КАРСТОВАЯ ДЕНУДАЦИЯ НА ТЕРРИТОРИИ СИБИРИ И ДАЛЬНЕГО ВОСТОКА: ОСОБЕННОСТИ СОВРЕМЕННОГО РАЗВИТИЯ

Abstract

Using he methods of J. Corbel and M. Pulina the estimation of a karstic denudation was accomplished for 127 river valleys of the Siberia and the Far East. Its magnitude varies from 1.1 to 62.0 mm/millennium within the region explored. The climatic conditions, especially precipitation, play the main role in the development of the karst. The intensity of karstic process has been revealed to differ in river basins with permafrost from that in the basins without permafrost.