Quartz Vein in Host Rock (Gossanous Matrtix)
Silicon Dioxide (SiO2) with iron oxides (Limonite/Hematite)
Rock Type: mineral

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.
Identified on: 4/25/2026
Mode: Standard