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Formula: Cu5(AsO4)2(OH)4
Anhydrous arsenate, triclinic
paramorph of monoclinic
cornwallite
Crystal System: Triclinic
Specific gravity: 4.64 measured, 4.85 calculated
Hardness: 4
Streak: Pale green
Colour: Apple green to dark green
Environments:
Cornubite is a rare secondary mineral in oxidised
copper deposits. Near Reichenbach
in the Oderwald, Germany, cornubite occurs in a silicified quartz vein
(AM 70.1333).
Localities
At Bou Azzer, Morocco cornubite has been found in quartz cavities
together with
scorodite
(MinRec 38.5.
At the type locality, Wheal Carpenter, Cornwall,
England cornubite occurs in copper-tin-silver
bearing hydrothermal veins, associated with cornwallite,
chalcophyllite,
olivenite, liroconite,
chenevixite, clinoclase,
pseudomalachite, bayldonite,
parnauite, tyrolite,
azurite, malachite,
cuprite, chrysocolla and
quartz
(HOM).
Cornubite from Wheal Carpenter - Image
At the San Rafael mine, Nye county, Nevada, USA, cornubite has been found with
olivenite and strashimirite
(R&M 85.6.517).
At the Tintic Mining District, Juab County, Utah, USA,cornubite is quite rare, but it has been found both at
the Centennial Eureka mine and at the Mammoth mines. At the Centennial Eureka mine, it occurs as well-formed
crystals and as rosettes of pale green platelike crystals, up to 0.5 mm in size, on
quartz associated with malachite.
It has also been found associated with enargite,
olivenite and clinoclase at
the Mammoth mine
(MinRec 55.2.196).
Cornubite from the Tintic Mining District -
Image
Stability
The Activity-pH diagram below was calculated at 298.2 K for some carbonates and copper arsenates for constant activity (roughly
equivalent to concentration) of H2AsO4- in solution, over a range of values of pH and of
H2CO3 activity
(MM 52.687).
The mineral formulae are:
azurite: Cu3(CO3)2(OH)2
malachite: Cu2(CO3)(OH)2
olivenite: Cu2(AsO4)(OH)
cornubite: Cu5(AsO4)2(OH)4
clinoclase: Cu3(AsO4)(OH)3
The Activity-pH diagram below was calculated at 298.2 K for some arsenates
and sulphates for constant activity (roughly equivalent to concentration) of H2AsO4- in solution,
over a range of values of pH and of SO42- activity
(MM 52.689).
The mineral formulae are:
chalcanthite: Cu(SO4).5H2O
antlerite: Cu2+3(SO4)(OH)4
brochantite: Cu4(SO4)(OH)6
olivenite: Cu2(AsO4)(OH)
cornubite: Cu5(AsO4)2(OH)4
clinoclase: Cu3(AsO4)(OH)3
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