John Muir Writings My First Summer in the Sierra
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The George Wright Forum
The George Wright Forum The GWS Journal of Parks, Protected Areas & Cultural Sites volume 34 number 3 • 2017 Society News, Notes & Mail • 243 Announcing the Richard West Sellars Fund for the Forum Jennifer Palmer • 245 Letter from Woodstock Values We Hold Dear Rolf Diamant • 247 Civic Engagement, Shared Authority, and Intellectual Courage Rebecca Conard and John H. Sprinkle, Jr., guest editors Dedication•252 Planned Obsolescence: Maintenance of the National Park Service’s History Infrastructure John H. Sprinkle, Jr. • 254 Shining Light on Civil War Battlefield Preservation and Interpretation: From the “Dark Ages” to the Present at Stones River National Battlefield Angela Sirna • 261 Farming in the Sweet Spot: Integrating Interpretation, Preservation, and Food Production at National Parks Cathy Stanton • 275 The Changing Cape: Using History to Engage Coastal Residents in Community Conversations about Climate Change David Glassberg • 285 Interpreting the Contributions of Chinese Immigrants in Yosemite National Park’s History Yenyen F. Chan • 299 Nānā I Ke Kumu (Look to the Source) M. Melia Lane-Kamahele • 308 A Perilous View Shelton Johnson • 315 (continued) Civic Engagement, Shared Authority, and Intellectual Courage (cont’d) Some Challenges of Preserving and Exhibiting the African American Experience: Reflections on Working with the National Park Service and the Carter G. Woodson Home National Historic Site Pero Gaglo Dagbovie • 323 Exploring American Places with the Discovery Journal: A Guide to Co-Creating Meaningful Interpretation Katie Crawford-Lackey and Barbara Little • 335 Indigenous Cultural Landscapes: A 21st-Century Landscape-scale Conservation and Stewardship Framework Deanna Beacham, Suzanne Copping, John Reynolds, and Carolyn Black • 343 A Framework for Understanding Off-trail Trampling Impacts in Mountain Environments Ross Martin and David R. -
Centennial Issue
YOSEMITE NATIONAL PARK Centennial Issue is been 100 years ture an appearance by since President Ben- President George Bush, jamin Harrison who has been invited. A I signed into law the number of other dig- act that established a large nitaries will also be in area around Yosemite attendance, and about Valley and the Mariposa the time of the ceremony, Big Trees as Yosemite a time capsule will be National Park. For the buried in front of the remainder of 1990 and Yosemite Valley Visitor until October, 1991, the Center. National Park Service Other centennial pro- will be celebrating the grams include a major park's centennial and ask- symposium that has been ing people to contemplate scheduled from October Yosemite's history and 13 to 19 in Concord and how the preservation Yosemite . The focus of idea, engendered in the symposium will be Yosemite, has taken on on natural and cultural new meaning in the face resource issues and on of global environmental future directions for park changes . There are hopes management. There are that from history we can also at least two museum learn the Iessons that will exhibits that will be open allow us to manage and through the end of the use Yosemite with the year. One is at the Califor- same foresight and wis- nia Academy of Sciences dom exemplified by those in San Francisco, the who first legislated the other at Yosemite 's own preservation of the place. museum . Please call the Participation in Yosemite Association at Yosemite's centennial (209) 379-2317 for infor- celebration is open to mation about any of everyone, and a variety of these programs or events. -
Investigating the El Capitan Rock Avalanche
BY GREG STOCK INVESTIGATING THE EL CapITAN ROCK AVALANCHE t 2:25 on the morning of March 26, 1872, one of avalanche, an especially large rockfall or rockslide that the largest earthquakes recorded in California extends far beyond the cliff where it originated. Most Ahistory struck along the Owens Valley fault near Yosemite Valley rockfall debris accumulates at the base the town of Lone Pine just east of the Sierra Nevada. The of the cliffs, forming a wedge-shaped deposit of talus. earthquake leveled most buildings in Lone Pine and sur- Occasionally, however, debris from a rock avalanche will rounding settlements, and killed 23 people. Although extend out much farther across the valley floor. seismographs weren’t yet available, the earthquake is esti- Geologist Gerald