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A scarpIn geology, a scarp is a type of cliff. See escarpment . See also Scarp, Scotland. is a type of cliff, formed by contraction .
Most cliffs have some form of talusTalus (which is Latin for ankle-bone), has several meanings: in mountaineering and climbing, talus is small broken rock found on mountain slopes and at the base of cliffs. It is used interchangeably with scree. in Greek mythology, Talus is an alternate sp slope at their base. In arid areas or under high cliffs, these are generally exposed jumbles of fallen rock. In areas of higher moisture, a soilSoil is the layer of minerals and organic matter, in thickness from centimetres to a metre or more, on the land surface. Its main components are mineral matter, organic matter, moisture, and air. Soils differ in the ratio of these components. Modern soil slope often obscures the talus.
Many cliffs also feature waterfallTower Fall in Yellowstone National Park A waterfall is usually a geological formation resulting from water, often in the form of a stream flowing over an erosion-resistant rock formation that forms a sudden break in elevation. Waterfalls may also be artifs or rock shelterA rock shelter is a shallow cave-like opening at the base of a bluff or cliff. Another term is rockhouse. Rock shelters form because a rock stratum such as sandstone that's resistant to erosion and weathering has formed a cliff or bluff, but a softer stras. Sometimes a cliff peters out at the end of a ridge, with tea tables or other types of rock columns remaining.
Some of the highest cliffs in the United States are to be found at Yosemite National Park in California, where some are three thousand feet (almost one thousand meters) high.
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