Where it forms, where it's found
20recorded occurrences
Physical
- Colour
- Pink · purple · blue · white · colourless
Optical
- UV response
- In hackmanite, green fluorescence is thought to be caused by partial substitution of Na+ by Mn, while partial substitution of Al3+ by Fe3+ leads to red luminescence and orange fluorescence is caused by the S2− . Ce3+ causes the fluorescence spectra to show an emission peak around 340 nm, Eu2+ leads to violet fluorescence, and the s2-type ions are associated with blue fluorescence, while the association of Ti3+ with oxygen vacancies may also lead to blue fluorescence.[[2]]
Chemical composition
Synonyms
- Hackmanit
- Hackmanita
Literature, links & citation
Citations
- 1901Borgström, L.H. (1901) Mineralogiska Notiser. 4. Hackmanit ett nytt mineral i sodalitgruppen. Geologiska Föreningen i Stockholm Förhandlingar: 23: 7: 563-566
- 1903Borgström, L.H. (1903) Hackmanit, ein neues Mineral der Sodalithgruppe. Zeitschrift für Kristallographie und Mineralogie: 37: 284-285.
- 1903Borgström, L.H. (1903) Uvarovite and Hackmanite. Journal of the Chemical Society: 84: 2: 304.
- 1936Lee, O. Ivan (1936) A new property of matter: Reversible photosensitivity in hackmanite from Bancroft, Ontario. American Mineralogist, 21 (12) 764-776
- 2013Goettlicher, Joerg, Kotelnikov, Alexey, Suk, Natalya, Kovalski, Andrey, Vitova, Tonya, Steininger, Ralph (2013) Sulfur K X-ray absorption near edge structure spectroscopy on the photochrome sodalite variety hackmanite.
Cite this entry
@misc{mineral2026,
author = {Mineral Index editorial board},
title = {Hackmanite — Mineral Index},
year = {2026},
url = {https://mineralindex.org/minerals/hackmanite-1789},
note = {Accessed 2026-05-11}
}