Ikaite

Ikaite
Glendonite (calcite pseudomorph after ikaite)
General
CategoryCarbonate mineral, hydrous carbonates subgroup
Formula
(repeating unit)
CaCO3·6H2O
IMA symbolIka[1]
Strunz classification5.CB.25
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(same H-M symbol)
Space groupC2/c[2]
Identification
ColorWhite when pure
Crystal habitNearly square prism; pyramidal; sigmoidal: square prism capped with oppositely canted pyramids; massive, tubular (tinolite vr.)
Mohs scale hardness3
LusterDull
StreakWhite
Specific gravity1.83
Optical propertiesBiaxial (−)[3]
Refractive indexnα = 1.455
nβ = 1.538
nγ = 1.545[4]
Birefringenced = 0.090
Other characteristicsDecomposes into water and calcite above 8 °C[3]
References[2]

Ikaite is the mineral name for the hexahydrate of calcium carbonate, CaCO3·6H2O. Ikaite tends to form very steep or spiky pyramidal crystals, often radially arranged, of varied sizes from thumbnail size aggregates to gigantic salient spurs. It is only found in a metastable state and decomposes rapidly by losing most of its water content once removed from near-freezing water. This "melting mineral" is more commonly known through its pseudomorphs.

  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. ^ a b Mineralienatlas.
  3. ^ a b Ikaite. Webmineral.
  4. ^ Ikaite. Mindat.

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