Past, Present and Future Issues in Great Basin Archaeology: Papers in Honor of Don D
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Great Basin Landscape Conservation Cooperative
September 2010 The Great Basin Landscape Conservation Cooperative What is a Landscape Conservation The Great Basin Landscape Cooperative? Conservation Cooperative Landscape Conservation Cooperatives (LCCs) are applied science and management partnerships between Interior Department bureaus and others involved in natural resource management and What is the Great Basin LCC? conservation. Secretarial Order No. 3289, issued on Sept. 14, 2009 The Great Basin LCC will be a self-directed partnership. The by Interior Secretary Ken Salazar, calls for the establishment of 21 Great Basin LCC will provide a range of scientific and technical LCCs nationwide to better integrate science and management to support tools for landscape-scale conservation design to a wide address climate change and related issues array of managers. These tools will help managers identify and target biological objectives for native species and habitats in the What will the Great Basin LCC do? face of climate change and other stressors. Open public access to In broad terms, the Great Basin LCC will help link and integrate Great Basin LCC products will promote acceptance and use of Interior’s proposed Climate Science Centers with resource managers the science in regional conservation strategies. This effort is being and science users; will bring additional Interior resources to bear on coordinated with other regional partnerships and will be set up in landscape-scale issues and opportunities; and will help in applying a manner that will facilitate coordination and the identification science and facilitating coordination on a wide range of efforts of needs, capacities and gaps. We will link our efforts to bring to respond to climate change, invasive species, wildfires, human additional science capacity to improve conservation strategies development and other change agents across the Great Basin. -
Ecoregions of Nevada Ecoregion 5 Is a Mountainous, Deeply Dissected, and Westerly Tilting Fault Block
5 . S i e r r a N e v a d a Ecoregions of Nevada Ecoregion 5 is a mountainous, deeply dissected, and westerly tilting fault block. It is largely composed of granitic rocks that are lithologically distinct from the sedimentary rocks of the Klamath Mountains (78) and the volcanic rocks of the Cascades (4). A Ecoregions denote areas of general similarity in ecosystems and in the type, quality, Vegas, Reno, and Carson City areas. Most of the state is internally drained and lies Literature Cited: high fault scarp divides the Sierra Nevada (5) from the Northern Basin and Range (80) and Central Basin and Range (13) to the 2 2 . A r i z o n a / N e w M e x i c o P l a t e a u east. Near this eastern fault scarp, the Sierra Nevada (5) reaches its highest elevations. Here, moraines, cirques, and small lakes and quantity of environmental resources. They are designed to serve as a spatial within the Great Basin; rivers in the southeast are part of the Colorado River system Bailey, R.G., Avers, P.E., King, T., and McNab, W.H., eds., 1994, Ecoregions and subregions of the Ecoregion 22 is a high dissected plateau underlain by horizontal beds of limestone, sandstone, and shale, cut by canyons, and United States (map): Washington, D.C., USFS, scale 1:7,500,000. are especially common and are products of Pleistocene alpine glaciation. Large areas are above timberline, including Mt. Whitney framework for the research, assessment, management, and monitoring of ecosystems and those in the northeast drain to the Snake River. -
The Road to Iconicity in the Pa- Leoart of the American West
