Possession-Age Chronologic and Lithologic Data
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Wisconsinan and Sangamonian Type Sections of Central Illinois
557 IL6gu Buidebook 21 COPY no. 21 OFFICE Wisconsinan and Sangamonian type sections of central Illinois E. Donald McKay Ninth Biennial Meeting, American Quaternary Association University of Illinois at Urbana-Champaign, May 31 -June 6, 1986 Sponsored by the Illinois State Geological and Water Surveys, the Illinois State Museum, and the University of Illinois Departments of Geology, Geography, and Anthropology Wisconsinan and Sangamonian type sections of central Illinois Leaders E. Donald McKay Illinois State Geological Survey, Champaign, Illinois Alan D. Ham Dickson Mounds Museum, Lewistown, Illinois Contributors Leon R. Follmer Illinois State Geological Survey, Champaign, Illinois Francis F. King James E. King Illinois State Museum, Springfield, Illinois Alan V. Morgan Anne Morgan University of Waterloo, Waterloo, Ontario, Canada American Quaternary Association Ninth Biennial Meeting, May 31 -June 6, 1986 Urbana-Champaign, Illinois ISGS Guidebook 21 Reprinted 1990 ILLINOIS STATE GEOLOGICAL SURVEY Morris W Leighton, Chief 615 East Peabody Drive Champaign, Illinois 61820 Digitized by the Internet Archive in 2012 with funding from University of Illinois Urbana-Champaign http://archive.org/details/wisconsinansanga21mcka Contents Introduction 1 Stopl The Farm Creek Section: A Notable Pleistocene Section 7 E. Donald McKay and Leon R. Follmer Stop 2 The Dickson Mounds Museum 25 Alan D. Ham Stop 3 Athens Quarry Sections: Type Locality of the Sangamon Soil 27 Leon R. Follmer, E. Donald McKay, James E. King and Francis B. King References 41 Appendix 1. Comparison of the Complete Soil Profile and a Weathering Profile 45 in a Rock (from Follmer, 1984) Appendix 2. A Preliminary Note on Fossil Insect Faunas from Central Illinois 46 Alan V. -
Isotopes, Inc. Radiocarbon Measurements V Milton A
[RADIOCARBON, VOL. 8, 1966, P. 161-203] ISOTOPES, INC. RADIOCARBON MEASUREMENTS V MILTON A. TRAUTMAN and ERIC H. WILLIS Isotopes, Inc., Westwood, New Jersey INTRODUCTION This list presents dates on samples measured at Isotopes, Inc., dur- ing the years 1963 to 1965 and measurements made previously for which sample data has been recently received. The many results which do not appear are withheld pending additional information or at the request of our clients. Procedures employed in sample pretreatment, preparation of CO2, and method of counting are generally unchanged, as are our methods of age calculation. Suitable bone samples are now pretreated by the method of Berger, Harney and Libby (1964). In May, 1965, the three counters and associated electronics previ- ously described (Isotopes I, II, III) were retired after producing well over 2000 radiocarbon dates, geophysical measurements, and ultralow- level C14 measurements. A completely new laboratory was activated em- ploying four new counters. Shielding consists of 31 cm of selected low- background steel, 10 cm paraffin and 2.5 cm "aged" lead. Each counter has its own multianode annular anticoincidence geiger counter. Elec- tronics were designed and fabricated at Isotopes, Inc. The counters have an active volume of 1 L and when operated at a normal pressure of 3 atm, yield background counts of slightly over 2 counts j min, Aox x 0.95 is ca. 18.7 at 24° C. C13/C12 ratios are measured periodically by our mass spectrometry section, but not routinely on samples unless requested by clients. ACKNOWLEDGMENTS It is recognized that data obtained at Isotopes, Inc. -
Identifying Potential Juvenile Steelhead Predators in the Marine Waters of the Salish Sea
