DOCSLIB.ORG

Ee Ee Eee Eee Eee Eeee Eeee Eeee Eee Eee

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Ee Ee Eee Eee Eee Eeee Eeee Eeee Eee Eee H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H H HHH H EEE H H E H H H H FREMONT PEAK NORTH QUADRANGLE H H EEEE H H H H WYOMING H United States Forest H H 7.5-MINUTE SERIES (TOPOGRAPHIC) H EEEE H H Department of Service H H 109°30'00" H H R H 32'30" 6 H 11142 EEEE 6 21 Agriculture 6 20 11200 11400 35'00" 728 6 618 19 616 17 43°15'00" H 109°37'30" 6 614000m E H 110006 13 H 12 H 10800 EEEE EE 9800 43°15'00" 10000 10200 801 11200 H R 105 W 105 R TRAIL 11600 W 106 R H H H EE 11000 11000 10600 9800 H 19 H 11807 R 19 H 24 R INK WELL 10846 H 11800 H 10800 23 H 728 22 EEE 10475 ½ R 10465 11000 21 ½ 9800 H H H H H H H H H 20 10600 10200 R 10150 47 4789 19 10800 89 10800 H H H H H H H H 11400 H 11200 H EEE 10000 DISTRICT 9980 11600 H R H H 11600 DISTRICT 10600 10400 9800 H 801 H 11200 11400 H H H H H EEE 12000 HH R 12065 H H H 728 H H H H 725 H H H H H 11800 H H H 10400 11400 HHH H 9600 HHH H H H HH TRAIL H H H H H 10400 11000 H H 10425 H H H H 10600 10400 H H 11400 1160011600 10000 Lake Native H 11200 H H 10800 Native Lake H H 47 4788 Klondike 11600 88 H H 11000 30 Lake 25 30 H R 11993 26 11000 27 9800 H 28 11000 10600 H 11215 29 Creek 10200 11800 H R 10170 11200 10200 H H 10860 H 10165 10600 30 R R I D G E 10000 H RANGER H H GLACIER H Klondike H R H 11030 9800 12000 RANGER 9800 H 10200 H H H H H H H 10600 H 10000 H Creek 11600 9800 H H H H H H H H 11400 801 H H H R H H H H H 11600 10800 H R H 11600 10800 H 4787000m N 10000 12210 4787 12200 H 11800 H 10145 H R 10400 10400 12165 11200 H 11400 10400 725 12000 12000 H H 10200 H 10800 11800 R 11835 11000 H H H Fourts 12000 H Moose Horn Lake H R 11165 H 11400 H 31 H R 31 11165 12015 35 36 11200 Dinwoody 34 11400 33 H H 32 12000 10000 10200 11600 H 31 11200 H WILD RIVER 726 10200 WASHAKIE 47 11400 47 10200 H H 86 86 H Creek 11000 H 12200 H O R S E 11000 10200 H H 10600 H GG Meadows S H O S H O N E R 11005 10600 H 11800 12000 10400 T 38 N R 11310 T 38 N H 10400 10400 H H 11600 T 37 N T 37 N H 10600 R R H H T 38 N T 38 N R 11755 Wilson 11600 10445 11183 R 12320 11400 H H T 37 N H T 37 N 12000 Don 725 10400 11600 H H H Lake H 10800 H H H H 11800 HH HH HH 10475 H H GG 12200 10600 11200 H 11000 H H H 12'30" H 4785 TRAIL Cub 4785 H 11400 10600 11000 H Dry Lake H 10400 10400 H H 12'30" H H H H H 10000 10200 H 10300 10000 H 10800 H 6 H Creek H 10400 11445 H 1 6 H H H 2 H Gannett H H 3 H 4 H 5 HH 6 H H R H HH 10495 GG 10285 H HHH H 10200 H H HH H H 10530 10400 H 11200 11800 H 11000 H H H 11200 10885 H H 11000 H R 12355 726 11400 H H H H H H 11600 10800 12400 H 47 H 47 H 84 H 84 12000 H H H 11200 F O R E S T 10200 GHGHGGGGGN A T I OGHG N A L 11800GHG 10000 H H 11000 11430 R 11400 H H H EEE 10670 H H 11600 12000 H 10800 12200 12035 H H R H H H EEE 11000 H 12600 11800 H H H 11200 H H 10800 11000 H R E H EE H H H H 11525 H H H H 12200 GLACIER H H H H H H 10800 GHGHGGGGGGGGHGGHG R 10600 12200 10800 10606 11200 H H H H 10695 H Noel 7 H H 7 H H 8 9 11 12 H 11400 Lake 12000 47 47 H 83 7 R 12706 10 83 12400 11000 11200 H 12165 11600 H 801 11400 H 11400 11800 11600 H 12800 12600 11600 H 11400 10800 13000 H GGGGGGGGGGGHGGHG H H H 10600 H R 12192 H 11600 H 10500 H 11800 11600 11000 H 11800 H H H 801 R H H 12700 11400 H 12000 F I T Z P A T R I C K R 13185 H H H H 12000 12800 H 12000 H H DISTRICT 10725 GHGHGGGGGGHGGHG12400 GGHGHG 47 13000 DISTRICT 47 H 82 82 H H 11800 H 12200 12400 H H 12600 11000 H 11600 12000 10800 11200 H 12200 11600 11400 13200 H 12800 H 12200 H 12000 11800 East Chimney 18 H 11075 11400 13 Sentinel GHGHGHGHGGGHGHGHHH R GGHGHG H 12400 R Rock 14 11632 16 15 H H H 12823 Heap Steep H H 12200 18 17 13400 RANGER 12000 13468 H Glacier R 12400 H RANGER H 11400 H 11800 H 12600 Mount H H Febbas H O R S E 11200 12600 H H H Heap Steep H H RIVER H 47 Blaurock H 47 H 81 Peak 81 D HH H Passs H H 12400 H I 12200 11800 H H 11600 N H 11600 GHGHGHW GHGGGHGHGHHGHGG GGG 13000 12200 O H 12600 H WASHAKIE 12800 12800 O Sunbeam WIND 12000 H D 12400 Peak H Y 12400 H G 13200 H 12600 L 12200 H A 12800 Creek 12600 Dry C 12600 R I D G E Ridge H 12200 H I W I L D E R N E S S 12400 12620 12600 10'00" H E Backpackers R R 12200 12200 12000 R H Pass 12282 12400 H H GHGHGHGHGHGGHGHGHHGHGG 10'00" Indian H H 12600 12000 H H 12800 Pass H 13200 12000 11400 11800 H H H 11800 H 12000 H 13200 H 47 13000 11200 11800 47 H 80 80 13400 11800 H H Elsie 11400 H 13722 Turret Cot H 19 H 13600 H H H Peak 24 22 23 11600 12200 H H 11000 H R 10800 H H 11400 H 11125 21 11600 H Doublet 20 13400 19 11200 Peak R 11400 H 10970 R GGGH13200 GHGH11200 GHGHGG 10600 Mount H 13000 11110 H 10715 11000 H Warren 11000 11800 H 10400 H H H 10800 10200 10800 10600 H 11200 11000 10400 9800 10600 H H 10000 H Helen Glacier R 10170 Lake 10800 H GGH47 GHGHGHGHGHGG 47 79 11000 79 North H H Creek H R 10750 12200 12000 11800 12600 H R 10800 11000 9800 H 12495 10200 12800 12200 H H Bull 12000 11400 12400 Fork H 10000 H 11525 10600 H 10000 H 12200 11200 9800 12600 10200 GGHGH12400 GHGHGHGHGHG H H H 11790 11200 10600 12086 H 10000 S FREMONT R 12000 30 10800 10895 25 R 11400 26 H 11600 27 H E 28 H I 29 10400 H FREMONT CO C 30 R 11385 A 000m 4778 11600 R 47 N H 11425 78 L 11800 10800 H H G 11200 10400 H T 10600 N 10400 10400 GGHH GHGHGHGHGHGHG H O H M Sacagawea Glacier H E 11400 12200 H R H F 11000 H 11800 1280012800 H 11000 H 12345 10600 R 10400 H 12200 12000 10200 R H 11485 GLACIERS 10400 12600 10185 H H 10800 GGHH GHGHGHGHGHGG 11000 R 12700 11200 R H R 13000 H 11400 H 47 10670 10600 47 77H 12400 12000 77 10800 H Mount H 12600 10725 10600 H Sacagawea 11800 11600 H 11400 H 13200H WIND 11530 10800 H 31 36 11000 34 10800 H GGHGHH GHGHGHGHGHG FREMONT 33 11200 10730 H 32 SUBLETTE 31 11400 H Lower Fremont H H 11400 10800 H RIVER 11600 35 R Glacier 11200 11145 Upper Fremont Glacier R 11715 H H H 11000 H 11200 11600 H CO H R 105 W 105 R R 106 W 106 R H 11200 CO H RANGE 12200 11400 H WASHAKIE H 11800 H H H 47 H 10790 47 BTNF H H 76 76 H GGGHPINEDALE 13200 GHGHGHGHGHGH 12200 R 12300 11600 PARALLEL NORTH 10743 T 37 N H H STANDARD H T 36 N H H H 11800 NINTH 11000 H H R 106 W 4 3 43°07'30" Femont T 37 N R 107 W 12000 5 6 H H T 37 N 6 22 RDH 6 H H 000m 21 H 1 H 6 6 BRIDGER WILD BRIDGER H H E T 36 N H H 6 19 20 Bull Lake Glacier 2 18 H Peak 6 11800 H 11400 109°30'00" T 36 N RD 3 6 17 H R 6 16 12200 11000 11200 H H 6 15 32'30" H H 43°07'30" H H 11400 6 14 10743 11400 6 13H 12 11000 H 35'00" H H H H H H H H H 109°37'30"H HIGHWAYS AND ROADS H H H H R 107 W 107 R R 106 R106 W H H H H H H H H H H H 5 H H H H H H GGHGHGHGHGHGH GGHH GG H Highway.............................................
Load more

