The Yosemite Valley (1910) by Galen Clark
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Sketch of Yosemite National Park and an Account of the Origin of the Yosemite and Hetch Hetchy Valleys
SKETCH OF YOSEMITE NATIONAL PARK AND AN ACCOUNT OF THE ORIGIN OF THE YOSEMITE AND HETCH HETCHY VALLEYS DEPARTMENT OF THE INTERIOR OFFICE OF THE SECRETARY 1912 This publication may be purchased from the Superintendent of Documents, Government Printing Office, Washington. I). C, for LO cents. 2 SKETCH OP YOSEMITE NATIONAL PARK AND ACCOUNT OF THE ORIGIN OF THE YOSEMITE AND HETCH HETCHY VALLEYS. By F. E. MATTHES, U. S. Geological Surrey. INTRODUCTION. Many people believe that the Yosemite National Park consists principally of the Yosemite Valley and its bordering heights. The name of the park, indeed, would seem to justify that belief, yet noth ing could be further from the truth. The Yosemite Valley, though by far the grandest feature of the region, occupies only a small part of the tract. The famous valley measures but a scant 7 miles in length; the park, on the other hand, comprises no less than 1,124 square miles, an area slightly larger than the State of Rhode Island, or about one-fourth as large as Connecticut. Within this area lie scores of lofty peaks and noble mountains, as well as many beautiful valleys and profound canyons; among others, the Iletch Hetchy Valley and the Tuolumne Canyon, each scarcely less wonderful than the Yosemite Valley itself. Here also are foaming rivers and cool, swift trout brooks; countless emerald lakes that reflect the granite peaks about them; and vast stretches of stately forest, in which many of the famous giant trees of California still survive. The Yosemite National Park lies near the crest of the great alpine range of California, the Sierra Nevada. -
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 . -
Galen Clark's Library
YOSEMITE VOLUME XXXVIII - NUMBER 12 DECEMBER 1959 IN COOPERATION •ITH THE NATIONAL PARR . SERVICE. In 1857, when 43 years of age, Galen Clark (left) was told that he had not long to live and should move from Mariposa to a more favorable climate of a higher elevation . This led t, his settling on the South Fork of the Merced River, at present day Wawona, and establishino a hotel to accommodate early-day visitors to Yosemite Valley and the Mariposa Grove . Clar4 died in 1910 at the ripe old age of 96. COVER — Galen Clark, Yosemite ' s first Guardian, at the base of the Grizzly Giant. —Photo by Watktus, 181t~ yosemite Since 1922, the monthly publication of the National Park Service and the Yosemite Natural NAILER! NOTE S History Association in Yosemite National Park. John C . Preston, Park Superintendent Douglass H . Hubbard, Park Naturalist Robert F. Upton, Associate Park Naturalist D^'tl F . McCrary, Assistant Park Naturalist Herbert D . Cornell, Junior Park Naturalist Keith A . Trexler, Park Naturalist Trainee 1 WOK., XXXVHI DEC'EAIBLR 1959 NO . 12 GALEN CLARK'S LIBRARY by Jim Fox, Ranger-Naturalist Probably the most revered pioneer Lodge of the Sierra Club, to which hi Yosemite history was Galen Clark . he was a charter member . They are In 1855 he first saw the Valley, and there now, kept in Yosemite Valley lit 1857 he established the first hostel available to the public. at what is now Wawona. It was at A survey of the books in the Galen that time the halfway point on the Clark Collection is of interest to the trail from Mariposa to Yosemite Val- historian as it may shed some light lay and was known as Clark 's on the interests of Clark. -
Yosemite National Park Foundation Overview
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Overview Yosemite National Park California Contact Information For more information about Yosemite National Park, Call (209) 372-0200 (then dial 3 then 5) or write to: Public Information Office, P.O. Box 577, Yosemite, CA 95389 Park Description Through a rich history of conservation, the spectacular The geology of the Yosemite area is characterized by granitic natural and cultural features of Yosemite National Park rocks and remnants of older rock. About 10 million years have been protected over time. The conservation ethics and ago, the Sierra Nevada was uplifted and then tilted to form its policies rooted at Yosemite National Park were central to the relatively gentle western slopes and the more dramatic eastern