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Earthquake Hazards in Western Washington The mega-thrust at the coast Shallow earthquakes in the crust of Puget Sound Deep earthquakes in the subducted Juan de Fuca Plate Which should you worry about?
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Three kinds of earthquakes: Plate Interface (megathrust, Cascadia, 1700) Intraslab (deep, Wadati-Benioff, Nisqually 2001) North American Plate (Shallow, crustal earthquakes, Seattle, 900)
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Deep Earthquakes Wadati-Benioff zone earthquakes Intraslab earthquakes Occur inside the cold subducting lithosphere Occur to depths of nearly 700 km in many subduction zones where the oceanic plate is old and cold In Cascadia, the subducting Juan de Fuca plate is young and warm; deepest earthquakes are only 100 km
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Earthquake Hazards in Western Washington The mega-thrust at the coast Shallow thrusts in the crust of Puget Sound Normal faulting in the subducted Juan de Fuca Plate There have been 3 events in the last 60 years: 1949, 1965 and 2001. There WILL be more in YOUR lifetime. The last one caused $1,000,000,000 in losses that were largely preventable.
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The Nisqually Earthquake February 28, 2001 10:54:33 AM PST Magnitude 6.8
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Intraslab Seismicity Largest intraslab earthquakes are in south sound region at base of microseismicity, including 1949 M7.1; 1965 M 6.5 and 2001 M6.8 Deepest earthquakes are downstream from large events Intraslab seismicity is virtually absent north and south of arch Intraslab focal mechanisms are widely scattered but generally are in-plane tension Should we prepare for M7 or M8 intraslab earthquakes?
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SHOW WEB ANIMATION!
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Discussion
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The largest intraslab earthquakes tend to occur at the base of the seismic zone.
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3-D Tomographic Inversion Active-Source Data ~92,000 first arrivals from active source experiments (e.g. SHIPS) ~92,000 first arrivals from active source experiments (e.g. SHIPS) 1200 wide-angle reflection times from SHIPS 1200 wide-angle reflection times from SHIPS
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Previous Tomography (Preston et al. 2003)
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Complication #2: Gouge zones
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Fault zones and Faults The ideal fault: San Gabriel Fault Photo Matt D’Allessio
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You are here Press, 20-12 Pacific and North American plates are main players
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USGS Prof. Paper, 1-2 North America map Show Movie #01
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Subduction under Alaska & Aleutian Is. 8 cm/yr of plate convergence –almost strike-slip in Aleutian Is. Site of large underthrusting earthquakes –1964 Alaska Earthquake M W =9.2 Volcanic arc & eruptions
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Not subduction! Embarrassing. (UT Austin) Strike-slip Alaska - Pacific boundary
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Queen Charlotte Fault System
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Alaska Most dangerous faults in US –8 quakes over M=8 in last 100 years Sparsely populated Main fault is subduction thrust –Only surfaces on ocean floor –Many secondary faults Also has volcanoes, tsunamis
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1899-1979 Alaska quakes Stars - M > 7.5 Triangles - 6.5 to 7.5 Yanev, p. 175 6.7 & 8 quakes in 2002
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Tectonic Setting of N. America Old stable interior East coast “passive margin” West coast “active margin” –Pacific - N. Am. plate interactions Transform motion at SAF Subduction under Alaska & Aleutian Is. –Juan de Fuca - N. Am. interactions Subduction under Northern California, Oregon, Washington, and British Columbia
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US Geology
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US Topography Topographic action mark tectonic activity
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Press, 20-6c Continental collision is cause of Appalachian Mts
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Now Passive margin US Europe Rifting
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USA seismicity Notice that all the action is in the West –most dramatic topography in the West Yosemite, Cascade Mts., Big Sur coast, etc. –few earthquakes in the East Some faults as far east as Yellowstone No action to west in Pacific plate either –Hawaii is special case - hot spot volcano
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US Seismicity
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Geology of western US - Fabric related to deformation
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Western boundary of North American Plate Type of boundary depends on orientation Plate boundaries move and change in time Past 30 My saw major changes & development of San Andreas Fault From 80 to 30 My Farallon plate subducted under west coast. –Juan de Fuca & Cocos plates are remnants of Farallon plate
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Cartoon of Western N. America tectonics Vidale
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Details: US and Mexico coast Three little plates subducting offshore Oregon, Washington, and B. Columbia –Juan de Fuca Plate –Gorda Plate –Explorer Plate Spreading ridge splitting Gulf of California –Separating Baja from N. America –Oblique because ridges are combined with transform faults Cocos Plate subducting to the south
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Exotic terrain placement Accretion of fragments to continent
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Exotic terrains Western N. Am (Cordillera) assembled from small pieces over past 200 My
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Changes in west coast A mid-ocean ridge subducted –Before that, just subduction on coast –First hit near LA 25 Mya –San Andreas fault system started then As ridge is subducting, two triple junctions are moving apart on coast –Mendocino Triple Junction moving north NA-Pacific-Juan de Fuca junction –NA-Pacific-Rivera junction off Baja California
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Note present San Andreas fault Show movie #02
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Oregon-Washington M 9 every 1000 years, last in 1700 Recent quakes –M 7.0 in 2000, 6.5 in 1965 in Seattle –M 7.1 in 1949 in Olympia Main fault is subduction zone Also volcanoes (like Mt. St. Helens) Not adequately prepared We’ve looked at these faults before –But biggest surface offshore
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Cascadia subduction zone 4 cm/yr convergence rate
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Pacific - Juan de Fuca spreading Subduction of J. de F. under N. Am. Iacopi, 27 Note: Plate motions Triple Junctions
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Cartoon view Show movie #09
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Also smaller faults in Seattle
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Oregon- Wash. Close-up Yeats, 5-2 Note: Volcanoes San Andreas Triple Junctions Mt. Hood From Portland
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Mt Rainier and Seattle
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Subduction under Pacific Northwest 4 cm/yr of plate convergence –like small convection cell - up at ridge down at subduction zone Site of great underthrusting earthquakes –None in historic record –But evidence for magnitude 9 quake in 1700 Tsunami sands in buried marsh Tsunami in Japan in 1700 Volcanic arc & eruptions –Mt. St. Helens, Mt. Rainier, Mt. Shasta
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Oregon-Washington X-sect Cascadia cross-section Keller, 7-5 Ridge Olympic Mts Cascade Mts
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Tsunami sand associated with the 1700 earthquake covering a Native fire pit on the banks of the Salmon River in Oregon. Fire-cracked rocks, charcoal and ashes delineate the fire pit that was dug into the sandy beach.
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Last 30 Mya of west coast tectonics Cape Mend.
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ETS Every 15 months Creager & Wech * BS Array
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Tremor Migration for four ETS events Wech, Creager and Melbourne, JGR, submitted
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Tremor and Slip summed over 4 ETS events Wech, Creager and Melbourne, JGR, submitted
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Episodic Tremor and Slip (McCausland et al., GRL 2005)
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Cascadia
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