Early Marine Survival Project Washington Department of Fish & Wildlife Identifying Potential Juvenile Steelhead Predators In the Marine Waters of the Salish Sea Scott F. Pearson, Steven J. Jeffries, and Monique M. Lance Wildlife Science Division Washington Department of Fish and Wildlife, Olympia Austen Thomas Zoology Department University of British Columbia Robin Brown Early Marine Survival Project Washington Department of Fish & Wildlife Cover photo: Robin Brown, Oregon Department of Fish and Wildlife. Seals, sea lions, gulls and cormorants on the tip of the South Jetty at the mouth of the Columbia River. We selected this photograph to emphasize that bird and mammal fish predators can be found together in space and time and often forage on the same resources. Suggested citation: Pearson, S.F., S.J. Jeffries, M.M. Lance and A.C. Thomas. 2015. Identifying potential juvenile steelhead predators in the marine waters of the Salish Sea. Washington Department of Fish and Wildlife, Wildlife Science Division, Olympia. Identifying potential steelhead predators 1 INTRODUCTION Puget Sound wild steelhead were listed as threatened under the Endangered Species Act in 2007 and their populations are now less than 10% of their historic size (Federal Register Notice: 72 FR 26722). A significant decline in abundance has occurred since the mid-1980s (Federal Register Notice: 72 FR 26722), and data suggest that juvenile steelhead mortality occurring in the Salish Sea (waters of Puget Sound, the Strait of Juan de Fuca and the San Juan Islands as well as the water surrounding British Columbia’s Gulf Islands and the Strait of Georgia) marine environment constitutes a major, if not the predominant, factor in that decline (Melnychuk et al. -
2021 WSTC Tolling Report and Tacoma Narrows Bridge Loan Update
2021 WSTC TOLLING REPORT & TACOMA NARROWS BRIDGE LOAN UPDATE January 2021 2021 WSTC TOLLING REPORT & TACOMA NARROWS BRIDGE LOAN UPDATE TABLE OF CONTENTS Introduction 4 SR 16 Tacoma Narrows Bridge 7 2020 Commission Action 7 2021 Anticipated Commission Action 7 SR 99 Tunnel 8 2020 Commission Action 8 2021 Anticipated Commission Action 8 SR 520 Bridge 9 2020 Commission Action 9 2021 Anticipated Commission Action 9 I-405 Express Toll Lanes & SR 167 HOT Lanes 10 2020 Commission Action 10 2021 Anticipated Commission Action 11 I-405 Express Toll Lanes & SR 167 HOT Lanes Low Income Tolling Program Study 11 Toll Policy & Planning 12 Toll Policy Consistency 12 Planning for Future Performance & Operations 12 Looking Forward To Future Tolled Facilities 13 2021 Tolling Recommendations 14 Summary of Current Toll Rates and Revenues by Facility 16 2021 Tacoma Narrows Bridge Loan Update 17 2019-21 Biennium Loan Estimates 17 2021-23 Biennium Loan Estimates 18 Comparison of Total Loan Estimates: FY 2019 – FY 2030 18 TNB Loan Repayment Estimates 19 2021 Loan Update: Details & Assumptions 20 Factors Contributing to Loan Estimate Analysis 20 Financial Model Assumptions 21 P age 3 2021 WSTC TOLLING REPORT & TACOMA NARROWS BRIDGE LOAN UPDATE INTRODUCTION As the State Tolling Authority, the Washington State Transportation Commission (Commission) sets toll rates and polices for all tolled facilities statewide, which currently include: the SR 520 Bridge, the SR 16 Tacoma Narrows Bridge, the I-405 express toll lanes (ETLs), the SR 167 HOT lanes, and the SR 99 Tunnel. -
Pre-Vashon Interglacial Deposit Investigation
Investigation of a Pre-Vashon Interglacial Fine-Grained Organic-Rich Sedimentary Deposit, South Lake Union, Seattle, Washington Cody Gibson A report prepared in partial fulfillment of the requirements for the degree of Master of Science Earth and Space Sciences: Applied Geosciences University of Washington March 2017 Project Mentors: Kathy Troost, University of Washington Matt Smith, GeoEngineers Inc. Internship Coordinator: Kathy Troost Reading Committee: Kathy Troost Juliet Crider MESSAGe Technical Report Number: 56 ©Copyright Cody Gibson i Executive Summary This study evaluates a fine-grained interglacial deposit found in the subsurface of the South Lake Union (SLU) area, Seattle, Washington. The nearly one-square-km SLU study area is defined as north of Denny Way, south of Aloha Street, east of Aurora Avenue, and west of Interstate 5. The evaluation required an in-depth study of over 600 existing geotechnical and environmental boring logs found for the study