Novarupta


Facts


  • Official Name: Novarupta
  • Seismically Monitored: Yes
  • Color Code: GREEN
  • Alert Level: NORMAL
  • Elevation: 841m (2759ft)
  • Latitude: 58.2654
  • Longitude: -155.1591
  • Smithsonian VNum: 312180
  • Pronunciation:
  • Nearby Towns:
    • Karluk 55 mi (88 km) SE
    • Kanatak 58 mi (93 km) SW
    • King Salmon 62 mi (99 km) NW
    • Larsen Bay 66 mi (107 km) SE
    • South Naknek 73 mi (118 km) NW

    Distance from Anchorage: 274 mi (441 km)

Description

From Miller and others (1998) [1] : "The Novarupta dome is about 400 m in diameter and 65 m high at its center [2] , and is surrounded by a 2-km-wide, funnel-shaped structure [3] [4] . The surface of the dome is completely fractured into chaotic blocks and crumble breccia. The dome is a plug-like feature emplaced within a low ejecta ring. Prominent scarps along the flanks of Baked, Falling, and Broken Mountains surrounding the Novarupta depression indicate considerable subsidence occurred following the 1912 eruption. Nearby stratovolcanoes (including Trident and Katmai) form a volcanic front trending N65E; Novarupta lies about 4 km behind the front. Linear fractures normal to the front extend between Novarupta and Trident [5] ."

Name Origin

R.F. Griggs named Novarupta in 1916. "Novarupta" means "new eruption"; the dome formed during the 1912 eruption of Novarupta and Katmai (Orth, 1971).


References Cited

[1] Catalog of the historically active volcanoes of Alaska, 1998

Miller, T. P., McGimsey, R. G., Richter, D. H., Riehle, J. R., Nye, C. J., Yount, M. E., and Dumoulin, J. A., 1998, Catalog of the historically active volcanoes of Alaska: U.S. Geological Survey Open-File Report 98-0582, 104 p.

[2] The stratigraphy of the ejecta from the 1912 eruption of Mount Katmai and Novarupta, Alaska, 1968

Curtis, G. H., 1968, The stratigraphy of the ejecta from the 1912 eruption of Mount Katmai and Novarupta, Alaska: in Coats, R. R., Hay, R. L., and Anderson, C. A., (eds.), Studies in volcanology, Geological Society of America Memoir MWR 0116, p. 153-210.

[3] The compositionally zoned eruption of 1912 in the Valley of Ten Thousand Smokes, Katmai National Park, Alaska, 1983

Hildreth, Wes, 1983, The compositionally zoned eruption of 1912 in the Valley of Ten Thousand Smokes, Katmai National Park, Alaska: Journal of Volcanology and Geothermal Research, v. 18, n. 1-4, p. 1-56.

[4] The vent of the 1912 Katmai eruption: gravity and magnetic measurements, 1991

Goodliffe, A. M., Stone, D. B., Kienle, Juergen, and Kasameyer, Paul, 1991, The vent of the 1912 Katmai eruption: gravity and magnetic measurements: Geophysical Research Letters, v. 18, n. 8, p. 1521-1524.

[5] New perspectives on the eruption on 1912 in the Valley of Ten Thousand Smokes, Katmai National Park, Alaska, 1987

Hildreth, Wes, 1987, New perspectives on the eruption on 1912 in the Valley of Ten Thousand Smokes, Katmai National Park, Alaska: Bulletin of Volcanology, v. 49, n. 5, p. 680-693.

Current Activity

No new updates for Novarupta 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 Novarupta

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.