Utah's Great Salt Lake now occupies a portion of the land area once covered by Lake Bonneville.Stark evidence of the flood remains in the form of smooth displaced boulders (melon gravels scablands and gravel bars.

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Its most vulnerable point was a natural dam of alluvial material blocking Red Rock Pass in southeastern Idaho.The lake eventually attained a surface area roughly equal to modern Lake Michigan, and a depth of more than 1,000 feet, because it had no natural drainage outlets.More information and photos: Lake Bonneville Flood, basalt boulders tumbled by Bonneville Flood - "Melon Gravel").

Over time about 1,000 cubic miles of water roared through the Snake River Canyon and emptied into the Columbia River near Pasco,.Unlike Lake Missoula, ice dams were not an issue at Lake Bonneville.