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Articles By Discover Geological Consultants

The Prospect Valley low-sulphidation epithermal gold mineralization hosted within a hanging wall sequence of amygdaloidal basalt, andesitic basalt and andesite.

The Prospect Valley property lies within the Southern Intermontane Tectonic Belt of the Canadian Cordillera. Lithologies within the Prospect Valley region include successions of Mesozoic (248-65 Ma) to Tertiary (65-1.8 Ma) volcanic and sedimentary rocks, which have been intruded by plutons of various compositions and ages from Late Triassic and/or Jurassic to Miocene(?). Locally thick deposits of Pleistocene and recent glacial till and alluvium are prevalent in all the major creek or river valleys.

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