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Systematic Variation of Late Pleistocene Fault Scarp Height in the Teton Range, Wyoming, USA: Variable Fault Slip Rates Or Variable GEOSPHERE; V
Research Paper THEMED ISSUE: Cenozoic Tectonics, Magmatism, and Stratigraphy of the Snake River Plain–Yellowstone Region and Adjacent Areas GEOSPHERE Systematic variation of Late Pleistocene fault scarp height in the Teton Range, Wyoming, USA: Variable fault slip rates or variable GEOSPHERE; v. 13, no. 2 landform ages? doi:10.1130/GES01320.1 Glenn D. Thackray and Amie E. Staley* 8 figures; 1 supplemental file Department of Geosciences, Idaho State University, 921 South 8th Avenue, Pocatello, Idaho 83209, USA CORRESPONDENCE: thacglen@ isu .edu ABSTRACT ously and repeatedly to climate shifts in multiple valleys, they create multi CITATION: Thackray, G.D., and Staley, A.E., 2017, ple isochronous markers for evaluation of spatial and temporal variation of Systematic variation of Late Pleistocene fault scarp height in the Teton Range, Wyoming, USA: Variable Fault scarps of strongly varying height cut glacial and alluvial sequences fault motion (Gillespie and Molnar, 1995; McCalpin, 1996; Howle et al., 2012; fault slip rates or variable landform ages?: Geosphere, mantling the faulted front of the Teton Range (western USA). Scarp heights Thackray et al., 2013). v. 13, no. 2, p. 287–300, doi:10.1130/GES01320.1. vary from 11.2 to 37.6 m and are systematically higher on geomorphically older In some cases, faults of known slip rate can also be used to evaluate ages landforms. Fault scarps cutting a deglacial surface, known from cosmogenic of glacial and alluvial sequences. However, this process is hampered by spatial Received 26 January 2016 Revision received 22 November 2016 radionuclide exposure dating to immediately postdate 14.7 ± 1.1 ka, average and temporal variability of offset along individual faults and fault segments Accepted 13 January 2017 12.0 m in height, and yield an average postglacial offset rate of 0.82 ± 0.13 (e.g., Z. -
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. -
Saddle and Pack Stock
National Park Service Grand Teton U.S. Department of Interior Grand Teton National Park John D. Rockefeller, Jr. Memorial Parkway Saddle and Pack Stock Horses and other stock have been historically used in the park and parkway. “Stock” is defned as horses, burros, mules, and llamas. Goats are not permitted due to the sensitivity of the local bighorn sheep population. Stock users share trails with hikers— please be considerate of other trail users. Many trails are rocky and traverse steep terrain. High country trails may remain blocked by snow and impassable to stock until late July. Please refrain from accessing trails that are overly muddy. Check with the park permits ofce 307-739-3309 prior to setting out. Many horse travelers camp in the adjoining national forest land and take day rides in the park. The primary trailheads for day use are: • Cathedral Group Turnout • Poker Flats Trailhead • Taggart Lake Trailhead Camping Backcountry Camping with Stock Stock Campsites Accessible by Vehicle Backcountry camping with stock is allowed only at There are eight camping areas with a total of 14 sites the fve designated stock sites in the park. Fires are not that allow stock in the John D. Rockefeller, Jr. Memorial allowed and a backcountry camping permit is required. Parkway along the unpaved road between Flagg Ranch The sites may be reserved in advance from early-January and Grassy Lake. The road is closed until June 1 for to mid-May through www.recreation.gov; the reservation grizzly bear migration. Park campgrounds prohibit stock. fee is $35. The fee for walk-in permits, available up to one day in advance, is $25. -
Grand Teton U.S
National Park Service Grand Teton U.S. Department of Interior Grand Teton National Park John D. Rockefeller, Jr. Memorial Parkway Saddle and Pack Stock Horses and other stock have been historically used in the park and parkway. “Stock” is defined as horses, burros, mules and llamas. Goats are not permitted due to the sensitivity of the local bighorn sheep population. Stock users share trails with hikers— please be considerate of other trail users. Many trails are rocky and traverse steep terrain. High country trails may remain blocked by snow and impassable to stock until late July. Please refrain from accessing trails that are overly muddy. Check with the park permits office (307) 739-3309 prior to setting out. Many horse travelers camp in the adjoining national forest land and take day rides in the park. The primary trailheads for day use are: • String and Leigh Lake Trailheads • Poker Flats Trailhead • Taggart Lake Trailhead Camping Backcountry Camping with Stock Stock Campsites Accessible by Vehicle Backcountry camping with stock is allowed only at There are eight camping areas with a total of 14 sites the five designated stock sites in the park. Fires are not that allow stock in the John D. Rockefeller, Jr. Memorial allowed and a backcountry camping permit is required. Parkway along the unpaved road between Flagg Ranch The sites may be reserved in advance from early-January and Grassy Lake. Obtain a permit for $2 after June 1 at the to mid-May through www.recreation.gov; the reservation Colter Bay Permits Office or the Craig Thomas Discovery fee is $35. -
