Mount Rainier National Park, Washington
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Mount Rainier National Park, WASHINGTON TEP~RJ\ ~EF's ' in Mount Rainier National Park
PUMICE AND OTHER PYROCLASTIC DEPOSITS IN Mount Rainier National Park, WASHINGTON TEP~RJ\ ~EF's ' in Mount Rainier National Park. Pumice and scoria layers from Mount Rainier volcano (note layers R, L, D, and C) typically are stained to fairly strong brown or reddish brown; interbedded lithic ash deposits have relatively neutral but somewhat darker brownish-gray colors. Ash beds from other volcanoes (note beds marked 0, set Y, set P, and WI characteristically are lighter in color than the locally derived deposits that enclose them. S1te is in an alpine meadow near Williwakas Glacier on the southeast flank of Mount Ramier . PUMICE AND OTHER PYROCLASTIC DEPOSITS IN Mount Rainier National Park, WASHINGTON By Donal R. Mullineaux 254924 GEOLOGICAL SURVEY BULLETIN 1326 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 74-600110 U.S. GOVERNMENT PRINTING OFFICE -1974 For sale by the Superintendent of· Documents, U.S. Government Printing Office, Washington, D.C. 20402- Price $1.35 (paper cover) Stock Number 2401-02550 Contents Page Abstract.................................................. 1 Introduction . 2 Previous work and acknowledgments . 4 Terminology . 6 General setting . 8 Brief description of tephra deposits . 8 Postglacial activity of Mount Rainier . 15 Eruptive history ........................ c............. 15 Volume............................................... 18 Kinds of eruptions . 18 Hazards from future eruptions of tephra . 21 Kinds of hazards . 21 Location . 22 Warning.............................................. 23 Ages of tephra layers and their use as marker beds . 23 Tephra from distant volcanoes . 27 Tephra layer 0 (Mazama ash) . 27 Distribution, thickness, and grain size . 29 Source and age . -
Itinerary: Mt. Rainier Loop
Itinerary: Mt. Rainier Loop Length: 78 miles Time to Allow: 4-5 hours Open Season: The route is usually snow-free by mid-June and remains open through late October. The road closes each year due to winter snowfall from November to early June. Driving Directions: From Packwood, travel northwest on Forest Road (FR) 52, also called Skate Creek Road, 23 miles to State Route (SR) 706. Turn right on SR 706 and travel east 41.9 miles into Mount Rainier National Park to SR 123. Turn right on SR 123 and travel south 5.4 miles to US Highway 12. Turn right on US Highway 12 and travel 7.3 miles west back to Packwood. Experience the grandeur of Mount Rainier, old-growth temperate rainforest, waterfalls, and impressive vistas! An excellent introduction to Mount Rainier National Park. Start: Begin this mountain adventure in the rural mountain community of Packwood located on Highway 12. Restaurants, car services, lodging, and campgrounds are available. Stop 1: Skate Creek Nestled deep in the forest, watch bubbling Skate Creek as you drive its namesake road. Along this winding, paved, but primitive road, see countless waterfalls cascade along the roadside. See blankets of drooping mosses and experience the beauty and serenity of this little gem. Memorable fall color displays have earned this road the honor of “Best Sunday Drive in Lewis County for Fall Color”. In the wintertime, this road is closed to vehicle traffic and the Skate Creek Sno-Park becomes a popular destination for the snowmobiling crowds. Stop 2: Nisqually Entrance Welcoming visitors to Mount Rainier National Park at the Nisqually Entrance stands a wooden entrance arch built in 1922 and reconstructed in 1973. -
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. -
Washington Geologic Newsletter
A PUBLICATION OF THE WASHINGTON STATE DIVISION OF GEOLOGY AND EARTH RESOURCES WASHINGTON GEOLOGIC NEWSLETTER JULY 1975 BERT l. COLE VOLUME 3 - NUMBER 3 COMMISSIONER Of PUBLIC LANDS DON LEE FRASER, SUPERVISOR VAUGHN E. LIVINGSTON, JR., STATE GEOLOGIST DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGY AND EARTH RESOURCES DEPARTMENT OF NATURAL RESOURCES, DIVISION Of GEOLOGY ANO EARTH RESOURCES. OLYMPIA, WASHING10N, 9850 4 INCREASED VOLCANIC ACTIVITY since the mid- l 800's. Some increases in perforo tion of the snow due to steam discharge were noted OF MOUNT BAKER1 WASHINGTON!