Which outcome accelerates when repeated freeze-thaw cycles destabilize Arctic slopes?

💡 Explanation

Accelerated destabilization leads to enhanced solifluction lobe formation, because the active layer's saturated soil undergoes creep down the slope due to gravity; periglacial mass wasting dominates, therefore increased lobe formation occurs, rather than reduced thermokarst.

• Which outcome during ocean current divergence induces upwelling?
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• Which outcome arises when a gyre's density gradient weakens?
• Which geological change results when acidic rainwater interacts with fractured limestone?
• Which property increases with increased rates of pedogenesis?
• Which process limits crustal accumulation along transform boundaries?