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Campsite Impact in the Wilderness of Sequoia and Kings Canyon National Parks Thirty Years of Change
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Campsite Impact in the Wilderness of Sequoia and Kings Canyon National Parks Thirty Years of Change Natural Resource Technical Report NPS/SEKI/NRTR—2013/665 ON THE COVER Examples of campsites surveyed in the late 1970s and again in 2006-2007. In a clockwise direction, these sites are in the Striped Mountain, Woods Creek, Sugarloaf, and Upper Big Arroyo areas in Sequoia and Kings Canyon National Parks. Photographs by: Sandy Graban and Bob Kenan, Sequoia and Kings Canyon National Parks. Campsite Impact in the Wilderness of Sequoia and Kings Canyon National Parks Thirty Years of Change Natural Resource Technical Report NPS/SEKI/NRTR—2013/665 David N. Cole and David J. Parsons Aldo Leopold Wilderness Research Institute USDA Forest Service Rocky Mountain Research Station 790 East Beckwith Avenue Missoula, Montana 59801 January 2013 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Technical Report Series is used to disseminate results of scientific studies in the physical, biological, and social sciences for both the advancement of science and the achievement of the National Park Service mission. The series provides contributors with a forum for displaying comprehensive data that are often deleted from journals because of page limitations. -
William J. Keith1, Maurice A. Chaffee*, Donald Plouffl, and Michael S
DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP MF-1416-B UNITED STATES GEOLOGICAL SURVEY MINERAL RESOURCE POTENTIAL OF THE CARSON-ICEBERG ROADLESS AREAS, CENTRAL SIERRA NEVADA, CALIFORNIA SUMMARY REPORT By William J. Keith1, Maurice A. Chaffee*, Donald Plouffl, and Michael S. Miller2 STUDIES RELATED TO WILDERNESS Under the provisions of the Wilderness Act (Public Law 88-577, September 3, 1964) and the Joint Conference Report on Senate Bill 4, 88th Congress, the U.S. Geological Survey and the U.S. Bureau of Mines have been conducting mineral surveys of wilderness and primitive areas. Areas officially designated as "wilderness," "wild," or "canoe" when the act was passed were incorporated into the National Wilderness Preservation System, and some of them are presently being studied. The act provided that areas under consideration for wilderness designation should be studied for suitability for incorporation into the Wilderness System. The mineral surveys constitute one aspect of the suitability studies. The act directs that the results of such surveys are to be made available to the public and be submitted to the President and the Congress. This report discusses the results of a mineral survey of the Carson-Iceberg Roadless Areas, Stanislaus and Toiyabe National Forests, Alpine and Tuolumne Counties, California. The Carson-Iceberg was established as a wilderness study area under the Joint Conference Report on Senate Bill 4, 88th Congress. It was later classified as recommended wilderness (C4-986 and C5-986) and further planning (B5-986) during the Second Roadless Area Review and Evaluation (RARE n) by the U.S. Forest Service, January 1979. -
Yosemite Valley Hiking Map U.S
Yosemite National Park National Park Service Yosemite Valley Hiking Map U.S. Department of the Interior To To ) S k Tioga n Tioga m e To o e k w r Road 10 Shuttle Route / Stop Road 7 Tioga . C Ranger Station C 4 n 3.I mi (year round) 6.9 mi ( Road r e i o 5.0 km y I e II.I km . 3.6 mi m n 6 k To a 9 m 5.9 km 18 Shuttle Route / Stop . C Self-guiding Nature Trail Tioga North 0 2 i Y n ( . o (summer only) 6 a Road 2 i s . d 6 m e 5.0 mi n m k i I Trailhead Parking ( 8.0 km m Bicycle / Foot Path I. it I.3 0 e ) k C m (paved) m re i ( e 2 ) ) k . Snow I Walk-in Campground m k k m Creek Hiking Trail .2 k ) Falls 3 Upper e ( e Campground i r Waterfall C Yosemite m ) 0 Fall Yosemite h I Kilometer . c r m 2 Point A k Store l 8 6936 ft . a ) y 0 2II4 m ( m I Mile o k i R 9 I. m ( 3. i 2 5 m . To Tamarack Flat North m i Yosemite Village 0 Lower (5 .2 Campground . I I Dome 2.5 mi Yosemite k Visitor Center m 7525 ft 0 Fall 3.9 km ) 2294 m . 3 k m e Cre i 2.0 mi Lower Yosemite Fall Trail a (3 To Tamarack Flat ( Medical Royal Mirror .2 0 y The Ahwahnee a m) k . -
