Mount Rainier NATIONAL PARK
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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. -
USGS Bulletin 2217
Field Guide to Hydrothermal Alteration in the White River Altered Area and in the Osceola Mudfl ow, Washington By David A. John, James J. Rytuba, Roger P. Ashley, Richard J. Blakely, James W. Vallance, Grant R. Newport, and Gary R. Heinemeyer Prepared for the Society of Economic Geologists Field Trip, November 6, 2003 Bulletin 2217 U.S. Department of the Interior U.S. Geological Survey Field Guide to Hydrothermal Alteration in the White River Altered Area and in the Osceola Mudflow, Washington By David A. John, James J. Rytuba, Roger P. Ashley, Richard J. Blakely, James W. Vallance, Grant R. Newport, and Gary R. Heinemeyer Bulletin 2217 U.S. Department of the Interior U.S. Geological Survey 1 U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. U.S. Geological Survey, Reston, Virginia: 2003 Electronic copies of this publication are available online at http://geopubs.wr.usgs.gov/bulletin/b2217/ Additional USGS publications can be found online at http://geology.usgs.gov/products.html For more information about the USGS and its products: Telephone: 1-888-ASK-USGS (1–888–275–8747) World Wide Web: http://www.usgs.gov/ Published in the Western Region, Menlo Park, California Manuscript approved for publication October 25, 2003 2 Contents Introduction ................................................................................................................................................... 1 Road log from Enumclaw to the White River Altered Area and the Osceola Mudflow along the lower White River, Washington ............................................................................................ -
Empowering a Generation of Climbers My First Ascent an Epic Climb of Mt
WWW.MOUNTAINEERS.ORG SPRING 2018 • VOLUME 112 • NO. 2 MountaineerEXPLORE • LEARN • CONSERVE in this issue: Empowering a Generation of Climbers An Interview with Lynn Hill My First Ascent Becoming Backwoods Barbie An Epic Climb of Mt. Rainier Via the Willis Wall tableofcontents Spring 2018 » Volume 112 » Number 2 Features The Mountaineers enriches lives and communities by helping people explore, conserve, learn about, and enjoy 24 Empowering a Generation of Climbers the lands and waters of the Pacific Northwest and beyond. An Interview with Lynn Hill 26 My First Ascent Becoming Backwoods Barbie 32 An Epic Climb of Mt. Rainier Via the Willis Wall Columns 7 MEMBER HIGHLIGHT Marcey Kosman 8 VOICES HEARD 24 1000 Words: The Worth of a Picture 11 PEAK FITNESS Developing a Personal Program 12 BOOKMARKS Fuel Up on Real Food 14 OUTSIDE INSIGHT A Life of Adventure Education 16 YOUTH OUTSIDE We’ve Got Gear for You 18 SECRET RAINIER 26 Goat Island Mountain 20 TRAIL TALK The Trail Less Traveled 22 CONSERVATION CURRENTS Climbers Wanted: Liberty Bell Needs Help 37 IMPACT GIVING Make the Most of Your Mountaineers Donation 38 RETRO REWIND To Everest and Beyond 41 GLOBAL ADVENTURES The Extreme Fishermen of Portugal’s Rota Vicentina 55 LAST WORD Empowerment 32 Discover The Mountaineers If you are thinking of joining, or have joined and aren’t sure where to star, why not set a date to Meet The Mountaineers? Check the Mountaineer uses: Branching Out section of the magazine for times and locations of CLEAR informational meetings at each of our seven branches. on the cover: Bam Mendiola, AKA “Backwoods Barbie” stands on the top of Mount Rainier. -
The Big One Opportunities That Rainier Has to Offer, Just in Time for You to Start Making Your Own Summer Hiking Plans
May + June 2011 » Washington Trails 21 On Trail Northwest Explorer » Living in the Northwest, we have no shortage of wilderness locations to escape into for a day—or a week. On any ol’ weekend, we could be climbing to the rim of smoldering Mount St. Helens, journeying through lush rain forests in the Olympics or trekking across the jagged ridges of the North Cascades. And while all of these places, and so many more locations, are outstanding, nothing quite compares with the majesty—or sheer immensity—of “The Mountain.” But when you think about hiking that Mountain, where do you even start? With over 240 miles of hiking trails (not counting mountaineering routes), spread over 378 square miles, there’s a lot to choose from. Add to that the incredible amount of scenic features—473 streams and rivers, 292 lakes, 122 waterfalls, 25 named glaciers, and more meadows, valleys, wildflowers, old-growth forest, and mind- numbing views than you can shake a trekking pole at—and the task of choosing a trail can no doubt be daunting. Thankfully, there are