Yosemite 10866411.Pdf
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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 . -
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. -
Nevada Fall Corridor
NEVADA FALL CORRIDOR: A CULTURAL LANDSCAPE REPORT by MARTI M. GERDES A THESIS Presented to the Interdisciplinary Studies Program: Historic Preservation and the Graduate School of the University of Oregon in partial fulfillment of the requirements for the degree of Master of Science August 2004 ii "Nevada Fall Corridor: A Cultural Landscape Report," a thesis prepared by Marti M. Gerdes in partial fulfillment of the requirements for the Master of Science degree in the Interdisciplinary Studies Program: Historic Preservation. This thesis has been approved and accepted by: Robert Z. Melnick, Chair of the Examining Committee 2 Date Committee in Charge: Robert Z. Melnick, Chair Cathy Gilbert Lee Roth Fred Walters Accepted by: Dean of the Graduate School iii C 2004 Marti M. Gerdes iv An Abstract of the Thesis of Marti M. Gerdes for the degree of Master of Science in the Interdisciplinary Studies Program: Historic Preservation to be taken August 2004 Title: NEVADA FALL CORRIDOR: A CULTURAL LANDSCAPE REPORT Approved: Robert Z. Melnick This study describes existing conditions, evaluates significance and historic integrity, and recommends treatment strategies to preserve historic elements of the Nevada Fall Corridor cultural landscape in Yosemite National Park. It reports findings from field investigation that examined and inventoried landscape features such as stone retaining walls, treadway material, bridges and causeways, and water features on both current-use and abandoned trail segments. The site was examined numerous times over a three-month period, with a followup visit one year later. Libraries and other archives were consulted for written and photographic historic documentation, which were analyzed against current conditions. -
Yosemite Valley Visitor Center
k e k e e r e C r Upper C n Yosemite o h y c r Fall n k A a e C e l r Yosemite Point a n C 6936ft y a Lower o 2114m i North Dome e d R t 7525ft i Yosemite n I 2294m m Fall e s ek o re Y U.S. Yosemite Valley Visitor Center C ya Court a Wilderness Center n e Museum Royal Arch T Lower Yosemite Medical Clinic Cascade Fall Trail Washington Columbia YOSEMITE Column Mirror Rock VILLAGE ROYAL Eagle Lake T ARCHES 4094ft Peak H 1248m 7779ft R The Ahwahnee Half Dome 2371m Sentinel Visitor E 8836ft Bridge Parking E North 2693m B Housekeeping Pines Camp 4 R Yosemite Camp Lower O Lodge Pines Chapel Stoneman T Bridge Middle H LeConte Brother E Memorial Road open ONLY to R Lodge pedestrians, bicycles, Ribbon S Visitor Parking and vehicles with Fall Swinging Bridge Curry Village Upper wheelchair emblem Pines Lower placards Sentinel Little Yosemite Valley El Capitan Brother Beach Trailhead for Moran 7569ft Four Mile Trail (summer only) R Point Staircase Mt Broderick i 2307m Trailhead 6706ft 6100 ft b Falls Horse Tail Parking 1859m b 2044m o Fall Trailhead for Vernal n Fall, Nevada Fall, and Glacier Point El Capitan Vernal C 7214 ft Nature Center John Muir Trail r S e e 2199 m at Happy Isles Fall Liberty Cap e n r k t 5044ft 7076ft ve i 4035ft Grizzly Emerald Ri n rced e 1230m 1538m 2157m Me l Peak Pool Silver C Northside Drive ive re Sentinel Apron Dr e North one-way Cathedral k El Capitan e Falls 0 0.5 Kilometer id To Tioga Road, Tuolumne Meadows Bridge Beach hs y ed R ut a y J and Hwy 120; and Hetch Hetchy Merc iv So -w horse trail onl o 0 0.5 Mile er -
Inventing Yosemite Valley: National Parks and the Language of Preservation
Inventing Yosemite Valley: National Parks and the Language of Preservation Yves Figueiredo ne of the intriguing facts about the giant sequoia has nothing to do with either its size or antiquity, but rather with its name. The species set a record for the number and variety of scientific denominations Oattributed to it by botanists around the world and it took no fewer than thir- teen different designations before Sequoiadendron giganteum was generally ac- cepted. In particular, this debate occasioned a bitter confrontation between British and American botanists. When it became clear that the existence of the tree was not another tall tale from the West, the English adopted in 1853 the term Wellingtonia gigantea to honor the memory of the Duke of Wellington. It would be a mild understatement to say that the Americans did not approve of the choice of an Old World statesman to name a New World wonder and they promptly retorted with Washingtonia gigantea. The current name was fi- nally agreed on when it became apparent that the tree was a cousin of the Coast Redwood Sequoia sempervirens.1 The sheer fact that such a heated debate could have happened over such a seemingly insignificant and rather technical matter shows that the real focus was not so much on the trees themselves as on what they stood for, and on the cultural role that they were to play in the post-Civil War United States. However, even more telling perhaps is the name by which the trees were most commonly designated by the public while the debate was raging in the higher spheres of scientific societies worldwide: sequoias were for every- body the “Big Trees” or “Mammoth Trees.” These names convey images of grandeur, of sheer size, and reveal the perception of the sequoia as above all a monument of nature. -
