
mineral
Quartz (Water-worn pebble)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Milky white to translucent with dark mineral inclusions/staining; Luster: Vitreous to waxy; Crystal Structure: Trigonal (often appears amorphous in smooth pebbles); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 (Mohs scale); Color: Milky white to translucent with dark mineral inclusions/staining; Luster: Vitreous to waxy; Crystal Structure: Trigonal (often appears amorphous in smooth pebbles); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Formed from silica-rich hydrothermal fluids or within igneous and metamorphic rocks. This specific specimen has been chemically or mechanically weathered and rounded by water transport in a river or beach environment over thousands of years.
Uses & applications
Industrial use for glass production, electronics (piezoelectric properties), abrasives, and as decorative stone or jewelry (when polished).
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. These specific rounded stones are often called 'river rocks' or 'beach pebbles' and their smooth texture is the result of natural rock tumbling by water.
Field identification & locations
Identify in the field by its hardness (will scratch glass and steel), lack of visible grains like sandstone, and its smooth, waxy surface when found in water beds. It is resistant to chemical weathering.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary