Standards for Rangeland Health
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Utah Geological Association Publication 30.Pub
Utah Geological Association Publication 30 - Pacific Section American Association of Petroleum Geologists Publication GB78 239 CENOZOIC EVOLUTION OF THE NORTHERN COLORADO RIVER EXTEN- SIONAL CORRIDOR, SOUTHERN NEVADA AND NORTHWEST ARIZONA JAMES E. FAULDS1, DANIEL L. FEUERBACH2*, CALVIN F. MILLER3, 4 AND EUGENE I. SMITH 1Nevada Bureau of Mines and Geology, University of Nevada, Mail Stop 178, Reno, NV 89557 2Department of Geology, University of Iowa, Iowa City, IA 52242 *Now at Exxon Mobil Development Company, 16825 Northchase Drive, Houston, TX 77060 3Department of Geology, Vanderbilt University, Nashville, TN 37235 4Department of Geoscience, University of Nevada, Las Vegas, NV 89154 ABSTRACT The northern Colorado River extensional corridor is a 70- to 100-km-wide region of moderately to highly extended crust along the eastern margin of the Basin and Range province in southern Nevada and northwestern Arizona. It has occupied a criti- cal structural position in the western Cordillera since Mesozoic time. In the Cretaceous through early Tertiary, it stood just east and north of major fold and thrust belts and also marked the northern end of a broad, gently (~15o) north-plunging uplift (Kingman arch) that extended southeastward through much of central Arizona. Mesozoic and Paleozoic strata were stripped from the arch by northeast-flowing streams. Peraluminous 65 to 73 Ma granites were emplaced at depths of at least 10 km and exposed in the core of the arch by earliest Miocene time. Calc-alkaline magmatism swept northward through the northern Colorado River extensional corridor during early to middle Miocene time, beginning at ~22 Ma in the south and ~12 Ma in the north. -
The Geology of the Tuff of Bridge Spring: Southern Nevada and Northwestern Arizona
UNLV Theses, Dissertations, Professional Papers, and Capstones 12-1993 The geology of the Tuff of Bridge Spring: Southern Nevada and northwestern Arizona Shirley Ann Morikawa University of Nevada, Las Vegas Follow this and additional works at: https://digitalscholarship.unlv.edu/thesesdissertations Part of the Geochemistry Commons, Geology Commons, Stratigraphy Commons, and the Volcanology Commons Repository Citation Morikawa, Shirley Ann, "The geology of the Tuff of Bridge Spring: Southern Nevada and northwestern Arizona" (1993). UNLV Theses, Dissertations, Professional Papers, and Capstones. 1453. The Geology of the TufT of Bridge Spring: Southern Nevada and Northwestern Arizona by Shirley Ann Morikawa A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology Geoscience Department University of Nevada, Las Vegas December, 1993 © 1994 Shirley Ann Morikawa All Rights Reserved The thesis of Shirley Ann Morikawa for the degree of Master of Science in Geology is approve . r, Ernest M. Duebendorfer, Ph.D. Graduate Faculty Representaf , Donna E.Weistrop, Ph.D. Dean of the Graduate College, Ronald W. Smith, Ph.D. University of Nevada, Las Vegas December, 1993 ii Abstract The Tuff of Bridge Spring (TBS) is a regionally-widespread, andesite to rhyolite (59 .50 to 74.91 wt. %) ash-flow tuff of mid-Miocene age (ca. 15.2 Ma) that is exposed in the northern Colorado River extensional corridor of southern Nevada and northwestern Arizona. Determination of the areal distribution, geochronology, lithology, geochemistry, and internal stratigraphy of the TBS is important for its establishment as a reliable stratigraphic reference horizon for tectonic reconstructions of the extensional corridor during the middle Miocene. -
Detrital-Zircon U-Pb Evidence Precludes Paleo–Colorado River Sediment in the Exposed Muddy Creek Formation of the Virgin River Depression
