Between about 20 000 and 14 000 years ago, a tongue of the Cordilleran ice sheet blocked the Clark Fork valley in northern Idaho and held back a lake in the valleys of western Montana. Dozens of times, and probably more than a hundred, the ice failed and the lake burst out across eastern Washington and down the Columbia towards the Pacific. The floods scoured about 30 000 square kilometres of land and left a landscape so strange that geologists argued over it for some 40 years.
A dam that could float
The ice was about a kilometre thick where it crossed the valley, according to a 2020 review led by O’Connor. Behind it Glacial Lake Missoula grew to about 7 770 square kilometres and about 2 100 cubic kilometres of water, more than 600 m deep at its largest.
Ice floats, and that limits what a glacier can hold back. The US National Park Service puts the release point at about nine-tenths of the height of the ice, so when the lake was full most of the dam lay under water, not standing as a wall above it. In the version set out by Waitt in 1985, the glacier’s bed lifted once the lake reached about 600 m, water began to run underneath, and tunnels widened rapidly into a catastrophic outflow. Then the ice settled and the lake refilled. Other studies favour overtopping or tunnelling.
From Idaho to the Pacific
A flood lasted about a week. The fastest water approached 36 m per second, about 130 km/h. It spread over the plateau of eastern Washington, stripping tens of metres of pale loess from the dark basalt below and cutting canyons, cataracts and potholes. At Wallula Gap, a 3.2 km opening, it slowed and backed up into Lake Lewis. Near Kalama it backed up again into Lake Allison, about 120 m above present sea level as far as Eugene in Oregon. Icebergs rode the water: the Bellevue Erratic, a boulder of about 90 tons, was carried as much as 800 km.
Columbian mammoths lived in the path. Their bones are among the most frequent fossils in the fine flood silts, mostly at 300 to 380 m above sea level, near the top of Lake Lewis. People, in the area since 16 600 to 15 300 years ago, almost certainly witnessed the last of the floods, the 2020 review concludes.
How big they really were
Estimates of peak flow differ widely. O’Connor’s review gives about 20 million cubic metres per second near the lake’s outlet and 5 to 15 million through Wallula Gap, more than ten times the Bonneville flood of about 18 000 years ago. Other estimates for the largest flood are about 2.7 million, 13 times the flow of the Amazon.
Recent work has shrunk the canyon-cutting floods. Lehnigk and Larsen found in 2022 that calculations based on today’s canyons and high-water marks overestimate the discharge by more than 80 per cent. A 2024 study estimated 3.1 million cubic metres per second for the upper Grand Coulee, where floods removed 67.8 cubic kilometres of rock, and found that the largest canyons could have formed in about six floods or fewer.
The geologist nobody believed
In 1923, after fieldwork on the Columbia Plateau, Bretz coined the name Channeled Scabland and argued that massive flooding had carved it. That ran against the uniformitarian view of the time, and he could not yet say where so much water had come from. Pardee, who had described Glacial Lake Missoula in 1910, suggested to him in 1925 that a draining glacial lake could do it. At a meeting in Washington on 12 January 1927 other geologists presented competing theories, and a bitter debate followed for about 40 years. By the 1950s the evidence favoured him, and hydraulic research and NASA satellite images in the 1970s vindicated him further. In 1979, aged 96, Bretz received the Penrose Medal, the Geological Society of America’s highest award. “All my enemies are dead, so I have no one to gloat over,” he told his son.
Where the floods can still be read
The Ice Age Floods National Geologic Trail links sites in four states. Dry Falls is a scalloped cliff about 120 m high and 5.6 km long, and PBS’s NOVA describes floodwaters more than 75 m deep pouring over it. On Camas Prairie in Montana, ripples of gravel stand 5 to 15 m high, and on Mount Sentinel and Mount Jumbo above Missoula, faint lines mark the old shores.


