Deception Pass Park Foundation

On a geological timescale, Cranberry Lake is a relatively recent addition to Deception Pass.  Around 15,000 years ago, during the Fraser Glaciation, the Puget Sound region was covered by a lobe of the Cordilleran Ice Sheet.  In some places, the sheet was over 3,000 feet thick.  The basin of Cranberry Lake was one of many regional geological features carved by the retreat of the ice sheet roughly 14,000 years ago.

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