Glacier Geomorphology In Tibet Stock Photo

Glaciers are quasi-plastic bodies. Glacier movement includes internal movement and bottom sliding, which are the driving forces for erosion, transportation, accumulation and shaping of various glacier landforms. However, it is not the only power to shape the glacier landscape. It is the combined action of various stresses such as freezing, snow erosion, avalanche and running water, which forms the landscape in the glacier area. Widely distributed in the plateau mountains of Europe, North America and western China