Lincoln County Public Lands Policy Plan
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Conaway Ranch in Rainbow Canyon
The Conaway Ranch in Rainbow Canyon Rainbow Canyon Rainbow Canyon is named for its spectacular rainbow colored rock walls. Meadow Valley Wash, a year-round spring fed stream, waters thousands of trees along its banks as it flows through the canyon. Ancient Man inhabited the canyon and artifacts recovered from caves carbon date their occupation to 5,000 years ago. In the 1860s, settlers established ranches in the canyon to supply beef, fruit and vegetables to the surrounding mining towns. The Conaway Ranch The history of the Property dates back to the 1860s when the Conaway Ranch was one of the first cattle ranches in the region. It was a favorite place of writer Zane Grey, who enjoyed staying at the ranch while he was writing about the wild west. Howard Hughes, Summa Corporation, owned the Conaway Ranch in the 1970s. He intended to develop a destination resort on the ranch. In the 1980s a developer drilled water wells, built a community sanitation system and leach field, and built a 9-hole golf course on the ranch. The golf course is grown over with natural cover, but pressure pumps and some underground infrastructure remain. A domestic well and the community leach field served several homes and golf club facilities during the years that the golf course operated, and currently serves two existing homes on the golf course. This information has been secured from sources we believe to be reliable, but we make no representations or warranties, expressed or implied, as to the accuracy of the information. Buyer must verify the information and bears all risk for any inaccuracies. -
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. -
VGP) Version 2/5/2009
Vessel General Permit (VGP) Version 2/5/2009 United States Environmental Protection Agency (EPA) National Pollutant Discharge Elimination System (NPDES) VESSEL GENERAL PERMIT FOR DISCHARGES INCIDENTAL TO THE NORMAL OPERATION OF VESSELS (VGP) AUTHORIZATION TO DISCHARGE UNDER THE NATIONAL POLLUTANT DISCHARGE ELIMINATION SYSTEM In compliance with the provisions of the Clean Water Act (CWA), as amended (33 U.S.C. 1251 et seq.), any owner or operator of a vessel being operated in a capacity as a means of transportation who: • Is eligible for permit coverage under Part 1.2; • If required by Part 1.5.1, submits a complete and accurate Notice of Intent (NOI) is authorized to discharge in accordance with the requirements of this permit. General effluent limits for all eligible vessels are given in Part 2. Further vessel class or type specific requirements are given in Part 5 for select vessels and apply in addition to any general effluent limits in Part 2. Specific requirements that apply in individual States and Indian Country Lands are found in Part 6. Definitions of permit-specific terms used in this permit are provided in Appendix A. This permit becomes effective on December 19, 2008 for all jurisdictions except Alaska and Hawaii. This permit and the authorization to discharge expire at midnight, December 19, 2013 i Vessel General Permit (VGP) Version 2/5/2009 Signed and issued this 18th day of December, 2008 William K. Honker, Acting Director Robert W. Varney, Water Quality Protection Division, EPA Region Regional Administrator, EPA Region 1 6 Signed and issued this 18th day of December, 2008 Signed and issued this 18th day of December, Barbara A. -
Protecting the Places We Love: How the Land And
Protecting the Places We Love How the Land and Water Conservation Fund Supports Outdoor Recreation in Nevada Protecting the Places We Love How the Land and Water Conservation Fund Supports Outdoor Recreation in Nevada Written by: James Horrox, Frontier Group Levi Kamolnick, Environment Nevada Research & Policy Center January 2020 Acknowledgments The authors thank Mauricia Baca, Executive Director, Get Outdoors Nevada, and Andy Maggi, Executive Director, Nevada Conservation League Education Fund, for their review of drafts of this document, as well as their insights and suggestions. The authors also thank Amy Lindholm, Robert Mergell, Janice Keillor, Shevawn Von Tobel, Kurt Kuznicki, Caleb Abbott, Colleen Wallace-Barnum, Sophia Kirschenman, Rich Mueller, Sally Grate and Olivia Holmes for the invaluable assistance they have provided. Thanks also to Tony Dutzik, Susan Rakov, Gideon Weissman, Elizabeth Ridlington and Adrian Pforzheimer of Frontier Group for editorial support. The authors bear responsibility for any factual errors. The recommendations are those of Environment Nevada Research and Policy Center. The views expressed in this report are those of the authors and do not necessarily reflect the views of our funders or those who provided review. 2020 Environment Nevada Research and Policy Center. Some Rights Reserved. This work is licensed under a Creative Commons Attribution Non-Commercial No Derivatives 3.0 U.S. License. To view the terms of this license, visit creativecommons. org/licenses/by-nc-nd/3.0/us. Environment Nevada Research & Policy Center is a project of Environment America Research & Policy Center, a 501(c)(3) organization. We are dedicated to protecting our air, water and open spaces. -
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. -
1 Chairman Wallace Called the Meeting to Order at 10 A.M. Roll Call
