Chapter 7.2: Existing Trails
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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. -
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 -
Puyallup Historic Survey Report Puyallup, Washington For
Puyallup Historic Survey Report Puyallup, Washington for The City of Puyallup, Pierce County, & the Washington State Department of Archaeology and Historic Preservation BOLA Architecture + Planning Seattle August 2007 Historic Survey Report Puyallup, Washington August 2007 CONTENTS 1. Introduction 1 Background Project Goals Project Schedule and Survey Methods The Survey Area Property Selection Criteria Acknowledgements Survey Grant Sponsorship 2. Historic Context Statement 7 Natural Setting First Peoples and Early Settlement Founding of the City Early Puyallup – An Agricultural Market Town Impact of Transportation – Railroads, the Interurban, and Road and Highway Systems The 1949 and 1965 Earthquakes Population Increases and Demographics Post-War Suburban Growth and Annexations The City’s Downtown Business Community Civic and Institutional Structures 3. Analysis 28 Determinants of Physical Form and Urban Design Features Building Types, Materials, and Architectural Styles 4. Survey Results 31 Findings The Survey List 5. Recommendations 39 City of Puyallup Preservation Goals and Policies The Next Step in Preservation 6. Bibliography and Sources 44 Appendices: "Historic Resource Survey Areas" and "Inventoried Properties" Maps Cover photo from the Ezra Meeker Historical Society, Puyallup, Washington. BOLA Architecture + Planning 320 Terry Avenue North Seattle, Washington 98109 206.447.4749 PUYALLUP HISTORIC SURVEY REPORT 1. Introduction Background Puyallup is one of Washington State’s oldest cities, and it contains a significant number of historic properties that reflect its origin as an agricultural settlement dating from the 1850s. Located eight miles east of Tacoma and Commencement Bay, the town was founded on the south side of the Puyallup River in the late 1870s, and its urban environment represents nearly 140 years of development. -
Page 85 TITLE 16—CONSERVATION § 110C Main Fork of Ohanapecosh
Page 85 TITLE 16—CONSERVATION § 110c main fork of Ohanapecosh River to the quarter and one-half acres, as generally depicted on the section line of section 9, township 14 north, map entitled ‘‘Mount Rainier National Park range 10 east, Willamette meridian; thence west- Proposed 1987 Boundary Adjustments’’, num- erly along the quarter section line of sections 9, bered 105–80,010B and dated January 1987, which 8, and 7 to the west boundary of said township; shall be on file and available for public inspec- thence due west to the right or west bank of tion in the Washington office of the National Muddy Fork of the Cowlitz River; thence north- Park Service, United States Department of the erly along the right bank of said Muddy Fork to Interior and at Mount Rainier National Park. a point exactly due east of post numbered 34 on (b) Forest boundary adjustment the south boundary of Mount Rainier National The boundaries of the Snoqualmie National Park as surveyed in 1908; thence due west to said Forest and of the Gifford Pinchot National For- post numbered 34; thence along the boundary of est, are hereby revised to include in the Sno- said park as surveyed in 1908 to post numbered qualmie National Forest approximately thirty- 35; thence easterly along the south boundary of one and one-half acres, to exclude from the Sno- said national park as surveyed in 1908 to the qualmie National Forest approximately thirty southeast corner thereof; thence northerly along acres, and to exclude from the Gifford Pinchot the east boundary of said national park as sur- National Forest approximately two hundred and veyed in 1908 to post numbered 59; thence along ten acres, as generally depicted on a map enti- the east boundary of said park as revised by sec- tled ‘‘Mount Rainier National Park Proposed tion 107 of this title, northerly to the point of 1987 Boundary Adjustments’’, numbered beginning. -
1912 the Mountaineers
