Sable Tin Deposit (Sobolinoye)
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Sable Tin Deposit (Sobolinoye)
The Sable Tin Deposit also known as "Sobolinoye" (Rus: Соболиное) is a high grade tin-copper deposit located in the Solnechny District of Khabarovsk Krai in the Russian Far East. Discovered in 1964 on the basis of 1:5000 – 1:10000 mapping which identified the presence of commercial concentrations of tin at surface. It is located within the Komsomolsk Ore (Tin) District, a major tin region within Russia with both historical and current mining activities. The deposit's resources were registered in 1987 and Technical Economic Conditions for design and construction were prepared by Gipronickel, a Norilsk subsidiary in 1993 but due to economic and political turbulence the deposit was never developed or exploited Location It is located 15 km directly north of Gorniy village and 35 km by unpaved road from the Pridorozhnoe intersection 12 km from Solnechny Town and 50 km: Industrialized city of Komsomolsk on Amur. Coordinates: 50°56'30 N and 136°28'30 ...
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Solnechny District
Solnechny District (russian: Со́лнечный райо́н) is an administrativeResolution #143-pr and municipalLaw #194 district (raion), one of the seventeen in Khabarovsk Krai, Russia. It is located in the center of the krai. The area of the district is . Its administrative center An administrative center is a seat of regional administration or local government, or a county town, or the place where the central administration of a commune A commune is an alternative term for an intentional community. Commune or comună or ... is the urban locality (a work settlement) of Solnechny. Population: The population of the administrative center accounts for 39.5% of the district's total population. Tin mining The district owes its origins to tin exploration and mining and the subsequent Solnechny Processing ComplexSolnechny GOK Academia Ru: http://dic.academic.ru/dic.nsf/enc_geolog/4759/%D0%A1%D0%BE%D0%BB%D0%BD%D0%B5%D1%87%D0%BD%D1%8B%D0%B9 which sourced its ore from Solnech ...
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Khabarovsk Krai
Khabarovsk Krai ( rus, Хабаровский край, r=Khabarovsky kray, p=xɐˈbarəfskʲɪj kraj) is a federal subject (a krai) of Russia. It is geographically located in the Russian Far East and is a part of the Far Eastern Federal District. The administrative centre of the krai is the city of Khabarovsk, which is home to roughly half of the krai's population and the largest city in the Russian Far East (just ahead of Vladivostok). Khabarovsk Krai is the fourth-largest federal subject by area, and has a population of 1,343,869 as of 2010. The southern region lies mostly in the basin of the lower Amur River, with the mouth of the river located at Nikolaevsk-on-Amur draining into the Strait of Tartary, which separates Khabarovsk Krai from the island of Sakhalin. The north occupies a vast mountainous area along the coastline of the Sea of Okhotsk, a marginal sea of the Pacific Ocean. Khabarovsk Krai is bordered by Magadan Oblast to the north, Amur Oblast, Jewish Au ...
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Solnechny (inhabited Locality)
Solnechny (russian: Со́лнечный; masculine), Solnechnaya (; feminine), or Solnechnoye (; neuter) is the name of several inhabited localities in Russia: Altai Krai As of 2010, two rural localities in Altai Krai bear this name: * Solnechny, Altai Krai, a settlement in Zavetilyichevsky Selsoviet of Aleysky District * Solnechnoye, Altai Krai, a '' selo'' in Solnechny Selsoviet of Pervomaysky District Amur Oblast As of 2010, two rural localities in Amur Oblast bear this name: * Solnechny, Amur Oblast, a settlement in Solnechny Rural Settlement of Skovorodinsky District * Solnechnoye, Amur Oblast, a '' selo'' in Priozerny Rural Settlement of Ivanovsky District Astrakhan Oblast As of 2010, one rural locality in Astrakhan Oblast bears this name: * Solnechny, Astrakhan Oblast, a settlement in Zabuzansky Selsoviet of Krasnoyarsky District Chelyabinsk Oblast As of 2010, one rural locality in Chelyabinsk Oblast bears this name: * Solnechny, Chelyabinsk Oblast, a settlement in Sol ...
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Komsomolsk-on-Amur
Komsomolsk-on-Amur ( rus, Комсомольск-на-Амуре, r=Komsomolsk-na-Amure, p=kəmsɐˈmolʲsk nɐɐˈmurʲə) is a types of inhabited localities in Russia, city in Khabarovsk Krai, Russia, located on the west bank of the Amur River in the Russian Far East. It is located on the Baikal-Amur Mainline, northeast of Khabarovsk. Population: Geography The city and its suburbs stretch for over along the left bank of the Amur River. The river at this point is up to wide. Lake Khummi is located southeast of the city.Google Earth The distance to Khabarovsk—the administrative center of the krai—is ; to the Pacific Ocean—about . The nearest other major town is Amursk, about south. It is about east of Moscow, and lies at the eastern end of the Baikal-Amur Mainline, BAM Railway. History The future site of Komsomolsk-on-Amur was conquered by the Mongols in the 13th century, becoming part of the Mongol Empire under the Mongol Yuan Dynasty. It was later held by the ...
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Badzhal Range
The Badzhal Range (russian: Баджальский хребет, ''Badzhalskiy Khrebet'') is a mountain range in Khabarovsk Krai, Russian Far East.Хабаровский край. Путеводитель. — Приамурские ведомости. 2003. ISBN 5-8003-0093-3 The mountains are mainly composed of volcanic rock, sandstone and shale, as well as chalk, and andesite-basalt, with granites, porphyry and gabbro-granodiorite intrusions. Geography The Badzhal Range consists of a system of separate ridges of moderate alpine relief with a total length of about .Баджальский хребет
: (in 30 vols.) - Ch. ed.
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Gorin (river)
The Gorin (russian: Горин), also known as "Goryun" and "Garin", is a river in Khabarovsk Krai, Russia. It is the 8th longest tributary of the Amur, with a length of and a drainage basin area of . It flows across the Solnechny and Komsomolsky districts. Over 80% of the river basin is covered by forests. The Komsomolsk Nature Reserve, a protected area, is in its lower course, in the area of its confluence with the Amur. Course The Gorin is a left tributary of the Amur. It has its sources in the northwestern slope of the Dayana Range, part of the Badzhal mountain system, about to the west of Komsomolsk-on-Amur. In its upper course the river flows roughly in an ENE direction within a narrow valley and towards its middle reaches the valley expands to a width between and . The lower course is very swampy and the river forms wide meanders. Finally it meets the Amur from its mouth. Google Earth The main tributaries of the Gorin are the long Khurmuli on the right, and ...
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Volcano
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ...
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Copper Mines In Russia
Copper is a chemical element with the symbol Cu (from la, cuprum) and atomic number 29. It is a soft, malleable, and ductile metal with very high thermal and electrical conductivity. A freshly exposed surface of pure copper has a pinkish-orange color. Copper is used as a conductor of heat and electricity, as a building material, and as a constituent of various metal alloys, such as sterling silver used in jewelry, cupronickel used to make marine hardware and coins, and constantan used in strain gauges and thermocouples for temperature measurement. Copper is one of the few metals that can occur in nature in a directly usable metallic form (native metals). This led to very early human use in several regions, from circa 8000 BC. Thousands of years later, it was the first metal to be smelted from sulfide ores, circa 5000 BC; the first metal to be cast into a shape in a mold, c. 4000 BC; and the first metal to be purposely alloyed with another metal, tin, to create bronze, c. 350 ...
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