Surficial Geology and Geomorphology of the Lake Tapps Quadrangle Washington

Total Page:16

File Type:pdf, Size:1020Kb

Surficial Geology and Geomorphology of the Lake Tapps Quadrangle Washington Surficial Geology and Geomorphology of the Lake Tapps Quadrangle Washington GEOLOGICAL SURVEY PROFESSIONAL PAPER 388-A Surficial Geology and Geomorphology of the Lake Tapps Quadrangle Washington By DWIGHT R. CRANDELL GEOLOGIC STUDIES IN THE PUGET SOUND LOWLAND, WASHINGTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 388-A A study of glacial^ interglacial^ and postglacial deposits in part of the Puget Sound lowland and in the foothills of the adjacent Cascade Range UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.G., 20402 CONTENTS Page Description of surficial deposits Continued page Abstract.__________________________________________ Al Wingate Hill drift._.-_-__ _ _- -- -.-- A29 Introduction _______________________________________ 2 Description _ __________-------------------_ 30 Location, culture, and accessibility________________ 2 Distribution-.-.---------------- ---------- -- 31 Purpose and scope ______________________________ 2 Weathering- _____________------------------ 31 Fieldwork and acknowledgments__________________ 3 Origin ________________-_------------------- 31 Earlier studies,_________________________________ 4 Stratigraphic relations and age. _ ..______--_-_- 32 General setting.____________________________________ 4 Till and gravel of pre-Vashon piedmont glacier.. 32 Drainage and relief__ ___________________________ 4 Evans Creek drift______ ___--_------------------- 32 Climate and vegetation__________________________ 6 Description ______________------------------ 32 Bedrock _______________________________________ 7 Provenance. __________-__--_--------------- 33 Physical geology of surficial deposits __________________ 7 Stratigraphic relations and age.. _. _ ___________ 35 Regional geologic setting_________________________ 7 Vashon drift....-------------------------------- 36 Depositional environments and provenance of sedi­ Till-.-- - 36 ments _______________________________________ Description ____________---------------- 36 Criteria used to establish stratigraphy,________________ 12 Distribution.. _ __- ______ -- 38 Provenance ____________________________________ 12 Topography ___ _ __ - -- - 38 Palynology _____________________________________ 12 Weathering -____ _ 38 Weathering.___________________________________ 12 Drift border.. _ ___ _ -_ -- ------- 38 Absolute age determinations_______________---_-- 13 Advance stratified drift_. _______ _ ___ _--- 39 Description of surficial deposits-______________________ 13 Recessional stratified drift. _ __________________ 40 Orting drift ____________________________________ 13 Ice-contact stratified drift. ___________ 40 Description ________________________________ 13 Kame and kame-field gravel __ ______ 40 Thickness. _________________________________ 15 Kame-terrace gravel. _________--__-_ 40 Distribution. _______________________________ 16 Ice-contact lacustrine sand. _ _________ 42 Weathering-_______________________________ 17 Proglacial lacustrine sand___--_-__------- 43 Origin.____________________________________ 17 Carbon River valley ________________ 43 Stratigraphic relations and age _______________ 17 Voight Creek valley. -_- __ _ 43 Lily Creek formation____________________________ 17 Glacial Lake Puyallup__________---_- 43 Description ________________________________ 17 Delta. ------------ _ _-----------_---- 44 Thickness, _ ________________________________ 18 Proglacial melt-water stream deposits _____ 44 Weathering ________________________________ 18 Terrace gravel along Carbon River_ _______________ 45 Distribution. _______________________________ 19 Description _______________-___---__-------- 45 Stratigraphic relations and age _______________ 21 Origin _ _ __ -_ --- 45 Origin_ ____________________________________ 22 Stratigraphic relations and age _______________ 45 Alderton formation _____________________________ 22 Osceola mudflow___ -- - 46 Description ________________________________ 22 Description ________________-_-------_------ 46 Distribution. _______________________________ 23 Thickness and volume____ ------------------- 47 Origin and environment of deposition.________ 23 Distribution and surface features ___________ 47 Stratigraphic relations.