A pediment is a very gently sloping (.5°-7°) inclined bedrock surface. It typically slopes down from the base of a steeper retreating desert cliff, or escarpment, but may continue to exist after the mountain has eroded away. It is caused by erosion. It develops when sheets of running water (laminar sheet flows) wash over it in intense rainfall events. It may be thinly covered with fluvial gravel that has washed over it from the foot of mountains produced by cliff retreat erosion. It is typically a concave surface gently sloping away from mountainous desert areas.
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It is not to be confused with merged groups of alluvial fans (bajadas), which also may appear to gently slope from an escarpment, but are composed of material eroded from canyons, not bedrock.
Three formational zones are recognized for pediments:
Coalescence of pediments over a large area results in a pediplain.
Processes responsible for carving pediments
History
In 1877 Grove Karl Gilbert first observed pediments in the Henry Mountains in Utah. He described the formation as "hills of planation cut across the upturned edges of tilted beds". Gilbert believed the origin of pediments in the Henry Mountains are due to stream planation and active erosion of deserts. This theory was advocated by Paige (1912), Blackwelder (1931), and Johnson 1932. Johnson came up with three zones of pediments.