Ice Age Floods National Geologic Trail
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CABINET GORGE DAM · WASHINGTON
360° · DRONE · 3D, SCHEDULED JUNE 2026
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Cabinet Gorge Dam

Cabinet Gorge Dam on the Clark Fork River sits near the single most consequential location in the entire Ice Age Floods story: the approximate site of the ice dam that created Glacial Lake Missoula. The Purcell Trench Lobe of the...

Location
Washington
48.087, -116.059
On the trail
Ice Age Floods NGT
WA · OR · ID · MT
Record
Documented site
scholarship integrated
Capture
June 2026
scheduled

Cabinet Gorge Dam on the Clark Fork River sits near the single most consequential location in the entire Ice Age Floods story: the approximate site of the ice dam that created Glacial Lake Missoula. The Purcell Trench Lobe of the Cordilleran Ice Sheet advanced down this valley and blocked the Clark Fork River near what is now the Idaho-Montana border, impounding a lake that grew to hold 500 cubic miles of water across 3,000 square miles of western Montana. When the ice dam failed -- an event that may have occurred 40 or more times over 2,500 years -- the lake's entire contents emptied through this narrow gorge in as little as 48 hours, producing the largest floods known to have occurred on Earth. Core samples taken during the dam's construction revealed multiple stages of ice damming and flooding, confirming the repeated catastrophic cycle. An AVISTA-maintained viewpoint at the dam includes Ice Age Floods interpretive signage and offers an excellent vantage point for pondering the most important question in flood geology: how exactly did an ice dam 2,000 feet thick fail catastrophically? Stand here and you stand at the trigger of the largest floods in Earth's history.

Site research

Status & accessibility

Cabinet Gorge Dam straddles the Idaho–Montana state line on the Clark Fork River, just east of Clark Fork, Idaho. The dam (Avista Utilities, 230 MW) is operational. A public overlook is accessible from a marked turnoff on Idaho Highway 200 east of Clark Fork. The overlook is free, open year-round, and best in spring during snowmelt high flows. The Cabinet Gorge Fish Hatchery (downstream) offers tours by arrangement.

Ice Age Floods context

Cabinet Gorge sits at the eastern end of the constriction where the Purcell Trench Lobe of the Cordilleran Ice Sheet repeatedly advanced south and west to dam the Clark Fork River, ponding Glacial Lake Missoula. Cores taken during the dam's construction in the 1950s revealed multiple stages of ice-dammed lake sediment and till, consistent with at least several dam-and-flood cycles at this exact location. The ice plug here typically rose around 2,000 feet (some estimates to 4,000 feet); when it failed, the entire impounded volume of Lake Missoula released through this gorge as the head of every Missoula flood. The narrowness of Cabinet Gorge is itself a flood-relevant feature: the constriction concentrated the discharge that subsequently spread across the Rathdrum Prairie and Channeled Scabland.

Recent research

Roy Breckenridge's "Mapping the Deluge: Sandpoint to Cabinet Gorge Dam" (Idaho Geological Survey Staff Report S-14-1) remains the field-trip standard. No new outburst-mechanism papers specifically targeting Cabinet Gorge since 2017; Balbas et al. (2017) sets the broader chronology at ~18.2 ± 1.5 ka for the largest flood and ~14.0–14.4 ka for the youngest.

IAFI presence

Strong. The IAFI Coeur du Deluge Chapter (Sandpoint) leads field trips along Highway 200 between Sandpoint and Cabinet Gorge, including boat trips up the Clark Fork River Delta to the historic dam location. The chapter is the most active interpretive presence for this segment of the trail.

Visitor info

Best May–June at peak runoff for dramatic flow over the spillway. Allow 30–60 minutes at the overlook. Pair with the Clark Fork Ice Dam site immediately west and the Lake Pend Oreille shoreline.

Sources

  • https://iafi.org/chapters/coeur-du-deluge-chapter/
  • https://iafi.org/must-see-floods-features-in-northern-idaho/
  • https://www.idahogeology.org/pub/Staff_Reports/2014/IGS_S-14-1.pdf
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 ↗
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