December 1987 #73
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Interest and the Panamint Shoshone (E.G., Voegelin 1938; Zigmond 1938; and Kelly 1934)
109 VyI. NOTES ON BOUNDARIES AND CULTURE OF THE PANAMINT SHOSHONE AND OWENS VALLEY PAIUTE * Gordon L. Grosscup Boundary of the Panamint The Panamint Shoshone, also referred to as the Panamint, Koso (Coso) and Shoshone of eastern California, lived in that portion of the Basin and Range Province which extends from the Sierra Nevadas on the west to the Amargosa Desert of eastern Nevada on the east, and from Owens Valley and Fish Lake Valley in the north to an ill- defined boundary in the south shared with Southern Paiute groups. These boundaries will be discussed below. Previous attempts to define the Panamint Shoshone boundary have been made by Kroeber (1925), Steward (1933, 1937, 1938, 1939 and 1941) and Driver (1937). Others, who have worked with some of the groups which border the Panamint Shoshone, have something to say about the common boundary between the group of their special interest and the Panamint Shoshone (e.g., Voegelin 1938; Zigmond 1938; and Kelly 1934). Kroeber (1925: 589-560) wrote: "The territory of the westernmost member of this group [the Shoshone], our Koso, who form as it were the head of a serpent that curves across the map for 1, 500 miles, is one of the largest of any Californian people. It was also perhaps the most thinly populated, and one of the least defined. If there were boundaries, they are not known. To the west the crest of the Sierra has been assumed as the limit of the Koso toward the Tubatulabal. On the north were the eastern Mono of Owens River. -
SMC-Guide-To-Mt-Sill-1.Pdf
Introduction The Swiss Arete Of Mount Sill -THEPALISADES Mount Sill is an impressive mountain, its cuboid mass looks large even from Highway 395. The original L Approach to Mount Sill 1 inhabitants of the Eastern Sierra called it “Ninamishi” or Guardian Of The Valley and it is clear why once O you have viewed it from the Owens Valley. Even close up, although its summit is lower than some of the N Glacier Trail E neighboring 14,000ft peaks, it still looks the tallest. The first technical climb up Mount Sill was the “Starr Route” climbed by ?????? in (first actual ascent), this the descent route if you are doing any of the P Sam Mack Second “modern’ routes on Mount Sill. Mount Meadow Third Lake Lake I Robinson 10,400ft 6 miles from N 12,967ft Glacier Lodge First ascent details... E trail turns to B The Swiss Arete up the north face of Mount Sill is a classic mountaineering challenge. You will enjoy a Mount Agassiz talus hopping I 13,893ft Sam Mack beautiful hike, a glacial experience, will have to cope with high-altitude and then you will be one with the Lake Temple 1. On the glacier trail beyond Sam Mack Crag S rocky ridge of the Palisades that contain seven of the fifteen 14,000ft peaks in California. Good rock and Meadow en route to Mount Sill. H moraine 12,999ft an exceptional summit experience with great views are the icing on the cake. O 12,165ft P 2 The approach from the trailhead is 10 miles (a round trip of 20 miles) with a total elevation gain of 6,353- Thunderbolt glacier lake O Glacier Mount feet, of which 1,000-foot is 4th and easy 5th class rock climbing with a obligatory moves of 5.6 and 5.7 at loose cliff Gayely W Mount MOVE QUICKLY the distinct crux. -
Mcgee Creek BCM Course Area Guide Backcountry
McGee Creek BCM Course Area Guide Backcountry Trip Code ________________________ Team Leader ________________________ Table of Contents Trail Summary ...................................................... 3 Trail Information .............................................................. 3 Trail Description .............................................................. 4 Route Description............................................................ 5 Trail Distances ................................................................ 5 Trail Elevation Profile ...................................................... 