A 15-Year-Old Sets out Alone for the Tetons: Part 1 of a Climber's Memoir
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Climbing the Sea Annual Report
WWW.MOUNTAINEERS.ORG MARCH/APRIL 2015 • VOLUME 109 • NO. 2 MountaineerEXPLORE • LEARN • CONSERVE Annual Report 2014 PAGE 3 Climbing the Sea sailing PAGE 23 tableofcontents Mar/Apr 2015 » Volume 109 » Number 2 The Mountaineers enriches lives and communities by helping people explore, conserve, learn about and enjoy the lands and waters of the Pacific Northwest and beyond. Features 3 Breakthrough The Mountaineers Annual Report 2014 23 Climbing the Sea a sailing experience 28 Sea Kayaking 23 a sport for everyone 30 National Trails Day celebrating the trails we love Columns 22 SUMMIT Savvy Guess that peak 29 MEMbER HIGHLIGHT Masako Nair 32 Nature’S WAy Western Bluebirds 34 RETRO REWIND Fred Beckey 36 PEAK FITNESS 30 Back-to-Backs Discover The Mountaineers Mountaineer magazine would like to thank The Mountaineers If you are thinking of joining — or have joined and aren’t sure where Foundation for its financial assistance. The Foundation operates to start — why not set a date to Meet The Mountaineers? Check the as a separate organization from The Mountaineers, which has received about one-third of the Foundation’s gifts to various Branching Out section of the magazine for times and locations of nonprofit organizations. informational meetings at each of our seven branches. Mountaineer uses: CLEAR on the cover: Lori Stamper learning to sail. Sailing story on page 23. photographer: Alan Vogt AREA 2 the mountaineer magazine mar/apr 2015 THE MOUNTAINEERS ANNUAL REPORT 2014 FROM THE BOARD PRESIDENT Without individuals who appreciate the natural world and actively champion its preservation, we wouldn’t have the nearly 110 million acres of wilderness areas that we enjoy today. -
Stability of Leaning Column at Devils Tower National Monument, Wyoming
Stability of Leaning Column at Devils Tower National Monument, Wyoming By Edwin L. Harp and Charles R. Lindsay U.S. Geological Survey Open-File Report 2006–1130 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia 2006 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Harp, Edwin L., and Lindsay, Charles R., 2006, Stability of Leaning Column at Devils Tower National Monument, Wyoming: U.S. Geological Survey Open-file Report 2006–1130, 10 p. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Cover photograph: Devils Tower with leaning column visible (red arrow) at lower left edge of vertical shadow on tower face. ii Contents Abstract .....................................................................................................................................................................................................1 Introduction ...............................................................................................................................................................................................1 -
PARK 0 1 5 Kilometers S Ri South Entrance Road Closed from Early November to Mid-May 0 1 5 Miles G Ra River S Access Sy
To West Thumb North Fa r ll ve YELLOWSTONE NATIONAL PARK 0 1 5 Kilometers s Ri South Entrance Road closed from early November to mid-May 0 1 5 Miles G ra River s access sy ad Grassy Lake L nch Ro a g Ra Reservoir k lag e F - Lake of Flagg Ranch Information Station R n the Woods to o Road not recommended 1 h a Headwaters Lodge & Cabins at Flagg Ranch s d for trailers or RVs. Trailhead A Closed in winter River G r lade C e access re e v k i R SS ERNE CARIBOU-TARGHEE ILD Glade Creek e r W Trailhead k Rive ITH a Falls n 8mi SM S NATIONAL FOREST 13km H Indian Lake IA JOHN D. ROCKEF ELLER, JR. D E D E J To South Bo C Pinyon Peak Ashton one C o reek MEMORIAL PARKWAY u 9705ft lt er Creek Steamboat eek Cr Mountain 7872ft Survey Peak 9277ft 89 C a n erry re B ek o z 191 i 287 r A