Franz Josef Land in the context of Alexandra Land


Franz Josef Land in the context of Alexandra Land

⭐ Core Definition: Franz Josef Land

Franz Josef Land (Russian: Земля́ Фра́нца-Ио́сифа, romanizedZemlya Frantsa-Iosifa) is a Russian archipelago in the Arctic Ocean. It is inhabited only by military personnel. It constitutes the northernmost part of Arkhangelsk Oblast and consists of 192 islands, which cover an area of 16,134 square kilometers (6,229 sq mi), stretching 375 kilometers (233 mi) from east to west and 234 kilometers (145 mi) from north to south. The islands are categorized in three groups (western, central, and eastern) separated by the British Channel and the Austrian Strait. The central group is further divided into a northern and southern section by the Markham Sound. The largest island is Prince George Land, which measures 2,741 square kilometers (1,058 sq mi), followed by Wilczek Land, Graham Bell Island and Alexandra Land.

Approximately 85% of the archipelago is glaciated, with large unglaciated areas on the largest islands and many of the smallest ones. The islands have a combined coastline of 4,425 kilometers (2,750 mi). Compared to other Arctic archipelagos, Franz Josef Land is highly dissected, as a result of it being heavily glaciated, with a very low ratio of total area to coastline of just ~3.6 square kilometers per coastline kilometer. Cape Fligely on Rudolf Island is the northernmost point of the Eastern Hemisphere. The highest elevations are found in the central and eastern group, with the highest point located on Wiener Neustadt Island, 620 meters (2,030 ft) above mean sea level.

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Franz Josef Land in the context of Barents Sea

The Barents Sea (/ˈbærənts/ BARR-ənts, also US: /ˈbɑːrənts/ BAR-ənts; Norwegian: Barentshavet, Urban East Norwegian: [ˈbɑ̀ːrəntsˌhɑːvə]; Russian: Баренцево море, romanizedBarentsevo More) is a marginal sea of the Arctic Ocean, located off the northern coasts of Norway and Russia and divided between Norwegian and Russian territorial waters. It was known earlier among Russians as the Northern Sea, Pomorsky Sea or Murman Sea ("Norse Sea"); the current name of the sea is after the historical Dutch navigator Willem Barentsz.

The Barents Sea is a rather shallow shelf sea with an average depth of 230 metres (750 ft), and it is an important site for both fishing and hydrocarbon exploration. It is bordered by the Kola Peninsula to the south, the shelf edge towards the Norwegian Sea to the west, the archipelagos of Svalbard to the northwest, Franz Josef Land to the northeast and Novaya Zemlya to the east. The islands of Novaya Zemlya, an extension of the northern end of the Ural Mountains, separate the Barents Sea from the Kara Sea.

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Franz Josef Land in the context of Kara Sea

The Kara Sea is a marginal sea, separated from the Barents Sea to the west by the Kara Strait and Novaya Zemlya, and from the Laptev Sea to the east by the Severnaya Zemlya archipelago. Ultimately the Kara, Barents and Laptev Seas are all extensions of the Arctic Ocean north of Siberia.

The Kara Sea's northern limit is marked geographically by a line running from Cape Kohlsaat in Graham Bell Island, Franz Josef Land, to Cape Molotov (Arctic Cape), the northernmost point of Komsomolets Island in Severnaya Zemlya.

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Franz Josef Land in the context of Severny Island

Severny Island (Russian: Се́верный о́стров, romanizedSevernyy ostrov, lit.'Northern Island') is a Russian Arctic island. It is the northern island of the Novaya Zemlya archipelago.It was historically called Lütke Land after Friedrich Benjamin von Lütke, who explored it. It lies approximately 400 km north of the Russian mainland. It has an area of 48,904 square kilometres (18,882 sq mi), making it the 30th-largest island in the world and the 3rd-largest uninhabited island in the world, although there was formerly a settlement at Lagerni on the northern shore of the narrow Matochkin Strait. It is part of the Russian Arctic National Park (along with Franz Josef Land which lies to the north).

