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1 Nevada Areas of Heavy Use December 14, 2013 Trish Swain
Nevada Areas of Heavy Use December 14, 2013 Trish Swain, Co-Ordinator TrailSafe Nevada 1285 Baring Blvd. Sparks, NV 89434 [email protected] Nev. Dept. of Cons. & Natural Resources | NV.gov | Governor Brian Sandoval | Nev. Maps NEVADA STATE PARKS http://parks.nv.gov/parks/parks-by-name/ Beaver Dam State Park Berlin-Ichthyosaur State Park Big Bend of the Colorado State Recreation Area Cathedral Gorge State Park Cave Lake State Park Dayton State Park Echo Canyon State Park Elgin Schoolhouse State Historic Site Fort Churchill State Historic Park Kershaw-Ryan State Park Lahontan State Recreation Area Lake Tahoe Nevada State Park Sand Harbor Spooner Backcountry Cave Rock Mormon Station State Historic Park Old Las Vegas Mormon Fort State Historic Park Rye Patch State Recreation Area South Fork State Recreation Area Spring Mountain Ranch State Park Spring Valley State Park Valley of Fire State Park Ward Charcoal Ovens State Historic Park Washoe Lake State Park Wild Horse State Recreation Area A SOURCE OF INFORMATION http://www.nvtrailmaps.com/ Great Basin Institute 16750 Mt. Rose Hwy. Reno, NV 89511 Phone: 775.674.5475 Fax: 775.674.5499 NEVADA TRAILS Top Searched Trails: Jumbo Grade Logandale Trails Hunter Lake Trail Whites Canyon route Prison Hill 1 TOURISM AND TRAVEL GUIDES – ALL ONLINE http://travelnevada.com/travel-guides/ For instance: Rides, Scenic Byways, Indian Territory, skiing, museums, Highway 50, Silver Trails, Lake Tahoe, Carson Valley, Eastern Nevada, Southern Nevada, Southeast95 Adventure, I 80 and I50 NEVADA SCENIC BYWAYS Lake -
Description and Correlation of Geologic Units, Cross
Plate 2 UTAH GEOLOGICAL SURVEY Utah Geological Survey Bulletin 135 a division of Hydrogeologic Studies and Groundwater Monitoring in Snake Valley and Utah Department of Natural Resources Adjacent Hydrographic Areas, West-Central Utah and East-Central Nevada DESCRIPTION OF GEOLOGIC UNITS SOURCES USED FOR MAP COMPILATION UNIT CORRELATION AND UNIT CORRELATION HYDROGEOLOGIC Alluvial deposits – Sand, silt, clay and gravel; variable thickness; Holocene. Qal MDs Lower Mississippian and Upper Devonian sedimentary rocks, undivided – Best, M.G., Toth, M.I., Kowallis, B.J., Willis, J.B., and Best, V.C., 1989, GEOLOGIC UNITS UNITS Shale; consists primarily of the Pilot Shale; thickness about 850 feet in Geologic map of the Northern White Rock Mountains-Hamlin Valley area, Confining Playa deposits – Silt, clay, and evaporites; deposited along the floor of active Utah, 300–400 feet in Nevada. Aquifers Qp Beaver County, Utah, and Lincoln County, Nevada: U.S. Geological Survey Units playa systems; variable thickness; Pleistocene through Holocene. Map I-1881, 1 pl., scale 1:50,000. D Devonian sedimentary rocks, undivided – Limestone, dolomite, shale, and Holocene Qal Qsm Qp Qea Qafy Spring and wetland related deposits – Clay, silt, and sand; variable thickness; sandstone; includes the Guilmette Formation, Simonson and Sevy Fritz, W.H., 1968, Geologic map and sections of the southern Cherry Creek and Qsm Quaternary Holocene. Dolomite, and portions of the Pilot Shale in Utah; thickness about 4400– northern Egan Ranges, White Pine County, Nevada: Nevada Bureau of QTcs 4700 feet in Utah, 2100–4350 feet in Nevada. Mines Map 35, scale 1:62,500. Pleistocene Qls Qlm Qlg Qgt Qafo QTs QTfs Qea Eolian deposits – Sand and silt; deposited along valley floor margins, includes Hintze, L.H., 1963, Geologic map of Utah southwest quarter, Utah Sate Land active and vegetated dunes; variable thickness; Pleistocene through S Silurian sedimentary rocks, undivided – Dolomite; consists primarily of the Board, scale 1:250,000. -
Friends of Nevada Wilderness 2007 Stewardship Accomplishments
