Valley of Ten Thousand Smokes — volcano
Captain Budd Christman, NOAA Corps. · Public domain

Valley of Ten Thousand Smokes

  • 2 min read
  • 58.394° N 155.385° W

Interesting facts

  • The 1912 eruption expelled about 30 times as much magma as the 1980 eruption of Mount St. Helens.
  • The blasts were heard as far away as Fairbanks and Juneau, and volcanic dust reached Wisconsin within two days and Algeria within two weeks.
  • Witnesses reported ball lightning near the ground, while severe static disrupted wireless transmissions across the region.
  • Rafts of floating pumice were still being seen in 1913 in Katmai Bay, about 240 kilometres away.
  • The vent lay about ten kilometres from Mount Katmai, yet magma drained from beneath Katmai, whose summit collapsed into a caldera some 600 metres deep.
  • Novarupta itself is a rhyolite lava dome about 90 metres high and 360 metres wide that plugged the vent as the eruption ended.
  • Pyroclastic flows filled the valley with about 11 cubic kilometres of pumice and ash in just 16 hours.
  • This was one of the few eruptions in recorded history to produce welded tuff, rock fused while still hot, which kept the fumaroles alive for some fifteen years.
  • In 1917, a metre below the surface of the ash, temperatures still reached 97 °C, and the escaping steam was 99.5 percent water vapour.
  • Apollo astronauts in training played what they called the Moon game here, planning traverses in unfamiliar terrain and radioing findings to geologists such as Gene Shoemaker.

Why it is worth it

In June 1912 a vent called Novarupta, on the Alaska Peninsula, produced the largest volcanic eruption of the twentieth century by volume, releasing roughly 13 cubic kilometres of magma in about sixty hours. Glowing flows of pumice and ash poured down the upper Ukak River valley and filled it to a depth of up to about 200 metres, burying some 100 square kilometres of forest and meadow. What had been an unnamed corridor used by Alutiiq travellers and grizzly bears became a flat, pale, lifeless plain – the Valley of Ten Thousand Smokes, in Katmai National Park and Preserve.

The name comes from the botanist Robert F. Griggs, who reached the valley in 1916 on an expedition for the National Geographic Society and found its floor pierced by uncountable fumaroles, where water trapped under the hot deposit was boiling off as steam. In 1916 he counted around a thousand plumes higher than 150 metres; a survey in 1918 recorded vent temperatures above 400 °C. As the deposit cooled, the steam faded – only a few hundred vents remained by 1929 and about ten by 1940. In 1918 the area was declared Katmai National Monument to protect the landscape the eruption had created. The same eruption caused the summit of nearby Mount Katmai to collapse into a caldera, setting off more than a hundred strong earthquakes.

The smokes are gone, but the landscape still feels freshly made. Vegetation has barely gained a foothold on the ash, and the River Lethe and Knife Creek have cut narrow gorges straight through the layered deposit, exposing its bands of pumice and welded tuff in vertical walls. Volcanoes of the Aleutian Range – Katmai, Trident, Mageik and others – surround the valley, and several remain active. In 1965 and 1966 NASA and the US Geological Survey brought groups of Apollo astronauts here for geology training; among them were Buzz Aldrin, Alan Bean, Edgar Mitchell, James Irwin, Charlie Duke, Gene Cernan and Harrison Schmitt, all of whom later walked on the Moon.

Getting there

The valley lies in the interior of Katmai National Park, on the Alaska Peninsula, about 440 km southwest of Anchorage. The nearest airport is King Salmon (AKN), about 80 km away, where the park has its headquarters. Katmai has no road connection to the rest of Alaska: visitors usually reach Brooks Camp by floatplane, and from there the park's only road runs about 32 km (20 miles) to an overlook at the edge of the valley.

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From the encyclopaedia

The Valley of Ten Thousand Smokes is a valley within Katmai National Park and Preserve in Alaska which is filled with ash flow from the eruption of Novarupta on June 6–8, 1912. Following the eruption, thousands of fumaroles vented steam from the ash. Robert F. Griggs, who explored the volcano's aftermath for the National Geographic Society in 1916, gave the valley its name, saying that "the whole valley as far as the eye could reach was full of hundreds, no thousands—literally, tens of thousands—of smokes curling up from its fissured floor."

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