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Updated: May 7, 2025
The magnetite is somewhat decomposed, the resulting hematite filling the spaces between the quartz grains. 15 Anorthosite Shore of Lake Michikamau. A coarse grained rock of dark gray color, in which labradorite is the chief mineral. Magnetite and Kaolin are present in small quantities.
The western end of Kasheshebogamog Lake lies within the limit of the anorthosite area, which extends from that point to Lake Michikamau, a direct distance of twenty miles and was the only anorthosite observed on the journey.
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