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Severo-Kurilsky District
Severo-Kurilsky District (russian: Се́веро-Кури́льский райо́н) is an administrative district (raion) of Sakhalin Oblast, Russia; one of the seventeen in the oblast.Law #25-ZO Municipally, it is incorporated as Severo-Kurilsky Urban Okrug.Law #524 It is located on the northern Kuril Islands to the east of the Island of Sakhalin and immediately southwest of the Kamchatka Peninsula. The area of the district is . Its administrative center is the town of Severo-Kurilsk on Paramushir island. Population: The population of Severo-Kurilsk accounts for almost 100% of the district's total population,No population was reported during the 2010 Census for the only rural locality in the district. though there is often a seasonal population on the island of Shumshu. Islands The district includes the following islands from north to south: }!!style="background: #CCC;" class="unsortable", ja, Name!!style="background: #CCC;" class="unsortable", Alternativenames!!style="ba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sakhalin Oblast
Sakhalin Oblast ( rus, Сахали́нская о́бласть, r=Sakhalínskaya óblast', p=səxɐˈlʲinskəjə ˈobləsʲtʲ) is a federal subjects of Russia, federal subject of Russia (an oblast) comprising the island of Sakhalin and the Kuril Islands in the Russian Far East. The oblast has an area of . Its administrative center and largest types of inhabited localities in Russia, city is Yuzhno-Sakhalinsk. As of the Russian Census (2010), 2010 Census, the oblast has a population of roughly 500,000. The vast majority of the oblast's residents are ethnic Russians, with a small minority of Koreans. Sakhalin Oblast is rich in natural gas and oil, and is List of federal subjects of Russia by GDP per capita, Russia's fourth wealthiest federal subject and wealthiest oblast. It borders by sea Khabarovsk Krai to the west and Kamchatka Krai to the north, along with Hokkaido, Japan to the south. Demographics Population: ;Vital statistics for 2012 *Births: 6,316 (12.8 per 1,000) *D ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Podgorny
Nikolai Viktorovich Podgorny, ''Mykola Viktorovych Pidhornyy'' rus, Никола́й Ви́кторович Подго́рный, p=nʲɪkɐˈlaj ˈvʲiktərəvʲɪtɕ pɐdˈgornɨj, links=yes ( – 12 January 1983) was a Soviet statesman who served as the Chairman of the Presidium of the Supreme Soviet, the head of state of the Soviet Union, from 1965 to 1977. Podgorny was born to a Ukrainian working-class family in the city of Karlovka in 18 February 1903. He later graduated from a local worker's school in 1926 before completing his education at the Kyiv Technological Institute of Food Industry in 1931. In 1930, Podgorny became a member of the ruling Communist Party of the Soviet Union and climbed up the Soviet hierarchy after years of service to the country's centrally planned economy. By 1953, Podgorny became Second Secretary of the Communist Party of Ukraine in 1953 before later serving as First Secretary of the Communist Party of Ukraine from 1957 to 1963. In October ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rasshua
Rasshua (russian: Расшуа, ja, 羅処和島), is an uninhabited volcanic island near the center of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean, from Ushishir and southwest of Matua. Its name is derived from the Ainu language for “fur coat”. Geology Rasshua is roughly oval, with a length of with a width of , and an area of . The island is a complex stratovolcano with three overlapping central cones within a 6 kilometer caldera whose eastern margin is beyond the shoreline. The island has five small fresh water lakes, and numerous hot springs. Rasshua Peak (russian: влк. Расшуа, ja, 幌茶々登山, Horochachanobori-yama), in the west of the island is the island’s highest point at . The peak has not erupted in historic times, although it emits quantities of volcanic gas and its sides are streaked with sulfur deposits. The easternmost cone ( ja, 長頭山, Chōtōzan; (russian: гора Циото) with a height of , vio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Matua (island)
Matua (russian: Матуа, ja, 松輪島, Matsuwa-tō) is an uninhabited volcanic island near the center of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean, across Golovnin Strait from Raikoke. Its name is derived from the Ainu language, from “hellmouth”. History Hunting and fishing parties of the Ainu have long visited Matua, but the island had no permanent habitation at the time of European contact. It appears on an official map showing the territories of the Matsumae Domain, a feudal domain of Edo period Japan dated 1644, and the Tokugawa shogunate officially confirmed these holdings in 1715. Some early European documents refer to the island as ''Raukoke''. The Empire of Russia claimed sovereignty over the island, which initially passed to Russia under the terms of the Treaty of Shimoda (1855), but reverted to the Empire of Japan per the Treaty of Saint Petersburg along with the rest of the Kuril islands. Japan formerly administered Matu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Raikoke
Raikoke (russian: Райкоке, ja, 雷公計島), also spelled Raykoke, is, as of 2019 a Russian uninhabited volcanic island near the centre of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean, distant from the island of Matua. Its name is derived from the Ainu language, from “hellmouth”. Geology Raikoke is roughly circular, with a length of with a width of , and an area of . The island is a stratovolcano, its lava composed primarily of basalt. The cone rises above a submarine terrace with a depth of to a maximum height of above sea level. The steep-walled crater is wide and deep with lava flows extending along the eastern half of the island. The volcano has most recently erupted in 1765, 1778, 1924 and 2019. The 1778 and 1924 Raikoke eruptions were classified on the Volcanic Explosivity Index scale (that ranges from zero to eight) as VEI-4 or greater. For comparison the volcano Anak Krakatoa eruption in 2018 was also rated as a VEI-4 ev ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shiashkotan
