The Solid Earth - Chapter 4: The Evolution of a Desert Landscape Flashcards

1
Q

Deserts are characterized as having interior drainage because they lack permanent ____

A

streams

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2
Q

T/F: Interior drainage implies a discontinuous pattern of intermittent streams that do not flow out of the desert to the ocean

A

True

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3
Q

In the ____ stage of landscape evolution, relief is greatest for as erosion lowers the mountains and sediments fill the basins, elevation differences diminish

A

early

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4
Q

The result of debris collected in a cone at the mouth of a canyon after runoff is an ______

A

alluvial fan

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5
Q

Moving down the alluvial fan, the size of the sediment and steepness of slope ____ and merge with the basin floor

A

decrease

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6
Q

When rainfall is abundant, streams may flow across the alluvial fans to the center of the basin with a shallow ___

A

playa lake

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7
Q

After playa lakes are evaporated and infiltrated, the bed that remains is called …

A

playa

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8
Q

An example of playa lake deposits that can be mined is ____ from Death Valley

A

borax

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9
Q

A ____ is formed with time as the mountain front is worn back and a sloping bedrock platform emerges

A

pediment

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10
Q

With the ongoing dissection of the mountain mass into an intricate series of ____ and divides, the local relief continues to diminish

A

valleys

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11
Q

The steady retreat of the mountain front elarges the ___ over time

A

pediment

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12
Q

By the late stages of erosion, the mountain areas are simply bedrock knobs above pediment and sediment basins, and these isolated erosional remnants are called _____

A

inselbergs

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