Mount Rainier Roads and Bridges
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Mount Rainier National Park
MOUNT RAINIER NATIONAL PARK • WASHINGTON • UNITED STATES DEPARTMENT OF THE INTERIOR NATIONAL PARK SERVICE Mount Rainier [WASHINGTON] National Park United States Department of the Interior Harold L. Ickes, Secretary NATIONAL PARK SERVICE Arno B. Cammerer, Director UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1936 Rules and Regulations [BRIEFED] Events kjERVING a dual purpose, park regulations are designed for the comfort and convenience of visitors as well as for the protection of natural beauties OF HISTORICAL IMPORTANCE and scenery. The following synopsis is for the guidance of visitors, who are requested to assist the park administration by observing the rules. Complete rules and regulations may be seen at the superintendent's office 1792 May 8. The first white man to sec "The Mountain" (Capt. and at ranger stations. George Vancouver, of the Royal English Navy) sighted Fires. the great peak and named it Mount Rainier. Light carefully and in designated places. Extinguish COMPLETELY before leaving 1833 September 2. Dr. William Eraser Tolmie of Nisqually camp, even for temporary absence. Do not guess your fire is out—KNOW it. Do not House, a Hudson's Bay post, entered the northwest corner throw burning tobacco or matches on road or trail sides. of what is now the park. He was the first white man to penetrate this region. Camps. Keep your camp clean. As far as possible burn garbage in camp fire, and empty 1857 July. Lieut. A. V. Kautz, of the United States Army garri son at Fort Steilacoom, and four companions made the cans and residue into garbage cans provided. If no can is provided, bury the refuse. -
An Inventory of Fish in Streams in Mount Rainier National Park 2001-2003
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science An Inventory of Fish in Streams at Mount Rainier National Park 2001-2003 Natural Resource Technical Report NPS/NCCN/NRTR—2013/717.N ON THE COVER National Park staff conducting a snorkel fish survey in Kotsuck Creek, Mount Rainier National Park, 2002. Photograph courtesy of Mount Rainier National Park. An Inventory of Fish in Streams at Mount Rainier National Park 2001-2003 Natural Resource Technical Report NPS/NCCN/NRTR—2013/717.N Barbara A. Samora, Heather Moran, Rebecca Lofgren National Park Service North Coast and Cascades Network Inventory and Monitoring Program Mount Rainier National Park Tahoma Woods Star Rt. Ashford, WA. 98304 April 2013 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Technical Report Series is used to disseminate results of scientific studies in the physical, biological, and social sciences for both the advancement of science and the achievement of the National Park Service mission. The series provides contributors with a forum for displaying comprehensive data that are often deleted from journals because of page limitations. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. -
2016 State of Our Watersheds Report Puyallup River Basin
2016 State of Our Watersheds Report Puyallup River Basin t’s the tribes that are putting the fish Iback in the waters. It’s our people do- ing that to make sure our livelihood will carry on, that our children will have this opportunity to get into a boat and go fishing so they can eat what they need. – NANCY SHIppENTOWER-GAmES PUYALLUp TRIBE OF INDIANS Puyallup Tribe of Indians The Puyallup watershed was one of the earliest areas to be settled by Euro-Americans in the Puget Sound region. Consequently, it was also one of the first watersheds in Puget Sound to experience the full impacts of indus- trial, urban and agricultural development. This development and conversion of floodplain, uplands and forestlands has completely altered the hydrologic conditions within the watershed Seattle to the detriment of salmonid production. The Puyallup are fishing people. They lived on food provided by the fisheries since time immemori- al. It was not until after the U.S. v. Washington court decision that they were able to exercise their rights to the fishery. Puyallup Tribe of Indians 163 History of the Puyallup River Basin The Puyallup River basin, WRIA 10, includes the White, Puyallup and Car- bon rivers, which have their origins in the glaciers of the northwestern slopes of Mount Rainier. The Puyallup River flows to Commencement Bay at the Port of Tacoma, the third largest port in the western United States. The Puyallup Basin has been substantially altered from its historic condition and is currently contained within a revetment and levee system throughout its lower 26 miles. -
