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The process by which a glacier loosens and moves rock is called glacial erosion. It occurs when the glacier's immense weight and movement cause it to pick up and carry rock fragments. As the glacier moves, these rocks scrape and grind against the underlying surface, gradually wearing it down and forming characteristic features like U-shaped valleys and striations on bedrock.
striations
The base of the glacier, where it is in contact with the rocks beneath it.
Through Plucking, when melt water freezes in the cracks of a mountain, and plucks out the loose rocks, and also abrasion, when the looses rocks scrape along the valley floor, to pick up even more till, and create striations, which are marks left on the valley floor. Ice also picks up even more rocks through landslides, or rocks falling over the hanging valley, (which is a steep drop created after interlocking spurs have been truncated, by the glacier cutting through them.) The rocks and other natural debris then is frozen, by the melt water, and is transported as the ice moves, in a glacial retreat, or advance.
the glacier dropped small rocks as it melted. An erratic is a large boulder left behind after a glacier has melted
A striation is a big or small gauge on a rocks surface usually caused by glaciers sliding past the rock. This tells us in which direction the glacier was traveling.
Striations are "scratches" left in bedrock by glaciers. A small particle of rock, generally pebble sized or smaller, becomes entrained in the base of the glacier and dragged along the surface of the bedrock. These can often be seen on hard bedrock surfaces that are resistant to subsequent weathering after the retreat of the glacier. Erratics are large rocks that are found out of place in the landscape, i.e. not near where they were formed. They are removed from their provenance by a glacier and transported away, before being deposited in a different part or the landscape when the glacier melts.
The process by which a glacier loosens and moves rock is called glacial erosion. It occurs when the glacier's immense weight and movement cause it to pick up and carry rock fragments. As the glacier moves, these rocks scrape and grind against the underlying surface, gradually wearing it down and forming characteristic features like U-shaped valleys and striations on bedrock.
smooth rocks create less friction on air.
The glacier can carry rocks. The moving of the glacier.
striations, striae
striations
On rocks - they are the parallel groves or scratches. Or on skeletal or cardiac muscle: they are the "strands" of the muscle.
why are most of rocks extremely smooth
The base of the glacier, where it is in contact with the rocks beneath it.
Glacier
Through Plucking, when melt water freezes in the cracks of a mountain, and plucks out the loose rocks, and also abrasion, when the looses rocks scrape along the valley floor, to pick up even more till, and create striations, which are marks left on the valley floor. Ice also picks up even more rocks through landslides, or rocks falling over the hanging valley, (which is a steep drop created after interlocking spurs have been truncated, by the glacier cutting through them.) The rocks and other natural debris then is frozen, by the melt water, and is transported as the ice moves, in a glacial retreat, or advance.