Fresh Water on Fort Yuma Desert
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California Vegetation Map in Support of the DRECP
CALIFORNIA VEGETATION MAP IN SUPPORT OF THE DESERT RENEWABLE ENERGY CONSERVATION PLAN (2014-2016 ADDITIONS) John Menke, Edward Reyes, Anne Hepburn, Deborah Johnson, and Janet Reyes Aerial Information Systems, Inc. Prepared for the California Department of Fish and Wildlife Renewable Energy Program and the California Energy Commission Final Report May 2016 Prepared by: Primary Authors John Menke Edward Reyes Anne Hepburn Deborah Johnson Janet Reyes Report Graphics Ben Johnson Cover Page Photo Credits: Joshua Tree: John Fulton Blue Palo Verde: Ed Reyes Mojave Yucca: John Fulton Kingston Range, Pinyon: Arin Glass Aerial Information Systems, Inc. 112 First Street Redlands, CA 92373 (909) 793-9493 [email protected] in collaboration with California Department of Fish and Wildlife Vegetation Classification and Mapping Program 1807 13th Street, Suite 202 Sacramento, CA 95811 and California Native Plant Society 2707 K Street, Suite 1 Sacramento, CA 95816 i ACKNOWLEDGEMENTS Funding for this project was provided by: California Energy Commission US Bureau of Land Management California Wildlife Conservation Board California Department of Fish and Wildlife Personnel involved in developing the methodology and implementing this project included: Aerial Information Systems: Lisa Cotterman, Mark Fox, John Fulton, Arin Glass, Anne Hepburn, Ben Johnson, Debbie Johnson, John Menke, Lisa Morse, Mike Nelson, Ed Reyes, Janet Reyes, Patrick Yiu California Department of Fish and Wildlife: Diana Hickson, Todd Keeler‐Wolf, Anne Klein, Aicha Ougzin, Rosalie Yacoub California -
Winter Observations on the Colorado Desert
MAR., 1902. ( THE CONDOR 37 In some respects the Oregon song sparrow is a remarkable form. It is darker than the races north and south of its range, and duplicates in coloring the sooty song sparrow of the Sitkan District. The races along the coast seem thus to alternate light and dark. But whilephea is nearly identical with ru@a in color, it is conspicuously smaller, and the ranges of the two are separated by several hundred miles. The present form occupies a strip along the coast from the northern limit of the redwoods (?) or at least from Rogue River north to Yaquina. The specimens from Crescent City are probably migrants as the breeding birds seem nearer deonensis (tho not precisely typical). The area ofi intergradation between cdeonen- sis and phcza is probably small, extending perhaps from Crescent City to Chetco R. (northern limit of Sequoia sempervivens). Lack of specimens prevents the exact determination of the limits of$hcPa at the north. I am indebted to Mr. Robert Ridgway and to Dr. C. Hart Merriam forthe use of specimens and types in the collection of the National Museum and in that of the Biological Survey. Winter Observations on the Colorado Desert. IT. S. DAGGETT, PASADENA, CAL. ROM Oct. 27 to Nov. 16, 1901, I dead birds floating on its surface, was spent at the American Girl Gold the cyanide tanks, two in number, con- F Mining Co.s‘ camp, located in the taining a strong solution of cyanide of Cargo Murchacho Mts on the Colorado potassium. Birds that essayed to Desert, five and one-half miles north- quench their thirst at this fount top- east of Ogilby, Cal., and some sixteen pled over dead in an instant. -
Birds of the California Desert
BIRDS OF THE CALIFORNIA DESERT A. Sidney England and William F. Laudenslayer, Jr. i INTRODUCTION i \ 1 The term, "California desert", as used herein, refers to a politically defined region, most of i which is included in the California Desert Conservation Area (CDCA) designated by the Federal Land ; and Management Act of 1976 (FLPMA). Of the 25 million acres in the CDCA, about one-half are i public lands, most of which are managed by the Bureau of Land Management (BLM) according to the "980 P California Desert Conservation Area Plan mandated by FLPMA. The California desert encompasses those portions of the Great Basin Desert (east of the White and lnyo Mountains and A south of the California-Nevada border), the Mojave Desert, and the Colorado Desert which occur " within California; it does not include areas of riparian, aquatic, urban, and agricultural habitats . adjacent to the Colorado River. (Also see chapters on Geology by Norris and Bioclimatology by E3irdsI4 are the most conspicuous vertebrates found in the California deserts. Records exist for at least 425 species (Garrett and Dunn 1981) from 18 orders and 55 families. These counts far exceed those for mammals, reptiles, amphibians and fish, and they are similar to totals for the entire state -- 542 species from 20 orders and 65 families (Laudenslayer and Grenfell 1983). These figures may seem surprisingly similar considering the harsh, arid climates often believed characteristic of I desert environments. However, habiiats found in the California desert range from open water and h marshes at the Salton Sea to pinyon-juniper woodland and limber pinelbristlecone pine forests on a few mountain ranges. -
