Fossil Birds from Manix Lake California
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Proceedings of the Third Conference on Fossil Resources in the National Park Service
^^ ;&J Proceedings of the Third Conference on Fossil Resources in the National Park Service Rachel Benton and Ann Elder, Editors Natural Resources Report NPS/NRFOBU/NRR-94/14 °>%HIL M©^m United States Department of the Interior • National Park Service Rocky Mountain Region • Fossil Butte National Monument The National Park Service disseminates reports on high priority, current resource management information, with application for managers, through the Natural Resources Report Series. Technologies and resource management methods; how to resource management papers; popular articles through the yearly highlights report; proceedings on resource management workshops or conferences; and natural resources program recommendations and descriptions and resource action plans are also disseminated through this series. Documents in this series usually contain information of a preliminary nature and are prepared primarily for internal use within the National Park Service. This information is not intended for use in the open literature. Mention of trade names or commercial products does not constitute endorsement or recommenda- tion for use by the National Park Service. Copies of this report are available from the following: Publications Coordinator National Park Service Natural Resources Publication Office P.O. Box 25287 (WASO-NRPO) Denver, CO 80225-0287 CfO Printed on Recycled Paper Proceedings of the Third Conference on Fossil Resources in the National Park Service 14-17 September 1992 Fossil Butte National Monument, Wyoming Editors: Rachel Benton -
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. -
2009 BLM Facts
BLM Oregon & Washington Bureau of Land Management of Bureau U.S. Department of the Interior the Interior of U.S. Department Oregon & Washington Bureau of Land Management BLM/OR/WA/AE-10/074+1792 The Bureau of Land Management Welcomes You to Oregon & Washington! Oregon & Washington i Welcome n early 2010, President Obama announced America’s Great Outdoors initiative Ito conserve our cherished lands and encourage Americans to enjoy the outdoors. And in this I’m reminded of William Shakespeare’s quote, “One touch of nature makes the whole world kin.” Throughout my years of experience, this great notion still rings true. I can attest that Americans have grown closer by the simple virtue of spending time together in nature. And it is on this note that I am thrilled to present our 2009 edition of BLM Facts. Between 96 pages of photos, maps, and detailed facts, I’m very pleased to highlight the diversity of the BLM’s multiple use mission. We serve the public lands by accomplishing what is perhaps the most extensive range of duties by any one agency. BLM foresters use scientific methods to plan for a sustainable growth of trees which also provide a healthy environment while still affording Americans homes, offices, and jobs. Our recreation planners and interpretive specialists present inspirational educational events and breathtaking locations for Americans to visit and create long-lasting memories. Resource specialists care for our special areas protected under the National Landscape Conservation System. Scientists at the BLM complete crucial research using the most current data to ensure we maintain these lands for future generations. -
Quaternary Studies Near Summer Lake, Oregon Friends of the Pleistocene Ninth Annual Pacific Northwest Cell Field Trip September 28-30, 2001
Quaternary Studies near Summer Lake, Oregon Friends of the Pleistocene Ninth Annual Pacific Northwest Cell Field Trip September 28-30, 2001 springs, bars, bays, shorelines, fault, dunes, etc. volcanic ashes and lake-level proxies in lake sediments N Ana River Fault N Paisley Caves Pluvial Lake Chewaucan Slide Mountain pluvial shorelines Quaternary Studies near Summer Lake, Oregon Friends of the Pleistocene Ninth Annual Pacific Northwest Cell Field Trip September 28-30, 2001 Rob Negrini, Silvio Pezzopane and Tom Badger, Editors Trip Leaders Rob Negrini, California State University, Bakersfield, CA Silvio Pezzopane, United States Geological Survey, Denver, CO Rob Langridge, Institute of Geological and Nuclear Sciences, Lower Hutt, New Zealand Ray Weldon, University of Oregon, Eugene, OR Marty St. Louis, Oregon Department of Fish and Wildlife, Summer Lake, Oregon Daniel Erbes, Bureau of Land Management, Carson City, Nevada Glenn Berger, Desert Research Institute, University of Nevada, Reno, NV Manuel Palacios-Fest, Terra Nostra Earth Sciences Research, Tucson, Arizona Peter Wigand, California State University, Bakersfield, CA Nick Foit, Washington State University, Pullman, WA Steve Kuehn, Washington State University, Pullman, WA Andrei Sarna-Wojcicki, United States Geological Survey, Menlo Park, CA Cynthia Gardner, USGS, Cascades Volcano Observatory, Vancouver, WA Rick Conrey, Washington State University, Pullman, WA Duane Champion, United States Geological Survey, Menlo Park, CA Michael Qulliam, California State University, Bakersfield, -
A Portion of South-Central Oregon