The Recession of Glaciers in Mount Rainier National Park, Washington
THE RECESSION OF GLACIERS IN MOUNT RAINIER NATIONAL PARK, WASHINGTON C. FRANK BROCKMAN Mount Rainier National Park FOREWORD One of the most outstanding features of interest in Mount Rainier National Park is the extensive glacier system which lies, almost entirely, upon the broad flanks of Mount Rainier, the summit of which is 14,408 feet above sea-level. This glacier system, numbering 28 glaciers and aggregating approximately 40-45 square miles of ice, is recognized as the most extensive single peak glacier system in continental United States.' Recession data taken annually over a period of years at the termini of six representative glaciers of varying type and size which are located on different sides of Mount Rainier are indicative of the rela- tive rate of retreat of the entire glacier system here. At the present time the glaciers included in this study are retreating at an average rate of from 22.1 to 70.4 feet per year.2 HISTORY OF INVESTIGATIONS CONDUCTED ON THE GLACIERS OF MOUNT RAINIER Previous to 1900 glacial investigation in this area was combined with general geological reconnaissance surveys on the part of the United States Geological Survey. Thus, the activities of S. F. Em- mons and A. D. Wilson, of the Fortieth Parallel Corps, under Clarence King, was productive of a brief publication dealing in part with the glaciers of Mount Rainier.3 Twenty-six years later, in 1896, another United States Geological Survey party, which included Bailey Willis, I. C. Russell, and George Otis Smith, made additional SCircular of General Information, Mount Rainier National Park (U.S. -
Chambers Creek
Section 3 - Physical and Environmental Inventory 3.1 Chambers Creek – Clover Creek Drainage Basin 3.2 Puyallup River Drainage Basin 3.3 Sewer Service Basins in the Puyallup and White River Drainage Basins 3.4 Nisqually River Drainage Basin 3.5 Kitsap Drainage Basin 3.6 City of Tacoma - North End WWTP 3.7 Joint Base Lewis Mcchord Sewer System – Tatsolo Point WWTP Pierce County Public Works and Utilities – Sewer Utility Unified Sewer Plan Update Section 3 Section 3 – Physical and Environmental Inventory Section 3 documents the land-use and environmental tenants of the four major basins in Pierce County and are organized around those basins. Chambers Creek – Clover Creek Drainage Basin - Section 3.1 Puyallup River Drainage Basin – Section 3.2 Nisqually River Drainage Basin – Section 3.4 Kitsap Drainage Basin – Section 3.5 3.1 Chambers Creek – Clover Creek Drainage Basin The Chambers Creek - Clover Creek Drainage Basin (Basin) is located in central Pierce County, between Puget Sound on the west and the ridge above the Puyallup River Valley on the east. Point Defiance and the southwest shore of Commencement Bay serve as the basin’s northern boundary, and the City of DuPont lies on the southern boundary. The basin encompasses approximately 104,258 acres (117 square miles) of land including the Cities of DuPont, including Northwest Landing, University Place, Lakewood, and Northwest Tacoma, Fircrest, the Towns of Ruston, and Steilacoom, as well as portions of Fort Lewis and McChord Military Reservations, and the unincorporated communities of South Hill, Frederickson, Mid County, Graham, Parkland, and Spanaway. 3.1.1 Topography Lowland topography is generally flat to gently rolling. -
Shriner Peak Fire Lookout 03/13/1991
