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Bolshevik Island
__NOTOC__ Bolshevik Island (russian: о́стров Большеви́к, ) is an island in Severnaya Zemlya, Krasnoyarsk Krai, Russian Arctic. The island is named after the political faction of the same name. History The island, together with the eastern coast of what was named Emperor Nicholas II Land, was discovered by Boris Vilkitsky at the time of the 1913 Arctic Ocean Hydrographic Expedition. Its insularity, however, wasn't proven until 1931, when Georgy Ushakov and Nikolay Urvantsev charted the archipelago during their 1930–32 expedition. Prima Polar Station, currently the only Polar station operating in Severnaya Zemlya, is located in this island near Cape Baranov. Geography It is the southernmost island and the second largest island in the group. The area of this island has been estimated at . The island is mountainous reaching a height of 935 m. About 31% of Bolshevik Island, totaling over , is covered by glaciers, the largest are Leningrad Glacier, Semyonov ...
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Krasnoyarsk Krai
Krasnoyarsk Krai ( rus, Красноя́рский край, r=Krasnoyarskiy kray, p=krəsnɐˈjarskʲɪj ˈkraj) is a federal subject of Russia (a krai), with its administrative center in the city of Krasnoyarsk, the third-largest city in Siberia (after Novosibirsk and Omsk). Comprising half of the Siberian Federal District, Krasnoyarsk Krai is the largest krai in the Russian Federation, the second largest federal subject (after neighboring Sakha) and the third largest subnational governing body by area in the world, after Sakha and the Australian state of Western Australia. The krai covers an area of , which is nearly one quarter the size of the entire country of Canada (the next-largest country in the world after Russia), constituting roughly 13% of the Russian Federation's total area and containing a population of 2,828,187 (more than a third of them in the city of Krasnoyarsk), or just under 2% of its population, per the 2010 Census. Geography The krai lies in the middl ...
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Semyonov-Tyan-Shansky Glacier
Pyotr Petrovich Semyonov or Semenov (russian: Пётр Петрович Семёнов; 2 January ''(New style: 14 January)'', 1827 – 26 February ''(New style: 11 March)'', 1914) was a Russian geographer and statistician who managed the Russian Geographical Society for more than 40 years. He gained international fame for his pioneering exploration of the Tian Shan mountains. He changed his surname to "Semyonov of Tian Shan" (Семёнов-Тян-Шанский, ''Semyonov-Tyan-Shansky'') at the age of 79. Several of his descendants, including a son, Andrey Semyonov-Tyan-Shansky, and a grandson Oleg Semenov-Tian-Shansky became scientists of note. Life Pyotr Semenov was born into a noble family and studied at Saint Petersburg University. Together with Fyodor Dostoyevsky, Semenov attended secret meetings of the "Petrashevsky Circle" (a literary discussion group of progressive-minded commoner-intellectuals in St. Petersburg). During the 1850s he studied geography and geology ...
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Spartak Fjord
Spartak may refer to: In sports *Spartak (sports society), an international fitness and sports society that unites some countries of the former Soviet Union In Russia *FC Spartak Moscow, a football club *FC Spartak Kostroma, a football club *PFC Spartak Nalchik, a football club *FC Spartak Vladikavkaz, a football club *HC Spartak Moscow, an ice hockey team *Spartak Saint Petersburg, a basketball team *Spartak Tennis Club, a tennis training facility *WBC Spartak Moscow, a women's basketball team In Ukraine *Spartak (Ukraine), a physical culture and multi-sport club *Spartak Ivano-Frankivsk, a football team *FC Spartak Sumy, a football club *Zakarpattia Uzhhorod, a football club, formerly known as Spartak Uzhhorod In Bulgaria *PFC Spartak Varna, a football team *PFC Spartak Pleven, a football team *FC Spartak Plovdiv, a football team *Spartak Sofia, a former football team In Serbia *FK Spartak Ljig, a football club *FK Spartak Subotica, a football team *FK Radnički (disambiguatio ...
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Akhmatov Fjord
Akhmatov Fjord, also known as Akhmatov Bay (russian: Залив Ахматова, ''Zaliv Akhmatova''), is a fjord in Severnaya Zemlya, Krasnoyarsk Krai, Russia.GoogleEarth This fjord is clogged by ice most of the year. History The fjord was named in 1913 after the Russian hydrographer who surveyed it in the course of the Arctic Ocean Hydrographic Expedition led by Boris Vilkitsky on behalf of the Russian Hydrographic Service. Geography Akhmatov Fjord is a fjord with a wide entrance in the northeastern area of Bolshevik Island, the southernmost island of Severnaya Zemlya. It is located southeast of Cape Unslicht on the Laptev Sea shore of the island, east of Mikoyan Bay. The fjord extends in a roughly northeast/southwest direction for about 56 km. The basin inside the fjord has smooth mountains on both sides. Near the mouth Akhmatov Fjord is about 17 km wide, and the inner fjord becomes narrower, averaging 5 km in width. Lishny Island and Yuzhny Island —among oth ...
