La Jolla Natural Radiocarbon Measurements IV
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The Archaeology and Paleoclimate of the Mud Lake Basin, Nye County, Nevada
University of Nevada, Reno Changing Landscapes During the Terminal Pleistocene/Early Holocene: The Archaeology and Paleoclimate of the Mud Lake Basin, Nye County, Nevada A thesis submitted in partial fulfillment of the requirements for the degree of Masters of Arts in Anthropology By Lindsay A. Fenner Dr. Geoffrey M. Smith/Thesis Advisor May, 2011 © by Lindsay A. Fenner 2011 All Rights Reserved THE GRADUATE SCHOOL We recommend that the thesis prepared under our supervision by LINDSAY A. FENNER entitled Changing Landscapes During The Terminal Pleistocene/Early Holocene: The Archaeology And Paleoclimate Of The Mud Lake Basin, Nye County, Nevada be accepted in partial fulfillment of the requirements for the degree of MASTER OF ARTS Geoffrey M. Smith, Ph.D., Advisor Gary Haynes, Ph.D., Committee Member Kenneth D. Adams, Ph.D., Graduate School Representative Marsha H. Read, Ph. D., Associate Dean, Graduate School May, 2011 i ABSTRACT Archaeological investigation along Pleistocene lakeshores is a longstanding and common approach to prehistoric research in the Great Basin. Continuing in this tradition, this thesis considers the archaeological remains present from pluvial Mud Lake, Nye County, Nevada coupled with an examination of paleoclimatic conditions to assess land-use patters during the terminal Pleistocene/early Holocene. Temporally diagnostic lithic assemblages from 44 localities in the Mud Lake basin provide the framework for which environmental proxy records are considered. Overwhelmingly occupied by Prearchaic groups, comprising 76.6% of all diagnostic artifacts present, Mud Lake was intensively utilized right up to its desiccation after the Younger Dryas, estimated at 9,000 radiocarbon years before present. Intermittently occupied through the remainder of the Holocene, different land-use strategies were employed as a result of shifting subsistence resources reacting to an ever changing environment. -
UNIVERSITY of CALIFORNIA Los Angeles Southern California
UNIVERSITY OF CALIFORNIA Los Angeles Southern California Climate and Vegetation Over the Past 125,000 Years from Lake Sequences in the San Bernardino Mountains A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Geography by Katherine Colby Glover 2016 © Copyright by Katherine Colby Glover 2016 ABSTRACT OF THE DISSERTATION Southern California Climate and Vegetation Over the Past 125,000 Years from Lake Sequences in the San Bernardino Mountains by Katherine Colby Glover Doctor of Philosophy in Geography University of California, Los Angeles, 2016 Professor Glen Michael MacDonald, Chair Long sediment records from offshore and terrestrial basins in California show a history of vegetation and climatic change since the last interglacial (130,000 years BP). Vegetation sensitive to temperature and hydroclimatic change tended to be basin-specific, though the expansion of shrubs and herbs universally signalled arid conditions, and landscpe conversion to steppe. Multi-proxy analyses were conducted on two cores from the Big Bear Valley in the San Bernardino Mountains to reconstruct a 125,000-year history for alpine southern California, at the transition between mediterranean alpine forest and Mojave desert. Age control was based upon radiocarbon and luminescence dating. Loss-on-ignition, magnetic susceptibility, grain size, x-ray fluorescence, pollen, biogenic silica, and charcoal analyses showed that the paleoclimate of the San Bernardino Mountains was highly subject to globally pervasive forcing mechanisms that register in northern hemispheric oceans. Primary productivity in Baldwin Lake during most of its ii history showed a strong correlation to historic fluctuations in local summer solar radiation values. -
