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Magnesite on Serpentine
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Collection |
John Betts - Fine Minerals |
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Description |
Translucent white Magnesite crystals lining a slender cavity in greenish Serpentine. The Magnesite is a secondary mineral formed from the decomposition of the serpentine, the bedrock underlying Staten Island. No damage. From John Betts' personal collection; collected ca. 1996. |
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Locality |
Abandoned I-278 highway exit, north of Deere Park, Staten Island, New York City, Richmond County, New York. |
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Dimensions |
6 x 3 x 2 cm. |
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Specimen Grade |
B |
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Photograph |
© www.johnbetts-fineminerals.com
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