Proposed Finding Against Acknowledgment of the Southern Sierra Miwuk Nation A.K.A
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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. -
Cultivating an Abundant San Francisco Bay
Cultivating an Abundant San Francisco Bay Watch the segment online at http://education.savingthebay.org/cultivating-an-abundant-san-francisco-bay Watch the segment on DVD: Episode 1, 17:35-22:39 Video length: 5 minutes 20 seconds SUBJECT/S VIDEO OVERVIEW Science The early human inhabitants of the San Francisco Bay Area, the Ohlone and the Coast Miwok, cultivated an abundant environment. History In this segment you’ll learn: GRADE LEVELS about shellmounds and other ways in which California Indians affected the landscape. 4–5 how the native people actually cultivated the land. ways in which tribal members are currently working to restore their lost culture. Native people of San Francisco Bay in a boat made of CA CONTENT tule reeds off Angel Island c. 1816. This illustration is by Louis Choris, a French artist on a Russian scientific STANDARDS expedition to San Francisco Bay. (The Bancroft Library) Grade 4 TOPIC BACKGROUND History–Social Science 4.2.1. Discuss the major Native Americans have lived in the San Francisco Bay Area for thousands of years. nations of California Indians, Shellmounds—constructed from shells, bone, soil, and artifacts—have been found in including their geographic distribution, economic numerous locations across the Bay Area. Certain shellmounds date back 2,000 years activities, legends, and and more. Many of the shellmounds were also burial sites and may have been used for religious beliefs; and describe ceremonial purposes. Due to the fact that most of the shellmounds were abandoned how they depended on, centuries before the arrival of the Spanish to California, it is unknown whether they are adapted to, and modified the physical environment by related to the California Indians who lived in the Bay Area at that time—the Ohlone and cultivation of land and use of the Coast Miwok. -
The Geography and Dialects of the Miwok Indians
UNIVERSITY OF CALIFORNIA PUBLICATIONS IN AMERICAN ARCHAEOLOGY AND ETHNOLOGY VOL. 6 NO. 2 THE GEOGRAPHY AND DIALECTS OF THE MIWOK INDIANS. BY S. A. BARRETT. CONTENTS. PAGE Introduction.--...--.................-----------------------------------333 Territorial Boundaries ------------------.....--------------------------------344 Dialects ...................................... ..-352 Dialectic Relations ..........-..................................356 Lexical ...6.................. 356 Phonetic ...........3.....5....8......................... 358 Alphabet ...................................--.------------------------------------------------------359 Vocabularies ........3......6....................2..................... 362 Footnotes to Vocabularies .3.6...........................8..................... 368 INTRODUCTION. Of the many linguistic families in California most are con- fined to single areas, but the large Moquelumnan or Miwok family is one of the few exceptions, in that the people speaking its various dialects occupy three distinct areas. These three areas, while actually quite near together, are at considerable distances from one another as compared with the areas occupied by any of the other linguistic families that are separated. The northern of the three Miwok areas, which may for con- venience be called the Northern Coast or Lake area, is situated in the southern extremity of Lake county and just touches, at its northern boundary, the southernmost end of Clear lake. This 334 University of California Publications in Am. Arch. -
Chapter 2. Native Languages of West-Central California
Chapter 2. Native Languages of West-Central California This chapter discusses the native language spoken at Spanish contact by people who eventually moved to missions within Costanoan language family territories. No area in North America was more crowded with distinct languages and language families than central California at the time of Spanish contact. In the chapter we will examine the information that leads scholars to conclude the following key points: The local tribes of the San Francisco Peninsula spoke San Francisco Bay Costanoan, the native language of the central and southern San Francisco Bay Area and adjacent coastal and mountain areas. San Francisco Bay Costanoan is one of six languages of the Costanoan language family, along with Karkin, Awaswas, Mutsun, Rumsen, and Chalon. The Costanoan language family is itself a branch of the Utian language family, of which Miwokan is the only other branch. The Miwokan languages are Coast Miwok, Lake Miwok, Bay Miwok, Plains Miwok, Northern Sierra Miwok, Central