CRevolution 2: Origin and Evolution of the Colorado River System II themed issue Detrital-zircon U-Pb evidence precludes paleo–Colorado River sediment in the exposed Muddy Creek Formation of the Virgin River depression William R. Dickinson1, Karl E. Karlstrom2, Andrew D. Hanson3, George E. Gehrels1, Mark Pecha1, Steven M. Cather4, and David L. Kimbrough5 1Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA 2Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 97131, USA 3Department of Geoscience, University of Nevada–Las Vegas, Box 454010, Las Vegas, Nevada 89154-7003, USA 4New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Place, Socorro, New Mexico 87801, USA 5Department of Geological Sciences, San Diego State University, San Diego, California 92182, USA ABSTRACT course through the Grand Canyon to enter the For comparative purposes, previously unpub- Grand Wash Trough at the eastern end of mod- lished detrital-zircon data for the Chuska Sand- Only since 5–6 Ma has the Colorado River ern Lake Mead (Blair and Armstrong, 1979; stone are included in the Supplemental File1. fl owed through the western Grand Canyon House et al., 2005; Crossey et al., 2014). Vari- For visual comparisons of detrital-zircon into the Grand Wash Trough at the eastern ous lines of evidence (Lucchitta, 1989; Pelletier, populations, we use frequency plots of grain end of Lake Mead. Before then, the river may 2010; Dickinson, 2013; Lucchitta et al., 2013) ages, with analytical age uncertainties (±1σ) have fl owed through a paleocanyon transit- argue that a Miocene Colorado River transited for each grain age taken into account, normal- ing the Kaibab uplift at a stratigraphic level the Kaibab uplift through a paleocanyon near ized to subtend equal areas beneath each curve above the present eastern Grand Canyon the present site of the eastern Grand Canyon, of graphical displays. -
Black Mountain Herd Management Area Wild Burro Gather and Population Control Plan Environmental Assessment
United States Department of the Interior Bureau of Land Management Environmental Assessment DOI-BLM-AZ-C010-2019-0030-EA Black Mountain Herd Management Area Wild Burro Gather and Population Control Plan Environmental Assessment Mohave County, Arizona U.S. Department of the Interior U.S. Department of the Interior Bureau of Land Management Bureau of Land Management Colorado River District Colorado River District Kingman Field Office Lake Havasu Field Office 2755 Mission Blvd. 1785 Kiowa Ave. Kingman, Arizona 86401 Lake Havasu City, Arizona 86403 (928) 718-3700 (928) 505-1200 February 2020 It is the mission of the Bureau of Land Management to sustain the health, diversity, and productivity of the public lands for the use and enjoyment of present and future generations. DOI-BLM-AZ-C010-2019-0030-EA Compliance for Section 508 of the Rehabilitation Act The contents of this document, when accessed electronically, may not be fully Section 508 compliant with all software applications and readers. Please contact the Kingman Field Office for assistance. We will try to assist you as best we can. This may require providing the information to you in a text-only format. Table of Contents CHAPTER 1 INTRODUCTION 1 1.1 Background 1 1.2 Purpose of and Need for Action 3 1.3 Plan Conformance 3 1.4 Relationship to Statutes, Regulations, Policies or other Plans 4 1.5 Decision to be Made 5 1.6 Scoping and Issue Identification 5 CHAPTER 2 PROPOSED ACTION AND ALTERNATIVES 5 2.1 Alternative A (Proposed Action) 6 2.2 Alternative B 6 2.3 Alternative C 7 2.4 Alternative -
Detrital Wash Watershed – Arizona Rapid Watershed Assessment April 2007
