Chalcophyllite from the Ting Tang Mine, Carharrack, Cornwall, England. Photo by Rob Lavinsky
General
Category
Arsenate minerals
Formula (repeating unit)
Cu 18Al 2(AsO 4) 4(SO 4) 3(OH) 24·36(H 2O)[1][2][3] or Cu 18Al 2(AsO 4) 3(SO 4) 3(OH) 27·33(H 2O)[4][5][6]
IMA symbol
Chp[7]
Strunz classification
8.DF.30
Dana classification
43.5.14.1
Crystal system
Trigonal
Crystal class
Rhomboedral (3) H-M symbol: (3)[2][3][4][6]
Space group
R3[8]
Identification
Color
Blue-green to emerald-green
Crystal habit
Crystals platy and six-sided, also as rosettes, drusy, foliated or massive.
Twinning
On {1010} as twin plane.
Cleavage
Perfect on {0001}
Fracture
Irregular
Mohs scale hardness
2
Luster
Vitreous to subadamantine, pearly on {0001}
Streak
Pale green
Diaphaneity
Transparent to translucent
Specific gravity
2.67 to 2.69[3][4][6] or 2.4 to 2.66[5]
Optical properties
Uniaxial (−)
Refractive index
nω = 1.618 to 1.632, nε = 1.552 to 1.575
Pleochroism
O blue-green, E almost colorless
Solubility
Soluble in acids and in ammonia
Other characteristics
Can be partially dehydrated. Alters to chrysocolla. Nonfluorescent, not radioactive
References
[8][3][4][5][6]
Chalcophyllite is a rare secondary copper arsenate mineral occurring in the oxidized zones of some arsenic-bearing copper deposits. It was first described from material collected in Germany. At one time chalcophyllite from Wheal Tamar in Cornwall, England, was called tamarite, but this name is now discredited[2] (not to be confused with the amphibole mineral taramite, which is quite different). At Wheal Gorland a specimen exhibiting partial replacement of liriconite, Cu 2Al(AsO 4)(OH) 4·(4H 2O), by chalcophyllite has been found.[2] The mineral is named from the Greek, chalco "copper" and fyllon, "leaf", in allusion to its composition and platy structure. It is a classic Cornish mineral that can be confused with tabular spangolite.
^"IMA Mineral List with Database of Mineral Properties".
^ abcdRocks & Minerals (2009) 84-5: 434 to 440
^ abcdHandbook of Mineralogy
^ abcdMindat.org
^ abcWebmineral data
^ abcdGaines et al (1997) Dana's New Mineralogy, Wiley
Chalcophyllite is a rare secondary copper arsenate mineral occurring in the oxidized zones of some arsenic-bearing copper deposits. It was first described...
has changed significantly. Similar natural compounds are the minerals chalcophyllite Cu 18Al 2(AsO 4) 3(SO 4) 3(OH) 27·36H 2O, conichalcite CaCu(AsO 4)(OH)...
aluminium and sulfate. Associated minerals include brochantite, spangolite, chalcophyllite, olivenite, tyrolite, parnauite, azurite and malachite. The main deposits...
secondary mineral in copper deposits in association with olivenite, chalcophyllite, clinoclase, cornwallite, strashimirite, malachite, cuprite and limonite...
area was also known for rarer and more valuable minerals including chalcophyllite, olivenite, mimetite and liroconite.[citation needed] Today, the ruins...
is associated with wroewolfeite, posnjakite, serpierite, devilline, chalcophyllite, connellite, brochantite, malachite and gypsum. There are two type localities...
Pradet, Var, Provence-Alpes-Côte d'Azur, France, associated minerals are chalcophyllite, cyanotrichite, parnauite, mansfieldite, olivenite, tennantite, covellite...
clinoclase and pseudomorphs after parnauite. Other associations are with chalcophyllite, chenevixite, pseudomalachite, bayldonite, tyrolite, azurite and chrysocolla...