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 62(2)
YosetNte A JOURNAL FOR MEMBERS OF THE YOSEMITE ASSOCIATION Spring 2000 Volume 62 Number 2 An Interview with Superintendent Mihalic Yosemite's new superintendent, David A. Mihalic, has arrived at a critical juncture in the park 's history. The National Park Service proposes that over twenty years of Yosemite planning efforts will culminate soon with the adoption of the much-discussed Yosemite Valley Plan. Interior Secretary Babbitt wants a record of decision by December 2000, so the plan is definitely on the fast track . Given Mihalic's previous successes in developing and implementing man- agement plans, he appears to be a good choice to direct this effort. BY BETH PRATT AN INTRYIIY WITH SUPERINTENDENT MIHALIC The resume of David Mihalic features a list of leader- ship roles in both planning efforts and partnerships throughout the national park system . He has been with the park service since 1972, when he began his career as a seasonal park ranger in Glacier National Park . During his tenure as Superintendent at Yukon-Charley Rivers National Preserve in Alaska, he completed the park 's first general management plan . He was named the winner of the National Park Service Director 's "Superintendent of the Year" award in 1993 for his work in developing a local biosphere community to protect the natural resources at Mammoth Cave National Park. He returned to Glacier as its Superintendent in 1994, where he led the park in crafting its General Management Plan. While in Glacier he received the Garrison Gold Award for Interpretive Excellence, the Hastings Foundation Annual Leadership Award for developing strong partnerships with gateway communities, and was Superintendent Mihalic with Secretary of the Interior Bruce Rabbit (right). -
Department of the Interior U.S. Geological Survey Rock Falls in Yosemite Valley, California by Gerald F. Wieczorek1, James B. Sn
DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY ROCK FALLS IN YOSEMITE VALLEY, CALIFORNIA BY GERALD F. WIECZOREK1, JAMES B. SNYDER2, CHRISTOPHER S. ALGER3, AND KATHLEEN A. ISAACSON4 Open-File Report 92-387 This work was done with the cooperation and assistance of the National Park Service, Yosemite National Park, California. This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards (or with the North American Stratigraphic Code). Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government 'USGS, Reston, VA 22092, 2NPS, Yosemite National Park, CA, 95389, 3McLaren/Hart, Alameda, CA 94501, 4Levine Fricke, Inc., Emeryville, CA 94608 Reston, Virginia December 31, 1992 CONTENTS Page Abstract ............................................... 1 Introduction .............................................. 1 Geologic History ........................................... 2 Methods of Investigation ..................................... 5 Inventory of historical slope movements ........................ 5 Location ............................................ 5 Time of occurrence .......:............................ 7 Size ............................................... 8 Triggering mechanisms ................................. 9 Types of slope movement ................................ 11 Debris flows ...................................... 11 Debris slides ...................................... 12 Rock slides ...................................... -
YOSEMITE National Park
YOSEMITE National Park UNITED STATES RAILROAD ADMINISTRATION N AT IONAL PARK. SERIES Glacier Point, Yosemite Valley. The Half Dome in background Pa£e two An Appreciation of Yosemite NationalPark By HARRIET MONROE, Editor of "Poetry, a Magazine of Verse" Written Especially for the United Slates Railroad Administration WICE—and each time through an entire July—I have tramped with the California Sierra Club through the grandest areas of the Yosemite National Park. I have camped in the Valley, in Tuolumne Meadows, and in the lost Hetch-Hetchy—sleeping to the sound of rushing waters with mountains towering around me. I have crossed Vogelsang Pass when the mountain hemlocks were just slipping off their wet mantles of snow; I have descended the formidable Tuolumne Canyon past the third fall; and under Mount Dana I have looked down over the red rocks of Bloody Canyon to Lake Mono, lying incredibly blue among the pink and lilac craters of dead volcanoes. My memories of this prismatically shattered earth are sharp in details of beauty, but all of them rise against white granite and falling waters. Never anywhere else can there be mountains so silver-white—El Capitan shouldering the sky, Cloud's Rest and the two great Domes giving back the sun, and Ritter, Lyell and Dana, fierce and jagged, guarding their inscrutable heights. And through the crevices of this gleaming granite run everywhere crystal streams—streams mad with joy that foam as they fly, and shout as they take enormous leaps over stark precipices. All kinds of falling waters—the delicate cascades of Illilouette; the wind-blown tulle of Bridal Veil; Nevada, lacy, white-fingered, taking her 600-foot leap like a step in a dance; Vernal, broad-shouldered, strong-bodied, massive, as he jumps like an athlete; and, most wonder ful of all, Yosemite, that Upper Yosemite Fall whose leap is 1,500 feet — a tall white living figure against the formidable cliff, a figure moving and breathing, tossing the spray from his eyes, shining tall and straight there like a young Greek god. -
