WRIA 18 Salmonid Habitat Limiting Factors Analysis
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1922 Elizabeth T
co.rYRIG HT, 192' The Moootainetro !scot1oror,d The MOUNTAINEER VOLUME FIFTEEN Number One D EC E M BER 15, 1 9 2 2 ffiount Adams, ffiount St. Helens and the (!oat Rocks I ncoq)Ora,tecl 1913 Organized 190!i EDITORlAL ST AitF 1922 Elizabeth T. Kirk,vood, Eclttor Margaret W. Hazard, Associate Editor· Fairman B. L�e, Publication Manager Arthur L. Loveless Effie L. Chapman Subsc1·iption Price. $2.00 per year. Annual ·(onl�') Se,·ent�·-Five Cents. Published by The Mountaineers lncorJ,orated Seattle, Washington Enlerecl as second-class matter December 15, 19t0. at the Post Office . at . eattle, "\Yash., under the .-\0t of March 3. 1879. .... I MOUNT ADAMS lllobcl Furrs AND REFLEC'rION POOL .. <§rtttings from Aristibes (. Jhoutribes Author of "ll3ith the <6obs on lltount ®l!!mµus" �. • � J� �·,,. ., .. e,..:,L....._d.L.. F_,,,.... cL.. ��-_, _..__ f.. pt",- 1-� r�._ '-';a_ ..ll.-�· t'� 1- tt.. �ti.. ..._.._....L- -.L.--e-- a';. ��c..L. 41- �. C4v(, � � �·,,-- �JL.,�f w/U. J/,--«---fi:( -A- -tr·�� �, : 'JJ! -, Y .,..._, e� .,...,____,� � � t-..__., ,..._ -u..,·,- .,..,_, ;-:.. � --r J /-e,-i L,J i-.,( '"'; 1..........,.- e..r- ,';z__ /-t.-.--,r� ;.,-.,.....__ � � ..-...,.,-<. ,.,.f--· :tL. ��- ''F.....- ,',L � .,.__ � 'f- f-� --"- ��7 � �. � �;')'... f ><- -a.c__ c/ � r v-f'.fl,'7'71.. I /!,,-e..-,K-// ,l...,"4/YL... t:l,._ c.J.� J..,_-...A 'f ',y-r/� �- lL.. ��•-/IC,/ ,V l j I '/ ;· , CONTENTS i Page Greetings .......................................................................tlristicles }!}, Phoiitricles ........ r The Mount Adams, Mount St. Helens, and the Goat Rocks Outing .......................................... B1/.ith Page Bennett 9 1 Selected References from Preceding Mount Adams and Mount St. -
Jefferson County Hazard Identification and Vulnerability Assessment 2011 2
Jefferson County Department of Emergency Management 81 Elkins Road, Port Hadlock, Washington 98339 - Phone: (360) 385-9368 Email: [email protected] TABLE OF CONTENTS PURPOSE 3 EXECUTIVE SUMMARY 4 I. INTRODUCTION 6 II. GEOGRAPHIC CHARACTERISTICS 6 III. DEMOGRAPHIC ASPECTS 7 IV. SIGNIFICANT HISTORICAL DISASTER EVENTS 9 V. NATURAL HAZARDS 12 • AVALANCHE 13 • DROUGHT 14 • EARTHQUAKES 17 • FLOOD 24 • LANDSLIDE 32 • SEVERE LOCAL STORM 34 • TSUNAMI / SEICHE 38 • VOLCANO 42 • WILDLAND / FOREST / INTERFACE FIRES 45 VI. TECHNOLOGICAL (HUMAN MADE) HAZARDS 48 • CIVIL DISTURBANCE 49 • DAM FAILURE 51 • ENERGY EMERGENCY 53 • FOOD AND WATER CONTAMINATION 56 • HAZARDOUS MATERIALS 58 • MARINE OIL SPILL – MAJOR POLLUTION EVENT 60 • SHELTER / REFUGE SITE 62 • TERRORISM 64 • URBAN FIRE 67 RESOURCES / REFERENCES 69 Jefferson County Hazard Identification and Vulnerability Assessment 2011 2 PURPOSE This Hazard Identification and Vulnerability Assessment (HIVA) document describes known natural and technological (human-made) hazards that could potentially impact the lives, economy, environment, and property of residents of Jefferson County. It provides a foundation for further planning to ensure that County leadership, agencies, and citizens are aware and prepared to meet the effects of disasters and emergencies. Incident management cannot be event driven. Through increased awareness and preventive measures, the ultimate goal is to help ensure a unified approach that will lesson vulnerability to hazards over time. The HIVA is not a detailed study, but a general overview of known hazards that can affect Jefferson County. Jefferson County Hazard Identification and Vulnerability Assessment 2011 3 EXECUTIVE SUMMARY An integrated emergency management approach involves hazard identification, risk assessment, and vulnerability analysis. This document, the Hazard Identification and Vulnerability Assessment (HIVA) describes the hazard identification and assessment of both natural hazards and technological, or human caused hazards, which exist for the people of Jefferson County. -
Geomorphic Character, Age and Distribution of Rock Glaciers in the Olympic Mountains, Washington