Deglaciation and Postglacial Environmental Changes in the Teton Mountain Range Recorded at Jenny Lake, Grand Teton National Park, WY
Quaternary Science Reviews 138 (2016) 62e75 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Deglaciation and postglacial environmental changes in the Teton Mountain Range recorded at Jenny Lake, Grand Teton National Park, WY * Darren J. Larsen , Matthew S. Finkenbinder, Mark B. Abbott, Adam R. Ofstun Department of Geology and Environmental Science, University of Pittsburgh, Pittsburgh, PA 15260, USA article info abstract Article history: Sediments contained in lake basins positioned along the eastern front of the Teton Mountain Range Received 21 September 2015 preserve a continuous and datable record of deglaciation and postglacial environmental conditions. Here, Received in revised form we develop a multiproxy glacier and paleoenvironmental record using a combination of seismic 19 February 2016 reflection data and multiple sediment cores recovered from Jenny Lake and other nearby lakes. Age Accepted 22 February 2016 control of Teton lake sediments is established primarily through radiocarbon dating and supported by Available online xxx the presence of two prominent rhyolitic tephra deposits that are geochemically correlated to the widespread Mazama (~7.6 ka) and Glacier Peak (~13.6 ka) tephra layers. Multiple glacier and climate Keywords: fl Holocene climate change indicators, including sediment accumulation rate, bulk density, clastic sediment concentration and ux, fl d13 d15 Lake sediment organic matter (concentration, ux, C, N, and C/N ratios), and biogenic silica, track changes in Western U.S. environmental conditions and landscape development. Sediment accumulation at Jenny Lake began Deglaciation centuries prior to 13.8 ka and cores from three lakes demonstrate that Teton glacier extents were greatly Grand Teton National Park reduced by this time. -
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. -
Structural Geology and History of the Buck Mountain Fault and Adjacent
Structural geology and history of the Buck Mountain fault and adjacent intra-range faults, Teton Range, Wyoming by Daniel Joseph Smith A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences Montana State University © Copyright by Daniel Joseph Smith (1991) Abstract: The Teton Range in northwestern Wyoming lies on the western margin of Laramide basement-involved deformation in the Rocky Mountain foreland. The study area is located in the central Teton Range and includes the high peaks of the range (the Cathedral Group) and several basement-involved deformation zones. The purpose of this study is to: 1) determine the geometry, kinematics and age of the Buck Mountain, Stewart and Static faults in the central Teton Range, and 2) to characterize post-Archean basement deformation in the Teton Range by examining mesoscopic and microscopic fabrics and alteration mineralogies in the study area. The north-striking Buck Mountain and northeast-striking Stewart faults exhibit brittle deformation including closespaced, unstable fractures and cataclasites. Slickenlines and drag folds indicate reverse dip-slip on the Buck Mountain fault. Both faults are interpreted to be Laramide on the basis of their basement-involved, contractional nature and brittle deformation. Static fault strikes northeast, dips steeply southeast and can be divided into two segments: 1) a southwest segment characterized by mylonitic rocks and exhibiting oriented chlorite, relict hornblende crystals, and rotated quartzo-feldspathic porphyroblasts (interpreted to be a Proterozoic phyllonite zone); and 2) a northeast segment that was reactivated by the Buck Mountain fault and exhibits brecciation and cataclasites. -
Grand Teton Loop Trail
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Grand Teton National Park