DRAFT March 24 and 25, 2017 Minutes Nevada Board of Wildlife Commissioners’ Meeting Agenda Clark County Shooting Complex 11357 N. Decatur Blvd. Las Vegas, NV 89131 #5 Public comment will be taken on every action item and regulation workshop item after discussion but before action on each item, and at the end of each day’s meeting. Public comment is limited to three minutes per person. The chairman, in his discretion, may allow persons representing groups to speak for six minutes. Persons may not allocate unused time to other speakers. Persons are invited to submit written comments on items or attend and make comment during the meeting and are asked to complete a speaker card and present it to the Recording Secretary. To ensure the public has notice of all matters the Commission will consider, Commissioners may choose not to respond to public comments in order to avoid the appearance of deliberation on topics not listed for action on the agenda. Forum restrictions and orderly business: The viewpoint of a speaker will not be restricted, but reasonable restrictions may be imposed upon the time, place and manner of speech. Irrelevant and unduly repetitious statements and personal attacks that antagonize or incite others are examples of public comment that may be reasonably limited. Please provide the Board of Wildlife Commissioners (“Commission”) with the complete electronic or written copies of testimony and visual presentations to include as exhibits with the minutes. Minutes of the meeting will be produced in summary format. Members Nevada -
Mineral Resources of the Mormon Mountains Wilderness Study Area, Lincoln County, Nevada
Mineral Resources of the Mormon Mountains Wilderness Study Area, Lincoln County, Nevada U.S. GEOLOGICAL SURVEY BULLETIN 1729-B or ^JSSr Chapter B Mineral Resources of the Mormon Mountains Wilderness Study Area, Lincoln County, Nevada By DANIEL R. SHAWE, H. RICHARD BLANK, JR., BRIAN P. WERNICKE, GARY J. AXEN, HARLAN N. BARTON, and GORDON W. DAY U.S. Geological Survey RICHARD L RAINS U.S. Bureau of Mines U.S. GEOLOGICAL SURVEY BULLETIN 1729 MINERAL RESOURCES OF WILDERNESS STUDY AREAS- SOUTHEASTERN NEVADA DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE: 1988 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Main entry under title: Mineral resources of the Mormon Mountains Wilderness Study Area, Lincoln County, Nevada. (Mineral resources of wilderness study areas southeastern Nevada ; ch. B) (U.S. Geological Survey bulletin ; 1729-B) Bibliography: p. Supt. of Docs, no.: I 19.3:1729-8. 1. Mines and mineral resources Nevada Mormon Mountains Wilderness. 2. Mormon Mountains Wilderness (Nev.). I. Shawe, Daniel R., 1925- . II. Series. III. Series: U.S. Geological Survey bulletin ; 1729-B. QE75.B9 no. 1729-B 557.3s 87-600429 [TN24.N3] [553'.09793'14] STUDIES RELATED TO WILDERNESS Bureau of Land Management Wilderness Study Areas The Federal Land Policy and Management Act (Public Law 94-579, October 21, 1976) requires the U.S. Geological Survey and the U.S. Bureau of Mines to conduct mineral surveys on certain areas to determine the mineral values, if any, that may be present. -
Lincoln County Conservation, Recreation and Development Act Of
H. R. 4593 One Hundred Eighth Congress of the United States of America AT THE SECOND SESSION Begun and held at the City of Washington on Tuesday, the twentieth day of January, two thousand and four An Act To establish wilderness areas, promote conservation, improve public land, and pro- vide for the high quality development in Lincoln County, Nevada, and for other purposes. Be it enacted by the Senate and House of Representatives of the United States of America in Congress assembled, SECTION 1. AUTHORIZATION OF APPROPRIATIONS. There are authorized to be appropriated such sums as are necessary to carry out this Act. SEC. 2. SHORT TITLE; TABLE OF CONTENTS. (a) SHORT TITLE.—This Act may be cited as the ‘‘Lincoln County Conservation, Recreation, and Development Act of 2004’’. (b) TABLE OF CONTENTS.—The table of contents for this Act is as follows: Sec. 1. Authorization of appropriations. Sec. 2. Short title; table of contents. TITLE I—LAND DISPOSAL Sec. 101. Definitions. Sec. 102. Conveyance of Lincoln County land. Sec. 103. Disposition of proceeds. TITLE II—WILDERNESS AREAS Sec. 201. Findings. Sec. 202. Definitions. Sec. 203. Additions to National Wilderness Preservation System. Sec. 204. Administration. Sec. 205. Adjacent management. Sec. 206. Military overflights. Sec. 207. Native American cultural and religious uses. Sec. 208. Release of wilderness study areas. Sec. 209. Wildlife management. Sec. 210. Wildfire management. Sec. 211. Climatological data collection. TITLE III—UTILITY CORRIDORS Sec. 301. Utility corridor and rights-of-way. Sec. 302. Relocation of right-of-way and utility corridors located in Clark and Lin- coln counties in the State of Nevada. -
Pioche Walking and Driving Tour
Pioche $50,000 State Parks Dougherty’s Walking and Fishing of Lincoln Fine Jewelry Driving Tour Tournament County Opens Page 4 Page 7 Page 8 Page 15 Spring, 2010 PIOCHE THEN AND NOW By Jim Kelly Lincoln County and specifically, Pioche, COURT HOUSE” opens with how and why it has the dubious honor of having one of the cost so much. The two main reasons you least known, yet costliest, monuments to could’ve read in this morning’s newspaper are greed, graft, and corruption, the Wild West has CORRUPT POLITICIANS and GREEDY ever seen. BANKS. It was originally contracted to be I’m a newcomer to the quiet little town of built at cost of $26,400. But due to design Looking down on Pioche from Treasure Hill. Pioche; I’ve only lived here permanently for changes, over runs, and many pockets being about 10 years now. I was born in Las Vegas, lined, it came to $88,000. So they decided to and my father was born in Las Vegas. My sell bonds to raise the required monies, and, as paternal grandfather emigrated from Ireland to you can imagine, very little, if any, went Las Vegas in 1910 or 1911. Shortly after his toward repaying this debt. By the time the arrival he met, courted and married Martha bonds were at three times the original value in Lynch, who was born here in Pioche, as was 1907, the cost had soared to whopping her father John H. Lynch. Martha’s grandfa- $435,000. It took another 30 years to pay off ther was born in Ely, Nevada and came to the note, with the usual interest rates of over Pioche in the 1860’s during the great silver 25%. -
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.