development of the national park idea. First, Galen Clark and slopes. The uplift increased the steepness of stream and river others lobbied to protect Yosemite Valley from development, beds, resulting in formation of deep, narrow canyons. About ultimately leading to President Abraham Lincoln’s signing 1 million years ago, snow and ice accumulated, forming glaciers the Yosemite Grant in 1864. The Yosemite Grant granted the at the high elevations that moved down the river valleys. Ice Yosemite Valley and Mariposa Grove of Big Trees to the State thickness in Yosemite Valley may have reached 4,000 feet during of California stipulating that these lands “be held for public the early glacial episode. The downslope movement of the ice use, resort, and recreation… inalienable for all time.” Later, masses cut and sculpted the U-shaped valley that attracts so John Muir led a successful movement to establish a larger many visitors to its scenic vistas today. -
Martin Mason Hazeltine Stereoview Collection, Dates: Circa 1870 Collection Number: H.Mss.0994 Creator: Hazeltine, M
http://oac.cdlib.org/findaid/ark:/13030/c80z7213 No online items Guide to the Martin Mason Hazeltine stereoview collection Finding aid prepared by Lisa L. Crane, MLIS Special Collections, Honnold/Mudd Library 800 North Dartmouth Ave Claremont, CA, 91711 Phone: (909) 607-3977 Email: [email protected] URL: http://libraries.claremont.edu/sc/default.html © 2012 Claremont University Consortium. All rights reserved. Guide to the Martin Mason H.Mss.0994 1 Hazeltine stereoview collection Descriptive Summary Title: Martin Mason Hazeltine stereoview collection, Dates: circa 1870 Collection number: H.Mss.0994 Creator: Hazeltine, M. M. (Martin Mason), 1827-1903 Creator: Soule, John P. Extent: 54 items Repository: Claremont Colleges. Library. Special Collectins, Honnold/Mudd Library. Claremont, CA 91711 Abstract: Fifty-three stereoviews, plus one duplicate, of Yosemite Valley and the California Big Trees scenic views. All marked with the studio imprint of John P. Soule. This "California" series of photographs was produced by the photographer Martin Mason Hazeltine (1827-1903), though no credit is given him on these images. Hazeltine, a Vermont native, moved to California and established a studio in Mendocino in the late 1860s. Among his works, he produced many western images, including this Yosemite series, and one on the Yellowstone. His photos were published by other firms, including J. P. Soule, and Lawrence & Houseworth. Physical location: Please consult repository. Language of materials: Languages represented in the collection: English. Access This collection is open for research. Publication Rights All requests for permission to reproduce or to publish must be submitted in writing to Special Collections. Preferred Citation [Identification of item], Martin Mason Hazeltine stereoview collection (H.Mss.0994). -
STORY of TRAIL BUILDING in YOSEMITE NATIONAL PARK by Gabriel Sovulewski of the 600 Miles of Trails That Keep Them So
DEPARTMENT OF THE INTERIOR HUBERT WORK, SECRETARY NATIONAL PARK SERVICE YOSEMITE NATURE NOTES VOL. VII APRIL, 1928 NO. 4 "LEARN TO READ THE TRAILSIDE" YOSEMITE NATIONAL EARL, CALIF . iq9 This is the official publication of the Education ..) Depart- ment of Yosemite National Park . I t is puh ishe .i each month by the National Park Service with the co-operation of th Yosemite Natural History Association, and its purpose is to supply dependable information on the natural history and scientific features of Yosemite National Park . The artic :es published herein are not copyrighted as it is intended that they shall be freely used by the press . Communications should be addressed to C . P . Russell, Park Naturalist, Yosemite National Park, California. E. P. LEAVITT Acting Superintendent YOSEMITE NATURE NOTES THE PUBLICATION OF THE YOSEMITE EDUCATIONAL DEPARTMENT AND THE YOSEMITE NATURAL HISTORY ASSOCIATION Published monthly Volume V 1I April, 1928 Number 4 THE STORY OF TRAIL BUILDING IN YOSEMITE NATIONAL PARK By Gabriel Sovulewski Of the 600 miles of trails that keep them so . After these many exist within Yosemite boundaries, years of trail building, his enthusi- by far the greater part have been asm for such construction wanes built within the past thirty years . not at all . Just now a trails corn- In searching the old park records mittee appointed by Director made by the state park guardians, Mather is expressing its beliefs re- and the army superintendents of garding interesting foot trails along ,the national park, it became appar- Yosemite walls, and Mr . Sovulewsk; ent that dependable trail history grins like a boy as he makes his ex- was exceedingly difficult to obtain . -