Recommended publications
  • 1967, Al and Frances Randall and Ramona Hammerly
    The Mountaineer I L � I The Mountaineer 1968 Cover photo: Mt. Baker from Table Mt. Bob and Ira Spring Entered as second-class matter, April 8, 1922, at Post Office, Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during March and April by The Mountaineers, P.O. Box 122, Seattle, Washington, 98111. Clubroom is at 719Y2 Pike Street, Seattle. Subscription price monthly Bulletin and Annual, $5.00 per year. The Mountaineers To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanent form the history and traditions of this region; To preserve by the encouragement of protective legislation or otherwise the natural beauty of North­ west America; To make expeditions into these regions m fulfill­ ment of the above purposes; To encourage a spirit of good fellowship among all lovers of outdoor life. EDITORIAL STAFF Betty Manning, Editor, Geraldine Chybinski, Margaret Fickeisen, Kay Oelhizer, Alice Thorn Material and photographs should be submitted to The Mountaineers, P.O. Box 122, Seattle, Washington 98111, before November 1, 1968, for consideration. Photographs must be 5x7 glossy prints, bearing caption and photographer's name on back. The Mountaineer Climbing Code A climbing party of three is the minimum, unless adequate support is available who have knowledge that the climb is in progress. On crevassed glaciers, two rope teams are recommended. Carry at all times the clothing, food and equipment necessary. Rope up on all exposed places and for all glacier travel. Keep the party together, and obey the leader or majority rule. Never climb beyond your ability and knowledge.
    [Show full text]
  • Wind/Big Horn Basin Plan Technical Memorandum
    WIND/BIG HORN BASIN PLAN TECHNICAL MEMORANDUM April 2, 2003 Subject: WIND RIVER RANGE GLACIERS Prepared By: Harold J. Hutson, P.E., P.G., BRS Engineering INTRODUCTION The Wind River Range of Wyoming is the headwaters of the three major drainage systems in the United States, the Wind-Missouri-Mississippi, Snake-Columbia, and Green-Colorado drainages. The range is also home to a total of 63 glaciers, covering 17 square miles, greater than the total of all other glaciers in the American Rockies at 12 square miles. Seven of the ten largest glaciers in the continental United States are located in the Wind River Range. Of the total area of glaciers in the Wind River Range, 77% by area are located in the Wind River drainages, with the remainder draining to the Green and Snake rivers. (Marston, et. al., 1991). Based upon a literature search of available documents relating to the glaciers in the Wind River Range, the glaciers have been retreating during recent times. Glaciers have been compared to natural reservoirs, which store water in the form of ice during cool periods both on an annual and long term climatological scale, and release water during warmer periods. The melt water from the glaciers contributes to the flow in the Wind River, and is thought to be important during late summer and early fall to supplement flows in the Wind River needed for irrigation and fisheries, and for the fulfillment of interstate water compacts. This report summarizes the results of the literature review, and addresses three potential scenarios for future impacts to the Wind River due to glacial changes.
