Misplaced Pages

#924075

29-517: The river is navigable in its lower reaches. The Kukhtuy river has its source at an elevation of 1,617 m (5,305 ft) in the Suntar-Khayata range. It flows relatively straight southwards through a mountainous area. The Yudoma Range rises on the right side and the Kukhtuy Range on the left side of its valley and its course is roughly parallel to rivers Okhota to the west and Ulbeya to

58-797: A United Nations subcommittee accepted the Russian argument, and in March 2014 the full United Nations Commission on the Limits of the Continental Shelf ruled in favor of the Russian Federation. Bowhead whales were first caught in 1847, and dominated the catch between 1852 and the late 1860s. Between 1850 and 1853 the majority of the fleet went to the Bering Strait region to hunt bowheads, but intense competition, poor ice conditions, and declining catches forced

87-658: A hot spring in the Suntar-Khayata Range. The birds feed underwater when air temperatures drop below −55 °C (−67 °F). Indeterminate Carnosauria remains, possible indeterminate Coelurosaur remains, indeterminate Sauropoda remains that had been previously referred to Camarasauridae indet, and indeterminate Theropoda remains have all been recovered from Suntar outcrops in Sakha Republic , Russia. cf. Stegosaurus cf. Stegosaurus sp. Sakha Republic, Russia. This Russian Far East location article

116-462: Is a granite mountain range rising along the border of the Sakha Republic in the north with Amur Oblast and Khabarovsk Krai in the south. The R504 Kolyma Highway passes through the northern part of the range by Kyubeme . The Suntar-Khayata is approximately 450–550 km long and 60 km wide. 2,959 metres (9,708 ft) high Mus-Khaya Mountain , located in the Sakha Republic,

145-454: Is a stub . You can help Misplaced Pages by expanding it . This paleontological site article is a stub . You can help Misplaced Pages by expanding it . Sea of Okhotsk The Sea of Okhotsk is a marginal sea of the western Pacific Ocean . It is located between Russia 's Kamchatka Peninsula on the east, the Kuril Islands on the southeast, Japan 's island of Hokkaido on the south,

174-974: Is a watershed divide between the Aldan River , of the Lena basin, and the Indigirka —both of the Arctic Ocean , and the Sea of Okhotsk . Some of the major watercourses having their source in the range are the Tyry , Eastern Khandyga , Tompo , Allakh-Yun and Yudoma belonging to the Lena basin, the Khastakh , Kuydusun and Taryn-Yuryakh to the Indigirka basin, the Kulu of the Kolyma River basin, while

203-662: Is connected to the Sea of Japan on either side of Sakhalin: on the west through the Sakhalin Gulf and the Gulf of Tartary ; on the south through the La Pérouse Strait . In winter, navigation on the Sea of Okhotsk is impeded by ice floes . Ice floes form due to the large amount of freshwater from the Amur River , lowering the salinity of upper levels, often raising the freezing point of

232-526: Is the highest point of the range. Berill Mountain , at 2,933 metres (9,623 ft) is the highest summit in Khabarovsk Krai. Mount Khakandya (Гора Хакандя) is an ultra-prominent peak that is 2,615 metres (8,579 ft) high. The Suntar-Khayata Range is geographically a southeastern prolongation of the Verkhoyansk Range . Until mid 20th century it was treated as a separate range, together with

261-584: The Kuril Islands were administered by Japan until 1945. Japan claims the southern Kuril Islands and refers to them as Northern Territories . The International Hydrographic Organization defines the limits of the Sea of Okhotsk as follows: :: On the Southwest. The Northeastern and Northern limits on the Japan Sea [In La Perouse Strait (Sôya Kaikyô). A line joining Sôni Misaki and Nishi Notoro Misaki (45°55'N). From Cape Tuik (51°45'N) to Cape Sushcheva]. :: On

290-706: The Okhota , Ulbeya , Inya , Kukhtuy and Yana flow into the Sea of Okhotsk. The range includes the southernmost glaciers in the Russian Far East outside of Kamchatka . Their status is not known. The strata of this geological formation date back to the Late Jurassic . Dinosaur remains are among the fossils that have been recovered from the formation. The higher slopes of the range are sparsely wooded, with mainly larch forests and tundra . A small population of Brown Dippers (Cinclus pallasi) winters at