Bedrock Geologic Map of Yosemite Valley, Yosemite National Park, California
: I / DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY L, BEDROCK GEOLOGIC MAP OF YOSEMITE VALLEY, YOSEMITE NATIONAL PARK, CALIFORNIA By Frank C. Calkins and others MISCELLANEOUS N,IVESTIGATONS SERIES Published by the U.S. Geological Survey, 1985 G DEPARTMENT OF THE INTERIOR TO ACCOMPAI{Y MAP I-1639 U.S, GEOLOGICAL SURVEY BEDROCK GEOLOGY OF THE YOSEMITE VALLEY AREA YOSEMITE NATIONAL PARK, CALIFORNIA Prepared by N. King Huber and Julte A. Roller From the wrttlngs of Frank C. Calklns 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. Tumer, also of the U.S. Geological Survey, of rock sculpfure, is carved into the west slope of the who began mapping the Yosemite and Mount Lyell 30- Siena 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 Tumer never creating one of the most scenic nafural landscapes in completed this sizable assignment, he recognized the North America (fig. 1). In Yosemite Valley and the differing types oI plutonic rocks and, for example, named adloining 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 geologc map shows the Yosemite National Park during the period 1913 through distibution of some of the different rocks that make up 1916, at the same time that Francois Matthes was this assemblage. -
The Museum of Modern Art Momaexh 1273 Masterchecklist
The Museum of Modern Art 11 West 53 Street, New York, N. Y. 10019 Tel. 956-6100 Cable: Modernart ,L ADAMS AJ.'lDTHEWEST exhibition organized by The Museum of Modern Art, New York, New York ;KLrST: 153 photographs Title and text panel Acknowledgement panel All photographs have Security plates on frames. MoMAExh_1273_MasterChecklist Dimensions Museum Unframed Box Number Title/Date/Proeess/Credit Framed No. 1979.53 Apple Orchard, Winter, Yosemite National 5 15/16 x 7 13/16" 5 Park, California. 12 x 15" n, 1920; p .c , 1927. Lent by the photographer. 1979.63 Diamond Cascade, Lyell Fork of the Merced 2 7/8 x 3 7/8" 5 Canyon, Yosemite National P0rk, California. 8 1/2 x 11" n, 1920; p .c , 1920. Lent by the photographer. 1979.62 Fall in Upper Tenaya Canyon, Yosemite 4 1/16 x 2 7/8" 5 National Park, California. 11 x 8 1/2" n v c , 1920; p ;c . 1920. Lent by the photographer. 1979.66 Merced Peak from Red Peak, Sierra ~evada, 2 7/8 x 3 7/8" 5 California. 8 1/2 x 11" n.e. 1920; p.e. 1920. Lent by the photographer. 1979.65 Summit of Red Peak, Sierra Nevada, 27/8x37/8" 5 California. 8 1/2 x 11" n i c , 1920; p .c , 1920. Lent by the photographer. 1979.67 The Back of Half Dome, Yosemite National 3 3/4 x 2 13/16" 5 Park, California. 11 x 8 1/2" n.e. 1920; p.e. 1920. Lent by the photographer. 1979.64 Vernal Fall and Liberty Cap from the north 3 13/16 x 2 13/16" 5 bank of the Merced River, Yosemite National 11 x 8 1/2" Park, California. -
Yosemite Foundation Document
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Yosemite National Park California December 2016 Foundation Document k e k e e r e C r Upper C n Yosemite o h y c r Fall n k A a e C e l r Yosemite Point a n C 6936ft y a Lower o 2114m i North Dome e d R t 7525ft i Yosemite n I 2294m m Fall e s ek o re Y U.S. Yosemite Valley Visitor Center C ya Court a Wilderness Center n e Museum Royal Arch T Lower Yosemite Medical Clinic Cascade Fall Trail Washington Columbia YOSEMITE Column Mirror Rock VILLAGE ROYAL Eagle Lake T ARCHES 4094ft Peak H 1248m 7779ft R The Ahwahnee Half Dome 2371m Sentinel Visitor E 8836ft Bridge Parking E North 2693m B Housekeeping Pines Camp 4 R Yosemite Camp Lower O Lodge Pines Chapel Stoneman T Bridge Middle H LeConte Brother E Memorial Road open ONLY to R Lodge pedestrians, bicycles, Ribbon S Visitor Parking and vehicles with Fall Swinging Bridge Curry Village Upper wheelchair emblem Pines Lower placards Sentinel Little Yosemite Valley El Capitan Brother Beach Trailhead for Moran 7569ft Four Mile Trail (summer only) R Point Staircase Mt Broderick i 2307m Trailhead 6706ft 6100 ft b Falls Horse Tail Parking 1859m b 2044m o Fall Trailhead for Vernal n Fall, Nevada Fall, and Glacier Point El Capitan Vernal C 7214 ft Nature Center John Muir Trail r S e e 2199 m at Happy Isles Fall Liberty Cap e n r k t 5044ft 7076ft ve i 4035ft Grizzly Emerald Ri n rced e 1230m 1538m 2157m Me l Peak Pool Silver C Northside Drive ive re Sentinel Apron Dr e North one-way Cathedral k El Capitan e Falls 0 0.5 Kilometer