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 1987 Geomorphic character, age and distribution of rock glaciers in the Olympic Mountains, Washington Steven Paul Welter Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geology Commons, and the Geomorphology Commons Let us know how access to this document benefits ou.y Recommended Citation Welter, Steven Paul, "Geomorphic character, age and distribution of rock glaciers in the Olympic Mountains, Washington" (1987). Dissertations and Theses. Paper 3558. https://doi.org/10.15760/etd.5440 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. For more information, please contact [email protected]. AN ABSTRACT OF THE THESIS OF Steven Paul Welter for the Master of Science in Geography presented August 7, 1987. Title: The Geomorphic Character, Age, and Distribution of Rock Glaciers in the Olympic Mountains, Washington APPROVED BY MEMBERS OF THE THESIS COMMITTEE: Rock glaciers are tongue-shaped or lobate masses of rock debris which occur below cliffs and talus in many alpine regions. They are best developed in continental alpine climates where it is cold enough to preserve a core or matrix of ice within the rock mass but insufficiently snowy to produce true glaciers. Previous reports have identified and briefly described several rock glaciers in the Olympic Mountains, Washington {Long 1975a, pp. 39-41; Nebert 1984), but no detailed integrative study has been made regarding the geomorphic character, age, 2 and distribution of these features. -
Salmon and Steelhead Habitat Limiting Factors
SALMON AND STEELHEAD HABITAT LIMITING FACTORS WATER RESOURCE INVENTORY AREA 16 DOSEWALLIPS-SKOKOMISH BASIN Hamma Hamma River, Ecology Oblique Photo, 2001 WASHINGTON STATE CONSERVATION COMMISSION FINAL REPORT Ginna Correa June 2003 ACKNOWLEDGEMENTS The WRIA 16 salmon habitat limiting factors report could not have been completed without considerable contributions of time and effort from the following people who participated in various capacities on the technical advisory group (TAG): Charles Toal, Washington Department of Ecology Doris Small, Washington Department of Fish and Wildlife Herb Cargill, Washington Department of Natural Resources Jeff Davis, Washington Department of Fish and Wildlife Jeff Heinis, Skokomish Tribe John Cambalik, Puget Sound Action Team Marc McHenry, US Forest Service Margie Schirato, Washington Department of Fish and Wildlife Marty Ereth, Skokomish Tribe Randy Johnson, Washington Department of Fish and Wildlife Richard Brocksmith, Hood Canal Coordinating Council Steve Todd, Point No Point Treaty Council In addition, the author also wishes to thank the following for extensive information regarding fish populations and habitat conditions and substantial editorial comments during development of the report: Dr. Carol Smith, WCC for the Introduction chapter of this report; Carol Thayer, WDNR, for extensive GIS analysis of DNR ownership; Carrie Cook-Tabor, USFWS, for data contribution on the Hamma Hamma; Denise Forbes, Mason County Public Works, for the county perspective on the Skokomish; Ed Manary, WCC, for his guidance -
A G~Ographic Dictionary of Washington
' ' ., • I ,•,, ... I II•''• -. .. ' . '' . ... .; - . .II. • ~ ~ ,..,..\f •• ... • - WASHINGTON GEOLOGICAL SURVEY HENRY LANDES, State Geologist BULLETIN No. 17 A G~ographic Dictionary of Washington By HENRY LANDES OLYMPIA FRAN K M, LAMBORN ~PUBLIC PRINTER 1917 BOARD OF GEOLOGICAL SURVEY. Governor ERNEST LISTER, Chairman. Lieutenant Governor Louis F. HART. State Treasurer W.W. SHERMAN, Secretary. President HENRY SuzzALLO. President ERNEST 0. HOLLAND. HENRY LANDES, State Geologist. LETTER OF TRANSMITTAL. Go,:ernor Ernest Lister, Chairman, and Members of the Board of Geological Survey: GENTLEMEN : I have the honor to submit herewith a report entitled "A Geographic Dictionary of Washington," with the recommendation that it be printed as Bulletin No. 17 of the Sun-ey reports. Very respectfully, HENRY LAKDES, State Geologist. University Station, Seattle, December 1, 1917. TABLE OF CONTENTS. Page CHAPTER I. GENERAL INFORMATION............................. 7 I Location and Area................................... .. ... .. 7 Topography ... .... : . 8 Olympic Mountains . 8 Willapa Hills . • . 9 Puget Sound Basin. 10 Cascade Mountains . 11 Okanogan Highlands ................................ : ....' . 13 Columbia Plateau . 13 Blue Mountains ..................................... , . 15 Selkirk Mountains ......... : . : ... : .. : . 15 Clhnate . 16 Temperature ......... .' . .. 16 Rainfall . 19 United States Weather Bureau Stations....................... 38 Drainage . 38 Stream Gaging Stations. 42 Gradient of Columbia River. 44 Summary of Discharge -