COMPLIMENTARY $3.95 2019/2020 YOUR COMPLETE GUIDE TO THE PARKS GRAND TETON NATIONAL PARK ACTIVITIES • SIGHTSEEING • DINING • LODGING TRAILS • HISTORY • MAPS • MORE OFFICIAL PARTNERS T:5.375” S:4.75” WELCOME S:7.375” WelcomeT:8.375” to Grand Teton National Park, FUN FACTS SO TASTY EVERYONE WILL WANT A BITE. where the majestic Teton Range rises Established: The park was created in 1929 but impressively along the western edge of the only protected the Teton range and the glacial scenic valley known as Jackson Hole. lakes at its base. In 1950, the park grew to its Whether you’ve come to relax and current size when John D. Rockefeller, Jr. do- take in the view or to actively explore nated land protecting the valley floor. Grand Teton’s many offerings, you will be Land Area: Grand Teton spans just over rewarded with opportunities to get closer 310,000 acres, covering the Teton mountain to the region’s unique natural beauty, wild- range, glacial lakes and part of the Jackson Hole valley. life and human history. Highest Elevation: 13,770 feet. The National Park Service (NPS) pro- Plants and Animals: Grand Teton is a part tects Grand Teton National Park and its of the Greater Yellowstone Ecosystem and is natural and cultural resources. The NPS home to a variety of animal life, including ea- and its primary park concessioners—Grand gles, black and grizzly bears and bison. Fish Teton Lodge Company, Forever Resorts are plentiful in the park’s bodies of water, and the Flagg Ranch Company—work while various amphibians and reptiles share the habitat. -
H in an EMERGENCY What's So Special About Grand
Grand Teton National Park & John D. Rockefeller, Jr., Memorial Parkway Summer, 1994 TEEWINOT. Welcome to Grand Teton National Park I hope your visit to Grand Teton National Park, YOUR national park, is a memorable one. Enjoy the Park and its spectacular scenery and 1 /''.M wildlife. •OTJK -:>iff| 1 To learn about the park, stop at visitor centers, ' - ^ * . *, 1^. 1 YJ • ''yya&*A attend ranger-led activities or ask a ranger. My staff and I are committed to helping you ^^^ ^', . ^^T Bfli ^ jz*^% '* have a safe and pleasant visit. ^?« ..'..:• r> Jack Neckels • <&. '- Superintendent fwrWSfmm^m^rWW^^' V Y %• ^.. .'"• ' "". ' ••*• t 'H- • • .. »'' 'f» • _j 4Ji IN AN EMERGENCY x **', (^H Call 911 View from the Cathedral Group Turnout on the Jenny Lake Scenic Drive or 739-3301 Park Dispatch International Visitors Des renseignements en francais sont disponibles aux centres des visiteurs dans le pare. What's So Special About Grand Teton National Park? Sie konnen Informationen auf Deutsch in den Besucherzentren bekommen. "... the range is most awe-inspiring, and yet at the same scenery and large concentrations of wildlife. Grand Se puede conseguir informacion en espanol en los time it has a mystical, entrancing beauty."—FritiofFryxell, Teton and the Rockefeller Parkway are adjacent to Centros de Visitantes. first ranger naturalist for Grand Teton National Park. Yellowstone National Park, and lie at the heart of the Greater Yellowstone Ecosystem. Being part of this Information in Hebrew and Japanese is also avail This is the most beautiful place I have ever been!"— ecosystem adds to the significance of Grand Teton able at park visitor centers. -
Moon Yellowstone & Grand Tetons 9Th Edition Index
420 Teton 188, 196, 203; Old Faithful and West cave: 308 421 Yellowstone 115; South Grand Teton 231, 252 Cave Falls: 196 Moon Yellowstone & Grand bobby socks trees: 101 Cave Falls Road: 197 Boiling River Hot Springs: 70 Celestine Pool: 95 Boy Scout Antler Auction: 271, 288 cell phones: 409 GRAND TET0N 9E YELLOWSTONE & Tetons 9th edition Index Bozeman: 393-394 Chain of Lakes: 153-155, 164; map 154 Bradley Lake: 236-238, 252, 254, 255; map 238 Chain of Lakes Trail: 164 INDEX Breccia Peak: 358 Chapel of the Transfiguration: 232 A Beauty Pool: 100 Beaver Pond Loop: 58 Bridge Bay: 161 Chico Hot Springs: 70 Absaroka-Beartooth Wilderness: 64 Bridger Gondola: 277 Chief Joseph Scenic Byway: 344 Bechler Falls: 196 INDEX Absaroka Mountains: 35, 57-58, 65 Bridger-Teton National Forest: 193-194, 202, 275, children, activities for: 234 Abyss Pool: 149, 172 Bechler Ranger Station: 196, 200 Bechler River: 196-197, 200 278, 280 children, traveling with: 410 accessibility: 409-410 YELLOWSTONE & Bechler River Trail: 113 Brink of the Lower Falls: 36, 144, 156 Chittenden Trail: 153 GRAND TET0N 9E Aerial Tram: 33, 273, 275, 277 Brink of the Upper Falls: 146, 156 Christian Pond: 197 air travel: 389, 393, 395, 396 Beck Lake Bike Park: 344 Beehive Basin: 319 Buffalo Bill Center of the West: 341 Chromatic Pool: 100 Alaska Basin: 306, 308 Buffalo Bill Dam: 343-344 Cirque Trail: 278 Albright Falls: 200 Beehive Geyser: 100 beer/breweries: Gateways 324; Jackson Hole 291, Buffalo Bill Museum: 341 Cistern Spring: 102 Albright Peak: 246 Buffalo Bill Reservoir: 346 Citizen