The combination of the weathering and erosion of the stream bank and the cutting into the bedrock from the velocity of the stream combine to make a "stream valley".
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What is stream valley?</h3>
A stream valley is an earthen dip where water is present at its lowest point. These valleys are the result of erosion, which is the transfer of decomposed rock or soil from one location to another.
The formation of stream valley is given below-
- The typically V-shaped stream valley is changed to a U-shaped valley because the U-shape offers the flowing glacier the least amount of frictional resistance.
- Because a glacier's cross section and viscosity are substantially greater than those of a river, its route has fewer and wider bends.
To know more about characteristics of weathering, here
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The answer is A an increase in nutrients. Bonus: It is typically nitrogen and phosphorous.
Its d you could have looked it up on google images
Answer:
Econystems
Explanation:
My answer is d because in class I learn about the ecnoystem
Answer:
Porosity is a characteristic of rocks that affects the rate of weathering.
Explanation:
The rocks of all types are weathering under the influence of natural factors/elements. The water, temperature, climate, humidity, precipitation, winds, ice, all have their say when it comes to weathering and each of them is dominant in some areas. It is not just them that affect the rate of erosion though, but also the type of rock and its characteristics.
One characteristic of the rocks that is very important for the rate of erosion is the porosity. The porosity is a characteristic that shows us how easy or hard the rocks let water or other liquids through them. If the coefficient is high, then the rate of erosion will be very high, but if the coefficient is low, then the rate of erosion will be also very low.
