Celestine (mineral) explained

Celestine
Category:Sulfate minerals
Formula:SrSO sometimes contains minor calcium and/or barium
Imasymbol:Clt[1]
Strunz:7.AD.35
System:Orthorhombic
Class:Dipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)
Symmetry:Pnma
Unit Cell:a = 8.359 Å,
b = 5.352 Å,
c = 6.866 Å; Z = 4
Color:White, pink, pale green, pale brown, black, pale blue, reddish, greyish; colourless or lightly tinted in transmitted light
Habit:Tabular to pyramidal crystals, also fibrous, lamellar, earthy, massive granular
Cleavage:Perfect on, good on, poor on
Fracture:Uneven
Tenacity:Brittle
Mohs:3.0–3.5
Luster:Vitreous, pearly on cleavages
Refractive:nα = 1.619–1.622 nβ = 1.622–1.624 nγ = 1.630–1.632
Opticalprop:Biaxial (+)
2V:Measured: 50°–51°
Birefringence:δ = 0.011
Dispersion:Moderate r < v
Pleochroism:Weak
Fluorescence:yellow, white blue (both short and long UV)
Streak:white
Gravity:3.95–3.97
Diaphaneity:Transparent to translucent
References:[2] [3] [4] [5]

Celestine (the IMA-accepted name)[6] or celestite[1] is a mineral consisting of strontium sulfate (SrSO). The mineral is named for its occasional delicate blue color. Celestine and the carbonate mineral strontianite are the principal sources of the element strontium, commonly used in fireworks and in various metal alloys.

Etymology

Celestine derives its name from the Latin word caelestis meaning celestial[7] which in turn is derived from the Latin word caelum meaning sky, air, weather, atmosphere and heaven.[8]

Occurrence

Celestine occurs as crystals, and also in compact massive and fibrous forms. It is mostly found in sedimentary rocks, often associated with the minerals gypsum, anhydrite, and halite. On occasion in some localities, it may also be found with sulfur inclusions.

The mineral is found worldwide, usually in small quantities. Pale blue crystal specimens are found in Madagascar. White and orange variants also occurred at Yate, Bristol, UK, where it was extracted for commercial purposes until April 1991.[9]

The skeletons of the protozoan Acantharea are made of celestine, unlike those of other radiolarians which are made of silica.

In carbonate marine sediments, burial dissolution is a recognized mechanism of celestine precipitation.[10] It is sometimes used as a gemstone.[11]

Geodes

Celestine crystals are found in some geodes. The world's largest known geode, a celestine geode 35feet in diameter at its widest point, is located near the village of Put-in-Bay, Ohio, on South Bass Island in Lake Erie. The geode has been converted into a viewing cave, Crystal Cave, with the crystals which once composed the floor of the geode removed. The geode has celestine crystals as wide as 18inches across, estimated to weigh up to 300lb each.

Celestine geodes are understood to form by replacement of alabaster nodules consisting of the calcium sulfates gypsum or anhydrite. Calcium sulfate is sparingly soluble, but strontium sulfate is mostly insoluble. Strontium-bearing solutions that come into contact with calcium sulfate nodules dissolve the calcium away, leaving a cavity. The strontium is immediately precipitated as celestine, with the crystals growing into the newly formed cavity.[12] [13] [14]

See also

External links

Notes and References

  1. Warr . L.N. . 2021 . IMA–CNMNC approved mineral symbols . Mineralogical Magazine . 85 . 3 . 291–320 . 10.1180/mgm.2021.43 . 2021MinM...85..291W . 235729616 . free .
  2. Web site: Celestine . Lexikon . Mineralien Atlas – Fossilien Atlas . mineralienatlas.de . en, de . 2022-09-25.
  3. Book: Celestine . Handbook of Mineralogy . RRUFF™ Database Project . University of Arizona Department of Geology . http://rruff.geo.arizona.edu/doclib/hom/celestine.pdf.
  4. Web site: Celestine . Mindat.org .
  5. Web site: Celestine . Webmineral . data .
  6. Web site: List of Minerals . 21 March 2011.
  7. Celestine . Collins English Dictionary . collinsdictionary.com .
  8. Celestial . 24 April 2024 . Merriam-Webster Dictionary . merriam-webster.com .
  9. Web site: Beneath our feet . Discover Yate's History . Yate Heritage Centre . yateheritage.co.uk .
  10. Baker . Paul A. . Bloomer . Sherman H. . 1988 . The origin of celestite in deep-sea carbonate sediments . Geochimica et Cosmochimica Acta . 52 . 2 . 335–339 . 1988GeCoA..52..335B . 10.1016/0016-7037(88)90088-9 .
  11. Book: Roger . Dedeyne . Ivo . Quintens . 2007 . Tables of Gemstone Identification . Glirico . 978-90-78768-01-2 . 174.
  12. Anenburg . Michael . Bialik . Or . Vapnik . Yevgeny . Chapman . Hazel . Antler . Gilad . Katzir . Yaron . Bickle . Mike . 2014 . The origin of celestine-quartz-calcite geodes associated with a basaltic dyke, Makhtesh Ramon, Israel . Geological Magazine . 151 . 5 . 798–815 . 10.1017/S0016756813000800 . 2014GeoM..151..798A . 129529427 .
  13. Carlson . Ernest . 1987 . Celestite replacements of evaporites in the Salina Group . Sedimentary Geology . 54 . 1–2 . 93–112 . 10.1016/0037-0738(87)90005-4 . 1987SedG...54...93C .
  14. Kile . Daniel . Dayvault . Richard . Hood . William . Hatch . H. Steven . 2015 . Celestine-bearing geodes from Wayne and Emery counties, southeastern Utah: Genesis and mineralogy . Rocks & Minerals . 90 . 4 . 314–337 . 10.1080/00357529.2015.1034489 . 2015RoMin..90..314K . 130452012 .