stacks of helpful guidebooks available to get you started. But even as great as most of those guidebooks are—full of inspiring photos and informative elevation profile graphs (a feature I particularly appreciate)—you’re still trying to whittle down from 50-plus options. And if you’re unfamiliar with The Mountain, what you’re really thinking Backpacking is, “Where do I go to get the really good stuff?” Well, this month, you’re in luck. From shorter starter trails to the granddaddy of round-the- mountain adventures, we’ll highlight five—and only five—of the most outstanding hiking the Big One opportunities that Rainier has to offer, just in time for you to start making your own summer hiking plans. -
Evaluating Titan2d Mass-Flow Model Using the 1963 Little Tahoma Peak Avalanches, Mount Rainier, Washington
Journal of Volcanology and Geothermal Research 139 (2005) 89–102 www.elsevier.com/locate/jvolgeores Evaluating Titan2D mass-flow model using the 1963 Little Tahoma Peak avalanches, Mount Rainier, Washington M.F. Sheridana,*, A.J. Stintona, A. Patrab, E.B. Pitmanc, A. Bauerb, C.C. Nichitac aDepartment of Geology, 876 Natural Science Complex, University at Buffalo, Buffalo NY, 14260, USA bDepartment of Mechanical and Aerospace Engineering, University at Buffalo, Buffalo NY, 14260, USA cDepartment of Mathematics, University at Buffalo, Buffalo NY, 14260, USA Accepted 29 June 2004 Abstract The Titan2D geophysical mass-flow model is evaluated by comparing its simulation results and those obtained from another flow model, FLOW3D, with published data on the 1963 Little Tahoma Peak avalanches on Mount Rainier, Washington. The avalanches, totaling approximately 10Â106 m3 of broken lava blocks and other debris, traveled 6.8 km horizontally and fell 1.8 km vertically (H/L=0.246). Velocities calculated from runup range from 24 to 42 m/s and may have been as high as 130 m/s while the avalanches passed over Emmons Glacier. Titan2D is a code for an incompressible Coulomb continuum; it is a depth-averaged, dshallow-waterT, granular-flow model. The conservation equations for mass and momentum are solved with a Coulomb-type friction term at the basal interface. The governing equations are solved on multiple processors using a parallel, adaptive mesh, Godunov scheme. Adaptive gridding dynamically concentrates computing power in regions of special interest; mesh refinement and coarsening key on the perimeter of the moving avalanche. The model flow initiates as a pile defined as an ellipsoid by a height (z) and an elliptical base defined by radii in the x and y planes. -
MOUNT RAINIER NATIONAL PARK Q
;;:4 L' L*I ! THE GEOLOGY 0F MOUNT RAINIER NATIONAL PARK q BY HOWARD A. COOMBS 4 II UNIVERSiTY OF WASHINGTON PUBLICATION S IN GEOLOGY Vol.3.No.2, pp. 131-212 July, 1936 THE GEOLOGY OF MOUNT RAINIER NATIONAL PARK BY HOWARD A. COOMBS PUBLISHED BY THE UNIVERSITY OF WASHINGTON SEATTLE, WASHINGTON 1936 CONTENTS PAGE Introduction 141 Location 141 Routes of Approach 141 Field Work 142 Acknowledgments 143 History 143 Review of Literature 144 Topography 145 Drainage 146 Climate 147 Fauna and Flora 148 Geology 149 Distribution and Relative Ages of the Rocks 149 The Puget Group 149 Keechelus Andesitic Series 150 Mineral Mountain Andesite Porphyry 152 Sheepskull Gap Tufts 154 Sourdough Mountain Breccias 155 Chinook Pass Diorite Porphyry 157 Longmire Acid Breccias 157 Starbo Altered Tufts 160 Cayuse Pass Acid Hornfels 161 Mowich Rypersthene Basalt 163 Summary 165 Relations and Age 165 Snoqualmie Granodiorite 167 Areal Extent 167 Petrography 168 Relations and Age 170 The Mount Rainier Volcanics 172 Composition 174 Microscopical Petrography 175 Plagioclase 175 Hypersthene 180 Monoclinic Hypersthene 184 Augite 184 Olivine 185 Hornblende 185 Holohyaline Groundmass 187 Hypo- and Holocrystalline Groundmass 187 Miscellaneous Features of the Groundmass 188 (135) CONTENTSContinued PAGE Physiography and Geomorphology 191 Introduction 191 The Cascades 191 Previous Literature 191 Pre-Rainier Topography 195 Pre-Rainier River Pattern 196 Pre-Rainier Structure 198 Conclusions 200 Summary 201 The Cone of Mount Rainier 202 The Summit Area 202 Glacial Erosion 204 Cleavers 204 Wedges 204 Intergiaciers 206 Asymmetrical Topography as a Result of Selective Glaciation. 207 Bibliography 211 Appendix A. Geologic Map of Mount Rainier National Park 212 ILLUSTRATIONS FIG. -
Get Ting to Know the Mountain a Wonderland Trail Journal