Wieczorek of the U.S. Geological mated to have been about a magnitude 7.5. Shock waves Survey and colleagues have identified at least five rock from the tembler radiated out across the Sierra Nevada. avalanche deposits in Yosemite Valley. The largest of these On that fateful morning, John Muir was sleeping in occurred in Tenaya Canyon, at the site of present-day a cabin near Black’s Hotel on the south side of Yosemite Mirror Lake. Sometime in the past, a rock formation on Valley, near present-day Swinging Bridge. The earth- the north wall of the canyon just east of and probably quake shook the naturalist out of bed. Realizing what similar in size to Washington Column collapsed into was happening, Muir bolted outside, feeling “both glad Tenaya Canyon. The rock debris piled up against the and frightened” and shouting “A noble earthquake!” He south canyon wall to a depth of over 100 feet. -
Mechanisms and Rate of Emplacement of the Half Dome Granodiorite
Mechanisms and rate of emplacement of the Half Dome Granodiorite Kyle J. Krajewski Chapel Hill 2019 Approved by: Allen F. Glazner Introduction Continental crust is largely composed of high-silica intrusive rocks such as granite, and understanding the mechanisms of granitic pluton emplacement is essential for understanding the formation of continental crust. With its incredible exposure, few places are comparable to the Tuolumne Intrusive Suite (TIS) in Yosemite National Park for studying these mechanisms. The TIS is interpreted as a comagmatic assemblage of concentric intrusions (Bateman and Dodge, 1970). The silica contents of the plutons increase from the margins inwards, transitioning from tonalities to granites, through both abrupt and gradational boundaries (Bateman and Chappell, 1979; Fig. 1). The age of the TIS also has a distinct trend, with the oldest rocks cropping out at the margins and the youngest toward the center. To accommodate this time variation, the TIS is hypothesized to have formed from multiple pulses of magma (Bateman and Chappell, 1979) . Understanding the volume, timing, and interaction of these pulses with one another has led to the formation of three main hypotheses to explain the evolution of the TIS. Figure 1. Simplified geologic map of the TIS. Insets of rocks on the right illustrate petrographic variation through the suite. Bateman and Chappell (1979) hypothesized that as the suite cooled, it solidified from the margins inward. Solidification of the chamber was prolonged by additional pulses of magma. These pulses expanded the chamber through erosion of the wall rock and breaking through the overlying carapace, creating a ballooning magma chamber. -
Saddlebrooke Hiking Club Hike Database 11-15-2020 Hike Location Hike Rating Hike Name Hike Description
SaddleBrooke Hiking Club Hike Database 11-15-2020 Hike Location Hike Rating Hike Name Hike Description AZ Trail B Arizona Trail: Alamo Canyon This passage begins at a point west of the White Canyon Wilderness on the Tonto (Passage 17) National Forest boundary about 0.6 miles due east of Ajax Peak. From here the trail heads west and north for about 1.5 miles, eventually dropping into a two- track road and drainage. Follow the drainage north for about 100 feet until it turns left (west) via the rocky drainage and follow this rocky two-track for approximately 150 feet. At this point there is new signage installed leading north (uphill) to a saddle. This is a newly constructed trail which passes through the saddle and leads downhill across a rugged and lush hillside, eventually arriving at FR4. After crossing FR4, the trail continues west and turns north as you work your way toward Picketpost Mountain. The trail will continue north and eventually wraps around to the west side of Picketpost and somewhat paralleling Alamo Canyon drainage until reaching the Picketpost Trailhead. Hike 13.6 miles; trailhead elevations 3471 feet south and 2399 feet north; net elevation change 1371 feet; accumulated gains 1214 northward and 2707 feet southward; RTD __ miles (dirt). AZ Trail A Arizona Trail: Babbitt Ranch This passage begins just east of the Cedar Ranch area where FR 417 and FR (Passage 35) 9008A intersect. From here the route follows a pipeline road north to the Tub Ranch Camp. The route continues towards the corrals (east of the buildings). -
3 They Are Wait- Ction: "Well It Ously, His Voice I ~?, ,K,~ Y White Nostrils ~, N I AM ~S~.N How Much All the Kings Men Owes to :The ~Y It Don T!
