Stationary observations proved that long-term measurements permit us to obt
ain significantly more precise values of soil creep velocity. Depending on
soil texture, the average creep velocity ranges from 0.4 to 1.25 mm/year. W
e recommend that these values be used for further studies of creep phenomen
a and soil cover formation, as well as for the calculation of slope denudat
ion and transportation of substances to Lake Baikal.