Spurr
Facts
- Official Name: Mount Spurr
- Seismically Monitored: Yes
- Color Code: GREEN
- Alert Level: NORMAL
- Elevation: 3374m (11069ft)
- Latitude: 61.2989
- Longitude: -152.2539
- Smithsonian VNum: 313040
- Pronunciation:
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Nearby Towns:
- Beluga 37 mi (60 km) SE
- Tyonek 40 mi (65 km) SE
- Nikiski 51 mi (81 km) SE
- Susitna 55 mi (89 km) NE
- Salamatof 56 mi (90 km) SE
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Subfeatures:
- Crater Peak
Description
From Miller and others (1998) [1] : "Mount Spurr is a Quaternary stratovolcano located near the northeastern end of the Aleutian volcanic arc. It is the easternmost historically active volcano in the Aleutian arc and is the highest of several snow- and ice-covered peaks that appear to define a large, dissected stratovolcano [2] ."Capps (1929) [3] suggested that a summit caldera, largely buried by ice, is associated with Mount Spurr. Later, Juhle and Coulter (1955) [2] disagreed with the caldera interpretation suggesting that the peaks around Mount Spurr only coincidentally resemble the rim of a large subsidence structure. Most recent studies, however, suggest that ancestral Mt. Spurr, constructed during late Pleistocene time [4] , was partially destroyed by a major Bezymianny-type eruption possibly as late as early Holocene time [5] [6] . The eruption produced a voluminous volcanic debris avalanche and subsequent pyroclastic flows that resulted in the formation of a 5- to 6-km-diameter explosion caldera. The volcanic debris avalanche contains blocks as much as 100 m in diameter and traveled a minimum of 25 km. The overlying pyroclastic flows are partially welded and are composed chiefly of high silica andesite. Present Mt. Spurr is the highest of several post-caldera, centrally located, ice-carved cones or domes.
"The youngest volcanic feature at Mount Spurr is a satellitic cone, Crater Peak, located in the breach in the caldera about 3.2 km south of Mount Spurr. Crater Peak has a summit crater that is itself slightly breached along the south rim; the north wall of the crater exposes the truncated remains of an older dome or lava lake. Crater Peak has been the source of all Late Holocene eruptive activity at Mt. Spurr [5] . Before the 1992 eruption, a small crater lake occupied the bottom of the crater."
Name Origin
A.H. Brooks named Mount Spurr in 1900, for Josiah Edward Spurr, a U.S. Geological Survey geologist who led an expedition in the area in 1898 (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.
intro and TOC PDF 268 KB
references PDF 43 KB [2] The Mt. Spurr eruption, July 9, 1953, 1955
Juhle, R. W., and Coulter, H. W., 1955, The Mt. Spurr eruption, July 9, 1953: Eos, v. 36, n. 2, p. 199-202.[3] The Mount Spurr region, Alaska, 1929
Capps, S. R., 1929, The Mount Spurr region, Alaska: U.S. Geological Survey Bulletin 0810-C, p. 141-172, 2 plates, scale 1:250,000.
full-text PDF 1.6 MB
plate 3 PDF 324 KB [4] Geochronology of eruptive events at Mt. Spurr, Alaska, 1986
Turner, D. L., and Nye, C. J., 1986, Geochronology of eruptive events at Mt. Spurr, Alaska: in Turner, D. L. and Wescott, E. M., (eds.), Geothermal energy resource investigations at Mt. Spurr, Alaska, University of Alaska Fairbanks Geophysical Institute Report UAG-R 308, p. 20-27, 1 plate, scale 1:2,860.[5] A reconnaissance of the major Holocene tephra deposits in the upper Cook Inlet region, Alaska, 1985
Riehle, J. R., 1985, A reconnaissance of the major Holocene tephra deposits in the upper Cook Inlet region, Alaska: Journal of Volcanology and Geothermal Research, v. 26, n. 1-2, p. 37-74.[6] Petrology, geochemistry, and age of the Spurr volcanic complex, eastern Aleutian arc, 1990
Nye, C. J., and Turner, D. L., 1990, Petrology, geochemistry, and age of the Spurr volcanic complex, eastern Aleutian arc: Bulletin of Volcanology, v. 52, n. 3, p. 205-226.Current Activity
May 15, 2024, 2:09 pmSummary of Current Activity
The Alaska Volcano Observatory (AVO) has detected a small increase in volcano seismic activity at Mount Spurr, which may indicate an intrusion of new magma deep beneath the volcano. An extended recent outage of the local seismic network from February to April 2024 limits precise determination of the onset of this activity, but elevated seismicity has been seen since the network returned on April 3. Since then, AVO has located an average of four earthquakes per day, with a peak of 33 recorded on April 26. These have typically been smaller than magnitude 1.0, and range in depth from near the summit of the volcano to as much as 18 miles (30 km) below sea level. This activity represents an increase in earthquake rate and occurrence of deeper (>12.4 miles or 20 km) low frequency earthquakes compared to recent years. These low frequency earthquakes are likely related to the migration of fluids. Minor uplift of the ground surface at the volcano of ~0.4 inches (~1 cm) has also been observed in local GPS data since November 2023, which is a deviation from the long-term trend and may be related to the seismicity. No significant changes to the ice and snow cover or gas and steam emissions have been observed in association with these geophysical observations. In clear viewing conditions, minor steaming is commonly visible from fumaroles in the summit crater region.
A figure showing recent located earthquakes at Mount Spurr can be seen here: https://avo.alaska.edu/image/view/195424
A figure showing the ground deformation data from GNSS (GPS) at two sites on Mount Spurr can be seen here: https://avo.alaska.edu/image/view/195423
Monitoring Status
Mount Spurr is monitored by an eleven-station seismic network, four continuous GPS receivers, four infrasound sensors, and web cameras. Data from five of the eleven stations are currently coming into AVO in real time, but the other six stations in the network are only recording data locally. AVO plans to restore real-time feeds from those stations and recover the stored data during maintenance visits this summer, beginning on May 20, 2024. Additional regional seismic stations and infrasound sensors located throughout south-central Alaska provide supporting data. AVO also monitors the volcano using satellite monitoring, lightning data, pilot reports, and airborne and ground observations to detect changes in the snow and ice surfaces, thermal emissions, and volcanic ash, steam, and gas emissions. AVO conducted a short observational overflight on May 14, 2024, and another to measure gas emissions and make observations is planned for June.
Prognosis and Hazards
The activity that we have observed at Mount Spurr over the past six weeks is consistent with the intrusion of magma deep beneath the volcano. Such an intrusion can cause subtle inflation or swelling of the volcano and generate earthquakes through the release magmatic gasses.
While these observations suggest that increased activity may be occurring deep beneath Mount Spurr, there is no indication that an eruption may occur soon, if at all. Intrusions of new magma under volcanoes do not always result in volcanic eruptions and activity may decline without an eruption occurring, such as during the previous intrusion under Mount Spurr that occurred in 2004. Prior to a significant eruption, AVO would expect months of volcanic unrest that would allow advanced warning. This would likely consist of a greater increase and shallowing of earthquakes, increased uplift of the ground surface as magma rises to shallower levels in the Earth’s crust, and signs of increased heat and magmatic gas emissions, such as localized melting of summit glaciers and debris flows.
If Mount Spurr were to erupt, the primary hazard would be airborne ash and ashfall on down-wind communities. The slopes of the volcano would also be affected by pyroclastic flows, and lahars, or mudflows formed from the melting of ice and snow due to volcanic activity, could inundate drainages on all sides of the volcano, particularly on the south and east flanks.
