Lewis River Hydroelectric Projects FERC Project Nos
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Geologic Map of the Simcoe Mountains Volcanic Field, Main Central Segment, Yakama Nation, Washington by Wes Hildreth and Judy Fierstein
Prepared in Cooperation with the Water Resources Program of the Yakama Nation Geologic Map of the Simcoe Mountains Volcanic Field, Main Central Segment, Yakama Nation, Washington By Wes Hildreth and Judy Fierstein Pamphlet to accompany Scientific Investigations Map 3315 Photograph showing Mount Adams andesitic stratovolcano and Signal Peak mafic shield volcano viewed westward from near Mill Creek Guard Station. Low-relief rocky meadows and modest forested ridges marked by scattered cinder cones and shields are common landforms in Simcoe Mountains volcanic field. Mount Adams (elevation: 12,276 ft; 3,742 m) is centered 50 km west and 2.8 km higher than foreground meadow (elevation: 2,950 ft.; 900 m); its eruptions began ~520 ka, its upper cone was built in late Pleistocene, and several eruptions have taken place in the Holocene. Signal Peak (elevation: 5,100 ft; 1,555 m), 20 km west of camera, is one of largest and highest eruptive centers in Simcoe Mountains volcanic field; short-lived shield, built around 3.7 Ma, is seven times older than Mount Adams. 2015 U.S. Department of the Interior U.S. Geological Survey Contents Introductory Overview for Non-Geologists ...............................................................................................1 Introduction.....................................................................................................................................................2 Physiography, Environment, Boundary Surveys, and Access ......................................................6 Previous Geologic -
Anthropological Study of Yakama Tribe
1 Anthropological Study of Yakama Tribe: Traditional Resource Harvest Sites West of the Crest of the Cascades Mountains in Washington State and below the Cascades of the Columbia River Eugene Hunn Department of Anthropology Box 353100 University of Washington Seattle, WA 98195-3100 [email protected] for State of Washington Department of Fish and Wildlife WDFW contract # 38030449 preliminary draft October 11, 2003 2 Table of Contents Acknowledgements 4 Executive Summary 5 Map 1 5f 1. Goals and scope of this report 6 2. Defining the relevant Indian groups 7 2.1. How Sahaptin names for Indian groups are formed 7 2.2. The Yakama Nation 8 Table 1: Yakama signatory tribes and bands 8 Table 2: Yakama headmen and chiefs 8-9 2.3. Who are the ―Klickitat‖? 10 2.4. Who are the ―Cascade Indians‖? 11 2.5. Who are the ―Cowlitz‖/Taitnapam? 11 2.6. The Plateau/Northwest Coast cultural divide: Treaty lines versus cultural 12 divides 2.6.1. The Handbook of North American Indians: Northwest Coast versus 13 Plateau 2.7. Conclusions 14 3. Historical questions 15 3.1. A brief summary of early Euroamerican influences in the region 15 3.2. How did Sahaptin-speakers end up west of the Cascade crest? 17 Map 2 18f 3.3. James Teit‘s hypothesis 18 3.4. Melville Jacobs‘s counter argument 19 4. The Taitnapam 21 4.1. Taitnapam sources 21 4.2. Taitnapam affiliations 22 4.3. Taitnapam territory 23 4.3.1. Jim Yoke and Lewy Costima on Taitnapam territory 24 4.4. -
Lewis River Hydroelectric Project Relicensing
United StatesDepartment of the Interior FISH AND WILDLIFE SERVICE Western Washington Fish and Wildlife Office 510 DesmondDr. SE, Suite 102 Lacey,Washington 98503 In ReplyRefer To: SCANNED 1-3-06-F-0177 sEPI 5 2006 MagalieR. Salas,Secretary F6deralEnergy Regulatory Commission 888First Sffeet,NE WashingtonD.C. 24426 Attention:Ann Ariel Vecchio DearSecretary Salas: This documenttransmits the U.S. Fish and Wildlife Service's(Service) Biological Opinion on the effectsto bull trout(Salvelinus confluentus),northern spotted owls (Srrlxoccidentalis caurina)and bald eagles(Haliaeetus leucocephalus) fromthe relicensingof the Lewis River HydroeiectricProjects: Merwin (FERC No. 935),Yale (FERC No. 2071),Swift No. 1 (FERC No. Zr 11),and swift No. 2 (FERCNo. 2213). Theaction that comprises this consultationunder theEndangered Species Act of 1973,as amended (16 U.S.C. l53I et seq.)is therelicensing of the Lewis-RiverHydroelectric Projects by the FederalEnergy Regulatory Commission and the interdependentactions contained in the SettlementAgreement (PacifiCorp et aL.2004e),dated November30,2004,and Washington Department of Ecology's401 Certifications. Consultationfor the relicensingof the Lewis River Plojectswas initiated by the Commission's letterto the Servicewhich was received in our officeon October11,2005. Based on our letter datedMarch15,2006,the deadline for completingthis consultationwas extended by mutual agreementuntil May 5, 2006. On June12,2006,with concurrenceby thelicensees,we submittedanother request for an extensionto SeptemberI,2006, to -
Soc 1-1 10.1 Socioeconomics Resource Study (Soc 1)
