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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.
The convection cells radiate heat.
It results in reduced intraocular pressure
Air pressure on earth results from the earth's gravitational pull on the earth's atmosphere. In some sense, pressure results from the weight of the air above the point at which one measures pressure. At higher altitudes, there is less air above, resulting in less weight, which translates into pressure.
It results in a lower atmospheric pressure.
The fracturing of rock along curved lines that results when pressure is removed from bedrock is called fracking.
Frost wedging would be the primary process. Other mechanical weathering processes resulting in the extension of rock fracturing could include pressure release from uplift, and plant root growth.
The sound results from the difference in air pressure in the bottle as the cork is removed.
Glacial polish results from the grinding action of glaciers as they move and slide over bedrock, smoothing and polishing the surface of rocks. This process is primarily caused by the abrasion of rock particles and debris carried by the glacier against the bedrock.
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.
These are known as striations. Please see the related link.
osmotic
temperature
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pressure of gas over its liquid equilibrium
phosphate
we produce from the cappilarries