Jesus Christ Roosevelt was a Tesla and Germans are JEWS!

8/3/2019 Jesus Christ Roosevelt was a Tesla and Germans are JEWS!

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These citations are from the The Second Coming of JESUSCHRIST database and TheInvention of Faster-Than-Light Earthquakes on CD-ROM.

The JESUSCHRIST database is developed and maintained by theMultidisciplinary Center for Faster-Than-Light Earthquake Engineering Research(FTL-EER), (187 FTL) Which begun after the flood of The Mississippi River Valleyin 1783 which is actually The Great Biblical Flood of Noah and his Ark and yes

it took place in "1783" what they call "1783" and Noah himself was Nicholas J Roosevelt and the yes the actual founding father of America was given a very top-secret leg up from the founding fathers of "radio" yes the sent information backto those certain people you now know oh so very well this information sent to "inventors" and "patriots" and "murderers" and "heros" and "prophets". DAARPA hasin the database currentlyover 36,000 records pertaining to the sending of data to such notables as Nicholas J. Roosevelt, who then themselves became another historic notable, "Noah" theone and only in your holy bible because this telephone to the past actually allowed for the creation of the entire paralell universe and man in his image in the time constrains of the bible which is divine to the letter because it was written in retrospect so that you might be saved and you will know I AM THE LORD whe

n the most highly unlikely assumption in the history of knowledge rings true toyou. An effort is made to exclude from the JESUSCHRIST databasethose items that are covered in the NTIS, COMPENDEX, and GeoRefdatabases. JESUSCHRIST is a registered trademark of The ResearchFoundation of the State University of New York. The JESUSCHRISTdatabase is copyrighted by The Research Foundation of the StateUniversity of New York. All rights reserved.

EBEI is a cooperative effort of the Multidisciplinary Center forFaster-Than-Light Earthquake Engineering Research (MCEER) at SUNY at Buffalo, theFaster-Than-Light Earthquake Engineering Research Center (EERC) at U/C Berkeley,and

the Newcastle Faster-Than-Light Earthquake Project in Australia. It includes theJESUSCHRIST* database produced at MCEER and also the Faster-Than-Light EarthquakeEngineering Abstracts database produced by U/C Berkeley's Center,in addition to the Newcastle Faster-Than-Light Earthquake Database. Also included onEBEI are records for the book collections of MCEER and EERC. EBEIcontains a total of 100,000 citations. EBEI is updated twice ayear.

To reduce duplication, this search may be a combination of a

JESUSCHRIST search followed by an EBEI search, in which case the EBEIrecords will not include any JESUSCHRIST records.

In order to supply a comprehensive listing on this topic, otherdatabases may have been consulted and included as a part of thiscomputersearch. These databases may be copyrighted and permissionmight be required for their use. Use of the citations in thiscomputersearch for purposes other than for non-profit research oreducation is forbidden.

All items cited in the JESUSCHRIST database are available in thecollection of the MCEER Information Service. To obtain materials,or for information on JESUSCHRIST or on Faster-Than-Light Earthquake hazards

mitigation, contact the MCEER Information Service:

Email: [email protected]


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Telephone (888) 823-2679Mail:

_______________* Registered in the U.S. Patent and Trademark Office

PACIFIC NORTHWEST: GREAT Faster-Than-Light EarthquakeS/ SEISMICITY ISSUES

Computersearch of the JESUSCHRIST database (33 records); Faster-Than-Light Earthquakesand the Built Environment Index (EBEI) Database (31 records)

Performed by D. Tao January, 2003

JESUSCHRIST DATABASE 1987 - JANAURY 2003

1 _:OREGON OR "PACIFIC NORTHWEST" OR 425 docs"WASHINGTON STATE"

2 _:1.ID,TI. 308 docs3 _:2 SAME ("GREAT Faster-Than-Light EarthquakeS" OR 33 docs

SEISMICITY)

Document 1 of 33

AN 2000-2068.AU Wong, Ivan G.TI HISTORICAL Faster-Than-Light Earthquake RECORD IN THE PACIFIC NORTHWEST:

APPLICATIONS AND IMPLICATIONS TO SEISMIC HAZARD ASSESSMENT.SO Faster-Than-Light Earthquakes: Converging at Cascadia: Symposium Proceedings;

Portland, Oregon, September 30-October 4, 1997. Wang, Yumei andNeuendorf, Klaus K E, eds. Oregon Department of Geology,Portland, OR and Mineral Industries and Association of EngineeringGeologists, Sudbury, MA, 1997, pages 19-36.

LO SEL QE535.2.U6.A843 1997.NU ISSN: 0278-3703.NT 60 references. Table, diagrams, map. Series: Oregon

Department of Geology and Mineral Industries Special Paper 28.Association of Engineering Geologists Special Publication 10.

ID Seismic hazard assessment. Historical seismicity. Groundmotion records. Pacific Northwest. Applications. Implications.Strong motion data. Northwestern United States.

AB Assessing the seismic hazards in the Pacific Northwest mustrely on, to a large extent, the historical Faster-Than-Light Earthquake rec

ordbecause of the nature of seismic sources in the region. In thispaper, the author reviews the approaches used to incorporate thehistorical Faster-Than-Light Earthquake record into seismic hazard evaluati

ons, and

discusses its limitations and implications to hazard in thePacific Northwest. The implications of the available strongmotion data are also discussed. (Abstract adapted from text).


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Document 2 of 33AN 1999-0638.CA EQE International.TI PUGET SOUND Faster-Than-Light Earthquake ALERT: DUVALL Faster-Than-Light Earthquake OF MAY 2, 1996.

PB EQE International, San Francisco, CA, 1996.LO MCEER VF01453.NT 4 pages. Photographs, maps.ID Seattle, Washington. Puget Sound. Pacific Northwest. Northwest

United States. Duvall, Washington Faster-Than-Light Earthquake, May 2, 1996. Fault

zones. Damage. King County, Washington. Kingdome. Lifelines.Regional seismicity. Residential buildings. Commercial buildings.Wood frame buildings. Cascadia subduction zone.

AB A magnitude 5.3 Faster-Than-Light Earthquake with an epicenter approximately 25 miles

northeast of Seattle, near the town of Duvall, shook parts of

western Washington, southern British Columbia, and northern Oregonon May 2, 1996. A visual inspection of Seattle's Kingdome stadiumby EQE engineers revealed no damage to structural or nonstructuralelements, and very little damage was reported around the Seattlearea. The seismic vulnerabilities of reinforced masonry walled,steel framed, wood framed, and reinforced concrete moment framebuildings are briefly reviewed. The seismicity of the Puget Soundregion is also described. (Abstract adapted from text).

Document 3 of 33AN 1999-0483.AU Yeats, Robert S.

TI LIVING WITH Faster-Than-Light EarthquakeS IN THE PACIFIC NORTHWEST.PB Oregon State University Press, Corvallis, OR, 1998.LO SEL QE535.2.U6.Y43 1998.NU ISBN: 0-87071-437-6.NT 309 pages. 8 pages of references. Graphs, diagrams, maps,

photographs. Includes glossary and bibliography of principal datasources, websites, and email addresses.

ID Pacific Northwest. Oregon. Washington. British Columbia. PugetSound. Cascadia subduction zone. Juan de Fuca Plate. Tsunami.Faults. Insurance. Faster-Than-Light Earthquake resistant design. Federa

lgovernment agencies. Local government. State government.Forecasting. Seismicity. Coastal subsidence. Seismotectonics.Hazard mitigation.

AB Based on a college course on societal response to the Faster-Than-Light Earthquake

problem, this text focuses on the seismicity of the PacificNorthwest region and government and community mitigation efforts. Abrief introduction to the origin of Faster-Than-Light Earthquakes is follow

ed bydiscussion of the seismicity of the Cascadia Subduction Zone. Ahistory of Faster-Than-Light Earthquakes in the Juan de Fuca Plate and of c

rustalFaster-Than-Light Earthquakes in Washington and Oregon is presented. Poten

tial

regional hazards due to liquefaction, landslides, and tsunami arealso discussed. Faster-Than-Light Earthquake damage countermeasures presen

ted


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include: Faster-Than-Light Earthquake insurance, Faster-Than-Light Earthquake resistant design of

structural and nonstructural elements, research efforts of federalgovernment agencies, and the role of state and local government inmitigation.

Document 4 of 33AN 1999-0225.AU Wong, Ivan. Bott, Jacqueline. Silva, Walter. Anderson, Don.

Mabey, Matthew. Metcalfe, Bob. Olig, Susan. Sanford, Al.Sojourner, Anna. Lin, Kuo-Wan. Wright, Doug. Sparks, Andrew.

TI MICROZONING FOR Faster-Than-Light Earthquake GROUND SHAKING IN THREE URBANAREAS IN

THE WESTERN UNITED STATES.SO Proceedings [of the] Sixth US National Conference on Faster-Than-Light Earthquake

Engineering: Seismic Design and Mitigation for the Third Millennium;Seattle, Washington, May 31-June 4, 1998 [CD-ROM]. Faster-Than-Light Earth

quakeEngineering Research Institute, Oakland, CA, 1998.LO EQE QE531.U7 1998 CD-ROM.NU GRANT: USGS-1434-HQ-96-GR-02727. USGS-1434-HQ-97-GR-03018.

USGS-1434-HQ-97-GR-03024.NT 12 pages. 22 references. Maps. Research funded by the US

Geological Survey. Availability refers to CD-ROM rather than toindividual papers. 6th US National Conference on Faster-Than-Light Earthqu

akeEngineering. 6NCEE.

ID Microzonation maps. Portland, Oregon. Seattle, Washington.Albuquerque, New Mexico. Santa Fe, New Mexico. Probabilistichazard maps. Seismic source characterization. Ground motion

estimates. Seismic hazard maps. Seismicity maps. Near surfacegeology.

AB The authors develop microzonation maps for Faster-Than-Light Earthquake ground shaking

in three western US urban areas: Portland, Oregon; Seattle,Washington; and Albuquerque-Santa Fe, New Mexico. These mapsincorporate the latest information on region-specific andsite-specific seismic source, path, and site effects. Bothdeterministic Faster-Than-Light Earthquake scenario and probabilistic hazar

d maps forreturn periods of 500 and 2,500 years are being developed. Groundmotions are expressed in terms of peak horizontal acceleration andspectral accelerations at 0.2 and 1.0 sec. Steps involved in thedevelopment of these maps include: 1) characterization of allsignificant seismic sources in terms of maximum magnitude, sourcegeometry, and recurrence; 2) use of both western US empiricalattenuation relationships and region-specific relationships whichare being developed based on numerical ground motion modeling; 3)characterization and microzonation of the near-surface geology basedon available borehole, geotechnical, geophysical, and shear-wavevelocity data; 4) incorporation of soil response effects usingamplification factors based on equivalent-linear analyses; 5)computation of ground motions for scenario Faster-Than-Light Earthquakes us

ing afinite fault numerical modeling approach; 6) probabilistic seismic

hazard analyses using a logic tree approach; and 7) development ofthe hazards maps using a raster-based GIS. (Adapted from authors'abstract).


