Earthquake liquefaction, caused by coseismic shakes, is controlled by soil conditions which are the results of geomorphic processes.
摘要地震液化是同震震动引起的,同时也受地貌活动创造的土壤条件控制。
英语百科
Soil liquefaction 土壤液化
(重定向自Earthquake liquefaction)
Soil liquefaction describes a phenomenon whereby a saturated or partially saturated soil substantially loses strength and stiffness in response to an applied stress, usually earthquake shaking or other sudden change in stress condition, causing it to behave like a liquid.