5 Map ....................................................................... 6 Key to Trail Map.................................................... 8 Camp Site Information .................................................... 8 Map Legend .................................................................... 9 Hazards ........................................................................... 9 Recommended Destinations ......................................... 10 Fishing ........................................................................... 10 Summits ........................................................................ 11 Daily Outline ....................................................... 12 Curriculum Checklist ........................................... 13 Team Leader Recommendations ....................... 14 Team Leader Comments .............................................. 14 Team Leader Feedback Form ..................................... -
Environmental Records in a High-Altitude Low-Latitude Glacier, Sierra Nevada, California" (2006)
Western Washington University Western CEDAR WWU Graduate School Collection WWU Graduate and Undergraduate Scholarship Winter 2006 Environmental Records in a High-Altitude Low- Latitude Glacier, Sierra Nevada, California Alison J. (Alison Jane) Gillespie Western Washington University Follow this and additional works at: https://cedar.wwu.edu/wwuet Part of the Geology Commons Recommended Citation Gillespie, Alison J. (Alison Jane), "Environmental Records in a High-Altitude Low-Latitude Glacier, Sierra Nevada, California" (2006). WWU Graduate School Collection. 794. https://cedar.wwu.edu/wwuet/794 This Masters Thesis is brought to you for free and open access by the WWU Graduate and Undergraduate Scholarship at Western CEDAR. It has been accepted for inclusion in WWU Graduate School Collection by an authorized administrator of Western CEDAR. For more information, please contact [email protected]. ENVIRONMENTAL RECORDS IN A HIGH-ALTITUDE LOW-LATITUDE GLACIER, SIERRA NEVADA, CALIFORNIA By Alison J. Gillespie Accepted in Partial Completion of the Requirements for the Degree Master of Science Moheb A Ghali, Dean of the Graduate School ADVISORY COMMITTEE Dr. Scott Babcock ENVIRONMENTAL RECORDS IN A HIGH-ALTITUDE LOW-LATITUDE GLACIER, SIERRA NEVADA, CALIFORNIA A Thesis Presented to The Faculty of Western Washington University In Partial Fulfillment Of the Requirements for the Degree Master of Science by Alison J. Gillespie February 2006 MASTER'S THESIS In presenting this thesis in partial fulfillment of the requirements for a master's degree at Western Washington University, I grant to Western Washington University the non-exclusive royalty-free rightto archive, reproduce, distribute, and display the thesis in any and all forms, including electronic format, via any digital library mechanisms maintained by WWU. -
The Ohio State University Research Foundation
RF Project 1227 Final Report THE OHIO STATE UNIVERSITY RESEARCH FOUNDATION 1314 KINNEAR ROAD COLUMBUS 12, OHIO i'iAPPIIm GLACIERS IN llESTERN UNITED STATES Dr. Arthur J. Brandenberger Department of Geodetic Science January 1962 National Sc i ence Foundation Grant No. NSF-G15997 RF Project 1227 FINAL REPORT by THE OHIO STATE UNIVERSITY RESEARCH FOUNDATION 1314 Kinnear Road Columbus 12, Ohio To NATIONAL SCIENCE FOUNDATION Washington 25, D. C. On MAPPING GLACIERS IN WESTERN UNITED STATES Burroughs Glacier Dinwoody Glacier Palisade Glacier Grant No. NSF- Gl 5997 (Successor to RF Project 943) For the period 21 December 1960 - 31 December 1961 Submitted by Dr. Arthur J. Brandenberger Project Supervisor Department of Geodetic Science Date January 1962 FOREWORD This report was prepared by Dr. Arthur J. Brandenberger, Project Supervisor, Department of Geodetic Science and The Institute of Polar Studies of The Ohio State University, und~r National Science Foundation Grant No. NSF - G15997, OSURF Project. No. 1227. The grant is administered under the dire,ction of Dr. Alan T. Waterman, Director, National Science Foundation. OSURF Project No. 