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

Lake Superior Agate

Silicon Dioxide (Chalcedony / Quartz, SiO2)

Hardness of 6.5 to 7 on the Mohs scale, waxy to vitreous luster, distinct concentric banding in shades of red, orange, and yellow (caused by iron oxidation), conchoidal fracture, and no true cleavage.

Identified More sedimentary
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Physical properties

Hardness of 6.5 to 7 on the Mohs scale, waxy to vitreous luster, distinct concentric banding in shades of red, orange, and yellow (caused by iron oxidation), conchoidal fracture, and no true cleavage.

Formation & geological history

Formed roughly 1.1 billion years ago during the Keweenawan Rift Zone volcanism. Groundwater rich in silica and iron percolated through gas cavities in basalt flows, depositing layers of microcrystalline quartz over millions of years.

Uses & applications

Widely used in jewelry, lapidary arts, and highly prized by rockhounds and mineral collectors.

Geological facts

The Lake Superior agate is the official state gemstone of Minnesota. The vibrant red and orange colors are a hallmark of iron oxide staining unique to the region's geological history.

Field identification & locations

Found primarily in gravel pits, riverbeds, and beaches around the Lake Superior region in North America. Look for waxy luster, translucent banding, and iron-stained exterior pitting when searching in the field.