    [Show full text]
  • Estimated Wind River Range (Wyoming, USA) Glacier Melt Water Contributions to Agriculture
    THE UNIVERSITY OF ALABAMA® University Libraries Estimated Wind River Range (Wyoming, USA) Glacier Melt Water Contributions to Agriculture Kyle Cheesbrough – University of Wyoming Jake Edmunds – University of Wyoming Glenn Tootle – University of Tennessee Greg Kerr – University of Wyoming Larry Pochup – University of Wyoming Deposited 10/17/2018 Citation of published version: Cheesbrough, K., Edmunds, J., Tootle, G., Kerr, G., Pochup, L. (2009): Estimated Wind River Range (Wyoming, USA) Glacier Melt Water Contributions to Agriculture. Remote Sensing, 1(4). DOI: https://doi.org/10.3390/rs1040818 © 2009 by the authors; licensee Molecular Diversity Preservation International, Basel, Switzerland. This work is licensed under a Creative Commons Attribution 4.0 International License. Remote Sens. 2009, 1, 818-828; doi:10.3390/rs1040818 OPEN ACCESS Remote Sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Estimated Wind River Range (Wyoming, USA) Glacier Melt Water Contributions to Agriculture Kyle Cheesbrough 1, Jake Edmunds 1, Glenn Tootle 2,*, Greg Kerr 1 and Larry Pochop 1 1 University of Wyoming, Department of Civil and Architectural Engineering, 1000 East University Avenue, Laramie, WY 82070, USA; E-Mails: [email protected] (K.C.); [email protected] (J.E.); [email protected] (G.K.); [email protected] (L.P.) 2 University of Tennessee, Department of Civil and Environmental Engineering, 223 Perkins Hall, Knoxville, TN 37996, USA * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-865-974-7777. Received: 4 September 2009; in revised form: 1 October 2009 / Accepted: 19 October 2009 / Published: 28 October 2009 Abstract: In 2008, Wyoming was ranked 8th in barley production and 20th in hay production in the United States and these crops support Wyoming’s $800 million cattle industry.
    [Show full text]
  • Nordic Hydrology, 25, 1994, 371-388 No Part May Be Reproduced by Any Process Wlthout Complete Rekrence
    Nordic Hydrology, 25, 1994, 371-388 No part may be reproduced by any process wlthout complete rekrence Assessment of Spatial Variability of Major-Ion Concentrations and DEL Oxygen-18 Values in Surface Snow, Upper Fremont Glacier, Wyoming, U.S.A. D. L. Naftz U.S. Geological Survey, Salt Lake City, UT 84104, U.S.A. P. F. Schuster and M. M. Reddy U.S. Geological Survey, Boulder, CO 80303, U.S.A. One hundred samples were collected from the surface of the Upper Fremont Glacier at equally spaced intervals defined by an 8,100 m 2 snow grid to assess the significance of lateral variability in major-ion concentrations and del oxy- gen-18 values. For the major ions, the largest concentration range within the snow grid was sodium (0.5056 mgll) and the smallest concentration range was sulfate (0.125 mgll). Del oxygen-18 values showed a range of 7.45 per mil. Comparison of the observed variability of each chemical constituent to the variability expected by measurement error indicated substantial lateral variab- ility within the surface-snow layer. Results of the nested ANOVA indicate most of the variance for every constituent is in the values grouped at the two smaller geographic scales (between 506 m2 and within 506 m2 sections). Cal- cium and sodium concentrations and del oxygen-18 values displayed the largest amount of variance at the largest geographic scale (between 2,025 m 2 sections) within the grid and ranged from 14 to 26 per cent of the total variance. The variance data from the snow grid were used to develop equations to evaluate the significance of both positive and negative concentrationlvalue peaks of nitrate and del oxygen-18 with depth, in a 160 m ice core.
