The correct statement that compares physical weathering to chemical weathering is:
Chemical weathering forms new substances while physical weathering does not.
*
1 point
Chemical weathering forms new substances while physical weathering does not
Physical weathering forms new substances while chemical weathering does not
Physical weathering and chemical weathering are the same process
Chemical weathering results int he breakdown of rocks while physical weathering does not.
5 answers
The correct statement that compares physical weathering to chemical weathering is:
Chemical weathering forms new substances while physical weathering does not.
It looks like you're listing processes related to physical and chemical weathering. Here's a breakdown of each process you've mentioned:
Physical Weathering:
Chemical Weathering:
To avoid repetition, note that "oxidation," "frost wedging," "exfoliation," and "carbonation" each belong to only one category of weathering:
If you have further questions or need more information, feel free to ask!
Glacial abrasion is a significant process through which a glacier erodes a valley, and it occurs as follows:
Formation of the Glacier: Glaciers form from the accumulation and compaction of snow over time, creating a large mass of ice. As the glacier moves, it drags along the materials embedded within it.
Incorporation of Sediment: As a glacier advances, it picks up a variety of sediments, including rocks, gravel, and smaller particles, from the valley floor and sides. These materials become embedded in the base and sides of the glacier.
Movement of the Glacier: As the glacier flows downhill under the influence of gravity, it carries the embedded sediments with it. The movement of the glacier is typically slow but relentless.
Abrasion Process: As the glacier moves, the rocks and sediments embedded in its base act like a powerful tool against the bedrock beneath. The pressure exerted by the weight of the glacier enhances the effect of the embedded rocks as they scrape and grind against the valley floor and walls.
Erosion of the Valley: This abrasive action results in the wearing away of the rock surface, smoothing and polishing it over time. The valley floor becomes wider and deeper, forming a characteristic U-shaped profile that is typical of glaciated valleys. The process also contributes to the creation of features such as striations (grooves carved into the rock by the moving sediment) and glacial polish (a smooth, shiny surface left on bedrock).
Effects Over Time: Over thousands of years, the continuous process of abrasion greatly modifies the landscape, contributing to the overall shape and morphology of the glacial valley. The sediment that is eroded can also be deposited downstream, forming features such as moraines, outwash plains, and other glacial landforms.
In summary, glacial abrasion is a process where the movement of glaciers, combined with the sediment they carry, erodes the underlying bedrock of a valley, leading to significant landscape changes over geological time scales.