Bugler Winter 2010-2011 Newspaper
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Washington State's Scenic Byways & Road Trips
waShington State’S Scenic BywayS & Road tRipS inSide: Road Maps & Scenic drives planning tips points of interest 2 taBLe of contentS waShington State’S Scenic BywayS & Road tRipS introduction 3 Washington State’s Scenic Byways & Road Trips guide has been made possible State Map overview of Scenic Byways 4 through funding from the Federal Highway Administration’s National Scenic Byways Program, Washington State Department of Transportation and aLL aMeRican RoadS Washington State Tourism. waShington State depaRtMent of coMMeRce Chinook Pass Scenic Byway 9 director, Rogers Weed International Selkirk Loop 15 waShington State touRiSM executive director, Marsha Massey nationaL Scenic BywayS Marketing Manager, Betsy Gabel product development Manager, Michelle Campbell Coulee Corridor 21 waShington State depaRtMent of tRanSpoRtation Mountains to Sound Greenway 25 Secretary of transportation, Paula Hammond director, highways and Local programs, Kathleen Davis Stevens Pass Greenway 29 Scenic Byways coordinator, Ed Spilker Strait of Juan de Fuca - Highway 112 33 Byway leaders and an interagency advisory group with representatives from the White Pass Scenic Byway 37 Washington State Department of Transportation, Washington State Department of Agriculture, Washington State Department of Fish & Wildlife, Washington State Tourism, Washington State Parks and Recreation Commission and State Scenic BywayS Audubon Washington were also instrumental in the creation of this guide. Cape Flattery Tribal Scenic Byway 40 puBLiShing SeRviceS pRovided By deStination -
Elwha River Restoration Site Bulletin 2012
Learn More About Elwha River Restoration 1 Lower Elwha Klallam 6 Feiro Marine Life Center Tribal Center 1 Interact with Elwha exhibits that Walk the 0.7 mile Warrior Path loop to feature a hands-on model of Glines Canyon Dam and Lake Mills. the Elwha River estuary. 6 Lower Elwha Road 315 N. Lincoln Street 2 Elwha River Bridge 2 7 Museum at the Carnegie 7 Cross the Elwha River bridge to get a Elwha River Learn about the historic Elwha Valley, birds eye view the river and connect to Bridge including Glines Canyon and Elwha the Olympic Discovery Trail. Elwha River dams, through informative exhibits. Elwha River Road Road 207 South Lincoln Street 3 3 Elwha Dam Viewpoint 8 Port Angeles Library Surround yourself with art created Stroll a short trail to an overlook to Port Angeles view ecosystem restoration at the Lake Aldwell for the September 2011 ceremony Former 9 Library celebrating the beginning of dam former site of the Elwha Dam. Delta Access 8 Lake Aldwell removal. June - Labor Day 2012 Lower Dam Road (drained) Elwha River Viewpoint 2210 South Peabody 4 4 Elwha River Viewpoint 9 Olympic National Park Observe a changing landscape where Visitor Center the Elwha River flows through the site View exhibits and ask a ranger about of the former Lake Aldwell reservoir. Elwha River Restoration updates. Highway 101 3002 Mount Angeles Road 5 5 Elwha Valley 10 Hurricane Ridge Experience Elwha Valley, with its Visitor Center spectacular river views and easy Enjoy vistas of the Elwha Valley and access to Madison Falls and other 10 surrounding mountains. -
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. -
History of the Club from a to Z
, . THE KLAHHANE CLUB GOLDEN ANNIVERSARY 1965 founded in 1915 I DEDICATION To the men and women who founded this Club our sincere appreciation To future members may this Club give you the same deep contentment in the outdoors and the same abiding friendships that it has granted to its members both past and present II PREFACE The desire to explore remote places, to enjoy the out-of-doors, to conquer difficult terrain, and to share these triumphs with congenial souls, has been the motivating force behind the formation of many an outdoor club. So it has been with the Klahhane Club. From the enjoyment of our heritage of mountain, sea, and forest, comes renewed strength and a spirit of delight which carries over into our workaday world. This is an enthusiasm which may be aroused in early childhood or later in life, but once aroused, it continues to delight throughout life, even after hiking days are done. May I conclude with a quotation from Mr. Thomas Gupthill, who wrote in the first Klahhane Annual of 1918, "Favored is he who is privi- leged to join that charmed circle of congenial spirits who find inspiration and recreation in unfrequented aisle and far reaches." by Primrose Bred! III PRESIDENT'S REMARKS Klahhane or good-times-out-of-doors has meant more to me during my fifty years of membership than any other organization. Being president (usually when no one else would take it) has been only a small part of it. There is some- thing inexplainable about its lure. You leave your safe comfortable home to go and climb a mountain. -