ekkehart malotkI The Road to Iconicity in the Pa- leoart of the American West Introduction Throughout the world, all paleoart traditions considered to be the earliest uniformly display a remarkable noniconicity, whether they occur as port- able objects or in the context of rock art. This uniformity is believed to be attributable not to cultural difusion but to an evolved, predisposing neuro- biology shared by all human beings. This panglobal similarity of the most basic phosphene-like motif repertoires also holds for the Pleistocene-Hol- ocene transition period in the American West. From Canada to Northwest Mexico and from Texas to the Paciic Coast, canyon walls, boulder faces and rock shelters served as canvases for the arriving Paleoamericans and their descendants. Their non-igurative, geocentric marking systems, summar- ily labeled here Western Archaic Tradition (Fig. 1), lasted for thousands of years until in very limited areas full-blown iconicity in the form of distinct biocentric styles set in around the Middle Holocene (Fig. 2). Many regions, however, remained committed to the graphic Western Archaic Tradition mode until A. D. 600 or later or never developed representational motifs. Preceding the onset of imagery featuring anthropomorphs and zoomorphs, a seemingly restricted vocabulary of igurative designs –, primarily animal and bird tracks as well as hand- and footprints – that can be regarded as proto-iconic forerunners along the developmental path of rock art, observ- able in the American West. 171171 ekkehart malotkI Fig. 1: Typical WAT petroglyphs from a site north of St. George, Utah (photograph E. Malotki). Fig. 2: Typical »biocentric« style imagery of the Middle/Late Holocene that marks an ideo- logical shift from the long-lasting noniconic rock art of the WAT (photograph E. -
The Museum of Northern Arizona Easton Collection Center 3101 N
MS-372 The Museum of Northern Arizona Easton Collection Center 3101 N. Fort Valley Road Flagstaff, AZ 86001 (928)774-5211 ext. 256 Title Harold Widdison Rock Art collection Dates 1946-2012, predominant 1983-2012 Extent 23,390 35mm color slides, 6,085 color prints, 24 35mm color negatives, 1.6 linear feet textual, 1 DVD, 4 digital files Name of Creator(s) Widdison, Harold A. Biographical History Harold Atwood Widdison was born in Salt Lake City, Utah on September 10, 1935 to Harold Edward and Margaret Lavona (née Atwood) Widdison. His only sibling, sister Joan Lavona, was born in 1940. The family moved to Helena, Montana when Widdison was 12, where he graduated from high school in 1953. He then served a two year mission for the Church of Jesus Christ of Latter-day Saints. In 1956 Widdison entered Brigham Young University in Provo, Utah, graduating with a BS in sociology in 1959 and an MS in business in 1961. He was employed by the Atomic Energy Commission in Washington DC before returning to graduate school, earning his PhD in medical sociology and statistics from Case Western Reserve University in Cleveland, Ohio in 1970. Dr. Widdison was a faculty member in the Sociology Department at Northern Arizona University from 1972 until his retirement in 2003. His research foci included research methods, medical sociology, complex organization, and death and dying. His interest in the latter led him to develop one of the first courses on death, grief, and bereavement, and helped establish such courses in the field on a national scale. -
The Diffusion of Maize to the Southwestern United States and Its Impact
PERSPECTIVE The diffusion of maize to the southwestern United States and its impact William L. Merrilla, Robert J. Hardb,1, Jonathan B. Mabryc, Gayle J. Fritzd, Karen R. Adamse, John R. Roneyf, and A. C. MacWilliamsg aDepartment of Anthropology, National Museum of Natural History, Smithsonian Institution, P.O. Box 37102, Washington, DC 20013-7012; bDepartment of Anthropology, One UTSA Circle, University of Texas at San Antonio, San Antonio, TX 78249; cHistoric Preservation Office, City of Tucson, P.O. Box 27210, Tucson, AZ 85726; dDepartment of Anthropology, Campus Box 1114, One Brookings Drive, Washington University, St. Louis, MO 63130; eCrow Canyon Archaeological Center, 23390 Road K, Cortez, CO 81321; fColinas Cultural Resource Consulting, 6100 North 4th Street, Private Mailbox #300, Albuquerque, NM 87107; and gDepartment of Archaeology, 2500 University Drive Northwest, University of Calgary, Calgary, Alberta, Canada T2N 1N4 Edited by Linda S. Cordell, University of Colorado, Boulder, CO, and approved October 30, 2009 (received for review June 22, 2009) Our understanding of the initial period of agriculture in the southwestern United States has been transformed by recent discoveries that establish the presence of maize there by 2100 cal. B.C. (calibrated calendrical years before the Christian era) and document the processes by which it was integrated into local foraging economies. Here we review archaeological, paleoecological, linguistic, and genetic data to evaluate the hypothesis that Proto-Uto-Aztecan (PUA) farmers migrating from a homeland in Mesoamerica intro- duced maize agriculture to the region. We conclude that this hypothesis is untenable and that the available data indicate instead a Great Basin homeland for the PUA, the breakup of this speech community into northern and southern divisions Ϸ6900 cal. -