PacifiCorp/Cowlitz PUD Lewis River Hydroelectric Projects FERC Project Nos. 935, 2071, 2111, 2213 TABLE OF CONTENTS 10.0 SOCIOECONOMICS.................................................................................... SOC 1-1 10.1 SOCIOECONOMICS RESOURCE STUDY (SOC 1).......................... SOC 1-1 10.1.1 Study Objectives......................................................................... SOC 1-1 10.1.2 Study Area .................................................................................. SOC 1-2 10.1.3 Methods ...................................................................................... SOC 1-5 10.1.4 Key Questions............................................................................. SOC 1-7 10.1.5 Results......................................................................................... SOC 1-8 10.1.6 Discussion................................................................................. SOC 1-49 10.1.7 Schedule.................................................................................... SOC 1-51 10.1.8 References................................................................................. SOC 1-52 10.1.9 Comments and Responses on Draft Report .............................. SOC 1-57 SOC 1 Appendix 1 Text of RCW 54.28.050 SOC 1 Appendix 2 Descriptive Text of Money Generation Model LIST OF TABLES Table 10.1-1. Local sources of socioeconomic information...................................SOC 1-5 Table 10.1-2. 1990 population distribution by age in the secondary study area. ................................................................................................SOC -
Ridgefield National Wildlife Refuge Clark County, Washington: a Preliminary Report
Portland State University PDXScholar Anthropology Faculty Publications and Presentations Anthropology 1999 Archaeological Investigations at 45CL1 Cathlapotle (1991-1996) , Ridgefield National Wildlife Refuge Clark County, Washington: a Preliminary Report Kenneth M. Ames Portland State University, [email protected] Cameron M. Smith Portland State University William L. Cornett Portland State University Elizabeth A. Sobel Portland State University Stephen C. Hamilton Portland State University SeeFollow next this page and for additional additional works authors at: https:/ /pdxscholar.library.pdx.edu/anth_fac Part of the Archaeological Anthropology Commons Let us know how access to this document benefits ou.y Citation Details Ames, K. M., U.S. Fish and Wildlife Service., & Portland State University. (1999). Archaeological investigations at 45CL1 Cathlapotle (1991-1996), Ridgefield National Wildlife Refuge, Clark County, Washington: A preliminary report. Portland, Or: U.S. Fish and Wildlife Service. This Technical Report is brought to you for free and open access. It has been accepted for inclusion in Anthropology Faculty Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Authors Kenneth M. Ames; Cameron M. Smith; William L. Cornett; Elizabeth A. Sobel; Stephen C. Hamilton; John Wolf; Doria Raetz; United States. Department of the Interior; U.S. Fish and Wildlife Service, Region 1; and Portland State University. Department of Anthropology This technical report is available at PDXScholar: https://pdxscholar.library.pdx.edu/anth_fac/61 Archaeological Investigations at 45CL1 Cathlapotle (1991-1996) , Ridgefield National Wildlife Refuge Clark County, Washington A Preliminary Report by Kenneth M. Ames, Cameron M. Smith, William L. -
GEOLOGIC MAP of the MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE of SOUTHERN WASHINGTON by Wes Hildreth and Judy Fierstein
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-2460 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE OF SOUTHERN WASHINGTON By Wes Hildreth and Judy Fierstein When I climbed Mount Adams {17-18 August 1945] about 1950 m (6400') most of the landscape is mantled I think I found the answer to the question of why men by dense forests and huckleberry thickets. Ten radial stake everything to reach these peaks, yet obtain no glaciers and the summit icecap today cover only about visible reward for their exhaustion... Man's greatest 2.5 percent (16 km2) of the cone, but in latest Pleis experience-the one that brings supreme exultation tocene time (25-11 ka) as much as 80 percent of Mount is spiritual, not physical. It is the catching of some Adams was under ice. The volcano is drained radially vision of the universe and translating it into a poem by numerous tributaries of the Klickitat, White Salmon, or work of art ... Lewis, and Cis pus Rivers (figs. 1, 2), all of which ulti William 0. Douglas mately flow into the Columbia. Most of Mount Adams and a vast area west of it are Of Men and Mountains administered by the U.S. Forest Service, which has long had the dual charge of protecting the Wilderness Area and of providing a network of logging roads almost INTRODUCTION everywhere else. The northeast quadrant of the moun One of the dominating peaks of the Pacific North tain, however, lies within a part of the Yakima Indian west, Mount Adams, stands astride the Cascade crest, Reservation that is open solely to enrolled members of towering 3 km above the surrounding valleys. -
