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New Oregon Tsunami Simulation Scenarios, Published Data, and Probable Effect on the Oregon Building Code
New Oregon Tsunami Simulation Scenarios, Published Data, and Probable Effect on the Oregon Building Code George R. Priest, Oregon Dept. of Geology and Mineral Industries Presentation to the workshop on Designing for Tsunamis: New Oregon Data & Anticipated Changes to the Building Code Portland State Office Building, Portland, Oregon May 18, 2015 Designing for Tsunamis 5-18-15 Cascadia Subduction Zone (CSZ) North American Plate Overrides Juan de Fuca Plate Along Cascadia Subduction Zone at a rate of 1.5 inches/year Designing for Tsunamis 5-18-15 What does the 10,000 year history of ~40 great Cascadia earthquakes and tsunamis mean for probabilistic tsunami hazard analysis (PTHA)? The last big Cascadia earthquake and local tsunami in the Northwest was January 26, 1700 at ~9:00 PM. (Satake et al., 2003, Journ. Geophys. Res., v 108, no. B11, p. 2535.) Designing for Tsunamis 5-18-15 Turbidites in a deep sea core. (picture provided by Chris Goldfinger, 2010) Taken from Atwater (2005) Deep Sea Clay Turbidite Sand Designing for Tsunamis 5-18-15 Cascadia Fault Rupture Lengths from Turbidite Data ~40 earthquakes over the last 10,000 years 19 earthquakes 4 earthquakes 7 earthquakes 10 earthquakes Recurrence Grays Harbor Seaside Newport Coos Bay Mw Mw Mw Mw ~9 Brookings 500 8.5-8.8 8.5-8.3 7.6-8.4 430 yrs 320 yrs 240 yrs yrs Eureka CONCLUSION: Recurrence of tsunamis ≥~200 yrs dominated by Cascadia sources. Illustration modified from Goldfinger et al. (2012) Designing for Tsunamis 5-18-15 Tsunami Hazard Assessment Focused on (1) Defining Cascadia Sources -
G. William Domhoff: the Adventures and Regrets of a Professor of Dreams and Power 1
G. William Domhoff: The Adventures and Regrets of a Professor of Dreams and Power Interviewed by Sarah Rabkin Edited by Irene Reti Santa Cruz University of California, Santa Cruz University Library 2014 This oral history is covered by a copyright agreement between G. William Domhoff and the Regents of the University of California dated February 12, 2014. Under “fair use” standards, excerpts of up to six hundred words (per interview) may be quoted without the University Library’s permission as long as the materials are properly cited. Quotations of more than six hundred words require the written permission of the University Librarian and a proper citation and may also require a fee. Under certain circumstances, not-for-profit users may be granted a waiver of the fee. For permission contact: Irene Reti [email protected] or Regional Oral History Project, McHenry Library, UC Santa Cruz, 1156 High Street, Santa Cruz, CA, 95064. Phone: 831-459-2847. Table of Contents Interview History 1 Early Life 3 A Passion for Sports 34 Duke University 52 Majoring in PsyChology 66 Graduate SChool at Kent State University 74 Calvin Hall 79 The Beginnings of Dream ResearCh 83 A European Adventure and Marriage 85 Moving to California 88 California State University, Los Angeles, and Dissertation ResearCh 90 The Beginnings of ResearCh in SoCiology 99 The Genesis of Who Rules America? 104 Coming to the University of California, Santa Cruz 105 RefleCtions on the College Core Courses 116 College Courses 120 Culture Break 122 A UCSC Baseball Team 123 More on the UCSC -
Deep-Water Turbidites As Holocene Earthquake Proxies: the Cascadia Subduction Zone and Northern San Andreas Fault Systems
University of New Hampshire University of New Hampshire Scholars' Repository Faculty Publications 10-1-2003 Deep-water turbidites as Holocene earthquake proxies: the Cascadia subduction zone and Northern San Andreas Fault systems Chris Goldfinger Oregon State University C. Hans Nelson Universidad de Granada Joel E. Johnson University of New Hampshire, Durham, [email protected] Follow this and additional works at: https://scholars.unh.edu/faculty_pubs Recommended Citation Goldfinger, C. Nelson, C.H., and Johnson, J.E., 2003, Deep-Water Turbidites as Holocene Earthquake Proxies: The Cascadia Subduction Zone and Northern San Andreas Fault Systems. Annals of Geophysics, 46(5), 1169-1194. http://dx.doi.org/10.4401%2Fag-3452 This Article is