Griggs

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Facts


  • Official Name: Mount Griggs
  • Seismically Monitored: Yes
  • Color Code: GREEN
  • Alert Level: NORMAL
  • Elevation: 2317m (7601ft)
  • Latitude: 58.3572
  • Longitude: -155.1037
  • Smithsonian VNum: 312190
  • Pronunciation:
  • Nearby Towns:
    • Karluk 59 mi (96 km) SE
    • King Salmon 61 mi (98 km) NW
    • Kanatak 64 mi (104 km) SW
    • Larsen Bay 70 mi (113 km) SE
    • Igiugig 73 mi (117 km) NW

    Distance from Anchorage: 268 mi (431 km)

Description

From Wood and Kienle (1990) [1] : "A spectacular, little-dissected cone, Mount Griggs towers 1,700 m above the north margin of the Valley of Ten Thousand Smokes, its summit only 10 km north of Novarupta. Uniquely among the stratovolcanoes of the Katmai district, it lies 10 km behind (northwest of) the remarkably linear (N66E-trending) volcanic front defined by Martin, Mageik, Trident, Katmai, and Snowy Mountain centers.
"Griggs's truncated summit is an expression of 3 concentric craters, the outermost of which is 1.5 km wide, breached to the southwest, and filled by a semi-annulus of ice wrapped around a young central cone containing the nested inner craters. The main outer crater probably originated by early Holocene collapse, and formation of a 1-cubic km-scale debris avalanche, remnants of which survive on the lower west-southwest flank and across the valley on Broken Mountain. Much of the amphitheater was subsequently filled by the nested inner cone. Outer slopes of the main and inner cones expose a few scoria flows and local scoria falls but principally consist of complexes of the thin brecciated lava tongues, overlapping and bifurcating in the manner so characteristic of summit-fed andesites on steep slopes. The total volume of Mount Griggs is ~25 cubic km.
"Griggs's products are chiefly olivine-pyroxene andesites; 27 samples range continuously from 54.5 to 63.5% SiO2. They are consistently more potassic than products of the other Katmai cluster volcanoes, their K2O contents being 1.3-1.4% at 57.5% SiO2 and 1.7-1.9% at 60%. Isotopic data also suggest a source mixture and plumbing system independent of the other nearby centers.
"Numerous SO2-rich fumarolic jets occur between 1,940-m and 2,180-m elevation atop the inner cone and along a steep chute on its upper southwest slope. Orifice temperatures (measured by Dave Johnston in 1978-9) range from 96 degrees to 108 degrees C, and their condensates have pH ~1. Each orifice is constructing its own mound of sulfur sublimate. Downhill fumaroles are hottest and loudest, their roar commonly audible from the valley floor."

Name Origin

Mount Griggs was named in 1956 by Gilbert Grosvenor, National Geographic Society, for Robert Fiske Griggs (1881-1952), botanist and leader of six National Geographic Society expeditions to the Katma District from 1915 to 1930. These expeditions lead to the 1918 creation of the Katmai National Monument. This volcano was previously called "Knife Peak" (Orth, 1971).


References Cited

[1] Volcanoes of North America: United States and Canada, 1990

Wood, C. A., and Kienle, Juergen, (eds.), 1990, Volcanoes of North America: United States and Canada: New York, Cambridge University Press, 354 p.

Current Activity

No new updates for Griggs volcano since March 18, 2022, 3:33 pm.

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Ash Forecasting

Mathematical models developed by the USGS forecast various aspects of how a volcanic ash plume will interact with wind—where, how high, and how fast ash particles will be transported in the atmosphere, as well as where ash will fall out and accumulate on the ground. AVO runs these models when a volcano is restless by assuming a reasonable hypothetical eruption, to provide a pre-eruptive forecast of areas likely to be affected. During an ongoing eruption, AVO will update the forecast with actual observations (eruption start time and duration, plume height) as they become available.

View the current airborne ash cloud models for Griggs

Ashfall thickness forecast

The Ash3d model was developed by the USGS to forecast how a volcanic ash plume will interact with wind and where ash will fall out and accumulate on the ground. AVO runs these models twice daily when a volcano is restless by assuming a reasonable hypothetical eruption altitude and duration. The map shows the model results of ashfall thickness for areas that are likely to be affected, if one were to occur. During an ongoing eruption, AVO will update the forecast with actual observations (eruption start time and duration, plume height) as they become available, and these plots will be automatically updated. The National Weather Service Anchorage Forecast Office will issue the official ashfall warning product and post them at weather.gov/afc

THESE PRODUCTS MAY NOT BE CURRENT.

During an actual eruption, see National Weather Service forecasts of ashfall:https://weather.gov/afc.

Ashfall Forecast

Click on the X on the graphic (upper right) to expand the map to show the map legend.

Ashfall Start Time

This map shows the modeled estimate of the time it would take for ashfall to begin following an eruption. It corresponds to the ashfall thickness forecast map shown above. This map uses the start time of either the twice-daily hypothetical model runs (time shown in the legend) or the actual eruption start time (if one were to occur). In the case of an actual eruption, the National Weather Service Anchorage Forecast Office will issue the official ashfall warning product that includes the ashfall start time and post them at weather.gov/afc

THESE PRODUCTS MAY NOT BE CURRENT.

During an actual eruption, see National Weather Service forecasts of ashfall:https://weather.gov/afc.

Ashfall Start Times Forecast

Click on the X on the graphic (upper right) to expand the map to show the map legend.
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