USGS Open-File Report 2007-1227
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ADOT Herbicide Treatment Program on Bureau of Land Management Lands in Arizona
October 2015 BLM DOI-BLM-AZ-0000-2013-0001-EA ADOT Herbicide Treatment Program on Bureau of Land Management Lands in Arizona Final Environmental Assessment Bureau of Land Management Environmental Assessment and Section 4(f) Evaluation ADOT Herbicide Treatment Program on Bureau of Land Management Lands in Arizona DOI-BLM-AZ-0000-2013-0001-EA Bureau of Land Management Arizona State Office One North Central Avenue, Suite 800 Phoenix, Arizona 85004-4427 October 2015 TABLE OF CONTENTS Table of Contents ............................................................................................................................. i List of Tables ................................................................................................................................... iii List of Figures .................................................................................................................................. iii Acronym List ................................................................................................................................... iv Section 1 – Proposed Action, Purpose and Need, and Background Information ........................... 1 1.1 Introduction...................................................................................................................... 1 1.2 Proposed Action Overview ............................................................................................... 3 1.3 Purpose and Need for Action .......................................................................................... -
Josie Pearl, Prospector on Nevada's Black Rock Desert
JUNE, 1962 40c • • • • . Author's car crossing the playa of Black Rock Desert in northwestern Nevada. On Black Rock Desert Trails When Dora Tucker and Nell Murbarger first began exploring the Black Rock country in northwestern Nevada they did not realize what a high, wide and wild country it was. On the Black Rock a hundred miles doesn't mean a thing. In the 10,000 square miles of this desert wasteland there isn't a foot of pavement nor a mile of railroad— neither gasoline station nor postoffice. Antelopes out-number human beings fifty to one. There's plenty of room here for exploring. By NELL MURBARGER Photographs by the author Map by Norton Allen S AN illustration of what the want to! Ain't nothin' there!" is known as "the Black Rock country," Black Rock country affords Thanking him, we accepted his re- the desert from which it derives its in the way of variety and con- port as a favorable omen and headed name actually is a stark white alkali trast, we made a J 50-mile loop trip out into the desert. Almost invariably playa, averaging a dozen miles in out of Gerlach last June. Our previous we find our best prowling in places width and stretching for 100 miles exploring of the region had been mostly where folks have told us there "ain't from Gerlach to Kings River. Merging in the northern and eastern sections, nothin'." imperceptibly with the Black Rock on so we hadn't the slightest idea of what Rising precipitously from the dead the southwest is the section known as we might find in the southern part. -
Uranium 2001: Resources, Production and Demand
