Ice Age FloodsIce Age Floods National Geologic Trail
Home·Field notes·salmon glacier 56°11'19.6"N 130°03'16.5"W
Bretz-era field site

salmon glacier 56°11'19.6"N 130°03'16.5"W

film set location of john carpenter's the thing (1982)

Year documented
PNW Ice Sheet Margins
Category
Other
Coordinates
56.1888, -130.0546WGS84
Trail
Ice Age Floods NGTWA / OR / ID / MT

Original field notebook

film set location of john carpenter's the thing (1982)— PNW Ice Sheet Margins

This is one of more than 1,800 field sites cataloged in the early scabland surveys — the bedrock of the Ice Age Floods scientific record. The Bretz-era researchers walked the ground first; modern cosmogenic dating, LiDAR, and remote sensing have since extended and refined what they mapped.

Capture roadmap

What this site looks like once Phase 1 lands.

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.

360° panoramic

Walk the site in your browser

Ground-level 360° panorama, every step along the feature, captured by Terrain360 field crews.

Phase 1 target · June–July 2026
Drone aerial

Read the landscape from above

Drone flyovers reveal the geometry of catastrophe — ripple marks, gravel bars, and scour patterns invisible from the ground.

Phase 1 target · June–July 2026
3D photogrammetry

Spin the geology in your browser

Photogrammetry and Gaussian-splat models let visitors rotate, measure, and inspect features in detail-page WebGL viewers.

Phase 1 target · June–July 2026
What we know now

How modern science extended the record

Mapping ice sheet margins is critical for understanding the timing and extent of glacial lake formation. Modern cosmogenic dating and LiDAR surveys continue to refine the ice sheet chronology in the Pacific Northwest.

Researchers studying Pacific Northwest ice sheet margins mapped the extent of the Cordilleran Ice Sheet, whose advance and retreat controlled the damming of Glacial Lake Missoula and the release of the catastrophic floods.