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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. -
Geologic Map of the Suquamish 7.5' Quadrangle and Part of the Seattle
Geologic Map of the Suquamish 7.5’ Quadrangle and Part of the Seattle North 7.5’ x 15’ Quadrangle, Kitsap County, Washington By Ralph A. Haugerud and Kathy Goetz Troost Pamphlet to accompany Scientific Investigations Map 3181 2011 U.S. Department of the Interior U.S. Geological Survey This page intentionally left blank Contents Introduction.....................................................................................................................................................1 Geologic framework .............................................................................................................................1 About this report ...................................................................................................................................2 Stratigraphy ....................................................................................................................................................3 Glacial and nonglacial deposits .........................................................................................................3 Deposits older than Olympia interglaciation of Armstrong and others (1965) ...................3 Deposits older than Vashon stade of Fraser glaciation of Armstrong and others (1965)..............................................................................................................................4 Vashon Drift ..................................................................................................................................4 Late-glacial deposits -
Nisqually 7.5-Minute Quadrangle, Thurston and Pierce Counties, Washington 122°45¢ Qgof Qgt 122°37¢30² 47°07¢30² 47°07¢30² Qps Anderson by Timothy J
WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN FILE REPORT 2003-10 Division of Geology and Earth Resources Ron Teissere - State Geologist Geologic Map of the Nisqually 7.5-minute Quadrangle, Thurston and Pierce Counties, Washington 122°45¢ Qgof Qgt 122°37¢30² 47°07¢30² 47°07¢30² Qps Anderson by Timothy J. Walsh, Robert L. Logan, Michael Polenz, and Henry W. Schasse Island Qml FORT LEWIS 22 Qml MILITARY RESERVATION 2003 Qf Qf 23 24 Sequalitchew 39 INTRODUCTION MAPPING METHODS Qgt Vashon till—Unstratified and, in most exposures, highly compacted REFERENCES CITED Qgt PUGET SOUND Adams Woods mixture of clay, silt, sand, and gravel deposited directly by glacier The Nisqually quadrangle is located at the south end of Puget Sound, straddling For the present map, we inspected available construction site excavations, gravel Armstrong, J. E.; Crandell, D. R.; Easterbrook, D. J.; Noble, J. B., 1965, Late Bender ice; gray where fresh and light yellowish brown where oxidized; 22 the Nisqually River, which is the boundary between Thurston and Pierce pits, and roadcuts. We surveyed the shorelines by boat and took samples and Pleistocene stratigraphy and chronology in southwestern British Columbia Wo ods unsorted and, in most exposures, of very low permeability; most Counties. It includes part of Fort Lewis, which has limited access to areas used measured sections at cliff exposures. Contacts between map units are commonly and northwestern Washington: Geological Society of America Bulletin, Qgog commonly matrix-supported but may be clast-supported; matrix for artillery training, and part of the Nisqually Indian Reservation, which also not exposed and are only approximately located. -
South Parcel Short Plat, PLNG2019-031
First American Title Insurance Company 7502 Lakewood Drive West, Ste A Lakewood, WA 98499 September 30, 2019 Rick Bond Gray & Osborne 1130 Rainier Avenue South Suite 300 Seattle, WA 98144 Phone: (206)284-0860 Fax: (206)283-3206 Title Officer: Lisa Polosky Phone: (253)382-2811 Fax No.: (253)382-2883 E-Mail: [email protected] Order Number: 3236808 Owner: City of Dupont Property: 1700 to 1780 Civic Drive Dupont, Washington 98327 Attached please find the following item(s): Guarantee Thank You for your confidence and support. We at First American Title Insurance Company maintain the fundamental principle: Customer First! Form 5003353 (7-1-14) Page 1 of 11 Guarantee Number: 3236808 CLTA #14 Subdivision Guarantee (4-10-75) Washington Subdivision Guarantee ISSUED BY First American Title Insurance Company Guarantee GUARANTEE NUMBER 5003353-3236808 SUBJECT TO THE EXCLUSIONS FROM COVERAGE, THE LIMITS OF LIABILITY AND THE CONDITIONS AND STIPULATIONS OF THIS GUARANTEE, FIRST AMERICAN TITLE INSURANCE COMPANY a Nebraska corporation, herein called the Company GUARANTEES Gray & Osborne the Assured named in Schedule A against actual monetary loss or damage not exceeding the liability stated in Schedule A, which the Assured shall sustain by reason of any incorrectness in the assurances set forth in Schedule A. This jacket was created electronically and constitutes an original document Form 5003353 (7-1-14) Page 2 of 11 Guarantee Number: 3236808 CLTA #14 Subdivision Guarantee (4-10-75) Washington SCHEDULE OF EXCLUSIONS FROM COVERAGE OF THIS GUARANTEE -