Bibliography
Bibliography Many books were read and researched in the compilation of Binford, L. R, 1983, Working at Archaeology. Academic Press, The Encyclopedic Dictionary of Archaeology: New York. Binford, L. R, and Binford, S. R (eds.), 1968, New Perspectives in American Museum of Natural History, 1993, The First Humans. Archaeology. Aldine, Chicago. HarperSanFrancisco, San Francisco. Braidwood, R 1.,1960, Archaeologists and What They Do. Franklin American Museum of Natural History, 1993, People of the Stone Watts, New York. Age. HarperSanFrancisco, San Francisco. Branigan, Keith (ed.), 1982, The Atlas ofArchaeology. St. Martin's, American Museum of Natural History, 1994, New World and Pacific New York. Civilizations. HarperSanFrancisco, San Francisco. Bray, w., and Tump, D., 1972, Penguin Dictionary ofArchaeology. American Museum of Natural History, 1994, Old World Civiliza Penguin, New York. tions. HarperSanFrancisco, San Francisco. Brennan, L., 1973, Beginner's Guide to Archaeology. Stackpole Ashmore, w., and Sharer, R. J., 1988, Discovering Our Past: A Brief Books, Harrisburg, PA. Introduction to Archaeology. Mayfield, Mountain View, CA. Broderick, M., and Morton, A. A., 1924, A Concise Dictionary of Atkinson, R J. C., 1985, Field Archaeology, 2d ed. Hyperion, New Egyptian Archaeology. Ares Publishers, Chicago. York. Brothwell, D., 1963, Digging Up Bones: The Excavation, Treatment Bacon, E. (ed.), 1976, The Great Archaeologists. Bobbs-Merrill, and Study ofHuman Skeletal Remains. British Museum, London. New York. Brothwell, D., and Higgs, E. (eds.), 1969, Science in Archaeology, Bahn, P., 1993, Collins Dictionary of Archaeology. ABC-CLIO, 2d ed. Thames and Hudson, London. Santa Barbara, CA. Budge, E. A. Wallis, 1929, The Rosetta Stone. Dover, New York. Bahn, P. -
Lahontan Cutthroat Trout Species Management Plan for the Upper Humboldt River Drainage Basin
STATE OF NEVADA DEPARTMENT OF WILDLIFE LAHONTAN CUTTHROAT TROUT SPECIES MANAGEMENT PLAN FOR THE UPPER HUMBOLDT RIVER DRAINAGE BASIN Prepared by John Elliott SPECIES MANAGEMENT PLAN December 2004 LAHONTAN CUTTHROAT TROUT SPECIES MANAGEMENT PLAN FOR THE UPPER HUMBOLDT RIVER DRAINAGE BASIN SUBMITTED BY: _______________________________________ __________ John Elliott, Supervising Fisheries Biologist Date Nevada Department of Wildlife, Eastern Region APPROVED BY: _______________________________________ __________ Richard L. Haskins II, Fisheries Bureau Chief Date Nevada Department of Wildlife _______________________________________ __________ Kenneth E. Mayer, Director Date Nevada Department of Wildlife REVIEWED BY: _______________________________________ __________ Robert Williams, Field Supervisor Date Nevada Fish and Wildlife Office U.S.D.I. Fish and Wildlife Service _______________________________________ __________ Ron Wenker, State Director Date U.S.D.I. Bureau of Land Management _______________________________________ __________ Edward C. Monnig, Forest Supervisor Date Humboldt-Toiyabe National Forest U.S.D.A. Forest Service TABLE OF CONTENTS Contents EXECUTIVE SUMMARY ……………………………………………………………………..1 INTRODUCTION……………………………………………………………………………….…2 AGENCY RESPONSIBILITIES……………………………………………………………….…4 CURRENT STATUS……………………………………………………………………………..6 RECOVERY OBJECTIVES……………………………………………………………………19 RECOVERY ACTIONS…………………………………………………………………………21 RECOVERY ACTION PRIORITIES BY SUBBASIN………………………………………….33 IMPLEMENTATION SCHEDULE……………………………………………………………..47 -
Radiocarbon Evidence Relating to Northern Great Basin Basketry Chronology
