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Some time during a 10–15 million-year period, lava flow after lava flow poured out, eventually reaching a thickness of more than 1.8 km (5,900 ft).
As the molten rock came to the surface, the Earth's crust gradually sank into the space left by the rising lava.
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Erosion resulting from the Missoula Floods has extensively exposed these lava flows, laying bare many layers of the basalt flows at Wallula Gap, the lower Palouse River, the Columbia River Gorge and throughout the Channeled Scablands.
The Columbia River Basalt Group is thought to be a potential link to the Chilcotin Group in south-central British Columbia, Canada.
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The lava, as it flowed over the area, first filled the stream valleys, forming dams that in turn caused impoundments or lakes.