Document Type

Article

Publication Date

6-2008

Digital Object Identifier (DOI)

https://doi.org/10.1029/2008EO230002

Abstract

After an 11-year period of repose, Pavlof volcano on the Alaska Peninsula (Figure 1) began an episode of Strombolian eruption lasting 31 days, from 14 August to 13 September 2007.

The eruption began abruptly on 14 August after a minor increase in seismicity the previous day. Nearly continuous lava fountaining, explosions, and lahars caused by minor disruption of the ice and snow cover on the volcano characterized the eruption. The eruption also produced diffuse ash plumes that reached 5–6 kilometers above sea level, but the plumes were too small and did not extend high enough to affect local or regional air travel. Melting of snow and ice on the upper part of the edifice by hot debris avalanches and lava resulted in numerous lahars that entered the sea and inundated a 2×106 square meter area on the volcanos southern slope.

Was this content written or created while at USF?

No

Citation / Publisher Attribution

Eos, Transactions American Geophysical Union, v. 89, issue 23, p. 209-211

©2008. American Geophysical Union. All Rights Reserved.

Share

COinS