Rhodochrosite

Rhodochrosite
General
CategoryCarbonate minerals
Formula
(repeating unit)
MnCO3
IMA symbolRds[1]
Strunz classification5.AB.05
Crystal systemTrigonal
Crystal classHexagonal scalenohedral (3m)
H-M symbol: (3 2/m)
Space groupR3c
Unit cella = 4.777, c = 15.67 [Å]; Z = 6
Identification
Formula mass114.95 g/mol
ColorPink, rose, rose-red, red, cherry-red, yellow, yellowish grey, grey, cinnamon-brown, white, may be banded; colourless to pale rose in transmitted light.
Crystal habitRhombohedral and scalenohedral crystals; also commonly bladed, columnar, stalactitic, botryoidal, granular or massive
TwinningOn {1012} as contact and lamellar
CleavageOn {1011} perfect; parting on {1012}
FractureUneven, conchoidal
TenacityBrittle
Mohs scale hardness3.5–4
LustreVitreous to pearly
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity3.7
Optical propertiesUniaxial (−)
Refractive indexnω = 1.814–1.816
nε = 1.596–1.598
Birefringenceδ = 0.218
Pleochroismweak
Ultraviolet fluorescenceNone
References[2][3][4]

Rhodochrosite is a manganese carbonate mineral with chemical composition MnCO3. In its pure form (rare), it is typically a rose-red colour,[5] but it can also be shades of pink to pale brown. It streaks white,[6] and its Mohs hardness varies between 3.5 and 4.5. Its specific gravity is between 3.45 and 3.6.[7] The crystal system of rhodochrosite is trigonal, with a structure and cleavage in the carbonate rhombohedral system. The carbonate ions (CO2−
3
) are arranged in a triangular planar configuration, and the manganese ions (Mn2+) are surrounded by six oxygen ions in an octahedral arrangement. The MnO6 octahedra and CO3 triangles are linked together to form a three-dimensional structure. Crystal twinning is often present. It can be confused with the manganese silicate rhodonite, but is distinctly softer.[8] Rhodochrosite is formed by the oxidation of manganese ore, and is found in South Africa, China, and the Americas.[6] It is one of the national symbols of Argentina.

Rhodochrosite forms a complete solid solution series with iron carbonate (siderite). Calcium (as well as magnesium and zinc, to a limited extent) frequently substitutes for manganese in the structure, leading to lighter shades of red and pink, depending on the degree of substitution. This is the reason for the pink color of rhodochrosite.

  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. ^ Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C., eds. (2003). "Rhodochrosite". Handbook of Mineralogy (PDF). Vol. V (Borates, Carbonates, Sulfates). Chantilly, VA, US: Mineralogical Society of America. ISBN 0962209740.
  3. ^ Rhodochrosite. Mindat.org
  4. ^ Rhodochrosite. Webmineral
  5. ^ Deer, William Alexander (1998). Rock-forming Minerals: Non-Silicates. Vol. 5B. Geological Society of London. pp. 150–152. ISBN 9781897799901.
  6. ^ a b Cairncross, Bruce (2015). Understanding Minerals & Crystals. Penguin Random House South Africa. p. 180. ISBN 9781775843344.
  7. ^ Ridgway, Robert Henderson (1933). Manganese: General Information. U.S. Department of the Interior, Bureau of Mines. p. 3.
  8. ^ Rhodonite. Mindat.org

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