Information Circular 96: Reconnaissance Investigation of Sand, Gravel, and Quarried Bedrock Resources in the Snoqualmie Pass
Reconnaissance Investigation of Sand, Gravel, and Quarried Bedrocl< Resources in the Snoqualmie Pass 1: 100,000 Quadrangle, Washington by William S. Lingley, Jr., David A. Knoblach, and Celia K. B. Nightingale WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 96 June 2002 Doug Sutherland- Commissioner of Public Lands DISCLAIMER Neither the State of Washington, nor any agency thereof, nor any of their em ployees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any informa tion, 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 other wise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the State of Washington or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the State of Washington or any agency thereof. WASHINGTON DEPARTMENT OF NATURAL RESOURCES Doug Sutherland-Commissioner ofPublic Lands DIVISION OF GEOLOGY AND EARTH RESOURCES Ron Teissere---State Geologist David K. Norman-Assistant State Geologist This report is available from: Publications Washington Division of Geology and Earth Resources PO Box 47007 Olympia, WA 98504-7007 Phone: (360) 902-1450 Fax: (360) 902-1785 E-mail: [email protected] Website: http://www.wa.gov/dnr/htdocs/ger/ ..,.,. Printed on recycled paper. ~.,. Printed in the United States of America ii Contents Introduction. l Background . 1 Intended readership . 1 Primary products . 1 Accuracy of estimates. 2 Threshold of significant resources . -
Pamphlet to Accompany Scientific Investigations Map 3277
Lidar–Revised Geologic Map of the Olalla 7.5' Quadrangle, King, Kitsap, and Pierce Counties, Washington Pamphlet to accompany Scientific Investigations Map 3277 2013 U.S. Department of the Interior U.S. Geological Survey Contents Contents ........................................................................................................................................................................................... ii Introduction to Revised Version of the Map .....................................................................................................................................1 Geologic Issues ............................................................................................................................................................................1 Base Map Issues ..........................................................................................................................................................................1 Geologic Summary ...........................................................................................................................................................................2 Introduction ..................................................................................................................................................................................2 Previous Mapping ........................................................................................................................................................................2 Acknowledgments -
The Cordilleran Ice Sheet
The Cordilleran Ice Sheet Derek B. ~ooth',Kathy Goetz roost', John J. clague2 and Richard B. waitt3 I Department Earth & Space Sciences, Universiy of Washington, Box 531310, Seattle, WA 98 195. USA (206)543-7923 Fax (206)685-3836. Deparmletzt of Earth Scie~~ces.Simon Fraser University, Burnabv, British Columbia, Canada ' U.S. Geological Survey, Cascade Volcano Observatory, Vancouver; WA, USA Introduction techniques yield crude but consistent chronologies of local and regional sequences of alternating glacial and nonglacial The Cordilleran Ice Sheet, the smaller of two great continen- deposits. These dates secure correlations of many widely tal ice sheets that covered North America during Quaternary scattered exposures of lithologically similar deposits and glacial periods, extended from the mountains of coastal south show clear differences among others. and southeast Alaska, along the Coast Mountains of British Besides improvements in geochronology and paleoenvi- Columbia, and into northern Washington and northwestern ronmental reconstruction (i.e. glacial geology), glaciology Montana (Fig. 1). To the west its extent would have been provides quantitative tools for reconstructing and analyzing limited by declining topography