area. My evaluation consisted of mapping the distribution, determining the depositional environment, and characterizing the organic-rich pre-Vashon deposits. The fine-grained organic-rich deposits correlate to the Olympia formation, which occurred prior to the last glaciation of the Puget Sound Lowland known as the Vashon. To characterize the subsurface conditions in SLU, I assigned the materials described on the boring logs to one of 3 basic layers: pre-Vashon, Olympia Formation (Qob), and Vashon. In the SLU, the Qob consists of grey silt with interbeds of sand and gravel, and has an abundance of organic debris including woody debris such as well-preserved logs and branches, fresh-water diatoms, and fresh-water aquatic deposits such as peat. -
Geology of Blaine-Birch Bay Area Whatcom County, WA Wings Over
Geology of Blaine-Birch Bay Area Blaine Middle Whatcom County, WA School / PAC l, ul G ant, G rmor Wings Over Water 2020 C o n Nest s ero Birch Bay Field Trip Eagles! H March 21, 2020 Eagle "Trees" Beach Erosion Dakota Creek Eagle Nest , ics l at w G rr rfo la cial E te Ab a u ant W Eagle Nest n d California Heron Rookery Creek Wave Cut Terraces Kingfisher G Nests Roger's Slough, Log Jam Birch Bay Eagle Nest G Beach Erosion Sea Links Ponds Periglacial G Field Trip Stops G Features Birch Bay Route Birch Bay Berm Ice Thickness, 2,200 M G Surficial Geology Alluvium Beach deposits Owl Nest Glacial outwash, Fraser-age in Barn k Glaciomarine drift, Fraser-age e e Marine glacial outwash, Fraser-age r Heron Center ll C re Peat deposits G Ter Artificial fill Terrell Marsh Water T G err Trailhead ell M a r k sh Terrell Cr ee 0 0.25 0.5 1 1.5 2 ± Miles 2200 M Blaine Middle Glacial outwash, School / PAC Geology of Blaine-Birch Bay Area marine, Everson ll, G Gu Glaciomarine Interstade Whatcom County, WA morant, C or t s drift, Everson ron Nes Wings Over Water 2020 Semiahmoo He Interstade Resort G Blaine Semiahmoo Field Trip March 21, 2020 Eagle "Trees" Semiahmoo Park G Glaciomarine drift, Everson Beach Erosion Interstade Dakota Creek Eagle Nest Glac ial Abun E da rra s, Blaine nt ti c l W ow Eagle Nest a terf California Creek Heron Glacial outwash, Rookery Glaciomarine drift, G Field Trip Stops marine, Everson Everson Interstade Semiahmoo Route Interstade Ice Thickness, 2,200 M Kingfisher Surficial GNeeoslotsgy Wave Cut Alluvium Glacial Terraces Beach deposits outwash, Roger's Glacial outwash, Fraser-age Slough, SuGmlaacsio mSataridnee drift, Fraser-age Log Jam Marine glacial outwash, Fraser-age Peat deposits Beach Eagle Nest Artificial fill deposits Water Beach Erosion 0 0.25 0.5 1 1.5 2 Miles ± Chronology of Puget Sound Glacial Events Sources: Vashon Glaciation Animation; Ralph Haugerud; Milepost Thirty-One, Washington State Dept. -
Development of a Hydrodynamic Model of Puget Sound and Northwest Straits
PNNL-17161 Prepared for the U.S. Department of Energy under Contract DE-AC05-76RL01830 Development of a Hydrodynamic Model of Puget Sound and Northwest Straits Z Yang TP Khangaonkar December 2007 DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor Battelle Memorial Institute, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof, or Battelle Memorial Institute. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. PACIFIC NORTHWEST NATIONAL LABORATORY operated by BATTELLE for the UNITED STATES DEPARTMENT OF ENERGY under Contract DE-AC05-76RL01830 Printed in the United States of America Available to DOE and DOE contractors from the Office of Scientific and Technical Information, P.O. Box 62, Oak Ridge, TN 37831-0062; ph: (865) 576-8401 fax: (865) 576-5728 email: [email protected] Available to the public from the National Technical Information Service, U.S. Department of Commerce, 5285 Port Royal Rd., Springfield, VA 22161 ph: (800) 553-6847 fax: (703) 605-6900 email: [email protected] online ordering: http://www.ntis.gov/ordering.htm This document was printed on recycled paper. -
Earthquake Hazard
