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The density of ice at 0°C is 0.9167 g/cm³. The density increases slightly at lower temperatures. Therefore, the volume and temperature of the glacier is needed in order to calculate the exact weight.
That is usually called a glacier
composition, size, weight
The force is created by the self weight of the overlying material.
A glacier is formed from frozen water, and snow accumulating high in the mountains adding weight and forcing forward movement downhill.
Snow falls in the accumulation area, usually the part of the glacier with the highest elevation, adding to theglacier'smass. As the snow slowly accumulates and turns to ice, and the glacier increases in weight, the weight begins to deform the ice, forcing the glacier to flow downhill.
There are three nouns. They are pressure, weight, and glacier.
Metamorphic
Pressure from weight of overlying rock.
Metamorphic
Metamorphic
The density of ice at 0°C is 0.9167 g/cm³. The density increases slightly at lower temperatures. Therefore, the volume and temperature of the glacier is needed in order to calculate the exact weight.
That is usually called a glacier
Aquifers can't support the weight of overlying structures.
If your mass increases, your weight also increases.
The process is called compaction.
A sedimentary rock is formed.