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Locality (geology)
Type locality, also called type area, is the locality where a particular rock type, stratigraphic unit or mineral species is first identified. If the stratigraphic unit in a locality is layered, it is called a stratotype, whereas the standard of reference for unlayered rocks is the type locality. The term is similar to the term type site in archaeology or the term type specimen in biology. Examples of geological type localities Rocks and minerals * Aragonite: Molina de Aragón, Guadalajara, Spain * Autunite: Autun, France * Benmoreite: Ben More (Mull), Scotland * Blairmorite: Blairmore, Alberta, Canada * Boninite: Bonin Islands, Japan * Comendite: Comende, San Pietro Island, Sardinia * Cummingtonite: Cummington, Massachusetts * Dunite: Dun Mountain, New Zealand. * Essexite: Essex County, Massachusetts, US * Fayalite: Horta, Fayal Island, Azores, Portugal * Harzburgite: Bad Harzburg, Germany * Icelandite: Thingmuli (Þingmúli), Iceland * Ijolite: Iivaara, Kuusamo, Finla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Locality
Locality may refer to: * Locality (association), an association of community regeneration organizations in England * Locality (linguistics) * Locality (settlement) * Suburbs and localities (Australia), in which a locality is a geographic subdivision in rural areas of Australia Science * Locality (astronomy) * Locality of reference, in computer science * Locality (statistics) * Principle of locality, in physics See also * Local (other) * Type locality (other) {{disambiguation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
France
France (), officially the French Republic ( ), is a country primarily located in Western Europe. It also comprises of Overseas France, overseas regions and territories in the Americas and the Atlantic Ocean, Atlantic, Pacific Ocean, Pacific and Indian Oceans. Its Metropolitan France, metropolitan area extends from the Rhine to the Atlantic Ocean and from the Mediterranean Sea to the English Channel and the North Sea; overseas territories include French Guiana in South America, Saint Pierre and Miquelon in the North Atlantic, the French West Indies, and many islands in Oceania and the Indian Ocean. Due to its several coastal territories, France has the largest exclusive economic zone in the world. France borders Belgium, Luxembourg, Germany, Switzerland, Monaco, Italy, Andorra, and Spain in continental Europe, as well as the Kingdom of the Netherlands, Netherlands, Suriname, and Brazil in the Americas via its overseas territories in French Guiana and Saint Martin (island), ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dun Mountain
Dun Mountain is a mountain in the Richmond Range near the city of Nelson in the Tasman District of New Zealand's South Island. It is located between the catchments of the Pelorus, Maitai and Roding Rivers. The mountain is named for its brown (Dun) colour. The colour is caused by the ultramafic rock which forms the mountain. Ultramafic Rock weathers to this colour and plant growth is also stunted due to the soils high heavy metal content. The ultramafic rock formed in the earth's mantle in the Permian and is now part of the Dun Mountain Ophiolite Belt. In 1859 the rock type dunite was first identified on the mountain and named after it. Between 1850 and 1865 small deposits of chromite and copper 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 pinkis ... were mined on the mountain leadi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dunite
Dunite (), also known as olivinite (not to be confused with the mineral olivenite), is an intrusive igneous rock of ultramafic composition and with phaneritic (coarse-grained) texture. The mineral assemblage is greater than 90% olivine, with minor amounts of other minerals such as pyroxene, chromite, magnetite, and pyrope. Dunite is the olivine-rich endmember of the peridotite group of mantle-derived rocks. Dunite and other peridotite rocks are considered the major constituents of the Earth's mantle above a depth of about . Dunite is rarely found within continental rocks, but where it is found, it typically occurs at the base of ophiolite sequences where slabs of mantle rock from a subduction zone have been thrust onto continental crust by obduction during continental or island arc collisions (orogeny). It is also found in alpine peridotite massifs that represent slivers of sub-continental mantle exposed during collisional orogeny. Dunite typically undergoes retrograde metamorp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cummington, Massachusetts
Cummington is a town in Hampshire County, Massachusetts, United States. The population was 829 at the 2020 census, down from 872 at the 2010 census. It is part of the Springfield, Massachusetts Metropolitan Statistical Area. History Cummington was first settled in 1762 and was officially incorporated in 1779. It was named after Colonel John Cumings, the original landholder. The first Congregational Church minister was Rev. James Briggs (1743–1825) of Norton, Massachusetts, and a graduate of Yale College around 1775. Briggs was the son of Deacon James and Damaris (White) Briggs, and the husband of Anna Wiswall. Although a small town, several Revolutionary War patriots are buried there, including Nathaniel Holbrook, Seth Wilder Sr., and Seth Wilder Jr. Noted poet and newspaper editor William Cullen Bryant was born in Cummington, and returned for many years to summer in the town. His house is now preserved and open to the public as the William Cullen Bryant Homestead. The to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cummingtonite
Cummingtonite ( ) is a metamorphic amphibole with the chemical composition , magnesium iron silicate hydroxide. Monoclinic cummingtonite is compositionally similar and polymorphic with orthorhombic anthophyllite, which is a much more common form of magnesium-rich amphibole, the latter being metastable. Cummingtonite shares few compositional similarities with alkali amphiboles such as arfvedsonite, glaucophane-riebeckite. There is little solubility between these minerals due to different crystal habit and inability of substitution between alkali elements and ferro-magnesian elements within the amphibole structure. Name and discovery Cummingtonite was named after the town of Cummington, Massachusetts, where it was discovered in 1824.Chester Dewey, "A Sketch of the Geology and Mineralogy of the Western Part of Massachusetts, and a Small Part of Adjoining States", in ''American Journal of Science'', first series, vol. 8, part 2, 1824, p. 1-60 It is also found in Sweden, South Afr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sardinia
