Olympic National Park Long-Range Interpretive Plan November 2010 Olympic National Park Long-Range Interpretive Plan November 2010
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Research Article Late Middle Miocene Emergence of the Olympic Peninsula Shown by Sedimentary Provenance
GeoScienceWorld Lithosphere Volume 2020, Article ID 7040598, 20 pages https://doi.org/10.2113/2020/7040598 Research Article Late Middle Miocene Emergence of the Olympic Peninsula Shown by Sedimentary Provenance 1 1,2 Samuel Shekut and Alexis Licht 1Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, USA 2Centre Européen de Recherche et d’Enseignement des Géosciences de l’Environnement (Cerege), UMR CNRS7330, 13545 Aix-en-Provence, France Correspondence should be addressed to Samuel Shekut; [email protected] Received 29 January 2020; Accepted 19 September 2020; Published 6 November 2020 Academic Editor: Tamer S. Abu-Alam Copyright © 2020 Samuel Shekut and Alexis Licht. Exclusive Licensee GeoScienceWorld. Distributed under a Creative Commons Attribution License (CC BY 4.0). The Olympic Peninsula is the uplifted portion of the Cascadia accretionary wedge and forms the core of a 200 km scale oroclinal bend on the west coast of Washington State. The accretionary wedge started forming 45 million years ago following the accretion of the Siletzia igneous province along the Cascadia subduction margin. Low-temperature thermochronology studies have shown that the core of the peninsula has been continuously exhumed for the last 14 million years. The earlier onset of oroclinal bending, uplift, and emergence remains poorly documented. Here, we explore the Cenozoic drainage history of the Cascadia forearc and accretionary wedge to reconstruct the deformation history of the Olympic Peninsula. We use detrital zircon provenance and grain petrography data from modern rivers draining the Cascades, the Cascadia forearc and accretionary wedge, as well as from Eocene to late middle Miocene sedimentary units from the same areas. -
2017-18 Olympic Peninsula Travel Planner
Welcome! Photo: John Gussman Photo: Explore Olympic National Park, hiking trails & scenic drives Connect Wildlife, local cuisine, art & native culture Relax Ocean beaches, waterfalls, hot springs & spas Play Kayak, hike, bicycle, fish, surf & beachcomb Learn Interpretive programs & museums Enjoy Local festivals, wine & cider tasting, Twilight BRITISH COLUMBIA VANCOUVER ISLAND BRITISH COLUMBIA IDAHO 5 Discover Olympic Peninsula magic 101 WASHINGTON from lush Olympic rain forests, wild ocean beaches, snow-capped 101 mountains, pristine lakes, salmon-spawning rivers and friendly 90 towns along the way. Explore this magical area and all it has to offer! 5 82 This planner contains highlights of the region. E R PACIFIC OCEAN PACIFIC I V A R U M B I Go to OlympicPeninsula.org to find more O L C OREGON details and to plan your itinerary. 84 1 Table of Contents Welcome .........................................................1 Table of Contents .............................................2 This is Olympic National Park ............................2 Olympic National Park ......................................4 Olympic National Forest ...................................5 Quinault Rain Forest & Kalaloch Beaches ...........6 Forks, La Push & Hoh Rain Forest .......................8 Twilight ..........................................................9 Strait of Juan de Fuca Nat’l Scenic Byway ........ 10 Joyce, Clallam Bay/Sekiu ................................ 10 Neah Bay/Cape Flattery .................................. 11 Port Angeles, Lake Crescent -
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. -
Fort Worden State Park Fort Worden State Park