A Joint Report by the OECD Nuclear Energy Agency and the International Atomic Energy Agency Uranium 2001: Resources, Production and Demand NUCLEAR ENERGY AGENCY ORGANISATION FOR ECONOMIC CO-OPERATION AND DEVELOPMENT ORGANISATION FOR ECONOMIC CO-OPERATION AND DEVELOPMENT Pursuant to Article 1 of the Convention signed in Paris on 14th December 1960, and which came into force on 30th September 1961, the Organisation for Economic Co-operation and Development (OECD) shall promote policies designed: − to achieve the highest sustainable economic growth and employment and a rising standard of living in Member countries, while maintaining financial stability, and thus to contribute to the development of the world economy; − to contribute to sound economic expansion in Member as well as non-member countries in the process of economic development; and − to contribute to the expansion of world trade on a multilateral, non-discriminatory basis in accordance with international obligations. The original Member countries of the OECD are Austria, Belgium, Canada, Denmark, France, Germany, Greece, Iceland, Ireland, Italy, Luxembourg, the Netherlands, Norway, Portugal, Spain, Sweden, Switzerland, Turkey, the United Kingdom and the United States. The following countries became Members subsequently through accession at the dates indicated hereafter: Japan (28th April 1964), Finland (28th January 1969), Australia (7th June 1971), New Zealand (29th May 1973), Mexico (18th May 1994), the Czech Republic (21st December 1995), Hungary (7th May 1996), Poland (22nd November 1996), Korea (12th December 1996) and the Slovak Republic (14 December 2000). The Commission of the European Communities takes part in the work of the OECD (Article 13 of the OECD Convention). -
Water Resources-Reconnaissance Series Report 54
STATE OF NEVADA ·DEPARTMENT OF CONSERVATION AND NATURAL RESOURCES DIVISION OF WATER RESOURCES Carson City / Photograph by Lawrence Radiation Laboratory· Sedan Crater was formed in the dry a ll uv ium of Yucca Flat by on underground atomic detonation. WATER RESOURCES-RECONNAISSANCE SERIES REPORT 54 REGIONAL GROUND-WATER SYSTEMS IN THE NEVADA TEST SITE AREA, NYE, LINCOLN, AND CLARK COUNTIES, NEVADA By F. Eugene Rush Prepared cooperatively by the Geological Survey, U.S. Department of the Interior 1970 WATER RESOURCES - RECONNAISSANCE: SEJUES REPORT 54 ·. REGIONAL GROUND-WATER SYSTEMS·IN THE NEVADA TEST SITE AREA, NYE, LINCOLN, AND CLARK COUN'riE:S, NEVADA By F. Eugene Rush PreparBd cooperatively by the Geological Survey, u.s. Department of the Interior 1971 -\ FOREWORD The progr~m of reconnaissance water-resources studies was authorized by the 1960 Legislature to be carried on by Division of Water Resources of the Departc.ment of· Conservation and Natural Resources in cooperation with the u.s. Geological Survey. This report is the 54th in the series to be prepared by the staff of the Nevada District Office of the U.S. Geological Survey. These 54 reports describe the hydrology of 185 valleys. The reconnaissance surveys make available pertinent information of great and immediate value to many State and Federal agencies, the State cooperating agency, and the public. As development takes place in any area, ,]c,,mands for more detailed information will arise, and studies to supply such information will be undertaken. In the meantime, these reconnaissance studies are timely and adequately In<'eet tlle immediate needs for information on the wate.r resources of the areas covered by the reports. -
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. -
Ground-Water Resources-Reconnaissance Series Report 20
