Rock Identifier
Lake Superior Agate (Silicon Dioxide (Chalcedony / Quartz), SiO2) — gemstone
gemstone

Lake Superior Agate

Silicon Dioxide (Chalcedony / Quartz), SiO2

Hardness of 7 on the Mohs scale; colors range from red, orange, and brown due to iron oxide staining; waxy to vitreous luster; microcrystalline (cryptocrystalline) crystal structure; no true cleavage, exhibits conchoidal fracture; specific gravity around 2.60 to 2.65.

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Physical properties

Hardness of 7 on the Mohs scale; colors range from red, orange, and brown due to iron oxide staining; waxy to vitreous luster; microcrystalline (cryptocrystalline) crystal structure; no true cleavage, exhibits conchoidal fracture; specific gravity around 2.60 to 2.65.

Formation & geological history

Formed roughly 1.1 billion years ago during the Keweenawan rifting event in the Midcontinent Rift System. Silica-rich hydrothermal solutions filled gas cavities in basaltic lava flows, precipitating concentric layers of chalcedony over time.

Uses & applications

Prized by lapidaries and collectors for cutting, polishing, jewelry making, and display specimens.

Geological facts

Lake Superior agates are the official state gemstone of Minnesota and are famous for their rich red and orange banding, which is caused by the oxidation of iron trapped within the original volcanic host rock.

Field identification & locations

Found primarily in glaciated gravel deposits, riverbeds, and fields throughout the Upper Midwest of the United States (Minnesota, Wisconsin, Michigan, Iowa). Key identifiers include waxy luster, conchoidal fracture, and distinct concentric banding.