Which process limits the height of topographic features along a transform fault boundary?

💡 Explanation

When tectonic plates slide past each other along a transform fault, topographic features may form due to localized compression or transpression; however, erosion continuously acts to lower these features because erosion rates are related to slope angle, steepness, and material properties. Therefore, uplift must equal erosion for mountain building to stall rather than rebound, phase change, or aftershocks resulting.

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