- STATE OF NEVADA ~~~..._.....,.,.~.:RVA=rl~ AND NA.I...U~ a:~~::~...... _ __,_ Carson City_ GROUND-WATER RESOURCES-RECONNAISSANCE SERIES REPORT 20 GROUND- WATER APPRAISAL OF THE BLACK ROCK DESERT AREA NORTHWESTERN NEVADA By WILLIAM C. SINCLAIR Geologist Price $1.00 PLEASE DO NOT REMO V~ f ROM T. ':'I S OFFICE ;:: '· '. ~- GROUND-WATER RESOURCES--RECONNAISSANCE SERIES .... Report 20 =· ... GROUND-WATER APPRAISAL OF THE BLACK ROCK OESER T AREA NORTHWESTERN NEVADA by William C. Sinclair Geologist ~··· ··. Prepared cooperatively by the Geological SUrvey, U. S. Department of Interior October, 1963 FOREWORD This reconnaissance apprais;;l of the ground~water resources of the Black Rock Desert area in northwestern Nevada is the ZOth in this series of reports. Under this program, which was initiated following legislative action • in 1960, reports on the ground-water resources of some 23 Nevada valleys have been made. The present report, entitled, "Ground-Water Appraisal of the Black Rock Desert Area, Northwe$tern Nevada", was prepared by William C. Sinclair, Geologist, U. s. Geological Survey. The Black Rock Desert area, as defined in this report, differs some~ what from the valleys discussed in previous reports. The area is very large with some 9 tributary basins adjoining the extensive playa of Black Rock Desert. The estimated combined annual recharge of all the tributary basins amounts to nearly 44,000 acre-feet, but recovery of much of this total may be difficult. Water which enters into the ground water under the central playa probably will be of poor quality for irrigation. The development of good produci1>g wells in the old lake sediments underlying the central playa appears doubtful. -
Rnnr 59 Rnnr 59
RNNR_59 RNNR_59 TERRY KATZER, HYDROGEOLOGIST 2-11-2018 EDUCATION B.S. in Geology - Mackay School of Mines - University of Nevada, Reno, 1953-1958 Twelve units of graduate hydrogeology - University of Nevada, Reno, 1964-1966 Many technical and administrative short courses Professional Affiliations Geological Society of America (Hydrology Division, Program Manager, 1924), Inactive Colorado River Water Users Association, Inactive National Water Well Association, Inactive American Water Works Association (Water Management Committee member, 1987-90, Co-chair 1989-1990), Inactive American Water Resources Association, Inactive Nevada Water Resources Association, Active Sewage and Waste Water Committee, Advisory to the Board of Commissioners, Clark County, Nevada (member 1986-1990, Chairman 1988). EXPERIENCE BY DATE I became familiar with drilling and collecting core samples in 1960 while working for a mineral exploration company in Nevada. The company had interests in not only Nevada, but also Canada and Southeast Alaska. I sited holes, logged and split core from many holes in those areas. When I went to work for the U.S. Geological Survey I found myself back in Alaska on a drill rig in the Aleutian Islands. In addition to other duties I spent a great deal of time on one hole in Amchitka; it was for the second of three nuclear shots. Returning to Nevada for the USGS I sited and sampled water wells for the Native Americans near McDermit. It was the first time I worked with a Cable Tool Rig and a Mud Rotary Rig. I was a project member on the USGS Geothermal Investigations in the Fallon area that were drilled with a Mud Rotary Rig. -
Ar Iz Onautah California Cal If Orn Ia Oregon Idaho
DESIGNATED GROUNDWATER BASINS OF NEVADA £ * # £ 47N £ £ J OREGON IDAHO k a 11 e Jackpot r 18E 19E 10 24E 25E e b 20E 21E 5 McDermitt r 47N Denio £ 22E 26E 28E i 23E C 27E d E E Owyhee g e 2 2 68E 69E 70E / / 1 66E 67E 1 55E 6 1 47N 63E 64E 65E 4 46N 3 44E 46E 49E 50E 51E 52E 53E 57E 59E 60E 61E 62E 45E 47E 48E 5 2 54E 47N 56E 58E 30E 31E 32E 33E s 140 34E 35E 38E 41E B l 36E 37E 39E l 13 U 40E 42E 43E ru C V a K n a r e n F i R 46N n e a y g 39 o v u Mountain i n s i v 41 R 12 R e iv r Jarbidge Peak City e * 45N 2 *Capitol Peak 34 46N r 46N * Matterhorn C O re w ek 45N No y Copper Mtn. rth h n Fo e * o R rk e 33B 37 lm i L R a 44N v it 45N