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Questions about Lake Manly’s age, extent, and source Michael N. Machette, Ralph E. Klinger, and Jeffrey R. Knott ABSTRACT extent to form more than a shallow n this paper, we grapple with the timing of Lake Manly, an inconstant lake. A search for traces of any ancient lake that inundated Death Valley in the Pleistocene upper lines [shorelines] around the slopes Iepoch. The pluvial lake(s) of Death Valley are known col- leading into Death Valley has failed to lectively as Lake Manly (Hooke, 1999), just as the term Lake reveal evidence that any considerable lake Bonneville is used for the recurring deep-water Pleistocene lake has ever existed there.” (Gale, 1914, p. in northern Utah. As with other closed basins in the western 401, as cited in Hunt and Mabey, 1966, U.S., Death Valley may have been occupied by a shallow to p. A69.) deep lake during marine oxygen-isotope stages II (Tioga glacia- So, almost 20 years after Russell’s inference of tion), IV (Tenaya glaciation), and/or VI (Tahoe glaciation), as a lake in Death Valley, the pot was just start- well as other times earlier in the Quaternary. Geomorphic ing to simmer. C arguments and uranium-series disequilibrium dating of lacus- trine tufas suggest that most prominent high-level features of RECOGNITION AND NAMING OF Lake Manly, such as shorelines, strandlines, spits, bars, and tufa LAKE MANLY H deposits, are related to marine oxygen-isotope stage VI (OIS6, In 1924, Levi Noble—who would go on to 128-180 ka), whereas other geomorphic arguments and limited have a long and distinguished career in Death radiocarbon and luminescence age determinations suggest a Valley—discovered the first evidence for a younger lake phase (OIS 2 or 4). -
Geology of the Panamint Butte Quadrangle, Inyo County, California
Geology of the Panamint Butte Quadrangle, Inyo County, California By WAYNE E; HALL GEOLOGICAL SURVEY BULLETIN 1299 Prepared in cooperation with the California Department of Conservation, Division of Mines and Geology KhCEIVED JUL161971 u.8.1 teuisfiUt, it UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1971 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 75-610447 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract_________________________________-_.-______-__--_-_--_--- 1 Introduction. ___________-______--_____--_----.--___--__-__--------- 2 Climate.and vegetation._________.__....__.._____-___________-__ 3 Water supply-________________________________________________ 3 Previous work__________________________.___._____._1________ 4 Acknowledgments- _______________._______..____-__-_---------_- 4 General geology.__________________________-__..____--_----_-_--__-- 5 Precambrian(?) rocks._____________.__________.._----___-___-_-_-__- 7 Paleozoic rocks._____.__.___--________-___-____-_-----_---_--.-.-_- 8 Cambrian System_____________________________________________ 8 Carrara Formation.__________________..-_____--____---__-_- 8 Bonanza King Formation___._.______..__._._.....____.____ 10 Nopah Formation._____...____-_-_.....____________-_-_-__- 11 Ordovician System___________________________________________ 13 Pogonip Group_____-__-______-____-_-..----------_--._-_-_- 13 Eureka Quartzite.______________-_____..___-_-_---_-----_--_ 16 Ely Springs Dolomite__---__-______________________________ 18 Silurian and Devonian Systems___________..__-_-__----_-__-___- 21 Hidden Valley Dolomite......._____________________________ 21 Devonian System_____________________________________________ 22 Lost Burro Formation.....__________________________________ 22 Mississippian System.___._____..____._.._..__.___..._._._..__. -
Jay Von Werlhof Imperial Valley College Desert Museum El Centro, California
DISTRIBUTION AS A FUNCTIONAL FACTOR OF ROCK ALIGNMENTS IN THE MOJAVE DESERT Jay Von Werlhof Imperial Valley College Desert Museum El Centro, California ABSTRACT This paper suggests that the distribution, setting, content, and form of early rock alignments in the Mojave Desert are directly related to the function of these features. Each of these factors will be described and discussed in turn, leading to an interpretive synthesis. Why a reliable model cannot be developed for locating rock alignment sites is also suggested. I am pleased to have been invited to present a paper in this noted also that a few isolated sites are uniquely present, which session honoring Dee Simpson. I have admired her life-long is another concern of research. Such sites, for example, might devotion to archaeology and the tenacity with which she works have been in the process of being developed into larger and toward goal completions. I am also indebted to her, along more complex sites but were never completed, as possibly that with Arda Haenzel, her co-worker at the San Bernardino at Lavic Lake (MacDonald 1993). Also, in complex sites con County Museum, for interesting me in earthen art back in taining numerous designs it is not clear whether the diverse el 1975 when few others thought that path worth treading. Since ements are even temporally related, or if each design exists as then, I have worked to advance the study of geogylphs and rock an entity from a different era. However, this type of earthen art alignments, and the paper I am presenting today is drawn appears to have been the earliest, and its association with the around a small sector of that study: distribution as a functional Lake Hill Pleistocene site (Davis 1978) focuses the Panamint factor of rock alignments in the Mojave Desert. -
