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.

• Which pedogenesis effect increases in seasonally flooded terrains?
• During coastal upwelling events, which outcome occurs due to nutrient-rich water rising to the surface?
• Which risk increases because of reduced flow velocity in an oxbow lake compared to the main river channel?
• Which feature characterizes glacial cirques formed in locations with significant permafrost?
• Which risk increases within subterranean cave ecosystem boundaries when agriculture increases phosphorus runoff upstream?
• Which risk increases on steep, saturated Arctic slopes undergoing seasonal thaw and solifluction?