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rapidcreekite

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Also known as IMA1984-035

Rapidcreekite is a rare mineral with formula Ca2(SO4)(CO3)·4H2O. The mineral is white to colorless and occurs as groupings of acicular (needle-shaped) crystals. It was discovered in 1983 in northern Yukon, Canada, and described in 1986. Rapidcreekite is structurally and compositionally similar to gypsum.

Wikidata facts

Subclass of
sulfate mineral
Image
Rapidcreekite - Rapid Creek, Yukon.jpg
Show 7 more facts
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
7.DG.20
Nickel-Strunz 9th edition (updated 2009)
7.DG.20
Commons category
Rapidcreekite
streak color
white
IMA Mineral Symbol
Rck
chemical formula
Ca₂(SO₄)(CO₃)·4H₂O
Sources (2)

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Encyclopedic overview

6 sections
Contents
  • Description
  • Structure
  • History
  • Occurrence
  • References
  • External links

{{Infobox mineral | name = Rapidcreekite | category = Sulfate mineralsCarbonate minerals | boxwidth = | boxbgcolor = | image = Rapidcreekite - Rapid Creek, Yukon.jpg | imagesize = 260px | caption = Rapidcreekite from the Rapid Creek area, Yukon, Canada | formula = Ca2(SO4)(CO3)·4H2O | IMAsymbol = Rck | molweight = | strunz = 7.DG.20 | dana = 32.2.1.1 | system = Orthorhombic | class = Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) | symmetry = Pcnb | unit cell = a = 15.517(2) Å b = 19.226(3) Å c = 6.1646(8) Å; Z = 8 | color = White to colorless | habit = Elongated, flattened to acicular crystals in radiating sprays or crust forming | twinning = | cleavage = Perfect on {010}Good on {100} | fracture = Splintery | tenacity = Brittle | mohs = 2 | luster = Vitreous | polish = | refractive = nα = 1.516nβ = 1.518nγ = 1.531 | opticalprop = Biaxial (+) | birefringence = δ = 0.015 | 2V = 45° (measured) | dispersion = None | pleochroism = | fluorescence= Non-fluorescent | absorption = | streak = White | gravity = 2.239 (calculated) | density = | melt = | fusibility = | diagnostic = | solubility = Dissolves slowly in 10% HCl | diaphaneity = Transparent | other = | references = }} Rapidcreekite is a rare mineral with formula Ca2(SO4)(CO3)·4H2O. The mineral is white to colorless and occurs as groupings of acicular (needle-shaped) crystals. It was discovered in 1983 in northern Yukon, Canada, and described in 1986. Rapidcreekite is structurally and compositionally similar to gypsum.

==Description== thumb|left|White crystals of rapidcreekite with quartz from the Rapid Creek area Rapidcreekite is transparent and white to colorless. The mineral occurs as isolated clusters or pervasive crusts of radiating sprays of acicular crystals up to in length.

Excerpted from Wikipedia’s “rapidcreekite” article, available under the CC BY-SA 4.0 licence.

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