LANDFORMS OF GLACIATED LOWLANDS
Landforms of glaciated lowlands are mainly depositional in nature, brought about by both valley glacier and continental ice sheets. The former leave behind the eroded material in only restricted areas. The imprint of ice sheets on the landscape is far…
LANDFORMS OF HIGHLAND GLACIATION
Glaciation generally gives rise to erosional features in the highlands and depositional features on the lowlands, though these processes are not not mutually mu exclusive because a glacier plays a combined role of erosion, transport and deposition throughout its course.…
LANDFORMS DUE TO WATER ACTION IN THE DESERTS
Wind erosion, transportation and deposition are most effective and widespread in desert regions, but few deserts in the world are entirely without rain or water. In some deserts, there are perennial rivers such as the Nile in Egypt which has…
LANDFORMS OF WIND DEPOSITION IN DESERTS
Materials that have been eroded and transported by winds must come to rest somewhere. The finest dust travels enormous distances in the air, and may be moved completely out of the desert. It has been estimated that some dust grains…
LANDFORMS OF WIND EROSION IN DESERTS
In the combined processes of abrasion, deflation and attrition, a wealth of characteristic desert landforms emerge. 1) Rock pedestals or mushroom rocks: The sand-blasting effect of winds against any projecting rock masses wear back the softer layer so that an…
Study Guide
