Axotomous antimony glance — is a partially obsolete, now trivial name under which at least two related minerals from the subclass of sulfosalts (complex sulfides),[1]: 16 containing antimony, lead and sulfur were known in mineralogy and mineragraphy. Moreover, all three words in the title had meaningful meaning from the point of view of scientific terminology.
| Axotomous antimony glance | |
|---|---|
 Bournonite (Potosí, Bolivia) | |
| General | |
| Category | Mineral |
- Axotomic, axotomous (German: axotomatisch) — meant that the mineral had a so-called perfect cleavage in a certain direction, giving a plane of easy fracture.[2]: 10
- Antimony — meant that the mineral contains a significant amount of antimony and is of interest as a natural mineral stibnite of one or more metals.
- Glance — meant not just the presence of a metallic luster (shine) on the surface of a mineral, but, first of all, belonging to a broad morphological group of minerals, the so-called glances.
Interpretationen und Versionen
editIn his “Treatise on mineralogy” of 1825, also called “The natural history of the mineral kingdom”, Friedrich Mohs gave only two mineralogical synonyms for axotomous antimony glance: Prismatoidal Antimony-Glance or Grey Antimony (with the note: “in part”),[3]: 26 since the latter name, including also the longer version gray antimony ore, often also meant other ores, primarily stibnite.[1]: 311
Mohs indicated an unequal-sided tetrahedral pyramid as the main crystalline form for antimony luster, and its cleavage, no doubt, was very perfect — axotomic (according to the basic definition of a mineral).[3]: 26 The chemical formula of the mineral was not given, but in the afterword to In describing the mineral, Mohs noted that “nothing as yet known” about the proportions of the individual components of this mineral species, except that it contains sulfur, antimony and lead: “The axotomous Antimony-glance seems to be a rare mineral, or at least not sufficiently attended to by mineralogists. It occurs in masses of considerable dimensions in Cornwall, sometimes along with the di-prismate Copperglance.”[3]: 27
Ten years later, James Dana, in his new system of mineralogy, returned to the question of the composition and properties of this mineral, calling it jamesonite or axotomic antimony glance. Among the properties of the mineral, James Dana especially notes a typical analytical reaction: “before the blowpipe, in an open tube, it affords a dense white smoke of oxyd of antimony”. Having indicated the detailed percentage composition of the content of individual elements in the mineral (according to Heinrich Rose), however, he does not provide a formula, noting that jamesonite “it occurs principally in Cornwall, associated with quartz and minute crystals of Bournonite”. [4]: 420–421
In 1856, the English mineralogist James Tennant in his fundamental reference book “Mineralogy and Crystallography”, summing up the development of science until the middle of the 19th century, gives only one (main) synonym for the mineral jamesonite — axotomous antimony glance, providing its chemical formula 3PbS + 2SbS3, prismatic and a brief listing of mineralogy and crystallographic properties. At the end there is a short explanation from the field of analytical chemistry: “<jamsonite> decomposed by warm hydrochloric acid, forming same of lead”, as well as an important clarification: “found sometimes with bournonite”.[5]: 501
Essential minerals
edit- Bournonite[6]: 285 (also berthonite, volchite or dystomic glance)[1] — mineral of the subclass of complex sulfides, composition copper-lead sulfoantimonide with the calculation formula CuPbSbS3.
- Jamesonite[7]: 24 [8]: 501 (also domingite, comuccite, pfaffite, gray antimony or feather ore)[1] — mineral of the subclass of complex ribbon sulfides, according to the composition of iron-lead sulfoantimonide with the calculation formula Pb4FeSb6S14.[9]
Gallery
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See also
editReferences
edit- ^ a b c d Krivovichev V. G. Mineralogical glossary. Scientific editor A. G. Bulakh. — St.Petersburg: St.Petersburg Univ. Publ. House. 2009. — 556 p. — ISBN 978-5-288-04863-0
- ^ F. Yu. Levinson-Lessing. Petrographic Dictionary. — Leningrad-Moscow: State Scientific and Technical Geological and Petroleum Publishing House, 1932. — 462 p.
- ^ a b c Friedrich Mohs, Wilhelm Haidinger. Treatise on mineralogy, or, The natural history of the mineral kingdom. — Edinburgh, Printed for A. Constable; London, 1825.
- ^ James Dwight Dana A. M. A System of Mineralogy: Including an Extended Treatise on Crystallography; With an Appendix, Containing the Application of Mathematics to Crystallographic Investigation, and a Mineralogical Bibliograph. — New Haven. Published by Durrie & Peck and Herrick & Noyes, 1837
- ^ James Tennant. Mineralogy and Crystallography. Being a classification of crystals, according to their form and an arrangement of minerals after their chemical composition. — London: Houlston and Stoneman, 1856.
- ^ Robert Jameson. Manual of Mineralogy: containing an account of simple minerals, and also a description and arrangement of mountain rocks. — Edinburgh, Archibald Constable & Co., 1821. — 494 p.
- ^ Thomas Egleston, Ph. D. Catalogue of Minerals and Synonyms. — Washington: Government Printing Office, 1887.
- ^ David Thomas Ansted, Walter Mitchell. Geology, Mineralogy, and Crystallography: Being a Theoretical, Practical, and Descriptive View of Inorganic Nature The Form and Classification of Crystals, and a Chemical Arrangement of Minerals. — London, Houlston and Stoneman, 1855. — 590 p.
- ^ Jamesonite generally has a very large number of synonyms, as well as regional and trivial names, which is unusual even for such noticeable minerals from a practical point of view. First of all, this is the already mentioned above domingite, comuccite, pfaffite, gray antimony or feather ore. In addition, jamesonite is also known by its English names: warrenite, wolfsbergite, plumite, rosellan, rosenite, sakharovaite, bleiantimonit, antimonial radiant glance, warrenite, falkmanite... In the old German mineralogical literature the following names for jamesonite were also found: lumpenerz, stahlantimonglanz, spiessglasfedererz, chalybinglanz, zundererz. Moreover, the term “axotomous antimony glance” until the beginning of the 19th century was considered scientific in the mineralogical environment and was predominant.
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