
sedimentary
Lake Superior Agate
Silicon dioxide (chalcedony variety quartz)
Hardness of 7 on the Mohs scale; displays concentric banding in shades of red, orange, and brown due to iron oxide staining; waxy to vitreous luster; microcrystalline (cryptocrystalline) crystal structure; no cleavage; specific gravity of approximately 2.60 to 2.65.
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Physical properties
Hardness of 7 on the Mohs scale; displays concentric banding in shades of red, orange, and brown due to iron oxide staining; waxy to vitreous luster; microcrystalline (cryptocrystalline) crystal structure; no cleavage; specific gravity of approximately 2.60 to 2.65.
Formation & geological history
Formed roughly 1.1 billion years ago during the Keweenawan Rift Zone event. Mineral-rich hydrothermal fluids deposited silica in gas cavities within basaltic lava flows over long periods.
Uses & applications
Prized by rockhounds and lapidaries for polishing, tumbling, and crafting into jewelry and decorative items.
Geological facts
Lake Superior agates are the official state gemstone of Minnesota and are famous for their rich red and orange banding caused by oxidized iron, which reflects the region's ancient volcanic and glacial history.
Field identification & locations
Easily identified in the field by its characteristic concentric fortification banding, waxy luster, and reddish-brown iron-stained exterior. Commonly found in glacial drift, gravel pits, and beaches around the Lake Superior region.
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