Teton Range, Wy
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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. -
Naturalist Pocket Reference
Table of Contents Naturalist Phone Numbers 1 Park info 5 Pocket GRTE Statistics 6 Reference Timeline 8 Name Origins 10 Mountains 12 Things to Do 19 Hiking Trails 20 Historic Areas 23 Wildlife Viewing 24 Visitor Centers 27 Driving Times 28 Natural History 31 Wildlife Statistics 32 Geology 36 Grand Teton Trees & Flowers 41 National Park Bears 45 revised 12/12 AM Weather, Wind Scale, Metric 46 Phone Numbers Other Emergency Avalanche Forecast 733-2664 Bridger-Teton Nat. Forest 739-5500 Dispatch 739-3301 Caribou-Targhee NF (208) 524-7500 Out of Park 911 Grand Targhee Resort 353-2300 Jackson Chamber of Comm. 733-3316 Recorded Information Jackson Fish Hatchery 733-2510 JH Airport 733-7682 Weather 739-3611 JH Mountain Resort 733-2292 Park Road Conditions 739-3682 Information Line 733-2291 Wyoming Roads 1-888-996-7623 National Elk Refuge 733-9212 511 Post Office – Jackson 733-3650 Park Road Construction 739-3614 Post Office – Moose 733-3336 Backcountry 739-3602 Post Office – Moran 543-2527 Campgrounds 739-3603 Snow King Resort 733-5200 Climbing 739-3604 St. John’s Hospital 733-3636 Elk Reduction 739-3681 Teton Co. Sheriff 733-2331 Information Packets 739-3600 Teton Science Schools 733-4765 Wyoming Game and Fish 733-2321 YELL Visitor Info. (307) 344-7381 Wyoming Highway Patrol 733-3869 YELL Roads (307) 344-2117 WYDOT Road Report 1-888-442-9090 YELL Fill Times (307) 344-2114 YELL Visitor Services 344-2107 YELL South Gate 543-2559 1 3 2 Concessions AMK Ranch 543-2463 Campgrounds - Colter Bay, Gros Ventre, Jenny Lake 543-2811 Campgrounds - Lizard Creek, Signal Mtn. -
A Brief History of the Trails of Grand Teton National Park 55
Pritchard: A Brief History of the Trails of Grand Teton National Park 55 A BRIEF HISTORY OF THE TRAILS OF GRAND TETON NATIONAL PARK JAMES A. PRITCHARD IOWA STATE UNIVERSITY AMES ABSTRACT reconstructed during the MISSION 66 era, but some of the stone stairs along the way from the boat dock This project investigated the history of the to Hidden Falls date back to the CCC era. backcountry trail system in Grand Teton National Park (GTNP). In cooperation with GTNP Cultural Walking on a beautiful mountain path, one Resources and the Western Center for Historic might never guess the extensive preparation of rock Preservation in GTNP, we located records describing materials (expediting drainage) that is required before the early development of the trail system. Only a few the surface ―treadway‖ is laid down (Barter et al. historical records describe or map the exact location 2006). In fact, trails are significant engineering of early trails, which prove useful when relocating achievements that need constant care and upkeep, trails today. The paper trail becomes quite rich, including annual clearance of vegetation and the however, in revealing the story behind the practical occasional repair to sections of trail. development of Grand Teton National Park as it joined the National Park Service system. Pre-existing Trails Archeological sites are present in the upper INTRODUCTION parts of Berry Creek drainage, thought to represent ―basecamps‖ occupied consistently over 8,000 years. Grand Teton National Park and its trail A notable pre-historic travel route traversed the system developed together during the early years of northern end of the Teton Range, from the west into National Park Service (NPS) administration. -
Jackson Hole Vacation Planner Vacation Hole Jackson Guide’S Guide Guide’S
Typeface “Skirt” light weight Globe Addition Book Spine Guide’s Guide’s Guide Guide Guide’s Guide™ Jackson Hole Vacation Planner 2014 EDITION Welcome! We hope this planner will help you create a great itinerary to Jackson Hole and the Greater Yellowstone Area. This guide is meant as a starting point for your research into where to stay, what to do and things you should not miss while in Jackson Hole. The information included in this vacation planner is based on years of personal experience here in Jackson Hole and the feedback of thousands of guests throughout the years. The suggestions included in this planner, including the suggested businesses, are not paid advertisements. The businesses, activities and events have been included at no charge based on our experience and the experience of other travelers. These are the places we frequent, we like or that we have heard from our guests to be excellent. Be aware that just because we didn’t include something doesn’t mean it’s bad and anything in here could change for the worse. Management, employees and quality can always change but we have done our best to steer you in the right direction. If you think something should be included or something should be removed feel free to email us your suggestions. We hope you enjoy our vacation planner and most importantly that you have a great vacation to Jackson Hole. Fun Facts: • Yellowstone is larger than Delaware and Rhode Island combined! • Jackson Hole is named after the trapper and explorer, Davey Jackson! • Grand Teton National Park is named -
