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Ukvushvuynen Range
The Ukvushvuynen Range (russian: горы Уквушвуйнен; zh, 乌克武什武伊年山), also known as Meingypilgyn Range (russian: Мэйнгыпильгынский хребет), is a range of mountains in Chukotka Autonomous Okrug, Russian Far East. Administratively the range is part of Anadyr District.Google Earth Geography The Ukvushvuynen Range is the easternmost subrange of the Koryak Highlands, East Siberian Mountains. It stretches roughly from east to west in southern Chukotka, between the Koyverelan Range to the west and Cape Navarin in the Bering Sea to the east. To the northwest rises the Rarytkin Range and the Velikaya River flows into the Anadyr Lowlands. To the southwest stretches the Komeutyuyam Range. The highest mountains of the Ukvushvuynen Range are located in its western part. The highest summit is high Gora Krasnaya (гора красная), rising to the south of lake Yanragytgyn. Other high peaks of the range are high Gora Tsirk (гора ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Pekulney
Lake Pekulney (russian: Пекульнейское озеро) is a lake of Anadyr District, Chukotka Autonomous Okrug, Russia. The lake has a basin area of which makes it the second largest lake in the Chukotka Autonomous Okrug after Lake Krasnoye, and the 27th largest in area in Russia. There are commercial fisheries of sockeye salmon in the lake. The Kakanaut Formation is a geological formation named after the small river flowing into the lake at the head of its northeastern bay.Michael C. Boulter, Helen Fisher eds. ''Cenozoic Plants and Climates of the Arctic'', p. 130 Geography Lake Pekulney is a coastal lagoon separated from the sea by a narrow spit at its southern end. It is roughly Y-shaped with Pekulveyem Bay in the northwest and Kakanaut Bay in the northeast. The Mayn Channel flows from it in the south connecting it with the Bering Sea. Pekulney Lake is connected by channels with neighboring Lake Vaamochka to the west. The village of Meynypilgyno is located between ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bering Sea
The Bering Sea (, ; rus, Бе́рингово мо́ре, r=Béringovo móre) is a marginal sea of the Northern Pacific Ocean. It forms, along with the Bering Strait, the divide between the two largest landmasses on Earth: Eurasia and The Americas. It comprises a deep water basin, which then rises through a narrow slope into the shallower water above the continental shelf, continental shelves. The Bering Sea is named for Vitus Bering, a Denmark, Danish navigator in Russian service, who, in 1728, was the first European to systematically explore it, sailing from the Pacific Ocean northward to the Arctic Ocean. The Bering Sea is separated from the Gulf of Alaska by the Alaska Peninsula. It covers over and is bordered on the east and northeast by Alaska, on the west by the Russian Far East and the Kamchatka Peninsula, on the south by the Alaska Peninsula and the Aleutian Islands and on the far north by the Bering Strait, which connects the Bering Sea to the Arctic Ocean's Chukchi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maastrichtian
The Maastrichtian () is, in the ICS geologic timescale, the latest age (uppermost stage) of the Late Cretaceous Epoch or Upper Cretaceous Series, the Cretaceous Period or System, and of the Mesozoic Era or Erathem. It spanned the interval from . The Maastrichtian was preceded by the Campanian and succeeded by the Danian (part of the Paleogene and Paleocene). The Cretaceous–Paleogene extinction event (formerly known as the Cretaceous–Tertiary extinction event) occurred at the end of this age. In this mass extinction, many commonly recognized groups such as non-avian dinosaurs, plesiosaurs and mosasaurs, as well as many other lesser-known groups, died out. The cause of the extinction is most commonly linked to an asteroid about wide colliding with Earth, ending the Cretaceous. Stratigraphic definitions Definition The Maastrichtian was introduced into scientific literature by Belgian geologist André Hubert Dumont in 1849, after studying rock strata of the Chalk Group c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kakanaut Formation
The Kakanaut Formation is a geological Formation (geology), formation in Siberia, whose strata date back to the Late Cretaceous (Maastrichtian). Dinosaur remains are among the fossils that have been recovered from the formation.Weishampel et al., 2004, pp.593-600 The flora of the formation is relictual, containing some of the youngest remains of the extinct plant orders Bennettitales and Czekanowskiales. Fossil content * ''Troodon, Troodon cf. formosus'' * Ankylosauria, Ankylosauria indet. * Dinosauria, Dinosauria indet. * Dromaeosauridae, Dromaeosauridae indet. * Hadrosauridae, Hadrosauridae indet. * Neoceratopsia, Neoceratopsia indet. * Ornithopoda, Ornithopoda indet. * Prismatoolithidae, Prismatoolithidae indet. * Spheroolithidae, Spheroolithidae indet. * Theropoda, Theropoda indet. * Tyrannosauridae, Tyrannosauridae indet. * Aves, ?Aves indet. See also * List of dinosaur-bearing rock formations * List of fossiliferous stratigraphic units in Russia References Bibliog ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kakanaut River
