
mineral
Lake Superior Agate
Banded Chalcedony / Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Red, orange, white, tan, and gray bands; Luster: Waxy to vitreous; Crystal Structure: Trigonal/Microcrystalline; Cleavage: None, conchoidal fracture; Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Red, orange, white, tan, and gray bands
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Red, orange, white, tan, and gray bands; Luster: Waxy to vitreous; Crystal Structure: Trigonal/Microcrystalline; Cleavage: None, conchoidal fracture; Specific Gravity: 2.58-2.64
Formation & geological history
Formed during the Mesoproterozoic era about 1.1 billion years ago in the North American Midcontinent Rift System. Silica-rich fluids deposited layers of microcrystalline quartz within gas cavities (vesicles) of volcanic basalt lava flows.
Uses & applications
Popular as a lapidary gemstone, used for jewelry, cabs, carvings, and highly sought after by rock collectors.
Geological facts
The Lake Superior Agate is the official state gemstone of Minnesota, designated in 1969. It is characterized by rich iron-stained color variations and fine, distinct fortification banding.
Field identification & locations
Identified by intricate fortification banding, waxy texture, and iron oxide color accents. Found around Lake Superior, particularly along beaches and gravel pits in Minnesota, Wisconsin, Michigan, and Iowa.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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