Which landform develops when solifluction lobes advance over previously deposited sediments?

💡 Explanation

When solifluction occurs in periglacial environments, repeated thawing and freezing causes saturated soil to flow downslope, with the lobe fronts forming small terraces with arcuate risers as they push against existing stable ground. Therefore a terraced slope forms, rather than braided streams, hanging valleys, or eskers, which relate to fluvial or glacial erosion/deposition.

• Which outcome arises when a major river's stream gradient decreases due to regional tectonic subsidence?
• Which mechanism allows strike-slip motion on the Mendocino transform fault to cause localized uplift along segments?
• Which cave formation increases when soluble rock dissolves?
• Which risk escalates dramatically where loess deposits form thick, unconsolidated layers?
• Which hazard dramatically increases when stratospheric tephra accumulates?
• Which outcome primarily results when upwelling zones experience increased stratification due to surface warming?