noun
: one of the alternating bands of finer and coarser material comprising a soil structure that are produced in sloping ground by solifluction — usually used in plural
noun
: one of the alternating bands of finer and coarser material comprising a soil structure that are produced in sloping ground by solifluction — usually used in plural
Webster's New International English Dictionary. Новый международный словарь английского языка Webster. 2012