brought to you for free and open access by University of New Hampshire Scholars' Repository. It has been accepted for inclusion in Faculty Publications by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. ANNALS OF GEOPHYSICS, VOL. 46, N. 5, October 2003 Deep-water turbidites as Holocene earthquake proxies: the Cascadia subduction zone and Northern San Andreas Fault systems Chris Goldfinger (1),C. Hans Nelson (2) (*), Joel E. Johnson (1)and the Shipboard Scientific Party (1) College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon, U.S.A. (2) Department of Oceanography, Texas A & M University, College Station, Texas, U.S.A. Abstract New stratigraphic evidence from the Cascadia margin demonstrates that 13 earthquakes ruptured the margin from Vancouver Island to at least the California border following the catastrophic eruption of Mount Mazama. These 13 events have occurred with an average repeat time of ¾ 600 years since the first post-Mazama event ¾ 7500 years ago. -
UA 128 Inventory Photographer Neg Slide Cs Series 8 16
Inventory: UA 128, Public Information Office Records: Photographs. Photographer negatives, slides, contact sheets, 1980-2005 Format(s): negs, slides, transparencies (trn), contact sheets Box Binder Title/Description Date Photographer (cs) 39 1 Campus, faculty and students. Marketing firm: Barton and Gillet. 1980 Robert Llewellyn negatives, cs 39 2 Campus, faculty, students 1984 Paul Schraub negatives, cs 39 2 Set construction; untitled Porter sculpture (aka"Wave"); computer lab; "Flying Weenies"poster 1984 Jim MacKenzie negatives, cs 39 2 Tennis, fencing; classroom 1984 Jim MacKenzie negatives, cs 39 2 Bike path; computers; costumes; sound system; 1984 Jim MacKenzie negatives, cs 39 2 Campus, faculty, students 1984 Jim MacKenzie negatives, cs 39 2 Admissions special programs (2 pages) 1984 Jim MacKenzie negatives, cs 39 3 Downtown family housing 1984 Joe ? negatives, cs 39 3 Student family apartments 1984 Joe ? negatives, cs 39 3 Downtown Santa Cruz 1984 Joe ? negatives, cs 39 3 Special Collections, UCSC Library 1984 Lucas Stang negatives, cs 39 3 Sailing classes, UCSC dock 1984 Dan Zatz cs 39 3 Childcare center 1984 Dan Zatz cs 39 3 Sailing classes, UCSC dock 1984 Dan Zatz cs 39 3 East Field House; Crown College 1985 Joe ? negatives, cs 39 3 Porter College 1985 Joe ? negatives, cs 39 3 Porter College 1985 Joe ? negatives, cs 39 3 Performing Arts; Oakes; Porter sculpture (The Wave) 1985 Joe ? negatives, cs Jack Schaar, professor of politics; Elena Baskin Visual Arts, printmaking studio; undergrad 39 3 chemistry; Computer engineering lab -
The Washington and Oregon Mid-Shelf Silt Deposit and Its Relation to the Late Holocene Columbia River Sediment Budget Mssd/Columbia River Sediment Budget
U.S. DEPARTMENT OF THE INTERIOR OPEN-FILE REPORT 99 - 173 U.S. GEOLOGICAL SURVEY version 1.0 science for a changing world THE WASHINGTON AND OREGON MID-SHELF SILT DEPOSIT AND ITS RELATION TO THE LATE HOLOCENE COLUMBIA RIVER SEDIMENT BUDGET MSSD/COLUMBIA RIVER SEDIMENT BUDGET By Stephen C. Wolf, Hans Nelson, Michael R. Hamer, Gita Dunhill, and R. Lawrence Phillips 125° 00' W 124° 00' W 123° 00' W The purpose of this report is to compile and analyze existing data which lend support to the development of a sediment budget for the Columbia River, coastal, Vancouver Island 130° 128° 126° 124° 122° and offshore regions of southwest Washington. This will contribute to the construction of a sediment budget model which will reflect sediment sources, depocenters, and the contribution to each region. Figure 1 describes the origin, distribution, and Baekley Canyon ° 48° thickness of the Mid-Shelf Silt Deposit (MSSD) based on analysis of seismic data 48 Nitinat Canyon acquired between 1976-1980 (Wolf et al., 1997). Sediment volumes deposited during Juan de Fuca Canyon the past 5000 years were calculated for each of the physiographic areal compartments Quinalt Canyon Strait of Juan de Fuca shown in Figure 2. Table 1 organizes the data from Figures 1 and 2 into tabular form. This table provides a representation of the percent volume and weight of sediment types Washington which contribute to the estimated Columbia River sediment budget. The Grays Canyon Nittrouer (1978), Nittrouer and Sternberg(1981) interpret and describe a sediment unit on the continental shelf as a compartments shown in Figure 2 are color co-ordinated with Table 1. -