1227 covers rellearch pe;rformed by, Dr,. Arthur J. Brandenberge;r, Project supervisor,; Dr. James B. Case" Mr. O. M. Miller, Mr. Sanjib K. Ghosh, Mr. Robert B. Forrest, Miss M. W. Hindman, Research Associates, and Mr. Peter Wilson, Research ASSistant, of The Department of Geodetic Science, The Ohio State University. A portion of this report, covers results reported in detail in the Final Report of RF Project No. 943, prepared by Dr. James B. Case. 11 ABSTRACT The subject of this research is the preparation of photogrammetric maps of the BurrougAs Glacier in Alask~, the Dinwoody Glacier in ~yoming and 'the Palisade Glacier in California. -
Prepared by Participants in December 1988 This Report Is Preliminary And
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY NATIONAL EARTHQUAKE HAZARDS REDUCTION PROGRAM, SUMMARIES OF TECHNICAL REPORTS VOLUME XXVII Prepared by Participants in NATIONAL EARTHQUAKE HAZARDS REDUCTION PROGRAM December 1988 OPEN-FILE REPORT 88-673 This report is preliminary and has not been reviewed for conformity with U.S.Geological Survey editorial standards Any use of trade names is for descriptive purposes only and does not imply endorsement by the USGS. Menlo Park, California 1988 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY NATIONAL EARTHQUAKE HAZARDS REDUCTION PROGRAM, SUMMARIES OF TECHNICAL REPORTS VOLUME XXVII Prepared by Participants in NATIONAL EARTHQUAKE HAZARDS REDUCTION PROGRAM Compiled by Muriel L. Jacobson The research results described in the following summaries were submitted by the investigators on October 15, 1988 and cover the period from May 1, 1988 through October 1, 1988. These reports include both work performed under contracts administered by the Geological Survey and work by members of the Geological Survey. The report summaries are grouped into the five major elements of the National Earthquake Hazards Reduction Program. Open File Report No. 88-673 This report has not been reviewed for conformity with USGS edi torial standards and stratigraphic nomenclature. Parts of it were prepared under contract to the U.S. Geological Survey and the opinions and conclusions expressed herein do not necessarily represent those of the USGS. Any use of trade names is for descriptive purposes only and does not imply endorsement by the USGS. The data and interpretations in these progress reports may be reevaluated by the investigators upon completion of the research. -
SWS Mountain Guides Palisades Mountaineering Camp I
SWS Mountain Guides 210 East Lake St. Mt. Shasta, Ca. 96067 [email protected] www.swsmountainguides.com Phone: 888.797.6867 / Fax: 877.797.6867 Palisades Mountaineering Camp I Basic Alpine Mountaineering Course with Summit Climbs The Palisades in the Eastern Sierra Nevada General Description: This course is a comprehensive introduction to alpine climbing, with an emphasis on the tools and techniques used in rock and ice and snow climbing. Topics to be covered: trip planning and preparation, route finding, map use, altimeter and compass use in navigation and route finding, an introduction to the technical equipment used in climbing (harnesses, ropes, and hardware), basic rock climbing techniques, anchor systems, belaying and rappelling. Presentation and instruction in the use of ice ax and crampons in snow and ice, self-arrest, self-belay and snow and ice protection hardware and anchors, roped team and glacier travel, glissading, physical hazards, mountain medicine, and more! Guide to client ratio is 1:4 to ensure individual attention. Location: Big Pine, California, Palisade Glacier, Eastern Sierra Nevada. Itinerary: After meeting at 8:00 am on the first day we will hike to a camp at approximately 11,000 ft; informal lectures will take place along the trail. Day two will be devoted to rock climbing instruction (equipment, technique, rappelling, etc.) at a nearby crag. On day three we will travel to a higher camp above the snowline, with the time dedicated to introducing you to ice ax and crampon use, ice and snow techniques (self-arrest, roped team travel, anchors, protection systems, and crevasse rescue). -
