Rick Thompson's Research in Portland, Oregon; Vancouver, Washington; and the Willamette Valley, Oregon.
It has been written that there is not much to see of the Lake Missoula Floods in Oregon. My research shows that there is plenty to see once we know where to look and what to look for. I concentrate on the largest of the floods because it did the most to reshape the land.
I first looked into the Lake Missoula floods as they tore through the Columbia River Gorge, shaping Beacon Rock, carving the cliffs at Cape Horn and overtopping Crown Point.
It next shot between Woodburn Hill and Prune Hill in the area of Camas, Washington, scooping out what is now Lacamas Lake and literally filling the Vancouver basin with rocks, gravel and sand all the way from Camas to LaCenter.
South of where the Columbia River now flows the Lake Missoula Flood carved the sides off of Chamberlain Hill, Rocky Butte and other east Portland volcanoes, left gravel bars as high as 300 feet and as much as eleven miles long. Between the buttes it cut channels that are now the pathways for highways, streets, railroad tracks and bicycle trails.
When the Lake Missoula floodwaters were impounded by an ice log jam near Kalama, Washington, it flooded south as far as Eugene, Oregon, cutting channels like Lake Oswego, Carver Gap and the Oregon City gap leaving tons of sediment and erratic boulders that had ridden in on icebergs that dotted the shores of the temporary lake.
Geologists have named this “Glacial Lake Allison” after an early 20th century geologist who did much research and documentation on the geology of the Willamette Valley.
My Lake Allison map, on the right, shows the water
depths in 100 foot increments during the height of the largest
Lake Missoula Flood. This map took over three years to create
and is extremely detailed.
Lake Missoula Flood Research