Not My Fault: Tickles from the Gorda Plate – a Good Reminder to Plan
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Best Wishes for Another Successful Asian Celebration!
With you for whatever comes next in life. Whatever you’re dreaming of — your first house, first year of college or first day of retirement — we’re here to help you get there. As an OCCU member, you’ll have 24/7 access to your accounts through our free online banking services including Internet Banking, mobile app, mobile deposit and online bill pay, plus 30,000 free ATMs nationwide and people in our branches who are genuinely glad to see you. That’s just the start. OregonCommunityCU.org COLLEGE MORTGAGE REFINANCING AUTO RETIREMENT BUSINESS SERVICES 541.687.2347 • 800.365.1111 Federally Insured by NCUA 2 Contents Main Stage & What’s New 4-5 Atrium Stage . 6 Martial Arts Stage . 7 Kumoricon Room . 8 Children’s Room . 9 THE 2015 OREGON Sponsored by Oregon Community Credit Union ASIAN CELEBRATION COMMITTEE and Copic Markers/Imagination International Chairpersons David Tam & Ardyn Wolfe Children’s Carnival . 9 Site Ken Nagao, Miriam Lasalita Arts & Crafts . 10 Finance Marvy Schuman, Chau Nguyen Arts exhibit sponsored by the University of Oregon Host/Tickets Frances Kucera Publicity/ Carrie Matsushita, David Tam, Asian Heritage & Justice . 11 Sponsors Marvy Schuman, Ardyn Wolfe An Event Is Born . 12-13 Advertising Marvy Schuman Main Stage Roger Yamaguchi, Ken Nagao Cooking Demonstrations . 15 Food Court Mike Takahashi Sponsored by Kikkoman Marketplace Sing Lee, Mengdan Lin Asian Marketplace . 16-17 Art Exhibit Teresa Hsu, Thaston Riklon, Kathy Hoy Food Court . 19 Crafts Jean Lee Children’s Room Shann Ormsbee Partner Events . 20 Martial Arts Alan Best Asian Resource Directory . 22 Asian Heritage Stephen Williamson Cooking Demos Maria Clark Warren, Jodi Willis, Site Map . -
Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information
Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information Index Abancay Deflection, 201, 204–206, 223 Allmendinger, R. W., 206 Abant, Turkey, earthquake of 1957 Ms 7.0, 286 allochthonous terranes, 26 Abdrakhmatov, K. Y., 381, 383 Alpine fault, New Zealand, 482, 486, 489–490, 493 Abercrombie, R. E., 461, 464 Alps, 245, 249 Abers, G. A., 475–477 Alquist-Priolo Act, California, 75 Abidin, H. Z., 464 Altay Range, 384–387 Abiz, Iran, fault, 318 Alteriis, G., 251 Acambay graben, Mexico, 182 Altiplano Plateau, 190, 191, 200, 204, 205, 222 Acambay, Mexico, earthquake of 1912 Ms 6.7, 181 Altunel, E., 305, 322 Accra, Ghana, earthquake of 1939 M 6.4, 235 Altyn Tagh fault, 336, 355, 358, 360, 362, 364–366, accreted terrane, 3 378 Acocella, V., 234 Alvarado, P., 210, 214 active fault front, 408 Álvarez-Marrón, J. M., 219 Adamek, S., 170 Amaziahu, Dead Sea, fault, 297 Adams, J., 52, 66, 71–73, 87, 494 Ambraseys, N. N., 226, 229–231, 234, 259, 264, 275, Adria, 249, 250 277, 286, 288–290, 292, 296, 300, 301, 311, 321, Afar Triangle and triple junction, 226, 227, 231–233, 328, 334, 339, 341, 352, 353 237 Ammon, C. J., 464 Afghan (Helmand) block, 318 Amuri, New Zealand, earthquake of 1888 Mw 7–7.3, 486 Agadir, Morocco, earthquake of 1960 Ms 5.9, 243 Amurian Plate, 389, 399 Age of Enlightenment, 239 Anatolia Plate, 263, 268, 292, 293 Agua Blanca fault, Baja California, 107 Ancash, Peru, earthquake of 1946 M 6.3 to 6.9, 201 Aguilera, J., vii, 79, 138, 189 Ancón fault, Venezuela, 166 Airy, G. -
Perspectives on Managing Natural Hazard Risk in Pacific Rim Countries
GUEST EDITORIAL Living on the Ring of Fire: Perspectives on Managing Natural Hazard Risk in Pacific Rim Countries Douglas Paton University of Tasmania, Australia rom the perspective of studying natural hazards, the peace and tranquillity that might be expected Ffrom a literal translation of its name does not always capture the reality of life for communities on the Pacific Rim. This reality is more readily discerned in its alter ego: the Ring of Fire. The latter leaves one in less doubt as to the hazardous circumstances likely to prevail in this region. In addition to the hazards posed by the numerous volcanoes that resulted in the ‘Ring of Fire’ appellation, communities situated around the Pacific Rim also have to contend with earthquakes, tsunami, storms, cyclones/typhoons, flood and bushfire. To this list