Hostname: page-component-848d4c4894-wzw2p Total loading time: 0 Render date: 2024-05-13T09:10:13.358Z Has data issue: false hasContentIssue false
  • English
  • Français

Schultenite from King County, Washington, USA; a second occurrence, and review

Published online by Cambridge University Press:  05 July 2018

R. Falls ,
B. Cannon  and
J. A. Mandarino
R. Falls
Affiliation:
Department of Mineralogy and Geology, Royal Ontario Museum, 100 Queen's Park, Toronto, Ontario, Canada M5S 2C6
B. Cannon
Affiliation:
Bart Cannon Minerals, 1041 NE 100 Street, Seattle, Washington, USA 98125
J. A. Mandarino
Affiliation:
Department of Mineralogy and Geology, Royal Ontario Museum, 100 Queen's Park, Toronto, and Department of Geology, University of Toronto, Toronto, Ontario, Canada M5S 2C6
Get access Rights & Permissions [Opens in a new window]

Abstract

Schultenite, PbHAsO4, known only from Tsumeb, Namibia, has been identified from a second occurrence: near North Bend, King County, Washington, USA. It occurs as euhedral crystals in a quartz-arsenopyrite-galena vein. It has a measured density of 6.07(3) g/cm3 and a calculated density of 6.079(4) g/cm3. The white to colourless crystals have a white streak, adamantine lustre, and fluoresce dull yellow under long wave ultraviolet light. Schultenite is monoclinic. Pa or P2/a; the unit cell parameters refined from the X-ray powder diffraction data are: a 5.827(3), b 6.743(3), c 4.847(3) Å, β 95.34(5)°; V 189.6(1) Å3; Z = 2; a:b:c = 0.8642:1:0.7188. The forms {010}, {001}, and {3̄22} were observed on the Washington schultenite crystals.

Keywords

schulteniteKing CountyWashington
Type
Research Article
Information
Mineralogical Magazine , Volume 49 , Issue 350 , March 1985 , pp. 65 - 69
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1985 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Claringbull, G. F. (1950) Mineral. Mag. 29, 287-90.Google Scholar
Embrey, P. G., and Hicks, R. P. (1977) Mineral. Rec. 8, 98-9.Google Scholar
Hänni, H. A., Stern, W. B. and Glor, M. (1978) Am. Mineral. 63, 213-15.Google Scholar
McDonnell, C. C., and Smith, C. M. (1916) J. Am. Chem. Soc. 38, 2030-3.Google Scholar
Mandarino, J. A. (1979) Can. Mineral. 17, 71-6.Google Scholar
Mandarino, J. A. (1981a) Ibid. 19, 441-50.Google Scholar
Mandarino, J. A. (1981b) Ibid. 19, 531-4.Google Scholar
Mellor, J. W. (1929) A Comprehensive Treatise on Inorganic and Theoretical Chemistry, 9, 193-4. Longmans, Green & Co., Ltd., London.Google Scholar
Morris, M. C., McMurdie, H. F., Evans, E. H., Paretzkin, B., de Groot, J. H., Newberry, R., Hubbard, C. R., and Carmel, S. J. (1977) Standard X-ray Diffraction Powder Patterns, NBS Monograph 25, Section 14, US Nat. Bur. Standards, Washington.Google Scholar
Palache, C., Berman, H., and Frondel, C. (1951) The System of Mineralogy, Vol. II, 661-3. John Wiley & Sons, New York.Google Scholar
Schulten, A. de (1904) Bull. Soc. Minkral. 27, 109-23.Google Scholar
Spencer, L. J. (1926) Mineral. Mag. 21, 149-55.Google Scholar