talajfolyásokat
Talajfolyásokat, often translated as soil creep or solifluction, refers to the slow, downhill movement of soil and regolith. This phenomenon is primarily driven by gravity acting on saturated soil. When the ground becomes saturated with water, such as during spring thaw or heavy rainfall, the soil particles become less cohesive and can move more easily. The water acts as a lubricant, reducing friction between soil particles.
Talajfolyásokat is most common in areas with permafrost, where the active layer of soil thaws during warmer
The visual evidence of talajfolyásokat can include tilted trees, bent fences, and bulging or heaved ground.