Rock Identifier
Azurite in Matrix (Azurite (Cu3(CO3)2(OH)2) in Rhyolite or Sandstone matrix) — mineral
mineral

Azurite in Matrix

Azurite (Cu3(CO3)2(OH)2) in Rhyolite or Sandstone matrix

Hardness: 3.5-4 (for azurite); Color: Deep blue to cyan-blue spots on a tan/grey rocky matrix; Luster: Vitreous to dull; Crystal structure: Monoclinic; Cleavage: Good; Specific gravity: 3.7-3.9

Hardness
3
Color
Deep blue to cyan-blue spots on a tan/grey rocky matrix
Luster
Vitreous to dull
Identified More mineral
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Physical properties

Hardness: 3.5-4 (for azurite); Color: Deep blue to cyan-blue spots on a tan/grey rocky matrix; Luster: Vitreous to dull; Crystal structure: Monoclinic; Cleavage: Good; Specific gravity: 3.7-3.9

Formation & geological history

Secondary mineral formed in the oxidized zones of copper ore deposits. It occurs when carbonated waters descend into the earth and react with copper-bearing minerals. The matrix is typically host rock like limestone, sandstone, or igneous rhyolite.

Uses & applications

Used primarily as a minor ore of copper, as a pigment historically, in jewelry as cabochons, and as a popular mineral specimen for collectors.

Geological facts

In antiquity, azurite was known as Lapis Armenium. It was a primary source of blue pigment for painters in the Middle Ages and Renaissance, though it has the tendency to weather into green malachite over time.

Field identification & locations

Identify by its distinctive bright blue color and association with other copper minerals like malachite. In the field, look for blue staining in copper-rich mining districts like those in Arizona or Morocco.