Highway Conditions Introduction
Chapter 4 Highway Conditions Introduction The Ebbetts Pass National Scenic Byway (NBS) began as a trail that American Indians most likely used for trade and a hunting access route, and was later utilized by fur trappers. By the early to mid 1800’s pioneers and miners crossed over the pass. With the discovery of silver and the demand for more supplies to be delivered to the region, so came improvements to the road. Today, the highway itself is managed and maintained by the California Department of Transportation (CalTrans). The road twists you further into the mountains narrowing with no centerline near Lake Alpine as it separates both the Carson-Iceberg and Mokelumne Wildernesses, luring the traveler farther away from society. The journey takes one both physically and psychologically closer to wildness. Beyond the crest of Ebbetts Pass, the descent winds through a rugged volcanic landscape overlooking the canyons below. This asphalt ribbon transitions back to a distinct, 2-lane highway with a centerline when you reach the floor of Silver Creek, just east of Silver Creek Campground. This portion of the byway is steep, narrow, and windy, and is not suitable for semi trucks, buses, and most Recreational Vehicles (RV’s). It is best left for smaller vehicle travel. Average Daily Traffic CalTrans collects data annually that reflects the number of vehicles that travel along Highway 4 in a given month. This data is compiled into average annual daily traffic counts (AADT). AADT numbers are calculated using electronic highway counters, determining the yearly figure and dividing by 365 days/year. -
Inyo National Forest Visitor Guide
>>> >>> Inyo National Forest >>> >>> >>> >>> >>> >>> >>> >>> >>> >>> >>> Visitor Guide >>> >>> >>> >>> >>> $1.00 Suggested Donation FRED RICHTER Inspiring Destinations © Inyo National Forest Facts “Inyo” is a Paiute xtending 165 miles Bound ary Peak, South Si er ra, lakes and 1,100 miles of streams Indian word meaning along the California/ White Mountain, and Owens River that provide habitat for golden, ENevada border between Headwaters wildernesses. Devils brook, brown and rainbow trout. “Dwelling Place of Los Angeles and Reno, the Inyo Postpile Nation al Mon ument, Mam moth Mountain Ski Area National Forest, established May ad min is tered by the National Park becomes a sum mer destination for the Great Spirit.” 25, 1907, in cludes over two million Ser vice, is also located within the mountain bike en thu si asts as they acres of pris tine lakes, fragile Inyo Na tion al For est in the Reds ride the chal leng ing Ka mi ka ze Contents Trail from the top of the 11,053-foot mead ows, wind ing streams, rugged Mead ow area west of Mam moth Wildlife 2 Sierra Ne va da peaks and arid Great Lakes. In addition, the Inyo is home high Mam moth Moun tain or one of Basin moun tains. El e va tions range to the tallest peak in the low er 48 the many other trails that transect Wildflowers 3 from 3,900 to 14,494 feet, pro vid states, Mt. Whitney (14,494 feet) the front coun try of the forest. Wilderness 4-5 ing diverse habitats that sup port and is adjacent to the lowest point Sixty-five trailheads provide Regional Map - North 6 vegetation patterns ranging from in North America at Badwater in ac cess to over 1,200 miles of trail Mono Lake 7 semiarid deserts to high al pine Death Val ley Nation al Park (282 in the 1.2 million acres of wil der- meadows. -
