Matches in DBpedia 2014 for { <http://dbpedia.org/resource/Anglesite> ?p ?o. }
Showing items 1 to 74 of
74
with 100 items per page.
- Anglesite abstract "Anglesite is a lead sulfate mineral with the chemical formula PbSO4. It occurs as an oxidation product of primary lead sulfide ore, galena. Anglesite occurs as prismatic orthorhombic crystals and earthy masses, and is isomorphous with barite and celestine. It contains 74% of lead by mass and therefore has a high specific gravity of 6.3. Color is white or gray with pale yellow streaks. It may be dark gray if impure.It was first recognized as a mineral species by William Withering in 1783, who discovered it in the Parys copper-mine in Anglesey; the name anglesite, from this locality, was given by F. S. Beudant in 1832. The crystals from Anglesey, which were formerly found abundantly on a matrix of dull limonite, are small in size and simple in form, being usually bounded by four faces of a prism and four faces of a dome; they are brownish-yellow in colour owing to a stain of limonite. Crystals from some other localities, notably from Monteponi in Sardinia, are transparent and colourless, possessed of a brilliant adamantine lustre, and usually modified by numerous bright faces. The variety of combinations and habits presented by the crystals is very extensive, nearly two hundred distinct forms being figured by V. von Lang in his monograph of the species; without measurement of the angles the crystals are frequently difficult to decipher. There are distinct cleavages parallel to the faces of the prism (110) and the basal plane (001), but these are not so well developed as in the isomorphous minerals barite and celestite.Anglesite is a mineral of secondary origin, having been formed by the oxidation of galena in the upper parts of mineral lodes where these have been affected by weathering processes. At Monteponi the crystals encrust cavities in glistening granular galena; and from Leadhills, in Scotland, pseudomorphs of anglesite after galena are known. At most localities it is found as isolated crystals in the lead-bearing lodes, but at some places, in Australia and Mexico, it occurs as large masses, and is then mined as an ore of lead.".
- Anglesite thumbnail Anglésite-touizit_Monocristal.jpg?width=300.
- Anglesite wikiPageID "740871".
- Anglesite wikiPageRevisionID "539457501".
- Anglesite caption "Anglesite Touizit Morroco".
- Anglesite category Sulfate_minerals.
- Anglesite cleavage "[001] good, [210] distinct".
- Anglesite color "Colorless to white, commonly tinted gray; orange, yellow, green, blue, rarely violet".
- Anglesite diaphaneity "Transparent to translucent".
- Anglesite formula "PbSO4".
- Anglesite fracture "Brittle to conchoidal".
- Anglesite fusibility "1.5".
- Anglesite gravity "6.3".
- Anglesite habit "Granular, banded, nodular to stalactitic".
- Anglesite hasPhotoCollection Anglesite.
- Anglesite luster "Adamantine crystals, dull when massive earthy".
- Anglesite mohs "2.5".
- Anglesite name "Anglesite".
- Anglesite opticalprop "Biaxial".
- Anglesite refractive "nα = 1.878".
- Anglesite refractive "nβ = 1.883".
- Anglesite refractive "nγ = 1.895".
- Anglesite streak "White".
- Anglesite strunz "7".
- Anglesite system "Orthorhombic – Dipyramidal".
- Anglesite wordnet_type synset-mineral-noun-1.
- Anglesite subject Category:Lead_minerals.
- Anglesite subject Category:Orthorhombic_minerals.
- Anglesite subject Category:Sulfate_minerals.
- Anglesite type Abstraction100002137.
- Anglesite type LeadMinerals.
- Anglesite type Material114580897.
- Anglesite type Matter100020827.
- Anglesite type Mineral114662574.
- Anglesite type OrthorhombicMinerals.
- Anglesite type Part113809207.
- Anglesite type PhysicalEntity100001930.
- Anglesite type Relation100031921.
- Anglesite type Substance100019613.
- Anglesite type SulfateMinerals.
- Anglesite type ChemicalSubstance.
- Anglesite type Mineral.
- Anglesite type ChemicalObject.
- Anglesite type Thing.
- Anglesite comment "Anglesite is a lead sulfate mineral with the chemical formula PbSO4. It occurs as an oxidation product of primary lead sulfide ore, galena. Anglesite occurs as prismatic orthorhombic crystals and earthy masses, and is isomorphous with barite and celestine. It contains 74% of lead by mass and therefore has a high specific gravity of 6.3. Color is white or gray with pale yellow streaks.".
- Anglesite label "Anglesiet".
- Anglesite label "Anglesit".
- Anglesite label "Anglesita".
- Anglesite label "Anglesita".
- Anglesite label "Anglesite".
- Anglesite label "Anglesite".
- Anglesite label "Anglezyt".
- Anglesite label "Anglésite".
- Anglesite label "Англезит".
- Anglesite label "انجليزيت".
- Anglesite label "硫酸鉛鉱".
- Anglesite sameAs Anglesit.
- Anglesite sameAs Αγγλεσίτης.
- Anglesite sameAs Anglesita.
- Anglesite sameAs Anglesita.
- Anglesite sameAs Anglésite.
- Anglesite sameAs Anglesite.
- Anglesite sameAs 硫酸鉛鉱.
- Anglesite sameAs Anglesiet.
- Anglesite sameAs Anglezyt.
- Anglesite sameAs Anglesita.
- Anglesite sameAs m.037d3n.
- Anglesite sameAs Q156526.
- Anglesite sameAs Q156526.
- Anglesite sameAs Anglesite.
- Anglesite wasDerivedFrom Anglesite?oldid=539457501.
- Anglesite depiction Anglésite-touizit_Monocristal.jpg.
- Anglesite isPrimaryTopicOf Anglesite.
- Anglesite name "Anglesite".