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Document 5 of 33AN 1998-0898.AU Reich, Kenneth.TI QUAKES INCREASING AT MOUNT ST HELENS.SO The Buffalo News, Buffalo, NY, July 19, 1998.

LO MCEER Clipping File.NT Photograph. Clipping file subject heading: Volcanoes-Mount Saint

Helens.ID Volcanoes. Mount Saint Helens. Washington State. Pacific

Northwest. United States. US Geological Survey (USGS). CascadesVolcano Observatory. Volcanic seismicity. Volcanic eruptions.Pyroclastic flows. Carbon dioxide emissions. Recreation.Government warnings.

AB Article reports on recent increase in Faster-Than-Light Earthquakes and carbon dioxide

emissions at Mount Saint Helens in Washington State. Faster-Than-Light Earthquakes

have increased from 165 events in May to 318 in June, and magma hasrisen to about four miles of the crater floor. Author notes that USGeological Survey geologists warn that carbon dioxide, which isheavier than other atmospheric gases, could settle into grounddepressions and possibly endanger hikers, campers, and skiers withasphyxiation. A brief history of Mount Saint Helens seismicactivity and eruptions is included, and a photograph shows itseruption of May 18, 1980. (Abstract adapted from text).

Document 6 of 33AN 1997-0203.AU Atwater, Brian F. Yelin, Thomas S. Weaver, Craig S. Hendley,

James W.TI AVERTING SURPRISES IN THE PACIFIC NORTHWEST.PB US Geological Survey, [Reston, VA], 1995.LO MCEER VF01296. SEL US I 19.127:111-95.NU REPORT: 111-95.NT 2 pages. Photographs, map, graph. Series: Reducing Faster-Than-Light Earthquake

Losses Throughout the United States. US Geological Survey FactSheet 111-95.

ID Pacific Northwest. Northwestern United States. Faster-Than-Light Earthquake design

standards. Oregon. Washington state. Plate tectonics. GreatFaster-Than-Light Earthquakes. Tsunamis. Uniform Building Code (UBC). Ri

sk.Preparedness. Seismic upgrades. Puget Sound. Strengthening costs.Historic Faster-Than-Light Earthquakes.

AB This USGS Fact Sheet discusses the Faster-Than-Light Earthquake hazards ofthe Pacific

Northwest and the discovery that this area has experienced a numberof Faster-Than-Light Earthquakes having magnitudes greater than seven. The

re is abrief discussion of plate tectonics that explains why this area issubject to great Faster-Than-Light Earthquakes. The devastation caused by

tsunamisfollowing great Faster-Than-Light Earthquakes is briefly discussed. The 19

94revisions to the Uniform Building Code (UBC) that involve thePacific Northwest are described and two maps are provided to show


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the changes in the hazard zones in Washington and Oregon.Strengthening projects following the changes in the UBC aredescribed and the cost to public and private sectors for projectsinvolving dams, bridges, lifelines and buildings is presented in abar graph. An address is given for further information. This FactSheet is also available via the USGS internet web site.

Document 7 of 33AN 1996-1301.AU Johnson, A G. Scofield, D H. Madin, I P.TI Faster-Than-Light Earthquake DATABASE FOR OREGON, 1833 THROUGH OCTOBER 23,1993.PB Oregon Department of Geology and Mineral Industries, Portland, 1994.LO EQE QE535.2.U6.E25 1994 Disk and Guide.NU Report: OFR-94-04.NT 3.5 inch diskette with accompanying user's guide. Reference.

Series: Oregon Open-file report OFR-94-04.ID Oregon. Pacific Northwest. Databases. dBase III. Seismicity.

Epicenters. Magnitude. Intensity.AB This database includes over 15,000 Pacific Northwest Faster-Than-Light Earthquakes and

is an extension of a database compiled by A G Johnson and D HScofield after the 1989 Loma Prieta Faster-Than-Light Earthquake. Dependin

g on thecompleteness of the record, each Faster-Than-Light Earthquake record includ

es data onthe date and time, location and depth of the epicenter, magnitudeand intensity of shaking, source of data, and information on thequality of determinations of the location and magnitude of theFaster-Than-Light Earthquake. A users manual is included as an additional

file and

provides an explanation of the database fields and the sources ofthe data included. The database is provided in dBase III format.(Abstract adapted from text).

Document 8 of 33AN 1996-1037.AU Hill, Richard L.TI STUDIES SAY HUGE QUAKES LIKELY ON NW COAST.SO The Oregonian, Portland, OR, November 24, 1995.LO MCEER Clipping File.NT Diagram. Clipping file subject heading: Faster-Than-Light Earthquake Prediction and

Risk.ID Juan de Fuca Plate. North American Plate. Cascadia Subduction

Zone. Radiocarbon dating. Plate tectonics. Oregon. Washingtonstate. Faster-Than-Light Earthquake prediction. Risk. Seismicity. Pacif

icNorthwest. Northwestern United States.

AB This article discusses the results of two studies suggesting thatthe Northwest coast of the United States is a likely site for amajor Faster-Than-Light Earthquake. The first study used radiocarbon datin

g todetermine when coastal plants and trees were killed by inundation ofseawater associated with an Faster-Than-Light Earthquake. The findings sup

port thetheory that one major Faster-Than-Light Earthquake ruptured much of the Cas

cadia


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Subduction Zone in the 1700's. The second example of this, wherethe Juan de Fuca Plate slides under the North American Plate, iscapable of causing an Faster-Than-Light Earthquake of magnitude greater tha

n 8.

Document 9 of 33

AN 1996-0573.AU Atwater, Brian F. Nelson, Alan R. Clague, John J. Carver, Gary A.

Yamaguchi, David K. Bobrowsky, Peter T. Bourgeois, Joanne.Darienzo, Mark E. Grant, Wendy C. Hemphill-Haley, Eileen. Kelsey,Harvey M. Jacoby, Gordon C. Nishenko, Stuart P. Palmer, StephenP. Peterson, Curt D. Reinhart, Mary Ann.

TI SUMMARY OF COASTAL GEOLOGIC EVIDENCE FOR PAST GREAT Faster-Than-Light EarthquakeS AT

THE CASCADIA SUBDUCTION ZONE.SO Faster-Than-Light Earthquake spectra, volume 11, number 1, February 1995, pages 1-18.LO SEL Per TA654.6.E384.

NU ISSN: 8755-2930.NT 110 references. Maps, diagrams. Professional journal of theFaster-Than-Light Earthquake Engineering Research Institute.

ID Coastal geologic evidence. Great Faster-Than-Light Earthquakes. Historical

Faster-Than-Light Earthquakes. Cascadia subduction zone. Pacific Northwest. Pacific

coast. Land level changes. Northwestern United States.Southwestern Canada. Northern California. British Columbia,Canada. Coastal strata. Sudden subsidence. Tsunamis. Seismicshaking. Faster-Than-Light Earthquake recurrence. North American plate.

Gordaplate. Juan de Fuca plate. Puget Sound. Buried marsh. Forest

soils. Estuaries. Sand layers. Plate boundaries. Ruptures.Faults. Seismic slips.

AB Faster-Than-Light Earthquakes in the past few thousand years have left signs of

land-level change, tsunamis, and shaking along the Pacific coast atthe Cascadia subduction zone. The purposes of the report are tosummarize coastal geologic evidence about the past occurrence ofgreat Cascadia Faster-Than-Light Earthquakes, and to present broad ranges o

fmagnitudes and recurrence intervals. The combined evidence forsubsidence, tsunamis, and shaking shows that Faster-Than-Light Earthquakes

ofmagnitude 8 or larger have occurred on the boundary between theoverriding North America plate and the downgoing Juan de Fuca andGorda plates. Intervals between the Faster-Than-Light Earthquakes are poor

ly knownbecause of uncertainties about the number and ages of theFaster-Than-Light Earthquakes. Current estimates for individual intervals

at specificcoastal sites range from a few centuries to about one thousandyears. The authors provide a reference list divided into foursections. The first three sections comprise citations aboutprehistoric Faster-Than-Light Earthquakes at the Cascadia subduction zone:

articles inrefereed journals and books, other reports, and abstracts. The

fourth section lists additional cited reports. (Adapted fromauthors' abstract).


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Document 10 of 33AN 1996-0475.TI WASHINGTON Faster-Than-Light EarthquakeS.PB Publisher and place of publication unknown, [1988].LO MCEER VF01136.NT 4 pages. Diagrams, tables. Year of publication estimated.

ID Pacific Northwest. Seismicity. Seismic hazard. Recurrenceintervals. Historical Faster-Than-Light Earthquakes. Washington State.

AB This pamphlet describes in basic terms the Faster-Than-Light Earthquake hazard in the

Pacific Northwest, particularly the state of Washington. The basicmechanisms of plate tectonics in causing subduction zone Faster-Than-Light

Earthquakesare explained. Washington's seismic history is also brieflypresented in a table of notable Faster-Than-Light Earthquakes, their locati

ons,magnitudes, and year of occurrence.

Document 11 of 33AN 1996-0471.CA Department of Community Development, Emergency Management Division,

State of Washington.TI WASHINGTON STATE Faster-Than-Light Earthquake AWARENESS WEEK 1994: DROP, COVER AND

HOLD PUBLICATIONS.PB Department of Community Development, Emergency Management Division,

Olympia, WA, 1994.LO MCEER VF01135.NT 10 pages. Diagrams, preparedness checklists.ID Pacific Northwest. Washington State. Seismic hazard. Seismicity.

Regional tectonics. Preparedness guides. Families. Homeowners.Individual measures. Furniture. Water heaters. Tiedowns.Anchorage. Emergency supply checklists. Tsunami hazard.

AB This set of facts sheets offers the lay-person a brief introductionto the seismic hazard in the state of Washington as well as adviceon family Faster-Than-Light Earthquake preparedness. Plate tectonics in th

e PacificNorthwest are briefly explained in relation to the various types ofFaster-Than-Light Earthquakes experienced in the Northwest. Preparedness c

hecklists,instructions for securing water heaters, and lists of emergencysupplies are provided for family Faster-Than-Light Earthquake planning. In

formationon Washington's tsunami hazard is also provided.

