Learning GOAL You will examine a complex series of rock layers and ide.pdf
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Learning GOAL You will examine a complex series of rock layers and identify which stuctural features are importam for determining the geologic history. This will help you to classify the nature of a major unconformity and describe its geologic. rignificure. A Figure AB.6.1A is a photogriph of part of the bottom of the Gind Canyon, which extends cast io west acros nonhem Arizona Tac photo was taken wes of Grand Canyon Vilage on the south rim of the Canyon, looking at the north side of the botsom of the canyoa. Carefaliy analyme the phoiograph for roct. layering. The very botiom rock layers in the foreground are folded Precamibrian metannombic rock called the Vishinu Schis, whech contains narrow white bodier of igneous rock. The Vichna Schist is oresiain here by relatively horizontal layers of sedincatary rock. Figure A 8.6.1 1. Using a pen or colored pencil on Fig. A8.6.18, carefully trace the contact between the Vishnu Schist and the relatively horizontal sedimentary rocks abone it. 2. Based on Figs. 8.2-8.10, what specific kind of uneonformity occurs along the contact you just traced on Fig. A8.6.1B? B REFLECT \&. DISCUSS The Vishnu Schist has a numerical age of about 1700 million years. The Lower Cambrian Tapeats Sandstone was deposited on top of the unconformity that yoe considered in part A . Imagine that you find reliable infor: mation indicating that the Tapeats Sandstone was deposited at the very start of the Cambrian Period. About bow much time is represented by the rock record that is "missing" across this unconformity-missing in the sense of erosion, nondeposition, of both prior to deposition of the Tapeats Sandstone on the erosional surface at the top of the Vishnu Schist? C Figure A8.6.2A is another photograph of part of the bottom of the Grand Canyon. The photo was taken east of Grand Canyon Village on the south rim of the Canyon, looking at the north side of the canyon. All of the rocks in this scene are sedimentary rocks. 1. Analyze this canyon scene. Then, using a pen or colored pencil on Fig. A8.6.2B, carefully trace the contact that marks a significant unconformity in the photo. 2. What kind of unconformity did you identify? Figure A 8.6.2 D REFLECT \& DISCUSS What evidence did you apply to justify drawing an unconformity where you did on Fig. A8.6.2.
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Kouris Company Consolidated Balance Sheets
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Dec. 31
Year 2 Year 1
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Current assets:
Cash and cash equivalents $ 634.0 $ 575.5
Accounts receivable, net of allowance 2,101.1 1,804.1
Inventories 1,514.9 1,373.8
Other current assets 429.9 401.3
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Property, plant, and equipment, net 1,620.8 1,614.5
Other long term assets 413.2 670.8
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Notes payable 75.4 425.2
Accounts payable 572.7 504.4
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Income taxes payable 107.2 83.0
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Unearned stock compensation (0.6) (5.1)
Accumulated other comprehensive loss (239.7) (192.4)
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Total stockholders' equity 3,990.7 3,839.0
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Income taxes 382.9
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Inventories 27.2 28.4
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Accrued liabilities 7.8 5.6
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Accumulated other comprehensive loss (0.9) (1.3)
Treasury stock (6.3) (5.4)
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Total stockholders' equity 68.7 63.2
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## streaming on ostream
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Natural birth techniques - Mrs.Akanksha Trivedi Rama University
Learning GOAL You will examine a complex series of rock layers and ide.pdf
- 1. Learning GOAL You will examine a complex series of rock layers and identify which stuctural features are importam for determining the geologic history. This will help you to classify the nature of a major unconformity and describe its geologic. rignificure. A Figure AB.6.1A is a photogriph of part of the bottom of the Gind Canyon, which extends cast io west acros nonhem Arizona Tac photo was taken wes of Grand Canyon Vilage on the south rim of the Canyon, looking at the north side of the botsom of the canyoa. Carefaliy analyme the phoiograph for roct. layering. The very botiom rock layers in the foreground are folded Precamibrian metannombic rock called the Vishinu Schis, whech contains narrow white bodier of igneous rock. The Vichna Schist is oresiain here by relatively horizontal layers of sedincatary rock. Figure A 8.6.1 1. Using a pen or colored pencil on Fig. A8.6.18, carefully trace the contact between the Vishnu Schist and the relatively horizontal sedimentary rocks abone it. 2. Based on Figs. 8.2-8.10, what specific kind of uneonformity occurs along the contact you just traced on Fig. A8.6.1B? B REFLECT &. DISCUSS The Vishnu Schist has a numerical age of about 1700 million years. The Lower Cambrian Tapeats Sandstone was deposited on top of the unconformity that yoe considered in part A . Imagine that you find reliable infor: mation indicating that the Tapeats Sandstone was deposited at the very start of the Cambrian Period. About bow much time is represented by the rock record that is "missing" across this unconformity-missing in the sense of erosion, nondeposition, of both prior to deposition of the Tapeats Sandstone on the erosional surface at the top of the Vishnu Schist? C Figure A8.6.2A is another photograph of part of the bottom of the Grand Canyon. The photo was taken east of Grand Canyon Village on the south rim of the Canyon, looking at the north side of the canyon. All of the rocks in this scene are sedimentary rocks. 1. Analyze this canyon scene. Then, using a pen or colored pencil on Fig. A8.6.2B, carefully trace the contact that marks a significant unconformity in the photo. 2. What kind of unconformity did you identify? Figure A 8.6.2 D REFLECT & DISCUSS What evidence did you apply to justify drawing an unconformity where you did on Fig. A8.6.2