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Curved Chalcanthite Crystals

The Mineral chalcanthite




Natural Chalcanthite crystals are very rare in nature. Well-formed crystals are easily grown synthetically from copper sulfate solutions. This can be done by dissolving a readily available chemical salt called copper sulfate, and then letting the water evaporate. This leaves behind a crystallized mass of Chalcanthite which can crystallize beautifully if grown properly. If a Chalcanthite crystal looks to good to be natural, it probably is, as good natural crystals are very hard to come accross. Unscrupulous mineral dealers have been known to sell large, synthetic Chalcanthite specimens without indicating that they are not natural.

Chalcanthite generally forms in arid regions and dry caves which are protected from moisture. It commonly forms stalactitic and botryoidal growths on the walls and ceilings of mine tunnels from the oxidation of copper sulfide minerals. Chalcanthite specimens must be kept away from water and moist conditions, since a chemical effect with water causes them to eventually crumble or dissolve. Some collectors specimens are coated with mineral oil and sprayed with laquer to seal the mineral and prevent it from absorbing water. Chalcanthite is a very fragile mineral, and care should be taken when handling any specimen.

The name Chalcanthite is derived from the Greek words "chalkos", which means copper and "anthos", flower, describing the curved and sometimes flowering formations of this mineral.
Chemical Formula CuSO4 · 5H2O
Composition Hydrous copper sulfate
Color Bright blue, sky-blue, greenish-blue
Streak White
Hardness 2.5
Crystal System Triclinic
Crystal Forms
and Aggregates
Crystals, which are rare in nature, are in short prismatic form and in thick tabular crystals. Most often as fibrous veins, which are commonly curved, and as and flowering curved masses of parallel fibrous crystals. Also botryoidal, stalactitic, encrusting, massive, as tiny, slender needles, and lenticular.
Transparency Translucent
Specific Gravity 2.3
Luster Vitreous, silky, dull
Cleavage Indiscernible
Fracture Conchoidal to splintery
Tenacity Brittle, thin projections slightly flexible
Other ID Marks 1) Has a sweetish, metallic taste. (Note of caution: Chalcanthite is poisonous and should not be taste-tested, unless the lick is minor and it is spit out and rinsed immediately.)
2) Dissolves slowly in water, turning the solution blue.
In Group Sulfates; Hydrous Sulfates
Striking Features Intense blue color and crystal forms
Environment Chalcanthite is a secondary copper mineral formed through the oxidation of copper sulfides.
Rock Type Sedimentary, Metamorphic
Popularity (1-4) 2
Prevalence (1-3) 2
Demand (1-3) 2


Chalcanthite AUCTIONS
OTHER NAMES
Blue Vitriol
Copper Sulfate
Copper Vitriol



USES
Chalcanthite is an important ore of copper in areas where it occurs in relative abundance, such as in Chile and Spain. It is also used as a root killer in sewer pipes by flushing Chalcanthite pellets down the toilet. Specimens are popular among collectors, and the synthetically grown crystals are often sold to unwary collectors.

NOTEWORTHY LOCALITIES
In Chuquicamata and El Teniente in Chile, large, fibrous Chalcanthite masses occur in abundance and are mined as an ore of copper. A sizable deposit also exists in Minas de Riotinto, Andalusia, Spain. Also comes from the Sao Domingos Mine, Portugal; and Lubin, Legnics, Poland. Large botryoidal crusts were found Tsumeb, Namibia.

In the U.S., the most prominent locality for Chalcanthite specimens is the Planet Mine, La Paz Co., Arizona. Other Arizona occurrences include Bisbee, Cochise Co.; Ajo and Tiger, Pinal Co.; Globe, Gila Co.; Morenci, Greenlee Co; and the Patagonia District, Santa Cruz Co. Also occurs in Bingham Canyon, Salt Lake Co., Utah; and Ducktown, Polk Co., Tennessee.

COMMON MINERAL ASSOCIATIONS
Brochantite, Malachite, Calcite, Aragonite, Gypsum, Chalcopyrite

DISTINGUISHING SIMILAR MINERALS
Few other minerals have the rich blue color and forms, making Chalcanthite hard to confuse with other minerals.


chalcanthite PHOTOS
 
ADDITIONAL RESOURCES
 
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