Голоценовые гляциальные формы в Северном Приохотье

The manifestations of Holocene glacial morphogenesis in the glacial corries of the Northern Priokhotye are investigated. The authors identify active (developing) glacial corries as well as degrading (dying) ones, which have a pronounced association with certain orographic zones. The corrie morphosculpture is most powerfully formed in the mountain ranges of the peninsulas in the northern part of the Sea of Okhotsk: Koni, Piagina, Taigonos. In the highest part of the Taynynot Range, some corries contain "shielded glaciers". Some of them are associated with stadial end- moraine shafts, which characterize glacier dynamics. The data obtained may be of significance for the correlation of glacial events during the neoglacial maximum and the Little Ice Age.