Usibwc Selects 12 Citizens Forum Board Members to Serve 2-Year Term; Public Meeting Set for July 25 in Yuma
International Boundary and Water Commission United States Section For immediate release July 11, 2018 USIBWC SELECTS 12 CITIZENS FORUM BOARD MEMBERS TO SERVE 2-YEAR TERM; PUBLIC MEETING SET FOR JULY 25 IN YUMA The United States Section of the International Boundary and Water Commission (USIBWC) has appointed 12 board members to serve on the Colorado River Citizens Forum (CRCF) Board. The first public meeting with the new board will take place Wednesday, July 25, 4:00 p.m. – 6:00 p.m. at the Yuma County Development Services, 2351 West 26th Street, Yuma, Arizona. The Colorado River Citizens Forum was established to facilitate the exchange of information between the USIBWC and the community about Commission projects and related activities in Yuma County, Arizona and Imperial County, California. The new board members are: Jim Buster: Southwest Resource Strategies Tom Davis: Yuma County Water Users Assoc. Matt Dessert: Imperial County Air Pollution Control District Bruce Kuhn: Imperial Irrigation District P. Brian McNeece: Imperial County Historical Society Juan Leal Rubio: Yuma County Phil Rosentrater: Salton Sea Authority Frank Ruiz: Audubon Society Meghan Scott: Yuma County Agriculture Water Coalition Jay Simonton: City of Yuma, Director of Utilities Roberta (Bobbi) Stevenson-McDermott: Yuma Natural Resource Conservation District Mark William White (Willie White): Fort Yuma Quechan Indian Tribe The board will also include Anna Morales, Area Operations Manager for the USIBWC’s Yuma Field Office. Board members will serve as volunteers for a two-year term. USIBWC Public Affairs Officer Lori Kuczmanski will provide an overview of the history of the International Boundary and Water Commission, from its early days surveying and marking the U.S.- Mexico border, to its growing role in water management, based on the Convention of 1906 and the 1944 Water Treaty. -
The Southern Emigrant Trail
THE SOUTHERN EMIGRANT TRAIL BY PHIL BRIGANDI Southernthe Emigrant Trail FALL 2010 1 PHIL BRIGANDI he Southern Emigrant Trail has a long and interesting history. In its heyday, it was the major overland route in and out of Southern T California, and it played a part in every era of California history for more than a century. Its most famous era was the Next came the squeeze through Box Canyon, and the period from the start of the Mexican War, through easy pull across Blair Valley—now a popular camping the California Gold Rush, and on to the days of the spot in the Anza-Borrego Desert State Park. Butterfield stage. But unlike many other early over- The long grade up the San Felipe Valley to War- land trails, the Southern Emigrant Trail survived ners Pass (today’s Teofulio Summit) finally brought the coming of the railroad, and was still being used travelers out of the desert. At Warners Ranch, the to cross the California desert well into the twentieth main trail divided, with one branch heading off to century. San Diego, and the other continuing on through The trail has been known by a variety of differ- Temecula and Isaac Williams’ Rancho del Chino on ent names over the years. In Mexican times it was its way to Los Angeles. the Sonora Road. Later it was the Gila Trail, the First to follow the trail were the Indians, who Fort Yuma Road, or simply the Southern Route. It probably followed animal trails to find the water- first came to be known as the Emigrant Road, or ing places along the way. -
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. -
Sonny Bono Salton Sea National Wildlife Refuge Complex
Appendix J Cultural Setting - Sonny Bono Salton Sea National Wildlife Refuge Complex Appendix J: Cultural Setting - Sonny Bono Salton Sea National Wildlife Refuge Complex The following sections describe the cultural setting in and around the two refuges that constitute the Sonny Bono Salton Sea National Wildlife Refuge Complex (NWRC) - Sonny Bono Salton Sea NWR and Coachella Valley NWR. The cultural resources associated with these Refuges may include archaeological and historic sites, buildings, structures, and/or objects. Both the Imperial Valley and the Coachella Valley contain rich archaeological records. Some portions of the Sonny Bono Salton Sea NWRC have previously been inventoried for cultural resources, while substantial additional areas have not yet been examined. Seventy-seven prehistoric and historic sites, features, or isolated finds have been documented on or within a 0.5- mile buffer of the Sonny Bono Salton Sea NWR and Coachella Valley NWR. Cultural History The outline of Colorado