~~ h,,. ~p~ wnxxEN Robert Penn Warrea bit in the full- d to enjoy the othe`S from a ~sive climax of S.All the King's Men: n's o'n'es, and houseboy, who The Matrix of Experience :r, Duckfoot is it commitment 3 they are wait- ction: "Well it his voice iously, ~?, ,K,~N I AM ~s~.n white nostrils ~, how much All the Kings Men owes to :the y actual of ~y it don t! .. politics Louisiana in the 'go's, I can only be sure that p the pee out of if I had never gone #o live in Louisiana and if Huey bong had ool, a complete, ~'' not existed, the nove} would never have :been written.But this and you're here is far from,saying, that my "state" in AIZ the Kmg's is comfoik Men gent in ~° Louisiana or an ofsthe other fo fla the nostrils of r { Y rtj'-nine stars in our g), or id my i white-slick face #hat Willie Stark is the Iate Senator. What Louisiana and aside, which was Senator Long gave me was aline of thinking and feeling that ff his long white did eventuate ~ the.novel out Nhatever was In thesummer of 1434 I was offered a job—a much-needed.. cuzdling and and j, job—as assistant professor at the Louisiana State Unive~ity, in knew that every- Baton Rouge. It was.:"Huey Long's University," and definitely ever done or said L, on the make—with a sensational Football team and with money which.had been '` to spend even for assistant professors at a `time when assistant pride ass and his professors were being 5red, not hired—as I knew all too well. -
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. -
The Role of Wildfire in Shaping the Structure and Function of California ‘Mediterranean’ Stream-Riparian Ecosystems in Yosemite National Park
The role of wildfire in shaping the structure and function of California ‘Mediterranean’ stream-riparian ecosystems in Yosemite National Park DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Breeanne Kathleen Jackson Graduate Program in Environment and Natural Resources The Ohio State University 2015 Dissertation Committee: S. Mažeika P. Sullivan, Advisor Amanda D. Rodewald Desheng Liu Copyrighted by Breeanne Kathleen Jackson 2015 Abstract Although fire severity has been shown to be a key disturbance to stream-riparian ecosystems in temperate zones, the effects of fire severity on stream-riparian structure and function in Mediterranean-type systems remains less well resolved. Mediterranean ecosystems of California are characterized by high interannual variability in precipitation and susceptibility to frequent high-intensity wildfires. From 2011 to 2014, I investigated the influence of wildfire occurring in the last 3-15 years across 70 study reaches on stream-riparian ecosystems in Yosemite National Park (YNP), located in the central Sierra Nevada, California, USA. At 12 stream reaches paired by fire-severity (one high- severity burned, one low-severity burned), I found no significant differences in riparian plant community structure and composition, stream geomorphology, or benthic macroinvertebrate density or community composition. Tree cover was significantly lower at reaches burned with high-severity fire, however this is expected because removal of the conifer canopy partly determined study-reach selection. Further, I found no difference in density, trophic position, mercury (Hg) body loading, or reliance on aquatically- derived energy (i.e., nutritional subsidies derived from benthic algal pathways) of/by riparian spiders of the family Tetragnathidae, a streamside consumer that can rely heavily on emerging aquatic insect prey. -
Summits on the Air – ARM for USA - Colorado (WØC)
Summits on the Air – ARM for USA - Colorado (WØC) Summits on the Air USA - Colorado (WØC) Association Reference Manual Document Reference S46.1 Issue number 3.2 Date of issue 15-June-2021 Participation start date 01-May-2010 Authorised Date: 15-June-2021 obo SOTA Management Team Association Manager Matt Schnizer KØMOS 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 11 Document S46.1 V3.2 Summits on the Air – ARM for USA - Colorado (WØC) Change Control Date Version Details 01-May-10 1.0 First formal issue of this document 01-Aug-11 2.0 Updated Version including all qualified CO Peaks, North Dakota, and South Dakota Peaks 01-Dec-11 2.1 Corrections to document for consistency between sections. 31-Mar-14 2.2 Convert WØ to WØC for Colorado only Association. Remove South Dakota and North Dakota Regions. Minor grammatical changes. Clarification of SOTA Rule 3.7.3 “Final Access”. Matt Schnizer K0MOS becomes the new W0C Association Manager. 04/30/16 2.3 Updated Disclaimer Updated 2.0 Program Derivation: Changed prominence from 500 ft to 150m (492 ft) Updated 3.0 General information: Added valid FCC license Corrected conversion factor (ft to m) and recalculated all summits 1-Apr-2017 3.0 Acquired new Summit List from ListsofJohn.com: 64 new summits (37 for P500 ft to P150 m change and 27 new) and 3 deletes due to prom corrections. -
