Johnbaumite Explained

Johnbaumite
Category:Apatite group
Formula:Ca5(AsO4)3OH
Imasymbol:Jbm[1]
Strunz:08.BN.05
Dana:41.08.03.03
System:Hexagonal
Class:Dipyramidal (8/m)
Symmetry:P63/m
Colour:Greyish white to colourless
Habit:Anhedral grains, granular minerals without the expression of crystal shapes and massive, uniformly indistinguishable crystals forming large masses.
Cleavage:Distinct
Fracture:Irregular/Uneven
Tenacity:Brittle
Mohs:≈ 4.5
Luster:Adamantine to greasy on fracture surfaces, vitreous on cleavage surfaces
Streak:White
Density:3.65 – 3.73 g/cm3
Opticalprop:Uniaxial (−)
Refractive:nω = 1.687 nε = 1.684
Birefringence:0.003
Pleochroism:Non-pleochroic
Extinction:Parallel
Diaphaneity:Transparent
References:[2] [3]

Johnbaumite is a calcium arsenate hydroxide mineral. It was first described in 1980, where it appeared in Franklin Township, Somerset County, New Jersey.[4] Johnbaumite was discovered at Harstigen mine in Sweden in the 19th century, but it was described as svabite.[5]

Etymology

It is named after geologist John Leach Baum (March 15, 1916 – October 16, 2011), who found the original specimen in 1944. He was a significant contributor to the geology and mineralogy of the Franklin deposit, and the Curator Emeritus at the Franklin Mineral Museum.

See also

Further reading

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: Johnbaumite . webmineral.com . 17 June 2022.
  3. Web site: Johnbaumite . Mindat.org . 17 June 2022.
  4. Pete J. Dunn, Donald R. Peacor, Nancy Newberry; Johnbaumite, a new member of the apatite group from Franklin, New Jersey. American Mineralogist 1980;; 65 (11–12): 1143–1145. doi:
  5. Cristian Biagioni, Marco Pasero; The crystal structure of johnbaumite, Ca5(AsO4)3OH, the arsenate analogue of hydroxylapatite. American Mineralogist 2013;; 98 (8–9): 1580–1584. doi: https://doi.org/10.2138/am.2013.4443