Mount Rainier National Park Mountaineering Report – 2005
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Outline for Thesis
THESIS APPROVAL The abstract and thesis of Thomas H. Nylen for the Master of Science in Geology presented October 25, 2001, and accepted by the thesis committee and the department. COMMITTEE APPROVALS: _______________________________________ Andrew G. Fountain, Chair _______________________________________ Scott F. Burns _______________________________________ Christina L. Hulbe _______________________________________ Keith S. Hadley Representative of the Office of Graduate Studies DEPARTMENTAL APPROVAL: _______________________________________ Michael L. Cummings, Chair Department of Geology ABSTRACT An abstract of the thesis of Thomas H. Nylen for the Master of Science in Geology presented October 25, 2001. Title: Spatial and Temporal Variations of Glaciers (1913-1994) on Mt. Rainier and the Relation with Climate Databases have been constructed for the purpose of studying glacier changes at Mt. Rainier. Glacier cover on Mt. Rainier decreased 18.5% (112.3 km2 to 88.1 km2) between 1913 and 1971 at a rate of about -0.36 km2 a-1. The total area in 1994 was 87.4 km2, which equates to a rate of -0.03 km2 a-1 since 1971. Glaciers with southerly aspect lost significantly more area than those with a northerly aspect, 26.5% and 17.5% of the total area, respectively. Measured and estimated total volumes for Mt. Rainier glaciers also decreased. From 1913 to 1971 the total volume decreased 22.7% from 5.62 km3 to 4.34 km3 and from 1971 to 1994 decreased 3.1% to 4.21 km3. Nisqually Glacier shows three cycles of retreat and advance but an overall loss of 0.44 km2 since 1931. Cross-correlation with snowfall suggests about a decade response time for the glaciers. -
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. -
Evidence of a Changing Climate Impacting the Fluvial Geomorphology of the Kautz Creek on Mt
EVIDENCE OF A CHANGING CLIMATE IMPACTING THE FLUVIAL GEOMORPHOLOGY OF THE KAUTZ CREEK ON MT. RAINIER by Melanie R. Graeff A Thesis Submitted in partial fulfillment of the requirements for the degree Master of Environmental Studies The Evergreen State College June, 2017 ©2017 by Melanie R. Graeff. All rights reserved. This Thesis for the Master of Environmental Studies Degree by Melanie R. Graeff has been approved for The Evergreen State College by ________________________ Michael Ruth, M.Sc Member of the Faculty ________________________ Date ABSTRACT Evidence of a Changing Climate Impacting the Fluvial Geomorphology of the Kautz Creek on Mt. Rainier Melanie Graeff Carbon dioxide emissions have stimulated the warming of air and ocean temperatures worldwide. These conditions have fueled the intensity of El Nino-Southern Oscillation and Atmospheric River events by supplying increased water vapor into the atmosphere. These precipitation events have impacted the fluvial geomorphology of a creek on the southwestern flank of the Kautz Creek on Mt. Rainier, Washington. Using GIS software was the primary means of obtaining data due to the lack of publications published on the Kautz Creek. Time periods of study were set up from a 2012 publication written by Jonathan Czuba and others, that mentioned observations of the creek that dated from 1960 to 2008. In combining those observations of the Kautz and weather data from the weather station in Longmire, Washington, this allowed for a further understanding of how climate change has affected the fluvial geomorphology of the Kautz Creek over time. GIS software mapping showed numerous changes on the creek since 2008. -
1 Trip Report; Mt. Rainier Via Kautz Glacier. on July 25 , 2010, Mick
Trip report; Mt. Rainier via Kautz Glacier. On July 25th, 2010, Mick Pearson, Nasa Koski and I began a three-day trip up Mt. Rainier, which included an ascent up the Nisqually, Wilson and Kautz Glaciers, and then a descent via the traditional, Disappointment Cleaver (DC) Route. During my eleven year mountaineering “career”, I never had the urge to climb Mt. Rainier, mostly because of trip reports that spoke of endless ropes of climbers ascending (read: clogging) the traditional route. I had experienced such crowds on Mt. Shasta in California and on the Nadelhorn in Switzerland and simply had no desire to be a part of another endless train of climbers up a mountain. My interests changed during a flight to the Northwest in 2008. I was visiting Seattle on my way to Mt. Baker when I caught a glimpse of Mt. Rainier from about 15,000 feet from the jet’s window. Although I was well aware of the often crowded situation on Rainier, the view of the mountain was fascinating and initiated thoughts of potentially ascending a less popular route, one with far fewer climbers and more challenge than the traditional route. In spring of 2010, I contacted Mick Pearson of Kaf Adventures, to inquire about the possibility of climbing Mt. Rainier together. Mick is an accomplished mountain/rock guide with experiences on many of the world’s famous mountain ranges. More importantly, he also was willing to establish a climbing partnership that included as much education and willingness to teach as it did desire to touch the top. -
