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7.2 and 7.3 Deserts and Winds

Across
A flat area on the floor of an undrained desert basin (playa) that fills and become a lake after heavy rain
A fan-shaped deposit of sediment formed when slope is abruptly
Solitary sand dunes shaped like crescents
Streams that carry water only after it rains
MUCH OF THE DEBRIS IN DESERT IS A RESULT OF WHAT?
Deposits of windblown silts, lacking visible layers, generally light yellow, and capable of maintaining a nearly vertical clit
This dunes is also called (sand seas)
A layer of coarse pebbles and gravel created when wind removed the finer material
Down
They look like backward barchans
Are long ridges of sand that form parallel to the prevailing wind
Form that is intermediate between a barchan and transverse
The source of most desert erosion
Are isolated hills of sand mostly found in parts of the Sahara and Arabian deserts
A hill or ridge of wind-deposited sand