Explanation:

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Block mountains are generally formed by the uplifting and tilting of large blocks of the Earth's crust. They are not typically associated with the bending of the Earth's crust. The correct process for the formation of block mountains is usually crustal extension and faulting.

Vosges Mountains, located in France and Germany, is an example of a block mountain.

Block Mountains are created when large areas are broken and displaced vertically. The uplifted blocks are termed as horsts and the lowered blocks are called graben. The Rhine valley and the Vosges mountain in Europe are examples of such mountain systems.