Rock Identifier
Lake Superior Agate (Silicon Dioxide (SiO2) with iron impurities) — mineral
mineral

Lake Superior Agate

Silicon Dioxide (SiO2) with iron impurities

Hardness: 7 on Mohs scale; Color: Red, orange, and white banding; Luster: Vitreous to waxy; Crystal structure: Trigonal/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.60-2.65

Hardness
7 on Mohs scale
Color
Red, orange, and white banding
Luster
Vitreous to waxy
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale; Color: Red, orange, and white banding; Luster: Vitreous to waxy; Crystal structure: Trigonal/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.60-2.65

Formation & geological history

Formed roughly 1.1 billion years ago during the Midcontinent Rift System. As lava cooled, gas bubbles created cavities which were later filled by silica-rich groundwater and iron oxides, creating distinct concentric bands.

Uses & applications

Primarily used for lapidary work, jewelry (cabochons), and as a highly sought-after collectible specimen. It is the official state gem of Minnesota.

Geological facts

Lake Superior Agates are unique because they were distributed across large areas of the Midwest by glaciers during the last ice age, rather than remaining in their volcanic source rock.

Field identification & locations

Identify in the field by looking for translucent waxy surfaces, distinct 'fortification' banding, and a pitted 'peel' or husk. Commonly found on beaches of Lake Superior, gravel pits, and riverbeds in Minnesota, Wisconsin, and Michigan.