Chalcophyllite
A variety of Minerals

What is Chalcophyllite?
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 (not to be confused with the amphibole mineral taramite, which is quite different). At Wheal Gorland a specimen exhibiting partial replacement of liriconite, Cu2Al(AsO4)(OH)4•(4H2O), by chalcophyllite has been found. 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.
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Key Characteristics
Characteristics of Chalcophyllite
Cleavage is perfect perpendicular to the c crystal axis, and twinning occurs with {1010} as the twin plane. Fracture is irregular. The mineral is soft, with hardness only 2, the same as gypsum. Specific gravity is generally given in the range 2.67 to 2.69, but Webmineral has 2.4 to 2.66. Chalcophyllite is soluble in acids and in ammonia. It is not fluorescent, nor radioactive. The water content varies at room temperature based on relative humidity. Chalcophyllite alters to chrysocolla, which is a copper-aluminium silicate with the formula (Cu,Al)2H2Si2O5(OH)4•n(H2O).
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Quick Facts
Physical Properties
- Color
- Emerald green, grass green, bluish green, blue; green in transmitted light
- Hardness (Mohs)
- 2
- Density
- 2.684 g/cm³
- Streak
- Pale green to bluish green
Chemical Properties
- Chemical Formula
- Cu18Al2(AsO4)4(SO4)3(OH)24 · 36H2O
- Elements
- Al, As, Cu, H, O, S
Also Known As

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