Ice Age Floods National Geologic Trail
Home·Sites·Columbia Plateau Trail North End
Columbia Plateau Trail North End Washington
Site profile

Columbia Plateau Trail North End

Stretching 130 miles along an abandoned railroad grade, the Columbia Plateau Trail is the longest rails-to-trails conversion in Washington state and traverses the heart of the Channeled Scablands. The northern end near Cheney places hikers...

Location
Washington
47.522, -117.517
On the trail
Ice Age Floods NGT
WA · OR · ID · MT
Record
Documented site
scholarship integrated
Capture
June 2026
scheduled

Stretching 130 miles along an abandoned railroad grade, the Columbia Plateau Trail is the longest rails-to-trails conversion in Washington state and traverses the heart of the Channeled Scablands. The northern end near Cheney places hikers and bikers directly in the Cheney-Palouse scabland tract, where the Missoula Floods carved a braided network of channels through millions of years of basalt bedrock in a matter of days. The trail follows the flood's path across terrain that looks like it was clawed by a giant hand: deep channels separated by sharp-edged basalt ridges, pothole lakes filling scour depressions, and scattered glacial erratics dropped by melting icebergs. Walking or cycling this trail, you traverse one of the most complete sequences of flood-carved terrain anywhere, from the initial scabland channels near Cheney through progressively larger flood features as you head south toward the Columbia River. The flat railroad grade makes the trail accessible to all abilities while passing through some of the most dramatic geology in the Pacific Northwest. This is perhaps the best way to experience the scablands at a human pace.

Site research

Status & accessibility

The Columbia Plateau Trail State Park is a 130-mile rail-trail along the abandoned Spokane, Portland and Seattle Railway corridor between Fish Lake (just outside Cheney, Washington) and the Columbia–Snake confluence at Pasco. The north end runs from Fish Lake Trailhead Regional Park to Cheney as a 3.75-mile paved segment, then continues south unpaved. A Discover Pass is required at staging areas. The trail passes through Turnbull National Wildlife Refuge for about 4.75 miles, which is a fee-managed refuge. Open year-round; the paved segment is also used for cross-country skiing and snowshoeing in winter.

Ice Age Floods context

The north end of the Columbia Plateau Trail crosses the eastern fringe of the Channeled Scabland, the landscape carved by Missoula flood waters that diverted south after being blocked by the Okanogan Lobe and Glacial Lake Columbia. Around Cheney and Fish Lake, the trail crosses flood-scoured basalt benches, drainless coulees, and the headward eroded scarps of the scabland's eastern tract. The Cheney–Spokane area was on the inflow side: Lake Missoula's outburst waters spilled across the Rathdrum Prairie and through the Spokane Valley into the scabland tract that this trail traverses.

Recent research

Balbas et al. (2017) places the largest floods at ~18.2 ± 1.5 ka and the last Missoula floods at ~14.7 ± 1.2 ka via 10Be cosmogenic dating. The O'Connor et al. (2020) review remains the regional synthesis.

IAFI presence

The IAFI Cheney-Spokane Chapter is the responsible chapter and is one of IAFI's most active chapters in field-trip programming. Eastern Washington University (Cheney) hosts the IAFI's digital records archive.

Visitor info

Spring (March–May) and fall (September–October) are best; summer heat and limited shade can be punishing. The Fish Lake to Cheney paved segment is the most family-friendly entry; the unpaved miles south of Cheney are best by bike or horse. Pair with Turnbull NWR for wildlife and the Cheney-area scabland geology overlooks.

Sources

  • https://parks.wa.gov/find-parks/state-parks/columbia-plateau-state-park-trail
  • https://www.wta.org/go-hiking/hikes/columbia-plateau-trail
  • https://en.wikipedia.org/wiki/Columbia_Plateau_Trail
How we will interpret it

What the June trip captures here.

Three vantages no single photograph can hold, the same treatment that made Dry Falls legible.

360° · ON THE GROUND
Walk the site

Ground-level panoramas along the feature, so the scale of the flood landscape is something you stand inside.

DRONE · THE FORM ★
Read it from above

An aerial reveals the geometry of catastrophe: scour, channels, and bars that are invisible at eye level.

3D · PHOTOGRAMMETRY
Spin the geology

A model of a key outcrop you can rotate and measure in the browser, the rock itself, on the page.

Capture window mid-June through mid-July 2026 · slots fill on this page as the campaign delivers.

Loading map…

Flood-extent overlay shows the maximum reach of the Missoula Floods.

On the trail

The site in its place along the flood path, with the maximum flood extent drawn over the modern map.

View on the interactive map Cinematic timeline · 3D flood · every captured site
Sources & attribution
IAFIIce Age Floods Institute, geologic context
T360Terrain360, immersive capture scheduled June 2026
NPSIce Age Floods National Geologic Trail
LINKExternal media · open ↗
All the sites
Captured, and coming this summer.
Browse all sites →