6/B2 National Park Service Westin Buildingding, 0^^920 I Aveni^^ WRO Pacific Northwest Region 2001 Sixth 1 SITE I D. NO INVENTORY Cultural Resources Division Seattle, Washington 98121 2 NAME(S) OF STRUCTURE (CARD 1 of 2) 5. ORIGINAL USE 7. CLASSIFICATION Shriner Peak Fire Lookout Fire Lookout 1932 3 SITE ADDRESS (STREET A NO) 6. PRESENT USE Fire Lookout Shriner Peak 0-052 and BackcounTi EASTING try Assistance COUNTY STATE SCALE 4 CITY/VICINITY 1 24 QUAD Ohanapecosh Lewis Washington OTHER , .NAME. 12 OWNER/AOMIN ADDRESS NPS/Mount Rainier National Park, Tahonia Woods-Star Route^ Ashford, WA., 98304 n ni r;rMiiMK)N and nACKr'.nnuNf) iiiruonv includini; crjN.-.mufuioN daims), mvsicAi oiMt nsions. maifmiai s, ma.kir ai ifraiions. fxiant f.ouipmfni. and IMPOniANI DUILDEHS. AMCMirFCrS. ENOINEERS. EIC Timber frame, two-story, square plan; hip roof, cedar shingles, projecting eaves; wrap around balcony, fixed sashes, rough lapped (Douglas Fir) exterior siding; wood floors, tongue-and-groove interior walls and ceilings; concrete foundation. In 1931 Superintendent O.A. Tomlinson reported that three fire lookouts were being manned by park personnel; Colonnades, Anvil Rock and Shriner Peak. Althdugh it is not known what kind of lookout existed then on Shrlner Peak, in 1932 a private contractor (engaged in road construction on the East Side Road) erected a new timber frame lookout. Measuring 14' X 14', it was built according to a standard design drafted by the National Park Service, Landscape Division (Branch of Plans and Design) in 1932. Thomas E. Carpenter, Landscape Architect recommended the design. Typically, the ground floor was used for storage and the one-room upper floor contained the fire finder, charts, supplies, a bed and cooking facilities. -
Carbon River Access Management Plan
United States Department of the Interior FISH AND WILDLIFE SERVICE Washington Fish and Wildlife Office 510 Desmond Dr. SE, Suite 102 Lacey, Washington 98 503 APR 2 6 20ll In Reply Refer To: 13410-2010-F-0488 Memorandum To: Superintendent, Mount Rainier National Park Ashford, Washington From: Manager, Washington Fish and Wildlife Lacey, Washington Subject: Biological Opinion for the Carbon River Access Management Plan This document transmits the Fish and Wildlife Service's Biological Opinion based on our review of the proposed Carbon River Access Managernent Plan to be implemented in Mount Rainier National Park, Pierce County, Washington. We evaluated effects on the threatened northern spotted owl (Sfrlx occidentalis caurina),marbled murrelet (Brachyramphus marmoratus),bttll trout (Salvelinus confluentus), and designated bull trout critical habitat in accordance with section 7 of the Endangered Species Act (Act) of 1973, as amended (16 U.S.C. 1531 et seq.). Your July 29,2010 request for formal consultation was received on August 2,2010. This Biological Opinion is based on information provided in the June 28, 2010 Biological Assessment and on other information and correspondence shared between our respective staff. Copies of all correspondence regarding this consultation are on file at the Washington Fish and Wildlife Office in Lacey, Washington. If you have any questions about this mernorandum, the attached Biological Opinion, or your responsibilities under the Act, please contact Vince Harke at (360) 753-9529 or Carolyn Scafidi at (360) 753-4068. Endangered Species Act - Section 7 Consultation BIOLOGICAL OPINION U.S. Fish and Wildlife Service Reference: 13410-2010-F-0488 Carbon River Access Management Plan Mount Rainier National Park Pierce County, Washington Agency: National Park Service Consultation Conducted By: U.S. -
Mount Rainier National Park, Washington
NATIONAL PARK . WASHINGTON MOUNT RAINIER WASHINGTON CONTENTS "The Mountain" 1 Wealth of Gorgeous Flowers 3 The Forests 5 How To Reach the Park 8 By Automobile 8 By Railroad and Bus 11 By Airplane 11 Administration 11 Free Public Campgrounds 11 Post Offices 12 Communication and Express Service 12 Medical Service 12 Gasoline Service 12 What To Wear 12 Trails 13 Fishing 13 Mount Rainier Summit Climb 13 Accommodations and Expenses 15 Summer Season 18 Winter Season 18 Ohanapecosh Hot Springs 20 Horseback Trips and Guide Service 20 Transportation 21 Tables of Distances 23 Principal Points of Interest 28 References 32 Rules and Regulations 33 Events of Historical Importance 34 Government Publications 35 UNITED STATES DEPARTMENT OF THE INTERIOR • Harold L. Ickes, Secretary NATIONAL PARK SERVICE Arno B. Cammerer, Director UNITED STATES GOVERNMENT PRINTING OFFICE • 1938 AN ALL-YEAR PARK Museums.