You Are D. B. Cooper
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses Winter 4-12-2018 You are D. B. Cooper James Bezerra Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Fiction Commons Let us know how access to this document benefits ou.y Recommended Citation Bezerra, James, "You are D. B. Cooper" (2018). Dissertations and Theses. Paper 4342. https://doi.org/10.15760/etd.6235 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. You Are D. B. Cooper by James Bezerra A thesis submitted in partial fulfillment of the requirements for the degree of Master of Fine Arts in Creative Writing Thesis Committee: Gabriel Urza, Chair Paul Collins Madeline McDonnell Portland State University 2018 2018 James Bezerra Abstract This thesis is a novel about the 1971 skyjacking of a plane out of Portland Airport. The novel is structured in the style of a choose-your-own-adventure book. It investigates the nature and identity of the skyjacker, who is known as D. B. Cooper. i Table of Contents Abstract …………………………………………………………………………… i You Are D. B. Cooper ……………………………………………………………. 1 Terminal Reference Section …...……………………………………………….. 197 ii You Are D. B. Cooper By James Bezerra 1 Look, it is not going to work out between us. Please set this book on fire. 2 I only know a few true things about D. B. Cooper: In 1971 a plane was hijacked after taking off from Portland Airport. -
Lewis River Acclimation Pond Site Recommendation
Lewis River Hydroelectric Projects FERC Project Nos. 935, 2071, 2111, 2213 Lewis River Acclimation Pond Project Final August 8, 2011 Contents 1.0 Introduction ........................................................................................................................ 1 2.0 General Plan ....................................................................................................................... 3 4.0 Site Descriptions ............................................................................................................... 7 4.1 Muddy River Site .................................................................................................................. 7 4.2 Clear Creek Site .................................................................................................................... 8 4.3 Crab Creek Site ..................................................................................................................... 8 4.4 Eagle Cliffs Alternative Site ................................................................................................. 9 5.0 Reporting ........................................................................................................................... 10 6.0 Attachments ..................................................................................................................... 11 ATTACHMENT A ........................................................................................................................ 12 ATTACHMENT B ........................................................................................................................ -
Engineering Geology in Washington, Volume I Wuhington Diviaion of Geology and Earth Resoul'ces Bulleti!I 78
The Cowlitz River Projects 264 ENGINEERING GEOLOGY IN WASHINGTON Aerial view of Mossyrock reservoir (Riffe Lake) and the valley of the Cowlitz River; view to the northeast toward Mount Rainier. Photograph by R. W. Galster, July 1980. Engineering Geology in Wuhington, Volume I . Washington Division of Geology and Earth Resources Bulletin 78 The Cowlitz River Projects: Mayfield and Mossyrock Dams HOWARD A. COOMBS University of Washington PROJECT DESCRIPTION unit) is at the toe of the dam on the north bank. The reservoir is 23.5 mi long. By impounding more than The Cowlitz River has its origin in the Cowlitz 1,600,000 acre-ft of water in the reservoir, the output of Glacier on the southeastern slope of Mount Rainier. The Mayfield Dam was greatly enhanced (Figures 3 and 4). river flows southward, then turns toward the west and passes through the western margin of the Cascade AREAL GEOLOGY Range in a broad, glaciated basin. It is in this stretch of The southern Cascades of Washington are composed the river that both Mossyrock and Mayfield dams are lo essentially of volcanic and sedimentary rocks that have cated. Finally, the Cowlitz River turns southward and been intruded by many dikes and sills and by small enters the Columbia River at Longview. batholiths and stocks of dioritic composition, as well as Mayfield Dam, completed in 1963, is 13 mi down plugs of andesite and basalt. Most of these rocks range stream from Mossyrock Dam, constructed 5 yr later. in age from late Eocene to Miocene (Hammond, 1963; Both are approximately 50 mi due south of Tacoma. -
