📖 what
What is solifluction?
Quick Answer
Solifluction is the slow downhill flow of water-saturated soil, often in cold regions where frozen ground prevents drainage.
The Full Story
Solifluction happens when the upper soil layer becomes soggy and slides or creeps over a frozen or impermeable layer beneath. It is common in periglacial environments, especially where seasonal thawing affects the active layer above permafrost. The process can form lobes, terraces, and gentle flow-like slopes. Although it moves slowly, solifluction is an important erosion process in polar and mountain landscapes.
Key Facts
1.It involves slow flow of saturated soil
2.It is common above permafrost
3.It can form distinctive lobed landforms
YouTube Angle
Suggested video title for this topic:
"When muddy ground slowly creeps downhill"
Was this answer helpful?
Tap a reaction — it helps us pick what to cover next.