What is weathering and how is it different from erosion?
Both are geological processes that influence the earth but weathering occurs in place and is when rocks/minerals break down due to wind, water, or other natural processes whereas erosion is when wind, water, and gravity move rocks and minerals to other locations. In both instances, the solid material breaks down, but when that breakdown is due to weathering, the materials remain in place whereas in erosion they are displaced.
Here's a really great website I found that explains the differences well: weathering vs. erosion .
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Weathering is a slow, continuous process that affects all substances exposed to the atmosphere. It is the breaking down of rocks and other materials on the Earth's surface.
Erosion is the process by which weathered rock and soil particles are moved from one place to another.
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Weathering is the process of breaking down rocks, soil, and minerals through exposure to the atmosphere, water, and biological organisms. It occurs in place, meaning the materials stay in the same location where they are weathered. Erosion, on the other hand, involves the movement and transportation of weathered materials by natural agents like water, wind, or ice. Erosion typically transports the weathered materials to a different location.
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When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
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