
mineral
Fairburn Agate
Cryptocrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Multi-colored bands (reds, yellows, oranges, whites, greys); Luster: Waxy to vitreous; Crystal Structure: Trigonal/Monoclinic microcrystals; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Multi-colored bands (reds, yellows, oranges, whites, greys)
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 Mohs; Color: Multi-colored bands (reds, yellows, oranges, whites, greys); Luster: Waxy to vitreous; Crystal Structure: Trigonal/Monoclinic microcrystals; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
Formation & geological history
Formed as ancient silica-rich groundwater deposited layers within cavities of limestone or volcanic hosts, primarily during the Pennsylvanian and Permian periods (approx. 250-300 million years ago), later weathering out into alluvial deposits.
Uses & applications
Highly prized as a state gemstone of South Dakota; used in lapidary work, jewelry, and by mineral collectors.
Geological facts
Designated as the South Dakota State Gemstone in 1966. They are world-renowned for their unique, sharp-angled 'fortification' patterns and vibrant color contrasts.
Field identification & locations
Identified by unique fortification banding and weather-worn 'holly-leaf' exterior texture. Primarily found in the Fairburn Agate Beds of the Black Hills/Badlands region in South Dakota and parts of Nebraska/Wyoming.
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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
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Granite
Granite (Phaneritic intrusive igneous rock)
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Septarian Pebble
Septarian nodule / Concretion
sedimentary