ЗАКОНОМЕРНОСТИ ФОРМИРОВАНИЯ ОБЛОМОЧНОГО МАТЕРИАЛА В ПРИУРЕЗОВОЙ ПОЛОСЕ ОЗЕРА БАЙКАЛ

Abstract

The weakness of accumulation is the characteristic feature of the Baikal coastal zone. The coarse sediments are predominant at the water edge. The type of the coast depends on the structure of the lake basin. High rocky banks are typical for the west flange, where accumulation is almost absent. The east low-graded flange has much of an entass-ments, enrockments, and pebble beaches.