Desert culture history largely follows a summary by Jerry Schaefer (2006). It is founded on the pioneering work of Malcolm J. Rogers in many parts of the Colorado and Sonoran deserts (Rogers 1939, Rogers 1945, Rogers 1966). Since then, several overviews and syntheses have been prepared, with each succeeding effort drawing on the previous studies and adding new data and interpretations (Crabtree 1981, Schaefer 1994a, Schaefer and Laylander 2007, Wallace 1962, Warren 1984, Wilke 1976). The information presented here was compiled by ASM Affiliates in 2009 for the Service as part of Cultural Resources Review for the Sonny Bono Salton Sea NWRC. Four successive periods, each with distinctive cultural patterns, may be defined for the prehistoric Colorado Desert, extending back in time over a period of at least 12,000 years. -
June Temperature Trends in the Southwest Deserts of the USA (1950–2018) and Implications for Our Urban Areas
atmosphere Article June Temperature Trends in the Southwest Deserts of the USA (1950–2018) and Implications for Our Urban Areas Anthony Brazel School of Geographical Sciences & Urban Planning, Arizona State University, Tempe, AZ 85287-5302, USA; [email protected] Received: 7 November 2019; Accepted: 9 December 2019; Published: 11 December 2019 Abstract: Within the United States, the Southwest USA deserts show the largest temperature changes (1901–2010) besides Alaska, according to the most recent USA National Climate Assessment report. The report does not discuss urban effects vs. regional effects that might be evident in trends. Twenty-five temperature stations with ca. 68-year records (1950 to 2018) have been accessed from US Global Historical Climate Network archives. Land cover data are accessed from a National Land Cover Database. June results considering both urban and rural sites show an astounding rate per year change among sites ranging from 0.01 to 0.05 C for maximum temperatures and 0.01 to 0.11 C − ◦ ◦ for minimum temperatures ( 0.8 to 3.2 C, and 0.8 to 8.0 C for the entire period). For maximum − ◦ ◦ temperatures, almost half of the sites showed no significant trends at a stringent 0.01 level of statistical significance, but 20 of 25 were significant at the 0.05 level. For minimum temperatures, over 75% of sites were significant at the 0.01 level (92% at 0.05 level of significance). The urban-dominated stations in Las Vegas, Phoenix, Tucson, and Yuma show large minimum temperature trends, indicating emerging heat island effects. Rural sites, by comparison, show much smaller trends. -
Smithsonian Miscellaneous Collections
-&? SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 82. NUMBER 6 THE PAST CLIMATE OF THE NORTH POLAR REGION BY EDWARD W. BERRY The Johns Hopkins University (Publication 3061) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION APRIL 9, 1930 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 82, NUMBER 6 THE PAST CLIMATE OF THE NORTH POLAR REGION BY EDWARD W. BERRY The Johns Hopkins University Publication 306i i CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION APRIL 9, 1930 ZU £or& (gafttmore (prees BALTIMORE, MD., U. S. A. THE PAST CLIMATE OF THE NORTH POLAR REGION 1 By EDWARD W. BERRY THE JOHNS HOPKINS UNIVERSITY The plants, coal beds, hairy mammoth and woolly rhinoceros ; the corals, ammonites and the host of other marine organisms, chiefly invertebrate but including ichthyosaurs and other saurians, that have been discovered beneath the snow and ice of boreal lands have always made a most powerful appeal to the imagination of explorers and geologists. We forget entirely the modern whales, reindeer, musk ox, polar bear, and abundant Arctic marine life, and remember only the seemingly great contrast between the present and this subjective past. Nowhere on the earth is there such an apparent contrast between the present and geologic climates as in the polar regions and the mental pictures which have been aroused and the theories by means of which it has been sought to explain the fancied conditions of the past are all, at least in large part, highly imaginary. Occasionally a student like Nathorst (1911) has refused to be carried away by his imagination and has called to mind the mar- velously rich life of the present day Arctic seas, but for the most part those who have speculated on former climates have entirely ignored the results of Arctic oceanography. -
A Field Guide to Biological Soil Crusts of Western U.S. Drylands Common Lichens and Bryophytes