______________________ 23 Age 49 Stuck drift_____________________________________ 23 Origin. _ __ __ __ - 50 Description ________________________________ 23 Terrace alluvium along White River -____.____-_-- 50 Distribution, _______________________________ 24 Electron mudflow__-___-___--_-----_--------_-_- 50 Weathering._______________________________ 24 Description ________________-------------_-- 50 Stratigraphic relations and age_______________ 24 Thickness _ _______________________________ 51 Puyallup formation _____________________________ 25 Age and origin.-.- ___ - --_-- 51 Description ________________________________ 25 Lacustrine deposits. _______________-___.____---- 52 Distribution, ___ ____________________________ 26 Colluvium ______-__-______-__------_--------__- 52 Weathering ________________________________ 26 Slumps. _____________--____-_-_-_-_----_--_ 52 53 Environment of deposition,__________________ 26 Earthflows-- _-_- --- ----- Flood-plain alluvium. ___________________________ 54 Stratigraphic relations and age _______________ 28 Alluvium of the Puyallup and Duwamish Salmon Springs drift ____________________________ 28 54 Description._______________________________ 28 White River valley-_______ 55 Distribution.. _ _____________________________ 29 South Prairie Creek valley _ 56 Stratigraphic relations and environment of Carbon River valley ______ 56 deposition. _ ______________________________ 29 Artificial fill _ . _ _ 56 IV CONTENTS Page Page Structure __________________________________________ A56 Geologic history and geomorphic development Continued Geologic history and geomorphic development__________ 57 Pleistocene time Continued Pre-Pleistocene time. ___________________________ 57 Vashon glaciation Continued Pleistocene time________________________________ 57 Retreat of the Puget lobe________________ A65 Pre-Orting drainage pattern__________________ 57 Recent time._______________-_--------------_-_- 67 Orting glaciation_______________ _____________ 58 Pre-Osceola course of the White River_________ 67 Alderton time ______________________________ 58 Osceola mudflow._-______-__----__------__-- 67 Electron mudflow-__________________________ 68 Mount Rainier volcanism and the filling Correlations. ______________------------------------_ 70 of the ancestral Mowich Valley____ _ ___ 58 Economic geology___________-__--_-----_---------_-- 71 Climate__________ ______________________ 59 Sand and gravel__________-_-_-----__-_-_------- 71 Stuck glaciation____________________________ 59 Clay_________________-__-_------_-_-___-_:_--- 72 Puyallup time____-_--__---_____________-___ 59 Volcanic breccia__________----_---_-____-_-_ 72 Drainage changes in the foothill area_---__ 59 Lily Creek formation________________________ 73 Volcanism and aggradation in ancestral Vashon drift_______________________________ 73 Puyallup Valley___-__________________ 59 Fill material. ____________-_-_-_-_------------__ 73 Development of the Wingate Hill surf ace __ 60 Travertine.______________-_---_-_-------------_ 73 Weathering and erosion in the lowland_ _ __ 61 Peat._-__-____________-_-_--_-------------__ 74 Engineering geology_________________________________ 74 Salmon Springs time ________________________ 62 Foundation conditions.__________________________ 74 Salmon Springs-Vashon interval ______________ 62 Earthquake damage_____________-_______-_---_-_ 75 Vashon glaciation___________________________ 63 Subsidence._ ___________________________________ 76 Valley glacier phase___--____________-_-_ 63 Drainage._._______________-_-____----_-_---_-- 76 Advance of the Puget lobe_______________ 63 Measured sections __________________________________ 76 Relation of Puget lobe to valley glaciers _ _ 63 References.________________________________________ 80 Ice-marginal channels in Cascade foothills-. 64 Index.___________________--_-------------_-------_ 83 ILLUSTRATIONS [Plates are in pocket] PLATE 1. Surficial geology of the Lake Tapps quadrangle, Washington. 2. Sequence of the Vashon deglaciation of the Lake Tapps quadrangle, Washington. Page FIGURE 1. Index map of Washington showing location of the Lake Tapps quadrangle_________-______------_-------_---- A3 2. Physiographic subdivisions of the Lake Tapps quadrangle.- _ ______________________---------_-------------- 5 3. Outcrop of till in the Orting drift at confluence of Kapowsin Creek and Puyallup River. ________-_-_-_--_----___ 15 4. Outcrop of gravel in Orting drift on north bank of Carbon River in sec. 33, southeast of Orting_ _________-_-_-_-_ 16 5. Deeply weathered mudflow in Lily Creek formation exposed near top of scarp in SW/4 sec. 22, southwest of Spar Pole Hill________________________.________..__________________-_____________--__-_--__-----------_ 18 6. Index map of the southern part of the Lake Tapps quadrangle, the adjacent Cascade Range, and Mount Rainier, showing the distribution of the Lily Creek formation.. _________________________________________________ 20 7. Upper mudflow in Alderton formation in NE% sec. 12, northwest of McMillin____ ____________________________ 22 8. Outcrop of mudflow in Puyallup formation on north wall of Fennel
