Kames and eskers are composed of till, hydrodynamically shaped by glacial ice and meltwater.
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Q12: U-trough valleys are characteristic of continental glaciers.
Q13: For valley glaciers, the cirque is the
Q14: Glacial drift refers to the poorly-sorted and
Q15: The difference between glacial till and outwash
Q16: Moraines are formed from outwash bulldozed by
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Q19: During the Pleistocene, the semiarid and arid
Q20: Isostatic rebound occurs because glacial ice causes
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Q22: During an Ice Age, which of the
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