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Panamint Valley Days
OPERATION PAGE 17 CALIFORNIA FOUR WHEEL DRIVE ASSOCIATION PANAMINT VALLEY DAYS PAGES 20-21 cal4wheel.com Official publication of the California Four Wheel Drive Association PLEASE THANK OUR SPONSORS FOR THEIR DONATIONS WITH YOUR SUPPORT GOLD SPONSORS 4wheelparts.com linex.com genright.com advanceadapters.com metalcloak.com crawlerconceptz.com magellangps.com poisonspyder.com bfgoodrichtires.com warn.com SILVER SPONSOR extremeterrain.com aftermarket.auburngear.com spiderwebshade.com BRONZE SPONSORS quadratec.com calcasuals.com 4xshaft.com rockhard4x4.com differentials.com bilsteinus.com arbusa.com magnaflow.com racelinewheels.com 4x4spod.com yukongear.com tuffyproducts.com WIN-A-JEEP SPONSORS To become a sponsor, contact David Jones at 530-367-2443 or [email protected] 2 IN GEAR October / November 2017 cal4wheel.com OPERATION DESERT FUN 2009 BY JESSE MAY WHO ARE WE? The California Four Wheel Drive Association, Inc. (founded in 1959) is a non-profit organization comprised of member clubs, individuals and business INSIDE firms, united in a common objective — the betterment President’s Message 7 of vehicle-oriented outdoor recreation. C4WDA Contacts 4 We represent four-wheelers, hunters, fishermen, District Meetings 3 and other outdoor recreationalists. Ours is the largest Safety Requirements 3 organization of its type in California. VP Reports 8-9 Natural Resource Consultants 10-11 THROUGH A UNITED EFFORT WE: Swamp Lake monster clearing 14 • Promote responsible use of public lands. Figure 8 race carnage under control 16 • Prevent legislation that would restrict off-road Operation Desert Fun info 17 vehicles and vehicle use. Hi Desert Round-Up raffle thanks 18 • Develop programs of conservation, education Donations 18 and safety. -
Technical Memorandum
Technical Memorandum DATE: July 3, 2019 PROJECT: 19-1-047 TO: Shawnda Grady, ESQ Ellison, Schneider, Harris & Donlan FROM: Eddy Teasdale, P.G., CHG. Mehrdad Bastani SUBJECT: Ground Water (Hydrologic) Technical Memorandum Report to Support San Bernardino Conditional Use Permit Related to Adequate Service Certification Water and Sewer (Form W2) - PVL Lime Plant APN: 0485-031-12 1 INTRODUCTION This Technical Memorandum (TM) describes the process used to determine groundwater availability and evaluate potential impacts of operating a new planned industrial well on existing groundwater users in the area. Provided herein are the key findings, conclusions, and preliminary recommendations regarding water availability for the proposed PVL processing plant in Trona, California (Project). Implementation of the Project will utilize water from a recently installed on-site production well. For drinking water, the Project proposed to utilize an estimated 1.3 gallons per minute (gpm). To meet operational requirements related to domestic and processing usage, the new planned well will need to produce a maximum of 30 gpm (49 AF/year). 2 GEOLOGY AND HYDROGEOLOGY Searles Valley is a north-trending structural valley that is bound by the Argus Range on the west and north and by the Slate Range on the north and east. The Garlock Fault is generally recognized as the southern limit of the groundwater basin, however topographically, the surface water drainage area of the valley continues south of the Garlock fault. The area of the Searles Valley drainage basin is estimated to be about 693 square miles. There are three primary hydrogeologic units within the Searles Valley, alluvial deposits, saline deposits and bedrock complex. -
Interest and the Panamint Shoshone (E.G., Voegelin 1938; Zigmond 1938; and Kelly 1934)
