
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
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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.
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Arenite (SiO2 based)
sedimentary
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Epidote
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metamorphic
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
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Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
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