UC Merced Journal of California and Great Basin Anthropology Title Radiocarbon Evidence Relating to Northern Great Basin Basketry Chronology Permalink https://escholarship.org/uc/item/52v4n8cf Journal Journal of California and Great Basin Anthropology, 20(1) ISSN 0191-3557 Authors Connolly, Thomas J Fowler, Catherine S Cannon, William J Publication Date 1998-07-01 Peer reviewed eScholarship.org Powered by the California Digital Library University of California REPORTS Radiocarbon Evidence Relating ity over a span of nearly 10,000 years (cf. to Northern Great Basin Cressman 1942, 1986; Connolly 1994). Stages Basketry Chronology 1 and 2 are divided at 7,000 years ago, the approximate time of the Mt. Mazama eruption THOMAS J. CONNOLLY which deposited a significant tephra chronologi Oregon State Museum of Anthropology., Univ. of Oregon, Eugene, OR 97403. cal marker throughout the region. Stage 3 be CATHERINE S. FOWLER gins after 1,000 years ago,' when traits asso Dept. of Anthropology, Univ. of Nevada, Reno, NV ciated with Northern Paiute basketmaking tradi 89557. tions appear (Adovasio 1986a; Fowler and Daw WILLIAM J. CANNON son 1986; Adovasio and Pedler 1995; Fowler Bureau of Land Management, Lakeview, OR 97630. 1995). During Stage 1, from 11,000 to 7,000 years Adovasio et al. (1986) described Early ago, Adovasio (1986a: 196) asserted that north Holocene basketry from the northern Great ern Great Basin basketry was limited to open Basin as "simple twined and undecorated. " Cressman (1986) reported the presence of and close simple twining with z-twist (slanting decorated basketry during the Early Holo down to the right) wefts. Fort Rock and Spiral cene, which he characterized as a "climax Weft sandals were made (see Cressman [1942] of cultural development'' in the Fort Rock for technical details of sandal types). -
Quaternary International Colonisation and Early Peopling of The
Quaternary International xxx (xxxx) xxx–xxx Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Colonisation and early peopling of the Colombian Amazon during the Late Pleistocene and the Early Holocene: New evidence from La Serranía La Lindosa ∗ Gaspar Morcote-Ríosa, Francisco Javier Aceitunob, , José Iriartec, Mark Robinsonc, Jeison L. Chaparro-Cárdenasa a Instituto de Ciencias Naturales, Universidad Nacional de Colombia, Bogotá, Colombia b Departamento de Antropología, Universidad de Antioquia, Medellín, Colombia c Department of Archaeology, Exeter, University of Exeter, United Kingdom ARTICLE INFO ABSTRACT Keywords: Recent research carried out in the Serranía La Lindosa (Department of Guaviare) provides archaeological evi- Colombian amazon dence of the colonisation of the northwest Colombian Amazon during the Late Pleistocene. Preliminary ex- Serranía La Lindosa cavations were conducted at Cerro Azul, Limoncillos and Cerro Montoya archaeological sites in Guaviare Early peopling Department, Colombia. Contemporary dates at the three separate rock shelters establish initial colonisation of Foragers the region between ~12,600 and ~11,800 cal BP. The contexts also yielded thousands of remains of fauna, flora, Human adaptability lithic artefacts and mineral pigments, associated with extensive and spectacular rock pictographs that adorn the Rock art rock shelter walls. This article presents the first data from the region, dating the timing of colonisation, de- scribing subsistence strategies, and examines human adaptation to these transitioning landscapes. The results increase our understanding of the global expansion of human populations, enabling assessment of key inter- actions between people and the environment that appear to have lasting repercussions for one of the most important and biologically diverse ecosystems in the world. -
Annotated Atlatl Bibliography John Whittaker Grinnell College Version June 20, 2012
1 Annotated Atlatl Bibliography John Whittaker Grinnell College version June 20, 2012 Introduction I began accumulating this bibliography around 1996, making notes for my own uses. Since I have access to some obscure articles, I thought it might be useful to put this information where others can get at it. Comments in brackets [ ] are my own comments, opinions, and critiques, and not everyone will agree with them. The thoroughness of the annotation varies depending on when I read the piece and what my interests were at the time. The many articles from atlatl newsletters describing contests and scores are not included. I try to find news media mentions of atlatls, but many have little useful info. There are a few peripheral items, relating to topics like the dating of the introduction of the bow, archery, primitive hunting, projectile points, and skeletal