Which topographical outcome results when Freeze-thaw weathering drives solifluction processes?

💡 Explanation

Lobate features appear because solifluction involves soil creep downslopes weakened by cyclical freeze-thaw, creating 'lobes' of soil. Therefore lobate features become visible rather than uniform decline because this deformation is specific to solifluction.

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• Which volcanic outcome develops due to isostatic rebound?
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