Almandine crystals with plagioclase feldspar. Almandine garnets are abundant at the location, both as bands in feldspar, and with muscovite mica. The specimen is 12 x 13 cm, and the largest crystal is just over 2 cm in diameter.
The garnets from the primary pegmatites in the general Evje/Iveland area are all of intermediate composition between almandine and spessartine, often with some Y2O3.Most of then have Mn>Fe and can be called spessartine. At the Steli quarry the almandine component has been dominant in the analysed samples.
The garnets from the primary pegmatites in the general Evje/Iveland area are all of intermediate composition between almandine and spessartine, often with some Y2O3.Most of then have Mn>Fe and can be called spessartine. At the Steli quarry the almandine component has been dominant in the analysed samples.
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Photo added: 31st Mar 2009