
mineral
Fairburn Agate
Cryptocrystalline Quartz (SiO2) with trace Iron Oxides
Hardness: 6.5-7 (Mohs), Color: red, white, orange, and gray bands, Luster: Waxy to vitreous, Crystal Structure: Microcrystalline, Cleavage: None (conchoidal fracture)
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs), Color: red, white, orange, and gray bands, Luster: Waxy to vitreous, Crystal Structure: Microcrystalline, Cleavage: None (conchoidal fracture)
Formation & geological history
Formed during the Mississippian Period about 330 million years ago within limestone cavities. They are sedimentary-hosted agates often found in river beds and gravel deposits after eroding from their host rock.
Uses & applications
Used primarily as a gemstone for jewelry, lapidary art, and as a highly sought-after collector's item due to unique fortification patterns.
Geological facts
The Fairburn Agate is the official state gemstone of South Dakota. It is named after the town of Fairburn, SD, where it was first discovered in the Black Hills.
Field identification & locations
Identified by sharp, angular 'fortification' bands and vibrant color contrasts. Found in the Buffalo Gap National Grasslands and southern Black Hills. Collectors look for 'holly leaf' or star-shaped banding patterns.
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Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral