Ice Age Floods National Geologic Trail
Ice Age Floods National Geologic Trail
Rocky Butte in northeast Portland is the eroded core of a Boring Lava Field volcano that became an island when the Missoula Floods transformed Portland into a temporary inland sea. At peak flood stage, water rose to over 400 feet above modern sea level in the Portland Basin,...
Rocky Butte in northeast Portland is the eroded core of a Boring Lava Field volcano that became an island when the Missoula Floods transformed Portland into a temporary inland sea. At peak flood stage, water rose to over 400 feet above modern sea level in the Portland Basin, submerging everything except the highest hills and volcanic remnants like Rocky Butte. As the floodwaters swirled around the butte, they deposited a long tail of sediment in its lee -- a pendant bar that now forms the neighborhood of Rose City. The butte's resistant basalt core survived the floods' erosive force, though softer surrounding material was stripped away. From the summit viewpoint, which features WPA-era stone walls, you can see the Portland Basin stretching in every direction -- a flat expanse of flood deposits surrounded by the West Hills, with Mount Hood looming to the east. The viewpoint makes the flood geography suddenly obvious: every flat area visible was once beneath floodwater, and every protruding hill was an island. Rocky Butte is the most accessible place in Portland to visualize what the city looked like as a lakebed 15,000 years ago.
Free public access via NE Rocky Butte Road in Portland, OR. The summit park (Joseph Wood Hill Park) is open daily, sunrise–sunset, with the historic 1930s CCC/WPA stone parapet at the top. Parking is limited and the access road is narrow; no fees. Closed at posted hours overnight to discourage problem use.
Rocky Butte is a Boring Lava cinder cone (~285,000–300,000 years old) — older than the floods by orders of magnitude. Its relevance to the floods is as a flood-survivor: during the largest Missoula Flood pulses, water in the Portland basin reached roughly 400 feet deep, leaving Rocky Butte standing as an island above the flow. The eastern face shows the most flood-related erosion. Erratic boulders deposited on the butte's lower slopes during floods are documented in IAFI/NPS interpretive material, and terraces cut along the flanks record flood water levels. The summit gives one of the clearest views of the Portland-basin flood floor from above.
No site-specific recent research. Allen, Burns, and Sargent's Cataclysms on the Columbia and the more recent O'Connor 2020 review cover the regional Portland-basin flood depths.
Within the IAFI Lower Columbia Chapter's coverage area; occasional field trips include Rocky Butte as a Portland-basin viewpoint.
Best at sunrise or sunset for views of Mount Hood, Mount St. Helens, Mount Adams, and Mount Rainier from the stone parapet. Allow 30–60 minutes. Pair with Crown Point and Portland Women's Forum to traverse the western Gorge flood-corridor from rim to rim.
Every site along the trail will receive the full Terrain360 capture treatment: ground-level 360° panoramas, drone aerial imagery, and photogrammetry-based 3D models that visitors can spin in their browser. This page reserves the slots; the imagery flows in as field capture completes.
Ground-level 360° panorama, every step along the feature, captured by Terrain360 field crews.
Drone flyovers reveal the geometry of catastrophe — ripple marks, gravel bars, and scour patterns invisible from the ground.
Photogrammetry and Gaussian-splat models let visitors rotate, measure, and inspect features in detail-page WebGL viewers.