109 VyI. NOTES ON BOUNDARIES AND CULTURE OF THE PANAMINT SHOSHONE AND OWENS VALLEY PAIUTE * Gordon L. Grosscup Boundary of the Panamint The Panamint Shoshone, also referred to as the Panamint, Koso (Coso) and Shoshone of eastern California, lived in that portion of the Basin and Range Province which extends from the Sierra Nevadas on the west to the Amargosa Desert of eastern Nevada on the east, and from Owens Valley and Fish Lake Valley in the north to an ill- defined boundary in the south shared with Southern Paiute groups. These boundaries will be discussed below. Previous attempts to define the Panamint Shoshone boundary have been made by Kroeber (1925), Steward (1933, 1937, 1938, 1939 and 1941) and Driver (1937). Others, who have worked with some of the groups which border the Panamint Shoshone, have something to say about the common boundary between the group of their special interest and the Panamint Shoshone (e.g., Voegelin 1938; Zigmond 1938; and Kelly 1934). Kroeber (1925: 589-560) wrote: "The territory of the westernmost member of this group [the Shoshone], our Koso, who form as it were the head of a serpent that curves across the map for 1, 500 miles, is one of the largest of any Californian people. It was also perhaps the most thinly populated, and one of the least defined. If there were boundaries, they are not known. To the west the crest of the Sierra has been assumed as the limit of the Koso toward the Tubatulabal. On the north were the eastern Mono of Owens River. -
SOUTHEASTERN INYO Tt;OUNTAINS, CALIFORNIA
CALIFORNIA STATE UNIVERSITY, NORTHRIDGE SUPERPOSED MESOZOIC DEFOR~~TIONS~ }) SOUTHEASTERN INYO tt;OUNTAINS, CALIFORNIA A thesis submitted in partial satisfaction of the requirements for the degree of 14aster of Science in Geology by Michael Robert Werner Janu(l.ry 3 i 979 The Thesis of Michael Robert Werner is approved: Or. L. Ehltg}rCSULA) Ca 1i forn i a State Un i vers ·j ty, Northridge ii ACKNOWLEDGEMENTS ~1y respectful thanks to George Dunn£ for suggesting this study and for his helpful comments throughoutthe investigation. I am grateful also to Rick Miller and Perry Eh1ig VJho reviewed the manuscript in various stages of preparation. !'r1y special thanks to my parents for theit~ emotiona1 and 1ogistica·i support, and to Diane Evans who typed the first draft. Calvin Stevens and Duane Cavit, California State University~ San Jose, provided valuable information on stratigraphy; and Jean Ju11iand, geologist of the Desert Plan Staff, BLM, Riverside, made available aerial photographs of the study area.· The Department of Geosciences, California State University. Northridge pi·ovided computer time and financial support. Terry Dunn, CSUN, typed the fina1 manuscript. iii TAaLE OF CONTENTS p~~ ACKNOl~LEDGEHENTS. .. 111 LIST OF ILLUSTRATIONS . vi ABSTRACT ... vii. INTRODUCTION 1 METHOD • 3 ROCK UNITS •. 5 PALEOZOIC STRATIGRAPHY . 5 Perdido Formation 7 Rest Spring Shale . .. 3 Keeler Canyon Formation 10 Owens Vulley Formation 14 MESOZOIC INTRUSIVE ROCKS . 16 • Hunter Mountain batholith 16 Andes 'ite porphyry di kas 17 CENOZOIC UNITS . 18 STRUCTURJl.L GEOLOGY 19 FOLDS • ~ . 19 Introduction 19 Folds in the Nelson Range . 21 F., - The San Lucas Canyon syncline 2"1 j r2 - Northwest-trending folds 31 Folds aajacent to the Hunter Mountain batholith 37 Folds in the Southeastern Inyo r'Jounta·ins 43 Southwest-trending folds 43 Northwest-trending folds . -
Middle Miocene to Recent Exhumation of the Slate Range, Eastern California, and Implications for the Timing of Extension and the Transition to Transtension
Middle Miocene to recent exhumation of the Slate Range, eastern California, and implications for the timing of extension and the transition to transtension J. Douglas Walker, Tandis S. Bidgoli, Brad D. Didericksen*, Daniel F. Stockli†, and Joseph E. Andrew Department of Geology, University of Kansas, Lawrence, Kansas 66045, USA ABSTRACT sional belt at the latitude of Las Vegas, Nevada, 2005) considered the Furnace Creek fault to be may have been stretched as much as 300% since active from ca. 9 to 5 Ma, and that this fault is a New mapping combined with fault-slip and ca. 16 Ma (e.g., Wernicke et al., 1988; Niemi component of the dextral regime (Fig. 1). Snow thermochronological data show that Middle et al., 2001). The earlier deformation resulted and Lux (1999) interpreted the change to dex- Miocene to recent extension and exhumation in primarily east-west extension across the tral deformation in Death Valley to have started of the Slate Range, eastern California, is pro- region (Wernicke et al., 1982, 1988), initiat- ca. 11 Ma (Fig. 1). Other studies that focus on duced by the active Searles Valley fault sys- ing ca. 15 Ma, as inferred by the ages of early different areas interpret younger ages for this tem and the Slate Range detachment, an older basin deposits of the Panuga (Snow and Lux, change to transtension. Hodges et al. (1989) Middle Miocene low-angle normal fault. Off- 1999) and Eagle Mountain formations (Niemi placed the transition as ca. 3.7 Ma in Pana- set Middle Miocene rocks record a combined et al., 2001) of the northern Death Valley area, mint Valley (Fig. -
