
mineral
Quartz (Milky or Smoky Quartz Pebble)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Translucent grey to milky white; Luster: Vitreous to greasy; Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Translucent grey to milky white
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Translucent grey to milky white; Luster: Vitreous to greasy; Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed from cooling silica-rich hydrothermal fluids or magma, frequently found in veins. This smooth pebble shape is the result of fluvial erosion (water wear) in the Seongjusan mountain area.
Uses & applications
Commonly used in glassmaking, electronics (piezoelectric properties), and as decorative gravel or gemstone (semiprecious).
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. The location provided, Seongjusan Natural Recreation Forest in Boryeong, is part of a region known for diverse granite and metamorphic rock formations.
Field identification & locations
Identify in the field by its ability to scratch glass, its lack of cleavage planes, and its characteristic waxy or glassy luster. This specimen is a typical river-worn pebble.
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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