Rock Identifier
K2 Jasper (K2 Granite) (Azurite in Granite (K(Mg,Fe)3AlSi3O10(OH,F)2 + Cu3(CO3)2(OH)2)) — igneous
igneous

K2 Jasper (K2 Granite)

Azurite in Granite (K(Mg,Fe)3AlSi3O10(OH,F)2 + Cu3(CO3)2(OH)2)

Hardness: 6-7 (Mohs scale), Color: White to grey granite matrix with bright blue circular inclusions, Luster: Vitreous to dull, Crystal Structure: Monoclinic (Azurite) in Phaneritic matrix, Cleavage: Indistinct in matrix, Specific Gravity: 2.6-2.9

Identified More igneous

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Physical properties

Hardness: 6-7 (Mohs scale), Color: White to grey granite matrix with bright blue circular inclusions, Luster: Vitreous to dull, Crystal Structure: Monoclinic (Azurite) in Phaneritic matrix, Cleavage: Indistinct in matrix, Specific Gravity: 2.6-2.9

Formation & geological history

Formed through the secondary mineralization of azurite within a pre-existing granite body. The azurite spots crystallized from copper-rich fluids that permeated the granite at high altitudes of the Karakoram Range.

Uses & applications

Primarily used for lapidary work, jewelry making (beads, cabochons), and as a popular semi-precious stone for metaphysical crystals and mineral collecting.

Geological facts

Despite being called 'K2 Jasper,' it is technically a granite, not a jasper. It is exclusively found near the base of K2 (the world's second-highest mountain) in Pakistan, making it rare and difficult to mine.

Field identification & locations

Identify by looking for the distinct 'ink-blat' or 'raindrop' blue spots of azurite against a speckled white and grey granite background. It is mostly sourced from the Skardu area of Pakistan.