solifluction

solifluction读音音标

英 [sɒlɪ\'flʌkʃən]

美 [ˌsoʊlə\'flʌkʃən]

solifluction意思解释

n.

泥流，泥流作用；

英英释义

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.