
sedimentary
Sand (Construction Grade)
Unconsolidated siliciclastic sediment (primarily SiO2)
Hardness: 7 (Mohs scale for quartz grains); Color: Tan, beige, or light brown; Luster: Dull to vitreous; Crystal structure: Trigonal (as individual quartz grains); Cleavage: None; Specific gravity: Approx 2.65.
- Hardness
- 7 (Mohs scale for quartz grains)
- Color
- Tan, beige, or light brown
- Luster
- Dull to vitreous
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Physical properties
Hardness: 7 (Mohs scale for quartz grains); Color: Tan, beige, or light brown; Luster: Dull to vitreous; Crystal structure: Trigonal (as individual quartz grains); Cleavage: None; Specific gravity: Approx 2.65.
Formation & geological history
Formed through the mechanical and chemical weathering of igneous (granitic) or metamorphic rocks over millions of years. It is transported by water or wind and deposited in alluvial plain or beach environments.
Uses & applications
Primary use is in construction as a fine aggregate for concrete, mortar, and asphalt. Also used in glass manufacturing, sandblasting, and water filtration systems.
Geological facts
Sand is the second most used natural resource in the world after water. While it seems infinite, specific 'angular' construction sand is a finite resource currently facing a global shortage due to urbanization.
Field identification & locations
Identified by its granular texture and visible mineral grains (usually quartz, feldspar, and mica). In the field, look for alluvial deposits, riverbeds, or glacial outwash plains. Use a hand lens to see grain rounding and sorting.
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