anatomy. Through the kindness of Lorenz Bruchert and Bill Tate, in 2008 I inherited the articles accumulated for Bruchert’s extensive atlatl bibliography (Bruchert 2000), and have been incorporating those I did not have in mine. Many previously hard to get articles are now available on the web - see for instance postings on the Atlatl Forum at the Paleoplanet webpage http://paleoplanet69529.yuku.com/forums/26/t/WAA-Links-References.html and on the World Atlatl Association pages at http://www.worldatlatl.org/ If I know about it, I will sometimes indicate such an electronic source as well as the original citation. The articles use a variety of measurements. Some useful conversions: 1”=2.54 -
North American Deserts Chihuahuan - Great Basin Desert - Sonoran – Mojave
North American Deserts Chihuahuan - Great Basin Desert - Sonoran – Mojave http://www.desertusa.com/desert.html In most modern classifications, the deserts of the United States and northern Mexico are grouped into four distinct categories. These distinctions are made on the basis of floristic composition and distribution -- the species of plants growing in a particular desert region. Plant communities, in turn, are determined by the geologic history of a region, the soil and mineral conditions, the elevation and the patterns of precipitation. Three of these deserts -- the Chihuahuan, the Sonoran and the Mojave -- are called "hot deserts," because of their high temperatures during the long summer and because the evolutionary affinities of their plant life are largely with the subtropical plant communities to the south. The Great Basin Desert is called a "cold desert" because it is generally cooler and its dominant plant life is not subtropical in origin. Chihuahuan Desert: A small area of southeastern New Mexico and extreme western Texas, extending south into a vast area of Mexico. Great Basin Desert: The northern three-quarters of Nevada, western and southern Utah, to the southern third of Idaho and the southeastern corner of Oregon. According to some, it also includes small portions of western Colorado and southwestern Wyoming. Bordered on the south by the Mojave and Sonoran Deserts. Mojave Desert: A portion of southern Nevada, extreme southwestern Utah and of eastern California, north of the Sonoran Desert. Sonoran Desert: A relatively small region of extreme south-central California and most of the southern half of Arizona, east to almost the New Mexico line. -
Quicksilver Deposits of Steens Mountain and Pueblo Mountains Southeast Oregon
Quicksilver Deposits of Steens Mountain and Pueblo Mountains Southeast Oregon GEOLOGICAL SURVEY BULLETIN 995-B A CONTRIBUTION TO ECONOMIC GEOLOGY QUICKSILVER DEPOSITS OF STEENS MOUNTAIN AND PUEBLO MOUNTAINS, SOUTHEAST OREGON By HOWEL WILLIAMS and ROBERT R. The object of this survey was to examine the quicksilver deposits with the hope of locating large tonnages of low-grade ore. The deposits occur in the south-central part of Harney County and are more than 100 miles from either Burns, Oreg., or Winuemucca, Nev., the nearest towns. The region is sparsely settled by stockmen; Fields, Denio, and Andrews are the only settlements. The range consisting of Steens Mountain and Pueblo Mountains is a dissected fault block, 90 miles long in a north-south direction and as much as 25 miles wide, tilted gently to the west. Pre-Tertiary rnetarnorphic and plutonic rocks occur at the southern end, but most of the block consists of Pliocene volcanic rocks. The major boundary faults on the east side of the range are concealed by alluvium. Minor northwestward-trending faults branch from them, their throws diminish ing toward the crest of the range; other minor fractures occur near, and parallel to, the mountain front. The quicksilver lodes were formed in and along these subsidiary fractures. The lodes occur in a more or less continuous belt just west of the eastern front of the range. They are steeply dipping and arranged in subparallel clusters, commonly standing out as resistant siliceous ribs against the softer kaolinized rocks that flank them. The lodes were formed in two hydrothermal stages, the first producing the reeflike masses of chalcedony and quartz with their halos of limonitic and calcitic clays and the second introducing silica and barite along with sulfides of iron, copper, and mercury.