The most raised part of the Sredne-Siberian plateau - mountains Putorana on which takes place a route. As mountains Putorana consider a basalt plateau on northwest suburb of the Sredne-Siberian plateau. It is stretched from an Arctic circle almost to 71® these and from 88® to 101® century д. (More than 500 km). In these limits the area of a province of Putorana makes 284000 клг. The average height of mountains 900 - 1200 m, and the highest - 1701 m is in their central part. The most typical line of mountains Putorana - a combination платообразных the levelled surfaces of hills and deep lake hollows, and also river valleys with каньонистыми coast. Differences in height 800 - 1000 m. In the west are most extended, the north and the east the basalt plateau breaks sharp ledges to 300 - 500 m of height to Western-Siberian and North Siberian plain and to a calcareous Kotujsky plateau. To the plateau south smoothly goes down, gradually passing to the general level of plateau with heights 500 - 700 m.        Above wood border - dense, places very firm ice crust. A valley gradually поварачивает on the left. The channel winds. Lifting not so abrupt, stony ( 34). On the right slope on a course eaves hang.
      For two hours have reached border of wood before merge of two sources. Over a narrow valley of the right source on a course eaves hang. Therefore we rise on the left source. Lifting became more abruptly. In an hour have risen on a plateau and have put camp as weather and visibility have started to spoil.
      At night it was cold enough.
      Plateau in upper courses of the right inflow of the river of Chopka - Holokit - the Stone - 1701 m (a radial exit from the Stone) - upper courses of the river of Kotuj - Kotujsky (ascension) - the river of Noku-Urek - the river of Kapchuk - an inhabited log hut in east gulf of the lake of Ajan.
      We go directly on Holokit. On the right the valley of a source of the river Holokit is visible.