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Hogbacks are formed through the process of erosion, where resistant rock layers are uplifted and tilted at an angle, creating a steep ridge. The softer rock layers around the hogback erode more quickly, exposing the harder layers that form the ridge. Over time, this differential erosion creates the distinctive shape of a hogback.

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Q: How are hogbacks formed?
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What is a hogback?

A hogback is a narrow, steep-sided ridge of land that has been geologically uplifted along a reverse fault. It typically has a steep slope on one side and a more gradual slope on the other. Hogbacks are common in areas with significant tectonic activity.


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