Detrital Wash Watershed – Arizona Rapid Watershed Assessment April 2007 Prepared by: USDA Natural Resource Conservation Service – Arizona University of Arizona, Water Resources Research Center In cooperation with: Arizona Association of Conservation Districts Arizona Department of Agriculture Arizona Department of Environmental Quality Arizona Department of Water Resources Arizona Game & Fish Department Arizona State Land Department USDA Forest Service USDI Bureau of Land Management Released by: Sharon Megdal David McKay Director State Conservationist University of Arizona U.S. Department of Agriculture Water Resources Research Center Natural Resources Conservation Service Principle Investigators: Dino DeSimone – Natural Resources Conservation Service, Phoenix, Arizona Keith Larson – Natural Resources Conservation Service, Phoenix, Arizona Kristine Uhlman – Water Resources Research Center, University of Arizona D. Phil Guertin – School of Natural Resources, University of Arizona Deborah Young – Associate Director, Cooperative Extension, University of Arizona The United States Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, gender, religion, age, disability, political beliefs, sexual orientation, and marital or family status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at -
Mineral Resources of the Mount Tipton Wilderness Study Area,89 795
I 19.3:1737-B Mineral Resources of the Mount Tipton Wilderness Study Area,89 _ 795 Mohave County, Arizona GEORGIA TECH LIBRI,RY DEC 07 1989 GOV IS DEPOSITORY COLLECTION U.S. GEOLOGICAL SURVEY BULLETIN 1737—B U UORTMENT OF 1H INTERIOR ..RECJLANM.M.T AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the cur- rent-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Sur vey publications released prior to the current year are listed in the most recent annual "Price and Availability List." Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated month ly, which is for sale in microfiche from the U.S. Geological Survey, Books and Open-File Reports Section, Federal Center, Box 25425, Denver, CO 80225. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Techniques of Water-Resources Investigations, Circulars, publications of general in Books of the U.S. -
Cenozoic Evolution of the Abrupt Colorado Plateau–Basin And
The Geological Society of America Field Guide 11 2008 Cenozoic evolution of the abrupt Colorado Plateau–Basin and Range boundary, northwest Arizona: A tale of three basins, immense lacustrine-evaporite deposits, and the nascent Colorado River James E. Faulds* Nevada Bureau of Mines and Geology, MS 178, University of Nevada, Reno, Nevada 89557, USA Keith A. Howard* U.S. Geological Survey, MS 973, Menlo Park, California 94025, USA Ernest M. Duebendorfer* Department of Geology, Northern Arizona University, Flagstaff, Arizona 86011, USA ABSTRACT In northwest Arizona, the relatively unextended Colorado Plateau gives way abruptly to the highly extended Colorado River extensional corridor within the Basin and Range province along a system of major west-dipping normal faults, including the Grand Wash fault zone and South Virgin–White Hills detachment fault. Large growth-fault basins developed in the hanging walls of these faults. Lowering of base level in the corridor facilitated development of the Colorado River and Grand Can- yon. This trip explores stratigraphic constraints on the timing of deformation and paleogeographic evolution of the region. Highlights include growth-fault relations that constrain the timing of structural demarcation between the Colorado Plateau and Basin and Range, major fault zones, synextensional megabreccia deposits, non- marine carbonate and halite deposits that immediately predate arrival of the Colo- rado River, and a basalt fl ow interbedded with Colorado River sediments. Structural and stratigraphic relations indicate that the current physiography of the Colorado Plateau–Basin and Range boundary in northwest Arizona began developing ca. 16 Ma, was essentially established by 13 Ma, and has changed little since ca. -
