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Gypsum is a relatively common mineral. It is used in construction as drywall and an ingredient in plaster and fertilizer. The name is derived from the Greek gypsos, meaning “chalk or plaster.” Gypsum is typically colorless to white, but due to impurities it can occur in shades of yellow, blue, pink, brown or gray. It commonly forms as flat, elongated prismatic crystals that are mostly transparent. Fed by a mineral rich solution that seeped through the rock, this sinuous specimen of gypsum grew from the wall of a cave. The “ramshorns” occurred as some crystal strands grew faster than others.

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  • Title: Sinuous Gypsum
  • Location: Baranca Del Cobre, Chihuahua, Mexico, North America
  • Type: Mineral
  • Rights: This image was obtained from the Smithsonian Institution. The image or its contents may be protected by international copyright laws. http://www.si.edu/termsofuse
  • External Link: View this object record in the Smithsonian Institution Collections Search Center
  • USNM Catalog Number(s): R13219
  • Photo Credit: Chip Clark, Smithsonian Institution National Museum of Natural History
  • Field: MIneral Sciences
Smithsonian National Museum of Natural History

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