deformation
This is false,cirques are caused when erosion at the beginning of a glacier wears down the walls of mountain peaks.Over time,this process creates bowl-shaped basins called cirques.
Mountains erode continuously. Erosion may be by water (rain or rivers), ice (glaciers) or wind.
Glaciers can carry both small particles and large boulders. The erosion caused by glaciers is caused by the rocks and debris carried along with the ice, NOT the ice itself.
the wind and rain mixed together makes a powerful force that over millions of years can erode the mountain side down. In dry areas there is less rain but there is wind. The wind can push sand and other objects against mountains also eroding the mountain slowly.
Wind and rain can slowlt erode away Mt. Rushmore leaving nothin but a small mountain or hill.
horn
Glacial horn
CONE
This is false,cirques are caused when erosion at the beginning of a glacier wears down the walls of mountain peaks.Over time,this process creates bowl-shaped basins called cirques.
horn
Look at textbook EARTH SCIENCE pg: 198-200
Arêtes can form in two ways. They can form when two glaciers erode parallel U-shaped valleys, or they can form when two glacial cirques erode headwards toward one another, although frequently this results in a saddle-shaped pass, called a col.
Ussually by three cirques A cirque is an origin point for glaciers in mountainous areas. It is a deep depression with three high walls and an open area from which the glacier moves forward, down the mountain side. Over time, as rock is eroded, these become wider and deeper. A mountain horn, such as the Matterhorn in the Alps forms when a peak is surrounded on two or more sides by cirques. As the cirques expand and rock is eroded the peak is honed into a point, forming a horn.
Answer: Cirques
The matterhorn is an arete or pyramidal peak. Formed as three glacial cirques erode back into mountainside.
An arête is a thin ridge of rock which is formed when two glaciers erode parallel U-shaped valleys. The arête is a thin ridge of rock that is left separating the two valleys Arêtes can also form when two glacial cirques erode head wards towards one another, although frequently this results in a saddle-shaped pass, called a col. The edge is then sharpened by freeze-thaw weathering. Where three or more cirques meet, a pyramidal peak is created. - (a famous example is the 'Matterhorn'). Form the above it must be clear that arêtes are landforms found in mountainous terrains that have been subject to glaciation. They are therefore very common in the Alps.
Wind can erode topsoil.Drugs erode family values.