Asbestiform (original) (raw)
Asbestiform is a crystal habit. It describes a mineral that grows in a fibrous aggregate of high tensile strength, flexible, long, and thin crystals that readily separate. The most common asbestiform mineral is chrysotile, commonly called "white asbestos", a magnesium phyllosilicate part of the serpentine group. Other asbestiform minerals include riebeckite, an amphibole whose fibrous form is known as crocidolite or "blue asbestos", and brown asbestos, a cummingtonite-grunerite solid solution series.
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dbo:abstract | Asbestiform is a crystal habit. It describes a mineral that grows in a fibrous aggregate of high tensile strength, flexible, long, and thin crystals that readily separate. The most common asbestiform mineral is chrysotile, commonly called "white asbestos", a magnesium phyllosilicate part of the serpentine group. Other asbestiform minerals include riebeckite, an amphibole whose fibrous form is known as crocidolite or "blue asbestos", and brown asbestos, a cummingtonite-grunerite solid solution series. The United States Environmental Protection Agency explains that, "In general, exposure may occur only when the asbestos-containing material is disturbed or damaged in some way to release particles and fibers into the air." "Mountain leather" is an old-fashioned term for flexible, sheet-like natural formations of asbestiform minerals which resemble leather. Asbestos-containing minerals known to form mountain leather include: actinolite, palygorskite, saponite, sepiolite, tremolite, and zeolite. (en) |
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dbo:wikiPageWikiLink | dbr:Amphibole dbr:Saponite dbr:Sepiolite dbr:Chrysotile dbr:Tensile_strength dbr:Actinolite dbc:Asbestos dbr:Leather dbr:Crystal_habit dbr:Palygorskite dbr:Asbestos dbc:Crystallography dbc:Mineral_habits dbc:Mineralogy dbr:Zeolite dbr:Serpentine_group dbr:Riebeckite dbr:Tremolite |
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dcterms:subject | dbc:Asbestos dbc:Crystallography dbc:Mineral_habits dbc:Mineralogy |
gold:hypernym | dbr:Habit |
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rdfs:comment | Asbestiform is a crystal habit. It describes a mineral that grows in a fibrous aggregate of high tensile strength, flexible, long, and thin crystals that readily separate. The most common asbestiform mineral is chrysotile, commonly called "white asbestos", a magnesium phyllosilicate part of the serpentine group. Other asbestiform minerals include riebeckite, an amphibole whose fibrous form is known as crocidolite or "blue asbestos", and brown asbestos, a cummingtonite-grunerite solid solution series. (en) |
rdfs:label | Asbestiform (en) |
owl:sameAs | freebase:Asbestiform yago-res:Asbestiform wikidata:Asbestiform https://global.dbpedia.org/id/4TXGU |
prov:wasDerivedFrom | wikipedia-en:Asbestiform?oldid=1045441681&ns=0 |
foaf:isPrimaryTopicOf | wikipedia-en:Asbestiform |
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is foaf:primaryTopic of | wikipedia-en:Asbestiform |