C o y B o a t il e eek ey r C C r l e w e O Lizard C k r k Creek e e e re k C k e e r m C ri g il ly P z z ri G Jackson Lake North Bitch Overlook Cre ek GRAND BRIDGER-TETON NATIONAL FOREST N O ANY k B C ee EB Cr TETON WILDERNESS W Moose Arizona Island Arizona 16mi Lake k e 26km e r C S ON TETON NY o A u C t TER h OL C im IDAHO r B ilg it P ch Moose Mountain rk Pacic Creek k WYOMING Fo e Pilgrim e C 10054ft Cr re e Mountain t k s 8274ft Ea c Leeks Marina ci a P MOOSE BASIN NATIONAL Park Boundary Ranger Peak 11355ft Colter Bay Village W A k T e E N e TW RF YO r O ALLS CAN C O Colter Bay CE m A ri N g Grand View Visitor Center il L PARK P A Point KE 4 7586ft Talus Lake Cygnet Two Ocean 2 Pond Eagles Rest Peak ay Lake Trailhead B Swan 11258ft er lt Lake o Rolling Thunder -
Los Cien Montes Más Prominentes Del Planeta D
LOS CIEN MONTES MÁS PROMINENTES DEL PLANETA D. Metzler, E. Jurgalski, J. de Ferranti, A. Maizlish Nº Nombre Alt. Prom. Situación Lat. Long. Collado de referencia Alt. Lat. Long. 1 MOUNT EVEREST 8848 8848 Nepal/Tibet (China) 27°59'18" 86°55'27" 0 2 ACONCAGUA 6962 6962 Argentina -32°39'12" -70°00'39" 0 3 DENALI / MOUNT McKINLEY 6194 6144 Alaska (USA) 63°04'12" -151°00'15" SSW of Rivas (Nicaragua) 50 11°23'03" -85°51'11" 4 KILIMANJARO (KIBO) 5895 5885 Tanzania -3°04'33" 37°21'06" near Suez Canal 10 30°33'21" 32°07'04" 5 COLON/BOLIVAR * 5775 5584 Colombia 10°50'21" -73°41'09" local 191 10°43'51" -72°57'37" 6 MOUNT LOGAN 5959 5250 Yukon (Canada) 60°34'00" -140°24’14“ Mentasta Pass 709 62°55'19" -143°40’08“ 7 PICO DE ORIZABA / CITLALTÉPETL 5636 4922 Mexico 19°01'48" -97°16'15" Champagne Pass 714 60°47'26" -136°25'15" 8 VINSON MASSIF 4892 4892 Antarctica -78°31’32“ -85°37’02“ 0 New Guinea (Indonesia, Irian 9 PUNCAK JAYA / CARSTENSZ PYRAMID 4884 4884 -4°03'48" 137°11'09" 0 Jaya) 10 EL'BRUS 5642 4741 Russia 43°21'12" 42°26'21" West Pakistan 901 26°33'39" 63°39'17" 11 MONT BLANC 4808 4695 France 45°49'57" 06°51'52" near Ozero Kubenskoye 113 60°42'12" c.37°07'46" 12 DAMAVAND 5610 4667 Iran 35°57'18" 52°06'36" South of Kaukasus 943 42°01'27" 43°29'54" 13 KLYUCHEVSKAYA 4750 4649 Kamchatka (Russia) 56°03'15" 160°38'27" 101 60°23'27" 163°53'09" 14 NANGA PARBAT 8125 4608 Pakistan 35°14'21" 74°35'27" Zoji La 3517 34°16'39" 75°28'16" 15 MAUNA KEA 4205 4205 Hawaii (USA) 19°49'14" -155°28’05“ 0 16 JENGISH CHOKUSU 7435 4144 Kyrghysztan/China 42°02'15" 80°07'30" -
GRAND TETON from NORTH Hole; Battle of Pierre's Hole
MP TETON NATIONAL PARK - WYOMING UNITED STATES Historic Events DEPARTMENT OF THE 1807-8 Discovery of the Tetons hy John GRAND Colter. INTERIOR 1811 The Astorians crossed Teton Pass. TETON Harold L. Ickes, Secretary 1810-45 "The Fur Era" in the Rocky Moun NATIONAL PARE tains, which reached its height be tween 1825 and 1840. WYOMING 1829 Capt. William Sublette named Jack SEASON JUNE 15 TO SEPTEMBER 15 son Hole after his partner in the fur ROADS OPEN MAY 15 TO OCTOBER 15 trade, David Jackson. 1832 Rendezvous of fur trappers in Pierre's GRAND TETON FROM NORTH Hole; Battle of Pierre's Hole. APPROACH ROAD NATIONAL PARK SERVICE 1842 Michaud attempted an ascent of the Newton B. Drury. Director Grand Teton. HE Grand Teton National Park HISTORY OF THE REGION i860 Jim Bridger guided Capt. W. F. embraces the most scenic portion C OHT EJi? S Reynolds' expedition through Teton Many of our national parks have country. T of the Teton Range of Wyo been carved from wilderness areas ming, witb an area of approximately 1872. William H. Jackson, with Hayden previously little known to man and 150 square miles,.or 96,000 acres. It geological survey party, took first seldom visited. The Tetons, on the photographs of Tetons. varies from 3 to 9 miles in width and is contrary, are remarkably rich in his 27 miles in length. The northern ex The Glacier-Covered 1877 Hayden survey party of Orestes St. toric associations. The Grand Teton Tetons, Copyright John made geological studies in the tremity of the park is about 1 1 miles itself has been referred to by an emi Crandall ... -
