Obsidian from the Mount Garibaldi area is exposed about 15 kilometres northeast of Squamish. The obsidian is part of the Ring Creek lava flow and is dated as Late Wisconsin in age. The rock is pitchy, black in colour, strong and brittle and generally uniform. Microscopic examination indicated that the composition is (CANMET Investigative Report 78-206):
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90% glass
8% feldspar
1% muscovite
1% magnetite and hematite
This obsidian is reported to have good potential as a pozzolan for use in the cement industry. It is considered that potential for similar obsidian deposit exists within the recent volanic flows of the area.