S 30A e t iv 4 140 r le e VU r 7 45N H u m Sun C 44N n bo 38 reek n ld 0 i t 40 u 68 9 Q Granite Peak 35 Wildhorse 44N 1 43N 33A * 8 3 29 Reservoir 9 44N 43N Vya U M a r 42N 43N ys Orovada* Santa Rosa Peak 30B 43N T 42N 27 *McAfee Peak 14 67 41N *Jacks Peak 42N A R S N 42N out h i F o v 41N e o r r r k t h 189B 189C L i 189A H t t l 40N Chimney e 41N 15 F 41N H Reservoir o u r r 25 e m k Tecoma v 42 40N i b 44 R o l d Humboldt t 36 R 40N i 39N 69 v r e 40N r e 93 v H U M B O L D T i £ 26 ¤ 189D 39N R t Montello ld 63 o b 39N 32 m R 38N 39N u E Li K O v 233 H e VU r 38N e 225 n l t VU in t u i Q ¤£95 L 31 38N 38N 66 Cobre 37N 16 37N Wells Ma 28 gg 80 ie ¨¦§ 37N Pilot Peak* A 37N Oasis 36N 36N C I r R e 93 e o ¤£ k c k 36N * Hole in the 36N Mtn. -
DESERT BIGHORN COUNCIL TRANSACTIONS VOLUME 8 A
DESERT BIGHORN COUNCIL TRANSACTIONS VOLUME 8 a Desert Bighorn Council A COMPILATION OF FORMAL PAPERS PRESENTED TO THE COUNCIL AT THE EIGHTH ANNUAL MEETING, APRIL 7, 8, AND 9, 1964, IN MEXICO AT THE AUDITORIO DE SOCIAL SEGURIDO IN MEXICALI AND AT THE HOTEL VILLA DEL MAR AT PUERTO SAN FELIPE, BAJA CALIFORNIA. THE DESERT BIGHORN COUNCIL TRANSACTIONS ARE PUBLISHED ANNUALLY AND ARE AVAILABLE BY WRITING THE . "DESERT BIGHORN COUNCIL" P. 0. BOX 440, LAS VEGAS, NEVADA. COVER DRAWING. BY PAT HANSEN. EIGHTH ANNUAL MEETING DESERT BHGI3ORN COUNCIL April 7, 8, 9, 1964 Mexicali and Puerto San Felipe, Baia California TABLE OF CONTEWS Page .. - program ........................................................ 111 Group Picture ................................................... vii Opening Remarks Dr. Rodolfo Hernandez Corzo, Chairman ............................. xv John P. Russo, Vice-Chairman ................................... x.ix . pp-ppp- . ........................................- -- ... -- --- - .- FORMAL PAPERS AND DISCUSSIONS DESERT BIGHORN SHEEP AT THE SAN DIEGO ZOOLOGICAL GARDEN George H. Pournelle, Curator of hlammals ............................ 1 .~DIXTIOSALNOTES ON PARASITES OF BIGHORN SHEEP ON THE DESERT GAME RANGE, NEVADA Rex W. Allen .............................................. 5 1-OXG-DISTASCE AND NIGHTTLME MOVEMENTS OF DESERT BIGHORh' SHEEP Gale hlonson ............................................... 11 IIESERT BIGHORN MAVAGEMENT NEEDS FROM THE ACADEhllC . porn?; OF VIEW U'ilIiamGraf .............................................. -
University of Nevada Reno Determination of Timing Of
University of Nevada Reno J Determination of Timing of Recharge for Geothermal Fluids in The Great Basin Using Environmental Isotopes and Paleoclimate Indicators A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science, in geology by Paul K. Buchanan 1" April, 1990 i MINES LIBRARY Tti GS Li a (ths The thesis of Paul K. Buchanan is approved by University of Nevada Reno April, 1990 11 ACKNOWLEGEMENTS This study was made possible by grant DE-FG07-88ID12784 from the United States Department of Energy, Geothermal Technology Division, administered by the Idaho Operations Office, Idaho Falls, Idaho. Additional financial assistance from the Nevada Section of the Geothermal Resources Council aided in the completion of this thesis. My thanks go to the Nevada geothermal power industry for allowing fluid sampling of deep powerplant production wells. Specifically, Chevron Resources, Oxbow Geothermal, Ormat Energy Systems, Geothermal Food Processors, Tad's Enterprises, Thermochem Inc., Elko Heat Co. and Elko School District are thanked. Thanks also to Dr. Robert Fournier of the United States Geological Survey for providing data on the Coso geothermal system. Michelle Stickles is to be commended for suffering through the proof reading of the initial drafts of this report. Thanks to my advisor, Jim Carr, and my committee members, Mel Hibbard and Gary Haynes, for taking on this project and putting up with my inconsistent scheduling and "last minute" rush. Special thanks to my cohorts at the Division of Earth Sciences and Mackay School of Mines for their cynical attitudes that helped keep it all in perspec- tive, through both the good and the bad times. -