Sardinia ( ; it, Sardegna, label=Italian, Corsican and Tabarchino ; sc, Sardigna , sdc, Sardhigna; french: Sardaigne; sdn, Saldigna; ca, Sardenya, label=Algherese and Catalan) is the second-largest island in the Mediterranean Sea, after Sicily, and one of the 20 regions of Italy. It is located west of the Italian Peninsula, north of Tunisia and immediately south of the French island of Corsica. It is one of the five Italian regions with some degree of domestic autonomy being granted by a special statute. Its official name, Autonomous Region of Sardinia, is bilingual in Italian and Sardinian: / . It is divided into four provinces and a metropolitan city. The capital of the region of Sardinia — and its largest city — is Cagliari. Sardinia's indigenous language and Algherese Catalan are referred to by both the regional and national law as two of Italy's twelve officially recognized linguistic minorities, albeit gravely endangered, while the regional law provides ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
San Pietro Island
San Pietro Island (Italian: ''Isola di San Pietro'', Ligurian Tabarchino: ''Uiza de San Pé'', Sardinian: ''Isula 'e Sàntu Pèdru'') is an island approximately off the South western Coast of Sardinia, Italy, facing the Sulcis peninsula. With an area of it is the sixth-largest island of Italy by area. The approximately 6,000 inhabitants are mostly concentrated in the fishing town of Carloforte, the only ''comune'' in the island. It is included in the province of South Sardinia. It is named after Saint Peter. The island is connected by regular ferry service to Portovesme and Calasetta. Geography The island is of volcanic origin. The rocks are of Cenozoic age, and include basalt, dacite and rhyolite (including the peralkaline variety comendite). The of its coasts are mostly rocky; the western and northern part includes some natural grottoes, unprotected landings, with a few small beaches, in general here the coast is usually very steep, rocky. The eastern coast, on which the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Comendite
Comendite is a hard, peralkaline igneous rock, a type of light blue grey rhyolite. Phenocrysts are sodic sanidine with minor albite and bipyramidal quartz. Iddings, Joseph Paxson, 1913, ''Igneous rocks: composition, texture and classification'', v. 2, pp. 94-96 Comendite occurs in the mountains Tibrogargan, Coonowrin, Tunbubudla, Coochin, Saddleback, Tibberoowuccum and Ngungun in the Glass House Mountains, South East Queensland, Australia. The blue colour is caused by very small crystals of riebeckite or arfvedsonite. Comendite also occurs in Sardinia, Corsica, Ascension Island, Ethiopia, Somalia and other areas of East Africa. The 1903 eruption of Changbaishan volcano in north-east China erupted comendite pumice. Comendite derives its name from the area of Le Commende on San Pietro Island San Pietro Island (Italian: ''Isola di San Pietro'', Ligurian Tabarchino: ''Uiza de San Pé'', Sardinian: ''Isula 'e Sàntu Pèdru'') is an island approximately off the South western Coa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bonin Islands
The Bonin Islands, also known as the , are an archipelago of over 30 subtropical and tropical islands, some directly south of Tokyo, Japan and northwest of Guam. The name "Bonin Islands" comes from the Japanese word ''bunin'' (an archaic reading of ''mujin''), meaning "no people" or "uninhabited". The only inhabited islands of the group are Chichijima (), the seat of the municipal government, and Hahajima (). Archeological evidence has revealed that some of the islands may have been prehistorically inhabited by members of an unknown Micronesian ethnicity. Ogasawara Municipality (''mura'') and Ogasawara Subprefecture take their names from the Ogasawara Group. The is also used as a wider collective term that includes other islands in Ogasawara Municipality, such as the Volcano Islands, along with three other remote islands ( Nishinoshima, Minamitorishima, and Okinotorishima). Geographically speaking, all of these islands are parts of the Nanpō Islands. A total population of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boninite
Boninite is an extrusive rock high in both magnesium and silica, thought to be usually formed in fore-arc environments, typically during the early stages of subduction. The rock is named for its occurrence in the Izu-Bonin arc south of Japan. It is characterized by extreme depletion in incompatible trace elements that are not fluid mobile (e.g., the heavy rare-earth elements plus Nb, Ta, Hf) but variable enrichment in the fluid mobile elements (e.g., Rb, Ba, K). They are found almost exclusively in the fore-arc of primitive island arcs (that is, closer to the ocean trench) and in ophiolite complexes thought to represent former fore-arc settings or at least formed above a subduction zone. Boninite is considered to be a ''primitive'' andesite derived from melting of metasomatised mantle. Similar Archean intrusive rocks, called sanukitoids, have been reported in the rocks of several early cratons. Archean boninite lavas are also reported. Petrology Boninite typically consi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blairmore, Alberta
Blairmore is a community in the Rocky Mountains within the Municipality of Crowsnest Pass in southwest Alberta, Canada. It was formerly incorporated as a town prior to 1979 when it amalgamated with four other municipalities to form Crowsnest Pass. Blairmore is the principal commercial centre of Crowsnest Pass. History Originally a Canadian Pacific Railway stop called Tenth Siding or The Springs (for the cold sulphur spring to the east), the settlement was renamed Blairmore in November 1898 and it got a post office the following year. A ten-year dispute over land ownership between the CPR station agent and the section foreman stunted early development. The community was incorporated as the Village of Blairmore on September 3, 1901. Blairmore's principal industry was lumber and, after 1907, coal. Other industries soon followed. Blairmore incorporated as a town on September 29, 1911. With the declining fortunes of the nearby community of Frank, Blairmore soon became the region's ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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