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Franz Josef Land in the context of Arkhangelsk Oblast

Arkhangelsk Oblast (Russian: Архангельская область, IPA: [ɐrˈxanɡʲɪlʲskəjə ˈobɫəsʲtʲ]) is a federal subject of Russia (an oblast). It includes the Arctic archipelagos of Franz Josef Land and Novaya Zemlya, as well as the Solovetsky Islands in the White Sea. Arkhangelsk Oblast also has administrative jurisdiction over the Nenets Autonomous Okrug (NAO). Including the NAO, Arkhangelsk Oblast has an area of 587,400 square kilometres (226,800 sq mi), it is the largest of first-level administrative divisions in Europe. Its population (including the NAO) was 1,227,626 as of the 2010 Census.

The city of Arkhangelsk, with a population of 301,199 as of the 2021 Census, is the administrative center of the oblast. The second largest city is the nearby Severodvinsk, home to Sevmash, a major shipyard for the Russian Navy. Among the oldest populated places of the oblast are Kholmogory, Kargopol, and Solvychegodsk; there are a number of Russian Orthodox monasteries, including the Antoniev Siysky Monastery and the World Heritage Site of the Solovetsky Islands in the White Sea.

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Franz Josef Land in the context of Nansen's Fram expedition

Nansen's Fram expedition of 1893–1896 was an attempt by the Norwegian explorer Fridtjof Nansen to reach the geographical North Pole by harnessing the natural east–west current of the Arctic Ocean. In the face of much discouragement from other polar explorers, Nansen took his ship Fram to the New Siberian Islands in the eastern Arctic Ocean, froze her into the pack ice, and waited for the drift to carry her towards the pole. Impatient with the slow speed and erratic character of the drift, after 18 months Nansen and a chosen companion, Hjalmar Johansen, left the ship with a team of Samoyed dogs and sledges and made for the pole. They did not reach it, but they achieved a record Farthest North latitude of 86°13.6′N before a long retreat over ice and water to reach safety in Franz Josef Land. Meanwhile, Fram continued to drift westward, finally emerging in the North Atlantic Ocean.

The idea for the expedition had arisen after items from the American vessel Jeannette, which had sunk off the north coast of Siberia in 1881, were discovered three years later off the south-west coast of Greenland. The wreckage had obviously been carried across the polar ocean, perhaps across the pole itself. Based on this and other debris recovered from the Greenland coast, the meteorologist Henrik Mohn developed a theory of transpolar drift, which led Nansen to believe that a specially designed ship could be frozen in the pack ice and follow the same track as Jeannette wreckage, thus reaching the vicinity of the pole.

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Franz Josef Land in the context of Cape Kohlsaat

Cape Kohlsaat (Russian: Мыс Кользат) is a point on the eastern shore of Graham Bell Island, the easternmost island of Franz Josef Land, Russia. It is also the easternmost limit of the Franz Josef Archipelago.

Its location is 81°14′N, 65°10′E, and it is important as a landmark, for Cape Kohlsaat marks the northwesternmost corner of the Kara Sea.

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Franz Josef Land in the context of Russian Arctic National Park

Russian Arctic National Park (Russian: Национальный парк "Русская Арктика") is a national park of Russia, which was established in June 2009. It was expanded in 2016, and it covers a large and remote area of the Arctic Ocean, the northern part of Novaya Zemlya (Severny Island), and Franz Josef Land.

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Franz Josef Land in the context of Victoria Island (Russian Arctic)

Victoria Island (Russian: Остров Виктория; Ostrov Viktoriya) is a small Arctic island of the Russian Federation. It is located at 80°9′N 36°46′E / 80.150°N 36.767°E / 80.150; 36.767, halfway between the Norwegian archipelago of Svalbard and the Russian archipelago of Franz Josef Land. It was annexed to the USSR in 1932 (six years after the rest of Franz Josef Land).

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Franz Josef Land in the context of British Channel

British Channel (Russian: Британский канал) is a strait in the western part of the Franz Josef Land archipelago in Arkhangelsk Oblast, Russia. It was first reported and named in 1875 by the Jackson–Harmsworth expedition.

The British Channel separates the westernmost island group from the rest of the Franz Josef Land archipelago. To the north the strait starts at the Queen Victoria Sea, in an southwesterly direction. It separates Prince Georg Land to the west from the smaller Koetlitz Island and Hooker Island to the east. About two-thirds down Prince Georg Land, the channel is split in two where the Nightingale Sound continues down the coast of Prince Georg Land and the De Bruyne Sound diverts to the southeast.

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