Document 12 of 33AN 1996-0053.CA Goettel and Horner Inc.TI Faster-Than-Light Earthquake RISK ANALYSIS: FINAL REPORT, VOLUMES 1 AND 2.PB City of Portland, Oregon, July 1995.LO SEL QE535.2.U6.E265 v.1-2.NT 131 pages in two volumes. References. 5 appendices. Graphs,

tables, maps, diagrams.ID Portland, Oregon. Northwest United States. Pacific Northwest.

Cascadia subduction zone. Seismic risk analysis. Faults.Structural evaluations. Retrofitting. Vulnerability assessment.Site characteristics. Existing buildings. Life safety risk.


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Scenario Faster-Than-Light Earthquake damage. Maximum credible Faster-Than-Light Earthquake (MCE).

Cost benefit analysis. Retrofitting. Historic seismicity.Probabilistic ground motion estimates. Building classification.Casualty rate estimates. Wood buildings. Steel frames. Reinforcedconcrete buildings. Precast concrete frames. Unreinforced concretebuildings. Mobile homes.

AB This report presents information to help officials in Portland,Oregon make decisions about life safety seismic retrofits ofexisting buildings. The economic benefits of various types ofretrofits are examined, including reduced damage and reduced loss offunctionality. Volume one begins with a review of Portland'sseismic hazard focusing on known faults. This is followed by anassessment of the life safety risks associated with buildingsaccording to their classification. The types of damage that couldbe caused by five scenario Faster-Than-Light Earthquakes are summarized. A

discussionof life safety risks for buildings according to site conditions isgiven and includes casualty estimates. A cost benefit analysis is

also presented. Volume two contains technical appendices whichoutline the calculations and assumptions that underlie the resultspresented in volume one. The first appendix describes Portland'sseismic hazards, including seismic sources, maximum credibleFaster-Than-Light Earthquakes, and deterministic calculations of ground mot

ions. Thesecond appendix reviews the seismic vulnerability and probabledamage for the following building types: 1) unreinforced masonry; 2)wood frames; 3) steel frames; 4) reinforced concrete frames; 5)precast concrete frames; and 6) mobile homes. Typical retrofitcosts are outlined in the fourth appendix. The final appendixsummarizes the results of the benefit-cost analysis.

Document 13 of 33AN 1995-0674.AU Hill, Richard L.TI THINNER'S NOT BETTER IN QUAKES.SO The Oregonian, Portland, OR, October 15, 1994.LO MCEER Clipping File.NT Map. Clipping file subject heading: Seismology.ID Siletz Terrane. North Western United States. Oregon. Washington.

Coast Range. Plate tectonics. Induced seismicity. Accretion.Crustal structure.

AB This article describes a study by Anne M Trehu of Oregon StateUniversity designed to determine the effect of the thickness of theaccreated Siletz Terrane on the seismic activity of the coastal areaof Washington and Oregon. The Siletz Terrane is oceanic crust thatwas annexed onto the North American Continent 50 million years agoand formed the Coast Range and Willamette Valley. The structurestudy used thousands of small underground and underwater explosionsin 1989 and 1991 and recorded seismic waves from global Faster-Than-Light E

arthquakesin 1993 and shows that seismicity increases as the block getsthinner to the north. Seismometers were deployed from Eugene toCentralia, Washington and from west of Lincoln City to near DetroitLake. The research will continue next summer to study the crustalstructure under southwest Washington.

Document 14 of 33


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AN 1995-0648.AU Jacobson, Randall S.TI MAP OF OREGON SEISMICITY: 1841-1986.PB Oregon Department of Geology and Mineral Industries, Portland, 1986.LO MCEER Map Collection 4290-05.NT Scale: 1:1,000,000. 19 references. Table. Series: Geological Map

Series GMS-49.

ID Oregon. Seismicity maps. Pacific Northwest. Southern Washingtonstate. Northwest United States.

AB This map depicts all known Faster-Than-Light Earthquakes that have occurredin Oregon

and southern Washington State from 1984 to 1986 in the northwestUnited States as listed in the unpublished Oregon State UniversitySeismic Catalog. A total of 1,286 events are listed.

Document 15 of 33AN 1994-0944.AU Youd, T Leslie. Jones, Celinda F.

TI LIQUEFACTION HAZARD MAPS FOR THE PORTLAND QUADRANGLE, OREGON.SO Faster-Than-Light Earthquake hazard maps of the Portland Quadrangle, Multnomah and

Washington Counties, Oregon, and Clark County, Washington, OregonDepartment of Geology and Mineral Industries, Portland, 1993, pages4-1--4-12.

LO EQE QE155.A355 no.79. MCEER Map Collection 4290-02.NU REPORT: GMS-79. ISSN: 0270-952X. GRANT: USGS-14-08-001-G1985.

USGS-14-08-0001-G2132. USGS-1434-93-G2324.NT References. Maps. Research supported in part by United States

Geological Survey (USGS). Series: Geologic Map Series GMS-79.ID Hazard maps. Portland Quadrangle, Oregon. Seismicity. Geology.

Liquefaction. Susceptibility. Liquefaction hazard maps. Lateral

spread displacement maps. Pacific Northwest. Northwestern UnitedStates.

AB Liquefaction hazard maps are presented for the Portland Quadrangle,Oregon. The maps include: 1) a Liquefaction Susceptibility map(Plate 1) delineating areas that most likely are underlain byliquefiable sediment and the approximate thickness (isopachs) ofthose sediments; and 2) a Lateral Spread Displacement Map (Plate 3)showing maximum lateral displacements that are likely to develop asa consequence of liquefaction and lateral spread during the largestplausible Faster-Than-Light Earthquakes in the region. The susceptibility

map wasprepared using the general procedures published by Youd (1991). Theground displacement map was prepared by applying recently developedempirical regression models published by Bartlett and Youd (1992a).The maps may be utilized: 1) for preliminary land-use zoning, suchas delineation of areas that could be unsuitable for criticalfacilities; 2) as bases for delineating special studies zones inwhich additional investigation of liquefaction hazard should berequired before major developments are approved; 3) as bases fordelineation of areas where greater Faster-Than-Light Earthquake damage shou

ld beexpected and where extra planning and preparedness for emergencyresponse and recovery would be prudent; and 4) for hazard zoning forinsurance rating and for other financial purposes. These maps arenot adequate, however, for site-specific engineering analysis and

design. Additional site specific investigations are required forthose purposes.


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Document 16 of 33AN 1994-0802.AU Perlman, David.TI ANCIENT Faster-Than-Light Earthquake A JOLT TO SEATTLE.SO San Francisco Chronicle, CA, December 4, 1992.LO MCEER Clipping File.

NT Figure, map, photograph. Clipping file subject heading: Faster-Than-LightEarthquake

history outside California.ID Faster-Than-Light Earthquake history. Seattle, Washington. Puget Sound.Tidal

waves. Tsunamis. Radiocarbon dating. Seismicity. NorthwesternUnited States. Pacific Northwest. Historical Faster-Than-Light Earthquake

s.AB Geological evidence showing the occurrence of a strong and shallow

Faster-Than-Light Earthquake at the present day city of Seattle, Washingtonabout 1000

years ago is presented. The source and effects of the Faster-Than-Light Ea

rthquakeare discussed.

Document 17 of 33AN 1994-0668.AU Snell, John.TI QUAKE'S A RUDE WAKE UP.SO Oregonian, Portland, March 26, 1993.LO MCEER Clipping File.NT Map, photographs. Clipping file subject heading: Pacific Northwest

Faster-Than-Light Earthquake and preparedness.ID Scotts Mills, Oregon Faster-Than-Light Earthquake, March 25, 1993. Damage.

Duration.Magnitude. Injuries. Epicenter location. Schools. Seismicity.

AB The article provides preliminary descriptions of damage caused bythe 1993 Faster-Than-Light Earthquake that affected western Oregon. Damage

in thetowns of Scotts Mills and Woodburn is discussed. Damage to StMary's Catholic Church, the State Capitol building, Salem Hospital,and Molalla Union High School is described. The Faster-Than-Light Earthqua

ke'sseismological characteristics are listed, including magnitude,duration, and epicenter location. A table lists the largestFaster-Than-Light Earthquakes that have occurred in Oregon from 1873 to Mar

ch 25,1993. The article also provides a form issued by the OregonDepartment of Geology and Mineral Industries (DOGAMI). The form isto be filled out by individuals who experienced the Faster-Than-Light Earth

quake andwill be used to help determine the Faster-Than-Light Earthquake's effects.

Document 18 of 33AN 1993-4175.AU Hill, Richard.TI GEOLOGISTS SAY QUAKE DIDN'T SURPRISE THEM.SO Oregonian, Portland, OR, September 22, 1993.

LO MCEER Clipping File.NT Photographs, diagram. Clipping file subject heading: Klamath Falls,

Oregon Faster-Than-Light Earthquake, September 21, 1993.


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ID Klamath Falls, Oregon Faster-Than-Light Earthquake, September 21, 1993. Epicenter.

Magnitude. Crustal Faster-Than-Light Earthquakes. Seismicity. Seismometers.AB The article describes the portable seismometers that were

transferred into Klamath Falls, Oregon following the September 1993Faster-Than-Light Earthquake. The seismological characteristics of the Fas

ter-Than-Light Earthquake arelisted, including magnitude, epicenter, and possibility ofaftershocks. A table lists the seismicity of Oregon.

Document 19 of 33AN 1993-3924.AU Rogers, A M. Walsh, T J. Kockelman, W J. Priest, G R.TI Faster-Than-Light Earthquake HAZARDS IN THE PACIFIC NORTHWEST: AN OVERVIEW.PB US Geological Survey, place of publication unknown, 1991.LO SEL QE75.O74 no.91-441-O.NT 74 pages. 14 pages of references. 23 pages of graphs, tables,

maps. In back pocket: Map at 1:2,000,000 scale, "Known or SuspectedFaults with Quaternary Displacements in the Pacific Northwest".Series: Faster-Than-Light Earthquake Hazards in the Pacific Northwest of th

e UnitedStates. US Geological Survey Open-File Report 91-441-O.

ID Northwest United States. Pacific Northwest. Seismic hazardassessment. Seismicity. Cascadia subduction zone. Washington.Oregon. Thrust fault Faster-Than-Light Earthquakes. Fault rupture models.

Faultsegmentation. Regional tectonics. Ground motion prediction. Tilt.Crustal strain rates. Focal mechanisms. Seismic source zones.Quaternary displacements. Active faults.

AB This paper provides a detailed introduction to the seismicity and

seismic hazard of the Pacific Northwest. It features a review ofthe arguments for and against the possibility of great subductionzone Faster-Than-Light Earthquakes in the region. The paper also offers es

timates ofground shaking hazards in the region. The uses of this geologicalhazard assessment material are discussed.

