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liroconite
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liroconite

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Liroconite is a complex mineral: Hydrated copper aluminium arsenate hydroxide, with the formula Cu2Al[(OH)4|AsO4]·4(H2O). It is a vitreous monoclinic mineral, colored bright blue to green, often associated with malachite, azurite, olivenite, and clinoclase. It is quite soft, with a Mohs hardness of 2–2.5, and has a specific gravity of 2.9–3.0. thumb|left|Vugs in gossan lined with lustrous, blue-green liroconite blades and sparkly, dark blue [[clinoclase microcrystals from Wheal Gorland (size: 3.4 × 3.0 × 2.0 cm)]] It was first identified in 1825 in the tin and copper mines of Devon and Cornwal

Key facts

Mineral.name
Liroconite
Mineral.boxbgcolor
278aa0
Mineral.boxtextcolor
fff
Mineral.image
Liroconite-Strashimirite-171815.jpg
Mineral.imagesize
260px
Mineral.category
Arsenate minerals
Mineral.formula
Cu2Al[(OH)4
Mineral.IMAsymbol
Lro
Mineral.strunz
8.DF.20
Mineral.system
Monoclinic
Mineral.class
Prismatic (2/m) (same H-M symbol)
Mineral.symmetry
I2/a
Mineral.unit cell
a = 12.66, b = 7.57 c = 9.89 [Å]; β = 91.25°; Z = 4
Mineral.color
Bright blue to green
Mineral.habit
Typically as striated flattened octahedral or lenticular crystals, also massive to granular
Mineral.cleavage
Indistinct on {110} and {011}
Mineral.fracture
Irregular/uneven, conchoidal
Mineral.mohs
2–

via Wikipedia infobox

Wikidata facts

Image
Liroconite-226219.jpg
Show 6 more facts
Commons category
Liroconite
Nickel-Strunz 9th edition (updated 2009)
8.DF.20
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
8.DF.20
IMA Mineral Symbol
Lro
chemical formula
Cu₂AlAsO₄(OH)₄·4H₂O
Strunz 8th edition (series ID, updated)
VII/D.11
Sources (1)

via Wikidata · CC0

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Article

3 sections
Contents
  • Structure
  • See also
  • References

{{Infobox mineral | name = Liroconite | boxwidth = | boxbgcolor =#278aa0 | boxtextcolor = #fff | image = Liroconite-Strashimirite-171815.jpg | imagesize = 260px | alt = | caption = | category = Arsenate minerals | formula = Cu2Al[(OH)4|AsO4]·4(H2O) | IMAsymbol = Lro | molweight = | strunz = 8.DF.20 | dana = | system = Monoclinic | class = Prismatic (2/m) (same H-M symbol) | symmetry = I2/a | unit cell = a = 12.66, b = 7.57 c = 9.89 [Å]; β = 91.25°; Z = 4 | color = Bright blue to green | colour = | habit = Typically as striated flattened octahedral or lenticular crystals, also massive to granular | twinning = | cleavage = Indistinct on {110} and {011} | fracture = Irregular/uneven, conchoidal | tenacity = | mohs = 2– | luster = Vitreous to resinous | streak = Light blue | diaphaneity = Transparent, translucent | gravity = 2.9–3 | density = | polish = | opticalprop = Biaxial (−) | refractive = nα = 1.612 nβ = 1.652 nγ = 1.675 | birefringence = δ = 0.063 | pleochroism = | 2V = Measured: 67° | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = | alteration = | other = | references = }} Liroconite is a complex mineral: Hydrated copper aluminium arsenate hydroxide, with the formula Cu2Al[(OH)4|AsO4]·4(H2O). It is a vitreous monoclinic mineral, colored bright blue to green, often associated with malachite, azurite, olivenite, and clinoclase. It is quite soft, with a Mohs hardness of 2–2.5, and has a specific gravity of 2.9–3.0. thumb|left|Vugs in gossan lined with lustrous, blue-green liroconite blades and sparkly, dark blue [[clinoclase microcrystals from Wheal Gorland (size: 3.4 × 3.0 × 2.0 cm)]] It was first identified in 1825 in the tin and copper mines of Devon and Cornwall, England. Although it remains quite rare it has subsequently been identified in a variety of locations including France, Germany, Australia, New Jersey and California.

The type locality for liroconite is Wheal Gorland in St Day, Cornwall in the United Kingdom. The largest crystal specimen on public display is in the Royal Cornwall Museum in Truro.

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