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR WATER-SUPPLY PAPER 220 GEOLOGY AND WATER RESOURCES OF A PORTION OF SOUTH-CENTRAL OREGON BY GERALD A. WARING WASHINGTON GOVERNMENT FEINTING OFFICE 1908 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIKEOTOK WATER-SUPPLY PAPER 22O GEOLOGY AND WATER RESOURCES OF A PORTION OF SOUTH-CENTRAL OREGON BY GERALD A. WARING WASHINGTON GOVERNMENT PRINTING OFFICE 1908 CONTENTS. Vage. Introduction.............................................................. 7 Objects of reconnaissance.............................................. 7 Area examined........................................................ 7 Acknowledgements..................................................... 8 Previous study......................................................... 8 Geography................................................................. 9 General features....................................................... 9 Topography............................................................. 9 Mountains........................................................ 9 Scarps.............................................................. 9 Minor features..................................................... 10 Lakes.................................................................. 11 Character of the lakes................................................ 12 Alkalinity........................................................ 12 . Climate............................................................... -
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. -
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. -
The California Deserts: an Ecological Rediscovery
3Pavlik-Ch1 10/9/07 6:43 PM Page 15 Rediscovery Copyrighted Material 3Pavlik-Ch1 10/9/07 6:43 PM Page 16 Copyrighted Material 3Pavlik-Ch1 10/9/07 6:43 PM Page 17 Indians first observed the organisms, processes, and history of California deserts. Over millennia, native people obtained knowledge both practical and esoteric, necessitated by survival in a land of extremes and accumulated by active minds recording how nature worked. Such knowledge became tradition when passed across generations, allowing cul- tural adjustments to the changing environment. The depth and breadth of their under- standing can only be glimpsed or imagined, but should never be minimized. Indians lived within deserts, were born, fed, and raised on them, su¤ered the extremes and uncertainties, and passed into the ancient, stony soils. Theirs was a discovery so intimate and spiritual, so singular, that we can only commemorate it with our own 10,000-year-long rediscov- ery of this place and all of its remarkable inhabitants. Our rediscovery has only begun. Our rediscovery is not based upon living in the deserts, despite a current human pop- ulation of over one million who dwelling east of the Sierra. We do not exist within the ecological context of the land. We are not dependant upon food webs of native plants and [Plate 13] Aha Macav, the Mojave people, depicted in 1853. (H. B. Molhausen) REDISCOVERY • 17 Copyrighted Material 3Pavlik-Ch1 10/9/07 6:43 PM Page 18 Gárces 1776 Kawaiisu Tribal groups Mono Mono Tribe Lake Aviwatha Indian place name Paiute Inyo Owens Valley -
SOUTHEASTSOUTHEAST OREGON 234 Photographing Oregon Southeast Oregon 235
Owyhee Lake at Leslie Gulch Chapter 12 SOUTHEASTSOUTHEAST OREGON 234 Photographing Oregon Southeast Oregon 235 change quickly to howling winds. Unlike the western part of the state, there’s not much chance you’ll run into a bear out here, but it is definitely rattlesnake coun- try. It’s an area of sparse human population, and most of the people who live here like it that way. Cowboy is spoken here. A good way to begin your exploration of this fascinating part of the state is by traveling the Oregon Outback National Scenic Byway, breaking away from the Cascades and journeying south and east into the Great Basin via OR 31. Fort Rock Rising up out of surrounding sagebrush desert, Fort Rock is a towering jagged rock formation, technically a tuff ring, set in an ancient seabed. It is also perhaps the most famous anthropological site in Oregon, as a pair of 9,000–year old sagebrush bark sandals were discovered here. Trails lead up into the bowl of this crater-like formation, and you can scramble to the top for views of the surround- ing desert. Fort Rock has been designated a National Natural Landmark, and an Oregon State Parks interpretive display at the base of the rock does a good job of Lone tree in Harney Valley ranch country near Burns relating the natural and human history of the area. The town of Fort Rock has a museum with several pioneer-days buildings that have good potential for ghost town-like photographs. Hours and access are SOUTHEAST OREGON limited so you can’t get the best angles during the golden hours, but it is possible to make some nice images from the parking area at those times. -
Vol. 23, No. the ORE.-BIN January 1961 STATE of OREGON Portland
THE ORE BIN Volume 23, 1961 Vol. 23, No. THE ORE.-BIN January 1961 STATE OF OREGON Portland, Oregon DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES Head Office: 1069 State Office Bldg., Portland 1, Oregon Telephone: CApitol 6-2161, Ext. 488 State Governing Board Hollis M. Dole, Director William Kennedy, Chairman, Portland Harold Banta Baker Stoff Earl S. Mollard Riddle R. G. Bowen Geologist Field Offices R. E. Corcoran Geologist 2033 First Street, Boker L. L. Hoogland Assayer and Chemist N. S. Wagner, Field Geologist Rolph S. Mason Mining Engineer H. C. Brooks, Field Geologist T. C. Matthews Spectroscopist 239 S. E. "H" Street, Grants Pass V. C. Newton, Jr. Petroleum Engineer Len Ramp, Field Geologist H. G. Schlicker Geologist Norman Peterson, Field Geologist M. L. Steere Geologist * * * * * * * * * * * * * * * * * * OREGON MINERAL PRODUCTION IN 1960 By Ralph S. Mason* Oregon's mineral industry produced its second highest value of row minerals in 1960. Following a nation-wide economic trend during the year, the industry was off approximately $3 million from lost year's record-breaking high of $49.8 million, according to preliminary estimates mode by the U. S. Bureau of Mines. The heavy construction commodities, crushed stone and sand and grovel, reflected construction log and were responsible for most of the change from lost year. Metal mining, aside from nickel, was quiet. The state's only uronium mine and one of the two mercury producers shut down. Industrial mineral products showed both gains and losses as compared to the previous year. Cement production was up 12 percent while clays declined 15 percent and diatomite 3 percent.