News & Features Getting to Know the Mountain ARNOSKI B AURIE L In July 2005, two brothers, Mike and Steve, embarked on a once-in-a-lifetime trip: completing the 93-mile Wonderland Trail around Mount Rainier. Above: Steve at Narada Falls. Right: hikers near Carbon River Glacier. A Wonderland Trail Journal By “Mike in Tac” hitting the road. After a couple of stops them and shared their space for 5 or 10 for errands and phone calls, we got our minutes. They never ran off—we finally permit and arrived here. left them! Thursday, July 7, 2005, 10:22 p.m. We wandered up to Eunice Lake and Back to the tent at 7:00 p.m. and we Mowich Lake Campground, fished a bit—no views, clouds totally raided the “free pile” of food at the 5,000 feet socked us in. I had terrible luck, lost ranger cabin for dinner. Lots of cocoa Overcast, fogged in, 74 degrees in a lure (Steve’s) on the first cast. Steve too. Met Tim—another guy (with two tent, 60 degrees outside had much better luck with his $7.50 friends—Joan and Todd, I think)—who Slept in a bit and said good-bye to Jane rod and reel. On the way back, we ran will start the Wonderland tomorrow as at 8:00 a.m. Steve and I then packed for a in to a couple of one-year-old bucks—no well. They’re doing an 8-day trip. couple of hours before having lunch and fear whatsoever. -
Mount Rainier NP: Wonderland:An Administrative History (Table of Contents)
Mount Rainier NP: Wonderland:An Administrative History (Table of Contents) MOUNT RAINIER Wonderland An Administrative History of Mount Rainier National Park TABLE OF CONTENTS Cover Asahel Curtis photograph of Rainier Park Company President Henry Rhodes (front), Mount Rainier National Park Superintendent O.A. Tomlinson (middle), and National Park Service Director Stephen Mather (right), against a backdrop of Mount Rainier, 1928. (Photo courtesy of the Washington State Historical Society, Tacoma, Washington) Introduction PART ONE: THE CULTURAL SETTING I. Historical Overview of Indians and Mount Rainier II. American Settlement and Mount Rainier PART TWO: FOUNDING YEARS, 1893-1915 III. Establishment of Mount Rainier National Park IV. The New Pleasuring Ground V. Rudiments of Administration VI. Natural Resource Protection in the Early Years PART THREE: YEARS OF PROMISE, 1915-1930 VII. Mission and Professionalism VIII. The Park Under Construction IX. The Rainier National Park Company PART FOUR: DEPRESSION AND WAR YEARS, 1930-1945 X. Visitor Use in the Depression Era XI. The Impact of the New Deal http://www.nps.gov/history/history/online_books/mora/adhi/contents.htm[4/10/2014 1:47:51 PM] Mount Rainier NP: Wonderland:An Administrative History (Table of Contents) XII. Research and Interpretation in the 1930s XIII. National Park Values in Wartime PART FIVE: CONTENTIOUS YEARS, 1945-1965 XIV. The Problem of Winter Use XV. The Problem of the Park Concession XVI. Mission 66 for Mount Rainier XVII. Natural Resource Protection Marginalized PART SIX: YEARS OF CONSOLIDATION, 1965-1995 XVIII. Administrative Development XIX. Zoning the Park XX. The Change in Resource Management XXI. An Overview of Park Science XXII. -
Mount Rainier National Park Place Names
Mount Rainier National Park Place Names Gary Fuller Reese. April 10, 2009. PREFACE. Because of its prominence as the "Great Mountain of the Pacific Northwest" Rainier was one of the first features in the Pacific Northwest named by early explorers. The center of a National Park since 1899 most prominent features around the mountain have received names, some of which have become official and some of which a common use. In 1919 Mount Rainier National Park Superintendent Roger Toll wrote about names in the National Park: "The park service is interested in having names applied to the various...scenic points that are now unnamed....the most desirable names...are the original Indian names, or, if these are too long and unpronounceable their English equivalents are often very good. "If no original name can be found, and a name is to be supplied, the Indian names may be drawn upon with advantage, but this should be done by an expert...Descriptive names are good. The only thing most difficult to avoid is the indiscriminate naming of scenic features after persons." While name origins have been found for many locations within the National Park there are a number of places for which origins are missing, especially on the northern side of the mountain. In 1916 Edmond S. Meany wrote about Mount Rainier. He listed many places for which he could not find a name origin. In 1932 the writers of the Encyclopedia of Information on Mount Rainier National Park made a list of locations on the mountain recording that they were unable to supply origins for numbers of them. -
Summits on the Air USA (W7W)
