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Compression stress leads to the formation of fault-block mountains, like the San Gabriel Mountains in California.
Compression stress causes fault-block mountains. Compression occurs when rock masses are pushed together, like when plates collide at convergent boundaries. This type of stress leads to rocks shortening laterally and thickening vertically, resulting in the formation of fault-block mountains. An example of this is the creation of the San Gabriel Mountains in California due to compressional stresses.
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