Valley of Ten Thousand Smokes

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.[1] 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."

Griggs camp during the 1917 expedition clearly showing the numerous "smokes"
Knife Creek Gorge

Prior to the eruption, the area now called the Valley of Ten Thousand Smokes was an unremarkable and unnamed portion of the Ukak River valley. Although never permanently inhabited by humans, it served as a pass for the Alutiiq people, as well as animals such as grizzly bears.[2][3]

The 1912 eruption was the largest eruption by volume in the 20th century, erupting a magma volume of about 13 cubic kilometers (3.1 cu mi). As many as 14 major earthquakes between 6 to 7, and over 100 earthquakes greater than 5, resulted from the collapse of the caldera at Mount Katmai and movement within the magmatic plumbing system.[4][5]

River eroding volcanic ash flow, Valley of Ten Thousand Smokes
Canyon cut in ash by River Lethe

The ash-filled valley covers a 40-square-mile (100 km2) area.[6] The ash can be up to 700 feet (210 m) deep.[7] In places deep canyons have been cut by the River Lethe, allowing observers to see the ash flow strata. Since the ash has cooled, most of the fumaroles are now extinct and despite its name the valley is no longer filled with 'smoke' (i.e. steam).[6] Vegetation still does not grow in the valley.[8] The signs of volcanic activity are still visible on nearby hills.

Katmai's most recent eruption was in 1927, but there have been non-eruptive events as recent as 2003. The Alaska Volcano Observatory still monitors Katmai's activity as part of the Katmai Cluster, where there are 5 active stratovolcanos within 15 kilometers (9 mi) of Katmai.

Visitors to the valley most commonly arrive via bus along the 20-mile (32 km) road from Brooks Camp, which is the only road in Katmai Park. The valley is a source of creative exploration by photographers and naturalists.[9]

Geology

Basement rocks in the area consist of the Late Jurassic Naknek Formation, which is composed of siltstones, and arkosic sandstones 1.7-2 km thick deposited in a marine shelf and submarine fan delta environment during the Oxfordian-Tithonian. Some 20 dioritic and granodioritic Tertiary plutons pierce the formation. Most prevalent though are the Quaternary stratovolcanoes along the Aleutian Arc associated with the Aleutian subduction zone.[5]:17–18

The 1912 Novarupta eruption was characterized by three main episodes spanning 60 hours. Episode I included both a rhyolitic ignimbrite and a simultaneous Plinian dispersal of rhyolitic tephra fallout. The ignimbrite consisted of 9 separate packages of pumiceous pyroclastic flow deposits, radiating outward 9 km, and which filled 11 km3 of the valley to a depth of 100-200 m in the upper portion and 35 m in the lower over the span of 16 hours. It is indurated in the upper valley while nonwelded in the lower. The ignimbrite is noted for its fumaroles, phreatic craters, welded tuff, and flattened fiamme. At the same time, a Plinian dispersal of 8.8 km3 of rhyolitic tephra occurred depositing layers A and B. Episode II consisted of a second Plinian dispersal, but one consisting of dacite tephra, depositing 4.8 km3 of layers C and D. Episode III was also a Plinian dispersal of dacite tephra depositing 3.4 km3 of layers F and G.[5]:4–5,18–20,45–48,143–146

The explosion from the eruption was heard as far away as Fairbanks and Juneau, while earthquakes continued until mid-Aug. Ball lightning near the ground was noted in addition to regular thunder and lightning, rare in South Alaska, while severe static disrupted wireless transmissions. Volcanic dust reached Wisconsin on 8 June, Algeria on 19 June and California on 21 June. Fields of pumice were seen floating in Katmai Bay, 241 km to the southwest, in 1913. Griggs noted 1000 fumarolic plumes over 500 feet high in 1916. In 1917, diffuse steam emanations were still evident and temperatures were 97° C just 1 m below the surface. In 1918, Jasper Sayre and Paul Hagelbarger noted 86 vents with temperatures greater than 190° C, the hottest being 432° C. The steam was measured to be 99.5% water vapor with some acidic gases of HCL, CO2, H2S and HF. Only a few hundred emanations were seen by 1929, and just 10 were left by 1940.[5]:4–5,18–20,45–48,143–146