1968 Mountaineer Outings
The Mountaineer The Mountaineer 1969 Cover Photo: Mount Shuksan, near north boundary North Cascades National Park-Lee Mann Entered as second-class matter, April 8, 1922, at Post Office, Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during June by The Mountaineers, P.O. Box 122, Seattle, Washington 98111. Clubroom is at 7191h Pike Street, Seattle. Subscription price monthly Bulletin and Annual, $5.00 per year. EDITORIAL STAFF: Alice Thorn, editor; Loretta Slat er, Betty Manning. Material and photographs should be submitted to The Mountaineers, at above address, before Novem ber 1, 1969, for consideration. Photographs should be black and white glossy prints, 5x7, with caption and photographer's name on back. Manuscripts should be typed double-spaced and include writer's name, address and phone number. foreword Since the North Cascades National Park was indubi tably the event of this past year, this issue of The Mountaineer attempts to record aspects of that event. Many other magazines and groups have celebrated by now, of course, but hopefully we have managed to avoid total redundancy. Probably there will be few outward signs of the new management in the park this summer. A great deal of thinking and planning is in progress as the Park Serv ice shapes its policies and plans developments. The North Cross-State highway, while accessible by four wheel vehicle, is by no means fully open to the public yet. So, visitors and hikers are unlikely to "see" the changeover to park status right away. But the first articles in this annual reveal both the thinking and work which led to the park, and the think ing which must now be done about how the park is to be used. -
Geologic Map of Washington - Northwest Quadrant
GEOLOGIC MAP OF WASHINGTON - NORTHWEST QUADRANT by JOE D. DRAGOVICH, ROBERT L. LOGAN, HENRY W. SCHASSE, TIMOTHY J. WALSH, WILLIAM S. LINGLEY, JR., DAVID K . NORMAN, WENDY J. GERSTEL, THOMAS J. LAPEN, J. ERIC SCHUSTER, AND KAREN D. MEYERS WASHINGTON DIVISION Of GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 •• WASHINGTON STATE DEPARTMENTOF 4 r Natural Resources Doug Sutherland· Commissioner of Pubhc Lands Division ol Geology and Earth Resources Ron Telssera, Slate Geologist WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Ron Teissere, State Geologist David K. Norman, Assistant State Geologist GEOLOGIC MAP OF WASHINGTON NORTHWEST QUADRANT by Joe D. Dragovich, Robert L. Logan, Henry W. Schasse, Timothy J. Walsh, William S. Lingley, Jr., David K. Norman, Wendy J. Gerstel, Thomas J. Lapen, J. Eric Schuster, and Karen D. Meyers This publication is dedicated to Rowland W. Tabor, U.S. Geological Survey, retired, in recognition and appreciation of his fundamental contributions to geologic mapping and geologic understanding in the Cascade Range and Olympic Mountains. WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 Envelope photo: View to the northeast from Hurricane Ridge in the Olympic Mountains across the eastern Strait of Juan de Fuca to the northern Cascade Range. The Dungeness River lowland, capped by late Pleistocene glacial sedi ments, is in the center foreground. Holocene Dungeness Spit is in the lower left foreground. Fidalgo Island and Mount Erie, composed of Jurassic intrusive and Jurassic to Cretaceous sedimentary rocks of the Fidalgo Complex, are visible as the first high point of land directly across the strait from Dungeness Spit. -
The Story of Three Olympic Peaks