Friends of Nevada Wilderness 2007 Stewardship Accomplishments The Friends of Nevada Wilderness Stewardship Program 249 volunteers completed 33 projects has two components – wilderness restoration and across Nevada to make 2007 a very monitoring, and wilderness education. Friends successful year for wilderness organizes volunteer restoration and monitoring projects stewardship. in coordination with our federal land management partners to help our wildlands heal from negative impacts such as damage caused by off-road vehicles, proliferation of invasive weeds, and lack of proper trail maintenance. Friends also helps our managing agencies with other data-collection needs such as recreational use and associated impacts. Our stewardship projects always include an educational component for our volunteers on the benefits of, and need to protect, wilderness in Nevada, along with updates to volunteers on current legislative activity concerning potential wilderness areas Volunteer crew © Photo by Brian Beffort and ways they can get involved. Wilderness Stewardship Program 2007 Accomplishments: Total Number of Restoration and Monitoring Projects: 33 Total Number of Volunteers: 249 Total Volunteer Hours Benefiting Wilderness: 6,048 Total Dollar Value In-Kind Labor: $85,193 Total Outreach Events/Educational Presentations: 21 Restoration & Monitoring Projects: Date: January 3, 2007 Project: OHV/snowmobile monitoring Location: Mt. Rose Wilderness and potential wilderness additions Agency and Other Partners: U.S. Forest Service and Snowlands Network Number of Volunteers: 3 Volunteer Hours: 9 In-Kind Labor: $135.00 Project Description: Friends of Nevada Wilderness volunteers snowshoed along the Mt. Rose Wilderness boundary and monitored illegal snowmobile intrusions into the wilderness and adjacent non-motorized roadless area through use of GPS and photographs, and reported findings to Forest Service. -
The Origin and Evolution of the Southern Snake Range Decollement, East Central Nevada Allen J
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Dayton University of Dayton eCommons Geology Faculty Publications Department of Geology 2-1993 The Origin and Evolution of the Southern Snake Range Decollement, East Central Nevada Allen J. McGrew University of Dayton, [email protected] Follow this and additional works at: https://ecommons.udayton.edu/geo_fac_pub Part of the Geology Commons, Geomorphology Commons, Geophysics and Seismology Commons, Glaciology Commons, Hydrology Commons, Other Environmental Sciences Commons, Paleontology Commons, Sedimentology Commons, Soil Science Commons, Stratigraphy Commons, and the Tectonics and Structure Commons eCommons Citation McGrew, Allen J., "The Origin and Evolution of the Southern Snake Range Decollement, East Central Nevada" (1993). Geology Faculty Publications. 29. https://ecommons.udayton.edu/geo_fac_pub/29 This Article is brought to you for free and open access by the Department of Geology at eCommons. It has been accepted for inclusion in Geology Faculty Publications by an authorized administrator of eCommons. For more information, please contact [email protected], [email protected]. TECTONICS, VOL. 12, NO. 1, PAGES 21-34, FEBRUARY 1993 THE ORIGIN AND EVOLUTION OF INTRODUCTION THE SOUTHERN SNAKE RANGE The origin,kinematic significance and geometrical evolu- DECOLLEMENT, EAST CENTRAL tion of shallowlyinclined normal fault systemsare NEVADA fundamentalissues in extensionaltectonics. Regionally extensivefaults that juxtapose nonmetamorphic sedimentary Allen J. McGrew1 rocksin theirhanging walls againstplastically deformed Departmentof Geology,Stanford University, Stanford, crystallinerocks in their footwallscommand special California attentionbecause they offer rare opportunitiesto characterize kinematiclinkages between contrasting structural levels. Thesefaults, commonly known as detachmentfaults, are the Abstract.Regional and local stratigraphic, metamorphic, subjectsof muchcontroversy. -
Appendix F3.14 Special Designations