COLLEGE EIGHT FROSH WELCOME to UCSC Welcome to UC Santa Cruz and Congratulations! This Is a Very Exciting Time in Your Life As You Begin a New Phase of Learning
ENVIRONMENT SOCIETY COLLEGE EIGHT FROSH Welcome Week Guide 2014 Week Welcome COLLEGE EIGHT WELCOME TO UCSC Welcome to UC Santa Cruz and congratulations! This is a very exciting time in your life as you begin a new phase of learning. Every year students tell us that a key factor to their success is getting involved on campus and making a difference in their community. We hope you take advantage of this week to learn as much as possible about your new environment. Fall Welcome Week has been planned for you to learn about the academic resources, to become familiar with the campus, and to learn about the Santa Cruz community. Use this guide to learn about the many workshops/events taking place campus-wide during Fall Welcome Week. Notice that some events are MANDATORY. Your academic and social transition to UC Santa Cruz is extremely important to us. We consider you a partner in your academic and social success here. Therefore we expect you to actively participate in the many programs and services this first week and well beyond. So, start now and begin making connections! 1 WELCOME TO COLLEGE EIGHT Welcome to College Eight and UC Santa Cruz! There are a number of things you’ll need to accomplish during your first several days on campus. This Orientation Schedule is designed to help guide you. Use it to learn about the many workshops, orientations, office hours and events across campus during Welcome Week. If you need more information ask an Orientation Leader (OL), Programs Assistant (PA), Resident Assistant (RA) or a member of our college staff. -
Santa Cruz Comics, a New Glossy Magazine to Successful Careers and Paradigm- That Takes Its Cue from Japanese Manga Comics
UC SANTA CRUZ MAGAZINE SPRING 2018 OMG!! Did you know it’s the Year of Alumni @UCSC? This is huuge!! From agroecology to astronomy, #UCSCAlumni are making a mark on the world! Rad! #thinkucsc #slugpower #noknownpredators UC SANTA CRUZ MAGAZINE SPRING 2018 10 Preventing plastic’s perils Chemistry professor Rebecca Braslau is working to make a new kind of plastic without phthalates, which can mimic hormones and cause health problems. 13 Alumni Weekend: Come home Alumni Weekend is April 27–29, 2018. Check out the full program of events and join fellow alumni for mingling, reminiscing, learning, and lingering. Join us as we share the beauty of diverse cultures 18 A rain check for undying love She sketched out a check for him from the “Cowell College Love Bank,” and they went their separate ways—until 39 years later. UC Santa Cruz has designated 2018 as the Year of Alumni, a time to savor, Comic relief celebrate, and promote the legacy 20 PROFESSIONAL CERTIFICATES of proud Banana Slugs who have Alumnus Doug Bragdon employs student artists made their mark as they’ve gone on with Santa Cruz Comics, a new glossy magazine to successful careers and paradigm- that takes its cue from Japanese manga comics. BIOSCIENCES shifting endeavors. These walls can talk This issue’s articles are about alumni 24 First-generation Salvadoran American Mauricio BUSINESS & MANAGEMENT or written by alumni. This is our way Ramirez—an alumnus and current grad student—finds of sharing stories of graduates whose voice, art, and inspiration in the murals of San Francisco’s lives were changed by UC Santa Mission District. -
Part A—Site Survey of the Northern Oregon
