Mountain Views Vol. 9, No. 2
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THE YOSEMITE by John Muir CHAPTER I The
THE YOSEMITE By John Muir CHAPTER I The Approach to the Valley When I set out on the long excursion that finally led to California I wandered afoot and alone, from Indiana to the Gulf of Mexico, with a plant-press on my back, holding a generally southward course, like the birds when they are going from summer to winter. From the west coast of Florida I crossed the gulf to Cuba, enjoyed the rich tropical flora there for a few months, intending to go thence to the north end of South America, make my way through the woods to the headwaters of the Amazon, and float down that grand river to the ocean. But I was unable to find a ship bound for South America--fortunately perhaps, for I had incredibly little money for so long a trip and had not yet fully recovered from a fever caught in the Florida swamps. Therefore I decided to visit California for a year or two to see its wonderful flora and the famous Yosemite Valley. All the world was before me and every day was a holiday, so it did not seem important to which one of the world's wildernesses I first should wander. Arriving by the Panama steamer, I stopped one day in San Francisco and then inquired for the nearest way out of town. "But where do you want to go?" asked the man to whom I had applied for this important information. "To any place that is wild," I said. This reply startled him. He seemed to fear I might be crazy and therefore the sooner I was out of town the better, so he directed me to the Oakland ferry. -
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air Canada (Alberta – VE6/VA6) Association Reference Manual (ARM) Document Reference S87.1 Issue number 2.2 Date of issue 1st August 2016 Participation start date 1st October 2012 Authorised Association Manager Walker McBryde VA6MCB Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged Page 1 of 63 Document S87.1 v2.2 Summits on the Air – ARM for Canada (Alberta – VE6) 1 Change Control ............................................................................................................................. 4 2 Association Reference Data ..................................................................................................... 7 2.1 Programme derivation ..................................................................................................................... 8 2.2 General information .......................................................................................................................... 8 2.3 Rights of way and access issues ..................................................................................................... 9 2.4 Maps and navigation .......................................................................................................................... 9 2.5 Safety considerations .................................................................................................................. -
(Ca. 1.45 Ga), WESTERN NORTH AMERICA: PSEUDOFOSSILS, FACIES, TIDES and SYNDEPOSITIONAL TECTONIC ACTIVITY in a MESOPROTEROZOIC INTRACRATONIC BASIN
SEDIMENTARY, MICROBIAL AND DEFORMATION FEATURES IN THE LOWER BELT SUPERGROUP (ca. 1.45 Ga), WESTERN NORTH AMERICA: PSEUDOFOSSILS, FACIES, TIDES AND SYNDEPOSITIONAL TECTONIC ACTIVITY IN A MESOPROTEROZOIC INTRACRATONIC BASIN A Thesis Submitted to the College of Graduate and Postdoctoral Studies In Partial Fulfillment of the Requirements For the Degree of Doctor of Philosophy In the Department of Geological Sciences University of Saskatchewan Saskatoon By Roy Gregory Rule © Copyright Roy Gregory Rule, July, 2020. All rights reserved. PERMISSION TO USE In presenting this thesis in partial fulfilment of the requirements for a Postgraduate degree from the University of Saskatchewan, I agree that the Libraries of this University may make it freely available for inspection. I further agree that permission for copying of this thesis in any manner, in whole or in part, for scholarly purposes may be granted by the professor or professors who supervised my thesis work or, in their absence, by the Head of the Department or the Dean of the College in which my thesis work was done. It is understood that any copying or publication or use of this thesis or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis. Requests for permission to copy or to make other uses of materials in this thesis in whole or part should be addressed to: Head of the Geological Sciences Geology Building University of Saskatchewan Saskatoon, Saskatchewan S7N 5E2, Canada Or Dean College of Graduate and Postdoctoral Studies University of Saskatchewan 116 Thorvaldson Building, 110 Science Place Saskatoon, Saskatchewan S7N 5C9, Canada i ABSTRACT Sedimentary, microbial and deformation features in the lower Belt Supergroup (ca. -