Appendix F3.14 Special Designations Clark, Lincoln, and White Pine Counties Groundwater Development Project Draft Environmental Impact Statement 228 ALT 93 93 Elko County White Pine County 278 Tooele County 2 Callao 489 Juab County Blue Mass Scenic Area 893 Gandy Salt Marsh Juab County 892 93 Millard County Eureka Opt. 1 McGill Delta Gandy Mountain Caves 50 486 Swamp Cedar Ely Rose Guano Bat Cave Baker Eureka Honeymoon Archaeological Site County Hill / City of Rocks Eskdale 6 White Pine County 487 159 Baker Snake Creek Nye County Shoshone Ponds Garrison Indian Burial Cave Fossil Mountain Opt. 2 894 Wah Baking Powder Flat Wah 318 Mountains 15 Sev Millard County Coun 6 Beaver County 21 White River Valley 93 Beaver County Iron County Opt. 3 Nye County Highland Range Lincoln County 375 Pioche Condor Canyon Panaca Garfield County Pahroc Rock Art Schlesser Mount Irish Pincushion 56 Iron County 318 Caliente 120 Hiko Washington County Opt. 4 317 93 Alamo Shooting Upper Beaver Kane Gallery Lower Meadow Dam Wash Valley Wash County Lower Meadow 89 Valley Mormon Wash 15 Mesa - Ely Nevada Utah Kane Springs Mormon Mesa - Ely Arizona 389 Lincoln County Mesquite Beaver Dam Slope Mormon Mesa Clark County 15 168 Virgin River Mormon Mesa/Arrow Canyon Virgin Mountains Project Components Gold Buried Storage Reservoir and Indian Coyote Arrow Canyon Springs Butte, Water Treatment Facility Springs 95 Part A Construction Support Area Pressure Reducing Station Primary Electrical Substation Hidden Secondary Electrical Substation Valley Pumping Station and Primary -
DIVISION C—OTHER PROVISIONS TITLE III—WHITE PINE COUNTY CON- SERVATION, RECREATION, and DE- VELOPMENT Subtitle A—Land Disp
G:\COMP\109\WHITE PINE COUNTY CONSERVATION, RECREATION, A....XML White Pine County Conservation, Recreation, and Development Act of 2006 [Title III of division C of Public Law 109–432] [As Amended Through P.L. 116–9, Enacted March 12, 2019] øCurrency: This publication is a compilation of the text of Public Law 109–432. It was last amended by the public law listed in the As Amended Through note above and below at the bottom of each page of the pdf version and reflects current law through the date of the enactment of the public law listed at https:// www.govinfo.gov/app/collection/comps/¿ øNote: While this publication does not represent an official version of any Federal statute, substantial efforts have been made to ensure the accuracy of its contents. The official version of Federal law is found in the United States Statutes at Large and in the United States Code. The legal effect to be given to the Statutes at Large and the United States Code is established by statute (1 U.S.C. 112, 204).¿ AN ACT To amend the Internal Revenue Code of 1986 to extend expiring provisions, and for other purposes. Be it enacted by the Senate and House of Representatives of the United States of America in Congress assembled, * * * * * * * DIVISION C—OTHER PROVISIONS * * * * * * * TITLE III—WHITE PINE COUNTY CON- SERVATION, RECREATION, AND DE- VELOPMENT SEC. 301. AUTHORIZATION OF APPROPRIATIONS. There are authorized to be appropriated such sums as are nec- essary to carry out this title. SEC. 302. ø16 U.S.C. 1241 note¿ SHORT TITLE This title may be cited as the ‘‘White Pine County Conserva- tion, Recreation, and Development Act of 2006’’. -
The Shrinking Sagebrush Sea
MISSION STATEMENT WildEarth Guardians protects and restores the wildlife, wild places and wild rivers of the American West. Inquiries about this report and WildEarth Guardians' work can be made directly to: Mark Salvo, WildEarth Guardians 503-757-4221, [email protected] Cartography and analyses: Kurt Menke, Bird's Eye View GIS Front cover photo: James Ownby © WildEarth Guardians All rights reserved. No part of this report may be used in any manner whatsoever without written permission from the publisher, WILDEARTH GUARDIANS, except in the case of brief quotations. Inquires should be addressed to: 312 Montezuma Avenue, Santa Fe, NM 87501 The Shrinking Sagebrush Sea Executive Summary In the sagebrush lands of the West… the natural landscape is eloquent of the interplay of forces that have created it. It is spread before us like the pages of an open book in which we can read why the land is what it is and why we should preserve its integrity. But the pages lie unread. Rachel Carson ● Silent Spring (1962) Despite its size, the Sagebrush Sea (scientifically known as “sagebrush steppe”) is one of the most endangered landscapes in North America. The Sagebrush Sea has been reduced in area by as much as 50 percent since European settlement. Livestock grazing, natural gas and oil development, agricultural conversion, roads, fences, powerlines and pipelines, off-road vehicle use, urban sprawl, mining, unnatural fire, and invasive weeds are fragmenting or degrading much of what remains. Greater sage-grouse are a sagebrush obligate species whose range has been significantly reduced with the loss of sagebrush steppe. -