Sierra Miwok, and Southern Sierra Miwok. Other languages spoken by native people who moved to Franciscan missions within Costanoan language family territories were Patwin (a Wintuan Family language), Delta and Northern Valley Yokuts (Yokutsan family languages), Esselen (a language isolate) and Wappo (a Yukian family language). Below, we will first present a history of the study of the native languages within our maximal study area, with emphasis on the Costanoan languages. In succeeding sections, we will talk about the degree to which Costanoan language variation is clinal or abrupt, the amount of difference among dialects necessary to call them different languages, and the relationship of the Costanoan languages to the Miwokan languages within the Utian Family. -
Ethnohistory and Ethnogeography of the Coast Miwok and Their Neighbors, 1783-1840
ETHNOHISTORY AND ETHNOGEOGRAPHY OF THE COAST MIWOK AND THEIR NEIGHBORS, 1783-1840 by Randall Milliken Technical Paper presented to: National Park Service, Golden Gate NRA Cultural Resources and Museum Management Division Building 101, Fort Mason San Francisco, California Prepared by: Archaeological/Historical Consultants 609 Aileen Street Oakland, California 94609 June 2009 MANAGEMENT SUMMARY This report documents the locations of Spanish-contact period Coast Miwok regional and local communities in lands of present Marin and Sonoma counties, California. Furthermore, it documents previously unavailable information about those Coast Miwok communities as they struggled to survive and reform themselves within the context of the Franciscan missions between 1783 and 1840. Supplementary information is provided about neighboring Southern Pomo-speaking communities to the north during the same time period. The staff of the Golden Gate National Recreation Area (GGNRA) commissioned this study of the early native people of the Marin Peninsula upon recommendation from the report’s author. He had found that he was amassing a large amount of new information about the early Coast Miwoks at Mission Dolores in San Francisco while he was conducting a GGNRA-funded study of the Ramaytush Ohlone-speaking peoples of the San Francisco Peninsula. The original scope of work for this study called for the analysis and synthesis of sources identifying the Coast Miwok tribal communities that inhabited GGNRA parklands in Marin County prior to Spanish colonization. In addition, it asked for the documentation of cultural ties between those earlier native people and the members of the present-day community of Coast Miwok. The geographic area studied here reaches far to the north of GGNRA lands on the Marin Peninsula to encompass all lands inhabited by Coast Miwoks, as well as lands inhabited by Pomos who intermarried with them at Mission San Rafael. -
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. -
On the Ethnolinguistic Identity of the Napa Tribe: the Implications of Chief Constancio Occaye's Narratives As Recorded by Lorenzo G
UC Merced Journal of California and Great Basin Anthropology Title On the Ethnolinguistic Identity of the Napa Tribe: The Implications of Chief Constancio Occaye's Narratives as Recorded by Lorenzo G. Yates Permalink https://escholarship.org/uc/item/3k52g07t Journal Journal of California and Great Basin Anthropology, 26(2) ISSN 0191-3557 Author Johnson, John R Publication Date 2006 eScholarship.org Powered by the California Digital Library University of California Journal of California and Great Basin Anthropology | Vol. 26, No. 2 (2006) | pp. 193-204 REPORTS On the Ethnolinguistic of foUdore, preserved by Yates, represent some of the only knovra tradhions of the Napa tribe, and are thus highly Identity of the Napa Tribe: sigiuficant for anthropologists mterested m comparative The Implications of oral hterature in Native California. Furthermore, the Chief Constancio Occaye^s native words m these myths suggest that a reappraisal of Narratives as Recorded the ethnohnguistic identhy of the Napa people may be by Lorenzo G. Yates in order. BACKGROUND JOHN R. JOHNSON Santa Barbara Museum of Natural History Lorenzo Gordin Yates (1837-1909) was an English 2559 Puesta del Sol, Santa Barbara, CA 93105 immigrant who came to the United States as a teenager. He became a dentist by profession, but bad a lifelong About 1876, Lorenzo G. Yates interviewed Constancio passion for natural history. Yates moved his famUy from Occaye, described as the last "Chief of the Napas," and Wisconsm to California in 1864 and settled m CentreviUe recorded several items of folklore from his tribe. Yates in Alameda County, which later became a district of included Constancio's recollections about the use of Fremont. -
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.