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Magnesiohornblende crystals from altered diorite from the Sarn Complex, Ll?n. Viewed under the microscope in crossed polarized light. National Museum of Wales specimen (NMW 93.12G). © National Museum of Wales.
magnesiohornblende is an amphibole, more specifically a calcic amphibole which occurs as a rock-forming mineral in basic igneous rocks and as amphibolite grade metamorphic rocks.
as with many other ferro-magnesian minerals, magnesiohorneblende has only been confirmed from a few localities in Wales, and there are even fewer analyses presented in the literature. It is quite likely that it is more abundant than these reports reflect.