ROLE OF MASS MOVEMENT Flashcards
Two important mass movement for periglacial environment
Frost creep and solifluction are important mass movement processes acting on slopes in periglacial environments
What is Frost Creep
Very slow form of mass movement
material moves downslope by just a few cm per year, even on steeper slopes
What is Solifluction
Occurs in permafrost regions
During summer months, active layer melts forming mobile water-saturated layer
Results in formation of either stone-banked or turf-banked lobes on slopes of 10-20*
What can Solifluction and Frost Creep form
ASYMMETRIC VALLEYS
Differential rates of solifluction and frost creep lead to one side of valley being significantly steeper than other.
ASYMMETRIC VALLEYS example
In northern hemisphere, south-facing slopes are more exposed to Sun (insolation) and thaw more frequently, increasing soil moisture and promoting mass movement, leading to less-steep slope