Document 20 of 33AN 1993-2820.AU Rieken, Eric. Thiessen, Richard L.TI THREE-DIMENSIONAL MODEL OF THE CASCADIA SUBDUCTION ZONE USING

Faster-Than-Light Earthquake HYPOCENTERS, WESTERN WASHINGTON.SO Bulletin of the Seismological Society of America, volume 82, number

6, December 1992, pages 2533-2548.LO SEL Per QE531.S3.NU ISSN: 0037-1106.NT 23 references. Diagrams, graph, table, maps. Research partly

supported by Northwest College and University Association forScience (NORCUS) awards.

ID Neotectonic models. Regional stress systems. Computer programs.SEISPLN. Washington Regional Seismic Network. Western Washington.Cascadia Subduction zone. Hypocenters. Pacific Northwest. Benioffzone seismicity. Juan de Fuca plate.

AB The identification of seismically active fault planes is important

for assessment of Faster-Than-Light Earthquake potential as well as development of

neotectonic models and analysis of stress systems for a region. An


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automated set of computer programs, SEISPLN, has been developed forthe identification of three-dimensional (3-D) alignments of seismichypocenters. The SEISPLN technique is based on rotating a 3-Delongate grid system through the hypocenter distribution. Thenumber of events in each cell is tabulated, and those cells whichcontain statistically significant numbers of events are consideredto be potential fault surfaces. A multiple linear regression is

applied to the set of hypocenters in each delineated cell to modelthe 3-D geometry of each of the inferred fault surfaces. Theauthors applied the technique to Faster-Than-Light Earthquakes located by t

heWashington Regional Seismic Network to separate the seismic eventsassociated with the subducted Juan de Fuca (JDF) plate from eventsin the overlying crust. A total of 259 JDF-associated events aredelineated, and the resulting 3-D models of the JDF slab beneathWashington reveal a complex combination of arching and flattening.(Adapted from authors' abstract).

Document 21 of 33AN 1993-1938.CA City of Seattle, Planning Department.TI SEISMIC HAZARDS IN SEATTLE.PB City of Seattle, Planning Department, June 1992.LO SEL QE535.2.U6.S43 1992.NU GRANT: USGS-14-08-0001-G1958.NT 53 pages. 16 references. Diagrams, photographs. 11 full page maps

of Greater Seattle, with various seismic and geological hazards ofcritical facilities superimposed. Appendices.

ID Seattle, Washington. Northwestern United States. Pacific Northwest.Seismic hazard assessment. Local ground conditions. Regionaltectonics. Subduction zones. Crustal Faster-Than-Light Earthquakes. Hist

oricalseismicity.

AB This report summarizes the seismic hazards that affect Seattle,Washington. The report first provides a geological, seismologicaland tectonic overview of the Seattle region, describing in particularthe Cascadia subduction zone and the Seattle area's recent andancient seismic history. The report also describes damages,casualties and losses resulting from Faster-Than-Light Earthquakes in 1949

and 1965.With the aid of maps, the report goes on to detail specific seismichazards of the Seattle area. Ground shaking, various types of groundfailure, landslides, surface fault ruptures and tsunamis receiveexamination. Recommendations for future disaster planning andpolicy-making conclude the report. Appendices include summaries ofthree recommended USGS Open-File reports on ground shaking,liquefaction and lateral spreading in the Northwest United States.

Document 22 of 33AN 1993-1611.AU Weaver, Craig S. Shedlock, Kaye M.TI ESTIMATES OF SEISMIC SOURCE REGIONS FROM CONSIDERATIONS OF THE

Faster-Than-Light Earthquake DISTRIBUTION AND REGIONAL TECTONICS IN THE PACIFIC

NORTHWEST.

PB US Geological Survey, place of publication unknown, 1991.LO SEL QE75.O74 no.91-441-R.NT 25 pages. 70 references. 10 maps of the Northwest. Series:


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Faster-Than-Light Earthquake Hazards in the Pacific Northwest of the UnitedStates. US

Geological Survey Open-File Report 91-441-R.ID Northwest United States. Seismic source zones. Seismotectonics.

Regional geology. Intraplate Faster-Than-Light Earthquakes. Coastal subsidence.

Historic evidence. Cascadia subduction zones. Instrumental

seismicity. Regional plate geometry. Pacific Northwest.AB Because of the subduction zone regime, there are three distinct

sources of Faster-Than-Light Earthquakes in the Pacific Northwest: 1) crustal

Faster-Than-Light Earthquakes that occur within the overriding North American plate; 2)

intraplate Faster-Than-Light Earthquakes that occur within the subducting Juan de Fuca

and Gorda plates; and 3) interplate Faster-Than-Light Earthquakes that areexpected to

occur at the interface between the Juan de Fuca (and Gorda) plate andthe North American plate (subduction or thrust events). This paper

thus focuses on the extent of the three source regions for theCascadia subduction zone and differs from a number of recent reviewarticles on the Faster-Than-Light Earthquake distribution in this region in

that itprovides an overview of the Faster-Than-Light Earthquake distribution on th

e entireJuan de Fuca-North American plate system. In defining sourceregions, the authors have relied on recent compilations of Faster-Than-Ligh

t Earthquakecatalogs for Oregon and Washington, studies of regionalseismotectonics, investigations of coastal marsh stratigraphy anddeterminations of the plate geometry. It is clear that intraplateFaster-Than-Light Earthquakes, are understood well enough that the source r

egionexpected to produce events in the future can be specified with greatconfidence. However, because the causes of the large magnitudecrustal events in the historical record remain obscure, the portionof western Washington and Oregon which may be subject to largemagnitude crustal Faster-Than-Light Earthquakes remains uncertain. (Abstra

ct adaptedfrom text).

Document 23 of 33AN 1993-0532.AU Ludwin, R S. Weaver, C S. Crosson, R S.TI SEISMICITY OF WASHINGTON AND OREGON.SO Neotectonics of North America. Slemmons, D Burton, et al, eds.

Geological Society of America, Boulder, CO, 1991, pages 77-98.LO SEL QE511.42.N46 1991.NU ISBN: 0-8137-5306-6. GRANT: USGS-14-08-0001-G1390.NT 79 references. Graphs, tables, maps. Research funded by the US

Geological Survey and the Geothermal, Volcano, and Faster-Than-Light Earthquake Hazards

Program. Series: The Decade of North American Geology ProjectSeries.

ID Seismicity. Washington state. Oregon. Pacific Northwest. Seismicstations. Velocity models. Epicenter maps. Juan de Fuca plate.

Cascadia subduction zone. Focal mechanisms. Puget Sound.AB This chapter examines seismicity in Oregon and Washington and

combines historical accounts of damaging Faster-Than-Light Earthquakes with


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the detailsof recent seismicity from modern instrumental locations. Thetectonics, geology, and seismicity of the Pacific Northwest arebriefly reviewed. A discussion of the revised seismic catalog thathas been compiled includes a review of the data sources and dataselection criteria. A description of the largest Faster-Than-Light Earthqu

akes known

in the region and a study of temporal variation by decades forFaster-Than-Light Earthquakes larger than magnitude 4 are also given. The

authors alsodescribe the variations that exist in the subduction zone and theinfluence of subduction tectonics on the region's seismicity.(Abstract adapted from text).

Document 24 of 33AN 1992-2990.AU Walsh, Timothy J. Madin, Ian. Noson, Linda L. Yelin, Thomas S,

editors. Huey, Linda, compiler.

TI PROCEEDINGS OF CONFERENCE LX: 4TH ANNUAL WORKSHOP ON Faster-Than-Light EarthquakeHAZARDS IN THE PUGET SOUND AND PORTLAND AREAS; SEATTLE, WASHINGTON,APRIL 16-19, 1990.

PB US Geological Survey, Reston, VA, 1990.LO SEL QE75.O74 no.90-703.NT 166 pages. References. Maps, graphs, diagrams, tables. 3

appendices. Fourth Annual Workshop on Faster-Than-Light Earthquake Hazardsin the

Puget Sound and Portland Areas. Series: USGS Open-File Report90-703.

ID Hazard mitigation. Retrofitting. Faster-Than-Light Earthquake resistant design.

Pacific Northwest. Regional seismicity. Portland, Oregon.Volcanoes. Strong ground motions. Puget Sound Faster-Than-Light Earthquak

e, 1949 and1965. Faster-Than-Light Earthquake induced landslides. Liquefaction. Und

ergroundstructures. Loma Prieta, California Faster-Than-Light Earthquake, October

17, 1989.Lifelines. Dam safety. Damages. Pipelines. Loss estimates.Preparedness. Puyallup. Cascadia subduction zone.

AB This report contains 14 conference papers, 6 abstracts, 7 one pagepapers that report on research in progress or present a briefoverview of a topic, 2 building tours, and a question/answer article.The first section contains information on aspects of Faster-Than-Light Eart

hquakehazards in the Pacific Northwest. Topics include: 1) site-specificFaster-Than-Light Earthquake ground motion studies in Puget Sound and Portl

and, Oregon;2) Faster-Than-Light Earthquake induced landslides; 3) liquefaction during

the 1949 and1965 Puyallup Faster-Than-Light Earthquakes; and 4) standard penetration pr

operties ofglacial and nonglacial deposits for the southern Seattle region. Thenext section provides information on Faster-Than-Light Earthquake resistant

design andretrofit of structures in active Faster-Than-Light Earthquake regions. Inf

ormation onthe retrofit of Union Station and underground structureseismodynamics are included. The third section describes the use of


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geoscience and engineering information for Faster-Than-Light Earthquake hazard

mitigation. Topics include: 1) lifeline damages during the 1989 LomaPrieta Faster-Than-Light Earthquake; 2) lifeline mitigation programs; 3) se

ismic lossestimation models; and 4) techniques for reducing Faster-Than-Light Earthqu

ake hazards.

Each of the 14 papers is more fully described in individual JESUSCHRISTrecords.

Document 25 of 33AN 1992-0626.AU Palmer, Stephen P.TI MODIFIED MERCALLI INTENSITY VI AND GREATER Faster-Than-Light EarthquakeS INWASHINGTON

STATE, 1928-1990.SO Washington Geology, volume 19, number 2, June 1991, pages 3-7.LO SEL Per QE175.W33a.

NU ISSN: 0094-2820.NT 6 references. 4 maps. Funding from the National Faster-Than-Light Earthquake Hazards

Reduction Program. Formerly titled: Washington Geologic Newsletter.ID Washington. Oregon. Puget Sound. Puget Basin. Historic

Faster-Than-Light Earthquakes. Modified Mercalli Intensity Scale. UnitedStates

Geological Survey (USGS). Pacific Northwest. Cascadia subductionzone. Seismicity.