To Download the 2018 Inyo County
VISITOR’S GUIDE TO IINNYYOOCCOOUUNNTTYY 11 TH EDITION www.TheOtherSideOfCalifornia.com Table of Contents Chamber of Commerce of Inyo County Birds Come Back to Owens Lake Page 4 Bishop Chamber of Commerce & Borax Wagons Find A New Home Page 6 Visitor Center 690 N. Main St. Bishop, CA 93514 Enchanting Fall Colors Page 8 760-873-8405 1-888-395-3952 760-873-6999 Enjoy Bishop’s Big Backyard Page 10 [email protected] www.bishopvisitor.com Appealing Adventures in Lone Pine Page 11 Death Valley Chamber of Commerce 118 Highway 127 Everyone Loves A Parade Page 12 P.O. Box 157 Shoshone, CA 92384 760-852-4524 Historic Independence Page 14 760-852-4144 www.deathvalleychamber.org Direct Results Media, Inc. Direct ResultsLone Media, Pine Inc. Big Pine: An Adventure Hub Page 15 Chamber of Commerce 124 Main St BusinessPO B oCardsx 749 Inyo County Fun Facts Page 16 Lone Pine, CA 93545 Rodney Preul Ph: 760-876-4444 Fx: 760-876-9205 Sales Associate Owens River Links LA And Inyo Page 17 [email protected] https://w3.5x2ww.lonepinechamber.org Inyo Attractions At A Glance Page 19 6000 Bel Aire Way Cell: 760-382-1640 Bakersfield, CA 93301 [email protected] The 2018 Inyo County Visitor Guide is produced by the Lone Pine Chamber of Government Agencies: Commerce and the County of Inyo. The Bureau of Land Management (BLM) contents do not necessarily reflect the views 760-872-4881 of the Lone Pine Chamber of Commerce or the County of Inyo. (Except for our view that Inyo County is a spectacular place to visit. -
Water Quality Analysis of the North Palisade Glacier Sierra Nevada Mountians, California
SENIOR THESIS Water Quality Analysis of the North Palisade Glacier Sierra Nevada Mountians, California by Eathan McIntyre Prepared for Dr. Jeff Marshall – Thesis Advisor Department of Geological Sciences Cal Poly Pomona University November 29, 2007 Cal Poly Pomona University 3801 W. Temple Avenue Pomona, California 91768 Water Quality Analysis of North Palisade Glacier TABLE OF CONTENTS SECTION PAGE 0.0 ABSTRACT .................................................................................................................0-1 1.0 INTRODUCTION........................................................................................................1-1 2.0 GLACIER DESCRIPTION .........................................................................................2-1 2.1 Physiography........................................................................................................2-1 2.2 Dynamics and Kinematics ...................................................................................2-2 2.3 Geologic History..................................................................................................2-3 3.0 PREVIOUS WORKS..................................................................................................3-1 3.1 Publications..........................................................................................................3-2 4.0 SAMPLE METHODS .................................................................................................4-1 4.1 Survey and Quality Control Activities.................................................................4-2 -
Easternsierra Copy
TEMPLE CRAG THE PALISADES Venusian Blind Arete - 5.7 Moon Goddess Arete - 5.8 Sun Ribbon Arete - 5.10 The Sierra Nevada By MOUNT SILL Robert “SP” Parker, The Swiss Arete - 5.6 Todd Vogel And POLEMONIUM PEAK Andy Hyslop U - Notch - WI3 V - Notch -WI3+ Photo caption right photographer Introduction THEPALISADES Although Mount Whitney is the highest peak, the Palisades is the Big Pine To Glacier Lodge Trailhead 15 miles L throne room of the Sierra Nevada. The Palisades, named by the south of O N Brewer party of the Whitney Survey in 1864, are home to seven of Lee Vining BIG PINE Bishop 120 4,000 ft E California's 14,000ft peaks and some of the regions finest alpine 120 food climbing. The Palisades are situated east of the town of Big Pine accomodation