Ley, So the Still Deeper Cañon of Lower Two Miles,That Is, Beyond Rather Than
THE CANON OF YOSEMITE 87 As Merced Cañon forms the southeast branch of Yosemite Val- ley, so the still deeper cañon of Tenaya Creek isits northeastern arm.Here the glacial story is less plain, and on first sight, from the heights on either side, it might be overlooked.For above the cañon's lower two miles,that is, beyond the foot of Mt. Watkins,it crowds to a narrow box-cañon between that great cliff and the steep incline of Clouds Rest.This might seem to be a V-shaped, stream-cut gorge, rather than to have the broader bottom commonly left by a glacier. But alittle exploration discovers glacial footprints in the terminal moraines and the lakes and filled lake-beds,withfineconnecting waterfalls, that mark aglacier's descent from the Cathedral Peak Range, south of the Tuolumne. We Overhung at Summit of the Half Dont,-. nrart have hardly entered the cañon, in- a tulle above the Valley floor nn.l Tena-u deed, before we are reminded of (allan.El Caption Is seen in the tllatanee. El Capitan moraine and the enclosed Yosemite Lake. A similar boulder ridge, thrown across the cañon here, is traversed by the road as it carries visitors on their early morning trips to see the sunrise reflections in Mirror Lake.This lakelet evidently occupies the lowermost of the glacial steps.It is a mere reminder of its former size, the delta of Tenaya Creek having stolen a mile from its upper end.Farther up the cañon, below and above Mt. Watkins, stream sediment has already turned similar lakes into meadows. -
Index of Surface-Water Records
GEOLOGICAL SURVEY CIRCULAR 72 January 1950 INDEX OF SURFACE-WATER RECORDS PART 11.PPACIFIC SLOPE BASINS IN CALIFORNIA TO SEPTEMBER 30, 1948 Prepared by San Francisco District UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director WASHINGTON, D. C. Free on application to the Director, Geological Survey, Washington 26, D. C. INDEX OF SURFACE-WATER RECORDS PART 11.PPACIFIC SLOPE BASINS IN CALIFORNIA TO SEPTEMBER 30, 1948 EXPLANATION The index lists the stream-flow ana reservoir stations in the Pacific Slope Basins in California for which records have been or are to be pub lished for periods prior to September 30, 1948. The stations are listed in downstream order. Tributary streams are indicated by indention. Station names are given in their most recently published forms. Paren theses around part of a station name indicate that the enclosed word or words were used in an earlier published name of the station or in a name under which records were published by some agency other than the Geological Survey. The drainage areas, in square miles, are the latest figures published or otherwise available at this time. Drainage areas that were obviously inconsistent with other drainage areas on the same stream have been omitted. Some drainage areas not published by the Geological Survey are listed with an appropriate footnote stating the published source of the figure of drainage area. Under "period of record" breaks of less than a 12-month period are not shown. A dash not followed immediately by a closing date shows that the station was in operation on September 30, 1948. -
Yosemite Roads and Bridges Man WAY B M Eaiimum
Yosemite's Bridges STGNEMLAN BRIDGE CONSTRUCTION - 1932 YOSEMITE FALLS Yosemite Village A variety of vehicular bridges span the main streams and lesser tributaries in the park. The oldest is the covered bridge at This structure exemplifies the National Park Service Rustic man WAY B m EAiimum Wawona, built as an open-deck structure in 1868 by Galen Style of architecture. Built of reinforced concrete, Ahwahnee Hotel Clark, the first settler and state-appointed Guardian of the the bridge is faced with native granite to blend s Yosemite Grant. In the 1870s it was converted to a covered in with its natural setting. Equestrian bridge by the Washburn brothers, natives of Vermont, who tunnels were designed in conjunction supposedly had it altered to remind them of their