319-665: The Skalisty Range , highest point 2,017 metres (6,617 ft), and the Sette Daban , highest point 2,017 metres (6,617 ft), to the southwest. The Yudoma-Maya Highlands are located to the south of the range and the Upper Kolyma Highlands to the northeast. The Suntar-Khayata system comprises a number of subranges, including the Khalkan Range , Net-Taga Range , Yudoma Range and Kukhtuy Range . The Suntar-Khayata

SECTION 10

#1732851451925

348-632: The 1640s. The Dutch captain Maarten Gerritsz Vries in the Breskens entered the Sea of Okhotsk from the south-east in 1643, and charted parts of the Sakhalin coast and Kuril Islands, but failed to realize that either Sakhalin or Hokkaido are islands. During this period, the sea was sometimes known as the Sea of Kamchatka . The first and foremost Russian settlement on the shore was the port of Okhotsk , which relinquished commercial supremacy to Ayan in

377-475: The 1840s. The Russian-American Company all but monopolized the commercial navigation of the sea in the first half of the 19th century. The Second Kamchatka Expedition under Vitus Bering systematically mapped the entire coast of the sea, starting in 1733. Jean-François de Galaup, comte de Lapérouse and William Robert Broughton were the first non-Russian European navigators known to have passed through these waters other than Vries. Ivan Krusenstern explored

406-685: The Kukhtuy is a spawning ground for the coho salmon . Other fish species are also abundant in its waters, such as the Amur whitefish , East Siberian grayling , whitespotted char and round whitefish . This article related to a river in the Russian Far East is a stub . You can help Misplaced Pages by expanding it . This Khabarovsk Krai location article is a stub . You can help Misplaced Pages by expanding it . Suntar-Khayata Suntar-Khayata Range ( Russian : Сунтар-Хаята , Yakut : Сунтаар Хайата )

435-640: The Russian EEZ, any country could fish there, and some began doing so in large numbers in 1991, catching perhaps as much as one million metric tons of pollock in 1992. This was seen by the Russian Federation as presenting a danger to Russian fish stocks, since the fish move in and out of the Peanut Hole from the Russian EEZ. The Russian Federation petitioned the United Nations to declare the Peanut Hole to be part of Russia's continental shelf . In November 2013,

464-448: The Russian oil drilling rig Kolskaya capsized and sank in a storm in the Sea of Okhotsk, some 124 km (77 mi) from Sakhalin island, where it was being towed from Kamchatka . Reportedly, its pumps failed, causing it to take on water and sink. The platform carried 67 people, of which 14 were rescued by the Magadan and the tugboat Natftogaz-55 . The platform was subcontracted to

493-401: The Sea of Okhotsk as a nesting site. The Okhotsk culture and the later Ainu people , a coastal fishing and hunter-gatherer people, were located around the lands surrounding the Sea of Okhotsk, as well as in northern Japan. Russian explorers Vassili Poyarkov (1639) and Ivan Moskvitin (1645) were the first Europeans to visit the Sea of Okhotsk (and, probably, the island of Sakhalin ) in

522-458: The Sea of Okhotsk is the subject of the most famous novel of the Japanese writer Takiji Kobayashi , The Crab Cannery Ship (1929). The Peanut Hole (named for its shape) was an area of open ocean at the center of the Sea of Okhotsk, about 55 km (30 mi) wide and 480 km (300 mi) long, that was surrounded by Russia's exclusive economic zone (EEZ). Since the Peanut Hole was not in

551-619: The Southeast. A line running from Nosyappu Saki (Cape Noshap, 43°23'N) in the Island of Hokusyû (Yezo) through the Kuril or Tisima Islands to Cape Lopatka (South point of Kamchatka ) in such a way that all the narrow waters between Hokusyû and Kamchatka are included in the Sea of Okhotsk. Some of the Sea of Okhotsk's islands are quite large, including Japan's second-largest island, Hokkaido, as well as Russia's largest island, Sakhalin. Practically all of