Holly Lake, Located in Paintbrush Canyon, Is Fastest Accessed from the String Lake Trailhead of Grand Tetons National Park. It
! HOLLY LAKE, GRAND TETONS NATIONAL PARK Holly Lake, located in Paintbrush Canyon, is fastest accessed from the String Lake trailhead of Grand Tetons National Park. It is 1.6 miles to the junction with the trail from Leigh Lake (which is also 1.6 miles but supposedly has a steeper incline than the trail from String Lake). It is then an additional 4.9 miles to Holly Lake, making the round-trip distance 13 miles total. The trailhead is located at an elevation of 6,880 ft, and the lake is located at 9,450 ft. The trail is quite easy to find and is well-travelled, though we did not encounter many hikers on the trail. Note that it is not safe to begin this hike !late in the day! On our drive in to Wilson, WY the previous day, we drove the Teton Scenic Byway and stopped to take a photo of this sign: ! ! Parking for the Holly Lake hike at the String Lake trailhead; if you arrive at the trailhead "early", ~8:00 am, there are very few vehicles (mainly those from hikers staying overnight), and can have a good selection of parking spaces; however, arriving later in the day (for a shorter hike, for example), parking would be difficult: ! ! Panorama of the tetons from near the trailhead: ! ! Panorama of Leigh Lake: ! ! Leigh Lake: ! ! Another panorama from the trail along the western rim of Leigh Lake: ! ! The trail leaves the rim of Leigh Lake near the northern end of the lake and ascends through some short trees: ! ! This may be a potential route to Rockchuck Peak, as we saw a hiker leave the trail near here who appeared to ascend towards the distant -
Backcountry Camping Brochure
National Park Service Grand Teton U.S. Department of the Interior Grand Teton National Park John D. Rockefeller, Jr. Memorial Parkway Backcountry Camping The North Fork of Cascade Canyon - Danielle Lehle photo Before Leaving Home Weather Planning Your Trip Group Size Boating This guide provides general information about backcountry use in Grand Teton National Individual campsites accommodate one to Register all vessels annually with the park. Park and the John D. Rockefeller, Jr. Memorial Parkway. The map on the back page is six people. Groups of seven to 12 people Purchase permits at the Craig Thomas, only for general trip planning and/or campsite selection. For detailed information, use a must use designated group sites that are Colter Bay or Jenny Lake (cash only) visitor topographic map or hiking guide. When planning your trip, consider each member of your larger and more durable. In winter, parties centers. Lakeshore campsites are located party. Backpackers should expect to travel no more than 2 miles per hour, with an additional are limited to 20 people. on Jackson and Leigh lakes. Camping is hour for every 1,000 feet of elevation gain. Do not plan to cross more than one mountain not allowed along the Snake River. Strong The table below summarizes weather at Moose, WY, 6467 feet. Temperatures in the Teton pass in a day. If you only have one vehicle, you may want to plan a loop trip. There is no Backcountry Conditions afternoon winds occur frequently. For Range can change quickly and be much colder at upper elevations. Check the local area shuttle service in the park, but transportation services are available; ask at a permits desk for Snow conditions vary annually. -
Paintbrush Divide Loop Trail
