
mineral
Yellow Quartz / Chalcedony
Silicon Dioxide (SiO2)
Hardness of 7 on the Mohs scale, waxy to vitreous luster, translucent to semi-opaque, yellow to honey-brown color caused by iron inclusions, lacks distinct cleavage, conchoidal fracture.
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Physical properties
Hardness of 7 on the Mohs scale, waxy to vitreous luster, translucent to semi-opaque, yellow to honey-brown color caused by iron inclusions, lacks distinct cleavage, conchoidal fracture.
Formation & geological history
Formed through the precipitation of silica-rich hydrothermal fluids in cavities, veins, or sedimentary gravel beds. Common in alluvial and river deposit environments.
Uses & applications
Used widely in lapidary arts, jewelry, tumbled stones, pocket stones, and decorative rock collections.
Geological facts
Yellow quartz varieties often get their coloration from microscopic trace amounts of iron oxides like goethite or hematite distributed within the crystal structure.
Field identification & locations
Identified by its hardness (scratches glass), waxy luster when wet or polished, and translucency when held up to light. Commonly found in riverbeds, beach gravels, and pegmatite regions worldwide.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Soil with Mineral Detritus and Quartz Fragments
Regolith / Silicate Mineral Aggregate
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Limonite / Goethite (Iron Ore Mineral nodule)
FeO(OH)·nH2O / FeO(OH)
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Schist
Schist
Metamorphic
Septarian Pebble
Septarian nodule / Concretion
sedimentary
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
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