CORDILLERAN ICE SHEET - GLACIAL LAKES MISSOULA & COLUMBIA |
Between 15,000 and 12,800 years ago we were in the last throes of the Ice Age and nearing the end of the Pleistocene Epoch. The Cordilleran Ice Sheet expanded southward into northern Washington, Idaho, and Montana.
A massive sheet of ice 4000 feet thick, the Cordilleran Ice Sheet had three main lobes: The Puget Lobe which scoured out the Puget Sound, the Okanogan Lobe which blocked the Columbia River at the site of the present day Grand Coulee Dam forming Glacial Lake Columbia, and the Purcell Lobe.
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