Birth of a Plate Boundary at Ca. 12 Ma in the Ancestral Cascades Arc, Walker Lane Belt of California and Nevada
Origin and Evolution of the Sierra Nevada and Walker Lane themed issue Birth of a plate boundary at ca. 12 Ma in the Ancestral Cascades arc, Walker Lane belt of California and Nevada Cathy J. Busby Department of Earth Science, University of California–Santa Barbara, Santa Barbara, California 93106, USA ABSTRACT Sierra Nevada range front (from Long Valley The Sierra Nevada frontal fault system was to the Tahoe Basin) lies squarely within the previously interpreted to accommodate Basin The Walker Lane belt of eastern Califor- Walker Lane belt, not to the west of it as pre- and Range extension (Bateman and Wahrhaftig, nia and western Nevada is the northernmost vious workers have inferred. 1966; Surpless et al., 2002), but recent GPS extension of the Gulf of California transten- The leading tip of Walker Lane transten- and earthquake focal mechanism studies have sional rift, where the process of continental sion is marked by large arc volcanic cen- shown that the faults currently accommodate rupture has not yet been completed, and rift ters sited in transtensional stepovers; these NW-SE–directed movement between the Sierra initiation can be studied on land. GPS and include the ca. 11.5–9 Ma Sierra Crest–Little Nevada microplate and the North American earthquake focal mechanism studies dem- Walker volcanic center; north of that, the ca. plate (shown on Fig. 3; Sonder and Jones, 1999; onstrate that the Walker Lane belt currently 6.3–4.8 Ma Ebbetts Pass volcanic center; and Unruh et al., 2003). The question is, when did accommodates NW-SE–directed movement north of that, the active Lassen volcanic cen- NW-SE Walker Lane transtension replace E-W between the Sierra Nevada microplate and ter. -
Matthew Greene Were Starting to Understand the Grave the Following Day
VANISHED An account of the mysterious disappearance of a climber in the Sierra Nevada BY MONICA PRELLE ILLUSTRATIONS BY BRETT AFFRUNTI CLIMBING.COM — 61 VANISHED Three months earlier in July, the 39-year-old high school feasted on their arms. They went hiking together often, N THE SMALL SKI TOWN of Mammoth Lakes in math teacher dropped his car off at a Mammoth auto shop even in the really cold winters common to the Northeast. California’s Eastern Sierra, the first snowfall of the for repairs. He was visiting the area for a summer climb- “The ice didn’t slow him down one bit,” Minto said. “I strug- ing vacation when the car blew a head gasket. The friends gled to keep up.” Greene loved to run, competing on the track year is usually a beautiful and joyous celebration. Greene was traveling with headed home as scheduled, and team in high school and running the Boston Marathon a few Greene planned to drive to Colorado to join other friends times as an adult. As the student speaker for his high school But for the family and friends of a missing for more climbing as soon as his car was ready. graduation, Greene urged his classmates to take chances. IPennsylvania man, the falling flakes in early October “I may have to spend the rest of my life here in Mam- “The time has come to fulfill our current goals and to set moth,” he texted to a friend as he got more and more frus- new ones to be conquered later,” he said in his speech. -
John Muir Trail Entry Points
