Rock Identifier
Fairburn Agate (Cryptocrystalline Quartz (SiO2) with trace Iron Oxides) — mineral
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
Identified More mineral
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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.