Lake Superior agate | |
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![]() Lake Superior agate from Duluth, Minnesota | |
General | |
Category | Tectosilicate minerals, quartz group, chalcedony variety, agate variety |
Formula | SiO2 (silicon dioxide) |
Crystal system | Trigonal (quartz) or monoclinic (moganite) |
Identification | |
Color | Red, orange, pale yellow, brown, white, grey, rarely blue |
Crystal habit | Cryptocrystalline silica |
Cleavage | None |
Fracture | Conchoidal, with very sharp edges |
Mohs scale hardness | 6.5–7 |
Luster | Waxy, vitreous when polished |
Streak | White |
Diaphaneity | Translucent to opaque |
Specific gravity | 2.58–2.64 |
Density | 2.6 g/cm³ |
Refractive index | 1.530–1.540 |
Birefringence | Up to +0.004 (B-G) |
Pleochroism | Absent |
Common impurities | Iron oxides (goethite, hematite, limonite)[1] |
Lake Superior agate is a type of agate found primarily near the shores of Lake Superior. It can also be found in interior regions of the U.S. states of Minnesota, Michigan, Wisconsin, Iowa, Nebraska, Kansas, and Missouri, and in the Canadian province of Ontario. As a gemstone, it is valued by collectors for its vibrant, iron-colored bands in shades of red and orange, but they may also be white, grey, pale yellow, or brown. Believed to be the world's oldest agates,[2] Lake Superior agates formed within the basaltic lava flows left behind from the Midcontinent Rift about 1.1 billion years ago. They are not named after the lake, but rather the Lake Superior Till, a Pleistocene glacial deposit in which they can be found.[3] In 1969, the Lake Superior agate was designated by the Minnesota Legislature as the official state gemstone.[4]
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