WebV-shaped Valley. A valley which resembles a 'v' in cross section. These valleys have steep sloping sides and narrow bottoms. Interlocking Spur. Spurs are the 'fingers' (ridges) of more resistant rock around which a … Web9 de jun. de 2009 · See answer (1) Best Answer. Copy. An interlocking spur is a natural feature which occurs in a river's upper course, where upward erosion is the dominant force in determining the river's course. As ...
Features of a glacial landscape - Glaciated upland …
WebSpurs, and interlocking spurs, are features found in the upper reaches of river valleys. They are erosional features, meaning that they are formed by water flowing over the land and eroding it as it moves. Imagine two gently sloping hillsides forming the sides of a small valley. As rain falls on these valley sides, the water runs down hill (it ... Web22 de dez. de 2024 · How is a truncated spur formed BBC Bitesize? The glacier uses the processes of plucking and abrasion to widen, steepen, deepen and smooth ‘V’-shaped river valleys into a ‘U’ shape. The interlocking spurs in the narrow V-shaped river valley are cut-off by the ice, creating truncated spurs . chiropractors in cheshire ct
Upper Course of a River - V-Shaped Valleys and Interlocking Spurs ...
Web10 de dez. de 2011 · An Old Revision Podcast from 2005 showing how a Waterfall forms WebThe interlocking spurs have been cut-off by the ice and changed to truncated spurs. When the ice melts the valley has changed from a V-shape to U-shape. It has very steep … WebOver time, rapids are formed. How are rapids formed BBC Bitesize? As the river erodes the landscape in the upper course, it winds and bends to avoid areas of hard rock. This creates interlocking spurs, which look a bit like the interlocking parts of a zip. When a river runs over alternating layers of hard and soft rock chiropractors in cheektowaga ny