BEDROCK GEOLOGY of the YOSEMITE VALLEY AREA YOSEMITE NATIONAL PARK, CALIFORNIA Prepared by N
DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I-1639 U.S. GEOLOGICAL SURVEY BEDROCK GEOLOGY OF THE YOSEMITE VALLEY AREA YOSEMITE NATIONAL PARK, CALIFORNIA Prepared by N. King Huber and Julie A. Roller From the writings of Frank C. Calkins and other sources PREFACE INTRODUCTION Frank Calkins' work in Yosemite was preceded by Yosemite Valley, one of the world's great natural works Henry W. Turner, also of the U.S. Geological Survey, of rock sculpture, is carved into the west slope of the who began mapping the Yosemite and Mount Lyell 30- Sierra Nevada. Immense cliffs, domes, and waterfalls minute quadrangles in 1897 and laid the foundation that tower over forest, meadows, and a meandering river, Calkins' work was built on. Although Turner never creating one of the most scenic natural landscapes in completed this sizable assignment, he recognized the North America (fig. 1). In Yosemite Valley and the differing types of plutonic rocks and, for example, named adjoining uplands, the forces of erosion have exposed, the El Capitan Granite. with exceptional clarity, a highly complex assemblage of Calkins mapped the valley and adjacent areas of granitic rocks. The accompanying geologic map shows the Yosemite National Park during the period 1913 through distribution of some of the different rocks that make up 1916, at the same time that Francois Matthes was this assemblage. This pamphlet briefly describes those studying the glacial geology of Yosemite. Calkins rocks and discusses how they differ, both in composition summarized the bedrock geology of part of Yosemite in and structure, and the role they played in the evolution the appendix of Matthes' classic volume "Geologic History of the valley. -
Yosemite: Warming Takes a Toll
Bay Area Style Tuolumne County Gives Celebrating Wealthy renowned A guide to donors’ S.F. retailer autumn’s legacies Wilkes best live on Bashford’s hiking, through Island Style ever-so- climbing their good Unforgettable Hawaiian adventures. K1 stylish and works. N1 career. J1 biking. M1 SFChronicle.com | Sunday, October 18,2015 | Printed on recycled paper | $3.00 xxxxx• Airbnb measure divides neighbors Prop. F’s backers, opponents split come in the middle of the night, CAMPAIGN 2015 source of his income in addition bumping their luggage down to work as a real estate agent over impact on tight housing market the alley. This is not an occa- and renewable-energy consul- sional use when a kid goes to ing and liability issues. tant, Li said. college or someone is away for a But Li, 38, said he urges “I depend on Airbnb to make By Carolyn Said Phil Li, who rents out three week. Along with all the house guests to be respectful, while sure I can meet each month’s suites to travelers via Airbnb. cleaners, it’s an array of com- two other neighbors said that expenses,” he said. “I screen A narrow alley separates “He’s running a hotel next mercial traffic in a residential they are not affected. Vacation guests carefully and educate Libby Noronha’sWest Portal door,” said Noronha, 67,a re- neighborhood,” she said of the rentals helped him after he lost them to come and go quietly.” house from that of her neighbor tired federal employee. “People noise, smoking, garbage, park- his job and remain a major Prop. -
Further Exploration in the Canadian Rocky Mountains Author(S): J
Further Exploration in the Canadian Rocky Mountains Author(s): J. Norman Collie and T. G. Bonney Source: The Geographical Journal, Vol. 21, No. 5 (May, 1903), pp. 485-499 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1775430 Accessed: 26-06-2016 12:56 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The Royal Geographical Society (with the Institute of British Geographers), Wiley are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 137.99.31.134 on Sun, 26 Jun 2016 12:56:46 UTC All use subject to http://about.jstor.org/terms The Geographical Journal. No. 5. MAY, 1903. VOL. XXI. FURTHER EXPLORATION IN THE CANADIAN ROCKY MOUNTAINS.* By J. NORMAN COLLIE, F.R.S. THE exploration of the main range of the Canadian Rocky mountains lying between the sources of the Athabasca river and the Kicking Horse pass has been the subject of two papers read by myself before the Royal Geographical Society. In these two papers I attempted to give a description of some of the great snowfields that exist amongst the Rocky mountains, and also as far as possible to make clear the geo- graphy of a mountain district up till that time but little known. -
