mineral

Quartz Vein in Host Rock (Gossanous Matrtix)

Silicon Dioxide (SiO2) with iron oxides (Limonite/Hematite)

Hardness: 7 (Mohs scale), Color: Milky white to translucent with reddish-brown staining, Luster: Vitreous (glassy), Crystal Structure: Trigonal, Cleavage: None/Conchoidal fracture.

Identified April 25, 2026More mineral →

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Physical properties

Hardness: 7 (Mohs scale), Color: Milky white to translucent with reddish-brown staining, Luster: Vitreous (glassy), Crystal Structure: Trigonal, Cleavage: None/Conchoidal fracture.

Formation & geological history

Formed through hydrothermal precipitation where mineral-rich hot fluids circulate through fractures in crustal rocks. The reddish coloration suggests oxidation of sulfide minerals within the vein.

Uses & applications

Quartz is used in glassmaking, abrasives, and electronics. This specific iron-stained variety is often collected as a representative specimen of mineralized veins or used as an indicator for prospecting other minerals like gold.

Geological facts

Iron-stained quartz veins like this are often referred to as 'gossan' or 'iron hat' by miners. They are historical indicators used by prospectors to find underlying ore deposits containing copper, lead, or gold.

Field identification & locations

Identify by its hardness (scratches glass), glassy luster on fresh surfaces, and the characteristic rusty-orange staining. Commonly found in mountainous regions near fault lines or volcanic activity.

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Sandstone (with potential mineral staining/concretions)

Arenite (SiO2 based)

sedimentary

Schist

Metamorphic

Epidote

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metamorphic

Nephrite Jade

Nephrite

Mineral/Rock

Banded Gneiss (River Rock/Pebble)

Gneiss (specifically a banded variety often found as a river rock)

Metamorphic Rock

Green Apatite on Albite

Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]

mineral