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Fjord
In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Iceland, Ireland, Kamchatka, the Kerguelen Islands, Labrador, Newfoundland, New Zealand, Norway, Novaya Zemlya, Nunavut, Quebec, the Patagonia region of Argentina and Chile, Russia, South Georgia Island, Tasmania, United Kingdom, and Washington state. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords wh ...
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Shokalsky Strait
Shokalsky Strait (russian: Пролив Шокальского) is a strait in Severnaya Zemlya, Russia. Geography The Shokalsky Strait is an up to a 50 km-wide strait that separates Bolshevik Island from October Revolution Island, connecting the Kara Sea in the west with the Laptev Sea in the east. It is named after Russian oceanographer Yuly Shokalsky Some fjords of Severnaya Zemlya have their mouths in the strait, such as Marat Fjord in October Revolution Island's eastern shore, as well as Partizan Fjord, Spartak Fjord and Thaelmann Fjord in Bolshevik Island northwestern coast. Cape Baranov and its adjacent Prima Polar Station are located in the northern part of Bolshevik Island facing the Shokalsky Strait.GoogleEarth The Krasnoflotskiye Islands are located at the western end of the strait.GoogleEarth See also *Mikoyan Bay Mikoyan Bay (russian: Залив Микояна, ''Zaliv Mikoyana'') is a bay in Severnaya Zemlya, Krasnoyarsk Krai, Russia.GoogleEarth It is c ...
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Mikoyan Bay
Mikoyan Bay (russian: Залив Микояна, ''Zaliv Mikoyana'') is a bay in Severnaya Zemlya, Krasnoyarsk Krai, Russia.GoogleEarth It is clogged by ice most of the year with many icebergs in the strait off the mouth of the bay. History This bay was named by the 1930–1932 expedition to the archipelago led by Georgy Ushakov and Nikolay Urvantsev after Soviet statesman Anastas Mikoyan (1895–1978). Geography Mikoyan Bay is a body of water in the northeastern area of Bolshevik Island, the southernmost island of Severnaya Zemlya. It is located southwest of Cape Unslicht on the Shokalsky Strait shore of the island. The headland on the western side of the mouth of the bay is Cape Baranov. The bay extends in a roughly north–south direction for about . The basin inside the bay has smooth mountains on both flanks. Mikoyan Bay is about 5.5 km wide, the shores of both sides running almost parallel to each other southwards from its mouth. There are two little islets in the bay, ...
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Lichen
A lichen ( , ) is a composite organism that arises from algae or cyanobacteria living among filaments of multiple fungi species in a mutualistic relationship.Introduction to Lichens – An Alliance between Kingdoms
. University of California Museum of Paleontology.
Lichens have properties different from those of their component organisms. They come in many colors, sizes, and forms and are sometimes plant-like, but are not s. They may have tiny, leafless branches (); flat leaf-like structures (

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Moss
Mosses are small, non-vascular flowerless plants in the taxonomic division Bryophyta (, ) '' sensu stricto''. Bryophyta (''sensu lato'', Schimp. 1879) may also refer to the parent group bryophytes, which comprise liverworts, mosses, and hornworts. Mosses typically form dense green clumps or mats, often in damp or shady locations. The individual plants are usually composed of simple leaves that are generally only one cell thick, attached to a stem that may be branched or unbranched and has only a limited role in conducting water and nutrients. Although some species have conducting tissues, these are generally poorly developed and structurally different from similar tissue found in vascular plants. Mosses do not have seeds and after fertilisation develop sporophytes with unbranched stalks topped with single capsules containing spores. They are typically tall, though some species are much larger. ''Dawsonia'', the tallest moss in the world, can grow to in height. There are a ...
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Coastal Plain
A coastal plain is flat, low-lying land adjacent to a sea coast. A fall line commonly marks the border between a coastal plain and a piedmont area. Some of the largest coastal plains are in Alaska and the southeastern United States. The Gulf Coastal Plain of North America extends northwards from the Gulf of Mexico along the Lower Mississippi River to the Ohio River, which is a distance of about . The Atlantic Coastal Plain runs from the New York Bight to Florida. The Coastal Plains of India lie on either side of the Deccan Plateau, along the western and eastern coasts of India. They extend for about 6,150 km from the Rann of Kutch in the west to West Bengal in the east. They are broadly divided into the Western Coastal Plains and the Eastern Coastal Plains. The two coastal plains meet at Kanyakumari, the southernmost tip of the Indian mainland. The eastern coastal plain is located between The Bay of Bengal and the eastern Ghats and the western coastal plain is located between ...
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Moraines
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Proven ...
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