and the Pacific Ocean; to the any ice sheet with geologic data to constrain its physical form east, it likely coalesced at times with the western margin of and history. Parts of the Cordilleran Ice Sheet, especially the Laurentide Ice Sheet to form a continuous ice sheet over its southwestern margin during the last glaciation, are well t.000 km wide. Because most of the marginal environments suited to such analyses. The approach allows interpretation of of the Cordilleran Ice Sheet were not conducive to preserving deposits and landforms at the now-exposed bed of the former an extensive depositional record, much of our understanding ice sheet, and it also suggests likely processes beneath other of this ice sheet has come from limited areas where preser- ice sheets where reconstructions are less well-constrained. -
P. Antipodarum 5-Mile Radius Survey 2013
2013 SURVEY FOR POTAMOPYRGUS ANTIPODARUM (NEW ZEALAND MUDSNAIL) WITHIN A FIVE-MILE RADIUS OF CAPITOL LAKE, THURSTON COUNTY, WASHINGTON. Edward J. Johannes Deixis Consultants 16827 51st Ave S. SeaTac, WA 98188 June 30, 2013 i TABLE OF CONTENTS INTRODUCTION.............................................................................................................................. 1 Background…………………………………………………………………………………….…. 1 History of Introduction……………………………………………………………………...….…. 1 Introduction in Capitol Lake……………………………………………..……...…………….…. 2 Previous Surveys for P. antipodarum in Capitol Lake drainage………………………….…. 2 PROJECT DESCRIPTION............................................................................................................... 3 Methods………………………………………………………………………………….….….…. 5 Field Collections……………………………………………………….....……..…….……. 5 Decontamination Procedures……………..………………………….....……..…….……. 5 Laboratory Procedures………………………………………………….....…..…….….…. 6 Identification Methods………………………………………………….....…..…….….…. 6 Museum Collections………………………………………………….....…..…….….…. 7 RESULTS......................................................................................................................................... 7 NZMS Found Within a 5-mile Radius of Capitol Lake and rate of movement……………... 7 Mollusks Found Within a 5-mile Radius of Capitol Lake……………………………………... 10 Introduced Mollusks…………………………………………………………....………….. 12 Family Hydrobiidae…………………………………………………………...….…..…. 12 Potamopyrgus antipodarum (Gray, 1853) (New Zealand -
OFR 2003-25, Geologic Map of the Tumwater 7.5-Minute Quadrangle, Thurston County, Washington
WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN FILE REPORT 2003-25 Division of Geology and Earth Resources Ron Teissere - State Geologist 122°52¢30² 123°00¢00² R.3W. R.2W. 57¢30² 55¢00² 47°07¢30² 47°07¢30² Qps INTRODUCTION DESCRIPTION OF MAP UNITS and boulders commonly faceted and (or) striated; ranges in ACKNOWLEDGMENTS adjacent oceans during the last glaciation: Geological Society of Qgt Qgof Qp Qgt Qp thickness from wispy, discontinuous layers less than 1 in. America DNAG Geology of North America, v. K-3, p. 111-125. Qp The Tumwater quadrangle is located at the south end of Puget Sound Quaternary Unconsolidated Deposits We have benefited greatly from discussions with Derek Booth and Qls Qps thick to more than 30 ft thick; thicknesses of 2 to 10 ft are In Qa and includes the cities of Tumwater and Olympia. The quadrangle is Kathy Troost (Univ. of Wash.) and Ray Wells and Brian Sherrod (U.S. Morrison, R. B., 1991, Introduction. Morrison, R. B., editor, Qp most common; may include outwash clay, sand, silt, and Qgt mostly urban and residential land. HOLOCENE NONGLACIAL DEPOSITS Geological Survey). This map is supported by the National Geologic Quaternary nonglacial geology—Conterminous U.S.: Geological Qps gravel, or ablation till that is too thin to substantially mask Qp Mapping Program under Cooperative Agreement No. 01HQAG0105 Society of America DNAG Geology of North America, v. K-2, p. 1- Qpg Fill—Clay, silt, sand, gravel, organic matter, shells, rip-rap, the underlying, rolling till plain; erratic boulders are Qf with the U.S. -
Possession-Age Chronologic and Lithologic Data
