1.1.2 it appears that all the non-perennial streams are eroding headwards.provide two reasons why they are able to erode headwards.​

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Answer 1

Non-perennial streams are able to erode headwards due to two main reasons:  high erosive power and the softness of the underlying rock.

Firstly, the flow of water is intermittent and during periods of rainfall, the water has a higher velocity due to the larger volume. This higher velocity allows for the stream to erode more effectively and thus move headwards.

Secondly, non-perennial streams tend to be located in areas with a higher gradient, which means that the water flows downhill more easily and thus can erode more effectively as well.

These two factors, intermittent flow and high gradient, enable non-perennial streams to erode headwards.

Non-perennial streams are eroding headwards due to their high erosive power and the softness of the underlying rock.

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