580-470: The east. South of the 61st parallel the river valley widens and the Kukhtuy meanders across a widening floodplain with many bogs and small lakes. Finally it flows into the Sea of Okhotsk on the northeastern side of the estuary of Okhotsk town. The main tributary of the Kukhtuy is the 178 kilometres (111 mi) long Gusinka (Гусинка) that joins it from the left. The river freezes around late October and stays frozen until mid May. The basin of

609-440: The eastern coast of Sakhalin in 1805. Mamiya Rinzō and Gennady Nevelskoy determined that Sakhalin was indeed an island separated from the mainland by a narrow strait. The first detailed summary of the hydrology of the Sea of Okhotsk was prepared and published by Stepan Makarov in 1894. The Sea of Okhotsk is rich in biological resources, with various kinds of fish, shellfish and crabs. The harsh conditions of crab fishing in

SECTION 20

#1732851451925

638-546: The end of World War II in 1945. Afterward, the Soviet Union occupied the territory. During the Cold War , the Sea of Okhotsk was the scene of several successful U.S. Navy operations (including Operation Ivy Bells ) to tap Soviet Navy undersea communications cables. These operations were documented in the 1998 book Blind Man's Bluff: The Untold Story of American Submarine Espionage . The sea (and surrounding area) were also

667-523: The fleet back to the Sea of Okhotsk. From 1854 to 1856, an average of over 160 vessels cruised in the sea each year. As catches declined between 1858 and 1860 the fleet shifted back to the Bering Strait region. The Russian military marine mammal program reportedly sources some of its animals from the Sea of Okhotsk. South Sakhalin was administered by Japan as Karafuto Prefecture from 1907 to 1949. The Kuril Islands were Japanese from 1855 and 1875 till

696-421: The global mean. Warming inhibits the formation of sea ice and also drives fish populations north. The salmon catch on the northern Japanese coast has fallen 70% in the last 15 years, while the Russian chum salmon catch has quadrupled. With the exception of Hokkaido , one of the Japanese home islands , the sea is surrounded on all sides by territory administered by the Russian Federation. South Sakhalin and

725-545: The island of Sakhalin along the west, and a stretch of eastern Siberian coast along the west and north. Its northeast corner is the Shelikhov Gulf . The sea is named for the port of Okhotsk , itself named for the Okhota River . The Sea of Okhotsk covers an area of 1,583,000 square kilometres (611,000 sq mi), with a mean depth of 859 metres (2,818 ft) and a maximum depth of 3,372 metres (11,063 ft). It

754-503: The name of Hokkaidō's Okhotsk Subprefecture , which faces the Sea of Okhotsk and is also known as the Okhotsk region ( オホーツク地方 , Ohōtsuku-chihō ) . Twenty-nine zones of possible oil and gas accumulation have been identified on the Sea of Okhotsk shelf, which runs along the coast. Total reserves are estimated at 3.5 billion tons of equivalent fuel, including 1.2 billion tons of oil and 1.5 billion cubic meters of gas. On 18 December 2011,

783-507: The scene of the Soviet attack on Korean Air Lines Flight 007 in 1983. The Soviet Pacific Fleet used the sea as a ballistic missile submarine bastion , a strategy that Russia continues. Despite its proximity to Japan, the Sea of Okhotsk has no native etymology in the Japanese language ; its name, Ohōtsuku-kai ( オホーツク海 ), is a transcription of the Russian name. This is also reflected in

812-572: The sea surface. The distribution and thickness of ice floes depends on many factors: the location, the time of year, water currents, and the sea temperatures. Cold air from Siberia forms sea ice in the northwestern Sea of Okhotsk. As the ice forms, it expels salt into the deeper layers. This heavy water flows east toward the Pacific, carrying oxygen and nutrients, supporting abundant sea life. The Sea of Okhotsk has warmed in some places by as much as 3°C (5.4°F) since preindustrial times, three times faster than

841-717: The sea's islands are either in coastal waters or belong to the various islands making up the Kuril Islands chain. These fall either under undisputed Japanese or Russian ownership or disputed ownership between Japan and Russia. Iony Island is the only island located in open waters and belongs to the Khabarovsk Krai of the Russian Federation . The majority of the sea's islands are uninhabited, making them ideal breeding grounds for seals , sea lions , seabirds , and other sea island fauna. Large colonies of crested auklets use

#924075