
mineral
Tumbled amber-colored chalcedony (likely carnelian or yellow agate)
Microcrystalline quartz, SiO₂; likely iron-bearing chalcedony
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; translucent honey-yellow to orange-brown, waxy to vitreous luster, cryptocrystalline quartz with no visible cleavage. The smooth, glossy surface indicates tumbling or polishing.
Identified More mineral →
Explore Tumbled amber-colored chalcedony (likely carnelian or yellow agate) in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness 6.5–7 Mohs; translucent honey-yellow to orange-brown, waxy to vitreous luster, cryptocrystalline quartz with no visible cleavage. The smooth, glossy surface indicates tumbling or polishing.
Formation & geological history
Forms when silica-rich groundwater fills cavities and fractures, with iron impurities producing yellow, orange, or red coloration; commonly Cenozoic to older volcanic-hosted deposits.
Uses & applications
Used as a lapidary stone for cabochons, beads, carvings, and inexpensive jewelry; also collected as an ornamental gemstone.
Geological facts
Carnelian is typically orange-red, while yellow varieties are often sold as yellow agate or citrine-colored chalcedony. Heat treatment can intensify orange coloration.
Field identification & locations
Identify by its fine-grained, glassy/waxy appearance, lack of cleavage, and ability to scratch ordinary glass; chalcedony feels cooler and harder than plastic or resin. Common sources include Brazil, India, Uruguay, Madagascar, and the United States.
More like this
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