Ice Age Floods National Geologic Trail
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SYLVAN LAKE · WASHINGTON
360° · DRONE · 3D, SCHEDULED JUNE 2026
awaiting field capture · this frame fills with the real scene
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Sylvan Lake

Sylvan Lake in eastern Washington is an outdoor classroom for Ice Age Floods evidence, hosting a remarkable concentration of features that tell the story from multiple angles. The lake's shores display ice-rafted glacial erratics --...

Location
Washington
47.320, -118.555
On the trail
Ice Age Floods NGT
WA · OR · ID · MT
Record
Documented site
scholarship integrated
Capture
June 2026
scheduled

Sylvan Lake in eastern Washington is an outdoor classroom for Ice Age Floods evidence, hosting a remarkable concentration of features that tell the story from multiple angles. The lake's shores display ice-rafted glacial erratics -- boulders carried from distant mountain ranges by icebergs floating in the floodwaters -- alongside giant ripple marks and flood-deposited sediments. Ringed craters, formed by kolk vortices that drilled into the bedrock, dot the surrounding terrain. The site's variety of features makes it particularly valuable for understanding the floods' diverse effects: erosion, deposition, and ice-rafting all happened simultaneously as the chaotic flood currents swept across this area. The erratics are especially compelling -- touch a granite boulder sitting on basalt bedrock and you are touching a rock that traveled hundreds of miles in a floating iceberg before being stranded when the water receded. Sylvan Lake rarely appears on tourist itineraries, making it a hidden gem for flood enthusiasts who want to see multiple lines of evidence in one compact location. The quiet setting also makes it an excellent place for reflection on the extraordinary events that shaped this landscape.

Site research

Status & accessibility

Public-web searches across Wikipedia, NPS, IAFI, and the City of Tualatin do not surface a site called "Sylvan Lake" on the Ice Age Floods National Geologic Trail or in standard Tualatin-area trail inventories. The name appears in the Portland area only as a residential pond/private feature near Sylvan-Highlands (off US-26 west of downtown Portland) and unrelated parks (e.g., Sylvan Lake State Park in Colorado). No current public status, hours, or access information could be verified.

Ice Age Floods context

If the intended site is the Sylvan area west of Portland, it lies above the highest Missoula-flood inundation contour (~400 feet asl in the Willamette Valley), so the floods did not directly inundate it. If the intended site is a privately held feature within the Tualatin floodplain, that area was inundated more than 40 times during flood maxima, with depths up to about 400 feet at peak, leaving erratics, slackwater silts (Willamette Silt / Lacustrine Pleistocene Silts), and the broad flat valley floor visitors see today. Without confirmation of the specific feature intended, the most defensible statement is that no published Ice Age Floods trail interpretation for "Sylvan Lake" could be located.

Recent research

No updates found because the site itself could not be definitively identified. Regional Willamette Valley flood-deposit work (O'Connor and Baker 2020; Bjornstad and Kiver 2012, updated) continues to refine the chronology and extent of slackwater deposition.

IAFI presence

No IAFI chapter, panel, or named partnership for a "Sylvan Lake" site could be located. The Lower Columbia Chapter covers the broader Willamette Valley including Tualatin and adjacent communities.

Visitor info

Cannot confirm. Recommend cross-checking the original IAFI/NPS source list, this entry may be a misnaming, a private/non-public feature, or an alternate label for an item already covered elsewhere in this batch (e.g., Tualatin Heritage Center or Tualatin Ice Age Walking Trail).

Sources

  • https://www.nps.gov/iafl/planyourvisit/oregon-state.htm
  • https://www.tualatinoregon.gov/community/ice-age-floods
  • https://iafi.org/category/places-things/oregon/
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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