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Snow-covered summit of the Mount Hood volcano above a forested landscape

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Mount Hood's acidic crater lake has swelled to the size of 20 swimming pools. No cause for alarm yet

A seasonal meltwater lake in the crater of Mount Hood is much larger this year than in previous years, according to the USGS, and its water is acidic, pH 4, about ten times more acidic than black coffee. It is held back by a dam of decomposed rock. Where would the water spill out, and why is this not yet cause for alarm?

4 min readmin read5 verified sourcessourcesČeština
Photo: Walter Siegmund (talk) · CC BY-SA 4.0 · Wikimedia Commons · cropped

Nobody has measured the volume of the lake at the foot of the Coalman Glacier, just below the summit, but the order-of-magnitude estimate is roughly 50 000 cubic metres, about 20 Olympic swimming pools. A preliminary measurement showed slightly acidic water. The Cascade volcanoes nevertheless remain at their normal level, and the USGS does not expect any impact on inhabited places.

01Observation

What the USGS actually observed

USGS scientists noticed the change on 6 October 2026 during a routine helicopter flight and described it in the weekly Cascades Volcano Observatory report of Friday 23 October. This is not a new lake. It is a seasonal meltwater feature, only much larger this year.

A water sample taken in the week before the report of 23 October had a preliminary pH of 4, about ten times more acidic than black coffee. The USGS describes such conditions as mildly acidic.

The NORMAL alert level and the GREEN aviation colour code in the report of 23 October apply to all the Cascade volcanoes in Washington and Oregon, not to Mount Hood alone. Routine airborne gas measurements at Mount Hood showed normal background degassing.

What we know and what we do not
ItemStatusNote
The lake is larger than in previous yearsStatus: observedNote: on 6 October 2026 from a helicopter
Water volumeStatus: unknown, estimate onlyNote: on the order of 50 000 m³, about 20 Olympic swimming pools
Water pHStatus: preliminary measurementNote: pH 4 from a sample collected in the week before the report of 23 October
NORMAL and GREEN levelStatus: applies to the whole CascadesNote: not to Mount Hood alone
Based on the weekly report of the USGS Cascades Volcano Observatory of 23 October 2026.

02Good to know

A dam of weathered rock is holding for now

The lake sits in a basin between the rock formation Crater Rock, the cliffs running down from the summit and a feature called Devil's Kitchen. The latter forms a dam made of hydrothermally altered rock and glacial moraine. The USGS describes it as a long-lived feature that appears stable based on current observations.

Rocky crater and Crater Rock below the summit of Mount Hood
CraterThe basin below the summitThe rocky basin below the summit of Mount Hood with Crater Rock, where the seasonal meltwater lake collects. The picture shows the terrain of the crater, not this year's state of the lake.Photo: Baseball Bugs · Public domain · Wikimedia Commons · cropped

If all the water were released suddenly, the USGS says it could trigger a debris flow, a surge of mud and rubble that on volcanoes is called a lahar. It would run down the White River valley and could reach the bridge on Highway 35. The terrain would keep it out of the Sandy River valley and away from Timberline and Government Camp.

Diagram of the basin with the lake between Crater Rock and Devil's Kitchen and an arrow showing a possible flow down the White River valley
Schematic layout of the basin and the direction of a possible flow down the White River valley. The illustration is not to scale.
Gravel bed of the White River below Mount Hood
The White River valley below Mount Hood, along which a possible flow from the crater would run.Photo: Fredlyfish4 · CC BY-SA 4.0 · Wikimedia Commons

According to the USGS, Mount Hood is an active volcano close to fast-growing communities, recreation areas and transport routes, and so it poses an elevated risk. Over the past century the most damage to roads and bridges has come from flows on the White River, Newton Creek, Eliot Branch and Ladd Creek.

03Iceland

Sudden outbursts of water are known in Iceland too

After the Gjálp eruption at the turn of September and October 1996, glacial meltwater collected in the Grímsvötn caldera and burst out several weeks later, on 5 November 1996. Peak discharge reached 33 000 m³/s on the Gígjukvísl and 22 000 m³/s on the Skeiðará, a flow that would empty the entire Mount Hood lake in under two seconds. There, though, the meltwater was supplied by the eruption, whereas at Mount Hood it is seasonal meltwater.

04Glacier

The Coalman Glacier below the summit

The Coalman Glacier lies just below the summit on the southern side of the mountain. According to the Oregon Glaciers Institute, its area shrank by roughly 73 % between the '50s of the last century and the '20s of this one, and the last observation dates from 2021. That figure says nothing about the cause of this year's lake.

Area of the Coalman Glacier
PeriodArea
The '50s (20th century)0.210 km²
The '20s (21st century), last observed in 20210.057 km²
Based on the Oregon Glaciers Institute.

05What next

What to watch for in the weekly reports

The USGS, together with the Forest Service, the National Weather Service, Portland Mountain Rescue and other agencies, is preparing further measurements and an assessment of the lake's stability. The observatory promises further updates as conditions develop, so its weekly reports will be decisive. Fakt počasí's live tools have nothing to add here.

Sources5 sources · every number and claim in the article comes from them
  1. USGS Cascades Volcano Observatory, weekly report of 23 October 2026 (weekly report of 23 October 2026)
  2. Oregon Glaciers Institute
  3. USGS, Lahars and Debris Avalanches at Mount Hood, Oregon
  4. USGS, Hazards Summary for Mount Hood
  5. USGS, Vatnajökull Jökulhlaup (photo by Oddur Sigurðsson, Icelandic Meteorological Office) (photo by Oddur Sigurðsson, Icelandic Meteorological Office)

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