Bieberite
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Bieberite
Bieberite (CoSO4 · 7H2O) is a pinkish red colored sulfate mineral high in cobalt content. The name is derived from the type locality at the copper deposit in Bieber, Hesse, Germany. It has been described and reported as far back as the 1700s.Sage (1791) ''Le Journal de physique et le radium, Paris'', 39: 53 (as Cobalt Vitriol).Klaproth, M.H. (1797) "''Untersuchung des natürlichen Kobaltvitriols von Herrengrund, Beiträge zur chemischen Kenntniss der Mineralkörper"'', Zweiter Band, Rottmann Berlin, pp. 320.Kopp (1808) ''Allgemeines Journal der Chemie, Berlin 1798-1803 (Scherer’s Journal)'', 6: 157 (as Kobaltvitriol).Beudant, F.S. (1832) ''Trailé élémentaire de Minéralogie, second edition, 2 volumes'', 2: 481 (as Red Vitrol. Sulphate of Cobalt. Rhodhalose).Haidinger (1845) 489 (as Bieberit).Winkelblech (1845) ''Ann. Chem.'', 13: 265.Marignac (1855) ''Mém. soc. phys. nat. Genève'', 14: 245 (artificial material).Goldschmidt, V. (1913) ''Atlas der Krystallformen. 9 volumes, at ...
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Sulfate Mineral
The sulfate minerals are a class of minerals that include the sulfate ion () within their structure. The sulfate minerals occur commonly in primary evaporite depositional environments, as gangue minerals in hydrothermal veins and as secondary minerals in the oxidizing zone of sulfide mineral deposits. The chromate and manganate minerals have a similar structure and are often included with the sulfates in mineral classification systems.Klein, Cornelis and Cornelius S. Hurlbut, 1985, ''Manual of Mineralogy,'' 20th ed., John Wiley and Sons, New York, pp. 347–354 . Sulfate minerals include: *Anhydrous sulfates **Barite BaSO4 ** Celestite SrSO4 **Anglesite PbSO4 **Anhydrite CaSO4 **Hanksite Na22K(SO4)9(CO3)2Cl *Hydroxide and hydrous sulfates **Gypsum CaSO4·2H2O **Chalcanthite CuSO4·5H2O **Kieserite MgSO4·H2O ** Starkeyite MgSO4·4H2O **Hexahydrite MgSO4·6H2O **Epsomite MgSO4·7H2O **Meridianiite MgSO4·11H2O **Melanterite FeSO4·7H2O **Antlerite Cu3SO4(OH)4 **Brochantite Cu4SO4 ...
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Sulfate Mineral
The sulfate minerals are a class of minerals that include the sulfate ion () within their structure. The sulfate minerals occur commonly in primary evaporite depositional environments, as gangue minerals in hydrothermal veins and as secondary minerals in the oxidizing zone of sulfide mineral deposits. The chromate and manganate minerals have a similar structure and are often included with the sulfates in mineral classification systems.Klein, Cornelis and Cornelius S. Hurlbut, 1985, ''Manual of Mineralogy,'' 20th ed., John Wiley and Sons, New York, pp. 347–354 . Sulfate minerals include: *Anhydrous sulfates **Barite BaSO4 ** Celestite SrSO4 **Anglesite PbSO4 **Anhydrite CaSO4 **Hanksite Na22K(SO4)9(CO3)2Cl *Hydroxide and hydrous sulfates **Gypsum CaSO4·2H2O **Chalcanthite CuSO4·5H2O **Kieserite MgSO4·H2O ** Starkeyite MgSO4·4H2O **Hexahydrite MgSO4·6H2O **Epsomite MgSO4·7H2O **Meridianiite MgSO4·11H2O **Melanterite FeSO4·7H2O **Antlerite Cu3SO4(OH)4 **Brochantite Cu4SO4 ...