/ in photographs taken during the period 1940-1956; On March 11, 1975, the U. S. Geological however, the present increased steam discharge prob Survey office in Tacoma, Washington received re ably represents the greatest volcanic activity on the ports of increased steam activity on Mount Boker, mountain during at least the last 84 years. a quiescent volcano located about 26 km south of Mount Baker (3,285 m) towers some l ,500 m the Canadian border in northwestern Washington. (meters) over the immediate Cascades. Possibly, sev The activity, which was first observed Morch 10, eral eruptions of Mount Baker occurred in the middle 1975, included a greatly increased emission of steam 19th century, In 1843, Mount Baker reportedly erup from a known fumarole field in Sherman Crater (on ted simultaneously with Mount St. Helens, covering the south side of the mountain about 300 meters below the Cascades with a light cover of volcanic ash. In the crest), the appearance of several new fumaroles 1854, the nearly perfect ondesi tic cone of Mount where none had been before, and a discoloration of Baker was obscured by rolling clouds of steam and gos, the steam and the snow around and in the crater. -
Federal Register / Vol
Wednesday, August 13, 2008 Part III Department of the Interior Fish and Wildlife Service 50 CFR Part 17 Endangered and Threatened Wildlife and Plants; Revised Designation of Critical Habitat for the Northern Spotted Owl; Final Rule VerDate Aug<31>2005 17:05 Aug 12, 2008 Jkt 214001 PO 00000 Frm 00001 Fmt 4717 Sfmt 4717 E:\FR\FM\13AUR2.SGM 13AUR2 rwilkins on PROD1PC63 with RULES_2 47326 Federal Register / Vol. 73, No. 157 / Wednesday, August 13, 2008 / Rules and Regulations DEPARTMENT OF THE INTERIOR Background habitat designation in the westside It is our intent to discuss only those provinces. The landscape management Fish and Wildlife Service topics directly relevant to the revised approach for the eastside provinces, designation of critical habitat in this identified in the 2008 final recovery 50 CFR Part 17 rule. For more information on the plan (USFWS 2008) and by the northern spotted owl and critical Sustainable Ecosystems Institute (SEI) [FWS-R1-ES-2008–0051; 92210-1117-0000- Scientific Panel (SEI 2008) as the most FY08-B4] habitat, please refer to the proposed rule published in the Federal Register on effective approach for managing RIN 1018-AU37 June 12, 2007 (72 FR 32450). northern spotted owl habitat in dry Prior and subsequent to the listing of forests, was not incorporated into this Endangered and Threatened Wildlife the northern spotted owl in 1990 (55 FR rule because it cannot be translated into and Plants; Revised Designation of 26114), many committees, task forces, critical habitat at this time, until the Critical Habitat for the Northern and work groups were formed to new approach called for by the recovery Spotted Owl develop conservation strategies for the plan is further defined. -
2010 CENSUS - CENSUS TRACT REFERENCE MAP: Lewis County, WA 121.217411W LEGEND Emmons Glacier
46.862203N 46.867049N 121.983702W 2010 CENSUS - CENSUS TRACT REFERENCE MAP: Lewis County, WA 121.217411W LEGEND Emmons Glacier Y P SYMBOL DESCRIPTION SYMBOL LABEL STYLE South Mowich Fryingpan Glacier A I Glacier E K R I C M Federal American Indian Puyallup Glacier E A Reservation L'ANSE RES 1880 0 Bumping Lk Ingraham Glacier 5 0 3 7 7 Off-Reservation Trust Land, Hawaiian Home Land T1880 Tahoma Glacier Oklahoma Tribal Statistical Area, Alaska Native Village Statistical Area, KAW OTSA 5340 Tribal Designated Statistical Area State American Indian W Tama Res 4125 ilson Glacier Reservation Kautz Glacier South Tahoma Glacier Nisqually Glacier Cowlitz Glacier State Designated Tribal Statistical Area Lumbee STSA 9815 Alaska Native Regional Corporation NANA ANRC 52120 State (or statistically equivalent entity) NEW YORK 36 County (or statistically Mount Rainier Natl Pk equivalent entity) ERIE 029 Minor Civil Division (MCD)1,2 Bristol town 07485 123 PIERCE 053 Consolidated City MILFORD 47500 S LEWIS 041 d R lley 1,3 Va e Incorporated Place s Davis 18100 i rad Pa Census Designated Place (CDP) 3 Incline Village 35100 ns Cany e on v e R t d S Census Tract 33.07 706 DESCRIPTION SYMBOL DESCRIPTION SYMBOL Interstate 3 Water Body Pleasant Lake W o l d 706 706 r o 2 R 2 F 1 U.S. Highway 0 e Cre d t at ek a d Swamp or Marsh Okefenokee Swamp Sk N N R R i v d sq e N u D ally Riv State Highway 4 Glacier Bering Glacier 4 Marsh Ln 4 Other Road N d D a R e t v F v or Na e R t D d F 4WD Trail, Stairway, 0 o r 1 r o 2 F Military Fort Belvoir D e t Alley, Walkway, -
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 -
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. -
Mo44*Uiscutu&I