00 WNAN 2007 New PAGE Template
Western North American Naturalist 81(1), © 2021, pp. 54–62 Cold tolerance of mountain stoneflies (Plecoptera: Nemouridae) from the high Rocky Mountains SCOTT HOTALING1,*,†, ALISHA A. SHAH2,†, MICHAEL E. DILLON3, J. JOSEPH GIERSCH4, LUSHA M. TRONSTAD5, DEBRA S. FINN6, H. ARTHUR WOODS2, AND JOANNA L. KELLEY1 1School of Biological Sciences, Washington State University, Pullman, WA 2Division of Biological Sciences, University of Montana, Missoula, MT 3Department of Zoology and Physiology and Program in Ecology, University of Wyoming, Laramie, WY 4Northern Rocky Mountain Science Center, U.S. Geological Survey, West Glacier, MT 5Wyoming Natural Diversity Database, University of Wyoming, Laramie, WY 6Department of Biology, Missouri State University, Springfield, MO ABSTRACT.—How aquatic insects cope with cold temperatures is poorly understood. This is particularly true for high-elevation species, which often experience a seasonal risk of freezing. In the Rocky Mountains, nemourid stoneflies (Plecoptera: Nemouridae) are a major component of mountain stream biodiversity and are typically found in streams fed by glaciers and snowfields, which are rapidly receding due to climate change. Predicting the effects of climate change on mountain stoneflies is difficult because their thermal physiology is largely unknown. We investigated cold tolerance of several alpine stoneflies (Lednia tumana, Lednia tetonica, and Zapada spp.) from the Rocky Mountains, USA. We mea- sured the supercooling point (SCP) and tolerance to ice enclosure of late-instar nymphs collected from a range of thermal regimes. SCPs varied among species and populations, with the lowest SCP measured for nymphs from an alpine pond, which was much more likely to freeze solid in winter than flowing streams. -
Grand Teton National Park Youngest Range in the Rockies
GRAND TETON NATIONAL PARK YOUNGEST RANGE IN THE ROCKIES the town of Moran. Others recognized that dudes winter better than cows and began operating dude ranches. The JY and the Bar BC were established in 1908 and 1912, respectively. By the 1920s, dude ranch- ing made significant contributions to the valley’s economy. At this time some local residents real- ized that scenery and wildlife (especially elk) were valuable resources to be conserved rather than exploited. Evolution of a Dream The birth of present-day Grand Teton National Park involved controversy and a struggle that lasted several decades. Animosity toward expanding governmental control and a perceived loss of individual freedoms fueled anti-park senti- ments in Jackson Hole that nearly derailed estab- lishment of the park. By contrast, Yellowstone National Park benefited from an expedient and near universal agreement for its creation in 1872. The world's first national park took only two years from idea to reality; however Grand Teton National Park evolved through a burdensome process requiring three separate governmental Mt. Moran. National Park Service Photo. acts and a series of compromises: The original Grand Teton National Park, set Towering more than a mile above the valley of dazzled fur traders. Although evidence is incon- aside by an act of Congress in 1929, included Jackson Hole, the Grand Teton rises to 13,770 clusive, John Colter probably explored the area in only the Teton Range and six glacial lakes at the feet. Twelve Teton peaks reach above 12,000 feet 1808. By the 1820s, mountain men followed base of the mountains. -
Evolution of Deformation in the Buck Mountain Fault Damage Zone, Cambrian Flathead Sandstone, Teton Range, Wyoming Stephanie R