    [Show full text]
  • It Is an Honor to Receive the Kirk Bryan Award. I Am Especially Pleased To
    Quaternary Geologist & Geomorphologist Newsletter of the Quaternary Geology and Geomorphology Division http://rock.geosociety.org/qgg Spring 2004 Vol. 45, No.1 Glacial lake that drained from head of Grasshopper Glacier, northern Wind River Range, Wyoming, in October, 2003. View is to west. Lake drained beneath glacier to north, and flooded to north then east down the drainage of Grasshopper Creek, to Down’s Fork Creek, and to Dinwoody Creek. Outwash deposits along the Down’s Fork Creek where an ephemeral lake ponded at Down’s Fork Meadows near the confluence of the Down’s Fork and Dinwoody creeks. Dinwoody Lakes are seen at upper left. View is to east. (More details of this event inside on p. 2) Photos provided by Dennis Dahms, courtesy of Liz Oswald, South Zone Hydrologist, Shoshone National Forest, Lander, Wyoming 1 Cover: Jökulhlaup at Grasshopper Glacier, Wind River Mountains, Wyoming A jökulhlaup, or glacial outburst flood, burst from an ice-dammed lake at the head of the Grasshopper Glacier, Wind River Mountains, Wyoming, in early September this year. The 30-acre lake drained an estimated 850 million gallons of water downslope, underneath the glacier, and, charged with subglacial sediment, flooded tributary valleys and into the Dinwoody River valley. The event was recorded at the USGS gage site (USGS 06221400 Dinwoody Creek above Lakes, near Burris, WY) about 20 mi downstream from the ice-dammed lake. The Grasshopper Glacier is situated at the continental divide nested between high-level erosion surfaces and the eastward-facing cirque walls of the mountain front. The glacier, oriented south to north, drops from an elevation of 12,000 ft down a steep (0.11) slope to its snout at about 11,300 ft elevation.
    [Show full text]
  • Undigitized Photo Index
    People States-Towns-Countries General Subjects Railroad Companies Denver People Abeyta Family Abbott, Emma Abbott, Hellen Abbott, Stephen S. Abernathy, Ralph (Rev.) Abreu, Charles Acheson, Dean Gooderham Acker, Henry L. Adair, Alexander Adami, Charles and Family Adams, Alva (Gov.) Adams, Alva Blanchard (Sen.) Adams, Alva Blanchard (Mrs. Elizabeth Matty) Adams, Alva Blanchard Jr. Adams, Andy Adams, Charles Adams, Charles Partridge Adams, Frederick Atherton and Family Adams, George H. Adams, James Capen (―Grizzly‖) Adams, James H. and Family Adams, John T. Adams, Johnnie Adams, Jose Pierre Adams, Louise T. Adams, Mary Adams, Matt Adams, Robert Perry Adams, Mrs. Roy (―Brownie‖) Adams, W. H. Adams, William Herbert and Family Addington, March and Family Adelman, Andrew Adler, Harry Adriance, Jacob (Rev. Dr.) and Family Ady, George Affolter, Frederick Agnew, Spiro T. Aichelman, Frank and Family Aicher, Cornelius and Family Aiken, John W. Aitken, Leonard L. Akeroyd, Richard G. Jr. Alberghetti, Carla Albert, John David (―Uncle Johnnie‖) Albi, Charles and Family Albi, Rudolph (Dr.) Alda, Frances Aldrich, Asa H. Alexander, D. M. Alexander, Sam (Manitoba Sam) Alexis, Alexandrovitch (Grand Duke of Russia) Alford, Nathaniel C. Alio, Giusseppi Allam, James M. Allegretto, Michael Allen, Alonzo Allen, Austin (Dr.) Allen, B. F. (Lt.) Allen, Charles B. Allen, Charles L. Allen, David Allen, George W. Allen, George W. Jr. Allen, Gracie Allen, Henry (Guide in Middle Park-Not the Henry Allen of Early Denver) Allen, John Thomas Sr. Allen, Jules Verne Allen, Orrin (Brick) Allen, Rex Allen, Viola Allen William T. Jr. (Col.) Allison, Clay Allott, Gordon L. Allott, Gordon L. (Mrs. Welda Hall) Almirall, Leon V.
