
sedimentary
Lake Superior Agate
Silicon Dioxide (Chalcedony variety)
Hardness of 6.5 to 7 on the Mohs scale, exhibits distinct concentric banding patterns in red, brown, and yellow tones, vitreous to waxy luster, microcrystalline (cryptocrystalline) crystal structure, conchoidal fracture with no true cleavage, and a specific gravity around 2.6
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Physical properties
Hardness of 6.5 to 7 on the Mohs scale, exhibits distinct concentric banding patterns in red, brown, and yellow tones, vitreous to waxy luster, microcrystalline (cryptocrystalline) crystal structure, conchoidal fracture with no true cleavage, and a specific gravity around 2.6
Formation & geological history
Formed roughly 1.1 billion years ago during the Keweenawan rifting event in the Midcontinent Rift System, where mineral-rich hydrothermal fluids filled gas cavities in basaltic lava flows
Uses & applications
Popularly used as a gemstone in jewelry, lapidary art, and highly sought after by rockhounds and mineral collectors
Geological facts
Lake Superior agates are the official gemstone of the US state of Minnesota, and their characteristic red and orange banding is caused by oxidized iron within the ancient volcanic environment
Field identification & locations
Identified primarily by its bold, concentric fortification bands and rich iron-oxide coloration; commonly found in glacial drift, gravel pits, and along the shores of Lake Superior and surrounding Midwestern US states
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