Shiashkotan (russian: Шиашкотан); ( ja, 捨子古丹島; Shasukotan-tō) is an uninhabited volcanic island near the center of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean, separated from Ekarma by the Ekarma Strait. Its name is derived from the Ainu language, from “Konbu village”. Geology Shiashkotan is roughly dumbbell-shaped, formed by two volcanic islands joined together by a narrow landspit. The island has a total length of with a width ranging from at its widest point to at its narrowest, and an area of . Both ends of the island are complex stratovolcanos, and landing is possible only on the sandy isthmus. * Pik Sinarka (russian: влк. Синарка; ja, 黒岳; ''Kurodake''), which rises to above sea level occupies the northern end of the island, and is the island’s highest point. Historical eruptions have occurred at Sinarka during 1825–1750, 1846, 1855, and the last and largest from 1872 to 1878. To the east from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chirinkotan
Chirinkotan (russian: Чиринкотан; Japanese 知林古丹島; Chirinkotan-tō) is an uninhabited volcanic island located in the centre of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. Its name is derived from the Ainu language for "mudslide". It is located west of Ekarma, its nearest neighbor. Geology Chirinkotan is at the far end of a volcanic chain extending nearly 50 km west of the central part of the main Kuril Islands arc. The island is the top of a partially submerged stratovolcano rising approximately from the floor of the Sea of Okhotsk, and is roughly circular with an area of . The island's highest point ("Masaochi" in Ainu) is high, and is still an active volcano with major eruptions recorded in 1760, 1884, 1900, 1979, 1986, 2004, and 2013. Reports of a 1955 eruption are unconfirmed. The caldera is approximately wide, with a depth of , and is breached on its south-east side. The shores of the island are steep cliffs, m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ekarma
Ekarma (russian: Экарма; Japanese 越渇磨島; Ekaruma-tō) is an uninhabited volcanic island near the center of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean, separated from Shiashkotan by the Ekarma Strait. Its name is derived from the Ainu language, from “safe anchorage”. Geology Ekarma is roughly oval, measuring by with an area of . The island consists of two overlapping stratovolcano, collectively called Pik Ekarma -(russian: влк.Экарма ; Japanese 越渇磨岳; ''Ekaruma-dake''), which rises to above sea level. Lava flows radiate in all directly from the central peak, forming an uneven shoreline. Numerous hot springs with sulphur deposits are on the northern slopes of the mountain. The last eruption of the mountain was in May 1980, during which ash emissions reaching a height of one kilometer were observed from a fishing vessel. History Ekarma was visited by hunting and fishing parties of Ainu at the time of European ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kharimkotan
Kharimkotan (russian: Харимкотан); Japanese 春牟古丹島; Harimukotan-tō, alternatively Harumukotan-tō or 加林古丹島; Karinkotan-tō) is an uninhabited volcanic island located from Onekotan near the northern end of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. Its name is derived from the Ainu language, from “village of many Cardiocrinum”. Geology Kharimkotan is roughly oval, measuring by with an area of . The landscapes of the island are quite diverse; however, a significant part of the island's surface is covered with fine yellow ash, resembling desert dunes. On the north-western cape are the ruins of an Ainu village and in the north of the island, on the shore of Severgin Bay, is the abandoned settlement of Severgino. There are a number of small freshwater lakes. Kharimkotan is separated by the Sixth Kuril Strait from Onekotan, located 15 kilometers to the northeast, and by the Severgin Strait from Shiashkotan, lo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Onekotan
Onekotan (russian: Онекотан; Japanese 温禰古丹島; Onekotan-tō, occasionally Onnekotan-tō, ain, オネコタン or オネコタㇴ) is an uninhabited volcanic island located near the northern end of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. Its name is derived from the Ainu language for "large village”. It is the second largest island, after Paramushir, in the northern subgroup of the Kurils. It is administratively included in the Severo-Kurilsky District of Sakhalin oblast, Russia. Geography and geology Onekotan is roughly rectangular, with a length of , and a width ranging from . It has an area of The island consists of two stratovolcanos connected by a relatively flat isthmus. * Krenitsyn -(russian: Креницын ; Japanese 黒石山; ''Kuroishiyama'') with a height of is the prominent caldera at the southern end of the island. This volcano was named after Captain Pyotr Krenitsyn of the Imperial Russian Navy. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Makanrushi
Makanrushi (russian: Маканруши; Japanese 磨勘留島; Makanru-tō) is an uninhabited volcanic island located near the northern end of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. Its name is derived from the Ainu language. Geology Makanrushi is roughly rectangular, with an area of The island consists of a dormant or extinct stratovolcano, Pik Mitaka -(russian: влк.Митака ; Japanese 三高山; ''Mitakayama''), which rises to above sea level. The island has steep cliff sides and no sandy beaches, making landing very difficult and dangerous even in calm weather. Makanrushi is 28 km away from Onekotan. Makanrushi thus lies behind the main currently-active arc of Kuril Island volcanoes. History Makanrushi appears to have never been inhabited. It appears on an official map showing the territories of Matsumae Domain, a feudal domain of Edo period Japan dated 1644, and these holdings were officially confirmed by the Tok ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antsiferov Island
Antsiferov Island (russian: Остров Анциферова; also known as Shirinki russian: Ширинки Japanese 志林規島; Shirinki-tō) is an uninhabited volcanic island located in the northern Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. Its former Japanese name is derived from the Ainu language for "place of tall waves". Its nearest neighbor is Paramushir, located 15 km away across the Luzhin Strait. It is currently named for the cossack explorer Danila Antsiferov, who first described it along with other northern Kuril islands in the early eighteenth century. Geology Antsiferov is a roughly circular island with an area of 6 km2 and is part of a spur range extending to the west of the main Kuril islands arc. The island is a stratovolcano with a diameter of 4.25 km and with a central peak (Japanese 蓮華岳; Renge-dake) with a height of 761 metres which is marked by a caldera which is 0.75 kilometre in diameter, which i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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