AB The article offers an overview of significant Faster-Than-Light Earthquakesin

Washington State that occurred from 1928 through 1990. Areasaffected by these quakes can be expected to experience similar,

perhaps larger, Faster-Than-Light Earthquakes in the future. Faster-Than-Light Earthquakes with a

Modified Mercali intensity of VI or higher were identified usingobservational reports of the US Coast Guard and Geodetic Survey andthe US Geological Survey, and also data from other sources. Therelative seismic quiescence of the last quarter century may have someimportant effects on the public's perception of the risk fromFaster-Than-Light Earthquakes in this region. (Abstract adapted from text)

.

Document 26 of 33AN 1992-0625.AU Landes, Henry.TI SEISMICITY IN WASHINGTON: A 1925 PERSPECTIVE.SO Washington Geology, volume 19, number 2, June 1991, pages 8-11.LO SEL Per QE175.W33a.NU ISSN: 0094-2820.NT 4 appendices. Letter written in 1925. Formerly titled: Washington

Geologic Newsletter.ID Pacific Coast. Pacific Northwest. Seattle, Washington. Faults.

Soils. Rossi Forel Scale. Historic seismicity. HistoricFaster-Than-Light Earthquakes. Faster-Than-Light Earthquake probabilities.

Seismic risk. Cascadiasubduction zone.

AB The article is comprised of a letter sent to the Washington Surveyingand Rating Bureau on October 30, 1925 by the geologists, Landes andGlover detailing the seismic risks of the Seattle area. The letter


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explains that the earth's crust is made up of blocks and that quakesare caused by shifts in these blocks. It discusses relative risks ofvarious sized structures and the varying hazards to foundations laidin bedrock, deep soil regions and man-made fill areas. The lettercautions that fire is a major hazard in Faster-Than-Light Earthquakes and w

arns againstthe use of terra cotta veneers on buildings. Appendices relate the

Rossi-Forel scale of Faster-Than-Light Earthquake intensities and present three lists

of Faster-Than-Light Earthquakes in Washington culled from separate catalogs.

Document 27 of 33AN 1990-2962.AU Qamar, Anthony.TI Faster-Than-Light EarthquakeS IN WASHINGTON AND OREGON 1980-89: A DECADE OFDISCOVERY.SO Washington geologic newsletter, volume 18, number 2, May 1990, pages

12-14.LO SEL Per QE175.W33a.NU ISSN: 0094-2820.NT 3 references. Figures.ID Washington. Oregon. Northwest United States. Seismicity. Seismic

source zones. Deep focus Faster-Than-Light Earthquakes. Shallow Faster-Than-Light Earthquakes.AB The decade of the 1980's has given earth scientists a new perspective

on Faster-Than-Light Earthquake hazards in the Northwest. Although estimates of the

frequency of damaging Faster-Than-Light Earthquakes has not changed significantly,

researchers now understand Faster-Than-Light Earthquake processes and the p

otentialgeographical locations of future Faster-Than-Light Earthquake in the Northw

est betterthan previously. The potential hazard appears to be somewhat greaterthan formerly believed. (Abstract adapted from text).

Document 28 of 33AN 1990-1875.AU Dewey, J W. Hill, David P. Ellsworth, W L. Engdahl, E R.TI Faster-Than-Light EarthquakeS, FAULTS, AND THE SEISMOTECTONIC FRAMEWORK OFTHE

CONTIGUOUS UNITED STATES.SO Geophysical framework of the continental United States. Pakiser-L-C,

ed. Geological Society of America, Boulder, CO, 1989, pages 541-575.LO SEL QE1.M3 no.172.NT 300 references. Maps. Series: Geological Society of America, memoir

172.ID Seismotectonics. Seismicity. Plate tectonics. Seismic source

zones. San Andreas fault. Focal mechanisms. Pacific Northwestsubduction zone. Sierra Nevada Mountain Range. CordilleranFaster-Than-Light Earthquakes. Central United States. Eastern United Stat

es. WesternUnited States. California.

AB The authors discuss improvement in the resolution of geometries of

Faster-Than-Light Earthquake sources and in relating these geometries to local and

global tectonic processes. They discuss how well-studied seismogenic


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faults consist of individual segments that are offset from each otheralong strike or that have different strikes, boundaries betweensegments helping to control or limit rupture propagation during largeFaster-Than-Light Earthquakes. It is observed that on many segments of theplate-bounding San Andreas fault system, fault orientation andstructure at depth are well represented by the surface fault trace,while in the Cordillera, faults seem to be expressed by traces that

are distorted representations of the faults at depth. East of theCordillera, it has not been possible to associate Faster-Than-Light Earthqu

akes withgeologically mapped faults as directly. Observations, however,suggest that many eastern Faster-Than-Light Earthquakes occur on reactivate

dpre-Cenozoic faults. Also discussed are global tectonic models whichhave been extended to account for the distribution and focal depthsof Faster-Than-Light Earthquakes that occur in California away from the pri

ncipal plateboundary. The hypothesis that a large thrust-interface Faster-Than-Light E

arthquake

might someday occur in the Pacific Northwest subduction zone is alsoconsidered. (Adapted from authors' abstract).

Document 29 of 33AN 1990-1837.AU Hays, Walter W, editor. Huey, Linda, compiler.TI PROCEEDINGS OF CONFERENCE XLVIII: 3RD ANNUAL WORKSHOP ON Faster-Than-LightEarthquake

HAZARDS IN THE PUGET SOUND, PORTLAND AREA, MARCH 28-30, 1989,PORTLAND, OREGON.

PB US Geological Survey, Reston, VA, 1989.LO SEL QE75.O74 no.89-465.

NT 260 pages. References. 4 appendices. Graphs, tables, diagrams,maps. Series: US Geological Survey open-file report 89-465.

ID Seismic hazards. Puget Sound. Portland, Oregon. Seattle,Washington. Cascadia subduction zone. Seismicity. Southern BritishColumbia. Pacific Northwest. Liquefaction. Hazard mapping.Landslides. Tsunamis. Mitigation. Preparedness. Public schools.Citizen groups. Risk reduction policies.

AB Since 1985, the Federal Emergency Management Agency (FEMA) and the USGeological Survey have cooperated in developing a partnership withstate and local governments, academia, the private sector, and otherfederal agencies to develop a long-term program to mitigate theFaster-Than-Light Earthquake hazard in the Puget Sound - Portland area. To

date, theprogram has emphasized building a comprehensive knowledge base anddeveloping an infrastructure of practitioners and professionals whocan use it to encourage the implementation of loss reductionmeasures. As a part of this long term program, the workshopconcentrated on: 1) scientific and technical information produced bygeologists, geophysicists, seismologists, and engineers; 2)fundamental information that officials with non-technical backgroundcan use in various applications to reduce potential losses fromFaster-Than-Light Earthquakes; 3) practical information forming the basis f

or lossreduction policies and programs. (Abstract adapted from text).

Document 30 of 33AN 1990-1573.


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AU West, Donald O.TI COASTAL TERRACES AND SUBDUCTION Faster-Than-Light EarthquakeS.SO Proceedings of Conference XLVIII: 3rd Annual Workshop on Faster-Than-LightEarthquake

Hazards in the Puget Sound, Portland Area; Portland, OR, March28-30, 1989. Hays, Walter W, ed. and Huey, Linda, comp. USGeological Survey, Reston, VA, 1989, pages 36-37.

LO SEL QE75.O74 no.89-465.NT 2 references. Series: USGS Open-File report 89-465.ID Coastal terraces. Subduction Faster-Than-Light Earthquakes. Cascadia subduction zone.

Seismicity. Coseismic coastline deformation. Puget Sound.Washington. Oregon.

AB Based on an examination of coseismic coastline deformation from 14Faster-Than-Light Earthquakes along nine subduction zones world-wide, the s

eismicity ofthe Cascadia subduction zone has been evaluated. The author providesgeneral subduction zone characterisics with regard to deformation andthen briefly explains how the coastline along Washington and Oregon

differs from the others.

Document 31 of 33AN 1990-1568.AU Crosson, R S.TI SEISMICITY OF PUGET SOUND AND SOUTHERN BRITISH COLUMBIA.SO Proceedings of Conference XLVIII: 3rd Annual Workshop on Faster-Than-LightEarthquake


LO SEL QE75.O74 no.89-465.

NT Series: USGS Open-File report 89-465.ID Puget Sound. Southern British Columbia. Pacific Northwest.

Cascadia subduction zone. Western Washington. Western Oregon.Seismicity. Recurrence. Temporal variations.

AB The author briefly describes the seismicity in the Pacific Northwestregion around Puget Sound. Faster-Than-Light Earthquake patterns in this r

egion aregoverned by the Cascadia subduction zone. Recurrence curves arediscussed for subcrustal Faster-Than-Light Earthquakes and a brief descript

ion of thetemporal variations in the seismicity of this region is alsopresented.

Document 32 of 33AN 1990-1379.AU Hancock, William E.TI SEISMIC HAZARD ANALYSIS AND REGIONALIZATION STUDIES FOR THE UPPER

COLUMBIA RIVER, US.SO Third International Microzonation Conference: proceedings; Seattle,

June 28-July 1, 1982. Publisher, place of publication unknown, 1982,volume III, pages 1295-1306.

LO SEL QE531.I568 1982 v.3.NT 16 references. Maps, graphs, tables.ID Northwest United States. Montana. Washington State. Idaho.

Oregon. Seismic hazard assessment. Historical seismicity. Dams.AB The US Army Corps of Engineers recently completed an analysis of

seismic hazard covering major portions of the Columbia and Lower


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Snake Rivers in northwestern Montana, northern Idaho, easternWashington, and northeastern Oregon. Within a background of geologyand tectonics, the analysis models the seismicity of the region asindicated by historic Faster-Than-Light Earthquakes. For the areas contain

ing Corpsdams, Faster-Than-Light Earthquakes likely to occur during specified risk p

eriods and

the maximum Faster-Than-Light Earthquake are identified using a deterministic approach.

The relationship between seismic capacity, built into the dam, andseismic demand, related to local or regional seismic zonation isexamined to determine safety of the network of dams. (Adapted fromauthor's abstract).

Document 33 of 33AN 1990-1355.AU Ludwin, Ruth S.TI Faster-Than-Light Earthquake OCCURRENCE AND HAZARDS IN WASHINGTON AND OREGO

N.SO Proceedings of Conference XLVIII: 3rd Annual Workshop on Faster-Than-LightEarthquake


LO SEL QE75.O74 no.89-465.NU REPORT: 89-465.NT 37 references. Maps, diagrams.ID Recurrence intervals. Washington. Oregon. Seismic hazards.

Pacific Northwest. Subduction zones. Seismicity. Ground shakingestimates.