-110.860 -110.850 -110.840 -110.830 -110.820 -110.810 -110.800 -110.790 -110.780 -110.770 -110.760 -110.750 -110.740 -110.730 -110.720 -110.710 9 , 6 0 0 0 0 8 , 0 00 6 1 6 ,60 8, 1 0 1 , 2 0 0 Mount Moran 12605 T East Horn ra p 9, 00 Trapper p 2 e r Lake L a 0 k 60 e , 1 T 1 .55 r 00 West Horn ,0 1 1 0 0 Thor Peak 6 , 43.830 0 1 43.830 Cirque Lake 0 0 00 4 ,4 Bearpaw Lake , 9 .25 9 00 ,6 0 0 1 0 6 , 0 9 0 1 0 ,8 0,0 0 8 .35 7,200 0 0 8 8,200 , 8,4 7 00 00 9,2 Leigh Lake 0 0 0 , 9 8,0 00 L e ig h L a k e Mystic Island 0 T 43.820 00 r 43.820 8, a i l 7,400 1.30 0 Leigh Canyon 7,00 9,200 7, 200 0 8,00 Leigh Lake 9,4 00 8,600 Mink Lake 0 0 6 0, 43.810 43.810 1 9,600 8 ,800 00 ,8 9 0 9,00 0 0 ,4 8 0 ,40 10 7 9,6 ,400 00 Grizzly Bear Lake Hol 4.90 ly La k e 0 Mount Woodring 11590 T 0 7,600 ra Leigh Lake ,4 il 0 1 0 l 0 i 0 0 00 a 1 0 1,4 2 r , , 1 7 T 1 0 e 0 k 8,0 a Boulder Island L h 43.800 g 43.800 9,8 i 00 e L ail Tr S n ke tri g Lak La e T lly r .75 1.50 Ho 10,400 8 , 80 0 00 9,8 Outlier Site 0 9, 60 0 0 2 P , ai 1 7 .80 ntb 0,6 1.75 rus 00 h Di 10,60 8 vid 0 ,4 00 e T ra 1.30 il Holly Lake Site Holly Lake 00 9 Paintbrush Divide 0 ,4 Lake Solitude ,4 10,00 9 00 9 ,2 0 2.25 0 Paint 0 0 N bru ,0 il s 8 ra o h C T r 10 ke t ,8 a a h L 0 n 0 g F y n on Tr ri o Paintbrush Canyon a t Cathedral Group r 9 il S 43.790 k ,8 43.790 00 il Turnout o Holly Lake Group Site ra f T e C k a La s lly 1 c 9,200 Ho 0 ad ,0 e Ca p 0 ny oo 0 on Rockchuck Peak L ke North Fork of S a L tr y i n 00 n n Cascade Canyon 9,6 g e J L .55 a k e T d r Access a Ramp o -
Pleistocene Glaciation of the Jackson Hole Area, Wyoming
Pleistocene Glaciation of the Jackson Hole Area, Wyoming Professional Paper 1835 U.S. Department of the Interior U.S. Geological Survey Cover. Pinedale-1 glacial moraine deposited by the Buffalo Fork lobe of the Greater Yellowstone Glacial System that headed 50 kilometers (30 miles) to the northeast in the high Absaroka Range. The flat surface in the middle distance is the Pinedale-1 outwash terrace. On this side of this flat terrace is a deep glacial kettle formed by the melting of a large block of glacial ice buried in this outwash gravel. The distant bench is on the far side of the Snake River (not visible) and is a Pinedale-2 terrace deposited by outwash from the Yellowstone Plateau ice cap. The Teton Range forms the skyline with Grand Teton the highest peak. Although the Teton Range has dramatic glacial features, the greatest effect on the surficial geology of Jackson Hole was that produced by the large glacial lobes that advanced into Jackson Hole along the southern margin of the Greater Yellowstone Glacial System. Pleistocene Glaciation of the Jackson Hole Area, Wyoming By Kenneth L. Pierce, Joseph M. Licciardi, John M. Good, and Cheryl Jaworowski Professional Paper 1835 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. Geological Survey William H. Werkheiser, Deputy Director exercising the authority of the Director U.S. Geological Survey, Reston, Virginia: 2018 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit https://www.usgs.gov or call 1–888–ASK–USGS. -
VARIOUS NOTES 117 but Evidently Not Previously Climbed
VariousNotes EDITED BY H. ADAMS CARTER UNITED STATES Tetons, Wyoming. In the past summer several new routes were made in the Tetons. A few of the more important climbs follow. Travsre between Bivouac and Rapold’s Peaks. Lying between Moran and Snowshoe Canyons is one of the most spectacularly pinnacled ridges of the Teton Range, which Leigh Ortenburger has labeled as “terrific.” After Bill Buckingham and I had reached the summit of Bivouac Peak by the ordinary route by midmorning on September 4, we started for Ray- nold’s Peak far to the west. Lying between us and our goal was a twisting, crumbling, knife-ridge, which lived up to Ortenburger’s evaluation. The actual climbing of the ridge proved not too difficult, it being clearly a problem of endurance and extreme care on the decomposed rock. Bill and I climbed all the major pinnacles, at times even rocking back and forth the summits of the smaller spires. Our greatest problem was water, and toward the end of the ridge a nearby lake was so tempting that we happily descended for refreshment. After this brief respite we took once again to the ridge and soon found ourselves on top of Raynold’s Peak. In all we took 11 hours for the traverse and all night for the return to Jackson Lake via Moran Canyon. JOHN FONDA West Ridge of the Middle Teton. The long west ridge of the Middle Teton was ascended for the first time on August 4, 1955, by William Buckingham and Mary Lou Nohr. From the south fork of Cascade Can- yon we followed a broad couloir into the lower end of the basin between the west ridges of the Grand and Middle Tetons. -
Grand Teton National Park
