They are formed by the downcutting of a river or stream channel into and the abandonment and lateral erosion of its former floodplain.
2.
The south side of the mountain has a broad shelf at a height of around 450 metres, the result of lateral erosion by glaciers in the Ice Age.
3.
This can happen as a result of tectonic uplift ( or subsidence ), natural damming created by a landslide, or headward or lateral erosion of the watershed between adjacent basins.
4.
While similar in general appearance, the mechanism behind the formation of interlocking spurs is different from that behind meanders, which arise out of a combination of lateral erosion and deposition.
5.
The downcutting, abandonment, and lateral erosion of a former floodplain can be the result of either changes in sea level, local or regional tectonic uplift; changes in local or regional climate; changes the amount of sediment being carried by the river or stream; change in discharge of the river; or a complex mixture of these and other factors.
6.
The early stage is characterized by narrow, V-shaped and steeply-sloping valleys at high elevation and relief with vertical erosion exceeding lateral erosion, the middle stage with U-shaped valleys with narrow floodplain where lateral erosion exceeding vertical erosion, and the late stage by broad U-shaped valleys with wide floodplains, extreme lateral erosion and peneplanation.
7.
The early stage is characterized by narrow, V-shaped and steeply-sloping valleys at high elevation and relief with vertical erosion exceeding lateral erosion, the middle stage with U-shaped valleys with narrow floodplain where lateral erosion exceeding vertical erosion, and the late stage by broad U-shaped valleys with wide floodplains, extreme lateral erosion and peneplanation.
8.
The early stage is characterized by narrow, V-shaped and steeply-sloping valleys at high elevation and relief with vertical erosion exceeding lateral erosion, the middle stage with U-shaped valleys with narrow floodplain where lateral erosion exceeding vertical erosion, and the late stage by broad U-shaped valleys with wide floodplains, extreme lateral erosion and peneplanation.
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