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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. -
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. -
Tahoma News Summer 2007
November 2006 Flood Makes History The flood of November 6 and 7, 2006 was an previous records. Record amounts fell throughout up here, washing it away there changing course, historical, natural event unlike any other that has other regions of the park. seeking the easiest path through the debris. This been recorded in Mount Rainier National Park’s is why glacial riverbeds are wide and rocky, with 108 year history. The snow levels during the storm stayed above the river itself braided into constantly changing 10,000 feet in elevation, with the majority of the channels. Long before National Park status, debris flows precipitation falling as rain. Some existing snow traveled from Mount Rainier to the Puget Sound. above 7,000 feet melted, adding to the runoff in the Recent research at Mount Rainier National Park Areas near Tacoma and Seattle are formed of rivers. has measured aggradation in most park rivers prehistoric debris from the mountain. to occur at a rate of 6 to 14 inches per decade. As the rain flowed down mountain-sides and In comparison, during the November flood, the In more recent park history (1946-47), a series roads to the main watersheds, it caused extreme riverbed where Tahoma Creek flows under the of heavy snowstorms caused extreme damage to soil erosion and slides. It uprooted large areas of Nisqually Road rose more than four feet. facilities. For two weeks, the main entrance to the trees that eventually caused log jams that redirected park was closed to the public due to the danger of water. -
1967, Al and Frances Randall and Ramona Hammerly
The Mountaineer I L � I The Mountaineer 1968 Cover photo: Mt. Baker from Table Mt. Bob and Ira Spring Entered as second-class matter, April 8, 1922, at Post Office, Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during March and April by The Mountaineers, P.O. Box 122, Seattle, Washington, 98111. Clubroom is at 719Y2 Pike Street, Seattle. Subscription price monthly Bulletin and Annual, $5.00 per year. The Mountaineers To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanent form the history and traditions of this region; To preserve by the encouragement of protective legislation or otherwise the natural beauty of North west America; To make expeditions into these regions m fulfill ment of the above purposes; To encourage a spirit of good fellowship among all lovers of outdoor life. EDITORIAL STAFF Betty Manning, Editor, Geraldine Chybinski, Margaret Fickeisen, Kay Oelhizer, Alice Thorn Material and photographs should be submitted to The Mountaineers, P.O. Box 122, Seattle, Washington 98111, before November 1, 1968, for consideration. Photographs must be 5x7 glossy prints, bearing caption and photographer's name on back. The Mountaineer Climbing Code A climbing party of three is the minimum, unless adequate support is available who have knowledge that the climb is in progress. On crevassed glaciers, two rope teams are recommended. Carry at all times the clothing, food and equipment necessary. Rope up on all exposed places and for all glacier travel. Keep the party together, and obey the leader or majority rule. Never climb beyond your ability and knowledge. -
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 -
UNIVERSITY of CALIFORNIA Los Angeles Development Of
UNIVERSITY OF CALIFORNIA Los Angeles Development of baddeleyite as a chronometer for recent silica-undersaturated lavas A thesis submitted in satisfaction of the requirements for the degree Master of Science in Geochemistry by Wan Ning Wu 2014 ABSTRACT OF THESIS Development of baddeleyite as a chronometer for recent silica-undersaturated lavas by Wan Ning Wu Master of Science in Geochemistry University of California, Los Angeles, 2014 Professor Axel K. Schmitt, Chair Baddeleyite is a frequently found accessory mineral in silica-undersaturated lavas. Because it is typically enriched in uranium, while having low initial lead, baddeleyite has long been a prime target for U-Pb geochronology for mafic rocks. The difficulties in retrieving small baddeleyite grains from volcanic samples and the lack of a detailed understanding of baddeleyite occurrence, however, have limited baddeleyite chronology largely to coarse-grained mafic intrusive rocks. In this thesis, the development of U-Th in-situ baddeleyite analysis using Secondary Ionization Mass Spectrometry (SIMS) is presented together with an assessment of baddeleyite occurrence in Quaternary silica- undersaturated lavas. Samples studied include the Cathedral Crag and Burroughs Mountain lava flows of Cascade arc volcanoes Mt. Baker and Mt. Rainier (Washington, USA), respectively, and Accademia, Punta Marmolite and Cuma lava domes of the Campi Flegrei caldera (Naples, Italy). Baddeleyite crystals were initially identified in cut and polished rock billets using scanning electron microscope (SEM) backscatter imaging and energy dispersive x-ray analysis, before they were separated by diamond-drilling for ii SIMS analysis. A total of 62 and 52 baddeleyite crystals were documented from Cathedral and Burroughs Mountain lava flows; 205, 42 and 15 baddeleyite crystals were documented from Accademia, Punta Marmolite and Cuma lava domes, respectively. -
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. -
7/' / 7? Title: Composition, Distribution and Succession of Subal Ne Meadows In
AN ABSTRACT OF THE THESIS OF Jan Alan Henderson for theDoctor of Philosophy inPlant Ecology (Botany) presented on 9 7/' / 7? Title: Composition, Distribution and Succession of Subal ne Meadows in Mount Rainier National Park Abstract approved: --' Dr. W. W. Chilcote In 1970 a phytoscxiological reconnaissance consisting of 135 plots in the Subalpine Meadow Zone was made. These samples were sorted using an association table and several Alpine Zone and very early seral communities were set aside, An additional hundred plots taken by M. 3. Hamann were incorporated with these and compiled in another association table and com- bined in a two-dimensional ordination.This analysis yielded 18 major and 16 minor described community types which were clustered into five vegetation types. A key to the vegetation and community types is also presented. Soil moisture and temperature data were taken during 1971 and 1972 and are used to help characterize selected important communities. Soil moistures did not drop much during either season, although differences between corn- munities are apparent. The difference in temperatures (of the top 2 cm of soil) of the same selected communities were more striking. The Festuca domi- nated communities experienced soil temperatures over350C, while maximum temperatures in other communities rarely ranged over 20 C Low mght- time temperatures were relatively similar from conimumty to commumty, ranging from near freezing to about + 5° C. Several successional patterns were uncovered. In general the com- munities in the Low-Herbaceous Vegetation Type are early seral and are replaced by members of the Wet-Sedge, Lush-Herbaceous and the Dry-Grass Vegetation Types. -
1934 the MOUNTAINEERS Incorpora.Ted T�E MOUNTAINEER VOLUME TWENTY-SEVEN Number One
THE MOUNTAINEER VOLUME TWENTY -SEVEN Nom1-0ae Deceml.er, 19.34 GOING TO GLACIER PUBLISHED BY THE MOUNTAIN�ER.S INCOaPOllATBD SEATTLI: WASHINGTON. _,. Copyright 1934 THE MOUNTAINEERS Incorpora.ted T�e MOUNTAINEER VOLUME TWENTY-SEVEN Number One December, 1934 GOING TO GLACIER 7 •Organized 1906 Incorporated 1913 EDITORIAL BOARD, 1934 Phyllis Young Katharine A. Anderson C. F. Todd Marjorie Gregg Arthur R. Winder Subscription Price, $2.00 a Year Annual (only) Seventy-five Cents Published by THE MOUNTAINEERS Incorporated Seattle, Washington Entered as second class matter, December 15, 1920, at the Postofflce at Seattle, Washington, under the Act of March 3, 1879. TABLE OF CONTENTS Greeting ........................................................................Henr y S. Han, Jr. North Face of Mount Rainier ................................................ Wolf Baiter 3 r Going to Glacier, Illustrated ............... -.................... .Har iet K. Walker 6 Members of the 1934 Summer Outing........................................................ 8 The Lake Chelan Region ............. .N. W. <J1·igg and Arthiir R. Winder 11 Map and Illustration The Climb of Foraker, Illitstrated.................................... <J. S. Houston 17 Ascent of Spire Peak ............................................... -.. .Kenneth Chapman 18 Paradise to White River Camp on Skis .......................... Otto P. Strizek 20 Glacier Recession Studies ................................................H. Strandberg 22 The Mounta,ineer Climbers................................................ -
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).