The Mountaineer. Volume Five Nineteen Hundred Twelve h611, •• , ,, The Mountaineen Sea11le. Wa1hla1100 :J1'.)1'1zec1 bv G oog I e 2,-�a""" ...._� _..,..i..c.. tyJ Vi) Copyright 1912 The Mountaineers Din,tiZ<'d by Google CONTENTS Page Greeting ................... ................................John Muir .......................................... Greeting ..................................................... Enos Mills ........................................ The Higher Functions of a Mountain Club................................................... \ Wm. Frederic Bade.......................... 9 Little Tahoma ............ ............................. .Edmond S. Meany............................ 13 Mountaineer Outing of 1912 on north side of Mt. Rainier....................... Mary Paschall ................................... 14 Itinerary of Outing of 1912................... .Charles S. Gleason........................... 26 The Ascent of Mt. Rainier.................... £. M.Hack ........................................ 28 Grand Park .............................................. 1=dmond S. Meany............................ 36 A New Route up Mt. Rainier.............. 'Jara Keen ........................................ 37 Naches Pass .............................................. Edmond S. Meany....... ,.................... 40 Undescribed Glaciers of Mt. Rainier .. Fran,ois Matthes ............................. 42 Thermal Caves ....................................... J. B. Flett .......................................... 58 Change in Willis -
2020 Wild Coho Forecasts for Puget Sound, Washington Coast, and Lower Columbia Washington Department of Fish & Wildlife Science Division, Fish Program by Marisa N
2020 Wild Coho Forecasts for Puget Sound, Washington Coast, and Lower Columbia Washington Department of Fish & Wildlife Science Division, Fish Program by Marisa N. C. Litz Contributors: This coho forecast was made possible through funding from numerous federal, state, and local sources and the participation of numerous WDFW, tribal, and PUD biologists. The following WDFW employees, listed in alphabetical order, provided field data used in the 2020 forecast: Kale Bentley and Brad Garner (Grays River), Clayton Kinsel (Skagit River and Big Beef Creek), Matt Klungle (Nisqually River), Jamie Lamperth (Mill, Abernathy, and Germany creeks), Peter Lisi (Lake Washington), John Serl (Cowlitz Falls), Pete Topping (Green River and Deschutes River), and Devin West (Bingham Creek, Chehalis River). Sources of smolt data from tribal and PUD biologists and sources of freshwater and marine environmental indicators are cited in the document. Thank you to Skip Albertson for compiling data from the WA Department of Ecology Marine Water Monitoring Program. Mara Zimmerman, Neala Kendall, Dan Rawding, and Josh Weinheimer most recently completed these forecasts and provided much guidance and assistance on this one. Dave Seiler, Greg Volkhardt, Dan Rawding, Mara Zimmerman, and Thomas Buehrens have contributed to the conceptual approaches used in this forecast. Introduction Run size forecasts for wild coho stocks are an important part of the pre-season planning process for Washington State salmon fisheries. Accurate forecasts are needed at the scale of management units to ensure adequate spawning escapements, realize harvest benefits, and achieve harvest allocation goals. Wild coho run sizes (adult ocean recruits) have been predicted using various approaches across Washington’s coho producing systems. -
CARBON RIVER ROAD Mount Rainier National Park Between
CARBON RIVER ROAD HAER No. WA-120 Mount Rainier National Park Between Carbon River Entrance and Ipsut Creek Longmire Vicinity Pierce County Washington I- y EHOTOCinAFH&- WRITTEN HISTORICAL AND DESCRIPTIVE DATA HISTORIC AMERICAN ENGINEERING RECORD National Park Service U.S. Department of the Interior P.O. Box 37127 Washington, D.C. 20013-7127 HISTORIC AMERICAN ENGINEERING RECORD CARBON RIVER ROAD Mount Rainier National Park HAER WA-120 37- UM6-\J I. INTRODUCTION Location: Between Carbon River Entrance and Ipsut Creek Campground, Mount Rainier National Park, Pierce County, Washington. Quads: Golden Lakes, Wash. Mowich Lake, Wash. UTMs: West End: Carbon River Entrance 10/582600/5204990 East End: Ipsut Creek 10/589000/5203050 Date of Construction: 1921 Owner: Mount Rainier National Park, National Park Service Use: Park road Significance: The second road built in Mount Rainier National Park, this 5-mile unpaved road provides access to the remote northwest corner of the park. In the late 1920s, plans were made to connect the road with the planned West Side Highway but these were never realized. Project Information: Documentation of the Carbon River Road is part of the Mount Rainier National Park Roads and Bridges Recording Project, conducted in summer 1992 by the Historic American Engineering Record. Richard H. Quin, Historian, 1992 CARBON RIVER ROAD HAER No. WA-120 (page 2) II. HISTORY This is one in a series of reports prepared for the Mount Rainier National Park Roads and Bridges Recording Project. HAER No. WA-35, MOUNT RAINIER NATIONAL PARK ROADS AND BRIDGES, contains an overview history of the park roads. Carbon River Road The Carbon River Road in the northwest corner of Mount Rainier National Park provides access to a remote corner of the park.