of acute events can be added hazards of a chronic nature such as salinity, environmental degradation and sea-level rise that represent growing threats to many Pacific Rim countries. The region also faces increased risk from health-related hazards. Sydney, for example, has been identified as a pandemic hotspot as a result of it being a hub linking the airways of Asia and the United States. Recognition of the risk these hazards pose to Pacific Rim modate this issue and offer insights into how personal, communities has stimulated interest in identifying how to community, societal, cultural and organizational factors facilitate sustainability by developing community and interact to facilitate sustainability. Furthermore, they do societal capacity to co-exist with the potentially hazardous so in a way that supports the growing recognition of a elements in the environment (Paton, 2006a). -
This Report Is Preliminary and Has Not Bee Reviewed for Conformity with US
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Northeast-trending subcrustal fault transects western Washington by Kenneth F. Fox, Jr.* Open-File Report 83-398 This report is preliminary and has not bee reviewed for conformity with U.S Geological Survey editorial standards and stratigraphic nomenclature. *U.S. Geological Survey 3^5 Middlefield Road Menlo Park, California 9^025 Page Table of Contents Tectonic setting......................................................... 1 Seisraicity............................................................... 4 Discussion............................................................... 4 References cited......................................................... 6 Figures Figure 1. Magnetic anomalies in the northeastern Pacific................ 8 Figure 2. Bathymetry at intersection of Columbia lineament and Blanco fracture zone................................................. 9 Figure 3. Plane vector representation of movement of Gorda plate........ 10 Figure 4. Reconstruction of Pacific-Juan de Fuca plate geometry 2 m.y. before present................................................ 11 Figure 5. Epicenters of historical earthquakes with intensity greater than V........................................................ 12 TECTONIC SETTING The north-trending magnetic anomalies of the Juan de Fuca plate are off set along two conspicuous northeast-trending lineaments (fig. 1), named the Columbia offset and the Destruction offset by Carlson (1981). The northeast ward projections of these lineaments intersect the continental area of western Washington, hence are of potential significance to the tectonics of the Pacific Northwest region. Pavoni (1966) suggested that these lineaments were left-lateral faults, and that the Columbia, 280 km in length, had 52 km of offset, and the Destruction, with a length of 370 km, had 75 km of offset. Based on Vine's (1968) correlation of the magnetic anomalies mapped in this area by Raff and Mason (1961), with the magnetic reversal time scale, Silver (1971b, p. -
USF Center for the Pacific Rim
Copyright 1988 -2007 USF Center for the Pacific Rim The Occasional Paper Series of the USF Center for the Pacific Rim :: www.pacificrim.usfca.edu Pacific Rim Report No. 52, January 2009 China’s Relations with Mexico and Cuba: A Study of Contrasts by Adrian H. Hearn, Ph.D. Adrian Hearn is a Senior Research Fellow at the University of Sydney, and Kiriyama Research Fellow at the University of San Francisco Center for the Pacific Rim. Adrian is conducting an anthropological study of the political and cultural implications of China’s deepening engagement with Latin America. Hearn has undertaken research in Cuba (three years), China (ten months), Senegal (one year), and Mexico (eight months), and is currently teaching a course on China-Latin America relations at the Universidad de Baja California. He is the author of Cuba: Religion, Social Capital, and Development (Duke University Press, 2008), China and Latin America: The Social Foundations of a Global Alliance (Duke University Press, forthcoming), and editor of Cultura, Tradición, y Comunidad: Perspectivas sobre el Desarrollo y Participación en Cuba (Imagen Contemporánea and UNESCO Center for Human Development 2008.) We gratefully acknowledge The Kiriyama Chair for Pacific Rim Studies at the USF Center for the Pacific Rim for underwriting the publication of this issue of Pacific Rim Report. In terms of economic openness and political ideology Mexico and Cuba are at opposite ends of the spectrum. Nevertheless, for China both hold high strategic value. Examining China’s relations with Mexico and Cuba opens an analytic window into the way that bilateral commercial, cultural, and diplomatic cooperation programs have adapted to distinct local conditions. -
