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tschermakite belongs to the hornblende group of calcic amphiboles, and is a rock-forming mineral found in basic igneous rocks and their high-grade metamorphic equivalents. The symbol at the start of the formula indicates that the crystal lattice includes an empty space (that is, not occupied by an atom), known as a vacancy.
there are two documented occurrences of tschermakite from Wales, both from the Llŷn. The modern amphibole classification scheme (see Leake et al., 1997) relies on chemical analyses of amphiboles rather than optical properties alone, it is therefore likely that other as yet un-analysed occurrences of tschermakite will be added to the localities listed below.