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Strandlines of Glacial Lake Columbia

View on map:47.924484°N 118.877367°W

Comments

"Strandlines (old shorelines) from Glacial Lake Columbia are etched into the hillsides in this area. At 2400ft, these are the highest elevation strandlines recognized for Glacial Lake Columbia." (see reference) 

Description


Location of Glacial Lake Columbia in Washington, USA.

Glacial Lake Columbia was the lake formed on the ice-dammed Columbia River behind the Okanogan lobe of the Cordilleran Ice Sheet when the lobe covered 500 square miles (1,300 km) of the Waterville Plateau west of Grand Coulee in central Washington state during the Wisconsin glaciation.[1] Lake Columbia was a substantially larger version of the modern-day lake behind the Grand Coulee Dam. Lake Columbia's overflow – the diverted Columbia River – drained first through Foster Coulee, and as the ice dam grew, through first Moses Coulee, and finally, the Grand Coulee.[2][3]

References

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