Discover Lake Mead from the East
Lake Mead National Park Service National Recreation Area U.S. Department of the Interior Discover... Lake Mead National Recreation Area from the East If you are exploring Lake Mead Joshua Tree Forest South Cove National Recreation Area by way Located on and around South Cove is the farthest east of Arizona here are some special Grapevine Mesa near Meadview, you can launch a boat in the places to discover. Arizona, is one of the largest and recreation area. Parking, densest Joshua tree forests of its restrooms, emergency call box Campgrounds kind in the world. and a launchramp are available. Bring the RV or a tent to camp Pay close attention to fluctuating out at Temple Bar. There is also The forest is designated as an water as reefs and sand bars can plenty of backcountry camping Area of Critical Environemental appear without warning. including a primitive campground Concern (ACEC). Hiking offers with restrooms at Pearce Ferry. the greatest opportunity for bird Backcountry Roads and wildlife observation. Stay on Grab extra water, a picnic lunch, Temple Bar Loop Trail the roads to protect the soil and a spare tire and a camera and go An easy walk from the ranger also it will make it easier to spot a discover the backcountry around station parking lot takes you on rattlesnake. east Lake Mead. Discover Gregg's an interpretive trail with 12 Hideout, Burro Spring, Hualapai stops. Be sure to pick up the guide Bay and Salt Spring. Please only and learn about the land, plants, drive on approved backcountry animals and history of the area. -
List of Travel Managment Plans by Travel Management Area
Attachment 1: List of Travel Management Plans By Travel Management Area Travel Management Planned Completion # Area(s) District Field Office Year NEPA 1 Littlefield Arizona Strip Arizona Strip 2017 EA 2 St. George Basin Arizona Strip Arizona Strip 2017 EA Colorado City 3 Mainstreet Arizona Strip Arizona Strip 2018 EA Uinkaret Yellowstone Mesa Grama Canyon Kanab Plateau 4 White Sage Arizona Strip Arizona Strip 2019 EA Buckskin House Rock 5 Imperial Hills Colorado River Yuma 2017 EA 6 Lower Colorado River Colorado River Yuma 2018 EA 7 Gila River Valley Colorado River Yuma 2019 EA Yuma East 8 White Hills Colorado River Kingman 2018 EIS Black Mountains Cerbat Mountains Music Mountains Crozier Hualapai Mountains Goodwin Mesa Bagdad Poachie Mountains 9 Cactus Plain Colorado River Lake Havasu 2018 EA Bouse 10 Alamo Colorado River Lake Havasu 2019 EA Wenden 11 Gila Gila Safford 2017 EA San Simon 12 Gila Box Riparian NCA Gila Safford 1998/2017 EIS 13 Dos Cabezas Gila Safford 2018 EA Aravaipa South 14 Picacho Gila Tucson 2018 EA Middle Gila South Lower San Pedro/Galiuro 15 San Pedro Riparian NCA Gila Tucson 2018 EIS 16 Sulphur Springs Gila Tucson 2019 EA Upper San Pedro Santa Rita Altar Upper Cienega Travel Management Planned Completion # Area(s) District Field Office Year NEPA Lower 17 Buckeye Hllls West/East Phoenix Sonoran 2017 EA 18 Upper Agua Fria River Basin Phoenix Hassayampa 2017 EA Bumble Bee (aka Black Canyon Corridor) 19 Aguila Phoenix Hassayampa 2018 EA Hassayampa River Basin Castle Hot Springs 20 Harquahala Mountains Phoenix Hassayampa 2019 EA Harquahala Plain 21 Gila Bend Mountains- Phoenix Lower 2019 EA Sentinel Sonoran Saddle Mountain Ajo . -
Geologic Map of the Northern White Hills, Mohave County, Arizona
