The area of sediment deposit by by glaciofluvial action beyond the glacial terminus is known as the
A) till plain.
B) terminal moraine.
C) outwash plain.
D) end moraine.

Question

Quizplus · Accepted Answer

The area of sediment deposit beyond the glacial terminus is known as the outwash plain. This is a flat or gently sloping plain that has been formed by meltwater streams that carry sediment away from the glacial terminus. The outwash plain is also known as the valley train, and it is typically composed of sand, gravel, and other sediment that has been sorted and deposited by the meltwater streams. The other options, such as the till plain, terminal moraine, and end moraine, refer to different types of glacial landforms, but they do not specifically refer to the area of sediment deposit by glaciofluvial action beyond the glacial terminus.

The Area of Sediment Deposit by By Glaciofluvial Action Beyond