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tyrolite
EntityQ1934730· pop 16· linked from 11 articles

Also known as Kupferschaum

Tyrolite is a hydrous calcium copper arsenate carbonate mineral with the formula CaCu5(AsO4)2CO3(OH)4⋅6H2O. Tyrolite forms glassy, blue to green orthorhombic radial crystals and botryoidal masses. It has a Mohs hardness of 1.5–2.0 and a specific gravity of 3.1–3.2. It is translucent with refractive indices of nα = 1.694, nβ = 1.726, and nγ = 1.730.

In the Vinony graph

Vinony's link graph records 11 inbound references to tyrolite, and connects out to Mohs scale of mineral hardness, Austria and water.

It sits within the topics Arsenate minerals, Calcium minerals and Copper(II) minerals.

Vinony links it to 15 Wikipedia language editions.

Key facts

Mineral.name
Tyrolite
Mineral.image
Tyrolite-256893.jpg
Mineral.imagesize
260px
Mineral.category
Arsenate and carbonate minerals
Mineral.IMAsymbol
Tyl
Mineral.strunz
8.DM.10
Mineral.system
Orthorhombic
Mineral.class
Prismatic (2/m) (same H-M symbol)
Mineral.symmetry
P2/c (no. 13) or C2/c (no. 15)
Mineral.color
Blue to green
Mineral.habit
Radial or botryoidal
Mineral.mohs
1.5–2.0
Mineral.luster
Vitreous
Mineral.diaphaneity
Translucent
Mineral.gravity
3.1–3.2
Mineral.refractive
nα = 1.694nβ = 1.726nγ = 1.730

via Wikipedia infobox

Wikidata facts

Subclass of
arsenate mineral
Named after
Tyrol
Image
Mineraly.sk - tirolit.jpg
Show 7 more facts
Nickel-Strunz 9th edition (updated 2009)
8.DM.10
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
8.DM.10
Commons category
Tyrolite
IMA Mineral Symbol
Tyl
chemical formula
Ca₂Cu₉(AsO₄)₄(CO₃)(OH)₈·11H₂O
Strunz 8th edition (series ID, updated)
VII/D.09
Sources (2)

via Wikidata · CC0

~1 min read

Encyclopedic overview

1 sections
Contents
  • References

Tyrolite is a hydrous calcium copper arsenate carbonate mineral with the formula CaCu5(AsO4)2CO3(OH)4⋅6H2O. Tyrolite forms glassy, blue to green orthorhombic radial crystals and botryoidal masses. It has a Mohs hardness of 1.5–2.0 and a specific gravity of 3.1–3.2. It is translucent with refractive indices of nα = 1.694, nβ = 1.726, and nγ = 1.730.

It is a secondary mineral formed by the weathering of associated copper and arsenic minerals. It was first described in 1845 for an occurrence in Schwaz, Tyrol, Austria.

Excerpted from Wikipedia’s “tyrolite” article, available under the CC BY-SA 4.0 licence.

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