Alternate freezing and thawing often leads to : A. Creep this occurrence usually occurs when the soils in that specific region is subjected to the temperature below 0 Celcius
Alternate freezing and thawing often leads to "creep".
Creep refers to the low mass development of soil and soil material down slants, driven fundamentally by gravity yet facilitated by immersion with water and by substitute freezing and thawing. Generally not distinguishable with the exception of through expanded perception.