Media Kit 2015 Table of Contents
MEDIA KIT 2015 TABLE OF CONTENTS Fact Sheet Olympic National Park at a Glance Lake Crescent Lodge Lake Quinault Lodge Lake Quinault Lodge Tours Sol Duc Hot Springs Resort Log Cabin Resort Activities Weddings and Special Events Media Resources About Aramark Parks and Destinations FACT SHEET ADDRESS Lake Crescent Lodge Sol Duc Hot Springs Resort 416 Lake Crescent Road 12076 Sol Duc Hot Springs Road Olympic National Park, WA 98363 Port Angeles, WA 98363 Reservations: 866-297-7367 Reservations: 866-297-7367 Lake Quinault Lodge Log Cabin Resort 345 South Shore Road 3183 East Beach Road Quinault, WA 98575 Port Angeles, WA 98363 Reservations: 866-297-7367 Reservations: 866-297-7367 WEBSITE www.olympicnationalparks.com www.facebook.com/olympicnationalpark LOCATION Olympic National Park is located on Washington’s Olympic Peninsula, which lies west of Seattle and due south of Victoria, Canada. The park includes three distinct ecosystems: coastal, rainforest and sub-alpine with amazing vistas such as glacier-covered mountains, sea stacks and mountain lakes. The park’s nearly million acres are mostly contained within Highway 101, which forms a loop around the peninsula. SEASON Olympic National Park is open year round and each season brings with it a special flair—from snow and storm watching in winter, to hiking and kayaking in summer. Lake Quinault Lodge is open year-round, while Lake Crescent Lodge, Sol Duc Hot Springs Resort and Log Cabin Resort on the north end of the park close for winter. VICTORIA B.C. PORT ANGELES LAKE SEQUIM CRESCENT LODGE PORT TOWNSEND LOG CABIN RESORT FORKS SOL DUC HOT SPRINGS HURRICANE RIDGE Olympic National Park BREMERTON SEATTLE LAKE QUINAULT LODGE Olympic National Forest TACOMA ABERDEEN OLYMPIA TO PORTLAND FACT SHEET HISTORY OF THIS LAND The history of Olympic National Park is as rich as the land and the water within it. -
2.4 Elwha River and Tributaries Page 2.4-1
Chapter 2.4 Elwha River and Tributaries Page 2.4-1 2.4 ELWHA RIVER AND TRIBUTARIES 2.4.1 Overview The Elwha River is the largest watershed in the EMMT area and it constitutes the westernmost watershed within the planning area (Figure 2.4-1). The Elwha mainstem is approximately 45 miles long, has 100 miles of tributary streams, has a basin averaging approximately ten miles wide in an east-west direction, and drains 321 square miles of the Olympic Peninsula. Eighty-three percent of the drainage, including the upper 35 miles of the mainstem, lies within Olympic National Park, and is therefore protected from timber harvest, agriculture, and other land-use disturbances. The river flows in a northerly direction into the Strait of Juan de Fuca, entering the strait five miles west of Port Angeles. The Elwha is the fourth largest river, by drainage area, among all Olympic Peninsula streams, with a watershed area smaller only than those of the Quillayute, Queets, and Quinault rivers. Two major hydroelectric developments have altered the historic condition of the Elwha River. The Elwha Dam, built at RM 4.9 beginning in 1910, now impounds the 2.5-mile long Lake Aldwell reservoir, and the Glines Canyon Dam, built at RM 13.4, now impounds the 2.8-mile long Lake Mills reservoir. Originally built and operated to produce electricity for Port Angeles and beyond (supplying power as far away as Bremerton and Port Townsend prior to 1921), the dams have been fully allocated to supplying power to the pulp mill now operated by Nippon Paper Industries USA since the early 1920s. -
Tectonic Evolution of the Cenozoic Olympic Subduction Complex, Washington State, As Deduced from Fission Track Ages for Detrital Zircons Mark T
