3/3 - Use the compass to measure the dip of this quartz vein question_DD280E1B_C3E9_2F69_41E3_4018810AD684.title = Q 2/3 - Using the compass, what is the approximate trend of the axial surface of these small folds? question_DD283E16_C3E9_2F7B_41D9_CE0E9DB02876.title = Q 3/3 - What inference can you make about the deformation that caused this style of folding? question_DD37AE1F_C3E9_2F69_41E2_1DCC0BB073C4.title = Q 1/3 - Which term best describes the geometry of the small folds localized in the layers above the compass? question_DD40CC93_C3E9_7379_41E4_129F4939A8EF.title = Q 2/2 - How would you prioritise geological field mapping tasks to explore for more orogenic gold deposits? question_DD470C97_C3E9_7379_41E0_4DBDA70ECB8A.title = Q 1/2 - How would you best go about deciphering the geological reasons why old timers found gold where they did. question_DDE46038_C3E9_53B7_41DB_52C94F27A4AB.title = Q 1/1 - What inferences can be made about the relative geological history from this outcrop? question_E0B36913_B9F0_B485_41E6_075CDA70CA9A.title = Q 2/2 - What is the asymmetry of the small scale folds? question_E34EB91A_B9F0_B487_41D5_E4432EAFB653.title = Q 1/2 - What is the approximate trend of the axial trace of the small scale folds? question_E47F8C49_B9F1_8C85_41D0_246D8B95347F.title = Q 1/1 – What is the correct younging symbol assuming fining-upwards of the graded bedding? question_E79189DD_B9F0_F7BD_41DF_75F2D42AC089.title = Q 1/1 - Using the compass, what is the approximate trend of the antiform? question_EA80153C_A41B_38B0_41CE_58F71FB01416.title = Q 1/2 - Which best describes the nature of contact? question_EA910543_A41B_38D0_41AF_4ECE0CC0E870.title = Q 2/2 - What is the approximate trend of the contract? \ \ question_EAFE6284_A41B_5850_41D7_AA4CA9B2EDC3.title = Q 1/1 - Using the concept of Anderson’s theory of dykes and sills and the orientation of the dyke, infer the orientation of the minimum principal stress (sigma 3) during dyke emplacement. question_EAFEC514_A41B_3870_41C3_8B9BE1D62094.title = Q 1/1 - Which describes and explains the nature of the offset of the dyke in this locality. question_EB894F10_AAAC_E7FB_41D3_7D4DE5A6E342.title = Q 1/2 - What is the strike of bedding? question_EB9D9F16_AAAC_E7E7_41D3_AA8F504444B9.title = Q 2/2 - What is the dip and dip direction of bedding? question_F12832F6_F401_48BB_41D5_62D8C27241F0.title = Q 6/6 - Based on meinerals present in the rock, which name best classifies this rock type? question_F58D1415_C369_3379_41E6_0502ED8B3461.title = Q 1/1 - What can you infer from the presence of talc at this outcrop? question_FB04574F_EC02_C9E9_41CE_221B6E568F06.title = Q 3/6 - White-weathering plagioclase fills the gaps between the well-defined green and red-weathering crystals. What is the term for this? question_FB056753_EC02_C9F9_41E5_BA5BFA6A5342.title = Q 2/6 - The smaller, dark green crystals in this rock form stubby prisms. Which mineral are these most likely to be? question_FB057758_EC02_C9F7_41E8_C6D0A92196E2.title = Q 1/6 - The larger red-wearing crystals (phenocrysts) in this rock are prismatic and have two cleavages almost at 90 degrees. Which mineral are these most likely to be? question_FB05E74A_EC02_C9EB_41CB_8100055D492E.title = Q 4/6 - Classify this rock type. question_FB1B7745_EC02_C9D9_416A_617A1D62C43E.title = Q 5/6 - Which describes the texture of this rock type? ### Question Screen quizQuestion_6BF6E879_7AC3_DB4A_41D0_A4C5A55A61B3.ok = OK ### Report Screen quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.completion = Completed quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.downloadCSV = Download .csv quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.elapsedTime = Time quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.items = Items Found quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.questions = Questions quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.questionsCorrect = Correct quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.questionsIncorrect = Incorrect quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.repeat = Repeat quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.submitToLMS = Submit quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.title = - SCORE - ### Timeout Screen quizTimeout_6BF79879_7AC3_DB4A_41DC_B9FEB819D849.repeat = Repeat quizTimeout_6BF79879_7AC3_DB4A_41DC_B9FEB819D849.score = View Score quizTimeout_6BF79879_7AC3_DB4A_41DC_B9FEB819D849.title = - TIMEOUT -