Eninsula Ovis Cana 5-Yea Ummary
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Section 3.3 Geology Jan 09 02 ER Rev4
3.3 Geology and Soils 3.3.1 Introduction and Summary Table 3.3-1 summarizes the geology and soils impacts for the Proposed Project and alternatives. TABLE 3.3-1 Summary of Geology and Soils Impacts1 Alternative 2: 130 KAFY Proposed Project: On-farm Irrigation Alternative 3: 300 KAFY System 230 KAFY Alternative 4: All Conservation Alternative 1: Improvements All Conservation 300 KAFY Measures No Project Only Measures Fallowing Only LOWER COLORADO RIVER No impacts. Continuation of No impacts. No impacts. No impacts. existing conditions. IID WATER SERVICE AREA AND AAC GS-1: Soil erosion Continuation of A2-GS-1: Soil A3-GS-1: Soil A4-GS-1: Soil from construction existing conditions. erosion from erosion from erosion from of conservation construction of construction of fallowing: Less measures: Less conservation conservation than significant than significant measures: Less measures: Less impact with impact. than significant than significant mitigation. impact. impact. GS-2: Soil erosion Continuation of No impact. A3-GS-2: Soil No impact. from operation of existing conditions. erosion from conservation operation of measures: Less conservation than significant measures: Less impact. than significant impact. GS-3: Reduction Continuation of A2-GS-2: A3-GS-3: No impact. of soil erosion existing conditions. Reduction of soil Reduction of soil from reduction in erosion from erosion from irrigation: reduction in reduction in Beneficial impact. irrigation: irrigation: Beneficial impact. Beneficial impact. GS-4: Ground Continuation of A2-GS-3: Ground A3-GS-4: Ground No impact. acceleration and existing conditions. acceleration and acceleration and shaking: Less than shaking: Less than shaking: Less than significant impact. -
BIGHORN SHEEP Ovis Canadensis Original1 Prepared by R.A
BIGHORN SHEEP Ovis canadensis Original1 prepared by R.A. Demarchi Species Information Distribution Global Taxonomy The genus Ovis is present in west-central Asia, Until recently, three species of Bighorn Sheep were Siberia, and North America (and widely introduced recognized in North America: California Bighorn in Europe). Approximately 38 000 Rocky Mountain Sheep (Ovis canadensis californiana), Rocky Bighorn Sheep (Wishart 1999) are distributed in Mountain Bighorn Sheep (O. canadensis canadensis), scattered patches along the Rocky Mountains of and Desert Bighorn Sheep (O. canadensis nelsoni). As North America from west of Grand Cache, Alberta, a result of morphometric measurements, and to northern New Mexico. They are more abundant protein and mtDNA analysis, Ramey (1995, 1999) and continuously distributed in the rainshadow of recommended that only Desert Bighorn Sheep and the eastern slopes of the Continental Divide the Sierra Nevada population of California Bighorn throughout their range. Sheep be recognized as separate subspecies. California Bighorn Sheep were extirpated from most Currently, California and Rocky Mountain Bighorn of the United States by epizootic disease contracted sheep are managed as separate ecotypes in British from domestic sheep in the 1800s with a small Columbia. number living in California until 1954 (Buechner Description 1960). Since 1954, Bighorn Sheep have been reintroduced from British Columbia to California, California Bighorn Sheep are slightly smaller than Idaho, Nevada, North Dakota, Oregon, Utah, and mature Rocky Mountain Bighorn Sheep Washington, resulting in their re-establishment in (McTaggart-Cowan and Guiguet 1965). Like their much of their historic range. By 1998, California Rocky Mountain counterpart, California Bighorn Bighorn Sheep were estimated to number 10 000 Sheep have a dark to medium rich brown head, neck, (Toweill 1999). -
Queen Victoria to Belong to Posterity
