Tsypnavolok
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Tsypnavolok
Tsypnavolok or Tsyp-Navolok (russian: Цыпнаволок, Цып-Наволок) is a rural locality (an inhabited locality) in Pechengsky District of Murmansk Oblast, Russia, located on the Rybachy Peninsula by Cape Tsypnavolok, by the Barents Sea. History During the 1860s, the Murmansk coast of the Kola Peninsula was actively being settled.Administrative-Territorial Division of Murmansk Oblast, p. 23 In 1867, a fishing village was established near Cape Tsypnavolok by Kola Norwegians (immigrants from Norway). In 1929, 114 ethnic Norwegians were registered in the area, and therefore in 1930 an ethnic Norwegian rural council (selsoviet) was established. In 1940, the Norwegians were transferred during the ethnic cleansing campaigns near the border, and the selsoviet was abolished. After World War II, the Norwegians were allowed to return to Murmansk Oblast, but they were to be settled in Port-Vladimir () on Shalim Island in Kolsky District. (A naval base was later establis ...
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Rybachy Peninsula
Rybachy Peninsula (russian: полуо́стров Рыба́чий, ''poluostrov Rybachiy''; se, Giehkirnjárga; no, Fiskerhalvøya; fi, Kalastajasaarento) is the northernmost part of continental European Russia. Its name is translated as "Fisher Peninsula". It is connected with the Sredny Peninsula, "Middle Peninsula" by a thin isthmus. So the peninsula is in fact nearly completely surrounded by water. Administratively, it is included into Pechengsky District of Murmansk Oblast and is within several hours of ride from Murmansk. Main occupations of the population are reindeer herding and (since 2003) petroleum drilling. History The peninsula lies in an area where borders were marked relatively late; the Norwegian-Russian border was drawn in 1826, leaving Rybachy on the Russian side of the border. At the time, several Norwegian settlers lived on the peninsula. After the Russian Revolution, the western parts of Sredny and Rybachy were ceded to Finland. After the Winter War ...
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Murmansk Oblast
Murmansk Oblast (russian: Му́рманская о́бласть, p=ˈmurmənskəjə ˈobləsʲtʲ, r=Murmanskaya oblast, ''Murmanskaya oblast''; Kildin Sami: Мурман е̄ммьне, ''Murman jemm'ne'') is a federal subject (an oblast) of Russia, located in the northwestern part of the country. Its administrative center is the city of Murmansk. As of the Russian Census (2010), 2010 Census, its population was 795,409. Geography Geographically, Murmansk Oblast is located mainly on the Kola Peninsula almost completely north of the Arctic Circle''2007 Atlas of Murmansk Oblast'', p. 2 and is a part of the larger Lapland (region), Sápmi (Lapland) region that spans over four countries.Ratcliffe, p. 1 The oblast borders with the Republic of Karelia in Russia in the south, Lapland, Finland, Lapland Region in Finland in the west, Troms og Finnmark, Troms and Finnmark County in Norway in the northwest, and is bounded by the Barents Sea in the north and the White Sea in ...
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Weather Station
A weather station is a facility, either on land or sea, with instruments and equipment for measuring atmospheric conditions to provide information for weather forecasts and to study the weather and climate. The measurements taken include temperature, atmospheric pressure, humidity, wind speed, wind direction, and precipitation amounts. Wind measurements are taken with as few other obstructions as possible, while temperature and humidity measurements are kept free from direct solar radiation, or insolation. Manual observations are taken at least once daily, while automated measurements are taken at least once an hour. Weather conditions out at sea are taken by ships and buoys, which measure slightly different meteorological quantities such as sea surface temperature (SST), wave height, and wave period. Drifting weather buoys outnumber their moored versions by a significant amount. Weather instruments Typical weather stations have the following instruments: * Thermometer for ...