John Muir Trail Entry Points Alphabetical list of Inyo National Forest trails that connect to John Muir Trail (JMT) Mileage and elevation are approximate for trip planning, not intended for navigation. * indicates there is no pass between entry point and JMT junction Elevation Miles to Trail Name (area) Elevation at TrailheadElevation of Pass at JMT JunctionMiles to Pass JMT Junction Baxter Pass (Independence) 6,000 ft. 12,270 ft. 10,200 ft. 8 13 Bishop Pass (South Lake/ Bishop) 9,800 ft. 11,960 ft. 8,700 ft. 5 10 Cottonwood Pass -PCT (Horseshoe 9,900 ft. 11,120 ft. 10,600 ft. 3.5 20.5 Meadow) Duck Pass (Mammoth Lakes) 9,100 ft. 10,795 ft. 10,200 ft. 6 7 High Trail (Agnew Meadows) 8,300 ft. * 9,850 ft. * 7.75 JMT North of Devils Postpile (Reds 7,560 ft. * 7,580 ft. * Meadow toward Yosemite) 0.25 JMT South of Devils Postpile (Reds 7,560 ft. * 7,580 ft. * Meadow toward Mt Whitney) 0.25 Kearsarge Pass (Independence) 9,100 ft. 11,800 ft. 10,500 ft. 4 6.5 McGee Pass (Crowley Lake) 8,000 ft. 11,875 ft. 9,500 ft. 7 11.5 Mono Pass (Rock Creek Road) 10,200 ft. 12,040 ft. 8,400 ft. 2.5 15 Mt Whitney Trail (Lone Pine) 8,300 ft. 13,700 ft. 13,480 ft. 8.2 8.7 Pine Creek Pass (Bishop) 7,400 ft. 11,120 ft. 8,075 ft. 7 20 Piute Pass (North Lake/ Bishop) 9,350 ft. 11,420 ft. -
California's Fourteeners
California’s Fourteeners Hikes to Climbs Sean O’Rourke Cover photograph: Thunderbolt Peak from the Paliasde Traverse. Frontispiece: Polemonium Peak’s east ridge. Copyright © 2016 by Sean O’Rourke. All rights reserved. No part of this book may be reproduced in any form without express permission from the author. ISBN 978-0-98557-841-1 Contents 1 Introduction 1 1.1 Who should read this .......................... 1 1.2 Route difficulty ............................. 2 1.3 Route points .............................. 3 1.4 Safety and preparedness ........................ 4 1.5 Climbing season ............................ 7 1.6 Coming from Colorado ........................ 7 2 Mount Langley 9 2.1 Southwest slope ............................ 10 2.2 Tuttle Creek ............................... 11 3 Mount Muir 16 3.1 Whitney trail .............................. 17 4 Mount Whitney 18 4.1 Whitney trail .............................. 19 4.2 Mountaineer’s route .......................... 20 4.3 East buttress *Classic* ......................... 21 5 Mount Russell 24 5.1 East ridge *Classic* ........................... 25 5.2 South Face ............................... 26 5.3 North Arête ............................... 26 6 Mount Williamson 29 6.1 West chute ............................... 30 7 Mount Tyndall 31 7.1 North rib ................................ 32 7.2 Northwest ridge ............................ 32 8 Split Mountain 36 8.1 North slope ............................... 37 i 8.2 East Couloir .............................. 37 8.3 St. Jean Couloir -
Stanford Alpine Club Journal, 1958
STANFORD ALPINE CLUB JOURNAL 1958 STANFORD, CALIFORNIA i-., r ' j , / mV « Club Officers 1956-57 John Harlin, President John Mathias, Vice President Karl Hufbauer, Secretary William Pope, Treasurer 1957-58 Michael Roberts, President Karl Hufbauer, Vice-President Sidney Whaley, Secretary- Ivan Weightman, Treasurer ADVISORY COUNCIL John Maling, Chairman Winslow Briggs Henry Kendall Hobey DeStaebler Journal Staff Michael Roberts, Editor Henry Kendall, Photography Sidney Whaley Lenore Lamb Contents First Ascent of the East Peak of Mount Logan 1 Out of My Journal (Peru, 1955) 10 Battle Range, 1957 28 The SAC Trans-Sierra Tour 40 Climbing Notes 51 frontispiece: Dave Sowles enroute El Cafitan Tree, Yosemite Valley. Photo by Henry Kendall Grateful acknowledgement is made to the following: Mr. Richard Keeble, printing consultant Badger Printing Co., Appleton, Wise., photographic plates, press work and binding. Miss Mary Vogel, Appleton, Wise., composition and printing of text. Fox River Paper Corporation, Appleton, Wise., paper for text and photographs. FIRST ASCENT OF THE EAST PEAK OF MOUNT LOGAN by GILBERT ROBERTS Mount Logon. North America's second highest peak at 19,850 feet, is also one of the world's largest mountain masses. Located in the wildest part of the St. Elias Range, it has seen little mountaineering activity. In 1925, the first ascent was accomplished by a route from the Ogilvie Glacier which gained the long ridge leading to the summit from King Col. This ascent had gone down as one of the great efforts in mountaineering history. McCarthy, Foster, Lambert, Carpe, Read, and Taylor ulti- mately reached the central summit after months of effort including the relaying of loads by dog sled in the long Yukon winter--a far cry from the age of the air drop. -