home state. with a new park bridle path. Yosemite Lodge Yosemite Rehabilitated by the Park Service in 1956, it can be seen today Drawn by David Fleming, at the Pioneer Yosemite History Center. HAER, 1991 Roads and Bridges Yosemite National Park, California Early bridges were wood and metal trusses. The previous Sentinel Bridge was an uncommon iron bowstring-arch truss. YRL WAWONA COVERED BRIDGE, 1868 The Wawona Tunnel was the longest vehicular tunnel in the Drawn by Dione DeMartelaere, HAER, 1991 West when completed in 1933. Significant for its state-of- Original Appearance the-art engineering, the tunnel played a greater role in Construction of retaining wall on Big Oak Flat Drawn by Dione DeMartelaere and preserving the visible landscape of Yosemite Valley. Road, 1939. YRL Marie-Claude LeSauteur, HAER 1991 Over the ensuing years more timber and iron trusses were built, but these eventually gave way to reinforced concrete structures; 1. -
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. -
2014 California Parks Training Conference
2014 California Parks Training Conference March 3-6 - Yosemite Lodge in Yosemite NP Welcome to Special Programs The Heritage of Parks Nationally acclaimed special presentations: in California Spirit of John Muir by Lee Stetson . Buffalo Soldier by National Park Ranger Shelton Johnson Screening of the new Ken Burn’s film Yosemite: A Gathering of Spirit. Plus Evening reception and banquet dinner at the famed Ahwahnee Hotel Galen Clark Memorial Ceremony in the Yosemite Cemetery on Clark’s 200th Birthday Anniversary Galen Clark live Meet and get your picture taken with Yosemite’s first Guardian (Miles Standish) Inside General Conference Information 2 Conference Co-Chairs Field Trips and Social Activities 2-3 Mike Lynch - CSPRA Sessions: Tuesday, March 4 and 4-6 Wednesday March 5 Jeff Ohlfs - PRAC Acknowledgements/Sponsors 7 PAGE 2 2014 CALIFORNIA PARKS TRAINING CONFERENCE General Conference Information Field Trips, Events & Special Presentations Conference Check-In Monday, March 3 Conference attendees will need to check in at the con- Ansel Adams Gallery Camera Walk, 9:00 a.m. to ference registration and information desk to receive 10:30 a.m. — Free Camera walks are led by staff their conference information packets, meal tickets, and photographers. Meet and depart from the Ahwahnee Ho- any pre-ordered conference apparel. The conference tel at 9 AM. Limited to 15 people. Reservations only, registration and information desk will be in the Garden call 209-372-4413 to reserve space on Saturday March 1 Terrace Room at the Yosemite Lodge starting Monday, ONLY. FREE. ON YOUR OWN ACTIVITY. March 3 at 12 noon and will be open throughout the Conference. -
The Mariposa County Setting
County of Mariposa General Plan – Volume I Countywide General Plan 1 THE MARIPOSA COUNTY SETTING This chapter of the General Plan lays out the County’s setting and projections for the future. 1.1 WHERE WE ARE he County of Mariposa is located in central California, adjacent to the San Joaquin Valley within the central Sierra Nevada. Mariposa County is surrounded by Tuolumne County on the north and east, Madera County on the south, and Merced and Stanislaus counties on the west (Figure 1-1). Mariposa County boundaries are approximately 25 minutes from Merced and one hour from the cities of Modesto, Madera, Sonora,T and Fresno. The Town of Mariposa is a little less than two hours from Fresno- Yosemite International Airport, three and one half hours from Oakland International Airport, four hours from Sacramento International Airport, and over four hours from San Francisco International Airport. Merced’s Amtrak train station is an inter-modal transfer point with the Yosemite Area Regional Transit System. Figure 1-1: Regional Map Page 1-1 County of Mariposa General Plan – Volume I Countywide General Plan 1.2 WHO WE ARE In January 2006 the California Department of Finance estimates that Mariposa County was home to 18,216 residents, up nearly six percent from the 2000 census, which was an increase of almost twenty percent from the 1990 census. At the build-out of the General Plan, the County analyzes a population potential of 28,000, which theoretically could be reached within the planning horizon of 2020 (Figure 1-2). The demographics of Mariposa County have not changed much between the 1990 census and 2000 census.