In geomorphology, solifluction is a slow mass wasting slope process, occurring in periglacial environments. Solifluction describes the slow downslope movement of water-saturated sediment due to recurrent freezing and thawing of the ground, affected by gravity.

Solifluction
Solifluction rates, processes and landforms: a global review
Morphometric analysis of solifluction lobes and rock glaciers in the Swiss Alps
Solifluction steps and risers, Lee Ridge, Glacier National Park, Montana, USA: a scale and pattern analysis
Rates and processes of periglacial solifluction: an experimental approach
Solifluction processes on permafrost and non‐permafrost slopes: results of a large‐scale laboratory simulation
Snow cover and soil moisture controls on solifluction in an area of seasonal frost, eastern Alps
Morphometry and Late Holocene activity of solifluction landforms in the Sierra Nevada, southern Spain.
Solifluction-induced modifications of archaeological levels: simulation based on experimental data from a modern periglacial slope a...
Laboratory simulation of periglacial solifluction: Significance of porewater pressures, moisture contents and undrained shear streng...