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A major characteristic of graded bedding is that the rock layers ____. are thick

ID: 157761 • Letter: A

Question

A major characteristic of graded bedding is that the rock layers ____.

are thick and easily distinguished from each other

show an upward decrease in grain size

formed because turbidity currents are less dense than sediment-free water

contain intersecting fractures called mud cracks

are always formed in deserts

a.

are thick and easily distinguished from each other

b.

show an upward decrease in grain size

c.

formed because turbidity currents are less dense than sediment-free water

d.

contain intersecting fractures called mud cracks

e.

are always formed in deserts

Explanation / Answer

c is the rigt answer, graded bedding means change in grain and clay size from the base to the bed . this is because chaneg in the currents and so there movement . they are also easily detactable as the size vary from one grade to another.

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