Detailed Structures of the Subducted Philippine Sea Plate Beneath
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 104, NO. B1, PAGES 1015-1033,JANUARY 10, 1999 Detailed structuresof the subductedPhilippine Sea plate beneath northeast Taiwan' A new type of double seismiczone Honn Kao and Ruey-JuinRau Instituteof Earth Sciences,Academia Sinica, Taipei, Taiwan Abstract. We studiedthe detailedstructure of the subductedPhilippine Sea plate beneath northeastTaiwan whereoblique subduction, regional collision, and back arc openingare all activelyoccurring. Simultaneousinversion for velocitystructure and earthquakehypocenters areperformed using the vast,high-quality data recorded by the TaiwanSeismic Network. We furthersupplement the inversionresults with earthquakesource parameters determined from inversionof teleseismicP and $H waveforms,a criticalstep to definethe positionof plateinterface and the stateof strainwithin the subductedslab. The mostinteresting feature is that relocatedhypocenters tend to occuralong a two-layeredstructure. The upperlayer is locatedimmediately below the plate interfaceand extendsdown to 70-80 krn at a dip of 40ø- 50ø. Below approximately100 km, the dip increasesdramatically to 700-80ø. The lower layer commencesat 45-50 km andstays approximately parallel to the upperlayer with a separationof 15+5 km in betweendown to 70-80 km. Below thatthe separationdecreases andthe two layersseem to graduallymerge into one Wadati-BenioffZone. We proposeto term the classicdouble seismic zones observed beneath Japan and Kuril as "type I" andthat we observedas "typeII," respectively.A globalsurvey indicates that type II doubleseismic zonesare alsoobserved in New Zealandnear the southernmostNorth Island,Cascadia, just northof the Mendocinotriple junction, and the Cook Inlet areaof Alaska. All of them are locatednear the terrniniof subductedslabs in a tectonicsetting of obliquesubduction. We interpretthe seismogenesisof type II doubleseismic zones as reflecting the lateralcompres- sivestress between the subductedplate and the adjacentlithosphere (originming from oblique subduction)and the downdipextension (from slabpulling force). -
On the Dynamics of the Juan De Fuca Plate
Earth and Planetary Science Letters 189 (2001) 115^131 www.elsevier.com/locate/epsl On the dynamics of the Juan de Fuca plate Rob Govers *, Paul Th. Meijer Faculty of Earth Sciences, Utrecht University, P.O. Box 80.021, 3508 TA Utrecht, The Netherlands Received 11 October 2000; received in revised form 17 April 2001; accepted 27 April 2001 Abstract The Juan de Fuca plate is currently fragmenting along the Nootka fault zone in the north, while the Gorda region in the south shows no evidence of fragmentation. This difference is surprising, as both the northern and southern regions are young relative to the central Juan de Fuca plate. We develop stress models for the Juan de Fuca plate to understand this pattern of breakup. Another objective of our study follows from our hypothesis that small plates are partially driven by larger neighbor plates. The transform push force has been proposed to be such a dynamic interaction between the small Juan de Fuca plate and the Pacific plate. We aim to establish the relative importance of transform push for Juan de Fuca dynamics. Balancing torques from plate tectonic forces like slab pull, ridge push and various resistive forces, we first derive two groups of force models: models which require transform push across the Mendocino Transform fault and models which do not. Intraplate stress orientations computed on the basis of the force models are all close to identical. Orientations of predicted stresses are in agreement with observations. Stress magnitudes are sensitive to the force model we use, but as we have no stress magnitude observations we have no means of discriminating between force models. -