$ Q ! B % > B ! > ! ! ¼ ! ! D ! $ ! ¼ ! ¼ % ¼ ! ! ¼% $ ! ¼ % % !$ ! ! ! ! %% $¼ $ ¼ % ! ¼ ¼ % % % % ¼ % % % ¼$ % % ¼ > ¼ $ ! ! ¼ ! ! ¼ !! ¼ % ¼ % Q % ¼ %$ B $ ¼ ! ! ! ! % $ ¼ % ! : ! ¼ ! ! ¼ % $ % ¼ ¼ % % % ¼ D $ : > B % > % % ¼ % ! ! !$ ¼ % $ % B > ! % D ¼ D > > $ % B % : $ North Sound North Sound/Fort Worden State Park Fort Worden State Park Cascadia Marine Trail Fort Worden State Park Take a walk along the 11,000 feet of beach or hike up the bluffs to take in a Number of Sites: Overflow Camping: bird's-eye view at the entrance to Puget Sound. Be sure to take a flashlight 3 In the rest of campground and explore the haunted house-like maze of the underground passageways. Port Townsend is a popular destination and the park hosts many conferences including several musical Water: Sanitation Facilities: workshops (Centrum's Festival of American Fiddle Tunes, Jazz Port Townsend, and the Port Available in the day-use area N of the Toilets opposite of pier and showers at Townsend Acoustic Blues Festival. pier and across the road campground; open year-round Natural History: Extras: Ownership: # Mingle with intertidal plants and animals indigenous to Puget Sound at the Port Townsend Picnic areas, food concessions in day-use Washington State Parks and Recreation Marine Science Center. The Marine Exhibit at the end of the pier houses touch pools andCoupeville area and Marine Science Center aquaria highlighting local marine habitats. On shore, a current Natural History Exhibit is ! Fees: Fire Restrictions: "Learning# from Whales...the! story of Hope," which inlcudes a fully reconstructed Orca Ebey's Landing SP $12/night for up to 8 in site Fireplaces available skeleton. ^ ! Known Hazards: Special Considerations: Whidbey ^ Currents N of Pt. Wilson are potentially Very popular day-use beach. -
Final Environmental Impact Statement
Final Environmental Impact Statement Elwha River Ecosystem Restoration Implementation Purpose and Need: The Elwha River ecosystem and native anadromous fisheries are severely degraded as a result of two hydroelectric dams (projects) and their reservoirs built in the early 1900s. Congress has mandated the full restoration of this ecosystem and its native anadromous fisheries through the Elwha River Ecosystem and Fisheries Restoration Act (Public Law 102-495). The Department of the Interior has found there is a need to return this river and the ecosystem to its natural, self-regulating state, and proposes to implement the Congressional mandate by removing both dams in a safe, environmentally sound and cost effective manner and implementing fisheries and ecosystem restoration planning. Only dam removal would fully restore the ecosystem or its native anadromous fisheries. Proposed Action: The U.S. Department of the Interior proposes to fully restore the Elwha River ecosystem and native anadromous fisheries through the removal of Elwha Dam and Glines Canyon Dam and implementing fish restoration and revegetation. Dam removal would occur over a 2-year period. Elwha Dam would be removed by blasting, and Glines Canyon Dam by a combination of blasting and diamond wire saw cutting. Lake Aldwell would be drained by a diversion channel, and Lake Mills by notching down Glines Canyon Dam. Stored sediment would be eroded naturally by the Elwha River. The proposed action is located in Clallam County, on the Olympic Peninsula, in Washington State. Lead/Cooperating agencies: The National Park Service is the lead agency. The U.S. Fish and Wildlife Service, U.S. -
GLACIERS Glacial Ice Is One of the Foremost Scenic and Scientific Values of Olympic National Park