[AMERICAN JOURNAL OF SCIENCE, VOL. 292, OCTOBER, 1992, P. 565-636) TECTONIC EVOLUTION OF THE CENOZOIC OLYMPIC SUBDUCTION COMPLEX, WASHINGTON STATE, AS DEDUCED FROM FISSION TRACK AGES FOR DETRITAL ZIRCONS MARK T. BRANDON* and JOSEPH A. VANCE** ABSTRACT. The Olympic subduction complex (OSC), exposed in the Olympic Mountains of northwest Washington State, consists of an imbricated assemblage of Cenozoic sandstone, mudstone, and minor pillow basalt. The tectonic evolution of the OSC has been difficult to resolve because of poor age control, especially for the more easterly parts of the complex. The fission track (FT) method is used here to date detrital zircons fromsandstones of the OSC in order to define better the timing of deposition, subduction accretion, and metamorphism. The external detector method was, used to determine grain ag-es for individual detrital zircons. For unreset samples, the detrital zircons retain pre-depositional FT ages, which are related to the thermal history of the source region from which the zircons were derived. The samples are inferred never to have seen temperatures in excess of about 175 to 185°C. For these samples, determination of the FT age of the youngest population of grain ages is especially useful because it repre sents the maximum age for deposition of the sediment. For reset sam£les, maximum temperatures are inferred to have exceeded 240° to 245 C, so that the zircons were annealed after deposition. Zircon grain ages from these samples show a restricted range of ages which can be used to define a coohng age for the rock following metamorphism. We report FT results for 19 sandstone samples with a total of 928 grain ages. -
< )Lyrn Pic :\Fountains, \Yashington
JUL 31 1978 PLEAS;: RETU1N JQ j..i2.~ .. \~~r: ~ I-· l1c~ S11 ~lt t'~lttt ~<- ~ <l f. tJ 1t' <)lyrn pic :\fountains, \Yashington- ~- \ 11 ~ 1l \-s i s cl f · ~ t S11l J r ltt (, 1i (J t 1 Zr >r 1 t ~ .., :_ J,-..~i~-,;.: ... ~~. ·~ The Structure of the Olympic Mountains, Washington-. Analysis of a Subduction Zone By R. W. TABOR and W. M. CADY GEOLOGICAL SURVEY PROFESSIONAL PAPER 1033 UN I TED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1978 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress Cataloging in Publication Data Tabor, Rowland W. The structure of the Olympic Mountains, Washington. Geological Survey Professional Paper 1033 Bibliography: p. 24-25. 1. Geology-Washington (State)-Olympic Mountains. I. Cady, Wallace Martin, 1912- joint author. II. Title. III. Series: United States Geological Survey Professional Paper 1033 QE176.038T3 557.97'94 76-606187 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock No. 024-001-03079-9 CONTENTS Page Page ~bstract____________________________________________________ 1 Structural geology of the eastern core-Continued Introduction ------------------------------------------------ 1 Tectonic fabric-Continued Summary of regional geology ---------------------------- 1 Pencil structures ____________________________________ 10 Procedure and acknowledgments ------------------------ 3 Stretched clast lineations ____________________________ 12 Structural geology of the -
Mount Rainier & Olympic National
COMPLIMENTARY $3.95 2019/2020 YOUR COMPLETE GUIDE TO THE PARKS MOUNT RAINIER, OLYMPIC & NORTH CASCADES ACTIVITIES • SIGHTSEEING • DINING • LODGING TRAILS • HISTORY • MAPS • MORE OFFICIAL PARTNERS T:5.375” S:4.75” WELCOME S:7.375” WelcomeT:8.375” to the national parks of West- you to explore and enjoy. From historic SO TASTY EVERYONE WILL WANT A BITE. ern Washington! Congress gave these sites along the Lewis and Clark trail to spectacular mountain reserves their com- the orca whales off the coast of San Juan mon mission when it established the Na- Island, a side trip to one of Washington’s tional Park Service in 1916. All national National Park Service sites listed in the parks share the same goal, to “conserve “More Washington Parks” chapter is sure the scenery and the natural and historic to be worth your while! objects and the wildlife therein, and to pro- vide for the enjoyment of the same...by such means as will leave them unimpaired for the enjoyment of future generations.” FUN FACTS Mount Rainier, Olympic and North Cas- cades National Parks—three of the more Established: Mount Rainier National than 400 parks in the National Park Sys- Park was established in 1899, Olympic tem—conserve more than 1.6 million acres was established in 1938 and North Cas- of public land and provide enjoyment for cades was established in 1968. millions of visitors each year. Within sight Land Area: The three national parks conserve more than 1.6 million acres of of greater Seattle’s rapidly growing popu- public land. -
MOUNTAIN Day Trip Map Hurricane Ridge, Madison Falls
