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Glacier morphology
Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. Types of glaciers range from massive ice sheets, such as the Greenland ice sheet or those in Antarctica, to small cirque glaciers perched on a mountain. Glaciers types can be grouped into two main categories, based on whether ice flow is constrained by the underlying bedrock topography.
==Unconstrained==
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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