OLYMPIC NATIONAL PARK Glaciers MOUNT OLYMPUS GLACIERS Glacial ice is one of the foremost scenic and scientific values of Olympic National Park. There are about sixty glaciers crowning the Olympics peaks; most of them are quite small in contrast to the great rivers of ice in Alaska. The prominent glaciers are those on Mount Olympus covering approximately ten square miles. Beyond the Olympic complex are the glaciers of Mount Carrie, the Bailey Range, Mount Christie, and Mount Anderson. In the company of these glaciers are perpetual snowbanks that have the superficial appearance of glacial ice. Because they are lacking in the criteria below, they are (aerial view) not true glaciers. True glaciers are structurally three layered bodies of frozen water. The top layer is snow; the middle neve, or mixed snow and ice; and the bottom layer is of pure ice, which is quite plastic in nature. Crevasses or deep cracks in the glaciers form as the ice is subjected to uneven flow over alpine terrain. Another structural feature is the bergschrund, which is a prominent crevasse-like opening at the head of the glacier where the ice has been pulled away from the mountain wall. The rate of glacial flow is quite variable, and Olympic glaciers are "slow-moving" in contrast to some in Alaska which occasionally move at the rate of several hundred feet per day for short periods of time. There is no great advance of Olympic glaciers today, but there is not a rapid melting back of the ice either. Forward surges in glacial flow often occur after a number of very heavy winters and cool summers, but such activity has been relatively infrequent with Olympic glaciers in recorded time. -
State Park Contact Sheet Last Updated November 2016
WASHINGTON STATE PARKS AND RECREATION COMMISSION Film Permit Application State Park Contact Sheet Last Updated November 2016 AREA MANAGER PHONE PARK NAME PARK AREA ADDRESS EMAIL (@parks.wa.gov) REGION Sharon Soelter ALTA LAKE STATE PARK (509) 923-2473 Alta Lake State Park Alta Lake Area 1B OTTO ROAD [email protected] Eastern PATEROS WA 98846 Brian Hageman FORT WORDEN STATE PARK Anderson Lake (360) 344-4442 Olympic View Area 200 BATTERY WAY State Park [email protected] Southwest PORT TOWNSEND, WA 98368-3621 Chris Guidotti BATTLE GROUND STATE PARK Battle Ground Lake (360) 687-4621 Battle Ground Area PO BOX 148 State Park [email protected] Southwest HEISSON, WA 98622 Kevin Kratochvil RASAR STATE PARK (360) 757-0227 Bay View State Park Rasar Area 38730 CAPE HORN ROAD [email protected] Northwest CONCRETE, WA 98237 Chris Guidotti BATTLE GROUND STATE PARK Beacon Rock (509) 427-8265 Battle Ground Area PO BOX 148 State Park [email protected] Southwest HEISSON, WA 98622 Joel Pillers BELFAIR STATE PARK (360) 275-0668 Belfair State Park South Sound Area 3151 N.E. SR 300 [email protected] Southwest BELFAIR, WA 98528 Jack Hartt DECEPTION PASS STATE PARK Ben Ure Island Marine (360) 675-3767 Deception Pass Area 41020 STATE ROUTE 20 State Park [email protected] Northwest OAK HARBOR, WA 98277 Ted Morris BIRCH BAY STATE PARK (360) 371-2800 Birch Bay State Park Birch Bay Area 5105 HELWEG ROAD [email protected] Northwest BLAINE WA 98230 Dave Roe MANCHESTER STATE PARK Blake Island Marine (360) 731-8330 Blake -
Bugler Making Connections
Olympic National Park National Park Service Park Newspaper U.S. Department of the Interior Summer 2002 EXPERIENCE YOUR AMERICA Bugler Making Connections... ow does one of the most intriguing stories of old-growth forest connections A couple stands enraptured, gazing from Hurricane Ridge at the Hunite flying squirrels, spotted owls and truffles? Flying squirrels, usually magnificence of wilderness. On this wintry morning, caps of ice cover arboreal and hidden from predators, glide down to the forest floor to dig for the mountaintops, caps of wool cover their heads. Half a century ago, fragrant truffles. The spores from these underground fungi mix with nitrogen- when they honeymooned here, their eyes met the same views. fixing bacteria and yeasts in the squirrel's stomach, creating crucial nutritious They revisit their youth and renew their bonds, with each other and pellets for trees and spreading the spores of the fungi. with the land. Continuity and connections. Furthermore, the tiny roots of these truffles interconnect