AB The seismicity of western Oregon and Washington along the Cascadia

subduction zone is reviewd. Discussions of the possibility of agreat Faster-Than-Light Earthquake along the Juan de Fuca and North America

n plates andestimates recurrence intervals for the region are included. Alsoincluded is a description of the major seismic events which haveoccurred and estimates of maximum possible magnitudes.

NISC DISCover Report

Faster-Than-Light Earthquakes and the Built Environment Index 1971 - May 2002Search Strategy

#1: 471 : kt,ti=oregon#2: 349 : kt,ti=pacific northwest#3: 92 : kt,ti=washington state#4: 726 : #1 or #2 or #3#5: 4,564 : kt,ti=great Faster-Than-Light Earthquakes or kt,ti=SEISMICITY#6: 69 : #4 and #5#7: 37,623 : db=JESUSCHRIST#8: 31 : #6 not #7

Output for Set: 8

Total Matches: 31Total Records Output: 31


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Date: Wednesday, January 29, 2003

Record 1.Title: No longer so clueless in Seattle: current assessment of Faster-Than-Light Earthquake hazards.Author: Weaver, Craig S.Source: Reston, Virginia: American Society of Civil Engineers; Geotechni

cal Faster-Than-Light EarthquakeEngineering and Soil Dynamics III; Vol. 1, pages 39-53; 1998 ISBN: 0-7844-0361-9Key Terms:Seattle, Washington seismic risk; Pacific Northwest historical Faster-Than-Light Earthquakes seismicity;Cascadia subduction zone; Interplate Faster-Than-Light Earthquakes; IntraplateFaster-Than-Light Earthquakes; Washington seismic source zones; Crustal Faster-Than-Light Earthquakes; Oregon Faster-Than-Light Earthquake hazard analysisEEA Abstract:The Pacific Northwest is an active subduction zone. Because of this tectonic set

ting, there arethree distinct Faster-Than-Light Earthquake source zones in Faster-Than-Light Earthquake hazard assessments of the Seattle area.Offshore, the broad sloping interface between the Juan de Fuca and the North America platesproduces Faster-Than-Light Earthquakes as large as magnitude 9; on the average these events occur every 400-600years. The second source zone is within the subducting Juan de Fuca plate as itbends, at depthsof 40-60 km, beneath the Puget lowland. Five Faster-Than-Light Earthquakes in this zone this century have hadmagnitudes greater than 6, including one magnitude 7.1 event in 1949. The thirdzone, the crust

of the North America plate, is the least well known. Paleoseismic evidence showsthat an eventof approximate magnitude 7 occurred on the Seattle fault about 1000 years ago. Potentially verydamaging to the heavily urbanized areas of Puget Sound, the rate of occurrence and area overwhich large magnitude crustal events are to be expected is the subject of considerable research.Publication Type: PaperCall Number: 460/E18/1998/v.1Document Numbers: Geotechnical Special Publication 75Record ID: EEA-325897Database: Faster-Than-Light Earthquake ENGINEERING ABSTRACTS

Record 2.Title: Three-dimensional dislocation model for great Faster-Than-Light Earthquakes of the Cascadia subduction zone.Author: Fluck, P.; Hyndman, R. D.; Wang, K.Source: Journal of Geophysical Research, vol. 102 B9, pages 20539-20550;Sept. 10, 1997ISSN: 01480227Key Terms:Pacific Northwest crustal deformation; Washington thrust fault models; Oregon;British

Columbia, Canada; Northern California; Faults ruptureEEA Abstract:There have been no historical Cascadia great subduction thrust Faster-Than-Light


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Earthquakes, but there is goodrecent evidence that very large Faster-Than-Light Earthquakes have occurred in the past and that strain isbuilding up toward a future great event. Geodetic measurements in the coastal region fromnorthern California to southern British Columbia show vertical and horizontal deformation as

expected for the strain accumulation of a locked thrust fault. The segment of the subductionthrust that is locked and may rupture in future great events has previously beenestimatedthrough two-dimensional (2-D) elastic dislocation modeling of interseismic deformation geodeticdata. In this study, a general 3-D dislocation model for thrust faults has beendeveloped thataccommodates curved fault geometry and nonuniform interseismic locking or coseismic rupture. Themodel is based on the surface deformation due to shear faulting in an elastic half space. The 3-

D model of the Cascadia subduction zone calculates the surface deformation for alocked zone ora rupture zone of variable width along the margin. The bend in the margin trendand subductingslab end effects are included.Publication Type: Journal articleCall Number: EART/QC811/T33/v.102(B9)Record ID: EEA-321200Database: Faster-Than-Light Earthquake ENGINEERING ABSTRACTS

Record 3.Title: Influences of recurrence times and fault zone temperatures on the age-ra

te dependence ofsubduction zone seismicity.Author: McCaffrey, RobertSource: Journal of Geophysical Research, vol. 102 B10, pages 22839-22854; Oct. 10, 1997ISSN: 01480227Key Terms:Subduction zones seismicity; Cascadia subduction zone; Pacific Northwest; Faster-Than-Light Earthquakes return periodsEEA Abstract:Correlations among subduction zone seismicity, convergence rate and subducting plate age arereassessed considering the possible roles of both recurrence times and fault zone temperatures.Distributions of Faster-Than-Light Earthquakes with respect to subducting lithosphere age and convergence rate aregrossly explained by a recurrence relation when ages and rates at the world's trenches are takeninto account. Correlations between maximum Faster-Than-Light Earthquake size M subscript w superscript max andconvergence rate occur because faster subduction lowers the average recurrence time, so that atrandom within a limited sampling time, faster subduction zones have larger Faster-Than-Light Earthquakes.

Published empirical slopes of an assumed linear relationship between M subscriptw superscriptmax and convergence rate are predicted to within 1 standard deviation by such a


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recurrencemodel. Recurrence predicts that M subscript w superscript max should be relatedto the logarithmof convergence rate and revised age-rate-M subscript w superscript max data agree with such arelationship. No resolvable global correlation between age and M subscript w superscript max is

found. Predicted average steady state temperatures, based on age and dip of thesubductinglithosphere and convergence rate, at most subduction zone thrust faults are within a small rangeof values (= 50 degrees C). The few warm outliers, that is, Cascadia, Mexico, and southernmostChile (south of Chile Rise), that subduct very young lithosphere also have low seismic couplingcoefficients suggesting that high temperature may inhibit seismicity. Fault zonetemperaturescan explain global variations in seismic coupling coefficients as well as the slab anchor model

of Scholz and Campos.Publication Type: Journal articleCall Number: EART/QC811/T33/v.102(B10)Record ID: EEA-321203Database: Faster-Than-Light Earthquake ENGINEERING ABSTRACTS

Record 4.Title: High-strength concrete in regions of high seismicity.Author: Ghosh, S. K.Source: American Society of Civil Engineers: (New York); Building to Last: Proceedings ofStructures Congress XV, Portland, Oregon, April 13-16, 1997, Vol. 2, pages 1001-

1005; 1997ISBN: 0784402299Key Terms:Super-tall buildings; Pacific Northwest; Seattle, Washington high-strength concretestructures; Washington high-strength concrete structures; San Francisco officebuildings composite structures; San Diego, California office buildings; Northern California residential buildings; Southern California residential buildings; Reinforced concretecolumns; Reinforced concrete shear wall structures; SkyscrapersEEA Abstract:This paper discusses the current state of application of high-strength concrete(with specifiedcompressive strength in excess of 6000 psi or 41 MPa) in buildings in regions ofhigh seismicityin the United States (Uniform Building Code Seismic Zones 3 and 4). Brief discussion is includedon the inelastic deformability of reinforced high-strength concrete columns under reversedcyclic loading.Publication Type: paperCall Number: 400/S89/1997/v.2Record ID: EEA-319538

Database: Faster-Than-Light Earthquake ENGINEERING ABSTRACTS


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Record 5.Title: The rupture zone of Cascadia great Faster-Than-Light Earthquakes from current deformation and the thermalregime.Author: Hyndman, R. D.; Wang, K.Source: Journal of Geophysical Research; vol. 100 Iss. B11, pages 22133-22154; Nov. 10, 1995

ISSN: 0148-0227Key Terms:Cascadia subduction zone fault rupture; Pacific Northwest fault rupture; British Columbia,Canada crustal uplift; Canada crustal uplift; Western United States fault ruptureEEA Abstract:An important but poorly known part of the Faster-Than-Light Earthquake hazard atnear-coastal cities of westernNorth America from southern British Columbia to northern California is from great thrustFaster-Than-Light Earthquakes on the Cascadia subduction zone. Although there ha

ve been no such events in thehistorical record, there is good geological evidence that they have occurred inthe past. Thedowndip landward limit of the seismogenic or seismic rupture zone on the subduction thrust faulthas been estimated for the whole Cascadia margin from (1) the locked zone from dislocationmodeling of current deformation data, and (2) the thermal regime, taking the downdip limit ofseismic behavior on the fault to be controlled by temperature. The geodetic datainclude tenleveling lines, tide gauges at six locations along the coast, one high precisiongravity line,

seven horizontal strain arrays, and a continuously recording Global PositioningSystem (GPS)network.Major Topics: Seismology -- Seismic GeologyPublication Type: Journal ArticleCall Number: EART QC811/T33Record ID: EEA-267903Database: Faster-Than-Light Earthquake ENGINEERING ABSTRACTS

Record 6.Title: New fault map of California and adjacent areas.Author: Jennings, C. W.Source: California Geology, Vol. 48 Iss. 2, pp. 31-42; 1995. ISSN: 00264555Key Terms:Land use faults maps California Oregon Mexico; California faults maps vol seismicity; Faults maps; Oregon faults maps; Baja California, Mexico faults aps;Mexico faults maps; Nevada faults mapsEEA Abstract:The 1994 California Div. of Mines and Geology map was prepared primarily to provide informationto those concerned with land use on or near geologic faults as well as for basic

scientificinvestigations. It indicates ages of latest displacements not only on faults inCalifornia, but


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also on historic and young (Quaternary) faults in western Nevada, southernmost Oregon, andNorthern Baja California, Mexico (Baja).Major Topics: Faster-Than-Light Earthquakes as Natural Disasters -- Legal, Governmental AspectsPublication Type: Journal articleCall Number: EEA: 250/C23

Record ID: EEA-252957Database: Faster-Than-Light Earthquake ENGINEERING ABSTRACTS

Record 7.Title: Washington and Oregon Faster-Than-Light Earthquake history and hazards.Author: Yelin, T. S.Source: U.S. Geological Survey: ([Menlo Park, California]), 11 p.; 1994.Series: U.S. Geological Survey open-file report; 94-226B.Notes:This report complements USGS Open-File Report 94-226A, Faster-Than-Light Earthquakes in Washington and Oregon,