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Greece
Greece,, or , romanized: ', officially the Hellenic Republic, is a country in Southeast Europe. It is situated on the southern tip of the Balkans, and is located at the crossroads of Europe, Asia, and Africa. Greece shares land borders with Albania to the northwest, North Macedonia and Bulgaria to the north, and Turkey to the northeast. The Aegean Sea lies to the east of the Geography of Greece, mainland, the Ionian Sea to the west, and the Sea of Crete and the Mediterranean Sea to the south. Greece has the longest coastline on the Mediterranean Basin, featuring List of islands of Greece, thousands of islands. The country consists of nine Geographic regions of Greece, traditional geographic regions, and has a population of approximately 10.4 million. Athens is the nation's capital and List of cities and towns in Greece, largest city, followed by Thessaloniki and Patras. Greece is considered the cradle of Western culture, Western civilization, being the birthplace of Athenian ...
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Irazú Volcano
The Irazú Volcano ( es, Volcán Irazú) is an active volcano in Costa Rica, situated in the Cordillera Central close to the city of Cartago. The name could come from either the combination of "ara" (point) and "tzu" (thunder) or a corruption of ''Iztarú'', which was the name of an indigenous village on the flanks of the volcano. In Costa Rica it is known by the name of "El Coloso" (The Colossus) due to the catastrophes that it has provoked in the past. The volcano's summit has several craters, one of which contains Diego de la Haya, a green crater lake of variable depth. At 11,260 feet (3,432 m), the Irazú Volcano is the highest active volcano in Costa Rica. It is easily visited from San José, with a road leading right up to the summit craters and a weekly bus service to the top. It is thus a popular tourist spot. The summit of the volcano also houses a few television transmitters for television stations in San José. From the top it is possible to see both the Atl ...
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Phillack
Phillack ( kw, Eglosheyl) is a village (and formerly a parish) in west Cornwall, England, United Kingdom. It is about one mile (1.6 km) northeast of Hayle and half-a-mile (0.8 km) inland from St Ives Bay on Cornwall's Atlantic ocean coast.Ordnance Survey: Landranger map sheet 203 ''Land's End'' The village is separated from the sea by a range of high sand dunes known as The Towans. Phillack has been in the civil parish of Hayle since 1935; before that it was a separate parish in its own right.
GENUKI website; Phillack. Retrieved June 2010
Phillack parish was originally in Redruth Registration District but the village now comes under Camborne-Redruth Registration District. There is some dispute over the origins of the name. In the 17th century, ''Phillack'' was believed to refer to the Irish Saint Felicitas who is said to have fo ...
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Cornwall
Cornwall (; kw, Kernow ) is a historic county and ceremonial county in South West England. It is recognised as one of the Celtic nations, and is the homeland of the Cornish people. Cornwall is bordered to the north and west by the Atlantic Ocean, to the south by the English Channel, and to the east by the county of Devon, with the River Tamar forming the border between them. Cornwall forms the westernmost part of the South West Peninsula of the island of Great Britain. The southwesternmost point is Land's End and the southernmost Lizard Point. Cornwall has a population of and an area of . The county has been administered since 2009 by the unitary authority, Cornwall Council. The ceremonial county of Cornwall also includes the Isles of Scilly, which are administered separately. The administrative centre of Cornwall is Truro, its only city. Cornwall was formerly a Brythonic kingdom and subsequently a royal duchy. It is the cultural and ethnic origin of the Cornish dias ...
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St Hilary, Cornwall
St Hilary is a civil parish and village in west Cornwall, England, United Kingdom. It is situated approximately five miles (8 km) east of Penzance and four miles (6.5 km) south of Hayle. Chynoweth is an area immediately north of St Hilary churchtown. The land of the parish is high enough to provide views of bays on both coasts, St Ives Bay five miles north and Mount's Bay two miles south.Mee, Arthur (1937) ''Cornwall''. (The King's England.) London: Hodder & Stoughton; p. 221 For the purposes of local government St Hilary has a parish council and elects councillors every four years. The principal local authority in the area is Cornwall Council. During the height of mining activity the population was three times that in the 1930s. Geology The area has many former mines: especially notable was a mine called Wheal Fortune which extended into the parish of Ludgvan. Penberthy Croft Mine, to the north of the parish, was designated a Site of Special Scientific Interest in 19 ...
