Average summer temperatures at the elevation of the equilibrium line are analyzed and accumulation on glaciers is computed from them. It is found that glaciation in the Northeast consists of five glacier systems (Kodar, Orulgan, Cherskiy Range, Suntar‐Khayata, and Kamchatka‐Koryak) with their own regime characteristics and character of glaciation. Extensive data are used to draw the boundary of the Pacific‐Asiatic glaciological province and it is established that the glacier systems of the Kodar and Orulgan ranges, receiving their main alimentation from the west, form part of the South and North Atlantic‐Eurasian province, respectively.