huge old-growth roots. They revisit their youth and renew their bonds, In a mutually beneficial relationship, the fungi stimulate tree root growth and the with each other and with the land. trees feed sugars and amino acids to the fungi. Through this underground network, the trees exchange nutrients among themselves, which essentially Just for a moment, during your trip to Olympic National Park, while creates one grand old-growth tree. standing beneath the glory of the mountains or amid the grandeur of evergreens, stop. Think of an intriguing natural or cultural feature that With the attention of the flying squirrel still focused on truffles, the keen-eyed you encountered during your visit. -
Flow of Blue Glacier, Olympic Mountains, Washington, U.S.A.*
Journa/ DiG/a ciD/OK)', Vol. 13, No. 68,1974 FLOW OF BLUE GLACIER, OLYMPIC MOUNTAINS, WASHINGTON, U.S.A.* By MARK F. MEIER, (U.S. Geological Survey, Tacoma, Washington g8408, U .S.A.) W. BARCLAY KAMB, CLARENCE R . ALLEN and ROBERT P. SHARP (California Institute of Technology, Pasaciena, California gl 109, U.S.A.) ABSTRACT. Velocity and stra in-rate patterns in a small temperate valley glacier display flow effects of channel geometry, ice thickness, surface slope, a nd ablation. Surface velocities of 20- 55 m /year show year to-year fluctuations of I .5- 3 m /year. Tra nsverse profiles of velocity have the form of a higher-order para bola modified by the effects of flow around a broad bend in the cha nnel, which makes the velocity profile asym metric, with maximum velocity displaced toward the outside of the bend. M arginal sliding rates are 5- 22 m/ year against bedrock a nd nil against debris. Velocity vectors diverge from the glacier center-line near the terminus, in response to surface ice loss, but converge toward it near the firn line because of channel narrowing. Plunge of the vectors gives an em ergence fl ow component that falls short of bala ncing ice loss by a bout I m /year. Center-line velocities vary systematically with ice thickness and surface slope. In the upper half of the reach studied , effects of changing thickness a nd slope tend to compensate, a nd velocities are nearly constant; in the lower half; the effects are cumula tive a nd velocities decrease progressively down-stream . -
UCLA SSIFI C ATI ON
F/m N.No. 10-300 REV. (9/77) / *7 3 UNITED STATES DEPARTMENT OF THE INTERIOR m2A NATIONAL PARK SERVICE NATIONAL REGISTER OF HISTORIC PLACES INVENTORY -- NOMINATION FORM SEE INSTRUCTIONS IN HOWTO COMPLETE NATIONAL REGISTER FORMS ___________TYPE ALL ENTRIES - COMPLETE APPLICABLE SECTIONS______ [NAME HISTORIC ROSEMARY INN AND/OR COMMON LOCATION STREET & NUMBER Barnes Point . Lake—Grescen _NOT FOR PUBLICATION CITY, TOWN CONGRESSIONAL DISTRICT 3rd- Donald L. Bonker Port Ancreles ^^-^f . —_ VICINITY OF ->-*-u- STATE CODE COUNTY CODE Washington 53 Clallam 009 UCLA SSIFI c ATI ON CATEGORY OWNERSHIP STATUS PRESENT USE f ^DISTRICT X-pUBLIC —OCCUPIED _ AGRICULTURE —MUSEUM ^BUILDING(S) —PRIVATE X-UNOCCUPIED —COMMERCIAL -JfARK —STRUCTURE —BOTH —WORK IN PROGRESS —EDUCATIONAL —PRIVATE RESIDENCE —SITE PUBLIC ACQUISITION ACCESSIBLE —ENTERTAINMENT —RELIGIOUS —OBJECT _|N PROCESS X-YES: RESTRICTED .^GOVERNMENT —SCIENTIFIC —BEING CONSIDERED — YES: UNRESTRICTED —INDUSTRIAL —TRANSPORTATION —NO —MILITARY —OTHER: QOWNER OF PROPERTY NAME United States Department of interior Matiion-a4— Park— &&ac\7\ r-^ m ympi r- STREET & NUMBER Natl.Park 600 East Park CITY, TOWN STATE Port Angeles VICINITY OF Washd natrm LOCATION OF LEGAL DESCRIPTION COURTHOUSE, REG.STRYOF DEEDS,.ETC. County ' Courthouse STREET & NUMBER East 4th & Lincoln Streets CITY, TOWN STATE Port j^cOaEL [1 REPRESENTATION IN EXISTING SURVEYS TITLE County Cultural Resource Survey DATE 1978 —FEDERAL —STATE _j£OUNTY __LOCAL DEPOSITORY FOR SURVEY RECORDS Clallam County Parks_ CITY. TOWN STATE Port Angeles Washington DESCRIPTION CONDITION CHECK ONE CHECK ONE —EXCELLENT —DETERIORATED X-UNALTERED X-ORIGINALSITE X-GOOD _RUINS —ALTERED —MOVED DATE. —FAIR _UNEXPOSED DESCRIBE THE PRESENT AND ORIGINAL (IF KNOWN) PHYSICAL APPEARANCE Rosemary Inn is a resort on Lake Crescent in the northwest corner of Washington State. -