Volume II, Chapter 11 Lewis River Subbasin—Lower North Fork
Volume II, Chapter 11 Lewis River Subbasin—Lower North Fork TABLE OF CONTENTS TABLE OF CONTENTS ..........................................................................................................................................2 11.0 LEWIS RIVER SUBBASIN—LOWER NORTH FORK ........................................ 11-3 11.1 Subbasin Description............................................................................................. 11-3 11.1.1 Topography & Geology ..................................................................................... 11-3 11.1.2 Climate............................................................................................................... 11-3 11.1.3 Land Use/Land Cover........................................................................................ 11-3 11.2 Focal Fish Species ................................................................................................. 11-6 11.2.1 Spring Chinook—Lewis Subbasin...................................................................... 11-6 11.2.2 Fall Chinook—Lewis Subbasin.......................................................................... 11-9 11.2.3 Coho—Lewis Subbasin (North Fork)............................................................... 11-12 11.2.4 Chum—Lewis Subbasin ................................................................................... 11-15 11.2.5 Summer Steelhead—Lewis Subbasin (North Fork).......................................... 11-17 11.2.6 Winter Steelhead—Lewis Subbasin (North Fork)........................................... -
Lewis River & Vancouver Lake
LEWIS RIVER–VANCOUVER LAKE WATER TRAIL P ADDLING GUIDE table Of cOntents overview Map/legend ............................................. 1 welcome .................................................................... 2 How to Use guide ..................................................... 3 safety ......................................................................... 4 etiquette .................................................................... 5 Trail Maps .............................................................. 6-21 n. Fork lewis river: woodland ........................6-7 e. Fork lewis river: la center ..........................8-9 lake river: n. ridgefield ................................ 10-11 Bachelor Island slough/ridgefieldr efuge ....12-13 lake river: s. ridgefield ................................14-15 lake river: s. green lake ...............................16-17 vancouver lake: west ....................................18-19 vancouver lake: east .....................................20-21 gear checklist ......................................................... 22 resources ................................................................ 23 credits & acknowledgements .............................. 24 notes ....................................................................... 25 Overview Map shOwing all rOutes he 32 river miles in this water trail include Vancouver TLake (more than 5 miles to circumnavigate), the full extent of Lake River (~11.5 miles), a section of the Columbia River along the west side of Bachelor -
Glaciation in the Lower Lewis River Basin, Southwestern Cascade Range, Washington
MauriceJ. Mundorftr 1428 SeaCtiff Dr. NV. Gig Harbor,Vashingron 91t335 Glaciation in the Lower Lewis River Basin, Southwestern Cascade Range, Washington Abstracl In pre Fraser time, accumulation of ice io the uplrr Le$'is Rivcr basin bccame so extensive that a largc ice-tongue cxtcndcrl do*'n vrlley and spread widely in the lower l-ewis River Basin, rcaching to wirhin abour 8 km of the prcscnt r()ute of Interstate Highway I'5. The ice-tongue, more than 60{J m $ick ar Cougar, sprcad across Chelatchie Prairic and into the East Fork lex'is Rivcr basin. extcnding dr)*'n rhnr valley to near Banlc Ground. The ice also fLowcd up Canyon and Stuuxon Creeks, and the l;rst lork l,ewis River. Extensive deltaic and ponded outwash deposits wcrc formcd at many places. c)dler fc,rtures of thc glaciation include boulder trains, erratic boulders, and rock drumlins. Glacial-caused drainage changcs include changes in the course of the Dast Fork Lewis R;ve. and Cnnyon Crcck. Although more dran ooe glacial advance may be represented, the maioriry ol thc deposits appe^r ro represcnt a sioglc giacial epiode. Carbon-l4 dating of wood from the ponded deposits indicates drat thcy are morc than 60,000 ycars old. The depth of weathcring and rind thickncss suggest rhar dre alaciation occurrcd in late Pleistocen€ time, considcrably bcfore the Fraserglaciarion. Younger, FraseFage glac;ers orig;natcd in cirques with floors at altitudcs of 825 to 915 m at the heads of many drainagcs in the Canyon and Siouxon Creck basirx.