Ridgecrest BUREAU of LAND MANAGEMENT
BLM SPECIAL EDITION 1998 EXAMPLES OF AGENCY SIGNS SURFACE MANAGEMENT STATUS DESERT ACCESS GUIDE Ridgecrest BUREAU OF LAND MANAGEMENT USDA FOREST SERVICE l:100,0()0-Scale topographic map showing: Highways, roads and other manmade structures Water features • Contours and elevations in meters Recreation sites • Coverage of former desert access guide #4 Ridgecrest NATIONAL PARK SERVICE UNITED STATES DEPARTMENT OF THE INTERIOR BUREAU OF LAND MANAGEMENT CALIFORNIA STATE PARKS Edited and published by the Bureau of Land Management National Applied Resource Sciences Center, Denver, Colorado in cooperation with the Bureau of Land Management California State Office. Planimetry partially revised by BLM from various source material. Revised information not field . he. i-rd Base map prepared by the U.S. Geological Survey. Compiled from USGS 1:24,000 and l:62,5O0-scale topographic maps dated 1949-1973, and from advance materials. Partially revised from aerial photographs taken 1973-1989 and other source data. Revised information not CALIFORNIA STATE field checked. Map edited 1993. VEHICULAR RECREATION AREA Help protect your public lands by observing posted Projection and 10,000-meter grid, zone 11: Universal OHV designations. Watch for OHV signs and read hari'.verse Mercator. 25,000-foot grid licks based on them carefully. California coordinate system, zone 4 and 5. 1927 North American Datum. For more information contact the HIM, USDA Forest Service, National Park Service, California State Park, or California State Motorized Vechicle Recreation Area Land lines are omitted in areas of extensive tract surveys. Office (see back panel for address and phone There may be private inholdings within the boundaries of numbers). -
California Rare & Endagered Birds
California brown pelican Pelecanus occidentalis californicus State Endangered 1971 Fully Protected Federal Endangered 1970 General Habitat: The California brown pelican uses a variety of natural and human-created sites, including offshore islands and rocks, sand spits, sand bars, jetties, and piers, for daytime loafing and nocturnal roosting. Preferred nesting sites provide protection from mammalian predators and sufficient elevation to prevent flooding of nests. The pelican builds a nest of sticks on the ground, typically on islands or offshore rocks. Their nesting range extends from West Anacapa Island and Santa Barbara Island in Channel Islands National Park to Islas Los Coronados, immediately south of and offshore from San Diego, and Isla San Martín in Baja California Norte, Mexico. Description: The brown pelican is one of two species of pelican in North America; the other is the white pelican. The California brown pelican is a large, grayish-brown bird with a long, pouched bill. The adult has a white head and dark body, but immature birds are dark with a white belly. The brown pelican weighs up to eight pounds and may have a wingspan of seven feet. Brown pelicans dive from flight to capture surface-schooling marine fishes. Status: The California brown pelican currently nests on West Anacapa Island and Santa Barbara Island in Channel Islands National Park. West Anacapa Island is the largest breeding population of California. In Mexico, the pelicans nest on Islas Los Coronados and Isla San Martín. Historically, the brown pelican colony on Islas Los Coronados was as large as, or larger than, that of recent years on Anacapa Island. -
The California Desert CONSERVATION AREA PLAN 1980 As Amended
