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  Formula: NaH(CO3)
  
  Carbonate
  
  Specific gravity: 2.21
  
  Hardness: 2½
  
  Streak: White
  
  Colour: Colourless, white, grey, buff
  
  Solubility: Readily soluble in water and glycerine
  
  Environments
  Nahcolite is naturally occurring sodium bicarbonate. It is found as a precipitate from hot springs, as 
  efflorescences around saline lakes and in brines, formed at a late stage in differentiated alkalic massifs, and as a 
  solid in liquid inclusions in a variety of other mineral species. Associated minerals include 
  trona, thermonatrite, 
  thénardite, halite, 
  gaylussite, burkeite, 
  northupite and borax 
  (HOM).
  
  Localities
  
  At the type locality, Mount Vesuvius, Metropolitan City of Naples, Campania, Italy, nahcolite has been found 
  in a lava tunnel associated with halite and 
  thénardite 
  (Mindat).
  
  Nahcolite from Mount Vesuvius - Image
  
  
  At Stufe di Nerone, Pozzuoli, Metropolitan City of Naples, Campania, Italy, in old Roman conduit, nahcolite 
  was found admixed with 
  trona and 
  thermonatrite as an efflorescence 
  (Dana). 
  
  At Little Mogadi Dry Lake, Kajiado County, Kenya, nahcolite occurs as fibrous 
  pseudomorphs 
  after gaylussite, and as alteration rims around 
  thermonatrite 
  (Dana). 
  
  
  At Searles Lake, San Bernardino County, California, USA, nahcolite occurs in thin beds associated with 
  gaylussite, thénardite, 
  burkeite, northupite, 
  borax and halite 
  (Dana). 
  
  Nahcolite from Searles Lake - Image
  
  At Anvil Points, Rifle, Garfield County, Colorado, USA, a number of underground openings have penetrated the 
  high-grade oil-shale facies that contain the cavities, some of which 
  were unleached and contain nahcolite, in crystalline, cleavable masses in concretions as large as five feet 
  across and as small as a pea. It also was found in layers up to four inches thick intercalcated between 
  oil-shale beds. The nahcolite in the concretions varies in 
  colour from colourless, through white, yellow, brown and black. Most often the colour is a dirty brown because of the 
  bitumen dispersed throughout the mineral. 
  
  The nahcolite occurring in the layers is pure white, translucent, and occurs as fibrous crystals at right 
  angles to the bedding. It has a pearly opalescence and resembles the satin spar variety of 
  gypsum 
  (AM 32.117-120).
  
  Nahcolite from Anvil Points - Image
  
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