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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Nisqually State Park Interpretive Plan
    NISQUALLY STATE PARK INTERPRETIVE PLAN OCTOBER 2020 Prepared for the Nisqually Indian Tribe by Historical Research Associates, Inc. We acknowledge that Nisqually State Park is part of the homelands of the Squalli-absch (sqʷaliʔabš) people. We offer respect for their history and culture, and for the path they show in caring for this place. “All natural things are our brothers and sisters, they have things to teach us, if we are aware and listen.” —Willie Frank, Sr. Nisqually State Park forest. Credit: HRA TABLE OF CONTENTS INTRODUCTION . 5 PART 1: FOUNDATION. .11 Purpose and Guiding Principles . .12 Interpretive Goals . 12 Desired Outcomes . .13 Themes. 14 Setting and Connections to Regional Interpretive Sites . 16 Issues and Influences Affecting Interpretation . .18 PART 2: RECOMMENDATIONS . .21 Introduction . 22 Recommended Approach . .22 Recommended Actions and Benchmarks . 26 Interpretive Media Recommendations . 31 Fixed Media Interpretation . .31 Digital Interpretation . 31 Personal Services . 32 Summary . 33 PLANNING RESOURCES . 34 HRA Project Team . 35 Interpretive Planning Advisory Group and Planning Meeting Participants . .35 Acknowledgements . 35 Definitions . 35 Select Interpretation Resources. 36 Select Management Documents . 36 Select Topical Resources. 36 APPENDICES Appendix A: Interpretive Theme Matrix Appendix B: Recommended Implementation Plan Appendix C: Visitor Experience Mapping INTRODUCTION Nisqually State Park welcome sign includes Nisqually design elements and Lushootseed language translation. Credit: HRA Nisqually State Park | Interpretive Plan | October 2020 5 The Nisqually River is a defining feature of Nisqually State Park. According to the late Nisqually historian Cecelia Svinth Carpenter, “The Nisqually River became the thread woven through the heart and fabric of the Nisqually Indian people.” —Carpenter, The Nisqually People, My People.
    [Show full text]
  • Recent Advances in North American Pleistocene Stratigraphy Richard Foster Flint Yale University, New Haven, Connecticut, U.S.A
    5 Recent advances in North American Pleistocene stratigraphy Richard Foster Flint Yale University, New Haven, Connecticut, U.S.A. Introduction The Glacial Map of North America (FLINT and others 1945) assembled the essentials of what was known of North American Pleistocene stratigraphy as of 1942; the map data were amplified by FLINT (1947). Since the map appeared, a large volume of field work by many geologists and some other scientists has resulted in much new information. The discussion that follows is a review of some of the more important advances made during the last decade, but chiefly during the last five years. Extent of Nebraskan drift sheet The outermost drift in southeastern Nebraska, northeastern Kansas, and northern Missouri had been thought to be probably Nebraskan, the oldest of the four American drift sheets. This opinion was based partly on the inference that because much of that drift consists only of scattered boulders, the drift must be the residuum of a sheet of till from which the fines had been removed by erosion, and that such removal must have required a long time. This argument loses force when it meets the fact that much of the drift in question cocupies a much-dissected belt of country with steep slopes, fringing the Missouri River, and some geologists have suspected that the outermost drift is not Nebraskan (First glacial) but Kansan (Second glacial). This view has been strengthened by test borings made in eastern Nebraska (E. C. REED, unpublished) and northeastern Kansas (FRYE & WALTERS 1950) where the outermost drift consists largely of continuous till.
