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Nitromagnesite

Cave Name:

Great Cave, Kentucky, USA

Speleothems:

  • -

Other occurrence:

  • transparent stalactites (7.5 cm long) (Independence Cave, Botswana)

  • small saline efflorescence on dolomite walls and floor blocks (Elephant, Uisib I and Kimberlite Caves, Namibia)

  • white crusts (Gâuab Aas Cave, Namibia)

First description of cave occurrence:

  • Larsen, E.S. 1921. The microscopic determination of the nonopaque minerals. U.S. Geological Survey Bulletin 679, 266pp

First description of non-cave occurrence:

  • Shepard, C.U. 1835. Nitromagnesite. in Treatise on Mineralogy: Second Part, Volume II Hezekiah Howe & Co. New Haven: 85

Other cave locations & References:

  • Independence Cave, Botswana: Anonymous 1980. Botswana 1979. South African Speleological Association Bulletin 1: 3-9

  • Elephant, Uisib I and Kimberlite Caves, Namibia: Martini, J. (pers. comm in Hill, C. & Forti, P. 1997. Cave Minerals of the World (2nd ed.). National Speleological Society, Huntsville AL, 464p)

  • Pulo di Molfetta caves, Apulia, Italy: Forti, P. & Palmisano, G. 1989. I nitrati del Pulo di Molfetta: mineralogia e meccanismi genetici. Atti 15 Congrezo Nazionale di Speleologia (Castelanna 1987): 229-250

  • Torch, Wolkberg, West Driefontien, Fountains and Chaos Caves, South Africa: Martini, J.E. & Kavalieris, I. 1978. Mineralogy of the Transvaal caves. Transactions of the Geological Society of South Africa 81: 47-54

  • Sophienhöhle, Germany: Hubbart, D.A., Herman, J.S., Mitchell, R.S. & Hammerschidt, E. 1991. Salpetre in four European caves: chemical, historical and mineralogical aspects (abs.). Natl. Speleol. Soc. Bull. 53(1): 25

Conservation and Protection:

  • Samples must be preserved in very dry conditions

IMA status: Approved

Group: Nitrates

Chemical formula:
[According to the official IMA-CNMNC List of Mineral Names (http://nrmima.nrm.se/imalist.htm)]

Mg(NO3)2·6H2O

Deposition and stability:

  • The source of nitrate is usually the bat guano (or in exceptional cases - an olive orchad above the cave (through capilarity), e.g. Pulo di Molfetta, Italy), quick evaporation causing the deposition of the mineral

  • In some caves, the minerals does not crystalised within the caves, but was obtained from the leachates from the soil (e.g. the caves from South Africa, that from Germany)

  • Very soluble in water. At high humidity it deliquesces and dissapears

Color: white or yellow
Mineral assemblage:
  • Associated with gypsum, as part of white crusts (caves in Namibia) or in dry cave soils (caves of South Africa)

  • Minor component (6-9%) of niter flower and crusts in Pullo di Molfetta, Italy

Crystal system:
  • Monoclinic


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Cave_mineral_ | by Dr. Radut