To West Thumb Road closed from early November to mid-May F al r ls ve YELLOWSTONE NATIONAL PARK Ri South Entrance ERNESS ILD Grassy Lake W E oad Reservoir L R Flagg Ranch O H r e te Information Station ak in R L w Trailhead A in y G s ed s os E ra cl Lake of the Woods N G I CARIBOU-TARGHEE W r r F ve e all i NATIONAL FOREST iv Huckleberry Mountain s R R 8mi 9615ft 13km 2930m Indian Lake JOHN D. ROCKEFELLER, JR. Pinyon Peak e k 9705ft a n 2958m S C o u MEMORIAL PARKWAY lte r No trailers or large RVs Creek on one-lane portion eek Steamboat Cr Mountain 7872ft 2399m Survey Peak 9277ft 2827m 89 a n o y err C z B r i e r e 191 k A 287 B a ek il re ey C o C ntant ek e r C C k l e w r O e re e C k Lizard k e Creek e r C m ri g ly il z P z ri G Jackson Lake N Overlook or th Bi BRIDGER-TETON NATIONAL FOREST S tch o u C re th ek N NYO k CA e B BB re it E C c W Arizona Island h Moose TETON WILDERNESS Arizona Cr ee Lake k 16mi 26km ON CANY ER OLT C Pilgrim Mountain IDAHO Moose Mountain 8274ft k 2522m ee WYOMING r 10054ft C rk 3064m o Leeks Marina F c Ranger Peak t ifi s c 11355ft E a a E P 3461m K MOOSE BASIN ek A Park Boundary re C L GRAND TETON im W r lg T A i W TER YON Colter Bay P O F N ALLS CA Colter Bay Village O C Visitor Center EA N Indian Arts Museum Grand View Point LA and Trailhead KE NATIONAL PARK 7327ft Cygnet Talus Lake 2233m Pond m y Eagles Rest Peak 4 a N B Swan 6 r 11258ft e 0 lt Lake 3431m O 2 o C LD Rolling Thunder Mountain ATI A M L S t A 10908ft North f K M Jackson Lake Lodge A E dger 3325m K 2 M Ba Cre o 7 Medical Clinic uth ek -
U-Th)/He and Fission Track Dating for a Comprehensive Thermochronological Analysis: Refining the Uplift History of the Teton Range
Integrating apatite (U-Th)/He and fission track dating for a comprehensive thermochronological analysis: refining the uplift history of the Teton Range Summer Jasmine Brown Thesis submitted to the faculty of the Virginia Polytechnic Institute and State University in partial fulfillment of the requirements for the degree of Master of Science In Geosciences James A. Spotila Richard D. Law Jefferey M. Rahl 04/29/2010 Blacksburg, Virginia Keywords: Teton Range, apatite, thermochronometry, exhumation Integrating apatite (U-Th)/He and fission track dating for a comprehensive thermochronological analysis: refining the uplift history of the Teton Range Summer Jasmine Brown ABSTRACT Uplift of the Teton Range is primarily controlled by displacement across the range-front Teton normal fault. The Tetons comprise the footwall block while the hanging wall encompasses Jackson Hole valley and a portion of the Snake River. Relative to the rest of the Rocky Mountains, the Tetons experienced the majority of uplift very recently, substantiating the need for a detailed investigation integrating structural analysis and bedrock thermochronometry. New low-temperature cooling ages are documented in three vertical transects across the Teton Range and at low elevations parallel to the Teton fault. Samples adjacent to the Teton fault are consistently young (~9 Ma) and represent a minimum estimate for the onset of Teton fault-related uplift. Modeling of time-temperature histories supports a ~9-11 Ma onset of rapid uplift, indicating that the Teton fault likely originated as a Basin and Range-type structure. A maximum throw of ~8 km occurs proximal to the Grand Teton, while the average throw for the entire ~100 km along-strike fault length is ~3.3 km. -
East Face of Thor Peak
East Face of Thor Peak R ic h a r d Po w n a l l F EW of the many mountaineers who frequent the Teton Range know or have heard of Thor Peak, a mountain rising to an ele vation of 12,018 feet, located at the head of Leigh Canyon and par tially hidden by the massive southeast shoulders of Mount Moran (12,594 ft). Were this peak more accessible, it would be one of the major climbs in the range. Because of its remoteness, it has escaped the notice of mountaineers. During the summer of 1949, Mike Brewer and I, while we were guiding1 on Mount Moran, noticed this handsome peak with an alluring east wall rising very sheer from a small glacier. We were immediately aware that we had found an unnoticed face which looked to be a very challenging climb. On checking the mountaineer ing files at the headquarters of Grand Teton National Park, we found no official record of an ascent on Thor Peak, though we were certain that the peak had been climbed. We were fairly certain, how ever, that the massive east wall had not been ascended. Here, we believed, was one of the last major first ascents remaining in this region. It was not until 18 July 1950 that Mike and I were able to make an attempt on the face. We set out from Mountaineering Headquarters at Jenny Lake at 6.00 A.M., crossed Leigh Lake in Mike’s fold-boat, and started bushwhacking up Leigh Canyon. We were travelling lightly, with a minimum of food and climbing gear.