What is Roche Moutonnee in Geography ? How is Roche Moutonnee formed ?

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What is Roche Moutonnee in Geography ? How is Roche Moutonnee formed ?

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What is Roche Moutonnee in Geography ?

Geographic formations formed as a result of glacial erosion, resembling camel hump in shape, are called Roche Moutonnee or sheepback. As more resistant rocks will wear less, this structure is formed. These strange shapes appear, due to the absence of the same level of wear.

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How is Roche Moutonnee formed ?

Roche Moutonnee or sheepback is formed by glacial eroding. Different etching levels between layers cause the formation of geographical structures in the form of camel humps. Roche Moutonnee can form in the high mountains with glacial formation.

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What is Roche Moutonnee ? How is Roche Moutonnee formed ?

As the glacier masses move along the surface, they come across hard rock masses. If these glacial masses cannot erode the rock masses, geographic structures with an oval shape are formed at the top. These geographical shapes resembling camel hump are called Roche Moutonnee.

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What are the factors affecting Roche Moutonnee formation ?

There are two main factors that are effective in Roche Moutonnee formation. The first is the presence of a glacier mass. The other factor is the ability of the glacier eroded rock to show different resistance.

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What are the reasons why Roche Moutonnee is not seen in our country ?

In our country, the approach that Roche Moutonnee is not seen is wrong. Roche Moutonnee can be seen in the high mountains of our country. But Roche Moutonnee formations are limited compared to other countries and regions. The main reason for this is that our country is located in the Midrail.

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Where does Roche Moutonnee form ?

Roche Moutonnee occurs in glaciers as a result of glacial erosion. It is formed by the glaciers shaping the bedrock.

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How high is a Roche Moutonnee?

The heights of a Roche Moutonnee vary from region to region, but can vary from a few meters to thirty-forty meters.