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................................................ -
What Can We Learn from Mount Rainier Meltwater? Claire Todd Pacific Lutheran University
What can we learn from Mount Rainier meltwater? Claire Todd Pacific Lutheran University Emmons Glacier, White River What can we learn from Mount Rainier meltwater? Claire Todd Pacific Lutheran University Luke Weinbrecht, Elyssa Tappero, David Horne, Bryan Donahue, Matt Schmitz, Matthew Hegland, Michael Vermeulen, Trevor Perkins, Nick Lorax, Kristiana Lapo, Greg Pickard, Cameron Wiemerslage, Ryan Ransavage, Allie Jo Koester, Nathan Page, Taylor Christensen, Isaac Moening-Swanson, Riley Swanson, Reed Gunstone, Aaron Steelquist, Emily Knutsen, Christina Gray, Samantha Harrison, Kyle Bennett, Victoria Benson, Adriana Cranston, Connal Boyd, Sam Altenberger, Rainey Aberle, Alex Yannello, Logan Krehbiel, Hannah Bortel, Aerin Basehart Emmons Glacier, White River Why meltwater? • Provides a window into the subglacial environment • Water storage and drainage • Sediment generation, storage and evacuation • Interaction with the hydrothermal system Geologic Hazards Emmons Glacier, • Outburst floods and debris flows White River Volcanic hazards • (e.g., Brown, 2002; Lawler et al., 1996; Collins, 1990) Field Sites - criteria • As close to the terminus as possible, to avoid • Contribution to discharge from non-glacial streams (snowmelt) • Impact of atmospheric mixing on water chemistry • Deposition or entrainment of sediment outside of the Emmons Glacier, subglacial environment White River • Single channel, to achieve • Complete (as possible) representation of the subglacial environment Carbon Emmons Glacier, White River Glacier Field Sites – Channel -
Periglacial Debris-Flow Initiation And
Seeing the True ShapeGeosphere, of Earth’s publishedSurface: onlineApplications on 6 March of 2012Airborne as doi:10.1130/GES00713.1 and Terrestrial Lidar in the Geosciences themed issue Periglacial debris-fl ow initiation and susceptibility and glacier recession from imagery, airborne LiDAR, and ground-based mapping Stephen T. Lancaster1,*, Anne W. Nolin1, Elizabeth A. Copeland1, and Gordon E. Grant2 1College of Earth, Ocean, and Atmospheric Sciences and Institute for Water and Watersheds, Oregon State University, Corvallis, Oregon 97331, USA 2U.S. Department of Agriculture Forest Service, Pacifi c Northwest Research Station, 333 SW First Avenue, Corvallis, Oregon 97331, USA ABSTRACT sion by overland fl ow of water. Using gully- et al., 1996; O’Connor et al., 2001; Osterkamp head initiation sites for debris fl ows that et al., 1986; Sobieszczyk et al., 2009; Walder Climate changes in the Pacifi c Northwest, occurred during 2001–2006, a data model and Driedger, 1994). USA, may cause both retreat of alpine gla- was developed to explore the viability of the There is concern among managers and ciers and increases in the frequency and method for characterization of debris-fl ow policymakers that glacier retreat, rising snow- magnitude of storms delivering rainfall at initiation susceptibilities on Mount Rainier. line elevations, and more frequent and more high elevations absent signifi cant snowpack, The initiation sites were found to occupy a intense storms are leading to greater debris- and both of these changes may affect the restricted part of the four-dimensional space fl ow hazards. On Washington’s Mount Rainier frequency and severity of destructive debris defi ned by mean and standard deviation of in August 2001, rapid melting of Kautz Glacier fl ows initiating on the region’s composite simulated glacial meltwater fl ow, slope angle, directed meltwater into the adjacent watershed volcanoes. -
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 -
Mt. Rainier Where & Why Accidents Happen the Majestic, 14,410-Foot Volcano of Mt
