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Why can rocks near active faults erode faster than heavy rainfall alone would suggest?

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Answer: Faults weaken rock by cracking it

Rain dissolves rock chemically — Rainwater can dissolve some minerals, but chemical dissolution alone does not explain why erosion can be enhanced near active faults. Fault-related deformation and shaking can mechanically weaken rock before water carries it away. Rainfall and rock damage can work together rather than being competing locations.

Faults weaken rock by cracking it ✓ — Fault-related cracking and rock damage can make material easier for water and gravity to remove. Active tectonics can therefore increase erosion not just by raising mountains, but by weakening the rock itself. The size of this effect varies with the fault system and local conditions.

Rock type is the only control — Rock type matters, but it is not the only control on erosion. The same kind of rock can resist erosion differently depending on how fractured or weakened it is. Fault proximity can therefore add information that rock type and rainfall alone miss.

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