Anadyrskiy Gulf
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Anadyrskiy Gulf
Anadyrsky District (russian: Ана́дырский райо́н; Chukchi: , ''Kagyrgyn rajon'') is an administrativeLaw #33-OZ and municipalLaw #148-OZ district (raion), one of the six in Chukotka Autonomous Okrug, Russia. It is located in the central and southern parts of the autonomous okrug and borders with Chaunsky District in the northwest, Iultinsky District in the north and northeast, the Gulf of Anadyr in the east, Koryak Okrug in the south, and with Bilibinsky District in the west and northwest. It also completely surrounds the territory of the town of okrug significance of Anadyr. The area of the district is .Official website of Anadyrsky DistrictGeneral information Its administrative center is the town of Anadyr (which is not administratively a part of the district). Population: In terms of area, this is the largest district in the autonomous okrug. The district is located in a mountainous region, the peaks of which provide the catchment areas for the Anadyr Rive ...
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Lake Maynits
A lake is an area filled with water, localized in a Depression (geology), basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the World Ocean, ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glacier, glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic dra ...
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Anadyr River
The Anadyr (russian: Ана́дырь; Yukaghir: Онандырь; ckt, Йъаайваам) is a river in the far northeast of Siberia which flows into the Gulf of Anadyr of the Bering Sea and drains much of the interior of Chukotka Autonomous Okrug. Its basin corresponds to the Anadyrsky District of Chukotka. Geography The Anadyr is long and has a basin of . It is frozen from October to late May and has a maximum flow in June with the snowmelt. It is navigable in small boats for about to near Markovo. West of Markovo it is in the Anadyr Highlands (moderate mountains and valleys with a few trees) and east of Markovo it moves into the Anadyr Lowlands (very flat treeless tundra with lakes and bogs). The drop from Markovo to the sea is less than . It rises at about 67°N latitude and 171°E longitude in the Anadyr Highlands, near the headwaters of the Maly Anyuy, flows southwest receiving the waters of the rivers Yablon and Yeropol, turns east around the Shchuchy Range an ...
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Spit (landform)
A spit or sandspit is a deposition bar or beach landform off coasts or lake shores. It develops in places where re-entrance occurs, such as at a cove's headlands, by the process of longshore drift by longshore currents. The drift occurs due to waves meeting the beach at an oblique angle, moving sediment down the beach in a zigzag pattern. This is complemented by longshore currents, which further transport sediment through the water alongside the beach. These currents are caused by the same waves that cause the drift. Hydrology and geology Where the direction of the shore inland ''re-enters'', or changes direction, for example at a headland, the longshore current spreads out or dissipates. No longer able to carry the full load, much of the sediment is dropped. This is called deposition. This submerged bar of sediment allows longshore drift or littoral drift to continue to transport sediment in the direction the waves are breaking, forming an above-water spit. Without the co ...
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Russkaya Koshka
Russkaya Koshka (Russian: Русская Кошка) is a spit that divides the Anadyr Estuary from the Gulf of Anadyr. The name literally translates as "the Russian cat"; but in fact ''koshka'' is the dialectal word for "sand spit A spit or sandspit is a deposition bar or beach landform off coasts or lake shores. It develops in places where re-entrance occurs, such as at a cove's headlands, by the process of longshore drift by longshore currents. The drift occurs due to ...". The spit is 16 km long and up to 2 km wide. It has an average elevation of 3 to 4 meters. An unusually low lighthouse stands at the end of the spit. The southern tip of the spit is Cape St. Basil (or St. Basilius) in old sources. The bay between the spit and the mainland is (or was) called Klinkowstroem Bay, an arm of the Anadyr Estuary. Spits of Russia Landforms of Chukotka Autonomous Okrug Landforms of the Bering Sea {{ChukotkaAutonomousOkrug-geo-stub ...