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Nodule (geology)
In sedimentology and geology, a nodule is a small, irregularly rounded knot, mass, or lump of a mineral or mineral aggregate that typically has a contrasting composition, such as a pyrite nodule in coal, a chert nodule in limestone, or a phosphorite nodule in marine shale, from the enclosing sediment or sedimentary rock. Normally, a nodule has a warty or knobby surface and exists as a discrete mass within the host strata. In general, they lack any internal structure except for the preserved remnants of original bedding or fossils. Nodules are closely related to concretions and sometimes these terms are used interchangeably. Minerals that typically form nodules include calcite, chert, apatite (phosphorite), anhydrite, and pyrite.Neuendorf, KKE, JP Mehl, Jr., and JA Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Boggs S, Jr. (2009) ''Petrology of Sedimentary Rocks.'' Cambridge University Press, Cambridge, Unite ...
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Sphalerite
Sphalerite (sometimes spelled sphaelerite) is a sulfide mineral with the chemical formula . It is the most important ore of zinc. Sphalerite is found in a variety of deposit types, but it is primarily in Sedimentary exhalative deposits, sedimentary exhalative, Carbonate-hosted lead-zinc ore deposits, Mississippi-Valley type, and Volcanogenic massive sulfide ore deposit, volcanogenic massive sulfide deposits. It is found in association with galena, chalcopyrite, pyrite (and other sulfide mineral, sulfides), calcite, dolomite (mineral), dolomite, quartz, rhodochrosite, and fluorite. German geologist Ernst Friedrich Glocker discovered sphalerite in 1847, naming it based on the Greek word ''sphaleros'', meaning "deceiving", due to the difficulty of identifying the mineral. In addition to zinc, sphalerite is an ore of cadmium, gallium, germanium, and indium. Miners have been known to refer to sphalerite as ''zinc blende'', ''black-jack'', and ''ruby blende''. Marmatite is an opaque ...
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Pyrite
The mineral pyrite (), or iron pyrite, also known as fool's gold, is an iron sulfide with the chemical formula Iron, FeSulfur, S2 (iron (II) disulfide). Pyrite is the most abundant sulfide mineral. Pyrite's metallic Luster (mineralogy), luster and pale brass-yellow hue give it a superficial resemblance to gold, hence the well-known nickname of ''fool's gold''. The color has also led to the nicknames ''brass'', ''brazzle'', and ''Brazil'', primarily used to refer to pyrite found in coal. The name ''pyrite'' is derived from the Greek language, Greek (), 'stone or mineral which strikes fire', in turn from (), 'fire'. In ancient Roman times, this name was applied to several types of stone that would create sparks when struck against steel; Pliny the Elder described one of them as being brassy, almost certainly a reference to what we now call pyrite. By Georgius Agricola's time, , the term had become a generic term for all of the pyrite group, sulfide minerals. Pyrite is usua ...
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Galena
Galena, also called lead glance, is the natural mineral form of lead(II) sulfide (PbS). It is the most important ore of lead and an important source of silver. Galena is one of the most abundant and widely distributed sulfide minerals. It crystallizes in the cubic crystal system often showing octahedral forms. It is often associated with the minerals sphalerite, calcite and fluorite. Occurrence Galena is the main ore of lead, used since ancient times, since lead can be smelted from galena in an ordinary wood fire. Galena typically is found in hydrothermal veins in association with sphalerite, marcasite, chalcopyrite, cerussite, anglesite, dolomite, calcite, quartz, barite, and fluorite. It is also found in association with sphalerite in low-temperature lead-zinc deposits within limestone beds. Minor amounts are found in contact metamorphic zones, in pegmatites, and disseminated in sedimentary rock. In some deposits the galena contains up to 0.5% silver, a byproduct that ...
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Chalcopyrite
Chalcopyrite ( ) is a copper iron sulfide mineral and the most abundant copper ore mineral. It has the chemical formula CuFeS2 and crystallizes in the tetragonal system. It has a brassy to golden yellow color and a hardness of 3.5 to 4 on the Mohs scale. Its streak is diagnostic as green-tinged black. On exposure to air, chalcopyrite tarnishes to a variety of oxides, hydroxides, and sulfates. Associated copper minerals include the sulfides bornite (Cu5FeS4), chalcocite (Cu2S), covellite (CuS), digenite (Cu9S5); carbonates such as malachite and azurite, and rarely oxides such as cuprite (Cu2O). Is rarely found in association with native copper. Chalcopyrite is a conductor of electricity. Etymology The name chalcopyrite comes from the Greek words , which means copper, and ', which means striking fire. It was sometimes historically referred to as "yellow copper". Identification Chalcopyrite is often confused with pyrite and gold since all three of these minerals have a yell ...
