Most glacial movement is a result of internal deformation.

Name: Most glacial movement is a result of internal deformation.
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Internal deformation refers to the movement of ice crystals within a glacier, which causes the glacier to flow as a solid mass. This is the most common form of glacial movement, although external factors such as the slope of the land and the presence of meltwater can also influence glacier motion.

Most Glacial Movement Is a Result of Internal Deformation