Which feature results when glacial isostatic rebound lags sea-level adjustments?

💡 Explanation

Emergent fjord coastlines appear due to isostatic rebound; this process uplifts land slowly after glacial retreat. Eustatic sea level rise occurs because melting adds water volume; therefore, uplift exceeds sea level rise, rather than moraines being submerged.

• Which feature results because varying rock densities impede stresses during Orogenic deformation?
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• Which mechanism limits meandering stream formation within deeply incised canyons?
• Which environmental shift results from prolonged effusive lava flows?
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• Which outcome results from stress during transform faulting?