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Solifluction, which is also known as soil fluction, is a geological term for a type of mass wasting. In solifluction, there exists 2 layers: an impermeable lower layer, and a sedimentary upper layer. When these layers exist on a hill and the top layer becomes saturated with water, the sediment begins to slowly slide down the hill over the lower layer.

More often than not, it occurs in periglacial environments, where a bottom layer of ice begins to melt, resulting in water saturation of the upper layer and the formation of a "flow".

Be careful not to get solifluction mixed with gelifluction though - gelifluction has a permanently frozen bottom layer, while solifluction doesn't.

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Related Questions

What season does solifluction occur?

Solifluction only occurs during the summer. :)


What primarily operates in areas permafrost?

solifluction


When does solifluction may occur?

Solifluction typically occurs in areas with permafrost or saturated ground that thaw during warmer periods. It is most commonly observed in Arctic and alpine regions. Factors such as freeze-thaw cycles, steep slopes, and presence of water can trigger solifluction movement.


Water-saturated debris over impermeable materials is called?

solifluction


Which process of mass wasting occurs primarily in permafrost regions?

solifluction


Is solifluction an important mass wasting process in areas of permafrost?

true


What kinds of mass wasting processes do you we see?

we have soil creep,solifluction,rock falls,earthflows,mud flows


Why is solifluction only a summertime?

In the summer, the soil thaws to some depth below the surface, but the water is trapped in the thawed soil because the permafrost zone is impermeable. Thus solifluction occurs only in the summer when the surface soil layer is thawed. In the winter the surface soil layer is frozen solid.


Where does solifluction occur?

Solifluction occurs in periglacial environments, such as areas near the edges of glaciers or in cold regions with frozen ground known as permafrost. It is a type of mass wasting where saturated soil flows slowly downhill over frozen ground due to the combination of thawing and freeze-thaw cycles.


Why is solifluction only a summertime phenomenon?

In the summer, the soil thaws to some depth below the surface, but the water is trapped in the thawed soil because the permafrost zone is impermeable. Thus solifluction occurs only in the summer when the surface soil layer is thawed. In the winter the surface soil layer is frozen solid.


What is the relationship between permafrost and solifluction?

Permafrost is permanently frozen ground that significantly impacts the landscape in cold regions. Solifluction is a process where thawed soil and sediment move slowly down slopes due to gravity, often occurring in areas underlain by permafrost. When the upper layers of permafrost thaw during warmer seasons, the saturated soil above can become unstable and flow, leading to solifluction features such as lobes and terraces. Thus, permafrost acts as a barrier that influences the dynamics of soil movement in these regions.


What Is the name of the process in which beach sediment moved down is called?

This process is known as longshore drift.