Which outcome occurs in forearc regions when a subducting plate exhibits a shallow angle of descent?

💡 Explanation

When a subducting plate has a shallow angle, the overriding plate experiences strong compressional forces because of increased friction, leading to uplift of the forearc region. Therefore rapid uplift of the continental margin results, rather than volcanic proximity, subsidence, or sediment deposition that correspond to steeper subduction angles.

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