Gelifluction is the slow, seasonal flow of water-saturated soil over frozen ground, often seen in Periglacial environments. This creeping movement, a form of Mass Wasting, gently reshapes slopes in regions like the Tundra.
Gelifluction is the slow, seasonal flow of water-saturated soil over frozen ground, often seen in Periglacial environments. This creeping movement, a form of Mass Wasting, gently reshapes slopes in regions like the Tundra.