Tyrolite

tyrolite

tennantite

erythrite

aurichalcite

Images

Formula: Ca2Cu9(AsO4)4(CO3)(OH)8.11H2O
Hydrated arsenate containing hydroxyl
Crystal System: Monoclinic
Specific gravity: 3 to 3.2 measured
Hardness: 1½ to 2
Streak: Paler than unpowdered colour
Colour: Turquoise-blue, blue-green; light bluish green in transmitted light.
Solubility: Soluble in acids and ammonia
Common impurities: S,O
Environments:

Hydrothermal environments

Tyrolite is an uncommon secondary mineral in the oxidised zone of copper deposits, typically formed by alteration of tennantite(HOM) and associated with tennantite, erythrite, malachite, azurite, brochantite, chrysocolla, aurichalcite, cuprite and iron oxyhydroxides (Dana, HOM).

Localities

The type locality is Falkenstein, Falkenstein mining district, Schwaz District, Tyrol, Austria.
Tyrolite from Falkenstein - Image

In the Tintic Mineral District, Utah, USA, some very fine specimens of tyrolite have been found. It is relatively common in the deposits where arsenate minerals are abundant. Specimens of quartz with goethite from several centimetres to tens of centimetres and with pale blue-green tyrolite sprays on fracture surfaces and in vein fillings are among the largest and finest Tintic examples of tyrolite. The best crystals occur in a matrix of quartz where enargite has been partially or wholly altered near voids where nice single crystals and crystal clusters are able to form. Single tyrolite crystals reach 1 cm only exceptionally. When tyrolite crystals embedded in quartz are first exposed by breaking the quartz, the tyrolite looks bright blue and glassy, but after a period of being exposed to the atmosphere the crystals very commonly dehydrate, becoming a much paler, less lustrous, opaque blue (MinRec 55.2.226).
The tyrolite is associated with chalcophyllite and conichalcite (Dana).
Tyrolite from Tintic - Image

At the Gold Hill Mine, Gold Hill, Gold Hill Mining District, Tooele County, Utah, USA, juanitaite occurs on the 46-meter level, as fine-grained coatings on cavity walls in quartz veins, associated with connellite, tyrolite and azurite (CM 40.254).
Tyrolite from Gold Hill - Image

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