AREA POPULATION 3500 Guatay ................, ............. 200 Jamul ................................ 952 Pine Valley ...................... 956 Campo .............................. 1256 Descan, o ... .. .. .... .. ...... ....... 776 Jacumba ............................ 852 Harbison Canyon ............ 1208 ALPINE ECHO Total .............................. 9273 Serving a Growing Area of Homes and Ranches VOL. 5-NO. 34 ----~- 36 ALPINE, CALIFORNIA, THURSDAY, AUGUST 30, 1962 PRICE TEN CENTS QUEEN VICTORIA TO BELONG TO POSTERITY Local Historical Society Works To Preserve Landmark A good crowd of members and guests assembled Sun day, August 26, when the Alpine Historical Society met in the Alpine Woman's Club at 2 p .m. As its first definite project in t he program of locating and preserving authentic historical data of local signifi- cance, the society has started to work on the acquisition of the fa Local Schools Lose mous ·old rock, called Queen Vic- toria which stands in the 2700 10 TeaC hterS block on Victoria Hill. Ten cE>rtificated employees have j After a brief discussion, Presi' left the Alpine Schools this sprina dent Ralph Walker appointed Or·· for greener pastures in other dis~ ville Palmer, president of the Vic tricts with mQ.re attractive sched- toria Hiil Civic Association, as ules. chairman in charge of the rock project. He will work with His Frank J<,seph has accepted a full torical Research committee chair· time administrative position in the man, Philip Hall. Mr. Palmer has Lawndale School, Los Angeles contacted owner of the rock and County. Mr. Joseph will have site, Edward Roper of San Diego, charge o:f a school with an enroH who has expressed willingness to ment of 830 pupils and 23 teach deed it to the society for preserva ers. -
Mule Deer and Antelope Staff Specialist Peregrine Wolff, Wildlife Health Specialist
STATE OF NEVADA Steve Sisolak, Governor DEPARTMENT OF WILDLIFE Tony Wasley, Director GAME DIVISION Brian F. Wakeling, Chief Mike Cox, Bighorn Sheep and Mountain Goat Staff Specialist Pat Jackson, Predator Management Staff Specialist Cody McKee, Elk Staff Biologist Cody Schroeder, Mule Deer and Antelope Staff Specialist Peregrine Wolff, Wildlife Health Specialist Western Region Southern Region Eastern Region Regional Supervisors Mike Scott Steve Kimble Tom Donham Big Game Biologists Chris Hampson Joe Bennett Travis Allen Carl Lackey Pat Cummings Clint Garrett Kyle Neill Cooper Munson Sarah Hale Ed Partee Kari Huebner Jason Salisbury Matt Jeffress Kody Menghini Tyler Nall Scott Roberts This publication will be made available in an alternative format upon request. Nevada Department of Wildlife receives funding through the Federal Aid in Wildlife Restoration. Federal Laws prohibit discrimination on the basis of race, color, national origin, age, sex, or disability. If you believe you’ve been discriminated against in any NDOW program, activity, or facility, please write to the following: Diversity Program Manager or Director U.S. Fish and Wildlife Service Nevada Department of Wildlife 4401 North Fairfax Drive, Mailstop: 7072-43 6980 Sierra Center Parkway, Suite 120 Arlington, VA 22203 Reno, Nevada 8911-2237 Individuals with hearing impairments may contact the Department via telecommunications device at our Headquarters at 775-688-1500 via a text telephone (TTY) telecommunications device by first calling the State of Nevada Relay Operator at 1-800-326-6868. NEVADA DEPARTMENT OF WILDLIFE 2018-2019 BIG GAME STATUS This program is supported by Federal financial assistance titled “Statewide Game Management” submitted to the U.S. -
Geology of Hawk Canyon, Anza-Borrego Desert State Park, California
GEOLOGY OF HAWK CANYON, ANZA-BORREGO DESERT STATE PARK, CALIFORNIA By Jeffrey D. Pepin Geological Sciences Department California State Polytechnic University Pomona, California 2011 Senior Thesis Submitted in partial fulfillment of the requirements for the Bachelor of Science Geology Degree Table of Contents Abstract ...............................................................................................................................1 Introduction ........................................................................................................................2 Purpose and Objectives ....................................................................................................2 Regional Geology .............................................................................................................4 Field Site Description .......................................................................................................9 Discussion of Previous Work Done in Hawk Canyon ...................................................11 Observational Data ..........................................................................................................12 Field Techniques ............................................................................................................12 Global Positioning System (GPS) Data and Notes ........................................................14 Orientation Data by Structure ........................................................................................20 Lithology ........................................................................................................................21 -