Pacific Rim Topic Paper for the National Federation of High
Pacific Rim 1 Pacific Rim Topic Paper For the National Federation of High Schools 2015 Topic Selection Meeting By Chad Flisowski, Galveston-Ball HS When I first began research on this topic, I was initially surprised that the term “Pacific Rim” was a commonly used term of art, as I knew that the many countries bordering the Pacific Basin were very different. Indeed, the 54 countries commonly identified as Pacific Rim come from four different continents and represent vast differences in development and challenges. Because of the size and complexity of this region, as well as the fact that the ground for debate had no clear common factor, led me to consider narrowing the focus while still staying in the same region. After looking at a variety of options, I settled on ASEAN, or the Association of Southeast Asian Nations. Comprised of ten nations – Indonesia, Malaysia, the Philippines, Singapore, Thailand, Brunei, Cambodia, Laos, Myanmar (Burma), and Vietnam – this organization represents an economic region that, according to the ASEAN Community in Figures (2014), would rank as the seventh largest economy if it were a single nation. ASEAN presents several interesting options that I will continue to explore as my research develops. First, it is about to celebrate its 50th year as an organization, since it was founded with the Bangkok Declaration in 1967. Second, it is dedicated to being both an economic and political organization, much like the European Union. Third, it is actively engaged in the region and has strong ties to regional powers like China and Japan. Fourth, among its aims are continued progress in development, education, and security. -
Internal Deformation of the Southern Gorda Plate: Fragmentation of a Weak Plate Near the Mendocino Triple Junction
Internal deformation of the southern Gorda plate: Fragmentation of a weak plate near the Mendocino triple junction Sean P.S. Gulick* Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, Pennsylvania 18015, Anne S. Meltzer USA Timothy J. Henstock* Department of Geology and Geophysics, Rice University, Houston, Texas 77005, USA Alan Levander ABSTRACT Gorda plate that may serve as the northern North-south compression across the Gorda-Paci®c plate boundary caused by the north- limit of in¯uence of the triple junction on the ward-migrating Mendocino triple junction appears to reactivate Gorda plate normal Juan de Fuca±Gorda plate system. Near the faults, originally formed at the spreading ridge, as left-lateral strike-slip faults. Both seis- triple junction, the plate shows evidence of mically imaged faults and magnetic anomalies fan eastward from ;N208E near the Gorda fragmenting (Fig. 1B). ridge to ;N758E near the triple junction. Near the triple junction, the Gorda plate is faulted pervasively and appears to be extending east-southeast as it subducts beneath GORDA PLATE DEFORMATION North America. Continuation of northeast-southwest±oriented deformation in the southern Oceanic crust imaged on seismic lines Gorda plate beneath the continental margin contrasts with the northwest-southeast±trend- MTJ-3, MTJ-5, and MTJ-6 is rough and per- ing structures in the overlying accretionary prism, suggesting partial Gorda±North Amer- vasively faulted (Fig. 3). The crust appears in ican plate decoupling. Southeast of the triple junction, a slabless window is generated by places to be broken into crustal blocks bound- removal of the subducting Gorda plate. -
The Gorda Deformation Zone
The Gorda Deformation Zone Miles Bodmer University of Oregon Goals • Better understand deformation of the Gorda Plate • Look at deformation at a range of depths (crust – lithosphere - asthenosphere) • Highlight some of my research What Makes The Gorda Interesting? • The Gorda is the oceanic plate outboard of southern Cascadia subduction zone • Southern Cascadia is where large megathrust earthquakes are thought to nucleate • 1/3 of the plate configuration that makes up the Mendocino triple junction • Seismically active Modified from Byrnes et al. (2017) Tectonic History • ~10 Ma Pacific plate motion changes • Ridges begin to reorganize • ~5 Ma the Blanco transform develops • ~4 MA Explorer plate breaks off • The Mendocino transform and Gorda ridge fail