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Azurite is a soft, deep blue copper mineral produced by weathering of
copper ore deposits. It is also known as Chessylite after the type locality at
Chessy-les-Mines near Lyon, France.[2] The mineral has been known since ancient
times, and was mentioned in Pliny the Elder's Natural History under the Greek
name kuanos : "deep blue," root of the English word cyan, and the Latin
name caeruleum. Azurite crystals are monoclinic, and when large enough to be
seen they appear as dark blue prismatic crystals. Azurite specimens are typically
massive to nodular, and are often stalactitic in form. Specimens tend to lighten
in color over time due to weathering of the specimen surface into malachite.
Azurite is soft, with a Mohs hardness of only 3.5 to 4. The specific gravity of
azurite is 3.77 to 3.89. Azurite is destroyed by heat, losing carbon dioxide and
water to form black, powdery copper(II) oxide. (source: Wikipedia)

The 2rd photo below shows nodules of Azurite on a large piece of malachite from Arizona,
and is on display at the Mewbourne College of Earth & Energy
at the University of Oklahoma

Photos by Michael Marcotte


Azurite, natural luster



poor quality, low color saturation
poor quality azurite with low color saturation



Green is malachite, natural luster with purplish-blue Azurite nodules
Green is malachite, natural luster with purplish-blue Azurite nodules

Moroccan Azurite
azurite from Morocco (photo by Michael Marcotte)


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