Book Description
The Cowichan Lake area lies at the southeastern end of the Vancouver Island Ranges and is characterized by fairly rugged topography accentuated by glaciation. The area is divided into two regions of differing structural style by a major thrust fault running along Cowichan Lake. This report introduces the geological setting of the areas and describes its lithology and stratigraphy, structure and tectonics from the Late Devonian to the Eocene, and the metamorphism and alteration of the area's sedimentary and igneous formations. The final section of the report reviews the history of mineral exploration in the area, outlines the regional metallogeny, and classifies the mineral deposits found in the area. The appendices include tabulated data, descriptions of mineral occurrences and fossils, and a summary of assessment report work recorded within the area.