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Knick points are an irregularity in the rivers long profile.

Knick points occur in the river when river rejuvenation has taken place, meaning that either the land has risen or sea level has dropped, increasing the gradient of the river at that point. This gives the river greater potential energy and more erosive power. If the knick point is big enough, a waterfall would form.

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12y ago
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1w ago

Knick points and waterfalls form in valley long profiles due to variations in rock hardness or structural changes in the underlying geology. The resistant rock types erode more slowly than surrounding softer rocks, creating sudden drops in the landscape and a steepening of the valley. This process creates a visible boundary in the landscape as the river erodes the softer rock below the knick point.

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Q: Why do knick points and waterfalls happen in valley long profiles?
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A valley that has been glaciated by a smaller side glacier and is left standing higher than the main U-shaped valley is a .?

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What are the most prominent features of a narrow V-shaped valley where the stream profile drops rapidly?

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Valley of the Minotaur happened in 1983.


What forms a glacier moves into a stream valley?

A 'V' shaped valley is formed by streams and water action. A 'U' shaped valley is formed by the gouging out of the valley walls by a glacier. A hanging valley is where side valleys are cut across by the main glacier. Hanging valleys often have waterfalls that fall into the main valley over a cliff.


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Glacial erosion formed Yosemite Valley. Meanwhile, the streams eroded the granite rock to form the waterfalls we know as Yosemite Falls and many others today.


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What happen to pfr in moreno valley?

No