Right-Sljp Offset of the Eocene Ballena River Valley Across the Elsinore Fault Zone, Southern California
http://dx.doi.org/10.7773/cm.v9i1.412 RIGHT-SLJP OFFSET OF THE EOCENE BALLENA RIVER VALLEY ACROSS THE ELSINORE FAULT ZONE, SOUTHERN CALIFORNIA Patrick L. Abbott Ronald P. Kies Dermis R. Kerr Department of GeologicaI Sciences San Diego State University San Diego, California 92182 U. S. A. ABSTRACT TWO small paleovalleys carved into granitic rocks of the Peninsular Ranges contain conglomerates similar to the Eocene Ballena Gravels farther west in San Diego County. These conglomerates are dominated by the distinctive, temporally restricted, Poway rhyolite clasts. The newly discovered fluvial conglomerates lie in the Vallecito Mountains east of the Elsinore fault zone. Extrapolation of the offset fluvial valley trends to the Elsinore fault suggests 37 kilometers (23 miles) of right slip. RESUMEN Dos valles pequeños paleolíticos, grabados en cuerpos graníticos de la Cor- dillera Peninsular, contienen conglomerados semejantes a las gravas de la Forma- ción Ballena del Eoceno, localizada al peste, en el Condado de San Diego. Este conglomerado es dominado por clastos riolíticos de la Formación Poway, los cuales son característicos y están temporalmente restringidos. Los conglomerados fluviales recientemente descubiertos, se encuentran en las Montanas del Vallecito, al este de la zona de la falla de Elsinore. Proyectando los rumbos de los conglome- rados fluviales y de las gravas a través de la falla de Elsinore, se observa un despla- zamiento de 37 km. (23 millas) en un sentido lateral-derecho. INTRODUCTION The Ballena Gravels (actually conglomerate ) were named by Fairbanks (1893) for a prominent, southwest-trending line of outcrops on the western flank of the batholithic Peninsular Ranges in San Diego County (figure 1). -
Ceramic Production and Circulation in the Greater Southwest
MONOGRAPH 44 Ceramic Production and Circulation in the Greater Southwest Source Determination by INAA and Complementary Mineralogical Investigations Edited by Donna M. Glowacki and Hector Neff The Cotsen Institute ofArchaeology University of California, Los Angeles 2002 IO Patayan Ceramic Variability Using Trace Elements and Petrographic Analysis to Study Brown and BuffWares in Southern California john A. Hildebrand, G. Timothy Cross,jerry Schaefer, and Hector Neff N THE LOWER COLORADO RivER and adjacent desert tain a large fraction of granitic inclusions, and when present and upland regions of southern California and in prehistoric pottery, me inclusions may not represent added 0 western Arizona, the late prehistoric Patayan temper but me remnants of incompletely weamered parent produced predominantly undecorated ceramics using a pad rock (Shepard 1964). In the lower Colorado River and Salton dle and anvil technique (Colton 1945; Rogers 1945a; Waters Trough regions, alluvial clays are available with a low iron 1982). Patayan ceramic vessels were important to both mixed content, hence their buff color, and which contain little or horticultural economies along the Colorado and adjacent no intrinsic inclusions. In this case, tempering materials may river systems, and to largely hunting and gathering econo be purposefully added to the alluvial clays. For the historic mies in the adjacent uplands. Patayan ceramic production Kumeyaay/ Kamia, a Yuman-speaking group known to have began at about AD 700 (Schroeder 1961), and continued into occupied both mountain and desert regions west of the low recent times among the Yuman speakers of this region, de er Colorado River (Hicks 1963), the same potters may have scendants of the Patayan (Rogers 1936). -
Science Newsletter
