Rock Identifier
Quartz (partially iron-stained) (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz (partially iron-stained)

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Milky white to yellowish-brown due to iron staining; Luster: Vitreous to waxy; Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture).

Hardness
7 on Mohs scale
Color
Milky white to yellowish-brown due to iron staining
Luster
Vitreous to waxy
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale; Color: Milky white to yellowish-brown due to iron staining; Luster: Vitreous to waxy; Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture).

Formation & geological history

Commonly forms in hydrothermal veins and pegmatites. It is a primary constituent of igneous, metamorphic, and sedimentary rocks, often accumulating in riverbeds and beaches due to its extreme resistance to weathering.

Uses & applications

Raw quartz is used in glassmaking, abrasives, and the electronics industry (silicon chips). In its crystalline form, it is used for jewelry, lapidary art, and spiritual collecting.

Geological facts

Quartz is one of the most abundant minerals in Earth's continental crust. The yellow-brown staining seen in samples like this is typically caused by goethite or limonite (iron oxide) inclusions or surface coatings.

Field identification & locations

Identify in the field by its hardness (it can scratch glass), lack of cleavage, and translucent appearance. It is found globally in almost every geological environment.