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alignment of grooves in bedrock
An ice front recedes when a glaciers rate of melting is greater than its rate of movement. It is the end of the glacier.
The gouging of bedrock by rock fragments dragged by glaciers results in the formation of grooves, scratches, and striations on the surface of the bedrock. These features, known as glacial striations, provide evidence of the direction and movement of past glaciers. These marks can also help geologists determine the extent and timing of glacial activity in an area.
cryosphere
in all directions
alignment of grooves in bedrock
Continental Glaciers
The movement of glaciers through the process of abrasion.The movement of glaciers.
The location of the glaciers affected the movement of people and animals by blocking them. They could not get to certain areas due to these glaciers.
movement of glaciers
1; the extensor, but not the flexor
In the same direction as the movement
An ice front recedes when a glaciers rate of melting is greater than its rate of movement. It is the end of the glacier.
movement of glaciers
the movement of glaciers
The gouging of bedrock by rock fragments dragged by glaciers results in the formation of grooves, scratches, and striations on the surface of the bedrock. These features, known as glacial striations, provide evidence of the direction and movement of past glaciers. These marks can also help geologists determine the extent and timing of glacial activity in an area.
they went north