A mountain miner parish whose surroundings are well known for several minerals. Deformed Cambrian-Ordovician gneiss, metaquartzite, granites, pegmatites and amphibolites. Mylonitic zone trending NNE controls intrusion of Tertiary calc-alkaline volcanics (trachyandesite). Lenses of hydrothermal breccia occupy semicicular arcs associated with domes and explosion breccias. Different alteration types include: argillization, sericitization+pyritization, silicification, propylization (chlorite+carbonate+hematite, +/- epidote, +/- pyrite).
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