While hiking up a mountain valley, you come upon a lake, dammed by wall of unconsolidated sediments. You suspect that those sediments may have been deposited across the valley by a glacier that has since melted away. Describe thoroughly what those sediments would look like and why they could not be from a stream. Viewing up the valley, what other clue would support it being a glaciated valley rather than a stream valley? Large boulders are strewn haphazardly throughout the valley as well? Does that evidence support a glacier depositing the boulders or a stream depositing the boulders? Defend your reasoning. An initial post and at least two replies are required.

Question

Derick Watkins

Geography

7 March, 12:50

While hiking up a mountain valley, you come upon a lake, dammed by wall of unconsolidated sediments. You suspect that those sediments may have been deposited across the valley by a glacier that has since melted away. Describe thoroughly what those sediments would look like and why they could not be from a stream. Viewing up the valley, what other clue would support it being a glaciated valley rather than a stream valley? Large boulders are strewn haphazardly throughout the valley as well? Does that evidence support a glacier depositing the boulders or a stream depositing the boulders? Defend your reasoning. An initial post and at least two replies are required.

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Answers (1)

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Royce Meadows · Answer 1

Answer and Explanation:

The lakes on cold valley are known as ribbon lake, looks extremely delicate level and having hanging valley. these are delivered due to over depending, which is attributes highlight of cold valley.

Different elements incorporate the valley will be U shaped, it will have stones, trough end, different advances and hanging valley.

The explanation behind this valley for not having a place with stream valley is that the stream valley are consistently V molded.