Yosemite National Park National Park Service
National Park Service U.S. Department of the Interior Yosemite National Park Tuolumne Wild and Scenic River Comprehensive Management Plan Draft Environmental Impact Statement Tuolumne River Values and Baseline Conditions After five years of study and stakeholder involvement, the Tuolumne Wild and Scenic River Comprehensive Management Plan and Draft Environmental Impact Statement (Tuolumne River Plan/DEIS) will be released in summer of 2011. In advance of the plan’s release, the NPS is providing the Tuolumne River Values and Baseline Conditions chapter as a preview into one of the plan’s most foundational elements. Sharing the baseline information in advance of the plan will give members of the public an understanding of river conditions today and specific issues that will be explored in the Tuolumne River Plan. Public comments on all elements of the Tuolumne River Plan, including the baseline conditions chapter, will be accepted when it is released for review this summer. What follows is a description of the unique values that make the Tuolumne stand apart from all other rivers in the nation. This chapter also provides a snapshot in time, documenting overall conditions and implications for future management. In particular the baseline chapter examines, • What are the outstandingly remarkable values that make the Tuolumne River worthy of special protection under the Wild and Scenic Rivers Act (WSRA)? • What do we know about the condition of these values (in addition to water quality and free-flow), both at time of designation in 1984 and -
Ndex to Geophysical \Bstracts 184-187 .961
ndex to Geophysical \bstracts 184-187 .961 JAMES W. CLARKE, DOROTHY B. VITALIANO, VIRGINIA S. NEUSCHEL, and others EOLOGICAL SURVEY BULLETIN 1146-E 'bstracts of current literature ~rtaining to the physics of e solid earth and to !ophysical exploration ~ITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office, Washington 25, D.C. Price 40 cents (single copy). Subscription price: $1.75 a year; 50 cents additional for forei~n mailing. Use of funds for printing this publication has been approved by the Director of the Bureau of the Budget (June 23, 1960). INDEX TO GEOPHYSICAL ABSTRACTS 184-187, 1961 By James W. Clarke and others AUTHOR INDEX A Abstract Abdullayev, R. N. See Afanas'yev, G. D 185-56 Academy of Sciences of the U.S.S.R. First photographs of the reverse sic;le of the moon------------------------------------------------------------------ 186-111 Adachi, Ryuzo. On the magnification of the record of a vibration by an electro magnetic-type transducer and a galvanometer----------------------------- 186-279 Adadurov, G. A., Balashov, D. B., and Dremin, A. N. Research on volume compressibility of marble under high pressure----'1"----------------------- 186-595 Adamiya, Sh. A. Age of the "young" granites of the Khrami crystalline massif- 187-43 Adams, J. A. S., Osmond, J. K., Edwards, George, and Henle, W. Absolute dating of the Middle Ordovician------------------------------------------ 184-29 Adams, W. M. , and Allen, D. C. Reading seismograms with digital computers - 186-203 Adams, W. -
Rationales for Animal Species Considered for Designation As Species of Conservation Concern Inyo National Forest
Rationales for Animal Species Considered for Designation as Species of Conservation Concern Inyo National Forest Prepared by: Wildlife Biologists and Natural Resources Specialist Regional Office, Inyo National Forest, and Washington Office Enterprise Program for: Inyo National Forest August 2018 1 In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. Additionally, program information may be made available in languages other than English. To file a program discrimination complaint, complete the USDA Program Discrimination Complaint Form, AD-3027, found online at http://www.ascr.usda.gov/complaint_filing_cust.html and at any USDA office or write a letter addressed to USDA and provide in the letter all of the information requested in the form. To request a copy of the complaint form, call (866) 632-9992. -
Glaciers of the Canadian Rockies
