Mariposite
Chromium-rich variety of mica

Mariposite is a mineral which is a chromium-rich variety of mica, which imparts an attractive green color to the generally white dolomitic marble in which it is commonly found. It was named for Mariposa, California, United States, though it can be found in several other places in the Sierra Nevada. It is also found in Marblemount, Washington, in the North Cascades, as well as in a few locations in Canada (Newfoundland, where it is called virginite, Ontario, and Quebec). Mariposite has also been found outside North America: in France, Austria, Spain, Sweden, China, Japan, Papua New Guinea, and Venezuela.
It is not recognized as a valid mineral by the International Mineralogical Association, but is a chromium-rich phengite, which is a high-silica variety of muscovite. It is the chromium that gives mariposite its distinctive green color.
The term "mariposite" also refers to the stone in which the green mica is found. This stone is metamorphic rock, containing varying amounts of dolomite and quartz. Larger proportions of quartz give it a more attractive, translucent appearance. It is used as a decorative construction material, in walls, monuments, and bridges. It is also made into jewelry.
01Chemical composition
The chemical formula of mariposite is K(Al,Cr)2(Al,Si)4O10(OH)2.


Sources and credits
This article is adapted from the Wikipedia article “Mariposite”, written by its contributors and licensed under CC BY-SA 4.0. Fathomly has changed the layout, removed citation markers, navigation and maintenance notices, and adjusted punctuation. This adapted version is shared under the same license. For references, see the original article.
Images, from Wikimedia Commons:
- Mariposite.jpg by Unknown author, CC BY-SA 3.0
- Mariposite monument Cathey's Valley.jpg by Unknown author, CC BY-SA 3.0
- Mariposite Cathey's Valley monument.jpg by Unknown author, CC BY-SA 3.0
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