the California Desert CONSERVATION AREA PLAN 1980 as amended U.S. DEPARTMENT OF THE INTERIOR BUREAU OF LAND MANAGEMENT U.S. Department of the Interior Bureau of Land Management Desert District Riverside, California the California Desert CONSERVATION AREA PLAN 1980 as Amended IN REPLY REFER TO United States Department of the Interior BUREAU OF LAND MANAGEMENT STATE OFFICE Federal Office Building 2800 Cottage Way Sacramento, California 95825 Dear Reader: Thank you.You and many other interested citizens like you have made this California Desert Conservation Area Plan. It was conceived of your interests and concerns, born into law through your elected representatives, molded by your direct personal involvement, matured and refined through public conflict, interaction, and compromise, and completed as a result of your review, comment and advice. It is a good plan. You have reason to be proud. Perhaps, as individuals, we may say, “This is not exactly the plan I would like,” but together we can say, “This is a plan we can agree on, it is fair, and it is possible.” This is the most important part of all, because this Plan is only a beginning. A plan is a piece of paper-what counts is what happens on the ground. The California Desert Plan encompasses a tremendous area and many different resources and uses. The decisions in the Plan are major and important, but they are only general guides to site—specific actions. The job ahead of us now involves three tasks: —Site-specific plans, such as grazing allotment management plans or vehicle route designation; —On-the-ground actions, such as granting mineral leases, developing water sources for wildlife, building fences for livestock pastures or for protecting petroglyphs; and —Keeping people informed of and involved in putting the Plan to work on the ground, and in changing the Plan to meet future needs. -
Geology of the Panamint Butte Quadrangle, Inyo County, California
Geology of the Panamint Butte Quadrangle, Inyo County, California By WAYNE E; HALL GEOLOGICAL SURVEY BULLETIN 1299 Prepared in cooperation with the California Department of Conservation, Division of Mines and Geology KhCEIVED JUL161971 u.8.1 teuisfiUt, it UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1971 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 75-610447 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract_________________________________-_.-______-__--_-_--_--- 1 Introduction. ___________-______--_____--_----.--___--__-__--------- 2 Climate.and vegetation._________.__....__.._____-___________-__ 3 Water supply-________________________________________________ 3 Previous work__________________________.___._____._1________ 4 Acknowledgments- _______________._______..____-__-_---------_- 4 General geology.__________________________-__..____--_----_-_--__-- 5 Precambrian(?) rocks._____________.__________.._----___-___-_-_-__- 7 Paleozoic rocks._____.__.___--________-___-____-_-----_---_--.-.-_- 8 Cambrian System_____________________________________________ 8 Carrara Formation.__________________..-_____--____---__-_- 8 Bonanza King Formation___._.______..__._._.....____.____ 10 Nopah Formation._____...____-_-_.....____________-_-_-__- 11 Ordovician System___________________________________________ 13 Pogonip Group_____-__-______-____-_-..----------_--._-_-_- 13 Eureka Quartzite.______________-_____..___-_-_---_-----_--_ 16 Ely Springs Dolomite__---__-______________________________ 18 Silurian and Devonian Systems___________..__-_-__----_-__-___- 21 Hidden Valley Dolomite......._____________________________ 21 Devonian System_____________________________________________ 22 Lost Burro Formation.....__________________________________ 22 Mississippian System.___._____..____._.._..__.___..._._._..__. -
An Outline of the Story of Trona, from BLM Records
