Rock Identifier
Green-and-gold apatite-bearing rock, possibly epidote skarn (Apatite-group mineral, commonly fluorapatite (Ca₅(PO₄)₃F), with probable epidote and quartz; exact identification requires testing) — mineral
mineral

Green-and-gold apatite-bearing rock, possibly epidote skarn

Apatite-group mineral, commonly fluorapatite (Ca₅(PO₄)₃F), with probable epidote and quartz; exact identification requires testing

AI-generated identification · may be incorrect

Glassy to resinous luster, translucent pale green to honey-yellow and brown zones, granular/irregular crystal texture, and no obvious cleavage. Apatite hardness is Mohs 5; epidote is 6–7, with specific gravity roughly 3.1–3.5.

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Physical properties

Glassy to resinous luster, translucent pale green to honey-yellow and brown zones, granular/irregular crystal texture, and no obvious cleavage. Apatite hardness is Mohs 5; epidote is 6–7, with specific gravity roughly 3.1–3.5.

Formation & geological history

Likely a hydrothermal or contact-metamorphic skarn or mineralized vein formed when hot fluids altered carbonate or igneous host rock, generally during a regional intrusive event rather than at a precisely determinable age.

Uses & applications

Apatite is used mainly for phosphate fertilizer and occasionally as a gemstone; epidote and mixed specimens are chiefly collector material, while skarn itself has limited construction value.

Geological facts

The vivid green color may reflect epidote, chlorite, or chromium-bearing minerals rather than apatite alone; visible color is insufficient for a confident species identification.

Field identification & locations

Commonly found near granitic intrusions and metamorphosed limestone, including localities in Mexico, Pakistan, Brazil, Norway, and the United States. Check streak, hardness, cleavage, crystal form, and use a gemological or mineralogical test for confirmation.