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Sulfide
Sulfide (British English also sulphide) is an inorganic anion of sulfur with the chemical formula S2− or a compound containing one or more S2− ions. Solutions of sulfide salts are corrosive. ''Sulfide'' also refers to chemical compounds large families of inorganic and organic compounds, e.g. lead sulfide and dimethyl sulfide. Hydrogen sulfide (H2S) and bisulfide (SH−) are the conjugate acids of sulfide. Chemical properties The sulfide ion, S2−, does not exist in aqueous alkaline solutions of Na2S. Instead sulfide converts to hydrosulfide: :S2− + H2O → SH− + OH− Upon treatment with an acid, sulfide salts convert to hydrogen sulfide: :S2− + H+ → SH− :SH− + H+ → H2S Oxidation of sulfide is a complicated process. Depending on the conditions, the oxidation can produce elemental sulfur, polysulfides, polythionates, sulfite, or sulfate. Metal sulfides react with halogens, forming sulfur and metal salts. :8 MgS + 8 I2 → S8 + 8 M ...
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Lighthouse
A lighthouse is a tower, building, or other type of physical structure designed to emit light from a system of lamps and lenses and to serve as a beacon for navigational aid, for maritime pilots at sea or on inland waterways. Lighthouses mark dangerous coastlines, hazardous shoals, reefs, rocks, and safe entries to harbors; they also assist in aerial navigation. Once widely used, the number of operational lighthouses has declined due to the expense of maintenance and has become uneconomical since the advent of much cheaper, more sophisticated and effective electronic navigational systems. History Ancient lighthouses Before the development of clearly defined ports, mariners were guided by fires built on hilltops. Since elevating the fire would improve the visibility, placing the fire on a platform became a practice that led to the development of the lighthouse. In antiquity, the lighthouse functioned more as an entrance marker to ports than as a warning signal for reefs a ...
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Shalim Island
Shalim (Šalām, Shalem, Salem, and Salim) is a god in Canaanite religion, mentioned in inscriptions found in Ugarit (Ras Shamra) in Syria.Golan, 2003, p. 82. "The name of the Canaanite deity of the setting sun Salim, or Salem, ..The names Shahar_(god).html" ;"title="f Shahar (god)">Sahar and Salimare rendered in modern scholarly texts as Shakhar and Shalim [...]" William F. Albright identified Shalim as the god of dusk and Shahar as god of the dawn.Albright, 199p. 187 cf. the Akkadian word for sunset, ''šalām šamši''. In the ''Dictionary of Deities and Demons in the Bible'', Shalim is also identified as the deity representing Venus or the "Evening Star" and Shahar the "Morning Star". His name derives from the triconsonantal Semitic root Š-L-M. Ugaritic inscriptions An Ugaritic myth known as ''The Gracious and Most Beautiful Gods'', describes Shalim and his brother Shahar as offspring of El through two women he meets at the seashore. They are both nursed by "The Lady" ...
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Kolsky District
Kolsky District (russian: Ко́льский райо́н) is an administrative district (raion), one of the six in Murmansk Oblast, Russia.Law #96-01-ZMO As a municipal division, it is incorporated as Kolsky Municipal District.Law #577-01-ZMO It is located in the northwest of the oblast, partially lies on the Kola Peninsula, and borders with the Barents Sea in the north and Finland in the west.Official website of Kolsky DistrictInformation About the District The area of the district is . Its administrative center is the town of Kola. Population: The population of Kola accounts for 23.4% of the district's total population. Geography Kolsky District is bordered on the west by Pechengsky District, on the southwest by Finland, and on the north by the Barents Sea. The terrain is mostly flat forest (taiga) and rocky tundra. The district mostly covers the Tuloma River and the Kola River, which flow north into Kola Bay and the Barents Sea. The Tuloma River flows out of Lake Notozer ...
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