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Wheal Alfred
Wheal Alfred is the site of a former copper and lead mine and a designated Site of Special Scientific Interest (SSSI) in west Cornwall, England, UK. The mine is located east of the town of HayleOrdnance Survey: Landranger map sheet 203 ''Land's End'' and is also a Geological Conservation Review site. The mine is famous to geologists for its important mineral specimens such as mimetite and pyromorphite Pyromorphite is a mineral species composed of lead chlorophosphate: Pb5( P O4)3 Cl, sometimes occurring in sufficient abundance to be mined as an ore of lead. Crystals are common, and have the form of a hexagonal prism terminated by the basal pla .... References Copper mines in Cornwall Sites of Special Scientific Interest in Cornwall Sites of Special Scientific Interest notified in 1990 Industrial archaeological sites in Cornwall {{Penwith-geo-stub ...
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Penberthy Croft Mine
Penberthy Croft Mine, is a disused mine and Site of Special Scientific Interest (SSSI) in Cornwall, England, UK. It is located to the north of the civil parish of St Hilary, east of the town of Penzance. The mine was designated a SSSI in 1993, is listed as of national importance in the Geological Conservation Review and is the world type locality for connellite and bayldonite. It is noted as the most important site in Britain for secondary ore minerals of lead, copper, and arsenic Arsenic is a chemical element with the symbol As and atomic number 33. Arsenic occurs in many minerals, usually in combination with sulfur and metals, but also as a pure elemental crystal. Arsenic is a metalloid. It has various allotropes, but ... and has had 40 mineral species recorded at the site. History A new 36-inch cylinder pumping engine was built in 1880, by Messrs George Eustice and Cooper which drained between nine and ten fathoms of water in the first four hours of work. Referenc ...
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United Kingdom
The United Kingdom of Great Britain and Northern Ireland, commonly known as the United Kingdom (UK) or Britain, is a country in Europe, off the north-western coast of the continental mainland. It comprises England, Scotland, Wales and Northern Ireland. The United Kingdom includes the island of Great Britain, the north-eastern part of the island of Ireland, and many smaller islands within the British Isles. Northern Ireland shares a land border with the Republic of Ireland; otherwise, the United Kingdom is surrounded by the Atlantic Ocean, the North Sea, the English Channel, the Celtic Sea and the Irish Sea. The total area of the United Kingdom is , with an estimated 2020 population of more than 67 million people. The United Kingdom has evolved from a series of annexations, unions and separations of constituent countries over several hundred years. The Treaty of Union between the Kingdom of England (which included Wales, annexed in 1542) and the Kingdom of Scotland in 170 ...
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England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ...
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Supergene (geology)
In ore deposit geology, supergene processes or enrichment are those that occur relatively near the surface as opposed to deep hypogene processes. Supergene processes include the predominance of meteoric water circulation (i.e. water derived from precipitation) with concomitant oxidation and chemical weathering. The descending meteoric waters oxidize the primary (hypogene) sulfide ore minerals and redistribute the metallic ore elements. Supergene ''enrichment'' occurs at the base of the oxidized portion of an ore deposit. Metals that have been leached from the oxidized ore are carried downward by percolating groundwater, and react with hypogene sulfides at the supergene-hypogene boundary. The reaction produces secondary sulfides with metal contents higher than those of the primary ore. This is particularly noted in copper ore deposits where the copper sulfide minerals chalcocite (Cu2S), covellite (CuS), digenite (Cu18S10), and djurleite (Cu31S16) are deposited by the descending surfa ...
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