Which risk notably increases as isostatic rebound lags tectonic uplift in fjord formation?

💡 Explanation

Increased landslide generation increases because differential stress accumulates during isostatic rebound. The resulting rock fracturing due to rebound and deglaciation promotes mass wasting processes/sedimentation, therefore landslides increase. This occurs rather than aquifer contamination, which primarily correlates with hydraulic gradient changes.

• Which outcome occurs when parent rock weathers during pedogenesis?
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• Which long-term geomorphic consequence primarily results when isostatic rebound occurs after glacial retreat in fjord regions?
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