—The park museum, headquarters for educational activities, MOUNT RAINIER NATIONAL PARK may be fully enjoyed throughout the and office of the park naturalist are located in the museum building at year. The summer season extends from early June to early November; the Longmire. Natural history displays and wild flower exhibits are main winter ski season, from late November well into May. All-year roads make tained at Paradise Community House, Yakima Park Blockhouse, and the park always accessible. Longmire Museum. Nisquaiiy Road is open to Paradise Valley throughout the year. During Hikes from Longmire.—Free hikes, requiring 1 day for the round trip the winter months this road is open to general traffic to Narada Falls, 1.5 are conducted by ranger naturalists from the museum to Van Trump Park, miles by trail from Paradise Valley. -
Kampmeier & Knutsen Pllc
KAMPMEIER & KNUTSEN PLLC ATTORNEYS AT LAW PAUL A. KAMPMEIER Licensed in Washington 206.858.6983 [email protected] October 28, 2020 Via Certified Mail – Return Receipt Requested Managing Agent Electron Hydro, LLC 1800 James Street, Suite 201 Bellingham, Washington 98225-4631 Managing Agent Electron Hydro, LLC 29711 Kapowsin-Electron Reservoir Road Orting, Washington 98360 Managing Agent Electron Holdings, Inc. 1800 James Street, Suite 201 Bellingham, Washington 98225 Managing Agent Electron Management LLC 1800 James Street, Suite 201 Bellingham, Washington 98225-4631 Managing Agent Tollhouse Energy Company 1800 James Street, Suite 201 Bellingham, Washington 98225 Re: Notice of Intent to File Suit under the Clean Water Act and the Resource Conservation and Recovery Act and Request for SWPPP and Site Log Book. Dear Managing Agents: This letter provides Electron Hydro, LLC, Electron Holdings, Inc., Electron Management LLC, and Tollhouse Energy Company (hereinafter referred to collectively as “Electron”) with sixty days’ notice of Citizens for a Healthy Bay’s and Puget Soundkeeper Alliance’s intent to file a citizen lawsuit against Electron under Section 505 of the Clean Water Act, 33 U.S.C. §1365, for the Clean Water Act (“CWA”) violations alleged and described in this letter. This letter also notifies Electron that after the required notice period Citizens for a Healthy Bay and Puget Soundkeeper Alliance (the “Conservation Groups”) intend to sue Electron under 42 U.S.C. § 6972 for alleged violations of the Resource Conservation and Recovery Act (“RCRA”). The Conservation Groups are non-profit organizations dedicated to protecting the natural environment of Puget Sound and its tributaries. Kampmeier & Knutsen, PLLC represent Citizens for a Healthy Bay and Puget Soundkeeper Alliance in this matter, and any response to this notice of intent to sue should be directed to Paul Kampmeier at Kampmeier & Knutsen PLLC at the address below. -
Volcanic Hazards • Washington State Is Home to Five Active Volcanoes Located in the Cascade Range, East of Seattle: Mt
CITY OF SEATTLE CEMP – SHIVA GEOLOGIC HAZARDS Volcanic Hazards • Washington State is home to five active volcanoes located in the Cascade Range, east of Seattle: Mt. Baker, Glacier Peak, Mt. Rainier, Mt. Adams and Mt. St. Helens (see figure [Cascades volcanoes]). Washington and California are the only states in the lower 48 to experience a major volcanic eruption in the past 150 years. • Major hazards caused by eruptions are blast, pyroclastic flows, lahars, post-lahar sedimentation, and ashfall. Seattle is too far from any volcanoes to receive damage from blast and pyroclastic flows. o Ash falls could reach Seattle from any of the Cascades volcanoes, but prevailing weather patterns would typically blow ash away from Seattle, to the east side of the state. However, to underscore this uncertainty, ash deposits from multiple pre-historic eruptions have been found in Seattle, including Glacier Peak (less than 1 inch) and Mt. Mazama/Crater Lake (amount unknown) ash. o The City of Seattle depends on power, water, and transportation resources located in the Cascades and Eastern Washington where ash is more likely to fall. Seattle City Light operates dams directly east of Mt. Baker and in Pend Oreille County in eastern Washington. Seattle’s water comes from two reservoirs located on the western slopes of the Central Cascades, so they are outside the probable path of ashfall. o If heavy ash were to fall over Seattle it would create health problems, paralyze the transportation system, destroy many mechanical objects, endanger the utility networks and cost millions of dollars to clean up. Ash can be very dangerous to aviation. -