APPENDIX I PART A: SITE SURVEY OF THE NORTHERN OREGON CONTINENTAL MARGIN AND ASTORIA FAN LaVerne D. Kulm and Roger A. Prince, School of Oceanography, Oregon State University, Corvallis, Oregon and Parke D. Snavely, Jr., Office of Marine Geology, U.S. Geological Survey, Menlo Park, California INTRODUCTION Dehlinger et al. (1968) and Emilia et al. (1968), respectively. The unconsolidated and consolidated sedi- A geophysical survey (gravity, magnetics, and seismic ments were sampled in previous studies of this area (Nelson, reflection profiling) was made for DSDP Sites 174 and 175 1968; Kulm and Fowler, 1972). These sites are located off on YALOC-70 by Oregon State University's R/V Yaquina central Oregon on the distal end of Astoria Fan (Site 174) (Figure 1). Seismic reflection profiles were made earlier in and on the adjacent lower continental slope (Site 175) 1970 by the U. S. Geological Survey on the USNS Bartlett (Figures 1 and 2). DSDP Site 176, selected for near Site 175 (Figure 2, G-F). Detailed gravity and shallow-water drilling at the beginning of Leg 18, was magnetics studies on the Oregon margin are described by surveyed in 1969 by Oregon State's R/V Cayuse (Figures 1 and 3). ,22= Seismic reflection profiles were made over the distal portion of Astoria Fan to locate a prominent seismic discontinuity that separates the strongly reflecting seaward transgressive sediments of the Astoria Fan above from a landward-dipping weakly to strongly reflecting section below. The anticlinal folds on the lower continental slope are believed to be uplifted turbidites from the adjacent abyssal plain or fan (Kulm and Fowler, 1972). -
Rethinking Turbidite Paleoseismology Along the Cascadia Subduction Zone
Rethinking turbidite paleoseismology along the Cascadia subduction zone Brian F. Atwater1, Bobb Carson2, Gary B. Griggs3, H. Paul Johnson4, and Marie S. Salmi4 1U.S. Geological Survey at University of Washington, Seattle, Washington 98195-1310, USA 2Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, Pennsylvania 18015-3001, USA 3Earth & Planetary Sciences Department, University of California–Santa Cruz, Santa Cruz, California 95064, USA 4School of Oceanography, University of Washington, Seattle, Washington 98195-7940, USA ABSTRACT A 130ºW 120º A stratigraphic synthesis of dozens of deep-sea cores, most of British them overlooked in recent decades, provides new insights into deep- Southern Columbia limit of 50º Fraser R. sea turbidites as guides to earthquake and tsunami hazards along the ice sheet B Cascadia subduction zone, which extends 1100 km along the Pacific Full-length coast of North America. The synthesis shows greater variability ruptures in Holocene stratigraphy and facies off the Washington coast than Waashingtonshington was recognized a quarter century ago in a confluence test for seismic Fig. triggering of sediment gravity flows. That test compared counts of 3A Holocene turbidites upstream and downstream of a deep-sea channel Columbia R. Partial junction. Similarity in the turbidite counts among seven core sites pro- BFZ Cascadia ruptures vided evidence that turbidity currents from different submarine can- Channel Oregon yons usually reached the junction around the same time, as expected Seaward of widespread seismic triggering. The fuller synthesis, however, shows edge of distinct differences between tributaries, and these differences suggest megathrust California sediment routing for which the confluence test was not designed. The 40ºN synthesis also bears on recent estimates of Cascadia earthquake mag- PACIFIC OCEAN 19 4 10 10 nitudes and recurrence intervals. -
G. B. GRIGGS Division of Natural Sciences, University of California, Santa Cruz, California 95060 L
G. B. GRIGGS Division of Natural Sciences, University of California, Santa Cruz, California 95060 L. D. KULM Department of Oceanography, Oregon State University, Corvallis, Oregon 97331 Sedimentation in Cascadia Deep-Sea Channel ABSTRACT Cascadia Channel is the most extensive deep-sea tain Foraminifera from neritic, bathyal, and abyssal channel known in the Pacific Ocean and extends depths which have been size-sorted. A sequence of across Cascadia Basin, through Blanco Fracture sedimentary structures occurs in the deposits Zone, and onto Tufts Abyssal Plain. The channel is similar to that found by Bouma in turbidites ex- believed to be more than 2200 km m length and posed on the continent. There is a sharp break in has a gradually decreasing gradient averaging the textural and compositional properties of each 1:1000. Maximum channel relief reaches 300 m on graded bed. The coarser grained, basal zone of each the abyssal plain and 1100 m in the mountains of bed represents deposition from the traction load; the fracture zone. The right (north and west) bank the finer grained, organic-rich, upper portion of is consistently about 30 m higher than the left each graded bed represents deposition from the (south and east). suspension load. Individual turbidity current se- Turbidity currents have deposited thick, olive- quences are thinnest in the upper and thickest in green silt sequences throughout upper and lower the lower channel. Recurrence intervals between Cascadia Channel during Holocene time. The sedi flows range from 400 years in the upper to 1500 ment is derived primarily from the Columbia years along portions of the lower channel. -