  • Time sequence of the 1912 Novarupta eruption showing three episodes of Plinian pumice falls over the span of 60 hours, and 9 packages of ignimbrite over the span of 16 hours
  • Sequence of 9 ignimbrite packages over the span of 16 hours during the 1912 Novarupta eruption
  • Contour lines, cm scale, showing accumulation of ash from 3 episodes of Plinian pumice falls over 60 hours during the 1912 Novarupta eruption
  • Funnel fumarole found in the valley
  • One of 60 phreatic craters, 20-60 m in diameter, with tuff rings and ejected welded ignimbrite
  • Springtime in the Valley of Ten Thousand Smokes

Astronaut training

The Katmai Peninsula in general, and the valley in particular, were used by NASA and the USGS to geologically train the Apollo astronauts in recognizing volcanic features, landforms and materials, especially fumaroles and vents. Two separate groups of astronauts trained here, the first in June-July 1965 and a second group in Aug. 1966. Their field exercises included simulating a lunar mission. "Playing the Moon game", involved pairing up astronauts and placing them in a location with very little prior information. They then planned traverses and collected representative samples. They communicated with their geologist instructors via radio. Astronauts who would use this training on the Moon included Apollo 11's Buzz Aldrin, Apollo 12's Alan Bean, Apollo 14's Edgar Mitchell, Apollo 15's James Irwin, Apollo 16's Charlie Duke, and Apollo 17's Gene Cernan and Jack Schmitt. Notable geologist instructors included Garniss Curtis and Gene Shoemaker.[10][11]

References
  1. "Valley of Ten Thousand Smokes Tour". Katmai National Park & Preserve. National Park Service. 2008-08-28. Retrieved 2009-01-14.
  2. "Valley of Ten Thousand Smokes and the 1912 Novarupta-Katmai Eruption - Katmai National Park & Preserve (U.S. National Park Service)". www.nps.gov. Retrieved 2017-10-27.
  3. Bodry, Catherine. "The Valley of Ten Thousand Smokes". Retrieved 2017-10-27.
  4. Hildreth, Wes; Firstein, Judy (2003). Geologic Map of the Katmai Volcanic Cluster, Katmai National Park, Alaska. USGS Geologic Investigations Series Pamphlet I-2778. pp. 15–16.
  5. Hildreth, W.; Fierstein, J. (2012). The Novarupta-Katmai eruption of 1912- largest eruption of the twentieth century; centennial perspectives. Reston: USGS Professional Paper 1791. p. 135.
  6. Scheffel, Richard L.; Wernet, Susan J., eds. (1980). Natural Wonders of the World. United States of America: Reader's Digest Association, Inc. p. 394. ISBN 0-89577-087-3.
  7. "The Valley of Ten Thousand Smokes in Katmai National Park and Preserve | Alaska Historical Society". alaskahistoricalsociety.org. Retrieved 2017-10-27.
  8. Harris, Ann G.; Tuttle, Esther; Tuttle, Sherwood D. (2004). Geology of National Parks. Kendall Hunt. ISBN 9780787299705.
  9. Freeburg, Gary (2012). Valley of 10,000 Smokes: Revisiting the Alaskan Sublime (First ed.). Staunton, VA: George F. Thompson Publishing. ISBN 978-1-938086-03-8.
  10. Phinney, William (2015). Science Training History of the Apollo Astronauts. NASA SP -2015-626. pp. 63–65, 189, 192, 222, 224.
  11. Bennett, Bo (2000). Rods & Wings. Anchorage: Publication Consultants. pp. 165–168. ISBN 9781888125627.

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