Pick up a free copy of this map and itinerary in the Main House. MOUNTAIN Day Trip Map Hurricane Ridge, Madison Falls Domaine 5 Madeleine Ediz Hook 146 Wildflower Lane Reservation for Port Angeles, WA Camp Hayden Rd. Native Birds Marine Dr. To S. Tumwater Truck Rte Old Olympic Hwy. Neah Bay 6 Elwha River 3 Race St. Observation 8 New Area Harbinger Day Winery Eatery 4 Mount Angeles Rd. To To Country Aire Sequim Lake Crescent Natural Foods Hurricane Olympic Hot Ridge Rd. Springs Rd. 7 For the 2019-2020 WINTER SEASON, Madison Falls November 29 through March 29, Trailhead 1 Hurricane Ridge Road is scheduled to be Road Closed Heart O the Hills open to uphill traffic from 9am to 4pm, to Vehicles Ranger Station Fridays, Saturdays and Sundays, Beyond this weather and road conditions permitting. Point Vehicles are required to carry tire chains 2 and be off the mountain by 5:00pm. Hurricane Ridge Trails Learn about skiing, snowboarding Visitor and tubing at hurricaneridge.com. Center 1. Heart O the Hills Ranger Station: This is an Olympic National Park gate. 15 mi. from us. $30 Park Entry Fee. Good for 7 days. Road conditions/weather, call (360) 565-3131. Webcam of the view: shorturl.at/efCDO Parking lot cam: shorturl.at/dnBRZ 2. Hurricane Ridge Visitor Center: 30 minutes from the gate to the parking lot. 5,242 ft. elevation. Restrooms open year-round. Snack bar and gift shop open in summer. Sweeping views of the Olympic Mountains. Great hikes right from the parking lot. 3. New Day Eatery: 102 W. -
An Administrative History of Olympic National Park
American Eden An Administrative History Of Olympic National Park By Hal K. Rothman National Park Service American Eden: An Administrative History Of Olympic National Park By Hal K. Rothman FINAL DRAFT ADMINISTRATIVE HISTORY July 2006 Not for public distribution Do not photocopy or quote Without the written permission of the National Park Service An American Eden Table of Contents List of Maps ................................................................................................................iii Introduction.................................................................................................................v 1. Before the Park: The Olympic Peninsula Before 1909...........................................1 2. Creating the Park...................................................................................................39 3. Planning and Administering Olympic National Park ...........................................87 4. Natural Resource Management...........................................................................151 5. Cultural Resource Management..........................................................................207 6. Interpreting the Wilderness … and More ...........................................................245 7. Running the Park.................................................................................................285 8. Threats to the Park ..............................................................................................327 Appendices A. Olympic National Park Superintendents -
Olympic Mountains Field Trip Guide
1 OLYMPIC MOUNTAINS FIELD TRIP GUIDE September 14-15, 2013 Jim Aldrich INTRODUCTION The Olympic Mountains of northwestern Washington are the result of the Juan de Fuca plate descending beneath the North American plate at the Cascadia subduction zone, accreting oceanic crust onto the Cascadia subduction wedge (Figure 1). The accreted oceanic sediments, structurally overlain on the east by Coast Range terrane, are largely below sealevel but are exposed on land in the Olympic Mountains (Olympic Structural Complex) (Figure 2). The Cascadia forearc, the area between the volcanic arc and subduction zone, has a topographic low (from north to south the Georgia Straits, Puget Sound, and Willamette Valley) and high (Insular Range of Vancouver Island and Coast Range of Washington and Oregon) (Figure 3). The forearc high is the crest of the accretionary wedge. Early investigations of the subduction process envisioned a snowplow model with accreted material being piled up against a rigid backstop in the overriding plate; however, the backstop material was deforming along with the accreted sediments in many convergent plate boundaries. Sandbox experiments by Davis et al. (1983) provided a solution to the backstop problem. The experimental box consisted of horizontal layers of sand (upper plate) overlying a sheet of Mylar on a flat rigid base with adjustable dip. As the Mylar sheet was pulled beneath the sand forward- and backward-verging thrusts formed creating a double-sided wedge (a pro-wedge and retro-wedge) at the point S the “subducting” plate (pro-plate), moved below the overriding plate (retro-plate) (Figure 4). These experiments served as the basis for an accretionary wedge model in which the crust of the overriding plate drapes over the subduction zone of mantle (at S or retro-shear zone), causing it to deform over a broad area while creating a doubly vergent wedge (Willett et al., 1993).