Chronology, Lithology and Paleoenvironmental Interpretations of the Penultimate Ice-Sheet Advance into the Puget Lowland, Washington State Kathy Goetz Troost A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy University of Washington 2016 Reading Committee: Derek Booth, Chair Michael Brown Estella Leopold Program Authorized to Offer Degree: Earth and Space Sciences ©Copyright 2016 Kathy Goetz Troost Page 2 of 239 University of Washington Abstract Chronology, Lithology and Paleoenvironmental Interpretations of the Penultimate Ice-Sheet Advance into the Puget Lowland, WA Kathy Goetz Troost Chair of Supervisory Committee: Dr. Derek B. Booth Earth and Spaces Sciences Stratigraphic nomenclature and chronology has been a problem for geologists seeking to understand the Quaternary history of the Puget Lowland of Washington State for over one hundred years. Accurate identification of deposits, and accurate age assignments for those deposits, can help us to better understand the paleoclimate of the region, the physical characteristics of deposits encountered during infrastructure projects, the timing of tectonic deformation and recent seismicity, and our geological history. Each of these has profound consequences on our daily lives. In this dissertation I have established a stratigraphic framework for the last million years of geologic history in the Puget Lowland, based on global climate patterns, abundant new absolute dates, and detailed mapping that synthesizes my work and the work of others over the last century. Two decades of detailed field mapping, absolute and relative dating, and analyses have identified new geologic units and clarified and expanded our understanding of many others that had been Page 3 of 239 previously identified but imprecisely described or understood. -
SR520 Geomorphology and Shoreline History Technical Memorandum
SR 520, I-5 to Medina: Bridge Replacement and HOV Project Geomorphology and Shoreline History of Lake Washington, Union Bay, and Portage Bay Technical Memorandum Prepared for Washington State Department of Transportation Federal Highway Administration Prepared by Kathy Goetz Troost Troost Geological Consulting Consultant Team Parametrix, Inc. CH2M HILL HDR Engineering, Inc. Parsons Brinckerhoff ICF Jones & Stokes Confluence Environmental Company Michael Minor and Associates PRR, Inc. Critigen Troost Geological Consulting AUGUST 2011 Geomorphology and Shoreline History of Lake Washington, Union Bay, and Portage Bay Executive Summary The Washington State Department of Transportation retained Troost Geological Consulting under subcontract to Parametrix, Inc. to conduct a geomorphological study of Lake Washington, Union Bay, and Portage Bay along the I-5 to Medina: Bridge Replacement and HOV project corridor. The purpose of the study was 1) to determine the presence of former shorelines and 2) to determine the history of water level rise. Samples were collected from continuously sampled borings drilled as part of the geotechnical engineering investigation. Logging and classification of the samples led to an understanding of the submerged strata in the three basins. Selected samples were subjected to analyses that aided in the identification of water depth, plant assemblages, depositional environment, landscape features, and depositional age. These analyses were used to construct the geologic history and geomorphic development for the study area. The depositional histories of Lake Washington, Union Bay, and Portage Bay are similar. Starting at the bottom, in general the strata in Union Bay and Portage Bay consist of glacial recessional silty gravelly deposits, overlain by glacial lake silt/clay with a weathered surface, overlain by diatomaceous peat or organic silt. -
Rediscovering a Petroglyph in the High Cascades Volume 54 David A
Journal Anthropology of Northwest Fall 2020 Volume 54 J ournal Number 2 O f N orthwest A nthropology “No One Asked for an Ethnography.” Reflections on Community-based Anthropology in Coast Salish Country N Thomas W Murphy 145 Image Rock: Rediscovering a Petroglyph in the High Cascades Volume 54 Volume David A. Kaiser and Julia Cleary 165 Coast Salish Social Complexity, Community Ties, and Resistance: Using Mortuary Analysis to Identify Changes in Coast Salish Society Before, During, and After the Early Number 2 Number Colonial Period Alexandra M. Peck 175 Confirmation Bias: Commentary on the 2020 JONA Article, “Salish Sea Islands Archaeology and Precontact History” Adam N. Rorabaugh, Kate Shantry, and James W. Brown 203 Historical Archaeology of Fort Boise’s Surgeon’s Quarters Porch Evidences the Behavior of Children Nathan J. May 240 Abstracts from the 72nd Annual Northwest Anthropological Conference, Kennewick, Washington, 20–23 March 2019 264 Journal of Northwest Anthropology List of Reviewers 2018–2019 278 Fall 2020 Fall W Journal of Northwest Anthropology Volume 54, Number 2 Fall 2020 CONTENTS Volume 54, Number 1 Volume 54, Number 2 1 “La Gente de Washington es la Más 145 “No One Asked for an Ethnography.” Tranquila” (People from Washington are Reflections on Community-based the Most Laid-Back): An Ethnographic Anthropology in Coast Salish Country Perspective on Honduran and Salvadoran Thomas W Murphy Migration to the Pacific Northwest Jordan Levy and Sandra Estrada 165 Image Rock: Rediscovering a Petroglyph in the High Cascades 22 Salish Sea Islands Archaeology and David A. Kaiser and Julia Cleary Precontact History Richard M.