FACT SHEET White River Management Agreement and Related Settlement Agreements Between Cascade Water Alliance and the Muckleshoot and Puyallup Tribes
FACT SHEET White River Management Agreement and Related Settlement Agreements between Cascade Water Alliance and the Muckleshoot and Puyallup Tribes The Cascade Water Alliance, the Muckleshoot Indian Tribe, and the Puyallup Tribe of Indians have entered into a set of agreements that will facilitate the development of Lake Tapps as a new source of municipal water supply while protecting and enhancing fishery resources in the White and Puyallup River Basins. The agreements also establish targets for Lake Tapps water levels designed to accommodate continued recreational use of the Reservoir. Information on Cascade and the two Tribes, together with a summary of some of the more important aspects of the agreements follows: Cascade Water Alliance The Cascade Water Alliance is an association of cities and water districts working together to ensure a clean, safe and reliable water supply today and well into the future. Members are the cities of Bellevue, Issaquah, Kirkland, Redmond, and Tukwila, the Covington Water District, and the Sammamish Plateau and Skyway Water and Sewer Districts. Today Cascade supplies over 350,000 residents and 22,000 businesses. Muckleshoot Indian Tribe The Muckleshoot Indian Tribe is a federally recognized Indian Tribe governing the Muckleshoot Indian Reservation. The White River flows through the Muckleshoot Reservation which is located downstream of the Buckley Diversion Dam. Muckleshoot is a successor in interest to tribes and bands that were parties to the Treaties of Point Elliot and Medicine Creek and possesses treaty reserved fishing rights on the White River and Upper Puyallup. Puyallup Tribe of Indians The Puyallup Tribe of Indians is a federally recognized Indian Tribe governing the Puyallup Reservation. -
1 New Chronologic and Geomorphic Analyses of Debris Flows on Mount
New Chronologic and Geomorphic Analyses of Debris Flows on Mount Rainier, Washington By Ian Delaney Abstract Debris flows on Mount Rainier are thought to be increasing in frequency and magnitude in recent years, possibly due to retreating glaciers. These debris flows are caused by precipitation events or glacial outburst floods. Furthermore, as glaciers recede they leave steep unstable slopes of till providing the material needed for mass-wasting events. Little is known about the more distant history and downstream effects of these events. Field observations and/or aerial photograph of the Carbon River, Tahoma Creek, and White River drainages provide evidence of historic debris flow activity. The width and gradient of the channel on reaches of streams affected by debris flows is compared with reaches not affected by debris flows. In all reaches with field evidence of debris flows the average channel width is greater than in places not directly affected by debris flows. Furthermore, trends in width relate to the condition of the glacier. The stable Carbon Glacier with lots of drift at the terminus feeds the Carbon River, which has a gentle gradient and whose width remains relatively consistent over the period from 1952 to 2006. Conversely, the rapidly retreating Tahoma and South Tahoma Glaciers have lots of stagnant ice and feed the steep Tahoma Creek. Tahoma Creek’s width greatly increased, especially in the zone affect by debris flow activity. The rock-covered, yet relatively stable Emmons Glacier feeds White River, which shows relatively