June The White Mountains beer P and are approached from Glacier Lodge trailhead by two narrow Lake North Fork of Big Pine Creek I and dramatic glacier-carved canyons following trails that zigzag To Palisades North Crocker N through slopes of sage, manzanita, and Jeffrey Pine to emerge in MAMMOTH 6 (6 miles to Temple Crag) Street E LAKES The Sierra Nevada an alpine wonderland. In summer the flowers by these pine- B shaded trails are abundant and kaleidoscopic. BISHOP Glacier Lodge Road I 168 395 S 168 The Palisade is a complex area of milky turquoise lakes fed by First Falls over-night H Big Pine parking O glaciers, lofty peaks and passes, deep gullies, hanging basins, Glacier (walk-in) day use The Palisades Lodge The Inyo P sunlight ridges, blocky talus slopes, turrets and towers capped by Mountains parking P a blue sky that is often interrupted by rushing clouds. -
Mono County Community Development Department P.O
Mono County Community Development Department P.O. Box 347 Planning Division P.O. Box 8 Mammoth Lakes, CA 93546 Bridgeport, CA 93517 (760) 924-1800, fax 924-1801 (760) 932-5420, fax 932-5431 [email protected] www.monocounty.ca.gov March, 2007 UPPER OWENS RIVER BASIN 1. Introduction Watershed approach California watershed programs and Mono County’s involvement What is a watershed assessment? Publicly perceived problems and issues Water quantity Water quality Aquatic habitat Recreation Wildfire Invasive species List of assorted issues Publicly perceived key resources Driving questions Watershed boundaries 2. Descriptive geography Climate Precipitation Snowpack Air temperature Wind Evaporation Topography Geology Soils Upland vegetation Wildfire history and risk Planning / Building / Code Compliance / Environmental / Collaborative Planning Team (CPT) Local Agency Formation Commission (LAFCO) / Local Transportation Commission (LTC) / Regional Planning Advisory Committees (RPACs 3. Riparian areas and wetlands Meadows Wetlands Threats to riparian areas and wetlands Restoration efforts 4. Fish and wildlife Fisheries Exotic aquatic species Terrestrial wildlife 5. Land use and human history Human history Land use Residential Roads Grazing Recreation Airport Off-highway vehicle use Mining Forestry Land ownership and interagency cooperation 6. Descriptive hydrology Runoff generation processes Water balance Streamflow averages and extremes Floods and droughts Baseflow Lakes Groundwater Diversions and storage Water rights, use and management Residential -
Wringing Light out of Stone
MOUNTAIN PROFILE THE PALISADES I DOUG ROBINSON Wringing Light out of Stone So this kid walks into the Palisades.... I was twenty, twenty-one—don’t remember. It was the mid-1960s, for sure. I’d been hanging in the Valley for a few seasons, wide-eyed and feeling lucky to be soaking up wisdom by holding the rope for Chuck Pratt, the finest crack climber of the Golden Age. Yeah, cracks: those stark highways up Yosemite’s smooth granite that only open up gradually to effort and humility. Later they begin to reveal another facet: shadowed, interior, drawing us toward hidden dimensions of our ascending passion. ¶ The Palisades, though, are alpine, which means they are even more fractured. It would take me a little longer to cut through to the true dimensions of even the obvious features. To my young imagination, they looked like the gleaming, angular granite in the too-perfect romantic pictures that I devoured out of Gaston Rébuffat’s mountaineering books. My earliest climbing partner, John Fischer, had already been there— crampons lashed to his tan canvas-and-leather pack—and he’d returned, wide-eyed, with the tale of having survived a starlit bivy on North Palisade. [Facing Page] Don Jensen climbing in the Palisades, Sierra Nevada, California, during the 1960s—captured in a photo that reflects the atmosphere of the French alpinist Gaston Rébuffat’s iconic images of the Alps. Many consider the Palisades to be the most alpine region of the High Sierra, although climate change has begun to affect the classic ice and snow climbs.