
sedimentary
Sandstone with Quartz Vein
Quartzose Sandstone with Hydrothermal Quartz
Hardness: 7 for quartz grains and vein, lower for cement; Color: Tan/brown with white quartz; Luster: Vitreous on quartz crystals, dull on matrix; Crystal structure: Trigonal (quartz); Specific gravity: 2.65
- Hardness
- 7 for quartz grains and vein, lower for cement
- Color
- Tan/brown with white quartz
- Luster
- Vitreous on quartz crystals, dull on matrix
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Physical properties
Hardness: 7 for quartz grains and vein, lower for cement; Color: Tan/brown with white quartz; Luster: Vitreous on quartz crystals, dull on matrix; Crystal structure: Trigonal (quartz); Specific gravity: 2.65
Formation & geological history
Formed through the accumulation, compaction, and cementation of mineral particles or rock fragments, predominantly quartz, followed by hydrothermal fluid deposition filling fractures with white quartz.
Uses & applications
Used primarily in educational settings, geological collections, and as decorative aggregate.
Geological facts
Sandstone makes up about 20-25% of all sedimentary rocks on Earth and is frequently found in deserts, riverbeds, and beach environments.
Field identification & locations
Can be identified by its gritty texture, visible sand grains, and distinct contrast with white quartz veining. Common in sedimentary basins worldwide.
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