Pan-American Current Research on Fluid Inclusions Rice University, Houston, Texas, U.S.A., June 12-14, 2018, Abstract Volume Evolution of deformation in the Buck Mountain Fault damage zone, Cambrian Flathead Sandstone, Teton Range, Wyoming Stephanie R. FORSTNER, Stephen E. LAUBACH, András FALL Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas, U.S.A. E-mail: [email protected] The Teton Range is a normal fault block that contains older reverse faults (Love et al., 1992). Although generally considered to be Late Cretaceous to early Tertiary structures, the timing, kinematic style, and history of these faults is conjectural. Faults include the Forellen Peak Fault to the north, the Buck Mountain Reverse Fault (BMRF) to the west and south, and the Teton normal fault to the east (Love et al., 1992). The BMRF is rooted in Precambrian crystalline rocks and dips steeply to the east about 60°. The fractured Cambrian Flathead sandstone, an orthoquartzite (90%+ quartz), rests nonconformably on the Precambrian. Its stratigraphic position and relative isotropic mineralogy make the Flathead an ideal horizon for studying brittle deformation. Oriented Flathead hand samples were collected from the footwall of the BMRF along a partially overturned syncline (Figure 1). Continuous SEM-Cathodoluminescence (SEM-CL) scanlines of these samples allow for a systematic kinematic analysis of the cemented opening-mode fractures. We quantify attributes such as; geometry, spacing, orientation, and cross-cutting relationships. In isotropic rock, mode-I fractures primarily propagate along the plane perpendicular to Shmin; therefore, microfractures can be used to indicate paleostress trajectories, strain, and relative fracture timing (Anders et al., 2014; Hooker et al. -
August 2017 RAMBLER
THE MONTHLY PUBLICATION OF THE WASATCH MOUNTAIN CLUB – AUGUST 2017 – VOLUME 96 NUMBER 8 1930 – 2017 Wasatch Mountain Club 2017-2018 PRESIDENT Julie Kilgore 801-244-3323 [email protected] VICE PRESIDENT Brett Matthews 801-831-5940 [email protected] TREASURERS Jason Anderson 385-355-0023 [email protected] Dave Rabiger 801-971-5836 [email protected] SECRETARY Barbara Boehme 801-633-1583 [email protected] BIKING CO-DIRECTORS Cindy Crass 801-803-1336 [email protected] Carrie Clark 801-931-4379 [email protected] Chris Winter 801-384-0973 [email protected] MOUNTAIN BIKING COORDINATOR Greg Libecci 801-699-1999 [email protected] BOATING CO-DIRECTORS Cindy Spangler 801-556-6241 [email protected] Tony Zimmer 440-465-2761 [email protected] BOATING EQUIPMENT CO-COORDINATORS Bret Mathews 801-831-5940 [email protected] Donnie Benson 801-466-5141 [email protected] CANOEING COORDINATOR Pam Stalnaker 801-425-9957 [email protected] RAFTING COORDINATOR Kelly Beumer 801-230-7969 [email protected] CLIMBING CO-DIRECTORS Mark Karpinski 801-886-7285 [email protected] Kathleen Waller 801-859-6689 [email protected] CANYONEERING COORDINATOR Rick Thompson [email protected] -
Harvard Mountaineering 3
HARVARD MOUNTAINEERING 1931·1932 THE HARVARD MOUNTAINEERING CLUB CAMBRIDGE, MASS. ~I I ' HARVARD MOUNTAINEERING 1931-1932 THE HARVARD MOUNTAINEERING CLUB CAMBRIDGE, MASS . THE ASCENT OF MOUNT FAIRWEATHER by ALLEN CARPE We were returning from the expedition to Mount Logan in 1925. Homeward bound, our ship throbbed lazily across the Gulf of Alaska toward Cape Spencer. Between reefs of low fog we saw the frozen monolith of St. Elias, rising as it were sheer out of the water, its foothills and the plain of the Malaspina Glacier hidden behind the visible sphere of the sea. Clouds shrouded the heights of the Fairweather Range as we entered Icy Strait and touched at Port Althorp for a cargo of salmon; but I felt then the challenge of this peak which was now perhaps the outstanding un climbed mOUlitain in America, lower but steeper than St. Elias, and standing closer to tidewater than any other summit of comparable height in the world. Dr. William Sargent Ladd proved a kindred spirit, and in the early