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  • Understanding Fold Mountains: The Role of Compressional Stress
    The type of stress in the Earth's crust that results in the formation of fold mountains is compressional stress.

    Here's why:

    * Compression: This occurs when two tectonic plates collide. The immense force pushes the rock layers together, causing them to bend and buckle.

    * Folding: The bending and buckling of the rock layers creates folds, which can be either anticlines (upward folds) or synclines (downward folds).

    * Mountain Formation: Over time, the accumulation of these folds can create large, elevated landforms known as fold mountains.

    Examples of Fold Mountains:

    * The Himalayas (formed by the collision of the Indian and Eurasian plates)

    * The Alps (formed by the collision of the African and Eurasian plates)

    * The Appalachian Mountains (formed by the collision of the North American and African plates)

    Other types of stress:

    * Tensional stress: Pulls rocks apart, leading to thinning and stretching of the crust. This is associated with the formation of rift valleys.

    * Shear stress: Causes rocks to slide past each other horizontally, leading to the formation of faults.

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