Stolbovoy Island

Stolbovoy

Столбовой остров
Stolbovoy Столбовой остров
Island
	Satellite image of Stolbovoy Island (Sentinel-2, 2019-08-03).
	Location of Stolbovoy Island
	Stolbovoy
	Coordinates: 74°04′15″N 135°59′30″E / 74.07083°N 135.99167°E
Country	Russian Federation
Federal subject	Far Eastern Federal District
Republic	Sakha Republic
Area
• Total	170 km2 (70 sq mi)
Elevation	222 m (728 ft)
Population
• Total	uninhabited

Stolbovoy Island (Russian: Столбовой остров) is a long and narrow island off the southwest side of the New Siberian archipelago in the eastern part of the Laptev Sea. It is located 184 km away from the Siberian coast and 100 km southwest of Kotelny Island, being thus quite detached from the New Siberian island group, although it belongs to the Lyakhov Islands subgroup of the New Siberian Islands.

History

According to Russian tradition in 1690 the Boyar Maxim Mukhoplev visited the island and found a number of crosses, the tombs of Russian seafarers who had previously been there.^[1] Stolbovoy was first charted by Yakov Sannikov in 1800.

There was a meteorological station located on the north-west coast of the island at the time of the USSR. In 2012 an automatic GLONASS (Global Navigation Satellite System) monitoring facility was installed in the same spot.^[2] Presently the island belongs to the Sakha Republic administrative division of the Russian Federation.

Geography and climate

Stolbovoy Island's area is approximately 170 km². Its length is 47 km and its maximum width is 10 km. The northernmost point of the island was named Cape Toll, in honor of Russian explorer Eduard Toll. There is a 5 km long lake in the northeast of the island. It is separated from the sea by a narrow spit. There is a 13 km long river, the Stolbovoy River, running northwards across the central part of the island.^[3]

The highest point of Stolbovoy Island is 222 meters. The island has 15–70 m high rocky cliffs, the lower relief down to the beach being dominated by conical mound-like stony structures.

The climate in the area is exceptionally severe, with prolonged, bitter winters, so that the waters of the Laptev Sea around Stolbovoy Island are covered by ice most of the year.

Geology

Tectonically deformed sedimentary rocks that accumulated during Late Jurassic to Early Cretaceous periods comprise Stolbovoy Island. These turbidites, which contain the fossils of marine pelecypods, consist of beds of sandstone coarsely and rhythmically interbedded with beds of siltstone and argillite. These rocks have been folded into a synclinal structure, thrust faulted, and intruded by small quartz diorite dikes.^[4]^[5]

Vegetation

Cryptogam herb covers practically barren Stolbovoy Island. All vegetation consists of dry to wet barren landscapes with scattered, herbs, lichens, mosses, and liverworts. Sedges, dwarf shrubs, and peaty mires are normally absent. These plants form a sparse (2–40%) and low-growing plant cover. The plants often grow in coarse-grained, often calcareous sediments^[6]

Views

Part of the coast of Stolbovoy showing the cliff formations.

The odd stony structures in the cliffs on Stolbovoy.

The undulated and desolate terrain of Stolbovoy.

References

^ Магидович В. И., Магидович И. П. Очерки по истории географических открытий. т. 3. М., 1984. С. 215
^ Северный морской путь оснащается современными приборами навигации
^ "Река Столбовая". Государственный водный реестр. Retrieved 18 March 2018.
^ Kos’ko, M.K., B.G. Lopatin, and V.G. Ganelin, 1990, Major geological features of the islands of the East Siberian and Chukchi Seas and the Northern Coast of Chukotka. Marine Geology. vol. 93, pp. 349–367.
^ Fujita, K., and D.B. Cook, 1990, The Arctic continental margin of eastern Siberia, in A. Grantz, L. Johnson, and J. F. Sweeney, eds., pp. 289–304, The Arctic Ocean Region. Geology of North America, vol L, Geological Society of America, Boulder, Colorado.
^ *CAVM Team, 2003, Circumpolar Arctic Vegetation Map. Scale 1:7,500,000. Conservation of Arctic Flora and Fauna (CAFF) Map No. 1. U.S. Fish and Wildlife Service, Anchorage, Alaska.

External links

anonymous, nd, Laptev Sea Alfred Wegener Institute for Polar and Marine Research – Research Unit Potsdam, Potsdam, Germany.
BirdLife International, 2008, RU118 Stolbovoy island. BirdLife's online World Bird Database: the site for bird conservation. Version 2.1. Cambridge, UK: BirdLife International.
Grigoriev, M., nda, ice-affected pebble beach of Stolbovoy Island Alfred Wegener Institute for Polar and Marine Research – Research Unit Potsdam, Potsdam, Germany
Grigoriev, M., ndb, rocky cliffs (15–70 m high) of Stolbovoy Island Alfred Wegener Institute for Polar and Marine Research – Research Unit Potsdam, Potsdam, Germany

[1] Магидович В. И., Магидович И. П. Очерки по истории географических открытий. т. 3. М., 1984. С. 215

[2] Северный морской путь оснащается современными приборами навигации

[МПР_России-3] "Река Столбовая". Государственный водный реестр. Retrieved 18 March 2018.

[kosko1-4] Kos’ko, M.K., B.G. Lopatin, and V.G. Ganelin, 1990, Major geological features of the islands of the East Siberian and Chukchi Seas and the Northern Coast of Chukotka. Marine Geology. vol. 93, pp. 349–367.

[fujita1-5] Fujita, K., and D.B. Cook, 1990, The Arctic continental margin of eastern Siberia, in A. Grantz, L. Johnson, and J. F. Sweeney, eds., pp. 289–304, The Arctic Ocean Region. Geology of North America, vol L, Geological Society of America, Boulder, Colorado.

[CAVMTeama-6] *CAVM Team, 2003, Circumpolar Arctic Vegetation Map. Scale 1:7,500,000. Conservation of Arctic Flora and Fauna (CAFF) Map No. 1. U.S. Fish and Wildlife Service, Anchorage, Alaska.

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