Lake Pekulney (russian: Пекульнейское озеро) is a lake of Anadyr District, Chukotka Autonomous Okrug, Russia. The lake has a basin area of which makes it the second largest lake in the Chukotka Autonomous Okrug after Lake Krasnoye, and the 27th largest in area in Russia. There are commercial fisheries of sockeye salmon in the lake. The Kakanaut Formation is a geological formation named after the small river flowing into the lake at the head of its northeastern bay.Michael C. Boulter, Helen Fisher eds. ''Cenozoic Plants and Climates of the Arctic'', p. 130 Geography Lake Pekulney is a coastal lagoon separated from the sea by a narrow spit at its southern end. It is roughly Y-shaped with Pekulveyem Bay in the northwest and Kakanaut Bay in the northeast. The Mayn Channel flows from it in the south connecting it with the Bering Sea. Pekulney Lake is connected by channels with neighboring Lake Vaamochka to the west. The village of Meynypilgyno is located between ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur only in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coastal Lagoon
A lagoon is a shallow body of water separated from a larger body of water by a narrow landform, such as reefs, barrier islands, barrier peninsulas, or isthmuses. Lagoons are commonly divided into ''coastal lagoons'' (or ''barrier lagoons'') and ''atoll lagoons''. They have also been identified as occurring on mixed-sand and gravel coastlines. There is an overlap between bodies of water classified as coastal lagoons and bodies of water classified as estuaries. Lagoons are common coastal features around many parts of the world. Definition and terminology Lagoons are shallow, often elongated bodies of water separated from a larger body of water by a shallow or exposed shoal, coral reef, or similar feature. Some authorities include fresh water bodies in the definition of "lagoon", while others explicitly restrict "lagoon" to bodies of water with some degree of salinity. The distinction between "lagoon" and "estuary" also varies between authorities. Richard A. Davis Jr. restrict ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maynits
Maynits (; ) is a freshwater lake in Anadyr District, Chukotka Autonomous Okrug, Russian Federation.Google Earth It has an area of almost . There are no permanent settlements on the shores of the lake. The name of the lake in Chukot is derived from ''Mainygytgyn'', meaning "big lake." Geography Maynits lies approximately in the middle of the Ukvushvuynen Range, part of the Koryak Mountains. It is located southeast of lake Yanragytgyn. The lake stretches roughly from north to south and has a larger northern section with a long and wide island in the middle near the northeastern lakeshore. The smaller southern section stretches from NNW to SSE for and has a width of about . Both sections are connected by a narrow sound. The lakeshore is pebbly, made up of small and regular pebbles. The long Gytgypokytkynvaam river enters the lake from the south and the Gytgyveem, a long tributary of the Nygchekveem, flows out of the northern end of the main lake. Maynits freezes in Octob ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yanragytgyn
Yanragytgyn (; ) is a freshwater lake in Anadyr District, Chukotka Autonomous Okrug, Russian Federation.Google Earth It has an area of . There are no permanent settlements on the shores of the lake. The name of the lake in Chukot means "a separate lake."Leontiev V.V. & Novikova K.A. ''Toponymic Dictionary of the North-East of the USSR'' / scientific. ed. G. A. Menovschikov; FEB AN USSR . North-East complex. Research institutes. Lab archeology, history and ethnography. - Magadan: Magad. Prince Publishing House, 1989 . Geography Yanragytgyn lies close to the northern slopes of the Ukvushvuynen Range, part of the Koryak Mountains. It is located southwest of lake Krasnoye and northwest of lake Maynits. The lake is roughly pear-shaped and stretches roughly from north to south. The southern section includes a few small islands close to the shore. Yanragytgyn lies in a swampy flat area of the southwestern part of the Anadyr Lowland dotted with thermokarst lakes. An unnamed tr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gora Krasnaya
Gora may refer to: *Gora (surname) *'' Gora'', a Bengali novel by Nobel laureate Rabindranath Tagore *Gora (musical instrument) *''G.O.R.A.'', a 2004 Turkish comedy film *Goparaju Ramachandra Rao ("Gora", 1902–1975), Indian social reformer and atheist activist Places *Gora (region), in southern Kosovo and north-eastern Albania * Gora, Croatia, a village near Petrinja, Croatia * Góra (other), places in Poland *Gora, Russia, several rural localities in Russia *Gora (Kakanj), a village in Bosnia and Herzegovina *Gora (Vogošća), a village in Bosnia and Herzegovina *Gora, Krško, a settlement in the Municipality of Krško, Slovenia *Gora nad Sodražico (also known as Gora), Slovenia, a community and parish comprising the villages of Betonovo, Kračali, Janeži, Petrinci, and Kržeti *Gora Ardan, a peak in the western plains of Turkmenistan *Gora Cemetery (other) *Gōra Station is a terminal railway station on the Hakone Tozan Line as well as the Hakone Tozan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Komeutyuyam Range
The Komeutyuyam Range (russian: Комеутюямский хребет; zh, 科梅乌秋亚姆斯基山) is a range of mountains in Chukotka Autonomous Okrug and Kamchatka Krai, Russian Far East. Administratively the northern section of the range belongs to the Anadyr District of Chukotka Autonomous Okrug, and the southern to Olyutorsky District of Kamchatka Krai.Google Earth Geography The Komeutyuyam Range is part of the Koryak Highland system. It stretches parallel to the Bering Sea coast, about inland, in a NE/SW direction between the western end of the Ukvushvuynen Range in the north and the Pikas Range in the south. The valley of the Pikasvayam, the largest tributary of the Ukelayat, marks its southern end. The highest point of the range is Mt Volokvyneitkon (гора Волоквынейткон) — or Mt Valvykvyneitkon (гора Валвыквынейткон), a high peak, located in the southwestern sector of the range, near the limit between Chukotka Auton ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