summer of 1926 We two, with Andrew Taylor, made an attempt on the mountain. Favored by exceptional weather, we reached a height of 9,000 feet but turned back Photo by Bradford Washburn when a great cleft intervened between the but tresses we had climbed and the northwest ridge Mount Fairweather from the Coast Range at 2000 feet of the peak. Our base was Lituya Bay, a beau (Arrows mark 5000 and 9000-foot camps) tiful harbor twenty miles below Cape Fair- s camp at the base of the south face of Mount Fair weather; we were able to land near the foot of the r weather, at 5,000 feet. -
Exploring Grand Teton National Park
05 542850 Ch05.qxd 1/26/04 9:25 AM Page 107 5 Exploring Grand Teton National Park Although Grand Teton National Park is much smaller than Yel- lowstone, there is much more to it than just its peaks, a dozen of which climb to elevations greater than 12,000 feet. The park’s size— 54 miles long, from north to south—allows visitors to get a good look at the highlights in a day or two. But you’d be missing a great deal: the beautiful views from its trails, an exciting float on the Snake River, the watersports paradise that is Jackson Lake. Whether your trip is half a day or 2 weeks, the park’s proximity to the town of Jackson allows for an interesting trip that combines the outdoors with the urbane. You can descend Grand Teton and be living it up at the Million Dollar Cowboy Bar or dining in a fine restaurant that evening. The next day, you can return to the peace of the park without much effort at all. 1 Essentials ACCESS/ENTRY POINTS Grand Teton National Park runs along a north-south axis, bordered on the west by the omnipresent Teton Range. Teton Park Road, the primary thoroughfare, skirts along the lakes at the mountains’ base. From the north, you can enter the park from Yellowstone National Park, which is linked to Grand Teton by the John D. Rockefeller Jr. Memorial Parkway (U.S. Hwy. 89/191/287), an 8-mile stretch of highway, along which you might see wildlife through the trees, some still bare and black- ened from the 1988 fires. -
Grand Teton National Park Wyoming
UNITED STATES DEPARTMENT OF THE INTERIOR RAY LYMAN WILBUR. SECRETARY NATIONAL PARK SERVICE HORACE M.ALBRIGHT. DIRECTOR CIRCULAR OF GENERAL INFORMATION REGARDING GRAND TETON NATIONAL PARK WYOMING © Crandall THE WAY TO ENJOY THE MOUNTAINS THE GRAND TETON IN THE BACKGROUND Season from June 20 to September 19 1931 © Crandill TRIPS BY PACK TRAIN ARE POPULAR IN THE SHADOWS OF THE MIGHTY TETONS © Crandall AN IDEAL CAMP GROUND Mount Moran in the background 'Die Grand Teton National Park is not a part of Yellowstone National Park, and, aside from distant views of the mountains, can not be seen on any Yellowstone tour. It is strongly urged, how ever, that visitors to either park take time to see the other, since they are located so near together. In order to get the " Cathedral " and " Matterhorn " views of the Grand Teton, and to appreciate the grandeur and majestic beauty of the entire Teton Range, it is necessary to spend an extra day in this area. CONTENTS rage General description 1 Geographic features: The Teton Range 2 Origin of Teton Range 2 Jackson Hole 4 A meeting ground for glaciers .. 5 Moraines 6 Outwash plains 6 Lakes 6 Canyons 7 Peaks 7 How to reach the park: By automobile . 7 By railroad 9 Administration 0 Motor camping 11 Wilderness camping • 11 Fishing 11 Wild animals 12 Hunting in the Jackson Hole 13 Ascents of the Grand Teton 13 Rules and regulations 14 Map 18 Literature: Government publications— Distributed free by the National Park Service 13 Sold by Superintendent of Documents 13 Other national parks ' 19 National monuments 19 References 19 Authorized rates for public utilities, season of 1931 23 35459°—31 1 j II CONTENTS MAPS AND ILLUSTRATIONS COVER The way to enjoy the mountains—Grand Teton in background Outside front.