Fossil Birds from Manix Lake California
Fossil Birds From Manix Lake California By HILDEGARDE HOWARD A SHORTER CONTRIBUTION TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 264-J Descriptions of late Pleistocene bira remains, including a new species offlamingo UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1955 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price 40 cents (paper cover) CONTENTS Page Page Abstract--__-_-----___-__-__-_--___________________ 199 Description of specimens—Continued Introduction _______________________________________ 199 Branta canadensis (Linnaeus)_--____--_____-_-___- 203 Description of specimens_____________________________ 201 Nyroca valisineria (Wilson) ?____________________- 203 Aechmophorus occidentalis (Lawrence)_____________ 201 Erismatura jamaicensis (Gmelin)__________________ 204 Pelecanus erythrorhynchos Gmelin_________________ 202 Aquila chrysaetos (Linnaeus)_____________________ 204 Phalacrocorax auritus (Lesson) ?_________________ 202 (?rws?_______________-_-______-____-_--__- 204 Ciconia maltha Miller_____.______________________ 202 Family Phalaropodidae__________________________ 204 Phoenicopterus copei Shufeldt?_.__________________ 202 Summary and conclusions__________________________ 204 Phoenicopterus minutus Howard, new species_ ______ 202 Literature cited___________________________________ 205 ILLUSTRATIONS PLATE 50. Phoenicopterus minutus Howard, new -
Nevada Archaeologist Volume 15 1997
NEVADA ARCHAEOLOGIST VOLUME 15 1997 NEV ADA ARCHAEOLOGICAL ASSOCIATION NEVADA Nevada and has no paid employees. The purpose of ARCHAEOLOGICAL NAA is to preserve Nevada's antiquities, encourage the ASSOCIATION study of archaeology, and to educate the public to the aims of archaeological research. Membership is open to any person signing the NAA Code of Ethics who is The design for the NAA logo was interested in archaeology and its allied sciences, and in adapted by Robert Elston from a the conservation of archaeological resources, Garfield Flat petroglyph. particularly in Nevada. Requests for membership and dues should be sent to the Executive Secretary at the address provided below. Make all checks and/or NEVADA ARCHAEOLOGICAL ASSOCIATION OFFICERS money orders payable to the Nevada Archaeological Association. Membership cards will be issued on the PRESIDENT BILL JOHNSON ................. 566-4390 payment of dues and the receipt of a signed Code of HENDERSON, NEVADA Ethics. Active members receive issues of the Association's newsletter, In Situ, and one copy of the SECRETARY PAT HICKS ....................... 565-1709 annual publication, Nevada Archaeologist. Members HENDERSON, NEVADA also meet once a year for paper presentations and the annual banquet at various locations throughout Nevada. TREASURER QYVIND FROCK ............... 826-8779 RENO,NEVADA DUES EDITOR, VOLUME 15 WILLIAM WHITE STUDENT ................................ $5.00 HENDERSON,NEVADA ACTIVE .................................. $12.00 ACTIVE FAMILY ..................... $15.00 1997 BOARD OF DIRECTORS SUPPORTING .......................... $25.00 SPONSOR ............................... $50.00 The Board of Directors of the Nevada Archaeological PATRON ................................ $100.00 Association is elected annually by the membership. Board members serve one year terms. Directors elect FuTURE ISSUES OF THE NEVADA ARCHAEOLOGIST the Association's officers from those members elected to the Board. -
The Pueblo in the Mojave Sink: an Archaeological Myth