2020-21 DOMESTIC EXCHANGE PROGRAM APPLICATION Note: the Last Day to Submit This Application to the Office of the Registrar Is Feb
UNIVERSITY OF CALIFORNIA, SANTA CRUZ OFFICE OF THE REGISTRAR Registrar, 1156 High Street, Santa Cruz, CA 95064 Phone (831) 459-4412 • FAX (831) 459-5051 [email protected] 2020-21 DOMESTIC EXCHANGE PROGRAM APPLICATION Note: The last day to submit this application to the Office of the Registrar is Feb. 22, 2020. After Feb. 22, 2020, contact [email protected] for assistance. For more information, see the Domestic Exchange Programs webpage. REQUESTOR Name (Last, First, Middle) _____________________________________________________________________________ Student ID __________________________________________ Birthdate ______________________________________ College ___________________________________________ Major ___________________________________________ Total credits (including this quarter) _____________________ ACADEMIC LEVEL Frosh Sophomore Junior Senior FINANCIAL AID I expect to receive UCSC financial aid during the exchange period. Yes No PREFERENCES University University of New Hampshire University of New Mexico Period 202020-21 Academic Year 202020 Fall Semester Only 202021 Spring Semester Only Please complete page 2 and the Proposed Course Study Plan beginning on page 3. Page 1 of 5 Revised: 11/27/2019 DIVISION OF UNDERGRADUATE EDUCATION Rachel Carson College • Cowell College • Crown College • Kresge College • Merrill College • Oakes College • Porter College • Stevenson College Campus Orientation • Enrollment Management • Financial Aid and Scholarships • Office of the Registrar • Undergraduate Admissions Campus Advising Coordination • Educational Partnership Center • Office of the Vice Provost and Dean • Summer Session UNIVERSITY OF CALIFORNIA, SANTA CRUZ OFFICE OF THE REGISTRAR Registrar, 1156 High Street, Santa Cruz, CA 95064 Phone (831) 459-4412 • FAX (831) 459-5051 [email protected] 2020-21 DOMESTIC EXCHANGE PROGRAM APPLICATION Note: The last day to submit this application to the Office of the Registrar is Feb. 22, 2020. -
Turbidity-Current Gateway to Escanaba Trough
Tufts Submarine Fan: Turbidity-Current Gateway to Escanaba Trough By Jane A. Reid and William R. Normark Bulletin 2216 U.S. Department of the Interior U.S. Geological Survey ii iii U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director U.S. Geological Survey, Reston, Virginia: 2003 U.S. Geological Survey Information Services Box 25286, Denver Federal Center Denver, CO 80225 This report and any updates to it are available online at: http://geopubs.wr.usgs.gov/bulletin/b2216/ Additional USGS publications can be found at: http://geology.usgs.gov/products.html For more information about the USGS and its products: Telephone: 1–888–ASK–USGS (1–888–275–8747) World Wide Web: http://www.usgs.gov/ Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement of the U.S. Government. Although this report is in the public domain, it may contain copyrighted materials that are noted in the text. Permission to reproduce those items must be secured from the individual copyright owners. Published in the Western Region, Menlo Park, California Manuscript approved for publication, September 26, 2003 Text edited by Peter H. Stauffer Production and design by Susan Mayfield ii iii Contents Abstract 1 Introduction 1 Data 2 Cascadia Channel and Tufts Submarine Fan 2 Cascadia Channel 2 Tufts Fan 3 Discussion 5 Age of Tufts Fan 5 Tufts Fan Elements and Tufts Abyssal Plain 6 Conclusions 6 References 7 Tables 1. Key turbidite beds in Escanaba Trough and water depth (top of flow) at the time of deposition of each bed 9 2.