Dungeness River Targeted Watershed Initiative FINAL REPORT
Dungeness River Targeted Watershed Initiative FINAL REPORT For E.P.A. Targeted Watershed Grant WS‐97098101‐0 Prepared By: Jamestown S’Klallam Tribe December 2009 FIGURES Figure 1. Dungeness Watershed on the Olympic Peninsula, Washington. ................................. 4 Figure 2. Dungeness Bay shellfish closure areas. ........................................................................ 6 Figure 3. Phase 1 MST (Ribotyping) sampling locations.............................................................. 9 Figure 4. Phase 2 MST (Bacteroides Target Specific PCR) sampling locations. ......................... 10 Figure 5. Mycoremediation Demonstration Site. ...................................................................... 11 Figure 6. Construction of Mycoremediation Demonstration Site............................................. 12 Figure 7. Schematic of Biofilitration Cells, with native plants and fungi in the Treatment cell and native plants only in the Control. Inflow water is split with equal volumes and fed to the two cells (not to scale). ........................................................ 13 Figure 8. Ground‐breaking excavation at the rain garden site, Helen Haller Elementary School, Sequim, WA.................................................................................................... 15 Figure 9. TWG fresh water monitoring stations and DOH marine monitoring stations. .......... 18 Figure 10. Fecal Coliform Concentration (CFU/100 ml) over 6‐Month Time Period (mean +/‐ standard deviation)................................................................................... -
Delineation of the Dungeness River Channel Migration Zone
Delineation of the Dungeness River Channel Migration Zone River Mouth to Canyon Creek Byron Rot Pam Edens Jamestown S’Klallam Tribe October 1, 2008 Acknowledgements This report was greatly improved from comments given by Patricia Olson, Department of Ecology, Tim Abbe, Entrix Corp, Joel Freudenthal, Yakima County Public Works, Bob Martin, Clallam County Emergency Services, and Randy Johnson, Jamestown S'Klallam Tribe. This project was not directly funded as a specific grant, but as one of many tribal tasks through the federal Pacific Coastal Salmon fund. We thank the federal government for their support of salmon recovery. Cover: Roof of house from Kinkade Island in January 2002 flood (Reach 6), large CMZ between Hwy 101 and RR Bridge (Reach 4, April 2007), and Dungeness River Channel Migration Zone map, Reach 6. ii Table of Contents Introduction………………………………………………………….1 Legal requirement for CMZ’s……………………………………….1 Terminology used in this report……………………………………..2 Geologic setting…………………………………………………......4 Dungeness flooding history…………………………………………5 Data sources………………………………………………………....6 Sources of error and report limitations……………………………...7 Geomorphic reach delineation………………………………………8 CMZ delineation methods and results………………………………8 CMZ description by geomorphic reach…………………………….12 Conclusion………………………………………………………….18 Literature cited……………………………………………………...19 iii Introduction The Dungeness River flows north 30 miles and drops 3800 feet from the Olympic Mountains to the Strait of Juan de Fuca. The upper watershed south of river mile (RM) 10 lies entirely within private and state timberlands, federal national forests, and the Olympic National Park. Development is concentrated along the lower 10 miles, where the river flows through relatively steep (i.e. gradients up to 1%), glacial and glaciomarine deposits (Drost 1983, BOR 2002).