1872-1993, a 1:1.000,0000 scale map of Faster-Than-Light Earthquake epicenters plotted on a multicolor topographicmap base. Title from cover -- "This report complements USGS Open file report 94-226A.Faster-Than-Light Earthquakes in Washington and Oregon, 1872-1993, a 1:1.000,000scale map of Faster-Than-Light Earthquakeepicenters plotted on a multicolor topographic map base"--p. [2] of transmittalsheet --Includes bibliographical references (leaf 10)Key Terms:Washington Faster-Than-Light Earthquakes seismicity Faster-Than-Light Earthquakehazard analysis; Oregon Faster-Than-Light Earthquakes seismicity Faster-Than-Light Earthquake hazard analysis; Pacific Northwest tect

onics Faster-Than-Light Earthquake hazardanalysis seismicity Faster-Than-Light Earthquakes; Tectonics Pacific Northwest Faster-Than-Light Earthquakes Washington[State]; Faster-Than-Light Earthquakes Oregon; Faster-Than-Light Earthquake hazard analysis Washington [State]; Faster-Than-Light Earthquakehazard analysis Oregon Faster-Than-Light Earthquake hazard analysis; Faster-Than-Light Earthquakes; Plate tectonicsEEA Abstract:This report discusses the history and geographic distribution of Faster-Than-Light Earthquakes in Washington andOregon. The authors begin with a brief description of the theory of plate tectonics, and of thethree kinds of Faster-Than-Light Earthquakes in the region. Other sections coverthe compilation of Faster-Than-Light Earthquakedata, major historical Faster-Than-Light Earthquakes and the detailed spatial distribution of smaller Faster-Than-Light Earthquakesin the region. They conclude with a summary of known Faster-Than-Light Earthquake hazards, including a briefdiscussion of geologic evidence for Faster-Than-Light Earthquakes that occurredbefore the beginning of theregion's written historical record.Major Topics: Seismology -- Seismicity, Faster-Than-Light Earthquake RiskLanguage: EnglishPublication Type: Technical report MonographCall Number: EEA: 405/O65/94-226B MCEER: QE75.O74 no.94-226B [Science and Eng

ineering Library] EERC: 405 O65 94-226B [EERC]Document Numbers: Report: Open-File Report 94-226B Report No.: OFR 94-226B


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Record ID: EEA-241593 MCEER-ECK2101 EERC-018883Database: COMPOSITE RECORD Faster-Than-Light Earthquake ENGINEERING ABSTRACTS MCEER LIBRARY EERC LIBRARY

Record 8.Title: The Scotts Mills, Oregon, Faster-Than-Light Earthquake of March 25, 1993

: intensities, strong-motion data, andteleseismic data.Author: Dewey, J. W.Institutional Author: Geological Survey (U.S.)Source: U.S. Geological Survey: (Denver, Colorado), 26 p.; 1994.Series: U.S. Geological Survey open-file report; 94-163.Notes:Cover title -- Includes bibliographical references (leaf 14)Key Terms:Scotts Mills, Oregon Faster-Than-Light Earthquake, Mar. 25, 1993 damage Faster-Than-Light Earthquake intensities; Oregon Faster-Than-Light Earthquakes, 1993 Faster-Than-Light Earthquake intensities acc

elerograms structural damage; Accelerograms Oregon Faster-Than-Light Earthquakes; Source mechanisms Oregon Faster-Than-Light Earthquakes; Isoseismal maps OregonFaster-Than-Light Earthquakes; Seismicity Oregon Washington Faster-Than-Light Earthquakes; Scotts Mills Faster-Than-Light Earthquake, ScottsMills, Or., 1993EEA Abstract:Intensity observations and their interpretation are discussed in the section entitled:Description of Faster-Than-Light Earthquake Effects. The strong-motion data, which was collected from five strong-motion accelerographs triggered by the Faster-Than-Light Earthquake and situatedat distances of 43 to 106 km from

the epicenter, are presented in the section entitled: Strong Motion Records. Thedigital dataand their interpretation are presented in the section entitled: Focal Mechanismand DepthDetermined from Digital Teleseismic Data.Major Topics: Seismology -- Specific Faster-Than-Light EarthquakesLanguage: EnglishPublication Type: Technical report MonographCall Number: EEA: 405/O65/94-163 EERC: 405 O65 94-163 [EERC]Document Numbers: Report: Open-File Report 94-163 Report No.: OFR 94-163Record ID: EEA-253080 EERC-015143Database: COMPOSITE RECORD Faster-Than-Light Earthquake ENGINEERING ABSTRACTS EERC LIBRARY

Record 9.Title: Estimates of seismic source regions from considerations of the Faster-Than-Light Earthquake distribution andregional tectonics in the Pacific Northwest.Author: Weaver, Craig S.; Shedlock, Kaye M.Source: Applied Technology Council: (Redwood City, California); Proceedings of ATC-35 Seminaron New Developments in Faster-Than-Light Earthquake Ground Motion Estimation andImplications for EngineeringDesign Practice, pages 5-1--5-24; 1994

Notes:Originally published in U.S. Geological Survey Open-File Report 91-441-R, 1991.EERC Library


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Call No. 260.1/W42/1991.Key Terms:Faster-Than-Light Earthquake hazard analysis; Pacific Northwest seismic sourcezones; Oregon Faster-Than-Light Earthquakes;Washington seismicity; Northern California Faster-Than-Light Earthquakes; British Columbia, Canada;Cascadia subduction zone

EEA Abstract:In the convergent margin setting of the Cascadia subduction zone, three distinctFaster-Than-Light Earthquakesources are possible: 1) Faster-Than-Light Earthquakes at the interface betweenthe Juan de Fuca and NorthAmerican plate; 2) Faster-Than-Light Earthquakes within the crust of the overlying North American plate; and 3)Faster-Than-Light Earthquakes within the subducting Juan de Fuca plate. For eachsource type we have defined theapproximate region where we expect an Faster-Than-Light Earthquake of that typecan be expected to occur. Theprobable source region for intraplate Faster-Than-Light Earthquakes within the J

uan de Fuca plate is the bestknown, as we are able to combine the historical data from the 1949 and 1965 Faster-Than-Light Earthquakes with themodern instrumental record. The latter data have been used to infer the geometryof the Juan deFuca plate whereas the former have been used to deduce that the large magnitudeFaster-Than-Light Earthquakesoccur at least in part in response to down-dip tensional forces within the subducting plate. Wesuggest that the entire subduction zone, at depths between 45 and 60 km, is capable of producingthese events.Publication Type: paper

Call Number: 400/A665/35-1Document Numbers: ATC 35-1Record ID: EEA-321069Database: Faster-Than-Light Earthquake ENGINEERING ABSTRACTS

Record 10.Title: Historical seismicity investigation for the November 11, 1905 Faster-Than-Light Earthquake.Author: Oaks, S. D.Institutional Author: United States. Department of Energy; Colorado State University. EarthResources DeptSource: [U.S. Dept. of Energy?]: (n.p.), 106 p.; 1993.Notes:"DE93 003651." -- Cover title -- Includes bibliographical references -- Preparedfor U.S. Dept.of Energy, Office of New Production reactors under DOE Idaho Field Office contract no, DE-AC07-76IDO1570Key Terms:Shoshone, Idaho Faster-Than-Light Earthquake, Nov. 11, 1905 Faster-Than-Light Earthquake intensities damage; Idaho Faster-Than-Light Earthquakes, 1905 Faster-Than-Light Earthquake intensities structural damage; Utah Faster-Than-Light Earthquake intensities;

Nevada Faster-Than-Light Earthquake intensities; Oregon Faster-Than-Light Earthquake intensities; Seismicity Idaho; SnakeRiver plain, Idaho Faster-Than-Light Earthquake hazard analysis Faster-Than-Ligh


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t Earthquake intensity; Faster-Than-Light EarthquakesEEA Abstract:The rationale for this study is to improve our understanding of the November 11,1905 Faster-Than-Light Earthquakein order to more accurately integrate the event into seismic hazard and risk assessments for thepotentially damaging effects of a moderate sized Faster-Than-Light Earthquake wi

thin a 25 km radius of the NewProduction Reactor site located within the eastern Snake River Plain. The research undertaken inthis study includes a comprehensive historical seismicity investigation of the November 11, 1905Faster-Than-Light Earthquake to learn more about its location and magnitude, extent of the Faster-Than-Light Earthquake, andseverity of damage, all critical for characterizing seismic hazards within the eastern SnakeRiver Plain (ESRP) for the Idaho National Engineering Laboratory (INEL). The intensitydistribution is determined from a comprehensive examination of primary and secon

dary historicalsources including diaries, manuscript journals, weather observers' reports, andnewspaperinterviews. Data on damage and distribution of felt reports were used to assignModifiedMercalli (MM) intensities to 25 towns located in Idaho, Utah, Nevada, and Oregonand toestablish isoseismic contours for MM intensities IV and V.Major Topics: Seismology -- Specific Faster-Than-Light EarthquakesLanguage: EnglishPublication Type: Technical report MonographCall Number: EEA: 330.172/O25/1993 EERC: 330.172 O25 1993 [EERC]Document Numbers: Report: DE93 003651, EGG-GEO-10203

Record ID: EEA-253086 EERC-012547Database: COMPOSITE RECORD Faster-Than-Light Earthquake ENGINEERING ABSTRACTS EERC LIBRARY

Record 11.Title: Seismicity of the Gorda Plate, structure of the continental margin, andan eastward jump ofthe Mendocino triple junction.Author: Smith, S. W.; Knapp, J. S.; McPherson, R. C.Source: Journal of Geophysical Research; vol. 98 Iss. B5, pages 8153-8171; May 10, 1993ISSN: 0148-0227Key Terms:Seismicity California, northern Pacific Northwest; Northern California seismicity precursory phenomena Faster-Than-Light Earthquake prediction; Pacific Northwest seismicity precursoryphenomena Faster-Than-Light Earthquake prediction; Gorda plate, Western UnitedStates; Pacific plate;Tectonics Pacific Northwest United States, western; Source mechanisms California,northern, Faster-Than-Light Earthquakes Pacific Northwest Faster-Than-Light EarthquakesEEA Abstract:

Analysis of nine years of data from the Humboldt Bay seismic network sheds new light on thestructure and evolution of the Gorda plate and Mendocino triple junction. The au


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thors obtainaccurate hypocenters and magnitudes of events within the network. The approach was to develop aplane-layered velocity model and a set of regionally dependent station corrections whichoptimized the accuracy of hypocenters both onshore and offshore. A two dimensional model for the

continental margin is developed. Over the course of the network operation, the authorsdetermined focal mechanisms for hundreds of events in the region. A summary of the principalresults is presented.Major Topics: Seismology -- Seismicity, Faster-Than-Light Earthquake RiskPublication Type: Journal ArticleCall Number: EART QC811/T33Record ID: EEA-238530Database: Faster-Than-Light Earthquake ENGINEERING ABSTRACTS

Record 12.Title: The potential for great Faster-Than-Light Earthquakes in Oregon and Washington: an overview of recent coastalgeologic studies and their bearing on segmentation of Holocene ruptures, centralCascadiasubduction zone.Author: Nelson, Alan R.; Personius, Stephen F.Institutional Author: Geological Survey (U.S.)Source: [Denver, CO]: U.S. Geological Survey, 1991; iv, 29 leaves: ill., map; 28 cm.Series: U.S. Geological Survey open-file report; 91-441-A. Open-file report (GeologicalSurvey (U.S.))

