
mineral
Yellow Quartz / Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Pale yellow to light brownish-orange. Luster: Vitreous to waxy. Crystal Structure: Hexagonal (Trigonal). Cleavage: None. Specific gravity: ~2.65.
- Hardness
- 7 on Mohs scale
- Color
- Pale yellow to light brownish-orange
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale. Color: Pale yellow to light brownish-orange. Luster: Vitreous to waxy. Crystal Structure: Hexagonal (Trigonal). Cleavage: None. Specific gravity: ~2.65.
Formation & geological history
Formed in microcrystalline or macrocrystalline quartz veins, secondary deposits, or stream gravels through hydrothermal crystallization and subsequent water erosion and natural tumbling.
Uses & applications
Commonly collected as river pebbles, used for decorative landscaping, jewelry making, tumbling, and gemstone collections.
Geological facts
Quartz is one of the most abundant minerals on Earth's crust. Smooth, rounded quartz pebbles like this are formed when water action erodes quartz veins over long periods.
Field identification & locations
Identified by its hardness (scratches glass readily), light translucent yellowish color, smooth rounded pebble texture, and lack of distinct cleavage planes. Extremely common in stream beds, beaches, and gravel deposits worldwide.
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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