Which phenomenon forms stepped topography within glacial lakes?

💡 Explanation

Stepped features appear due to isostatic rebound following deglaciation and subsequent sediment loading, because the crust readjusts in stages exposing previous lakebeds; therefore, the land slowly rises rather than having kettle collapse.

• Which mechanism impacts discharge rates in river-streams during orographic lift?
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• Which outcome results when large-scale wind patterns encounter significant topographic barriers?
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