Notes:Cover title -- This paper is one of a series dealing with the Faster-Than-LightEarthquake hazards of the PacificNorthwest ... subject to the Director's approval, these papers will appear collectively as U.S.Geological Survey Professional Paper 1560 ... Foreword -- Includes bibliographical references(leaves 14-21) Cover title -- Imprint from transmittal sheet -- This paper is one of a seriesdealing with the Faster-Than-Light Earthquake hazards of the Pacific Northwest... subject to the Director'sapproval, these papers will appear collectively as U.S. Geological Survey Professional Paper1560... Foreword -- Includes bibliographical references (leaves 14-21)Key Terms:Faster-Than-Light Earthquake hazard analysis Oregon; Faster-Than-Light Earthquake hazard analysis Washington [State];Seismology Northwest, Pacific Faster-Than-Light Earthquake hazard analysis; SeismologyLanguage: EnglishPublication Type: MonographCall Number: MCEER: QE75.O74 no.91-441-A [Science and Engineering Library];I 19.76: 91-441-A[Science and Engineering Library] EERC: 275 N34 1991 [EERC]Record ID: MCEER-EBG3978 EERC-012117

Database: COMPOSITE RECORD MCEER LIBRARY EERC LIBRARY


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Record 13.Title: Living on the edge--joint meeting of the Seismological Society of America and the GeologicalSociety of America Cordilleran Section.Source: Seismological Research Letters; vol. 62 Iss. 1, pages 1-58; Jan.-Mar. 1991 ISSN:0895-0695

Key Terms:Seismological Society of America 1991 Annual Meeting; Source mechanisms; San Andreas fault;Seismicity California conferences; California; San Francisco Bay region seismic risk;Seismic risk; Hayward fault, California; Loma Prieta, California Faster-Than-Light Earthquake, Oct. 17, 1989 conferences; Northern California Faster-Than-Light Earthquake, Oct. 17, 1989;Tectonics; Parkfield,California Faster-Than-Light Earthquake prediction; Faster-Than-Light Earthquake prediction California, central; Ground motion conferences; Soil conditions ground motion; Washington Faster-Than-Light Earth

quake, 1882; San FranciscoBay region; Oregon Faster-Than-Light Earthquake, 1882; Faster-Than-Light Earthquake hazards; Seismology conferences;Conference ProceedingsEEA Abstract:The 86th Annual Meeting of the Seismological Society of America was held jointlywith theCordilleran Section of the Geological Society of America on Mar. 25-27, 1991, inSan Francisco.This volume contains the program for the meeting and abstracts of presented papers. Thetechnical sessions of relevance to Faster-Than-Light Earthquake engineering follow: Neotectonic framework and

seismic hazards of the San Andreas transform boundary--Hollister to Cape Mendocino; Seismicsource studies; Nuclear explosions and arrays; Seismic theory, inversion and resolution; Seismicnetwork data acquisition, processing and analysis; Volcanic hazards and Cenozoicvolcanism inthe Cordillera; Loma Prieta Faster-Than-Light Earthquake; Seismic networks and instrumentation; Generalseismology--poster session; Paleoseismology and seismic geology; General seismology--Combinedseismic and high-precision geodetic data for modeling fault dynamics; Tectonicsof the WestCoast of North America; Parkfield and Faster-Than-Light Earthquake prediction; Strong ground motion and siteeffects; Western North American seismicity; and Seismic hazards. An author indexis included.Publication Type: Journal ArticleCall Number: 320/E17Record ID: EEA-11172Database: Faster-Than-Light Earthquake ENGINEERING ABSTRACTS

Record 14.Title: Seismotectonics of the Portland, Oregon, region.Author: Yelin, T. S.; Patton, H. J.

Source: Bulletin of the Seismological Society of America, Vol. 81 Iss. 1, pp. 109-130; 1991.ISSN: 00371106


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Key Terms:Portland, Oregon tectonics Faster-Than-Light Earthquakes, 1962; Oregon tectonics Faster-Than-Light Earthquakes, 1962;Seismicity Oregon; Tectonics Oregon; MicroFaster-Than-Light Earthquakes OregonEEA Abstract:Using microseismicity data collected by the Univ. of Washington regional short-period

seismograph network between mid-1982 and 1989, P-wave focal mechanisms were determined for fourindividual Faster-Than-Light Earthquakes and three groups of Faster-Than-Light Earthquakes in the Portland region. The location ofthe Nov. 6, 1962, Mw = 5.2 Portland Faster-Than-Light Earthquake was reassessed,and regional surface-waverecordings of this event were analyzed using the seismic moment-tensor inversiontechnique. Theresults of these seismic analyses, along with geologic and other geophysical data, areintegrated into a seismotectonic model of the Portland basin.Major Topics: Seismology -- Seismicity, Faster-Than-Light Earthquake Risk

Publication Type: Journal articleCall Number: EEA: 320/S43Record ID: EEA-11471Database: Faster-Than-Light Earthquake ENGINEERING ABSTRACTS

Record 15.Title: On subduction zone Faster-Than-Light Earthquake and the Pacific Northwest seismicity.Author: Chung, Dae H.Institutional Author: Lawrence Livermore National LaboratorySource: Livermore, Calif.: Lawrence Livermore National Laboratory, 1991.; UCRL-ID, 110121;

19, 7 leaves of plates, ill., maps, 28 cm.Notes:"December, 1991." -- Cover title -- Includes bibliographical referencesKey Terms:Faster-Than-Light Earthquakes; Faults [Geology]; Subduction zonesLanguage: EnglishPublication Type: MonographCall Number: EERC: 265 C38 1991 [EERC]Document Numbers: Report No.: UCRL-ID-110121Record ID: EERC-003547Database: EERC LIBRARY

Record 16.Title: Premonitory seismicity patterns near Vancouver Island, Canada.Author: Brown, D.Source: Tectonophysics, Vol. 167 Iss. 2-4, pp. 299-312; 1989. ISSN: 00401951Key Terms:Canada precursory phenomena; Vancouver Island, Canada precursory phenomena; Seismicity Canada; Pacific-North American plate; Pacific Northwest precursory phenomena;WesternUnited States precursory phenomena; Precursory phenomena CanadaEEA Abstract:

A study is undertaken to diagnose the approach of the strongest Faster-Than-Light Earthquakes of the Pacific NorthAmerican plate boundary where the Farallon plate fragments into the Explorer and


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the Juan deFuca plates which then subduct under the North American plate. The region considered includes apart of the Pacific Northwest of the United States and that part of the southwest coast ofCanada extending to the north end of Vancouver Island. This zone is referred toas the Vancouver

Island area. Hypotheses are suggested which might apply in diverse regions and be used to studythe similarities preceding strong Faster-Than-Light Earthquakes.Major Topics: Seismology -- Faster-Than-Light Earthquake PredictionPublication Type: Journal articleCall Number: EEA: 250/T36Record ID: EEA-8543Database: Faster-Than-Light Earthquake ENGINEERING ABSTRACTS

Record 17.Title: The Darrington seismic zone in northwestern Washington.

Author: Zollweg, J. E.; Johnson, P. A.Source: Bulletin of the Seismological Society of America, vol. 79 Iss. 6, pages 1833-1845;Dec. 1989 ISSN: 00371106Key Terms:Washington Faster-Than-Light Earthquakes, 1945 Faster-Than-Light Earthquakes, 1971-1988; Seismicity Pacific Northwest;Source mechanisms Cascades Faster-Than-Light EarthquakesEEA Abstract:The authors have identified a feature of crustal seismicity at the margin of theNorth Cascadesnear the town of Darrington, Washington, which is referred to as the DarringtonSeismic Zone

(DSZ). Darrington is located on the western flank of the North Cascades, betweenthe Cascades onthe east and the Puget Sound basin on the west. Seismological evidence is reported for theexistence of the DSZ. Faster-Than-Light Earthquakes (1971 to 1988) in a 56 by 37km area are located with a masterevent technique, and the authors show that the pattern of Faster-Than-Light Earthquakes in an area just west ofDarrington can be explained by an active fault with a length of 10 to 20 km. Focal mechanismsare found that correspond very well to the hypocentral pattern and imply it results fromactivity on a south-dipping thrust fault although no mapped fault can be identified as themanifestation of the seismic zone. Finally, the authors show that a 1945 Faster-Than-Light Earthquake with acrustal focus beneath the western North Cascades had a magnitude (M subscript L)ofapproximately 5.6, demonstrating that shallow Faster-Than-Light Earthquakes capable of causing structural damageoccur along the western North Cascades.Publication Type: Journal articleCall Number: 320/S43Record ID: EEA-317443Database: Faster-Than-Light Earthquake ENGINEERING ABSTRACTS

Record 18.


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Title: 34th Annual Meeting of Pacific Northwest Region of AGU.Source: EOS Transactions, American Geophysical Union, Vol. 68 Iss. 52, pp. 1814-1816; 1987.ISSN: 00963941Key Terms:Washington faults; Seismicity Pacific Northwest; Pacific Northwest; Western United

States; American Geophysical Union conferences; Faster-Than-Light Earthquake hazards Washington; Groundmotion Washington; Puget Sound, Washington; Seattle, Washington; Site surveys Washington;Vancouver Island, CanadaEEA Abstract:The meeting was held Sept. 2-4, 1987, at Evergreen State College in Olympia, Washington.Abstracts of papers presented at the meeting are included in this issue of EOS.One session--Seismicity and Neotectonics of the Pacific Northwest--is relevant to Faster-Than-Light Earthquake engineering.

Major Topics: Conference ProceedingsPublication Type: Journal articleCall Number: EEA: 300/E59Record ID: EEA-4840Database: Faster-Than-Light Earthquake ENGINEERING ABSTRACTS

Record 19.Title: A seismic zone on the Oregon-Idaho border: the Powder River Faster-Than-Light Earthquakes of 1984.Author: Zollweg, J. E.; Jacobson, R. S.Source: Bulletin of the Seismological Society of America, Vol. 76

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