MONTANA N7 4Qea
E 12, p( /F- o77 (r 2) Sf(jji PGJ/F-077(82) National Uranium Resource Evaluation 6 BOZEMAN QUADRANGLE 41 MONTANA n7 4QeA/ University of Montana Missoula, Montana and Montana State University Bozeman, Montana E2T oFi Issue Date August 1982 SATESO9 PREPARED FOR THE U.S. DEPARTMENT OF ENERGY Assistant Secretary for Nuclear Energy Grand Junction Area Office, Colorado rmetadc957781 Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed in this report, or represents that its use would not infringe privately owned rights. Reference therein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. This report is a result of work performed by the University of Montana and Montana State University, through a Bendix Field Engineering Corporation subcontract, as part of the National Uranium Resource Evaluation. NURE was a program of the U.S. Department of Energy's Grand Junction, Colorado, Office to acquire and compile geologic and other information with which to assess the magnitude and distribution of uranium resources and to determine areas favorable for the occurrence of uranium in the United States. Available from: Technical Library Bendix Field Engineering Corporation P.O. -
Yosemite Spring Fling
Santa Ana College Community Services Program Presents.... YOSEMITE SPRING FLING FEATURING 2 NIGHTS AT THE TENAYA LODGE, WATERFALLS & THE SUGAR PINE RAILROAD APRIL 28-30, 2013 ~ 3 DAY TOUR Via TOUR PACE ACTIVITY LEVEL AY Y AY TINERARY Leisurely On the Go Low High ~D B D I ~ Yosemite is magnificent in the Spring! Renowned for TOUR HIGHLIGHTS its magnificent valley, great granite domes and peaks, w Two nights at the Tenaya Lodge at Yosemite – waterfalls and giant sequoias, Yosemite National an elegant and secluded 4-star mountain Park is a national treasure. This 3-day getaway offers resort featuring an indoor pool and spa a truly wonderful combination of natural wonders, w Extensive guided sightseeing with a local spring bloom and rustic elegance with two nights at guide to see Yosemite Valley to see the beauty the Tenaya Lodge. of El Capitan, Half Dome and the spectac- ular waterfalls – overflowing this time of year w Ride the rails through the Sierra Nevada Tenaya Lodge Lobby Forest’s majestic woods aboard the historic narrow gauge Yosemite Mountain Sugar Pine wDAY 2 ~ YOSEMITE NATIONAL PARKw Railroad Following an included breakfast buffet at the w A traditional Basque lunch in the Central Valley hotel, a local guide will join us for the day to provide a guided tour of the Yosemite Valley. FINE HOTELS / GREAT LOCATIONS Welcome to Yosemite National Park, embracing Yosemite Valley a spectacular tract of of mountain-and-valley scen- w Nights 1-2 Tenaya Lodge at Yosemite ery in the Sierra Nevada. Set aside as a national Yosemite South Entrance, CA wDAY 1 ~ ARRIVE YOSEMITEw park in 1890, the park harbors a grand collection After meeting at our departure points this TOUR INCLUSIONS of waterfalls, meadows and forests. -
THE COLLECTED POEMS of HENRIK IBSEN Translated by John Northam
1 THE COLLECTED POEMS OF HENRIK IBSEN Translated by John Northam 2 PREFACE With the exception of a relatively small number of pieces, Ibsen’s copious output as a poet has been little regarded, even in Norway. The English-reading public has been denied access to the whole corpus. That is regrettable, because in it can be traced interesting developments, in style, material and ideas related to the later prose works, and there are several poems, witty, moving, thought provoking, that are attractive in their own right. The earliest poems, written in Grimstad, where Ibsen worked as an assistant to the local apothecary, are what one would expect of a novice. Resignation, Doubt and Hope, Moonlight Voyage on the Sea are, as their titles suggest, exercises in the conventional, introverted melancholy of the unrecognised young poet. Moonlight Mood, To the Star express a yearning for the typically ethereal, unattainable beloved. In The Giant Oak and To Hungary Ibsen exhorts Norway and Hungary to resist the actual and immediate threat of Prussian aggression, but does so in the entirely conventional imagery of the heroic Viking past. From early on, however, signs begin to appear of a more personal and immediate engagement with real life. There is, for instance, a telling juxtaposition of two poems, each of them inspired by a female visitation. It is Over is undeviatingly an exercise in romantic glamour: the poet, wandering by moonlight mid the ruins of a great palace, is visited by the wraith of the noble lady once its occupant; whereupon the ruins are restored to their old splendour.