Mojave National Preserve National Park Service U.S. Department of the Interior Sweeney Granite Mountains Desert Research Center Science Newsletter Updates on respiratory disease affecting desert bighorn sheep in and near Mojave National Preserve 1 1 Clinton W. Epps , Daniella Dekelaita , and Brian Dugovich2 Desert bighorn sheep (Ovis canadensis nelsoni) are an iconic mammal of the desert southwest and are found in small mountain ranges scattered across Mojave National Preserve (Preserve) and nearby desert habitats in southeastern California. In many areas, they are the only large native herbivore that can persist, inhabiting places that are too hot, dry, and sparsely vegetated for deer. California is thought to be home to ~3000-5000 desert bighorn in total (1); desert bighorn sheep are uniquely adapted for the harsh environment of the southwest deserts and populations appear to be resilient in spite of threats from poaching, climate change, drought, and habitat fragmentation (2, 3). In the Mojave Desert, bighorn sheep populations are strongly fragmented by expanses of flat desert between Figure 1. Map of Mojave National Preserve and nearby areas in southeastern California, mountain ranges, and in some cases, by showing mountain ranges (white polygons) where respiratory disease of bighorn sheep is being studied using GPS collars, remote cameras, disease screening of captured animals, behavioral and physical barriers such as fecal DNA, immunological and genetic measures, and other methods. The respiratory interstate highways (4). Yet, southeastern pathogen Mycoplasma ovipneumoniae was first reported at Old Dad Peak in spring of 2013 (large red star); current infection or past exposure has been confirmed at other red-starred California, including the Preserve, represents the ranges. -
Antelope, Deer, Bighorn Sheep and Mountain Goats: a Guide to the Carpals
J. Ethnobiol. 10(2):169-181 Winter 1990 ANTELOPE, DEER, BIGHORN SHEEP AND MOUNTAIN GOATS: A GUIDE TO THE CARPALS PAMELA J. FORD Mount San Antonio College 1100 North Grand Avenue Walnut, CA 91739 ABSTRACT.-Remains of antelope, deer, mountain goat, and bighorn sheep appear in archaeological sites in the North American west. Carpal bones of these animals are generally recovered in excellent condition but are rarely identified beyond the classification 1/small-sized artiodactyl." This guide, based on the analysis of over thirty modem specimens, is intended as an aid in the identifi cation of these remains for archaeological and biogeographical studies. RESUMEN.-Se han encontrado restos de antilopes, ciervos, cabras de las montanas rocosas, y de carneros cimarrones en sitios arqueol6gicos del oeste de Norte America. Huesos carpianos de estos animales se recuperan, por 10 general, en excelentes condiciones pero raramente son identificados mas alIa de la clasifi cacion "artiodactilos pequeno." Esta glia, basada en un anaIisis de mas de treinta especlmenes modemos, tiene el proposito de servir como ayuda en la identifica cion de estos restos para estudios arqueologicos y biogeogrMicos. RESUME.-On peut trouver des ossements d'antilopes, de cerfs, de chevres de montagne et de mouflons des Rocheuses, dans des sites archeologiques de la . region ouest de I'Amerique du Nord. Les os carpeins de ces animaux, generale ment en excellente condition, sont rarement identifies au dela du classement d' ,I artiodactyles de petite taille." Le but de ce guide base sur 30 specimens recents est d'aider aidentifier ces ossements pour des etudes archeologiques et biogeo graphiques. -
Genital Brucella Suis Biovar 2 Infection of Wild Boar (Sus Scrofa) Hunted in Tuscany (Italy)
microorganisms Article Genital Brucella suis Biovar 2 Infection of Wild Boar (Sus scrofa) Hunted in Tuscany (Italy) Giovanni Cilia * , Filippo Fratini , Barbara Turchi, Marta Angelini, Domenico Cerri and Fabrizio Bertelloni Department of Veterinary Science, University of Pisa, Viale delle Piagge 2, 56124 Pisa, Italy; fi[email protected] (F.F.); [email protected] (B.T.); [email protected] (M.A.); [email protected] (D.C.); [email protected] (F.B.) * Correspondence: [email protected] Abstract: Brucellosis is a zoonosis caused by different Brucella species. Wild boar (Sus scrofa) could be infected by some species and represents an important reservoir, especially for B. suis biovar 2. This study aimed to investigate the prevalence of Brucella spp. by serological and molecular assays in wild boar hunted in Tuscany (Italy) during two hunting seasons. From 287 animals, sera, lymph nodes, livers, spleens, and reproductive system organs were collected. Within sera, 16 (5.74%) were positive to both rose bengal test (RBT) and complement fixation test (CFT), with titres ranging from 1:4 to 1:16 (corresponding to 20 and 80 ICFTU/mL, respectively). Brucella spp. DNA was detected in four lymph nodes (1.40%), five epididymides (1.74%), and one fetus pool (2.22%). All positive PCR samples belonged to Brucella suis biovar 2. The results of this investigation confirmed that wild boar represents a host for B. suis biovar. 