    [Show full text]
  • Geology of Michigan and the Great Lakes
    35133_Geo_Michigan_Cover.qxd 11/13/07 10:26 AM Page 1 “The Geology of Michigan and the Great Lakes” is written to augment any introductory earth science, environmental geology, geologic, or geographic course offering, and is designed to introduce students in Michigan and the Great Lakes to important regional geologic concepts and events. Although Michigan’s geologic past spans the Precambrian through the Holocene, much of the rock record, Pennsylvanian through Pliocene, is miss- ing. Glacial events during the Pleistocene removed these rocks. However, these same glacial events left behind a rich legacy of surficial deposits, various landscape features, lakes, and rivers. Michigan is one of the most scenic states in the nation, providing numerous recre- ational opportunities to inhabitants and visitors alike. Geology of the region has also played an important, and often controlling, role in the pattern of settlement and ongoing economic development of the state. Vital resources such as iron ore, copper, gypsum, salt, oil, and gas have greatly contributed to Michigan’s growth and industrial might. Ample supplies of high-quality water support a vibrant population and strong industrial base throughout the Great Lakes region. These water supplies are now becoming increasingly important in light of modern economic growth and population demands. This text introduces the student to the geology of Michigan and the Great Lakes region. It begins with the Precambrian basement terrains as they relate to plate tectonic events. It describes Paleozoic clastic and carbonate rocks, restricted basin salts, and Niagaran pinnacle reefs. Quaternary glacial events and the development of today’s modern landscapes are also discussed.
    [Show full text]
  • Lesson 9. Sand Forests, Savannas, and Flatwoods
    LESSON 9. SAND FORESTS, SAVANNAS, AND FLATWOODS Wind blown sand deposits are relatively common in the northern half of Illinois accounting for about 5 percent of the land area of the state (Figure 9.1). Most occur on glacial outwash plains resulting from erosional events associated with Wisconsin glaciation. The most extensive are the Kankakee sand deposits of northeastern Illinois, the Illinois River sand deposits in the central part of the state, and the Green River Lowlands in northwestern Illinois. Other sand deposits are associated with the floodplain of the Mississippi River in northwestern Illinois, and the Chicago Lake Plain and beaches along Lake Michigan in northeastern Illinois. The Kankakee sand deposits were formed about 14,500 years ago as glacial moraines were breached during a major re-advance of the Wisconsin Glacier. These glacial meltwaters were mostly discharged into the Kankakee River Valley creating the Kankakee Torrent. The Kankakee Valley could not accommodate this extensive flood and at the peak of the flow the water spread out over the surrounding uplands forming a series of large glacial lakes (Lake Watseka, Lake Wauponsee, Lake Pontiac, and Lake Ottawa). During this period glacial sands were deposited in these lakes. Large quantities of sand were removed during the Kankakee Torrent, but extensive deposits were left behind forming the Kankakee Sand Area Section of the Grand Prairie Natural Division. The Illinois River sand deposits were also formed during the Kankakee Torrent. The outlet channel for the Kankakee Torrent was along the Illinois River Valley and the Torrent was entrenched in bedrock, moving rapidly and scouring broad areas of the bedrock.
    [Show full text]
  • 38,000 Fresh-Water Mussel Shells from S Side of Road Cut on State Highway 113, Approx
    U. S. Geological Survey Radiocarbon Dates VII Item Type Article; text Authors Ives, Patricia C.; Levin, Betsy; Robinson, Richard D.; Rubin, Meyer Citation Ives, P. C., Levin, B., Robinson, R. D., & Rubin, M. (1964). U. S. Geological Survey radiocarbon dates VII. Radiocarbon, 6, 37-76. DOI 10.1017/S0033822200010547 Publisher American Journal of Science Journal Radiocarbon Rights Copyright © The American Journal of Science Download date 02/10/2021 21:25:40 Item License http://rightsstatements.org/vocab/InC/1.0/ Version Final published version Link to Item http://hdl.handle.net/10150/654046 I:RADIOCARUON, Vol.. 6, 1964, P. 37-761 U. S. GEOLOGICAL SURVEY RADIOCARBON DATES VII* PATRICIA C. IVES, BETSY LEVIN, RICHARD D. ROBINSON, and MEYER RUBIN U. S. Geological Survey, Washington, D. C. This date list contains the results of measurements made during 1961, 1962 and 1963. The method of counting, utilizing acetylene gas, remains essen- tially unchanged, except for the addition of some solid state electronics. The method of computation, using the Libby half-life of 5568 ± 30 yr, is con- tinued. The error listed is always larger than the one-sigma statistical counting error commonly used, and takes into account known uncertainty laboratory factors, and does not include external (field or atmospheric) variations. Unless otherwise stated, collectors of all samples are members of the U. S. Geological Survey. SAMPLE DESCRIPTIONS A. Eastern U. S. W-1132. Copperas Gap, Arkansas >38,000 Fresh-water mussel shells from S side of road cut on State Highway 113, approx. 1 mi SW of Arkansas River, SE'/4 NE'/4 SE'/4 sec.
