About: Hidalgoite

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Hidalgoite, PbAl3(AsO4)(SO4)(OH)4, is a rare member of the beudantite group and is usually classified as part of the alunite family. It was named after the place where it was first discovered, the Zimapán mining district, Hidalgo, Mexico. At Hidalgo where it was initially discovered, it was found as dense white masses in alternating dikes of quartz latite and quartz monzonite alongside other secondary minerals such as sphalerite, arsenopyrite, cerussite and trace amounts of angelsite and alamosite, it was then rediscovered at other locations such as Australia where it occurs on oxidized shear zones above greywacke shales especially on the anticline prospects of the area, and on fine grained quartz-spessartine rocks in Broken Hill, Australia. Hidalgoite specimens are usually associated with

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  • La hidalgoïta és un mineral de la classe dels fosfats, que pertany al grup de la beudantita. És l'anàleg d'arsènic de la hinsdalita i l'anàleg d'alumini de la beudantita. El seu nom prové de la seva localitat tipus. (ca)
  • Hidalgoit ist ein selten vorkommendes Mineral aus der Mineralklasse der „Phosphate, Arsenate und Vanadate“. Es kristallisiert im trigonalen Kristallsystem mit der chemischen Zusammensetzung PbAl3[(OH)6|SO4|AsO4], ist also ein Blei-Aluminium-Sulfat-Arsenat mit zusätzlichen Hydroxidionen. Hidalgoit findet sich überwiegend in Form körniger bis kompakter, porzellanartiger oder poröser Massen und Rissfüllungen. Auch kleine, sphärolithische bzw. nierige Mineral-Aggregate sind bekannt. Sehr selten entwickelt Hidalgoit auch mikroskopisch kleine Kristalle mit skalenoedrischem Habitus. In reiner Form ist Hidalgoit farblos und durchsichtig. Allerdings ist er aufgrund seiner polykristallinen Ausbildung meist durchscheinend weiß oder nimmt durch Fremdbeimengungen eine hellgrüne, pistaziengrüne oder smaragdgrüne Farbe an. (de)
  • Hidalgoita mineral bat da. (eu)
  • Hidalgoite, PbAl3(AsO4)(SO4)(OH)4, is a rare member of the beudantite group and is usually classified as part of the alunite family. It was named after the place where it was first discovered, the Zimapán mining district, Hidalgo, Mexico. At Hidalgo where it was initially discovered, it was found as dense white masses in alternating dikes of quartz latite and quartz monzonite alongside other secondary minerals such as sphalerite, arsenopyrite, cerussite and trace amounts of angelsite and alamosite, it was then rediscovered at other locations such as Australia where it occurs on oxidized shear zones above greywacke shales especially on the anticline prospects of the area, and on fine grained quartz-spessartine rocks in Broken Hill, Australia. Hidalgoite specimens are usually associated with copper minerals, clay minerals, iron oxides and polymetallic sulfides in occurrence. Hidalgoite is categorized under the trigonal crystal system and R3m space group and can be denoted by the H-M symbol (32/m). Physical properties of hidalgoite include its gray white to light gray color, a white streak, specific gravity of 3.96 and a hardness of 4.5. Hidalgoite specimens are usually translucent to sub opaque, and the brittle nature of mineral produces conchoidal fractures. It has an earthy luster. (en)
  • L'hidalgoite è un minerale appartenente al gruppo della beudantite, solfato basico di piombo ed alluminio scoperto nel 1948 e descritto nel 1953 in base ad un ritrovamento avvenuto nella miniera di San Pascual nel distretto minerario di Zimapan, stato di Hidalgo, Messico. Il nome è stato attribuito in relazione allo Stato dove si trova la località di ritrovamento. Il minerale è l'analogo dell'hinsdalite con l'arsenico al posto del fosforo e l'analogo della beudantite con l'alluminio al posto del ferro. L'hidalgoite è insolubile in acido cloridrico, nitrico e solforico. (it)
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  • 41397488 (xsd:integer)
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  • Hidalgoite from a mine in Utah (en)
dbp:category
dbp:class
  • H-M symbol: (en)
  • Hexagonal scalenohedral (en)
dbp:color
  • White, pale green, pistachio-green, emerald-green (en)
dbp:diaphaneity
  • Translucent (en)
dbp:formula
  • PbAl34 (en)
dbp:fracture
  • Irregular to conchoidal (en)
dbp:gravity
  • 3.710000 (xsd:double)
dbp:habit
  • Massive, porcellaneous to porous; spherulitic aggregates (en)
dbp:imagesize
  • 260 (xsd:integer)
dbp:imasymbol
  • Hid (en)
dbp:luster
  • Earthy or dull in aggregates (en)
dbp:mohs
  • 4.500000 (xsd:double)
dbp:name
  • Hidalgoite (en)
dbp:opticalprop
  • Uniaxial (en)
dbp:refractive
  • nω = 1.713–1.730 nε 1.715–1.735 (en)
dbp:streak
  • White (en)
dbp:strunz
  • 8 (xsd:integer)
dbp:symmetry
  • Rm (en)
dbp:system
dbp:tenacity
  • Brittle (en)
dbp:unitCell
  • a = 7.04, c = 16.99 [Å]; Z = 3 (en)
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  • La hidalgoïta és un mineral de la classe dels fosfats, que pertany al grup de la beudantita. És l'anàleg d'arsènic de la hinsdalita i l'anàleg d'alumini de la beudantita. El seu nom prové de la seva localitat tipus. (ca)
  • Hidalgoita mineral bat da. (eu)
  • L'hidalgoite è un minerale appartenente al gruppo della beudantite, solfato basico di piombo ed alluminio scoperto nel 1948 e descritto nel 1953 in base ad un ritrovamento avvenuto nella miniera di San Pascual nel distretto minerario di Zimapan, stato di Hidalgo, Messico. Il nome è stato attribuito in relazione allo Stato dove si trova la località di ritrovamento. Il minerale è l'analogo dell'hinsdalite con l'arsenico al posto del fosforo e l'analogo della beudantite con l'alluminio al posto del ferro. L'hidalgoite è insolubile in acido cloridrico, nitrico e solforico. (it)
  • Hidalgoit ist ein selten vorkommendes Mineral aus der Mineralklasse der „Phosphate, Arsenate und Vanadate“. Es kristallisiert im trigonalen Kristallsystem mit der chemischen Zusammensetzung PbAl3[(OH)6|SO4|AsO4], ist also ein Blei-Aluminium-Sulfat-Arsenat mit zusätzlichen Hydroxidionen. (de)
  • Hidalgoite, PbAl3(AsO4)(SO4)(OH)4, is a rare member of the beudantite group and is usually classified as part of the alunite family. It was named after the place where it was first discovered, the Zimapán mining district, Hidalgo, Mexico. At Hidalgo where it was initially discovered, it was found as dense white masses in alternating dikes of quartz latite and quartz monzonite alongside other secondary minerals such as sphalerite, arsenopyrite, cerussite and trace amounts of angelsite and alamosite, it was then rediscovered at other locations such as Australia where it occurs on oxidized shear zones above greywacke shales especially on the anticline prospects of the area, and on fine grained quartz-spessartine rocks in Broken Hill, Australia. Hidalgoite specimens are usually associated with (en)
rdfs:label
  • Hidalgoïta (ca)
  • Hidalgoit (de)
  • Hidalgoite (en)
  • Hidalgoita (eu)
  • Hidalgoite (it)
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foaf:isPrimaryTopicOf
foaf:name
  • Hidalgoite (en)
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