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Bilibino District
Bilibinsky District (russian: Били́бинский райо́н; , ''Bilibinkèn rajon'') is an administrativeLaw #33-OZ and municipalLaw #43-OZ district (raion), one of the six in Chukotka Autonomous Okrug, Russia. It is located in the west of the autonomous okrug and borders with Chaunsky District in the northeast, Anadyrsky District in the east, Koryak Okrug of Kamchatka Krai in the southeast, Magadan Oblast in the southwest, and the Sakha Republic in the west. The area of the district is .Official website of Bilibinsky DistrictGeneral information Its administrative center is the town of Bilibino. Population: The population of Bilibino accounts for 74.8% of the district's total population. Archeological finds indicate that the territory of what is now Bilibinsky District was first inhabited in the early Neolithic. Following the establishment of Anadyrsk by Semyon Dezhnyov in the 17th century, the Bolshoy Anyuy River, which flows through the modern district, was an importa ...
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Maly Anyuy River
The Maly Anyuy (russian: Ма́лый Аню́й; ''maly'' meaning "little") is a river in the Kolyma basin in the Russian Far East. Most of the basin of the Maly Anyuy and its tributaries belongs to the Chukotka Autonomous Okrug administrative region of Russia. Geography The Maly Anyuy flows roughly westwards, south and west of the Ilirney Range, making a wide bend by the Chuvanay Range —flowing first northwards and then westwards again at the feet of the Kyrganay Range— in western Chukotka Autonomous Okrug. Just after crossing into the Sakha Republic, it meets the Bolshoy Anyuy, merging with it into a single channel ( Anyuy proper) before meeting the Kolyma close to its delta. Its length is and its basin surface . The El'gygytgyn Meteorite Crater is about from its source. The most important inhabited localities in the Maly Anyuy valley are Aliskerovo and Bilibino, on the shores of smaller tributaries. Fauna Among the fish found in the Maly Anyuy are different specie ...
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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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Ilirney Range
The Ilirney Range (russian: Илирнейский кряж) is a range of mountains in Chukotka Autonomous Okrug, Russian Far East. Administratively the range is part of Bilibino District. The village of Ilirney is located southwest of the central area of the range. Bilibino is located to the west of the western end.Google Earth Geography The highest point of the Ilirney Range is high mount Dvukh Tsirkov (гора Двух Цирков, meaning "Two Circuses"). Other high peaks of the range are high mount Sypuchiy Kamen (Сыпучий Камень) and high mount Radialnaya (радиальная). To the southeast of the mountain range rises the Anyuy Range, to the west it borders with the Kyrganay and Chuvanay ranges, to the north with the Rauchuan Range and to the east with the Anadyr Plateau. The Ilirney Range is part of the East Siberian System of mountains and is one of the subranges of the Anadyr Highlands. Two beautiful lakes are located below the southern slopes ...
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Chuvan Mountains
The Chuvanay Range (russian: Чуванайские Горы), also known as Chuvan Mountains (Чуванский хребет), is a range of mountains in Chukotka Autonomous Okrug, Russian Far East. Administratively the range is part of Bilibino District. The village of Keperveyem is located at the feet of the range in its northwestern end, on the other side of the Maly Anyuy River. Bilibino is located about further to the north.Google Earth Geography The highest point of the Chuvanay Range is high mount Chuvanay (гора Чуванаи). To the east and northeast the mountain range is limited by the course of the Maly Anyuy River, which makes a wide bend, flowing first northwards and then again westwards. To the south the range is bound by the Kulpolney River and to the west by the valley of the Tenvelveyem —left hand tributaries of the Maly Anyuy. A few other tributaries of the Maly Anyuy have their source in the range, flowing between both and joining the left bank of t ...
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Kyrganay Range
The Kyrganay Range (russian: хребет Кырганай or хребет Кыргонай) is a range of mountains in Chukotka Autonomous Okrug, Russian Far East. Administratively the range is part of Bilibino District. The village of Keperveyem is located at the feet of the range in its western end. Bilibino is located about further to the north. Google Earth Geography The Kyrganay Range rises above the northern bank of the Maly Anyuy River. To the east the mountain range is limited by the Egilknyveyem River and to the west by the valley of the Maly Keperveyem River, both right hand tributaries of the Maly Anyuy River. To the south, on the other side of the Maly Anyuy, rises the Chuvanay Range. The ghost town of Aliskerovo, beyond which rises the Ilirney Range, lies at the eastern end of the Kyrganay Mountains. The highest point of the Kyrganay Range is an unnamed high summit. The Kyrganay Range is part of the East Siberian System of mountains and is one of the subranges ...
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Kolyma Highlands
Kolyma (russian: Колыма́, ) is a region located in the Russian Far East. It is bounded to the north by the East Siberian Sea and the Arctic Ocean, and by the Sea of Okhotsk to the south. The region gets its name from the Kolyma River and mountain system, parts of which were not accurately mapped by Russian surveyors until 1926. Today the region consists roughly of the Chukotka Autonomous Okrug and the Magadan Oblast. The area, part of which is within the Arctic Circle, has a subarctic climate with very cold winters lasting up to six months of the year. Permafrost and tundra cover a large part of the region. Average winter temperatures range from (even lower in the interior), and average summer temperatures, from . There are rich reserves of gold, silver, tin, tungsten, mercury, copper, antimony, coal, oil, and peat. Twenty-nine zones of possible oil and gas accumulation have been identified in the Sea of Okhotsk shelf. Total reserves are estimated at 3.5 billion tons of ...
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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

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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East Siberian Sea
The East Siberian Sea ( rus, Восто́чно-Сиби́рское мо́ре, r=Vostochno-Sibirskoye more) is a marginal sea in the Arctic Ocean. It is located between the Arctic Cape to the north, the coast of Siberia to the south, the New Siberian Islands to the west and Cape Billings, close to Chukotka, and Wrangel Island to the east. This sea borders on the Laptev Sea to the west and the Chukchi Sea to the east. This sea is one of the least studied in the Arctic area. It is characterized by severe climate, low water salinity, and a scarcity of flora, fauna and human population, as well as shallow depths (mostly less than 50 m), slow sea currents, low tides (below 25 cm), frequent fogs, especially in summer, and an abundance of ice fields which fully melt only in August–September. The sea shores were inhabited for thousands of years by indigenous tribes of Yukaghirs, Chukchi and then Evens and Evenks, which were engaged in fishing, hunting and reindeer husbandry. ...
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Gold
Gold is a chemical element with the symbol Au (from la, aurum) and atomic number 79. This makes it one of the higher atomic number elements that occur naturally. It is a bright, slightly orange-yellow, dense, soft, malleable, and ductile metal in a pure form. Chemically, gold is a transition metal and a group 11 element. It is one of the least reactive chemical elements and is solid under standard conditions. Gold often occurs in free elemental ( native state), as nuggets or grains, in rocks, veins, and alluvial deposits. It occurs in a solid solution series with the native element silver (as electrum), naturally alloyed with other metals like copper and palladium, and mineral inclusions such as within pyrite. Less commonly, it occurs in minerals as gold compounds, often with tellurium (gold tellurides). Gold is resistant to most acids, though it does dissolve in aqua regia (a mixture of nitric acid and hydrochloric acid), forming a soluble tetrachloroaurate anion. Gold is ...
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