Chukotka Mountains
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Chukotka Mountains
The Chukotka Mountains ( rus, Чукотское нагорье) or Chukotka Upland ''(Чукотская горная страна)'' is a mountainous area in the Chukotka Autonomous Okrug, Far Eastern Federal District, Russia.Chukchi Highlands
/ Great Russian Encyclopedia; in 35 vol.] / Ch. ed. Yu.S. Osipov . - M .: , 2004—2017.
The of this system are largely barren and desolate. About half of their area is above the

Palyavaam Range
, image = Горное правобережье р. Паляваам.jpg , image_size = , image_caption = View of the Palyavaam River , pushpin_map = Russia Chukotka Autonomous Okrug , pushpin_map_size = , pushpin_map_caption= Location of the mouth in the Chukotka Autonomous Okrug, Russia , source1_location = Palyavaam Range , source1_coordinates = , source1_elevation = , mouth_location = Chaun , mouth_coordinates = , mouth_elevation = , progression = Chaun→ East Siberian Sea , subdivision_type1 = Country , subdivision_name1 = Russia , subdivision_type2 = Federal subject , subdivision_name2 = Chukotka Autonomous Okrug , length = , discharge1_avg = , basin_size = The Palyavaam (russian: Паляваам) is a river in the Chukotka Autonomous Okrug, Russian Far East. It is long, and has a drainage basin of . There is a small populated place in ...
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Ridge
A ridge or a mountain ridge is a geographical feature consisting of a chain of mountains or hills that form a continuous elevated crest for an extended distance. The sides of the ridge slope away from the narrow top on either side. The lines along the crest formed by the highest points, with the terrain dropping down on either side, are called the ridgelines. Ridges are usually termed hills or mountains as well, depending on size. Smaller ridges, especially those leaving a larger ridge, are often referred to as spurs. Types There are several main types of ridges: ;Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more joints where the valleys formed or other chance occurrences. This type of ridge is generally somewhat random in orientation, often ...
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Amguema River
The Amguema (russian: Амгуэ́ма, ckt, Оʼмваам, O'mvaam; in its upper course Вульвывее́м, Vulvyveyem Dictionary of names of hydrographic objects of Russia and other countries - members of the CIS
(1999), p. 22
) is a stream located in Far East Siberia. It empties into the between and

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Chantal Range
The Chantal Range (russian: Чантальский хребет) is a range of mountains in far North-eastern Russia. Administratively the range is part of the Chukotka Autonomous Okrug of the Russian Federation. The area of the range is desolate and uninhabited.Wielka Encyklopedia Gór i Alpinizmu, tom 2 Góry Azji, Katowice: Wydawnictwo STAPIS, 2005, . Geography The Chantal Range is located in the central area of the Chukotka Mountains, part of the East Siberian System of ranges. This mountain chain runs in a roughly WSW/ENE direction for about 100 km. It is limited to the west by the bank of the Chantalveergyn River, beyond which rises the Ekiatap Range; to the north it borders with the Palyavaam range, and to the south with the Ekityk Range. The highest point of the range is Iskhodnaya peak, reaching —or according to other sources.ЧУКОТСКОЕ НАГОРЬЕ • Большая российская энциклопедия - электронная версия, big ...
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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ...
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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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Chaun Bay
The Chaunskaya Bay or Chaun Bay (russian: Чаунская губа) is an Arctic bay in the East Siberian Sea, in the Chaunsky District of Chukotka, northeast Siberia. There is Port of Pevek. Geography The bay is open to the north and is 140 km in length. Its maximum width is 110 km.GoogleEarth Its mouth is defined by Cape Shelagsky, the end of the Shelag Range, to the east and an unnamed part of Ayon Island to the west. It narrows where the Pevek Peninsula on the east approaches Ayon Island. Owing to is northerly location Chaunskaya Bay is covered with ice most of the year. This bay is the center of one of the larger lowlands in Chukotka. A number of rivers flow into the southeastern corner: Chaun River, Ichuveyem River, Palyavaam River, Lelyuveyem River and Pucheveyem River. There is a protected natural area in the southeast. Lake Elgygytgyn is about 160 km southeast and the town of Bilibino about 160 km southwest. History The first Russian to re ...