    [Show full text]
  • Chesseborough Thesis.Pdf
    Cheesbrough, Kyle S., Glacial Recession in Wyoming’s Wind River Range , M.S., Department of Civil and Architectural Engineering, December 2007 Abstract The Wind River Range (WRR), located in western Wyoming, is host to more than 60 glaciers making it the largest concentration of glaciers in the Rocky Mountain region. Several studies have been performed on the glaciers of the WRR, dating back to the 1930’s focusing on only the largest, most accessible glaciers such as Gannett and Dinwoody Glaciers. Each of the previous studies have documented the WRR glaciers as being in an overall receding trend since 1850, with some localized periods of advancement (Pochop et al., 1990). This study documents glacial surface area change, volume change and change in terminus position for 42 glacial complexes in the WRR from 1985 through 2005, through utilization of remote sensing techniques. The use of remote sensing techniques allows more of the glaciers in the WRR to be analyzed, rather than focusing on only the most geographically accessible glaciers. In addition to documenting the area changes since 1985 for all of the WRR glaciers, the changes in surface area and terminus position for nine selected glaciers was estimated from 1966 through 2001 using aerial photographs. It has been noted in previous studies that glaciers of smaller area are typically more sensitive to changes in climate than large glaciers (Granshaw & Fountain, 2006). Out of the 42 glacial complexes analyzed, 25 of them had an area of <0.5 km 2 in 1985, while the others were >0.5 km 2 in 1985.
    [Show full text]
  • 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.
    [Show full text]
  • Glacial Lake Reflectance As a Proxy for Changing Glacial Conditions and Impacts on Streamflow Lance Diangelis
    University of North Dakota UND Scholarly Commons Theses and Dissertations Theses, Dissertations, and Senior Projects January 2018 Glacial Lake Reflectance As A Proxy For Changing Glacial Conditions And Impacts On Streamflow Lance Diangelis Follow this and additional works at: https://commons.und.edu/theses Recommended Citation Diangelis, Lance, "Glacial Lake Reflectance As A Proxy For Changing Glacial Conditions And Impacts On Streamflow" (2018). Theses and Dissertations. 2400. https://commons.und.edu/theses/2400 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. GLACIAL LAKE REFLECTANCE AS A PROXY FOR CHANGING GLACIAL CONDITIONS AND IMPACTS ON STREAMFLOW by Lance Vincent DiAngelis Bachelor of Arts, University of Phoenix, 2011 Master of Science, University of Saint Francis, 2013 A Thesis Submitted to the Graduate Faculty Of the University of North Dakota In partial fulfillment of the requirements For the degree of Master of Science Grand Forks, North Dakota December 2018 PERMISSION Title Glacial Lake Reflectance as a Proxy for Changing Glacial Conditions and Impacts on Streamflow Department Earth System Science and Policy Degree Master of Science In presenting this thesis in partial fulfillment of the requirements for a graduate degree from the University of North Dakota, I agree that the library of this University shall make it freely available for inspection. I further agree that permission for extensive copying for scholarly purposes may be granted by the professor who supervised my thesis work or, in his absence, by the Chairperson of the department or dean of the School of Graduate studies.
    [Show full text]
  • The Fate of Dinwoody Glacier: Present State of Mass Balance and Downstream Impacts of Glacier Runoff
    THESIS THE FATE OF DINWOODY GLACIER: PRESENT STATE OF MASS BALANCE AND DOWNSTREAM IMPACTS OF GLACIER RUNOFF. Submitted by Brooke E. Stamper Graduate Degree Program in Ecology In partial fulfillment of the requirements For the Degree of Master of Science Colorado State University Fort Collins, Colorado Summer 2018 Master’s Committee: Advisor: Andrew K. Bliss Neil S. Grigg Steven R. Fassnacht Copyright by Brooke E. Stamper 2018 All Rights Reserved ABSTRACT THE FATE OF DINWOODY GLACIER: PRESENT STATE OF MASS BALANCE AND DOWNSTREAM IMPACTS OF GLACIER RUNOFF. The Wind River Range in Wyoming supports many of the few remaining continental glaciers of the North American Rocky Mountains; the glacier meltwater runoff feeds four major river sys- tems within the U.S. West. Runoff from glaciers affects downstream ecosystems by influencing the quantity, seasonality, and chemistry of the water. We describe the present state of Dinwoody Glacier, the fourth largest glacier in the Wind River Range. We utilize photogrammetry, snow depth measurements, and ablation measurements to characterize surface mass balance for summer of 2017. Localized and nearby stream gauge measurements help to quantify glacial meltwater runoff inputs to Dinwoody Creek. Both of these methods allowed us to put the changes of the Dinwoody Glacier into the broader context of the Missouri River Watershed. If melted, Dinwoody Glacier would no longer provide a reliable source of melt water for thousands of people living in the Missouri River Watershed. Understanding how shrinking glaciers and decreasing melt-water runoff will impact communities and ecosystems downstream is critical for effective environmental management. The response of the Wind River glaciers to future climate is uncertain; however, past research has shown declines in glacial mass, snow cover, snowmelt timing and stream power.
