+Gelifluction is the slow, seasonal flow of water-saturated soil over frozen ground, often seen in [Periglacial](/wiki/periglacial) environments. This creeping movement, a form of [Mass Wasting](/wiki/mass_wasting), gently reshapes slopes in regions like the [Tundra](/wiki/tundra).
+## See also
+- [Permafrost](/wiki/permafrost)
+- [Solifluction](/wiki/solifluction)
+- [Frost Heave](/wiki/frost_heave)
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