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Shakhtyorsky, Chukotka Autonomous Okrug
Shakhtyorsky (russian: Шахтёрский), is an urban-type settlement in Anadyrsky District of Chukotka Autonomous Okrug, Russia. As of 2008, it is in the process of being abolished due to it no longer being considered economically viable to continue mining in the area.Shakhtyorsky
- www.dead-cities.ru
Population: 328 ( 2002 Census); As a result of the cessation of mining activities, the population of the settlement has continued to decline. By 2005, an environmental impact report prepared for the Kupol Gold Project indicated that the population of Shakhtyorsky had fallen to just 93 people.
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Ugolnye Kopi
Ugolnye Kopi (russian: У́гольные Ко́пи, lit. ''coal mines'') is an urban locality (an urban-type settlement) in Anadyrsky District of Chukotka Autonomous Okrug, Russia, located east of Anadyr, the administrative center of the autonomous okrug, on the opposite side of the Anadyr River. It served as the administrative center of Anadyrsky District until June 2011. Population: with an estimated population as of 1 January 2015 of 3,666. It is a mainly mining town that also hosts the region's main airport. History Pre-history Traces of fossil flora and fauna dating to the late Cretaceous and Paleocene were discovered on the territory of modern Ugolnye Kopi in 2003, in the area known as the Golden Ridge, in the Ugolnoye and Pervomaysky fields. These areas exhibit extensive fossil flora and fauna composition; the fossilized plant remains are well-preserved. There are currently about 130 items in the Chukotka Heritage Museum in Anadyr. Pollen grains extracted fro ...
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Anadyrsky Liman
Anadyrskiy Liman (russian: Анадырский Лиман) or Anadyr Estuary is an estuary on the Gulf of Anadyr in Chukotka Autonomous Okrug, Siberia, Russian Federation. Geography It is called a liman because it is separated from the Gulf of Anadyr by the Russkaya Koshka spit in the north and another spit (Geka Point) in the south. The channel into the Gulf of Anadyr through the bar is in the east. The Anadyr Lowlands are located to the west. Google Earth Anadyrskiy Liman is divided into three parts. The outer bay receives the Tretya River (its mouth is the notch on the south shore). The southern part of the outer bay is shallow. The inner bay is called Onemen Bay and receives the Velikaya through a narrow bay on the southwest. They are separated by a promontory, with the town of Anadyr at its tip. North of the promontory is a series of lakes which form the mouth of the Kanchalan River. The Anadyr River The Anadyr (russian: Ана́дырь; Yukaghir: Онандыр ...
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Estuary
An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environments and are an example of an ecotone. Estuaries are subject both to marine influences such as tides, waves, and the influx of saline water, and to fluvial influences such as flows of freshwater and sediment. The mixing of seawater and freshwater provides high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world. Most existing estuaries formed during the Holocene epoch with the flooding of river-eroded or glacially scoured valleys when the sea level began to rise about 10,000–12,000 years ago. Estuaries are typically classified according to their geomorphological features or to water-circulation patterns. They can have many different names, such as bays, ...
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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 ...
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Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ...
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Semyon Dezhnyov
Semyon Ivanovich Dezhnyov ( rus, Семён Ива́нович Дежнёв, p=sʲɪˈmʲɵn ɪˈvanəvʲɪtɕ dʲɪˈʐnʲɵf; sometimes spelled Dezhnyov; c. 1605 – 1673) was a Russian explorer of Siberia and the first European to sail through the Bering Strait, 80 years before Vitus Bering did. In 1648 he sailed from the Kolyma River on the Arctic Ocean to the Anadyr River on the Pacific. His exploit was forgotten for almost a hundred years and Bering is usually given credit for discovering the strait that bears his name. Biography Dezhnyov was a Pomor Russian, born about 1605, possibly in the town of Veliky Ustyug or the village of Pinega. According to the anthropologist Lydia T. Black, Dezhnyov was recruited for Siberian service in 1630, possibly as a service man or government agent. He served for eight years in Tobolsk and Yeniseisk, and then went to Yakutia in 1639, or possibly earlier. He is said to have been a member of the Cossack detachment under Beketov, who is cred ...
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