    [Show full text]
  • Biography Denver General Subject Railroads States and Cities Misc
    Biography Denver General Subject Railroads States and Cities Misc. Visual Materials BIOGRAPHY A Abeyta family Abbott, Emma Abbott, Hellen Abbott, Stephen S. Abernathy, Ralph (Rev.) Abot, Bessie SEE: Oversize photographs Abreu, Charles Acheson, Dean Gooderham Acker, Henry L. Adair, Alexander Adami, Charles and family Adams, Alva (Gov.) Adams, Alva Blanchard (Sen.) Adams, Alva Blanchard (Sen.) (Adams, Elizabeth Matty) Adams, Alva Blanchard Jr. Adams, Andy Adams, Charles Adams, Charles Partridge Adams, Frederick Atherton and family Adams, George H. Adams, James Capen (“Grizzly”) Adams, James H. and family Adams, John T. Adams, Johnnie Adams, Jose Pierre Adams, Louise T. Adams, Mary Adams, Matt Adams, Robert Perry Adams, Mrs. Roy (“Brownie”) Adams, W. H. SEE ALSO: Oversize photographs Adams, William Herbert and family Addington, March and family Adelman, Andrew Adler, Harry Adriance, Jacob (Rev. Dr.) and family Ady, George Affolter, Frederick SEE ALSO: oversize Aichelman, Frank and Agnew, Spiro T. family Aicher, Cornelius and family Aiken, John W. Aitken, Leonard L. Akeroyd, Richard G. Jr. Alberghetti, Carla Albert, John David (“Uncle Johnnie”) Albi, Charles and family Albi, Rudolph (Dr.) Alda, Frances Aldrich, Asa H. Alexander, D. M. Alexander, Sam (Manitoba Sam) Alexis, Alexandrovitch (Grand Duke of Russia) Alford, Nathaniel C. Alio, Giusseppi Allam, James M. Allegretto, Michael Allen, Alonzo Allen, Austin (Dr.) Allen, B. F. (Lt.) Allen, Charles B. Allen, Charles L. Allen, David Allen, George W. Allen, George W. Jr. Allen, Gracie Allen, Henry (Guide in Middle Park-Not the Henry Allen of Early Denver) Allen, John Thomas Sr. Allen, Jules Verne Allen, Orrin (Brick) Allen, Rex Allen, Viola Allen William T.
    [Show full text]
  • Glaciers of North America—
    Glaciers of North America— GLACIERS OF THE CONTERMINOUS UNITED STATES GLACIERS OF THE WESTERN UNITED STATES By ROBERT M. KRIMMEL With a section on GLACIER RETREAT IN GLACIER NATIONAL PARK, MONTANA By CARL H. KEY, DANIEL B. FAGRE, and RICHARD K. MENICKE SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–2 Glaciers, having a total area of about 580 km2, are found in nine western states of the United States: Washington, Oregon, California, Montana, Wyoming, Colorado, Idaho, Utah, and Nevada. Only the first five states have glaciers large enough to be discerned at the spatial resolution of Landsat MSS images. Since 1850, the area of glaciers in Glacier National Park has decreased by one-third CONTENTS Page Abstract ---------------------------------------------------------------------------- J329 Introduction----------------------------------------------------------------------- 329 Historical Observations -------------------------------------------------------- 330 FIGURE 1. Historical map of a part of the Sierra Nevada, California ------ 331 2. Early map of the glaciers of Mount Rainier, Washington------- 332 Glacier Inventories -------------------------------------------------------------- 332 Mapping of Glaciers------------------------------------------------------------- 333 TABLE 1. Areas of glaciers in the western conterminous United States -- 334 Landsat Images of the Glaciers of the Western United States--------- 335 FIGURE 3. Temporal
    [Show full text]