Two basins have similar rain and rock type; one lies nearer active faults. Why erode faster?
Show answer & explanation
Answer: Fault-damaged bedrock
Fault-damaged bedrock ✓ — Right. The surprising point is that a fault can change the material, not just the shape of the land. Repeated tectonic damage leaves fractured, weaker near-surface rock, so the same river power can remove more material. The 2026 Science study found higher erosional efficiency near active faults even after comparing rain, rock type, and topography.
Extra storm runoff — Almost, but the stem already holds rainfall similar. More runoff can speed erosion during storms, yet the reported pattern persisted when precipitation and rock type were compared with fault distance. The twist is that the fault can act like a rock-softening machine, letting erosion do more work without needing extra rain.
Naturally softer rock — Not quite. The stem holds rock type similar, and the study compared lithology with fault distance rather than assuming softer rocks explain the pattern. The memorable part is that the same kind of rock can behave differently after tectonic damage. Fractures and weakened contacts let rivers remove it more easily.
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