California State University, San Bernardino CSUSB ScholarWorks Theses Digitization Project John M. Pfau Library 2002 The pueblo in the Mojave Sink: An archaeological myth Barbara Ann Loren-Webb Follow this and additional works at: https://scholarworks.lib.csusb.edu/etd-project Part of the Archaeological Anthropology Commons Recommended Citation Loren-Webb, Barbara Ann, "The pueblo in the Mojave Sink: An archaeological myth" (2002). Theses Digitization Project. 2107. https://scholarworks.lib.csusb.edu/etd-project/2107 This Thesis is brought to you for free and open access by the John M. Pfau Library at CSUSB ScholarWorks. It has been accepted for inclusion in Theses Digitization Project by an authorized administrator of CSUSB ScholarWorks. For more information, please contact [email protected]. THE PUEBLO IN THE MOJAVE SINK: AN ARCHAEOLOGICAL MYTH A Thesis Presented to the Faculty of California State University, San Bernardino In Partial Fulfillment of the Requirements for the Degree Masters of Arts in Interdisciplinary Studies by Barbara Ann Loren-Webb March 2003 THE PUEBLO IN THE MOJAVE SINK: AN ARCHAEOLOGICAL MYTH A Thesis Presented to the Faculty of California State University, San Bernardino by Barbara Ann Loren-Webb March 2003 Approved by: Russell Barber, Chair, Anthropology Date Pete Robertshesw, Anthropology ABSTRACT In 1929 Malcolm Rogers published a paper in which he stated that there was evidence of an Anasazi or Puebloan settlement or pueblo, in the Mojave Sink Region of the Mojave Desert. Since then, archaeologists have cited Rogers' publication and repeated his claim that such a pueblo was located in the Western Mojave Desert. The purpose of this thesis started out as a review of the existing evidence and to locate this pueblo. -
Springsnails (Gastropoda, Hydrobiidae) of Owens and Amargosa River California-Nevada
Springsnails (Gastropoda, Hydrobiidae) Of Owens And Amargosa River California-Nevada R Hershler Proceedings of The Biological Society of Washington 102:176-248 (1989) http://biostor.org/reference/74590 Page images from the Biodiversity Heritage Library, http://www.biodiversitylibrary.org/, made available under a Creative Commons Attribution-Noncommercial License http://creativecommons.org/licenses/by-nc/2.5/ PROC. BtOL SOC. WASH. 102(t). t989, pp. 176-248 SPRINGSNAILS (GASTROPODA: HYDROBIIDAE) OF OWENS AND AMARGOSA RIVER (EXCLUSIVE OF ASH MEADOWS) DRAINAGES, DEATH VALLEY SYSTEM, CALIFORNIA-NEVADA Robert Hershler Abstract. - Thirteen springsnail species (9 new) belonging to Pyrgulopsis Call & Pilsbry, 1886, and Tryonia Stimpson, 1865 aTe recorded from the region encompassing pluvial Owens and Amargosa River (exclusive of Ash Meadows) drainages in southeastern California and southwestern Nevada. Discriminant analyses utilizing shell morphometric data confirmed distinctiveness of the nine new species described herein, as: Pyrgulopsis aardahli, P. amargosae, P. olVenensis, P. perlubala, P. wongi, Tyronia margae, T. robusla, T. rowlandsi, and 1: salina. Of the 22 springsnails known from Death Valley System, 17 have very localized distributi ons, with endemic fauna concentrated in Owens Valley, Death Valley, and Ash Meadows. A preliminary analysis showed only partial correlation betwecn modern springs nail zoogeography and configuration of inter·connected Pleistocene lakes comprising the Death Valley System. This constitutes the second part of a sys List of Recognized Taxa tematic treatment of springsnails from the Pyrgu/opsis aardah/i, new species. Death Valley System, a large desert region P. amargosac. new species. in southeastern California and southwest P. micrococcus (Pilsbry. 1893). ern Nevada integrated by a se ries of la kes P. -
Geology and Soils
3.7 GEOLOGY AND SOILS This section of the Program Environmental Impact Report (PEIR) describes the geological characteristics of the SCAG region, identifies the regulatory framework with respect to laws and regulations that govern geology and soils, and analyzes the significance of the potential impacts that could result from development of the Connect SoCal Plan (“Connect SoCal”; “Plan”). In addition, this PEIR provides regional-scale mitigation measures as well as project-level mitigation measures to be considered by lead agencies for subsequent, site-specific environmental review to reduce identified impacts as appropriate and feasible. Information regarding paleontological resources was largely obtained from the Paleontological Resources Report prepared by SWCA and included as Appendix 3.7 of this PEIR. 3.7.1 ENVIRONMENTAL SETTING 3.7.1.1 Definitions Alluvium: An unconsolidated accumulation of stream deposited sediments, including