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K.R. Kore, S.R. McNutt, and D.H. Christensen
Systematic Search for Background Seismicity Rate Changes and Correlations at Alaskan Volcanoes This project got started because it was noticed that groups of volcanoes seemed to increase and decrease in seismicity levels at the same time. We wanted to quantify this observation. K.R. Kore, S.R. McNutt, and D.H. Christensen Geophysical Institute, University of Alaska Fairbanks
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Strain Rate Seismicity Rate
Overview and Goals Strain Rate Seismicity Rate Identify background seismicity rate changes Temporally correlate “events” between volcanoes along the Aleutian Arc Speculate as to the cause of the “events”
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The Alaskan Volcanoes Strandline Lake Spurr Wrangell Redoubt Iliamna
Katmai Augustine Aniakchak Pavlof Shishaldin Intro, data, and map: Highlight: Wrangell, Strandline, Spurr, Redoubt, Iliamna, Augustine, Katmai, Venia, Pavlof, Shish, Maku, Akutan. Label all volcanoes used in study Akutan Veniaminof Okmok Dutton Westdahl Makushin
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Identification of Rate Changes
Estimate minimum magnitude of completeness Exclude swarms & eruptions Perform AS(t) function of the z-test with min. 3 mo. rate Exclude man- made changes
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Volcanoes with Rate Changes
Strandline Lake Spurr Wrangell Redoubt Iliamna Katmai Augustine Aniakchak Pavlof Shishaldin The volcanoes in grey are too quiet, meaning there are not enough earthquakes at these volcanoes to do a statistically significant study. Veniaminof Akutan 12 of 16 Volcanoes Length of Monitoring Time Activity/ Sensitivity Level Okmok Dutton Westdahl Makushin
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Eruption Examples of when rate changes occurred
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Coincident “Events” Ho: All volcanic events are random and independent
95% Confidence Level 10,000 synthetic catalogs per time window Random generation of events Probability of occurrence
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Early 1996 Events Redoubt 5/11 Iliamna 5/8 Augustine 2/19 Akutan 3/10
120 Day window P=0.004 Iliamna increases, Redoubt and Augustine decrease Akutan- swarm Regional earthquakes: Adak June 9th – 10th (M7.9, M7.2) Akutan 3/10 Intro, data, and map: Highlight: Wrangell, Strandline, Spurr, Redoubt, Iliamna, Augustine, Katmai, Venia, Pavlof, Shish, Maku, Akutan. Label all volcanoes used in study
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Late 1996 Events Strandline Lake 8/31 Spurr 10/11 Augustine 9/25
Katmai 10/16 60 Day window P=0.0001 Strandline, Katmai: swarms Pavlof: eruption Augustine increase, Spurr decrease Amukta eruption Speculated Slow Slip Event (McNutt and Marzocchi, 2004) Pavlof 9/16 Intro, data, and map: Highlight: Wrangell, Strandline, Spurr, Redoubt, Iliamna, Augustine, Katmai, Venia, Pavlof, Shish, Maku, Akutan. Label all volcanoes used in study Amukta 9/18
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1998 Events Strandline Lake 3/28 Spurr 4/2 Redoubt 5/1 60 Day window
All rate decreases Plume from Spurr 3/28 Lake Becharof/ Ukinrek Maars swarm 5/8-5/9 Slow Slip Event, Cook Inlet - Late 1998 (Ohta et al., 2004) Strandline Lake 3/28 Spurr 4/2 Spurr: 3/26 plume noted in ANC. Rate change on 4/2 Strandline Lake: 3/28 Redoubt:5/1 Lake Becharof Redoubt 5/1
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2002 Events 60 Day window P=0.0206 All rate decreases Wrangell 11/17
10/23 M6.7 11/03 M7.9 60 Day window P=0.0206 All rate decreases Denali Fault Earthquake Sequence: Oct. 23rd - Nov. 3rd Wrangell 11/17 Spurr: 10/25 and 12/16 Strandline: 10/29 and 12/18 Wrangell: 11/17 Strandline Lake 10/29 Spurr 10/25
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The Four Cases Early 1996: Akutan, Iliamna, Redoubt, Augustine:
120 Day Window, P=0.004 Late 1996: Spurr, Strandline Lake, Augustine, Katmai, Pavlof: 60 Day Window, P=0.0001 1998: Strandline Lake, Spurr, Redoubt: 60 Day Window, P=0.0148 2002: Wrangell, Strandline Lake, Spurr: 60 Day Window, P=0.0206 These four cases are strong evidence that the volcanoes can react together to larger stress changes. They can also react independently to local changes.
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Conclusions and Speculations
Probabilities of independent volcanoes having events close in time tend to be low. This suggests that the volcanoes are reacting to regional events which change the stresses governing the volcanoes, such as: Regional Earthquakes Slow Slip Events Other more subtle stress changes
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