THE STORY OF THREE OLYMPIC PEAKS The countless thousands who. from year to year. admire the three prominent peaks at the southeastern end of the Olympic Range would find themselves gazing at the wonderfully beautiful picture with even keener rapture if they but knew a part of the history interlocked with the names these peaks bear-Ellinor. The Brothers. and Constance. There are probably no other geographical features in the Pacific Northwest whose names involve a richer history. A beautiful and tender modesty screened the identity of the personalities behind those names. while a sin gle one of the four people survived. The last of the four was gathered to her fathers two years ago. and it is now possible to learn who were the people whose names have become so well known as geographical terms. In the first place let us see when and by whom the names were given to the mountains. The most accessible source is the Pacific Coast Pilot. which says: "When a vessel is going northward. and is clear of Vashon Island. the Jupiter Hills show over Blake Island. with Mount Constance to the southward. "1 A little further on the same work says; "Behind the Jupiter Hills is Mount Constance. 7777 feet elevation; Th~ Brothers. 6920 feet. and Mount Ellinor. estimated at 6500 feet. These great masses. rising so abruptly in wild, rocky peaks. are marks all over Admiralty Inlet and Puget Sound. but seem to overhang the main part of [Hood] Canal. The Brothers. a double peak. is less than seven miles from the water."2 Similar information is given in the reports made aI the time of the surveys. -
NMFS. 2016. Puget Chinook, Hood Canal Summer-Run
Science, Service, Stewardship 2016 5-Year Review: Summary & Evaluation of Puget Sound Chinook Salmon Hood Canal Summer-run Chum Salmon Puget Sound Steelhead National Marine Fisheries Service West Coast Region Portland, OR U.S. Department of Commerce I National Oceanic and Atmospheric Administration I National Marine Fisheries Service This page intentionally left blank 5-Year Review: Puget Sound NOAA Fisheries 5-Year Review: Puget Sound Species Species Reviewed Evolutionarily Significant Unit or Distinct Population Segment Chinook Salmon Puget Sound Chinook Salmon (Oncorhynchus tshawytscha) Chum Salmon Hood Canal Summer-run Chum Salmon (O. keta) Steelhead Puget Sound Steelhead (O. mykiss) i 5-Year Review: Puget Sound NOAA Fisheries This page intentionally left blank ii 5-Year Review: Puget Sound NOAA Fisheries Table of Contents 1 ∙ GENERAL INFORMATION ................................................................................................................................... 1 1.1 INTRODUCTION ......................................................................................................................................................... 1 1.1.1 Background on listing determinations .......................................................................................................... 1 1.2 METHODOLOGY USED TO COMPLETE THE REVIEW ............................................................................................................ 2 1.3 BACKGROUND – SUMMARY OF PREVIOUS REVIEWS, STATUTORY AND REGULATORY ACTIONS, AND -
Dosewallips River Powerlines Reach Restoration Project
Secure Rural Schools and Community Self-Determination Act of 2000 Public Law 110-343 Title II Project Submission Form USDA Forest Service Name of Resource Advisory Committee: Olympic Peninsula Project Number (Assigned by Designated Federal Official): Funding Fiscal Year(s): 2019-22 2. Project Name: Dosewallips River Powerlines 3a. State: Washington Reach Restoration Project 3b. County(s): Jefferson 4. Project Submitted By: Tami Pokorny, Jefferson 5. Date: 01/31/2019 County Environmental Public Health natural resources program coordinator 6. Contact Phone Number: 360/379-4498 7. Contact E-mail: [email protected] 8. Project Location: Dosewallips River RM 1.3-2.5 a. National Forest(s): Olympic NF is b. Forest Service District: Hood Canal upstream c. Location (Township-Range-Section) Sec. 34, T26 N, R 2W 9. Project Goals and Objectives: To improve floodplain and channel migration processes on the Dosewallips River in the largely protected Powerlines Reach by developing a preliminary design for high value restoration actions. These actions will improve floodplain conditions by restoring habitat structure and complexity to modified portions of the reach to benefit spawning and incubating of Hood Canal Summer Chum salmon. The design will be selected in consultation with a technical group convened by the County to include representation from the Lazy C and Brinnon communities. This SRS Title II request is needed to match a portion of RCO Salmon Recovery Funding Board grant #18-1228. The project’s objectives are to: i. Provide for regular communication and open exchange of ideas among project consultants, partners, landowners, and other community members. -