to reorient Atwater and Stock, 1998 Magnetic Anomalies • Clear bending of anomalies in Gorda • Juan de Fuca shows signs of reorganization • Formation of new segments • Ridge rotation • Pacific side near Gorda does not show similar signs of reorganization • Variable spreading rates Wilson (2002) Gorda Is Stagnating • Gorda motion becomes increasingly independent in the last 3 Ma • At 0.5 Ma the Pacific controls Gorda motion Riddihough (1984) Seismicity Throughout The Plate 1964 – 1980 Star: M 5.7 (Jay Patton http://earthjay.com/) Wilson (1989) Historic seismicity (USGS www.earthquake.usgs.gov) Large Events In The Plate Correlate With Bathymetry Chaytor (http://activetectonics.coas.oregonstate.edu/gorda.htm) Deformation Accommodated By Left-lateral Faults • Bathymetry clearly shows ridges associated with faulting • Ridges appear smoothly deformed, kinked, or undeformed depending on the region • Moment tensors show dominantly left-lateral strike-slip motion with some normal faulting • Faults show clear regions of deformation Chaytor et al. -
Pacific Rim Specialty Cocktails House Infusions Bar Features Inglorious
Pacific Rim Specialty Cocktails Inglorious Cocktails obscure | unknown | unsung Queen of Thorns 11 Raynal VSOP brandy | Barolo Chinato vermouth | sparkling wine | lime juice | rose Red Lotus 9 Poblano Gimlet 12 Arbor vodka | Soho lychee liqueur | cranberry juice | lime wedge Hendrick's Gin | Cocchi Americano Bianco | poblano pepper | lime juice Pimm’s Cup 9 Pimm’s #1 | Fever Tree ginger brew | lemon juice | cucumber Seasonal Gin & Tonic 10 Moletto tomato infused gin | dill | house tonic with cinchona bark, Bee’s Knees 10 lemongrass, citrus, Rose hips Arbor ‘Spring’ gin | lemon juice | honey syrup Summerthyme 12 Martinez 11 Reyka vodka | Momokawa ‘Pearl’ Nigori sake | raspberry | lemon juice | Ransom Old Tom gin | Carpano Antica Formula vermouth | thyme Luxardo Maraschino | house-made blood orange bitters | orange twist Nanas Punch 11 Singapore Sling 10 Barsol pisco | Olmeca Altos Plata tequila | pineapple syrup| lemon juice Bombay ‘Sapphire – East’ gin | Cherry Heering | Bénédictine | lime juice | angostura bitters | soda Bitter Breeze 12 Paper Plane 11 Batavia Arrack sugarcane spirit | Amaro Nonino Quintessentia | lemon Maker’s Mark bourbon | Amaro Nonino Quintessentia | Contratto aperitif | juice | passionfruit | espresso orgeat lemon juice Shochu Lemonade 11 Sazerac 9 Kurokame Honkaku shochu | house lemonade | Madeira | zinfandel Rittenhouse rye | Vieux Carré absinthe | demerara | Peychaud’s bitters | reduction lemon twist Quiet T Please 11 Saratoga 10 House infused Chamomile Quiet Man Irish whiskey | honey syrup | soda Knob Creek -
Mineralogy and Chemistry
State of Oregon Department of Geology and Mi neraf Industries 910 State Office Building 1400 SW Fifth Avenue Port1 and, Oregon 97201 OPEN-FILE REPORT 0-89-09 MINERAL DEPOSITS RECOVERED FROM NORTHERN GORDA RIDGE: MINERALOGY AND CHEMISTRY Martin R. Fi sk and Katherine J. Howard CoI1 ege of Oceanography Oregon State Uni versi ty, Corval 1 i s , Oregon 97331 Final Report for Contract No. 63-630-8803 Submi tted to: Oregon Department of Geology and Mineral Industries and the Gorda Ridge Technical Task Force Released June 1989 This report is based on results of a research progrm directed by the joint federal-state Gorda Ridge Technical Task Force, managed by the Oregon Department of Geology and Hineral Industries, and funded by the Minerals Pbnagement Service, U.S. Deparbmt of the Interior, thtough Cooperative Agremmt. Opinions expressed are those of the authors and do not constitute endarsement by the qwtsoring agencies or the Task Force. Ple Oregon Departmmt of Geology and Mineral Industries is publishing this paper because the subject matter is consistent with the mission of the -t. To facilitate thly distribution of information, ame era-ready cqy submitted by the authors has not h edited by the staff of the -on Wpmtwnt of Geology and nineral Industries. TABLE OF CONTENTS List of Fig- ........................................................................................... 3 ListofTables ............................................................................................. 3 Absbact. ....................................................................................................