    [Show full text]
  • 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
    [Show full text]
  • The Ice Age in Pennsylvania 13
    Educational Series 6 PENNSYLVANIA AND THE ICE AGE An Equal Opportunity/ Affirmative Action Employer Recycled Paper 2200–BK–DCNR3061 COMMONWEALTH OF PENNSYLVANIA Tom Ridge, Governor DEPARTMENT OF CONSERVATION AND NATURAL RESOURCES John C. Oliver, Secretary OFFICE OF CONSERVATION AND ENGINEERING SERVICES Richard G. Sprenkle, Deputy Secretary BUREAU OF TOPOGRAPHIC AND GEOLOGIC SURVEY Donald M. Hoskins, Director FRONT COVER: The wooly mammoth—a Pennsylvania resident during the Ice Age (modified from Thomas, D. J., and others, 1987, Pleistocene and Holocene geology of a dynamic coast, Annual Field Conference of Pennsyl- vania Geologists, 52nd, Erie, Pa., Guidebook, front cover). Educational Series 6 Pennsylvania and the Ice Age by W. D. Sevon and Gary M. Fleeger PENNSYLVANIA GEOLOGICAL SURVEY FOURTH SERIES HARRISBURG 1999 When reproducing material from this book, please cite the source as follows: Sevon, W. D., and Fleeger, G. M., 1999, Pennsylvania and the Ice Age (2nd ed.): Pennsylvania Geological Survey, 4th ser., Educational Series 6, 30 p. Pennsylvania World Wide Web site: www.state.pa.us Department of Conservation and Natural Resources World Wide Web site: www.dcnr.state.pa.us Bureau of Topographic and Geologic Survey World Wide Web site: www.dcnr.state.pa.us/topogeo Illustrations drafted by John G. Kuchinski First Edition, 1962 Fifth Printing, May 1978 Second Edition, May 1999 PENNSYLVANIA AND THE ICE AGE by W. D. Sevon and Gary M. Fleeger Have you heard the story of the Ice Age, a time when large sheets of moving ice (glaciers) blanketed the northern half of North America? Unbelievable though it may seem, half of our continent was once buried beneath thousands of feet of ice.
    [Show full text]
  • Northwest Area Fire Weather Annual Operating Plan
    2011 Seattle Portland Medford Spokane Northwest Area Pendleton Fire Weather Boise Annual Operating ODF Salem Plan NWCC Predictive Services Table of Contents Introduction………………………………………………………………..3 NWS Services and Responsibilities……………………………………….4 Wildland Fire Agency Services and Responsibilities……………………..8 Joint Responsibilities……………………………………………….……..9 New for 2011……………………………………………………………..10 Seattle……………………………………………………………………..11 Portland………………………………………………………………..….22 Medford………………………………………………………….…….….34 Spokane…………………………………………………….……………..45 Pendleton……………………………………………………….…….…...57 Boise…………………………………………………….……………..….68 ODF Salem Weather Center………………………………………………74 NWCC Predictive Services……………………………………………….78 Plan Approval……………………………………………………………..84 Appendix A: Links to Fire Weather Agreements and Documents…….…85 Appendix B: Forecast Service Performance Measures…………………..86 Appendix C: Reimbursement for NWS Provided Training……………...87 Appendix D: IMET Reimbursement Billing Contacts…………………...88 Appendix E: Spot Request WS Form D-1……………………………….89 2 INTRODUCTION a. The Pacific Northwest Fire Weather Annual Operating Plan (AOP) constitutes an agreement between the Pacific Northwest Wildfire Coordinating Group (PNWCG), comprised of State, local government and Federal land management agencies charged with the protection of life, property and resources within the Pacific Northwest from threat of wildfire; and the National Weather Service (NWS), National Oceanic and Atmospheric Administration, U.S. Department of Commerce, charged with providing
    [Show full text]