the glacier picks up the sediments, rocks, till, debris, and soil and carries them along while the glacier moves and will eventually drop them.
The central part of the glacier moves fastest than its edges as it is thickest from the center.
As a glacier moves outward or downward, it can transport and move various objects. These can include rocks, boulders, sediments, soil, and even smaller glaciers or icebergs. The immense weight and pressure exerted by the glacier allows it to pick up and carry these objects along with it as it advances.
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The feature that is the result of a glacier carving out rock as it moves is a roche moutonnees. It is a rock formation created by the passage of glacier ice. Or a terminal moraine
it is when a glacier moves into a large rock mass, cutting its way through.
The central part of the glacier moves fastest than its edges as it is thickest from the center.
As a glacier moves outward or downward, it can transport and move various objects. These can include rocks, boulders, sediments, soil, and even smaller glaciers or icebergs. The immense weight and pressure exerted by the glacier allows it to pick up and carry these objects along with it as it advances.
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it's a valley glacier, it moves slowly carrying debris and melted snow.
Any large mass of ice that moves slowly over ice is called a glacier.
The feature that is the result of a glacier carving out rock as it moves is a roche moutonnees. It is a rock formation created by the passage of glacier ice. Or a terminal moraine
The feature that is the result of a glacier carving out rock as it moves is a roche moutonnees. It is a rock formation created by the passage of glacier ice. Or a terminal moraine
it is when a glacier moves into a large rock mass, cutting its way through.
Plucking is the process in which a glacier freezes around cracked and broken rock and when it moves downhill, the rock is plucked from the back wall of the glacier.
Glacier
Glacier
The center or axis of a glacier generally moves the fastest when the glacier is moving by internal plastic flow. This is due to the greater pressure and thickness of ice at the center, causing it to flow more readily than the slower moving edges and margins of the glacier.