SUB-SECTION 4G.2 PUYALLUP TRIBE ALL HAZARD MITIGATION PLAN EARTHQUAKE HAZARD Table of Contents TABLE OF CONTENTS ............................................................................................... 1 IDENTIFICATION DESCRIPTION ................................................................................ 2 DEFINITION ............................................................................................................. 2 TYPES .................................................................................................................... 2 SECONDARY HAZARDS: ................................................................................................ 3 PROFILE ................................................................................................................... 5 LOCATION AND EXTENT ............................................................................................... 5 VULNERABILITY ....................................................................................................... 15 IMPACTS ............................................................................................................... 16 RESOURCE DIRECTORY .......................................................................................... 24 REGIONAL ............................................................................................................. 24 NATIONAL ............................................................................................................. 24 ENDNOTES ............................................................................................................ -
SR 16 Tacoma Narrows Bridge to SR 3 Congestion Study – December 2018
SR 16, Tacoma Narrows Bridge to SR 3, Congestion Study FINAL December 28, 2018 Olympic Region Planning P. O. Box 47440 Olympia, WA 98504-7440 SR 16 Tacoma Narrows Bridge to SR 3 Congestion Study – December 2018 This page intentionally left blank. SR 16 Tacoma Narrows Bridge to SR 3 Congestion Study – December 2018 Washington State Department of Transportation Olympic Region Tumwater, Washington SR 16 Tacoma Narrows Bridge to SR 3 Congestion Study Project Limits: SR 16 MP 8.0 to 29.1 SR 3 MP 30.4 to 38.9 SR 304 MP 0.0 to 1.6 December 2018 John Wynands, P.E. Regional Administrator Dennis Engel, P.E. Olympic Region Multimodal Planning Manager SR 16 Tacoma Narrows Bridge to SR 3 Congestion Study – December 2018 This page intentionally left blank. SR 16 Tacoma Narrows Bridge to SR 3 Congestion Study – December 2018 Title VI Notice to Public It is the Washington State Department of Transportation’s (WSDOT) policy to assure that no person shall, on the grounds of race, color, national origin or sex, as provided by Title VI of the Civil Rights Act of 1964, be excluded from participation in, be denied the benefits of, or be otherwise discriminated against under any of its federally funded programs and activities. Any person who believes his/her Title VI protection has been violated, may file a complaint with WSDOT’s Office of Equal Opportunity (OEO). For additional information regarding Title VI complaint procedures and/or information regarding our non- discrimination obligations, please contact OEO’s Title VI Coordinator at (360) 705-7082. -
Chapter 13 -- Puget Sound, Washington
514 Puget Sound, Washington Volume 7 WK50/2011 123° 122°30' 18428 SKAGIT BAY STRAIT OF JUAN DE FUCA S A R A T O 18423 G A D A M DUNGENESS BAY I P 18464 R A A L S T S Y A G Port Townsend I E N L E T 18443 SEQUIM BAY 18473 DISCOVERY BAY 48° 48° 18471 D Everett N U O S 18444 N O I S S E S S O P 18458 18446 Y 18477 A 18447 B B L O A B K A Seattle W E D W A S H I N ELLIOTT BAY G 18445 T O L Bremerton Port Orchard N A N 18450 A 18452 C 47° 47° 30' 18449 30' D O O E A H S 18476 T P 18474 A S S A G E T E L N 18453 I E S C COMMENCEMENT BAY A A C R R I N L E Shelton T Tacoma 18457 Puyallup BUDD INLET Olympia 47° 18456 47° General Index of Chart Coverage in Chapter 13 (see catalog for complete coverage) 123° 122°30' WK50/2011 Chapter 13 Puget Sound, Washington 515 Puget Sound, Washington (1) This chapter describes Puget Sound and its nu- (6) Other services offered by the Marine Exchange in- merous inlets, bays, and passages, and the waters of clude a daily newsletter about future marine traffic in Hood Canal, Lake Union, and Lake Washington. Also the Puget Sound area, communication services, and a discussed are the ports of Seattle, Tacoma, Everett, and variety of coordinative and statistical information. -
