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After prolonged drought, which topographical consequence develops because of aeolian deflation?

A)Lag deposits (desert pavement) form
B)Barchan dunes become parabolic dunes
C)Yardangs elongate along wind direction
D)Sand seas stabilize through vegetative cover

💡 Explanation

Lag deposits form because wind deflation winnows away fine particles, leaving behind larger rocks and gravel; this forms desert pavement. The result is surface armouring, therefore protecting the underlying sediment rather than processes affecting shifting dunes, stabilization or yardang formation.

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