Rock Identifier
Lake Superior Agate (Silicon Dioxide (SiO2) - Banded Chalcedony) — mineral
mineral

Lake Superior Agate

Silicon Dioxide (SiO2) - Banded Chalcedony

Hardness: 6.5-7 on Mohs scale; Color: Red, orange, white, tan, and brownish tones caused by iron inclusions; Luster: Waxy to vitreous; Crystal structure: Microcrystalline (trigonal); Cleavage: None, exhibits conchoidal fracture.

Hardness
6
Luster
Waxy to vitreous
Identified More mineral
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Physical properties

Hardness: 6.5-7 on Mohs scale; Color: Red, orange, white, tan, and brownish tones caused by iron inclusions; Luster: Waxy to vitreous; Crystal structure: Microcrystalline (trigonal); Cleavage: None, exhibits conchoidal fracture.

Formation & geological history

Formed approximately 1.1 billion years ago during the Midcontinent Rift System in North America. Silica-rich water deposited fine layers of quartz inside gas cavities (vesicles) of basaltic lava flows.

Uses & applications

Popular for lapidary work, jewelry (cabochons, pendants), decorative displays, and tumbling. Highly sought after by mineral collectors.

Geological facts

Lake Superior agate is the official state gemstone of Minnesota. Its rich red and orange colors are caused by varying amounts of iron oxidation.

Field identification & locations

Look for a polished, waxy exterior with fine concentric banding or peel-like layers of red, white, and orange, often found weathered along gravel pits, lake shores, and river beds in the Upper Midwest of North America.