How would you explain flattening strain in a shear zone with a clear strike-slip offset?
What will be an ideal response?
Answer: Flattening strain in a (strike-slip) shear zone forms when there is shortening across the zone. This can be the result of anisotropic volume loss, but the shortening is more likely to be compensated by extension in a perpendicular direction, in which case we have transpression.
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Where are the highest sheet and rill erosion rates and resultant loss of cropland in the U.S.? What will be an ideal response?
Match the glacial landform with the material it is made of. (Note: Some answers will be used more than once.)
A) Solid rock B) Till C) Sands and gravels 1) Outwash plain 2) End moraine 3) Erratic 4) Esker 5) Drumlin 6) ArĂȘte
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____ is the world leader in wind energy production
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