Aegirine

Etymology

The name aegirine is derived from Ægir , a Norse mythological figure (god of the sea), as the mineral was first described from Norway.

A synonym for the mineral is acmite (from Greek ἀκμή "point, edge") in reference to the typical pointed crystals.

Chemistry and description

Aegirine is the sodium endmember of the aegirine–augite series.

It has the chemical formula NaFeSi2O6, in which the iron is present as the ion Fe3+. In the aegirine–augite series, the sodium is variably replaced by calcium with iron(II) and magnesium replacing the iron(III) to balance the charge. Aluminum also substitutes for the iron(III). Acmite is a fibrous green-colored variety.

Aegirine occurs as dark green monoclinic prismatic crystals. It has a glassy luster and perfect cleavage, "in two directions at near 90 degree angles". It is described on Mindat.org as "slightly resinous", with its colour "dark green to greenish black, reddish brown, [or] black" Its Mohs hardness is 6 and its specific gravity is between 3.5 and 3.6.

Associated minerals include augite, nepheline, andradite, baryte, quartz, spessartine, riebeckite, biotite, sodalite, and albite.

Occurrence

The acmite variety was first described in 1821, at Kongsberg, Norway, and the aegirine variety in 1835 for an occurrence in Rundemyr, Øvre Eiker, Buskerud, Norway.

This mineral commonly occurs in alkalic igneous rocks, nepheline syenites, carbonatites, and pegmatites. It also appears in regionally metamorphosed schists, gneisses, and iron formations; in blueschist facies rocks, and from sodium metasomatism in granulites. It may occur as an authigenic mineral in shales and marls. It occurs in association with potassic feldspar, nepheline, riebeckite, arfvedsonite, aenigmatite, astrophyllite, catapleiite, eudialyte, serandite, and apophyllite.

Major localities include Mont Saint-Hilaire, Quebec, Canada; Kongsberg, Norway; Narsarssuk, Greenland; Kola Peninsula, Russia; Magnet Cove, Arkansas, US; Kenya; Scotland, and Nigeria.

Aegirine also occurs in the syenite at the Bowral quarries in New South Wales, Australia, as described in a 1906 paper by geologist and later Antarctic explorer Douglas Mawson.

Uses

Aegirine is sometimes used as a gemstone.

References

References

1. Warr, L.N.. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine.
2. (2001). "Handbook of Mineralogy". Mineral Data Publishing.
3. "Aegirine".
4. "Aegirine Mineral Data".
5. Hurlbut, Cornelius S.; Klein, Cornelis, 1985, ''[https://archive.org/details/manualofmineralo00klei/page/n13/mode/2up Manual of Mineralogy]'', 20th ed., {{ISBN. 0-471-80580-7 (via [[Internet Archive]]
6. {{Cite EB1911
7. Dana, James Dwight. (1855). "Manual of Mineralogy". Durrie & Peck.
8. "AEGIRINE (Sodium Iron Silicate)".
9. (2 January 2016). "Pre-Antarctic Mawson in South Australia and western New South Wales". [[Informa UK]].
10. "The Minerals and Genesis of the Veins and Schlieren Traversing the Aegirine-Syenite in the Bowral Quarries". ''[[Proc. Linn. Soc. N.S.W.]]'', 381, pp. 580-607.
11. Manutchehr-Danai, Mohsen. (9 March 2013). "Dictionary of Gems and Gemology". Springer Science & Business Media.