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Volcanic Seismology and Deep Long Period Earthquakes

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Title: Volcanic Seismology and Deep Long Period Earthquakes


1
Volcanic Seismology and Deep Long Period
Earthquakes
Wendy McCausland Graduate Research Assistant D
epartment of Earth and Space Sciences,
University of Washington Advisors Dr. Steve Mal
one - University of Washington/PNSN
Dr. Chris Newhall - University of
Washington/USGS
2
Dr. Steve MaloneResearch Professor Department
of Earth and Space Sciences
  • Research Interests
  • Seismicity of the Cascade volcanoes
  • Earthquake and volcanic hazards
  • Strong-motion seismology
  • Computer applications in seismic data acquisition
    and network analysis
  • Pacific Northwest Seismic Network (PNSN)
  • http//www.ess.washington.edu/SEIS/PNSN/

3
Current Stations Pacific Northwest Seismograph
Network
  • 138 Short-period
  • 15 others
  • 21 Broad-band
  • 9 others
  • 69 Strong-motion
  • 35 NSMP sites

4
Dr. Chris NewhallAffiliate Professor, Dept of
Earth and Space SciencesResearch Scientist,
U.S.G.S.
  • Leader of the World Organization of Volcano
    Observatories (WOVO)
    http//www.wovo.org
  • Member of the USGS' Volcano Disaster Assistance
    Team
  • Recent work focuses on
  • Processes of volcanic unrest (seismicity, ground
    deformation, gas emission, etc)
  • Applications of this research to eruption
    forecasting
  • Developing a web-accessible database of volcanic
    unrest, linked to the Smithsonian database of
    historical volcanic eruptions WOVOdat
    http//www.wovo.org/wovodat.htm
  • Helps colleagues from the Cascades Volcano
    Observatory (CVO) and a number of countries
    during volcanic crises

5
Recent Seismic and Volcanic Activity near Goma,
Democratic Republic of the Congo
6
Graduate Students
  • Studies of particularly puzzling or previously
    unrecognized patterns of unrest,
  • Sarah Albano - groundwater response to volcanic
    strain
  • Wendy McCausland - unusual volcanic seismicity,
    DLP events
  • Jeff Witter - circulation of magma in volcanic
    conduits as a mechanism for non-explosive
    volatile emission at passively degassing
    volcanoes, excess SO2 degassing
  • Josh Jones seismicity of Oldoinyo Lengai, Mount
    Hood
  • Adam Haulter Avalanche events at Mount Rainier
  • Thesis study of ephemeral processes
  • Cami Apfelbeck - chemical and thermal evolution
    of the new caldera lake at Pinatubo
  • Shannon Hayes - world-record-setting sediment
    transport from Pinatubo's pyroclastic deposits

7
What is Volcanic Seismology?
  • Study of
  • Earthquakes
  • At or near volcano (
  • Generated by volcanic processes
  • Velocity structure of the volcano
  • Seismic attenuation at the volcano

8
Volcanic Seismicity Why Study?
  • To understand
  • Dynamics of active volcanic systems
  • Physical properties of bubbly magma
  • Map the extent and evolution of source regions

  • Stress conditions, both regional and local
  • Ultimately leads to better
  • Forecasting of eruptive behavior
  • Assessment of volcanic hazards

9
Volcanic Seismicity Why Different from
Tectonic?
  • Seismicity that
  • precedes,
  • accompanies, and
  • follows volcanic eruptions, intrusions

Number of earthquakes higher than in normal
crust- hot fluids and low rock strengths lead to
many small often unfelt earthquakes
Shallower depths (1-9 km) than tectonic
Occurrence pattern swarms vs mainshock-aftershock
sequences
Different types associated with different
processes high frequency, low frequency, explosio
ns, tremor
Non-Uniform stress field leads to complex Focal
Mechanisms including volumetric components in
addition to simple shear
10
Volcanic Earthquake Types
  • High frequency events
  • (volcano- tectonic) - A
  • Low frequency or Long
  • period events - C, F, I, J
  • Hybrid events -B
  • Explosion quakes -E
  • Volcanic tremor D, G, H
  • Avalanche events

(From McNutt, 2000)
11
Recent Eruptive History of Cascade Volcanoes

Young Cascades Volcanoes
Monitored Cascades Volcanoes
12
Relative Seismicity at Cascade Volcanoes
13
Seismicity in the Cascades Region1990-2001
M0.5
14
Deep Long Period Earthquakes
  • Deep ? 10 - 35 km depth
  • Long Period ? 1 s
  • Importance
  • source not well understood
  • attributed to migration of magmatic fluids
  • eruption triggering at silicic centers-
  • Ex. Pinatubo, 1991 (White, 1996)

15
Deep Long Period Earthquakes
  • Examples in Washington/Oregon Cascades
  • Mt. Rainier
  • Mt. Baker
  • Mt. St. Helens
  • In California (Pitt et al, 2002)
  • Mammoth Mountain- Devils Postpile
  • Mono Craters
  • Sierra Nevada (south of Yosemite, west of
    Mammoth)
  • Lassen Peak
  • Mt. Shasta - Medicine Lake
  • Clear Lake
  • In Japan
  • Fuji
  • Izu Oshima

16
Deep Long Period Seismicity and Volcano Locations
Deep Long Period Seismicity and Volcano Location
s
Non- low frequency earthquakes
DLPs
Volcano
17
Mount Hood
18
Mt Hood Earthquakes
19
Mount St. Helens
20
Mt St Helens Seismicity
21
Mt St Helens Relocations
Mount St. Helens
447 events from 1998 swarm
22
Mt St Helens Stress Model
Mount St. Helens
Major compressive axes
23
Mount St. Helens - 2 decades
24
Current Seismicity atMount St. Helens
25
Deep LPs Mt St Helens
Z 27 km
26
Mount Rainier
27
Mt Rainier Seismicity
28
Mt. Rainier Velocity Tomography
29
Mt Rainier DLP Events
30
Mt Rainier DLP Earthquakes
Depth 10 13 km Spatially distinct from Volca
no-tectonic (VT) events Similar depth to deepes
t VT events Reflect injection of basaltic magma
into system? Result from Resonance of flui
d-filled crack? Unsteady non-linear flow in irre
gular conduit? Another yet unknown mechanism?
31
Mt Rainier DLPsFiltered for Low and High
Frequencies
32
Mt Rainier Comparing a Long Period with a High
Frequency Event
33
Focal Mechanisms for VT events and locations of
DLPs
Focal Mechanisms for Events in 3 Different Dep
th
Ranges and Deep LP Locations
34
Comparison of spectral content of DLP vs VTs at
2 stations
Red is DLP Blue is VT
35
Spectrogram for High Frequency and Low Frequency
Events Station FMW
36
In Summary
  • Volcanic earthquakes are key to underlying
    processes and forecasting
  • Deep Long Period Earthquakes
  • Occur at many volcanoes in the Cascades,
    including Mount Rainier and Mount St. Helens
  • Related to magma but exact mechanisms unknown
  • Extent and number unknown in Cascades, because
    this is just a sample of triggered events
  • Also occur at Japanese volcanoes, including Fuji,
    Izu Oshima, and others
  • I am interested to compare DLP events in the
    Cascades and Japan
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