Glaciers of North America— GLACIERS OF CANADA GLACIERS OF THE CANADIAN ROCKIES By C. SIMON L. OMMANNEY 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–1 The Rocky Mountains of Canada include four distinct ranges from the U.S. border to northern British Columbia: Border, Continental, Hart, and Muskwa Ranges. They cover about 170,000 km2, are about 150 km wide, and have an estimated glacierized area of 38,613 km2. Mount Robson, at 3,954 m, is the highest peak. Glaciers range in size from ice fields, with major outlet glaciers, to glacierets. Small mountain-type glaciers in cirques, niches, and ice aprons are scattered throughout the ranges. Ice-cored moraines and rock glaciers are also common CONTENTS Page Abstract ---------------------------------------------------------------------------- J199 Introduction----------------------------------------------------------------------- 199 FIGURE 1. Mountain ranges of the southern Rocky Mountains------------ 201 2. Mountain ranges of the northern Rocky Mountains ------------ 202 3. Oblique aerial photograph of Mount Assiniboine, Banff National Park, Rocky Mountains----------------------------- 203 4. Sketch map showing glaciers of the Canadian Rocky Mountains -------------------------------------------- 204 5. Photograph of the Victoria Glacier, Rocky Mountains, Alberta, in August 1973 -------------------------------------- 209 TABLE 1. Named glaciers of the Rocky Mountains cited in the chapter -
Documenting Twentieth Century Glacier Change with Repeat Photography in the Sierra Nevada, California HASSAN J BASAGIC; ANDREW G
Documenting Twentieth Century Glacier Change with Repeat Photography in the Sierra Nevada, California HASSAN J BASAGIC; ANDREW G. FOUNTAIN Department of Geography, Portland State University, Portland, Oregon, 97207 Introduction Repeat Photography Quantifying Glacier Change Alpine glaciers are important indicators of climate trends within a region and play a We gathered historical photos from the USGS Earth Science Photographic Archive (http://libraryphoto.er.usgs.gov/) significant role in the hydrology of alpine ecosystems. The Sierra Nevada of California and re-photographed following methods outlined by Harrison (1960) and Klett et al. (1984). The data Change in glacier area was calculated for Lyell Glacier in Yosemite National Park for contains approximately 497 alpine glaciers and perennial ice features (Raub, 1980). serve as a visual comparison of change through time. Below are the results from four of the ten the three time periods of 1883, 1944, 2003. Early photographs and a map by I.C. These glaciers provide an opportunity to determine regional responses to warming locations. Russell indicate that the Lyell glacier extent was near or at the Matthes, or Little Ice global temperatures over the past century. Historical photos of glaciers taken by early Age maximum (Russell, 1885). The 1944 extent was delineated from aerial and explorers, land surveyors, and park rangers in the late 19th century and early 20th ground based photographs. The 2003 extent was collected in the field with GPS. century are valuable records of past conditions. Repeat photography of glaciers is a Dana Glacier useful way to determine how these Sierra Nevada glaciers and perennial ice features have changed through time. -
Harvard Mountaineering 1
HARVARD MOUNTAIN · ERING Volume I • Number 1 JUNE, 1927 THE HARVARD MOUNTAINEERING CLUB CAMBRIDGE, MASS. Foreword Contents HE Harvard Mountaineering Club is now in its third year. ..... 3 Organized in November, 1924, with some ten or a dozen FOREWORD .......... charter members, it has grown rapidly, until there are now By Henry S. Hall, Jr. Tsome thirty active members and fifteen qualifying members in the 5 IN SEARCH OF MOUNT CLEARWATER . University, as well as thirty odd graduate members, some of whom are former active members and others Harvard graduates By W. Osgood Field who are or have been active mountaineers. Active membership 'MOUNT :MORAN AND THE TETONS . is limited to those who have had at least some real mountaineer By Beverly F. Jefferson 18 ing experience in the Alps, Canadian Rockies, or equivalent THE LYELL PEAKS AND :MOUNT FORBES . regions. Qualifying membership was established last fall to By Alfred J. Ostheimer, 3rd enable men 'who had done little or no active mountaineering, IMPRESSIONS OF DOLOMITE CLIMBING. ....... but who were interested, to be carried in the club rolls, so that they might attend its meetings and take part in its other By Lincoln O'Brien 31 activities. LIST OF ~t[E:\'1BERS . The original idea of forming such a club came to two Harvard graduates, who with an undergraduate were camped in the summer of 1923 at the base of a certain fine peak in the Canadian Rockies, which they were keenly hoping to climb. Fortune Club Officers favored. The peak was climbed, and a year from the following 1926--27 winter several undergraduates were found who enjoyed moun 1924-25 Pres.