U.S. Department of the Interior U.S. Geological Survey Tracking Magma at Alaskan Volcanoes: 2005 - 2011 J.A. Power, S. G. Prejean, S.D. Stihler, Z. Lu, C.J. Nye, D.J. Schneider, J.T. Freymueller, P.F. Cervelli, S.R. McNutt.
Jan 08, 2016
U.S. Department of the InteriorU.S. Geological Survey
Tracking Magma at Alaskan Volcanoes: 2005 - 2011
J.A. Power, S. G. Prejean, S.D. Stihler, Z. Lu, C.J. Nye, D.J. Schneider, J.T. Freymueller, P.F. Cervelli, S.R. McNutt.
Organization:
KasatochiOkmok
Pavlof
Spurr
Augustine
Redoubt
• Aleutian Arc Volcanoes• AVO Monitoring • Communication• Recent Unrest/Eruptions
1. Spurr (2005)2. Kastochi (2008)3. Augustine (2006)4. Redoubt (2009)5. Okmok (2008)6. Pavlof (2007)
• Summary
Alaskan Volcanic Centers
Alaska Volcano Observatory Monitoring
Monitoring Techniqueso SeismologyoContinuous GPSoRemote Sensing (visual & InSAR)oWebcamsoAirborne Gas (SO2 & CO2)oGeologyoPressureoOthers
Seismic Stations in Alaska
Red = AVO, Yellow = AEIC, Purple = WCATWC, Black = GSN
AVO Volcano Communication
•ALASKA VOLCANO OBSERVATORY
•ALASKA DEPARTMENT OF EMERGENCY SERVICES
•US AIR FORCE
•NOAA/NATIONAL WEATHER SERVICE
•FEDERAL AVIATION ADMINISTRATION
•Others
http://vaac.arh.noaa.gov/interagency_plan.pdf
Mount Spurr: 2005
Historical Eruptions19531992
Crater Peak1953 & 1992 Vent
Spurr Summit~6000 Years BP
Monitoring Equipment9 SP Seismometers3 BB Seismometers
3 CGPS1 Webcam
Anchorage
2004 - 2006
2004 – 2007 Spurr Seismicity is characterized by:1.Shallow VTs beneath Spurr Summit.2.Small magnitudes.3.Deep Long-Period Events to SE.4.Changes in stress direction (D. Roman).
Gas (CO2) Flux Thermal – Snow Melt
Geodesy – CGPS Inflation
Spurr Summit 2005……Unrest is driven by a deep
intrusion marked by DLP and shallow seismicity, snow melt, gas flux, and inflation.
Yellow: July 26, 2004 – January 12, 2006
Photo by Jerry Morris
Kasatochi Volcano: 2008 VEI 4
No Local Monitoring!
Historical EruptionsNone
KasatochiKorovin
Great Sitkin
Explosions
RED, First Explosion
ORANGEM5.6
August 7, 2008August 6, 2008
Closest Seismometer ~ 37 km
YELLOW, Evacuation Effort Started
Evacuation Complete
GOES Band 4m5: 09 Aug 2008 0100 UTC
Ash Cloud on August 9, 2008
Kasatochi in retrospect…Successful forecast was possible because of
large energy release at a long dormant center.
If the volcano had been seismically monitored, we would have had weeks to months of warning.
Kasatochi area seismicity from the AEIC earthquake catalog
May June AugustJulyAprilMarch
2
4
6
Ear
thqu
ake
Mag
nitu
de
2008
Aleutian Volcano Seismic Moment
1 fringe = 11.76 cm
Augustine Volcano: 2006 VEI 3
Historical Eruptions19861976
1963-64193518821812
2006 Monitoring Equipment9 SP Seismometers4 BB Seismometers
5 CGPS
Augustine……The 2006 eruption was proceeded by
8 to 9 months of increasing shallow seismicity, Distal VTs, deformation (inflation), and gas flux. This pattern of precursory activity was similar to the 1986 and 1976 eruptions.
60 Minutes
RED
ORANGE
Fisher et al., 2010
Photo by C. Read
Redoubt Volcano: 2009 VEI 3
Historical Eruptions1989-90
1965 – 6619331902
2009 Monitoring Equipment5 SP Seismometers
5 BB Seismometers (installed 2009)5 CGPS (4 installed in 2009)
Sulfer Smell
DLP Characteristics•Z ~ 28 – 37 km•ML ~ 0.7 – 1.4•SEH ~ 0.5 – 2.5 km•SEZ ~ 1.0 – 3.0 km
Snow Melt
Deformation
Grapenthin, et al., Submitted Geodetic Observations during the 2009 eruption of Redoubt Volcano, Alaska, JVGR, Submitted.
The 2009 eruption was also preceded by a small inflation observed at AC17~30 km northeast of the edifice beginning in July 2008 (Grapenthin et al.Submitted).
January 21 – February 20 February 21 – March 23
Redoubt 2009 Shallow Precursory Seismicity
Redoubt 2009 …… The 2009 Eruption was proceeded by marked increases in
gas flux, deformation, and Deep Long-Period (DLP) seismicity. Short-term forecasting was difficult because of pervasive tremor and swarms of shallow events – a strong contrast to the 1989-90 activity.
6 Hours
Orange
YellowOrange
Red
Okmok Volcano: 2008VEI 4
Photo by C. Read
Historical Eruptions1997198819831981
+ 12 more since 1805
~9.5 km
Monitoring Equipment6 SP Seismometers4 BB Seismometers
4 CGPS
24 Hours
30 Minutes
Eruption Begins
RED
1
3
2
Ear
thqu
ake
Mag
nitu
de
Month in 2008
0
1 2 3 4 5 6 7 8 9 10
Okmok in Retrospect: Very short precursors! 6 hours before eruption: No unusual activity (although some CGPS stations are inoperable). No advance warning was issued! Co-eruption signals are strong!
COLOR CODE: GREEN RED
Subsidence of >50 cm
Okmok Co-Eruption Signals
1 fringe = 2.83 cm
Pavlof Volcano: 2007 VEI 2
Aeromap 1996
Historical Eruptions1996-97
1988198619831981
+ 34 since 1790
Monitoring Equipment6 SP Seismometers
3 d
ays
1 Hour
Pavlof in retrospect…Frequently active or open-vent system that exhibits very
mild precursory activity.
Yellow
Orange
Strombolian Eruption Reported
Neither the 2007 or 1996-97 eruptions show deformation in InSAR, however, CGPS data is not available.
Summary
Kastatochi and Spurr suggest long dormant vents activate over months to years.
Long dormant vents and flank intrusions can involve large release of seismic energy.
Aleutian events suggest deformation (CGPS & InSAR) and DLP seismic events hold promise for extending forecasting window.
Frequently active centers (Okmok & Pavlof) can activate much faster and with very weak short-lived precursors.