Mo44*UIscUtu&i NATIONAL PARK I UNITED STATES Historic Events DEPARTMENT OF THE MOUNT INTERIOR 1792 Capt. George Vancouver, of the Royal OPEN British Navy, first white man to re HAROLD L. ICKES, Secretary ALL RAINIER cord sight of "The Mountain," named YEAR it Mount Rainier in honor of his NATIONAL PARK friend, Admiral Peter Rainier. WASHINGTON l9 41 1833 Dr. William Fraser Tomlie entered NATIONAL PARK SERVICE northwest corner of what is now the NEWTON B. DRURY, Director park. First white man to penetrate ADMINISTRATION BUILDING AT LONGMIRE this region. CO^TE^TS OUNT RAINIER NATIONAL with cinders and steam-shredded parti 1857 Lt. A. V. Kautz and four companions M PARK was established by act of cles, lumps of lava, and occasional flows Congress, approved by President Mc- Wild Flowers Color the Alpine made first attempt to scale Mount of liquid lava that have solidified into Kinley, March 2, 1899- A subsequent Meadows Cover Rainier but did not reach summit. layers of hard andesite rock. Judging act, January 31, 1931, extended the east "The Mountain" 3 by the steep inclination of the lava and boundary to the summit of the Cascade cinder layers visible in its flanks, it is Flowers and Forests 4 Range, the boundary recommended by thought to have once attained an alti Mount Rainier Summit Climb . 4 1870 Hazard Stevens and P. B. Van Trump the original bill. The park embraces tude of 16,000 feet. In subsequent ex Winter Sports 4 made the first successful ascent via 377.78 square miles (241,782 acres). -
MOUNTAINEERS.Orgmountaineerspring 2019 • VOLUME 113 • NO
WWW.MOUNTAINEERS.ORGMountaineerSpring 2019 • VOLUME 113 • NO. 2 EXPLORE • LEARN • CONSERVE in this issue: Three Generations Outside The Baby Peakbagger Confessions of an Old Scrambling Student tableofcontents tyingin Features The Mountaineers is a nonprofit 20 The Baby Peakbagger As CEO of The Mountaineers I have the organization, founded in 1906 Spring 2019 » Volume 113 » Number 2 Exploring Mount Rainier National Park with my daughter opportunity to attend many events across and dedicated to the responsible The Mountaineers enriches lives and communities by the organization throughout the year. One enjoyment and protection of natural areas. helping people explore, conserve, learn about, and enjoy 24 Three Generations Outside of my very favorite events is our Volunteer A love letter to my sons and granddaughters the lands and waters of the Pacific Northwest and beyond. Recognition Dinner, which takes place in EDITOR 30 Confessions of an Old Scrambling Student January. I love this event because it celebrates Peter Dunau Using mountains to take on aging the creativity, hard work, and commitment of CONTRIBUTING EDITOR our incredible volunteers. Kristina Ciari 39 A New Program Center for our Kitsap Branch DESIGNER For me, and most everyone who volunteers Opportunities abound in revamped building Sarah Kulfan, Beans n' Rice at The Mountaineers, volunteering is a way of PROOFREADERS sharing the joy of being outdoors with others. Trevor Dickie, Elaine Kelly, Hailey Oppelt Columns Tom and sons on Mt. Rainier We volunteer as an act of love for our wild CHIEF EXECUTIVE OFFICER 5 READER FEEDBACK places and out of gratitude for those who Tom Vogl introduced us to a lifetime of outdoor adventure. -
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 -
Debris Properties and Mass-Balance Impacts on Adjacent Debris-Covered Glaciers, Mount Rainier, USA
Natural Resource Ecology and Management Publications Natural Resource Ecology and Management 4-8-2019 Debris properties and mass-balance impacts on adjacent debris- covered glaciers, Mount Rainier, USA Peter L. Moore Iowa State University, [email protected] Leah I. Nelson Carleton College Theresa M. D. Groth Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/nrem_pubs Part of the Environmental Monitoring Commons, Glaciology Commons, Natural Resources Management and Policy Commons, and the Oceanography and Atmospheric Sciences and Meteorology Commons The complete bibliographic information for this item can be found at https://lib.dr.iastate.edu/ nrem_pubs/335. For information on how to cite this item, please visit http://lib.dr.iastate.edu/ howtocite.html. This Article is brought to you for free and open access by the Natural Resource Ecology and Management at Iowa State University Digital Repository. It has been accepted for inclusion in Natural Resource Ecology and Management Publications by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. Debris properties and mass-balance impacts on adjacent debris-covered glaciers, Mount Rainier, USA Abstract The north and east slopes of Mount Rainier, Washington, are host to three of the largest glaciers in the contiguous United States: Carbon Glacier, Winthrop Glacier, and Emmons Glacier. Each has an extensive blanket of supraglacial debris on its terminus, but recent work indicates that each has responded to late twentieth- and early twenty-first-century climate changes in a different way. While Carbon Glacier has thinned and retreated since 1970, Winthrop Glacier has remained steady and Emmons Glacier has thickened and advanced.