Geologic Map of the Northern White Hills, Mohave County, Arizona By Keith A. Howard, Susan S. Priest, Scott C. Lundstrom, and Debra L. Block Miniature hoodoos formed where a young lag deposit of rounded pebbles and cobbles (2 to 15 cm across), reworked from the Bullhead Alluvium, overlies highly erodible gypsiferous mudstone of the Muddy Creek Formation(?) in northern Detrital Valley, Arizona. Roundstone pebble concentrations reworked downslope can sometimes mimic in-place ancestral Colorado River gravels. Pamphlet to accompany Scientific Investigations Map 3372 2017 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. Geological Survey William H. Werkheiser, Acting Director U.S. Geological Survey, Reston, Virginia: 2017 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov/ or call 1–888–ASK–USGS (1–888–275–8747). For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/. To order USGS information products, visit http://store.usgs.gov/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Howard, K.A., Priest, S.S., Lundstrom, S.C., and Block, D.L., 2017, Geologic map of the northern White Hills, Mohave County, Arizona: U.S. -
(BLM-AZIM-99-012) for the White Hills Evaluation Area, Mohave County, AZ
DESERT TORTOISE COUNCIL 4654 East Avenue S #257B Palmdale, California 93552 www.deserttortoise.org [email protected] Via email only 28 February 2020 Mike Blanton, Rangeland Management Specialist Bureau of Land Management, Kingman Field Office 2755 Mission Boulevard Kingman, Arizona 86401 https://go.usa.gov/xdgb2 RE: Evaluation of Standards for Rangeland Health (BLM-AZIM-99-012) for the White Hills Evaluation Area, Mohave County, AZ Dear Mr. Blanton, The Desert Tortoise Council (Council) is a non-profit organization comprised of hundreds of professionals and laypersons who share a common concern for wild desert tortoises and a commitment to advancing the public’s understanding of desert tortoise species. Established in 1975 to promote conservation of tortoises in the deserts of the southwestern United States and Mexico, the Council routinely provides information and other forms of assistance to individuals, organizations, and management and regulatory agencies on matters potentially affecting desert tortoises within their geographic ranges. We appreciate this opportunity to provide comments on the above-referenced project. Given the location of the White Hills Evaluation Area in habitats occupied by Agassiz’s desert tortoise (Gopherus agassizii) (synonymous with “Mojave desert tortoise”) and Sonoran desert tortoise (Gopherus morafkai) (synonymous with “Morafka’s desert tortoise”), our comments pertain to enhancing protection of these species during grazing activities authorized by the Bureau of Land Management (BLM). Proposed Action: -
Geologic Map of the White Hills West 7 ½' Quadrangle, Mohave County
Arizona Geological Survey DGM-97 (White Hills West) 114°30' 114°27'30" 114°25' 114°22'30" 18 18 18 18 18 18 18 19 19 19 19 19 19 Description of Map Units 0 3000 4000 5000 6000 7000 8000 9000 0000 1000 2000 3000 4000 5000 0 0 0 0 0 2 2 ' 6 6 5 9 9 3 3 4 GEOLOGIC MAP OF THE ° 5 3 Qi2 Other units Qya Qi Qi WHITE HILLS WEST 7 ½' 2 2 Qya Qya Qys Qi2 Qy2r Qya Qi2 ' Qi3 Qiy 5 Disturbed ground (Holocene) - Heavily disturbed ground due to mining, extensive excavation, 4 Qi3 Qi3 ° d Qy3 Qi3 5 construction of earth dams, and highways. Qiy Qi2 3 QUADRANGLE, Qi2 Qi3 Qiy Qi2 Qya Qi2 Qya Qya Qi3 Qys Qy3 Qi Quaternary talus and colluvium (Holocene) - Unconsolidated to weakly consolidated very poorly sorted Qi2 3 Qtc Qi3 Qya MOHAVE COUNTY, ARIZONA Qi2 Qya Qi2 Qi3 angular rock debris deposited on and at the base of bedrock slopes and mantling highly eroded Qi Qya Qi3 0 Qya 2 0 bedrock hills. 0 Qi3 Qy3r Qi2 Qy 0 0 Qya 3 0 1 1 6 Qy2r Qi2 6 9 9 3 Qi2 3 Qi2 Qi3 Arizona Geological Survey Digital Geologic Map DGM-97, version 1.0 Qi2 Qi2 Qya Qya Qi3 Qiy Holocene debris flow deposits (Holocene) - Snouts, levees, scoured debris flow channels, and debris Qi3 Qy3 Qi Qyd 2 flow-deposited fans. Qyd deposits are located on or at the base of steep bedrock slopes along the Qi4 Qiy Qi2 Xgn Scale 1:24,000 White Hills and along some channels within and near the mountain front.