AAC Publications Danger Zones: Mt. Rainier Where & Why Accidents Happen The majestic, 14,410-foot volcano of Mt. Rainier, just 55 miles from Seattle, is one of the most popular mountaineering destinations in North America. Lined by massive glaciers on all sides, the mountain is attempted by about 10,000 people a year. It’s also the site of numerous accidents and close calls. More than 95 mountaineers have died on Rainier’s slopes, including the tragic loss of six climbers in late May 2014 after an avalanche high on Liberty Ridge. This article aims to prevent future tragedies by analyzing the accident history of popular routes. We reviewed more than 110 reports from Mt. Rainier in Accidents in North American Mountaineering over the past 20 years. In addition, we examined the causes of climbing fatalities from 1984 through 2013, as tracked by Mountrainierclimbing.us. The data reveal accident trends on specific routes, suggesting how climbers might best prepare to avoid future incidents. Geologically, Mt. Rainier sits on the Ring of Fire around the Pacific Ocean basin. Geologists consider Mt. Rainier to be an active, potentially dangerous volcano. More immediately, heavy snowfall and highly active glaciers shape the challenging terrain of the mountain. Although there are more than 40 routes and variations up Mt. Rainier, the vast majority of climbers follow two lines: 1) up the Muir Snowfield to Camp Muir, followed by a summit attempt via the Ingraham Glacier or Disappointment Cleaver, or 2) the Emmons/Winthrop Glaciers route above Camp Schurman. With one prominent exception—Liberty Ridge—most accidents occur along these routes. -
MOUNT • RAINIER NATIONAL • PARK Wbtm
wBtmmm wcy«yS&jfli .V&2Smmmmmmm\ fmWk\ mmmWmZfWmVWm W&* M §?'/*£¥&LWrnA Ur+Jmmmm m$af •5-t'' s '•* f •' •' '• Jvfl MOUNT • RAINIER NATIONAL • PARK r~Wask inatopis Trail Guide MOUNT RAINIER NATIONAL PARK Washington This Trail Guide is printed in such a way that the Wonderland Trail Section 1 is the Carbon River area. By starting a trip in this section of the park (such as the one around Mount Rainier on the Wonderland Trail) the hiker may come out periodically at devel oped areas, such as Longmire or Yakima Park, to renew supplies or to dry off if the weather has been wet. However, the hiker may begin long trips anywhere, or short trips as he pleases, by noting the maps in this trail guide and the descriptions of the vari ous trails in each sec tion. 1 SECTION 1 about 50 feet in a setting of trees, "coasting" and the Mowich Lake Carbon River WONDERLAND TRAIL ferns, and moss-covered rocks. Trail intersection is reached. It is Up again out of the trees and into four-tenths of a mile from here to the sunshine of the alpine meadows beautiful Mowich Lake, which oc is a land of flowers and cool, pure cupies an old glacial cirque and is Summary of Trail head wall of a glacial cirque of water. Here are miles of open the largest body of water in Mount Mileages such enormous proportions as to trail through Seattle and Spray Rainier National Park. Mowich is stagger the imagination. At its Parks. In a few spots the trail a Chinook Indian word meaning There are 26.3 miles of the Wonder feet begin the ice masses of the Car reaches rocky country, snowfields, "deer." land Trail in this section of the park. -
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 -
Mount Rainier National Park, Washington
MOUNT RAINIER NATIONAL PARK \ //c^^^ Mount Rainier NATIONAL PARK WASHINGTON Medical Service 18 OPEN ALL YEAR Gasoline Service 18 What To Wear 18 Contents Trails 18 "The Mountain" 6 Fishing 20 Wealth of Gorgeous Flowers 8 Mount Rainier Summit Climb 20 The Forests 10 Accommodations and Expenses .... 21 How To Reach the Park 12 Ohanapecosh Hot Springs 23 Administration 14 Horseback Trips and Guide Service ... 24 Free Public Campgrounds 15 Transportation 24 Post Offices 18 Principal Points of Interest 26 Communication and Express Service ... 18 References 30 Events OF HISTORICAL IMPORTANCE I792 May 8. Capt. George Vancouver, of the Royal British Navy, first white 1899 March 2. Mount Rainier National Park established by act of Congress. man to record sight of "The Mountain"; named it Mount Rainier in honor of his friend Admiral Peter Rainier. I909 Regular (horse-drawn) stage service was started between Ashford and Longmire. I°33 September 2. Dr. William Eraser Tolmie entered northwest corner of what is now the park. First white man to penetrate this region. 1911 October 8. President Taft visited the park. I057 July 16- Lt. A. V. Kautz, of the United States Army, and four companions I9I3 Government surveyors of the United States Geological Survey established made first attempt to scale Mount Rainier but did not reach summit. the elevation of Mount Rainier as 14,408 feet above sea level. 1870 August 17. Hazard Stevens and P. B. Van Trump, of Olympia, Wash., 1 made the first successful ascent of Mount Rainier via Gibraltar route. J93 March 24. Mather Memorial Parkway established.