Summits on the Air U.S.A. (W7W) Association Reference Manual (ARM) Document Reference S39.1 Issue number 2.0 Date of issue 01-Dec-2016 Participation start date 01-July-2009 Authorised Date 08-Jul-2009 obo SOTA Management Team Association Manager Darryl Holman, WW7D, [email protected] Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Summits on the Air – ARM for USA W7W-Washington Table of contents Change Control ................................................................................................................... 4 Disclaimer ........................................................................................................................... 5 Copyright Notices ............................................................................................................... 5 1.0 Association Reference Data .......................................................................................... 6 2.1 Program Derivation ....................................................................................................... 7 2.2 General Information ...................................................................................................... 7 2.3 Final Access, Activation Zone, and Operating Location Explained ............................. 8 2.4 Rights of Way and Access Issues ................................................................................ -
Mount Rainier National Park Place Names
Mount Rainier National Park Place Names Gary Fuller Reese. April 10, 2009. PREFACE. Because of its prominence as the "Great Mountain of the Pacific Northwest" Rainier was one of the first features in the Pacific Northwest named by early explorers. The center of a National Park since 1899 most prominent features around the mountain have received names, some of which have become official and some of which a common use. In 1919 Mount Rainier National Park Superintendent Roger Toll wrote about names in the National Park: "The park service is interested in having names applied to the various...scenic points that are now unnamed....the most desirable names...are the original Indian names, or, if these are too long and unpronounceable their English equivalents are often very good. "If no original name can be found, and a name is to be supplied, the Indian names may be drawn upon with advantage, but this should be done by an expert...Descriptive names are good. The only thing most difficult to avoid is the indiscriminate naming of scenic features after persons." While name origins have been found for many locations within the National Park there are a number of places for which origins are missing, especially on the northern side of the mountain. In 1916 Edmond S. Meany wrote about Mount Rainier. He listed many places for which he could not find a name origin. In 1932 the writers of the Encyclopedia of Information on Mount Rainier National Park made a list of locations on the mountain recording that they were unable to supply origins for numbers of them. -
Mount Rainier : a Record of Exploration
Presented to the UNIVERSITY OF TORONTO LIBRARY by the ONTARIO LEGISLATIVE LIBRARY 1980 Mount Rainier THE MACMILLAN COMPANY NEW YORK BOSTON CHICAGO DALLAS ATLANTA SAN FRANCISCO MACMILLAN & CO., LIMITED LONDON BOMBAY CALCUTTA MELBOURNE THE MACMILLAN CO. OF CANADA, LTD. TORONTO ( . t . * Mount Rainier. JSL- Record of Exploration to* Edited by Edmond 6". Meany in the President The Mountainttrt Profetsor of History University of Washington. of " " Sound Author of Vancouver^ Discovery of Puget " History of the State of Washington," etc. New Tork The Macmillan Company 1916 : .<-. reserved . ^tll . rights \^4tt t *' EP -a / COPYRIGHT, 1916, BY THE MACMILLAN COMPANY. Set up and electrotyped. Published November, 1916. J. 8. Gushing Co. Berwick & Smith Co. Norwood, Maas., U.S.A. TCo GENERAL HAZARD STEVENS EARLY LOVER OF THE MOUNTAIN, THIS BOOK IS AFFECTIONATELY DEDICATED PREFACE MOUNT RAINIER NATIONAL PARK is visited annually by increasing thousands of tourists. Many of them seek information about the discoveries and explorations of the mountain and its environs. Much of the information sought, especially that about the origin of place names, has never been published. The annals of discovery and ex- ploration, which have been published, have often appeared in books, pamphlets, or periodicals not easily accessible. It is the purpose of this work to gather the essential por- tions of the desired information within a compact, usable form. During the summer of 1915, the mountain was for the first time encircled by a large company of travelers. Small parties, carrying their luggage and provisions on their backs, had made the trip a number of times. The Moun- taineers Club, in 1915, conducted a party of one hundred, with fully equipped pack train and commissary, around the mountain.