Report on Spurr (United States) — 10 August-16 August 2005
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
10 August-16 August 2005
Managing Editor: Gari Mayberry
Please cite this report as:
Global Volcanism Program, 2005. Report on Spurr (United States). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 10 August-16 August 2005. Smithsonian Institution and US Geological Survey.
61.299°N, 152.251°W; summit elev. 3374 m
All times are local (unless otherwise noted)
The level of seismic activity at Mt. Spurr decreased during the previous month, but remained above background levels during 5-12 August. Gas and heat emissions remained at elevated levels, and minor steaming continued from the summit "melt/collapse pit." Satellite imagery showed no indications that an eruption was imminent. Spurr remained at Concern Color Code Yellow.
Geological Summary. The summit of Mount Spurr is a large lava dome constructed at the center of a roughly 5-km-wide horseshoe-shaped caldera open to the south. The volcano lies 130 km W of Anchorage and NE of Chakachamna Lake. The caldera was formed by a late-Pleistocene or early Holocene debris avalanche and associated pyroclastic flows that destroyed an ancestral edifice. The debris avalanche traveled more than 25 km SE, and the resulting deposit contains blocks as large as 100 m in diameter. Several ice-carved post-caldera cones or lava domes lie in the center of the caldera. The youngest vent, Crater Peak, formed at the breached southern end of the caldera and has been the source of about 40 identified Holocene tephra layers. Eruptions from Crater Peak in 1953 and 1992 deposited ash on the city of Anchorage.
Source: US Geological Survey Alaska Volcano Observatory (AVO)