Fundamental Concepts of Recharge in the Desert Southwest: A
Water Sci. and Appl. Groundwater Recharge in a Desert Environment: The Southwestern United States Vol. 9 FundamentalConcepts of Rechargein the Desert Southwest: A RegionalModeling Perspective Alan L. Flint, LorraineE. Flint, and JosephA. Hevesi U.S. GeologicalSurvey, Sacramento, California JoanB. Blainey U.S. GeologicalSurvey, Tucson, Arizona Rechargein arid basinsdoes not occur in all years or at all locationswithin a basin.In the desertSouthwest potential evapotranspiration exceeds precipitation on an averageannual basis and, in many basins,on an averagemonthly basis. Groundwatertravel time from the surfaceto the water table and rechargeto the water table vary temporallyand spatiallyowing to variationsin precipitation,air temperature,root zone and soil propertiesand thickness,faults and fractures,and hydrologicproperties of geologicstrata in the unsaturatedzone. To highlightthe fundamentalconcepts controlling recharge in the Southwest,and addressthe tem- poral and spatial variability of recharge, a basin characterizationmodel was developedusing a straightforwardwater balanceapproach to estimatepotential rechargeand runoff and allow for determinationof the locationof rechargewith- in a basin.It providesa meansfor interbasincomparison of the mechanismsand processesthat result in rechargeand calculatesthe potential for rechargeunder current,wetter, and drier climates.Model estimatesof rechargecompare favor- ably with othermethods estimating recharge in the Great Basin. Resultsindicate that net infiltration occursin less than 5 percentof -
Nevada Hydrographic Areas and Sub-Areas/Listed Alphabetically by Primary County of Location Basin Area Area Area Num
Appendix A-4--Nevada Hydrographic Areas and Sub-Areas/Listed Alphabetically by Primary County of Location Basin Area Area Area Num. Num. (sq.mi.) (acres) Desig Hydrograph Area/Sub-Area Counties [1] [2] [3] [4] Nearest Cities [6] Name Included [5] Carson City, 8 104 69 44,160 Eagle Valley Carson City Yes Douglas Frenchman, 10 125 43 27,520 Stingaree Valley Churchill Yes Eastgate 5 77 58 37,120 Fireball Valley Churchill Nixon, Fernley No Frenchman, 10 126 110 70,400 Cowkick Valley Churchill Yes Eastgate 10 133 416 266,240 Edwards Creek Valley Churchill Eastgate, Austin No 10 127 216 138,240 Eastgate Valley Area Churchill Eastgate Yes Bradys Hot Springs, 5 75 178 113,920 Brady Hot Springs Area Churchill, Lyon Yes Fernley Churchill, Frenchman, Fallon, 10 124 285 182,400 Fairview Valley Yes Mineral Eastgate Churchill, 10 123 227 145,280 Rawhide Flats Schurz, Fallon No Mineral, Lyon Churchill, 4 74 164 104,960 White Plains Lovelock, Fernley Yes Pershing Churchill, 10 128 1,303 833,920 Dixie Valley Dixie Valley, Fallon Yes Pershing, Lander Churchill, 8 101 2,022 1,294,080 Carson Desert Fallon, Stillwater Yes Pershing, Lyon North Las Vegas, 13 217 80 51,200 Hidden Valley Clark No Moapa Boulder City, 10 167 530 339,200 Eldorado Valley Clark Yes Searchlight Las Vegas, 13 212 1,564 1,000,960 Las Vegas Valley Clark Yes Henderson 13 223 533 341,120 Gold Butte Area Clark Overton, Logandale No 10 165 96 61,440 Jean Lake Valley Clark Jean, Goodsprings Yes Three Lakes Valley-Southern 13 211 311 199,040 Clark Indian Springs Yes Part Bunkerville, 13 224