sands, silts, clays or gravels. Extrusive Igneous Rocks: Rocks that crystallize from molten magma on earth’s surface. Fault: A fracture or fracture zone in rock along which movement has occurred. Formation: A laterally continuous rock unit with a distinctive set of characteristics that make it possible to recognize and map from one outcrop or well to another. The basic rock unit of stratigraphy. Holocene: An interval of time relating to, or denoting the present epoch, which is the second epoch in the Quaternary period, from approximately 11,000 years ago to the present time. Liquefaction: The process by which water-saturated sandy soil materials lose strength and become susceptible to failure during strong ground shaking in an earthquake. The shaking causes the pore-water pressure in the soil to increase, thus transforming the soil from a stable solid to a more liquid form. -
Zzyzx Mineral Springs— Cultural Treasure and Endangered Species Aquarium
Cultural and Natural Resources: Conflicts and Opportunities for Cooperation Zzyzx Mineral Springs— Cultural Treasure and Endangered Species Aquarium Danette Woo, Mojave National Preserve, 222 East Main Street, Suite 202, Barstow, California 92311; [email protected] Debra Hughson, Mojave National Preserve, 222 East Main Street, Suite 202, Barstow, California 92311; [email protected] A Brief History of Zzyzx Human use has been documented at Soda Dry Lake back to the early predecessors of the Mohave and Chemehuevi native peoples, who occupied the land when the Spanish explorers first explored the area early in the 19th century. Soda Springs lies in the traditional range of the Chemehuevi, who likely used and modified the area in pursuit of their hunter–gatherer econo- my.Trade routes existed between the coast and inland to the Colorado River and beyond for almost as long as humans have occupied this continent. These routes depended on reliable springs, spaced no more than a few days’ walk apart, and Soda Springs has long been a reliable oasis in a dehydrated expanse. The first written record of Soda Springs Soda Springs, dubbed “Hancock’s Redoubt” comes from the journals of Jedediah Strong for Winfield Scott Hancock, the Army Smith, written in 1827 when he crossed Soda Quartermaster in Los Angeles at the time. The Lake on his way to Mission San Gabriel. Army’s presence provided a buffer between Smith was the first American citizen to enter the emigrants from the East and dispossessed California by land. He crisscrossed the west- natives. California miners also traveled the ern half of the North American continent by Mojave Road on their way to the Colorado foot and pack animal from 1822 until he was River in 1861. -
BLM Worksheets
Panamint/Argus Description/Location: Panamint/Argus, subdivided into 2 units: Panamint Lake Unit and the Mountain Unit. Located between Argus Wilderness and Death Valley National Park. Nationally Significant Values: Ecological: This area encompasses an essential movement corridor which links wildlife habitats in the China Lake Naval Air Weapons Station and Argus Wilderness to those protected by the Death Valley National Park. This corridor was developed by the SC Wildlands group (Science and Collaboration for Connected Wildlands). SC Wildlands was part of a team that worked with the California Departments of Transportation and Fish and Game on a statewide habitat connectivity effort from which this unit was developed. The habitat suitability and movement needs of over 40 selected focal species were used in this process. Desert Bighorn sheep and Mojave ground squirrels are two of those focal species that occur here. In addition, the area provides excellent habitat for foraging and nesting of numerous raptor species, including golden eagles and prairie falcons. The Slate, Argus, and Panamint Mountain ranges would be included in this large unit. These ranges provide habitat for Nelson's desert bighorn sheep, Townsend’s big‐eared bats, and the federally threatened Inyo California towhee. The abandoned mines in this area have historically housed the largest maternity colonies of Townsend’s big‐eared bats in the Western Mojave Desert. It is likely that unsurveyed mines in the Slates and Argus Range also house large colonies. The area also includes Mohave ground squirrel (MGS) core habitat within the MGS Conservation Area. This is 1 of only 11 core population centers.