An Outline the Story of the Trona Area from Bureau of Land Management Records March 2014 Larry M Vredenburgh Bureau of Land Management 3801 Pegasus Drive Bakersfield, CA 93308 [email protected] BLM Web Resources Over the last few years Bureau of Land Management land records have been made available to the public on two websites. The Official Federal Land Records Site (http://www.glorecords.blm.gov/), hosts transcribed records as well as original documents, survey plats and Master Title Plats. The Bureau of Land Management’s Land & Mineral Legacy Rehost 2000 System website, known as LR2000, (http://www.blm.gov/lr2000/) compliments the “GLO Records” site by providing additional ways to query BLM records, as well as more detailed reports on land use authorizations. These websites provide researchers with a treasure trove of historic information. I have utilized a sample of this information to create an outline of the story of the development of the Trona area. Land Patents According to no less a source than Wikipedia, a land patent is, “. an exclusive land grant made by a sovereign entity over the land in question. To make such a grant “patent”, a sovereign (proprietary landowner) must document the land grant, securely sign and seal the document (patent), and openly publish the documents for the public to see.” On March 4, 1788, the first land patent was issued by the United States of America to John Martin in what is now Belmont County, Ohio. Twenty- four years later, in 1812, the General Land Office (GLO) was created to handle and dispose of public lands. -
2020 Volume 2
Society for the Conservation of Bighorn Sheep Sheep Sheet - Volume 2 – September 2020 www.desertbighorn.org Before the project began, collection box area in sad shape After the project: a formal, robust spring box Redwood Spring Box Installed at Castle Mine Spring By Debbie Miller Marschke SCBS has been working to improve the natural spring at the Castle Mine location for many years. Mining ruins and a dilapidated cabin remain as evidence that this spring has a history of folks teasing out the precious water from this location. There is always an overgrowth of vegetation at the spring which is proof positive that the spring is active, even if the flow rate is minimal. Bighorn Sheep biologists have GPS data from collared sheep in the mountain range that prove the Bighorn Sheep wander along the backbones of the ridges; occasionally they visit this spring but they mainly depend on the big game guzzlers to the north of this location. Nevertheless, each water location in a mountain range is crucial in the network of water sources available. SCBS crews have dug out and cleared the guzzler intake Johnson screen several times on previous occasions which has been very frustrating because a spring box had never been installed. The water seeps from the entrance of an old mine adit in the side of a hill. The hill face and adit entrance are unstable, and thus dirt caves in and has buried the intake system time and time again. On the weekend of May 15-17, 2020, a modest SCBS strike force sought to make one final but meaningful attempt to boost water output from Castle Mine spring. -
Some Desert Watering Places
DEPAETMENT OF THE INTEEIOE UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DiRECTOK WATER-SUPPLY PAPER 224 SOME DESERT WATERING PLACES IN SOUTHEASTEEN CALIFORNIA AND SOUTHWESTERN NEVADA BY WALTER C. MENDENHALL WASHINGTON GOVERNMENT PRINTING OFFICE 1909 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR WATER-SUPPLY PAPEK 224 SOME DESERT WATERING PLACES IN SOUTHEASTEEN CALIFOKNIA AND SOUTHWESTEKN NEVADA BY WALTER C. MENDENHALL WASHINGTON GOVERNMENT PRINTING OFFICE 1909 CONTENTS. Page. Introduction______________________________________ 5 Area considered_________________________________ 5 Mineral resources and industrial developments______________ . 6 Sources of data__________________________________ 7 Physical features__________________________________ 8 General character of the region______________________ 8 Death Valley basin__________________________________ 9 Soda Lake_____________________________________ 30 Salton Sink______________________________________ 10 A great trough_______________________________ 30 Fault lines__________________.____ ______________ 11 Climate______________________. ____ ______________ 11 Water supply_________ _________________________ 13 Origin_________________________________________ 13 Rivers______________________________________ 13 Springs__________________________________________ 15 Finding water_______________________________ 16 Camping places_______________________________ 16 Mountain springs and tanks______________________ 17 Dry lakes____________________________________