Geologic Map GM-57, Geologic Map of the Port Townsend North And
WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-57 122°52¢30² R2W R1W 50¢ 47¢30² 122°45¢ GEOLOGIC SETTING Landslide deposits—Gravel, sand, silt, clay, and boulders; clasts angular to Deposits of the Possession Glaciation ACKNOWLEDGMENTS modified from G. W. Thorsen (written Qls commun., 2004) and Easterbrook (1994) 1 rounded; unsorted; generally loose, unstratified, broken, and chaotic, but may Lower to middle Eocene Crescent Formation basaltic rocks form the basement for the Possession Drift (columnar sections and cross section only)—Glaciomarine This map was produced in cooperation with the U.S. Geological Survey National locally retain primary bedding structure; may include liquefaction features; Qgp 0–15 ft Qml till (regraded) northeastern Olympic Peninsula and are the oldest rocks exposed in the map area (Tabor and p drift and underlying till; distinguished from equivalent Vashon facies by Cooperative Geologic Mapping Program, Agreement Number 04HQAG0069, which partially 15–30 ft Qgt Qb Qc Qd Qf deposited by mass wasting processes other than soil creep and frost heave; Vashon till Qguc w Qf Cady, 1978). They consist mostly of columnar to massive flows with oxidized tops and stratigraphic position. Glaciomarine drift facies variegated; typically clay and silt- supported our mapping project. We thank Gerald W. Thorsen for extensive geologic advice, Qmw typically in unconformable contact with surrounding units. Scarps are shown Qd locally developed paleosols overlain by basaltic cobble to boulder conglomerate. rich diamicton; buff, gray, to dark gray; compact and commonly with vertical site-specific and general expertise, field trips, radiocarbon age data, and review of map and Vashon advance Qml Qguc where supported by lidar (light distance and ranging, based on airborne laser ~35 ft Qga outwash sand Qgo Qgt Qb The rocks of the Crescent Formation are overlain by an unnamed sandstone and siltstone desiccation cracks and shells; locally indistinguishable from till. -
Flattery Rocks National Wildlife Refuge
nacortes-Friday H A arbor Ferry Pe ar P oi FFrriiddaayynt Harbor y Harbor Ba r e n t a n m e r C e h s i F AAnnaaccoorrtteess 124°0'0"W 123°0'0"W n Tillicum k i l 1a a c pl 17 nd k U a ³² 1a a s c Belmont ³² r b P k a ³² p Glen J Park m y u Lake Ba * H " Luxton West Bay Y Colwood T Braemar James A Happy N Heights VViiccttoorriiaa D Bay Iceberg Valley A U t 1 Poin ³² N O S A C C Chibahdehl N Tatoosh Mushroom Slant Rocks Kydikabbit A Island U Rock Rock MIIDDWAAYY Point Koitlah British Columbia British Columbia J y Cr a Point anb Sah-da-ped-thl Warmhouse err B N y L Look- t a n k t Titacoclos CLASSET Beach Waadah i A e Through Rock CLASSET Po Albert ne Falls Island S or Cape r Head C Fuca t e Kan Archawat t gar Pillar Flattery First t oo Peak O in NEEAH Beach Second s (1308'') Bahokus re t o V C ek BAY Beach h Troxell il lage BAY Third n Peak i c W d Beach o t (1380'') R P e a B Av S A N J Y a y a w y M U A N C O U N T t r y Vie k c e c o Y IS h t T L A N C r R N D C O U N T Y t S U a ucket o O Y e d o T r l E ke C N e 14 ell ape F C N U Trox k C ³² A O re J U C e N O N W WAAAATTCCHH k S A R S d hi d Waatch F E N dbey Isla n Point E F n AS ad Hobuck J r ost Y F Beach Hobuck k a u r o Lake T e e C L C o l A y Bahobohosh r Y C A N N L A a Point L D T S T Waatch n A M A U ek a k N e O r Peak e C t ml re O Y n l M a C U T U C i Strawberry (1350') a d N C (1350') ka In u e h J N U n e T O O Fakkema B Rock R on s a Shipwreck Y N C T Y g es ati n N N e v C n r s s A e U n i U e u Point J C O d O u l N M S an J u an I sla nd s Silver Lake Sooes