Water Supply Forum Resiliency Project, Water Quality Assessment
Water Supply Forum Regional Water Supply Resiliency Project Water Quality Resiliency Assessment Technical Memorandum Snohomish, King, and Pierce Counties, Washington May 6, 2016 This page is intentionally left blank. Water Quality Resiliency Assessment Contents 1.0 Introduction ............................................................................................................ 1 1.1 Description of Risk ....................................................................................................... 1 1.2 Objectives .................................................................................................................... 1 2.0 Methodology .......................................................................................................... 1 2.1 Multibarrier Approach ................................................................................................... 1 2.2 Risk Event Prioritization ............................................................................................... 3 3.0 Results .................................................................................................................. 4 3.1 Risk Event Prioritization ............................................................................................... 4 3.2 Mitigation Measures ..................................................................................................... 6 4.0 Detailed Review of Risk Events ........................................................................... 11 4.1 Wildfire ........................................................................................................................11 -
OFR 2003-23, Geologic Map of Squaxin Island 7.5-Minute
WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN FILE REPORT 2003-23 Division of Geology and Earth Resources Ron Teissere - State Geologist Qp Qp Qp Qp Geologic Map of the Squaxin Island 7.5-minute Quadrangle, Qb Qgt Mason and Thurston Counties, Washington Qgt Qgt Qp Qgt Qp by Robert L. Logan, Michael Polenz, Timothy J. Walsh, and Henry W. Schasse Qp Qp Qp Qp 2003 Qp Qp Qp Qp Qp Qgt Qgof Qls INTRODUCTION with Possession glacial outwash deposits. Once Possession ice no deep troughs with sandy sediments characterized by northward-directed longer impounded the lake (but sea level was still significantly below paleocurrent indicators. These sediments provide evidence that The Squaxin Island quadrangle is located at the south end of Puget modern sea level), existing drainages, such as the Skokomish, drainage reorganized to flow northward through the recently formed Qgt Sound and covers a complex of inlets and passages that weave between Qp Qp Nisqually, and Puyallup Rivers, deeply and rapidly incised into their outwash plain. The thickness of these sediments (unit Qgos) varies Qgt Squaxin Island and mainland peninsulas. The quadrangle is rural former alluvial plains and became entrenched. At least initially, stage 3, substantially throughout the area, reaching more than 400 ft just south Qgt Qp Qp residential and agricultural land. Qgof Qp called the Olympia nonglacial interval locally (Armstrong and others, of the map area in a geotechnical borehole at the Port of Olympia Qp Qgt Qp Qp 1965), was characterized by downcutting and erosion. As sea level (Washington Public Power Supply System, 1974). Unit Qgos is Qgof GEOLOGIC HISTORY began to rise, most deposition was confined to these entrenched important because it is widespread throughout the populous South Late Wisconsinan–age Vashon Drift covers most of the quadrangle.