Why is the erosional work of the river maximum in the mountainous course?
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Answer:
iscussing various types of endogenic and exogenic processes. We have also seen that erosion and deposition are some of the exogenic processes. In this post, we are dealing with the geomorphic agents – running water and groundwater, which causes erosion and deposition. They form various erosional (destructional) and depositional (constructional) landforms
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In the upper course of a stream slopes are steep and waterway channels are restricted. At the point when a waterway runs over exchanging layers of hard and delicate stone, rapids and cascades may frame. Cascades regularly structure where water surges down steep slopes in upland regions and rapidly disintegrates the stones.
Explanation:
- It begins from the wellspring of the waterway in uneven or bumpy regions. The stream streams down the lofty slant and, therefore, its speed and dissolving power are at their greatest. Streams are not many, with poor coordination.
- We have additionally observed that disintegration and statement are a portion of the exogenic procedures. In this post, we are managing the geomorphic operators – running water and groundwater, which causes disintegration and affidavit. They structure different erosional (pulverization) and depositional (constructional) landforms.
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