AND SCHELL CREEK DIVISIONS of the James O. Klemmedson
An Inventory of Bristlecone Pine in the Snake, Mount Moriah, Ward Mountain, and Schell Creek Divisions of the Humboldt National Forest Authors Klemmedson, James O.; Beasley, R. Scott Publisher Laboratory of Tree-Ring Research, University of Arizona (Tucson, AZ) Rights Copyright © Arizona Board of Regents. The University of Arizona. Download date 02/10/2021 17:39:02 Link to Item http://hdl.handle.net/10150/302516 Report AN INVENTORY OF BRISTLECONE PINE IN THE SNAKE, MOUNT MORIAH, WARD MOUNTAIN, AND SCHELL CREEK DIVISIONS OF THE HUMBOLDT NATIONAL FOREST Prepared by James O. Klemmedson and R. Scott Beasley* Submitted to REGIONAL FORESTER, U.S. FOREST SERVICE OGDEN, UTAH in accordance with a COOPERATIVE AGREEMENT between the FOREST SERVICE and LABORATORY OF TREE-RING RESEARCH UNIVERSITY OF ARIZONA for A JOINT INVENTORY AND DENDROCHRONOLOGICAL STUDY OF BRISTLECONE PINE * Department of Watershed Management, University of Arizona INTRODUCTION Bristlecone pine, Pinus aristata Engeim., is a species which inhabits high altitudes of the mountainous southwestern United States. It occurs from the Front Range of Colorado through Utah, northern New Mexico and Arizona to the White Mountains of California along the Nevada border in the west. Bristlecone pine commonly occurs in small open groves on arid slopes, but it also grows in association with limber and ponderosa pines, white fir, Douglas - fir, and Engelmann spruce, generally above the 8000 -foot level. This tree has little economic value as a timber species, but does provide a protective and beautifying cover to the landscape. A newly -acquired interst in bristlecone pine stems from the discovery that these trees reach tremendous ages. -
Shallow-Crustal Metamorphism During Late Cretaceous Anatexis in the Sevier Hinterland Plateau: Peak Temperature Conditions from the Grant Range, Eastern Nevada, U.S.A
Shallow-crustal metamorphism during Late Cretaceous anatexis in the Sevier hinterland plateau: Peak temperature conditions from the Grant Range, eastern Nevada, U.S.A. Sean P. Long1*, Emmanuel Soignard2 1SCHOOL OF THE ENVIRONMENT, WASHINGTON STATE UNIVERSITY, PULLMAN, WASHINGTON 99164, USA 2LEROY EYRING CENTER FOR SOLID STATE SCIENCE, ARIZONA STATE UNIVERSITY, TEMPE, ARIZONA 85287, USA ABSTRACT Documenting spatio-temporal relationships between the thermal and deformation histories of orogenic systems can elucidate their evolu- tion. In the Sevier hinterland plateau in eastern Nevada, an episode of Late Cretaceous magmatism and metamorphism affected mid- and upper-crustal levels, concurrent with late-stage shortening in the Sevier thrust belt. Here, we present quantitative peak temperature data from the Grant Range, a site of localized, Late Cretaceous granitic magmatism and greenschist facies metamorphism. Twenty-two samples of Cambrian to Pennsylvanian metasedimentary and sedimentary rocks were analyzed, utilizing Raman spectroscopy on carbonaceous material, vitrinite reflectance, and Rock-Eval pyrolysis thermometry. A published reconstruction of Cenozoic extension indicates that the samples span pre-extensional depths of 2.5–9 km. Peak temperatures systematically increase with depth, from ~100 to 300 °C between 2.5 and 4.5 km, ~400 to 500 °C between 5 and 8 km, and ~550 °C at 9 km. The data define a metamorphic field gradient of ~60 °C/km, and are corroborated by quartz recrystallization microstructure and published conodont alteration indices. Metamorphism in the Grant Range is correlated with contemporary, upper-crustal metamorphism and magmatism documented farther east in Nevada, where metamorphic field gradients as high as ~50 °C/km are estimated. -
Table 7 - National Wilderness Areas by State