A Field Guide to Biological Soil Crusts of Western U.S. Drylands Common Lichens and Bryophytes Roger Rosentreter Matthew Bowker Jayne Belnap Photographs by Stephen Sharnoff Roger Rosentreter, Ph.D. Bureau of Land Management Idaho State Office 1387 S. Vinnell Way Boise, ID 83709 Matthew Bowker, Ph.D. Center for Environmental Science and Education Northern Arizona University Box 5694 Flagstaff, AZ 86011 Jayne Belnap, Ph.D. U.S. Geological Survey Southwest Biological Science Center Canyonlands Research Station 2290 S. West Resource Blvd. Moab, UT 84532 Design and layout by Tina M. Kister, U.S. Geological Survey, Canyonlands Research Station, 2290 S. West Resource Blvd., Moab, UT 84532 All photos, unless otherwise indicated, copyright © 2007 Stephen Sharnoff, Ste- phen Sharnoff Photography, 2709 10th St., Unit E, Berkeley, CA 94710-2608, www.sharnoffphotos.com/. Rosentreter, R., M. Bowker, and J. Belnap. 2007. A Field Guide to Biological Soil Crusts of Western U.S. Drylands. U.S. Government Printing Office, Denver, Colorado. Cover photos: Biological soil crust in Canyonlands National Park, Utah, cour- tesy of the U.S. Geological Survey. 2 Table of Contents Acknowledgements ....................................................................................... 4 How to use this guide .................................................................................... 4 Introduction ................................................................................................... 4 Crust composition .................................................................................. -
A HISTORY of YUMA, ARIZONA , 1540-1920 by Frank D
A history of Yuma, Arizona, 1540-1920 Item Type text; Thesis-Reproduction (electronic) Authors Robertson, Frank Delbert, 1900- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 07/10/2021 03:02:13 Link to Item http://hdl.handle.net/10150/551109 A HISTORY OF YUMA, ARIZONA , 1540-1920 by Frank D. Robertson A Thesis submitted to the faculty of the Department of History in partial fulfillment of the requirements for the degree of Master of Arts in the Graduate College University of Arizona 1 9 4 2 4 ^ 2/ 3 / TABLE OF CONTENTS Chapter Page INTRODUCTION........................... i I. THE COMING OF THE WHITE MAN AND THE YUMA INDIANS........................ 1 Early Explorers and Missionaries-- Alarcon-- Di'az— Onate— Kino— G-arces- -Missions Established— The Yuma Massacre— Missions Destroyed--The Yuma Indian Tribes--Cocopas— Yumas— Mohaves— Indian Legends— Social and Economic Conditions— Tribal War II. TRAPPERS AND FORTY-NINERS.............. 26 Fur Trappers--Pattie and Son— Saint Vrain— Pauline Weaver— Trails to the Southwest--The Old Yuma Trail— First Colorado River Ferry— Glanton Murder — California Militia at the Junction — Fort Yuma— The Oatman Massacre-- Return of Olive Oatman III. YUMA IN THE FORMATIVE PERIOD 1854-1875.• 48 The Poston Survey— Description in 1859— Three Settlements at the Junction--Yuma Town Site Registered in San Diego County Records— California Officials Collect Taxes in Yuma— Cattle Drives through Yuma — Stage and Mail through Yuma— Lynching in Arizona City— Flood of 1862— Coming of Contreras Family— Several Business Houses Established — A Catholic Church Built— Freighting Out of Yuma— Elementary School— Miss Post— First Legal Execution--The Territorial Penitentiary— The Settled Community 14 < 4 u u Chapter Page IV. -
Colorado River Citizens Forum Yuma County Development Services, Aldrich Hall Yuma, AZ 85364 January 22, 2020 *Tentative Meeting Notes
Colorado River Citizens Forum Yuma County Development Services, Aldrich Hall Yuma, AZ 85364 January 22, 2020 *Tentative Meeting Notes Board Members in attendance: Meghan Scott, Yuma County Agriculture Water Coalition Matt Dessert, Imperial County Air Pollution Control District Tom Davis, Yuma County Water Users Association Jim Buster, Southwest Resource Strategies Phil Rosentrater, Salton Sea Authority Brian McNeece, retired Professor Frank Ruiz, Audubon Society Mark William White, Fort Yuma Quechan Indian Tribe Roberta (Bobbi) Stevenson-McDermott, Yuma Natural Resource Conservation District Member, Arizona Association of Conservation Districts Board Member USIBWC Staff in attendance: Anna Morales, Area Operations Manager, USIBWC, Yuma, Arizona 28 Members of the public in attendance Welcoming and Introduction Remarks: At 4:00 p.m. Citizens Forum Co-Chair Anna Morales convened the meeting by welcoming the group and provided a brief description of the meeting agenda items. Board members and audience briefly introduced themselves. Presentation One: The Colorado River Basin Salinity Control Program-Reducing Downstream Damages by Millions of Dollars; Don A. Barnett, Executive Director, Colorado River Basin Salinity Control Program Mr. Barnett provided an overview of the Colorado river Basin Salinity Control Program. The Colorado River is more than 1,450 miles long (2330 km), drains 246,000 square-miles (1/12 of the continental US), has an annual flow of about 16 M acre-feet, had an annual salt load of 9-10 million tons. The Colorado River supplies water to 40 million people in the United States and 1.5 million acre-feet is delivered to Mexico annually. Nearly 5.5 million acres in the U.S.