2 and plays an important role in the epidemiology of brucellosis in central Italy. Additionally, epididymis localization confirms the possible venereal transmission. Citation: Cilia, G.; Fratini, F.; Turchi, B.; Angelini, M.; Cerri, D.; Bertelloni, Keywords: Brucella suis biovar 2; wild boar; surveillance; epidemiology; reproductive system F. -
Anza-Borrego Desert State Park Bibliography Compiled and Edited by Jim Dice
Steele/Burnand Anza-Borrego Desert Research Center University of California, Irvine UCI – NATURE and UC Natural Reserve System California State Parks – Colorado Desert District Anza-Borrego Desert State Park & Anza-Borrego Foundation Anza-Borrego Desert State Park Bibliography Compiled and Edited by Jim Dice (revised 1/31/2019) A gaggle of geneticists in Borrego Palm Canyon – 1975. (L-R, Dr. Theodosius Dobzhansky, Dr. Steve Bryant, Dr. Richard Lewontin, Dr. Steve Jones, Dr. TimEDITOR’S Prout. Photo NOTE by Dr. John Moore, courtesy of Steve Jones) Editor’s Note The publications cited in this volume specifically mention and/or discuss Anza-Borrego Desert State Park, locations and/or features known to occur within the present-day boundaries of Anza-Borrego Desert State Park, biological, geological, paleontological or anthropological specimens collected from localities within the present-day boundaries of Anza-Borrego Desert State Park, or events that have occurred within those same boundaries. This compendium is not now, nor will it ever be complete (barring, of course, the end of the Earth or the Park). Many, many people have helped to corral the references contained herein (see below). Any errors of omission and comission are the fault of the editor – who would be grateful to have such errors and omissions pointed out! [[email protected]] ACKNOWLEDGEMENTS As mentioned above, many many people have contributed to building this database of knowledge about Anza-Borrego Desert State Park. A quantum leap was taken somewhere in 2016-17 when Kevin Browne introduced me to Google Scholar – and we were off to the races. Elaine Tulving deserves a special mention for her assistance in dealing with formatting issues, keeping printers working, filing hard copies, ignoring occasional foul language – occasionally falling prey to it herself, and occasionally livening things up with an exclamation of “oh come on now, you just made that word up!” Bob Theriault assisted in many ways and now has a lifetime job, if he wants it, entering these references into Zotero. -
2009Nature Notes Vol. 9, No. 3 RH Final.Pub
Zion National Park News National Park Service U.S. Department of the Interior Nature Notes The Lush Desert High noon. A blazing sun burns rippling waves of heat across the sandy earth making the distance appear almost fluid. Tumble- weeds bounce over the land past bare bones, bleached white, crisp, and brittle in the scorching sun. Flies buzz past. A small group of turkey vultures peck at coyote carrion. A dry wind blows any sense of well-being away, and even the air smells empty. This is the desert. What Mary Austin called “a land of little rain” is an environment that often seems forbidding. We perceive these lands with words in mind such as harsh, barren, unin- viting, and scarce. Yet in the desert that is Zion National Park, people have been living for thousands of years. The plant life in Zion, at first glance, may also seem harsh and mini- The abundant medicinal and edible uses of the prickly pear cactus and datil yucca hide behind the malistic—certainly anything but lush. In dig- plants' defensive spines and sharp tips. Photo by Sally Wier ging deeper, however, we see that these plants, so symbolic of the desert, are a key encounter with a skunk. The strongly candies, and syrups. Supporting pads of the part of what has made this place a home to scented smoke not only cleansed humans of cacti, though intimidating to the touch, are humans for so long. surface odors, it had the ability to cleanse the a rich resource as well. Once rid of their soul as well.