Table 7 - National Wilderness Areas by State * Unit is in two or more States ** Acres estimated pending final boundary determination + Special Area that is part of a proclaimed National Forest State National Wilderness Area NFS Other Total Unit Name Acreage Acreage Acreage Alabama Cheaha Wilderness Talladega National Forest 7,400 0 7,400 Dugger Mountain Wilderness** Talladega National Forest 9,048 0 9,048 Sipsey Wilderness William B. Bankhead National Forest 25,770 83 25,853 Alabama Totals 42,218 83 42,301 Alaska Chuck River Wilderness 74,876 520 75,396 Coronation Island Wilderness Tongass National Forest 19,118 0 19,118 Endicott River Wilderness Tongass National Forest 98,396 0 98,396 Karta River Wilderness Tongass National Forest 39,917 7 39,924 Kootznoowoo Wilderness Tongass National Forest 979,079 21,741 1,000,820 FS-administered, outside NFS bdy 0 654 654 Kuiu Wilderness Tongass National Forest 60,183 15 60,198 Maurille Islands Wilderness Tongass National Forest 4,814 0 4,814 Misty Fiords National Monument Wilderness Tongass National Forest 2,144,010 235 2,144,245 FS-administered, outside NFS bdy 0 15 15 Petersburg Creek-Duncan Salt Chuck Wilderness Tongass National Forest 46,758 0 46,758 Pleasant/Lemusurier/Inian Islands Wilderness Tongass National Forest 23,083 41 23,124 FS-administered, outside NFS bdy 0 15 15 Russell Fjord Wilderness Tongass National Forest 348,626 63 348,689 South Baranof Wilderness Tongass National Forest 315,833 0 315,833 South Etolin Wilderness Tongass National Forest 82,593 834 83,427 Refresh Date: 10/14/2017 -
Lunar Crater Volcanic Field (Reveille and Pancake Ranges, Basin and Range Province, Nevada, USA)
Research Paper GEOSPHERE Lunar Crater volcanic field (Reveille and Pancake Ranges, Basin and Range Province, Nevada, USA) 1 2,3 4 5 4 5 1 GEOSPHERE; v. 13, no. 2 Greg A. Valentine , Joaquín A. Cortés , Elisabeth Widom , Eugene I. Smith , Christine Rasoazanamparany , Racheal Johnsen , Jason P. Briner , Andrew G. Harp1, and Brent Turrin6 doi:10.1130/GES01428.1 1Department of Geology, 126 Cooke Hall, University at Buffalo, Buffalo, New York 14260, USA 2School of Geosciences, The Grant Institute, The Kings Buildings, James Hutton Road, University of Edinburgh, Edinburgh, EH 3FE, UK 3School of Civil Engineering and Geosciences, Newcastle University, Newcastle, NE1 7RU, UK 31 figures; 3 tables; 3 supplemental files 4Department of Geology and Environmental Earth Science, Shideler Hall, Miami University, Oxford, Ohio 45056, USA 5Department of Geoscience, 4505 S. Maryland Parkway, University of Nevada Las Vegas, Las Vegas, Nevada 89154, USA CORRESPONDENCE: gav4@ buffalo .edu 6Department of Earth and Planetary Sciences, 610 Taylor Road, Rutgers University, Piscataway, New Jersey 08854-8066, USA CITATION: Valentine, G.A., Cortés, J.A., Widom, ABSTRACT some of the erupted magmas. The LCVF exhibits clustering in the form of E., Smith, E.I., Rasoazanamparany, C., Johnsen, R., Briner, J.P., Harp, A.G., and Turrin, B., 2017, overlapping and colocated monogenetic volcanoes that were separated by Lunar Crater volcanic field (Reveille and Pancake The Lunar Crater volcanic field (LCVF) in central Nevada (USA) is domi variable amounts of time to as much as several hundred thousand years, but Ranges, Basin and Range Province, Nevada, USA): nated by monogenetic mafic volcanoes spanning the late Miocene to Pleisto without sustained crustal reservoirs between the episodes. -
Geology of the Southern Reveille Range, Nye County, Nevada
UNLV Theses, Dissertations, Professional Papers, and Capstones 5-2008 Geology of the southern Reveille Range, Nye County, Nevada Matthew Alan McKelvey University of Nevada, Las Vegas Follow this and additional works at: https://digitalscholarship.unlv.edu/thesesdissertations Part of the Geology Commons, Stratigraphy Commons, and the Volcanology Commons Repository Citation McKelvey, Matthew Alan, "Geology of the southern Reveille Range, Nye County, Nevada" (2008). UNLV Theses, Dissertations, Professional Papers, and Capstones. 1447. http://dx.doi.org/10.34917/3434676 This Thesis is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in UNLV Theses, Dissertations, Professional Papers, and Capstones by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. GEOLOGY OF THE SOUTHERN REVEILLE RANGE, NYE COUNTY, NEVADA by Matthew Alan McKelvey Bachelor of Science Austin Peay State University 2001 A thesis submitted in partial fulfillment of the requirements for the Master Degree of Science in Geoscience Department of Geoscience