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Points Of The Compass
The points of the compass are a set of horizontal, radially arrayed compass directions (or azimuths) used in navigation and cartography. A compass rose is primarily composed of four cardinal directions—north, east, south, and west—each separated by 90 degrees, and secondarily divided by four ordinal (intercardinal) directions—northeast, southeast, southwest, and northwest—each located halfway between two cardinal directions. Some disciplines such as meteorology and navigation further divide the compass with additional azimuths. Within European tradition, a fully defined compass has 32 'points' (and any finer subdivisions are described in fractions of points). Compass points are valuable in that they allow a user to refer to a specific azimuth in a colloquial fashion, without having to compute or remember degrees. Designations The names of the compass point directions follow these rules: 8-wind compass rose * The four cardinal directions are north (N), east (E), ...
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Anadyr Highlands
The Anadyr Highlands ( rus, Анадырское нагорье, r=Anadyrskoye Nagorye) are a mountainous area in the Chukotka Autonomous Okrug, Far Eastern Federal District, Russia. Geography The Anadyr Highlands are one of the two main mountain regions of Chukotka Autonomous Okrug. They rise southwest of the Chukotka Mountains, in the western Chukotka region. Medium height mountain ranges stretch in roughly WNW/ESE direction west of a large plateau and in a SW/NE direction in the south. The highlands rise between the Chaun Lowlands in the north, the Anadyr Lowlands in the southeast, the Kolyma Mountains in the southwest and the Kolyma Lowlands, where the Kolyma River flows, in the west.Google Earth Among the rivers that have their source in the mountains, the main ones are the Anadyr River flowing off the highland limits to the southeast as the Belaya, the Bolshoy Anyuy and the Maly Anyuy —flowing westwards on both sides of the Anyuy Range. The Enmyvaam flows southwards ou ...
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Chukchi Peninsula
The Chukchi Peninsula (also Chukotka Peninsula or Chukotski Peninsula; russian: Чуко́тский полуо́стров, ''Chukotskiy poluostrov'', short form russian: Чуко́тка, ''Chukotka''), at about 66° N 172° W, is the easternmost peninsula of Asia. Its eastern end is at Cape Dezhnev near the village of Uelen. The Chukotka Mountains are located in the central/western part of the peninsula, which is bounded by the Chukchi Sea to the north, the Bering Sea to the south, and the Bering Strait to the east, where at its easternmost point it is only about from Seward Peninsula in Alaska; this is the smallest distance between the land masses of Eurasia and North America. The peninsula is part of Chukotka Autonomous Okrug of Russia."Chukchi Peninsula"
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Isthmus
An isthmus (; ; ) is a narrow piece of land connecting two larger areas across an expanse of water by which they are otherwise separated. A tombolo is an isthmus that consists of a spit or bar, and a strait is the sea counterpart of an isthmus. Isthmus vs land bridge vs peninsula ''Isthmus'' and ''land bridge'' are related terms, with isthmus having a broader meaning. A land bridge is an isthmus connecting Earth's major landmasses. The term ''land bridge'' is usually used in biogeology to describe land connections that used to exist between continents at various times and were important for migration of people and various species of animals and plants, e.g. Beringia and Doggerland. An isthmus is a land connection between two bigger landmasses, while a peninsula is rather a land protrusion which is connected to a bigger landmass on one side only and surrounded by water on all other sides. Technically, an isthmus can have canals running from coast to coast (e.g. the Panama ...
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Amguema
Amguema (russian: Амгуэма; Chukchi: , ''Oʼmvaam'') is a village ('' selo'') in Iultinsky District of Chukotka Autonomous Okrug, in the Far Eastern Federal District of Russia. Population: the village is based on the Iultin-Egvekinot road, one of the few significant roads in the Okrug. Reindeer herding is the most significant economic activity in the village. Municipally, Amguema is subordinated to Iultinsky Municipal District and incorporated as Amguema Rural Settlement. Demographics The most recent census figures show a population of 531, of which 279 are men and 252 women. The village is a traditional Chukchi settlement, in which most of the citizens are reindeer herders,Strogoff, p.126 taking advantage of the pasture present around the river Amguema ( Chukchi: ). It is the only native settlement in the district to have a stable economy, thanks in part to the available land. The population as of 2006 was 570, up slightly on the 2003 estimate of 548,
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