Gazetteer of Surface Waters of California
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTI8 SMITH, DIEECTOE WATER-SUPPLY PAPER 296 GAZETTEER OF SURFACE WATERS OF CALIFORNIA PART II. SAN JOAQUIN RIVER BASIN PREPARED UNDER THE DIRECTION OP JOHN C. HOYT BY B. D. WOOD In cooperation with the State Water Commission and the Conservation Commission of the State of California WASHINGTON GOVERNMENT PRINTING OFFICE 1912 NOTE. A complete list of the gaging stations maintained in the San Joaquin River basin from 1888 to July 1, 1912, is presented on pages 100-102. 2 GAZETTEER OF SURFACE WATERS IN SAN JOAQUIN RIYER BASIN, CALIFORNIA. By B. D. WOOD. INTRODUCTION. This gazetteer is the second of a series of reports on the* surf ace waters of California prepared by the United States Geological Survey under cooperative agreement with the State of California as repre sented by the State Conservation Commission, George C. Pardee, chairman; Francis Cuttle; and J. P. Baumgartner, and by the State Water Commission, Hiram W. Johnson, governor; Charles D. Marx, chairman; S. C. Graham; Harold T. Powers; and W. F. McClure. Louis R. Glavis is secretary of both commissions. The reports are to be published as Water-Supply Papers 295 to 300 and will bear the fol lowing titles: 295. Gazetteer of surface waters of California, Part I, Sacramento River basin. 296. Gazetteer of surface waters of California, Part II, San Joaquin River basin. 297. Gazetteer of surface waters of California, Part III, Great Basin and Pacific coast streams. 298. Water resources of California, Part I, Stream measurements in the Sacramento River basin. -
5.1 Historic Period Human Interaction with the Watershed
Upper Carson River Watershed Stream Corridor Assessment 5. Human Interaction With the Watershed 5.1 Historic Period Human Interaction With the Watershed The purpose of this section is to summarize human activities that have had some effect on the Carson River watershed in Alpine County, California. Regional prehistory and ethnography are summarized by Nevers (1976), Elston (1982), d’Azevedo (1986), and Lindstrom et al. (2000). Details of regional history can be found in Maule (1938), Jackson (1964), Dangberg (1972), Clark (1977), Murphy (1982), Marvin (1997), and other sources. A book published by the Centennial Book Committee (1987) contains an excellent selection of historic photographs. Particularly useful is a study on the historical geography of Alpine County by Howatt (1968). 5.1.1 Prehistoric Land Use Human habitation of the Upper Carson River Watershed extends thousands of years back into antiquity. Archaeological evidence suggests use of the area over at least the last 8,000 to 9,000 years. For most of that time, the land was home to small bands of Native Americans. Their number varied over time, depending on regional environmental conditions. For at least the last 2,000 years, the Washoe occupied the Upper Carson River Watershed. Ethnographic data provides clues as to past land use and land management practices (see extended discussions in Downs 1966; Blackburn and Anderson 1993; Lindstrom et al. 2000; Rucks 2002). A broad range of aboriginal harvesting and hunting practices, fishing, and camp tending would have affected the landscape and ecology of the study area. Shrubs such as service berry and willow were pruned to enhance growth.