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HISTORY of the TOIYABE NATIONAL FOREST a Compilation
HISTORY OF THE TOIYABE NATIONAL FOREST A Compilation Posting the Toiyabe National Forest Boundary, 1924 Table of Contents Introduction ..................................................................................................................................... 3 Chronology ..................................................................................................................................... 4 Bridgeport and Carson Ranger District Centennial .................................................................... 126 Forest Histories ........................................................................................................................... 127 Toiyabe National Reserve: March 1, 1907 to Present ............................................................ 127 Toquima National Forest: April 15, 1907 – July 2, 1908 ....................................................... 128 Monitor National Forest: April 15, 1907 – July 2, 1908 ........................................................ 128 Vegas National Forest: December 12, 1907 – July 2, 1908 .................................................... 128 Mount Charleston Forest Reserve: November 5, 1906 – July 2, 1908 ................................... 128 Moapa National Forest: July 2, 1908 – 1915 .......................................................................... 128 Nevada National Forest: February 10, 1909 – August 9, 1957 .............................................. 128 Ruby Mountain Forest Reserve: March 3, 1908 – June 19, 1916 .......................................... -
Northern Paiute and Western Shoshone Land Use in Northern Nevada: a Class I Ethnographic/Ethnohistoric Overview
U.S. DEPARTMENT OF THE INTERIOR Bureau of Land Management NEVADA NORTHERN PAIUTE AND WESTERN SHOSHONE LAND USE IN NORTHERN NEVADA: A CLASS I ETHNOGRAPHIC/ETHNOHISTORIC OVERVIEW Ginny Bengston CULTURAL RESOURCE SERIES NO. 12 2003 SWCA ENVIROHMENTAL CON..·S:.. .U LTt;NTS . iitew.a,e.El t:ti.r B'i!lt e.a:b ~f l-amd :Nf'arat:1.iern'.~nt N~:¥G~GI Sl$i~-'®'ffl'c~. P,rceP,GJ r.ei l l§y. SWGA.,,En:v,ir.e.m"me'Y-tfol I €on's.wlf.arats NORTHERN PAIUTE AND WESTERN SHOSHONE LAND USE IN NORTHERN NEVADA: A CLASS I ETHNOGRAPHIC/ETHNOHISTORIC OVERVIEW Submitted to BUREAU OF LAND MANAGEMENT Nevada State Office 1340 Financial Boulevard Reno, Nevada 89520-0008 Submitted by SWCA, INC. Environmental Consultants 5370 Kietzke Lane, Suite 205 Reno, Nevada 89511 (775) 826-1700 Prepared by Ginny Bengston SWCA Cultural Resources Report No. 02-551 December 16, 2002 TABLE OF CONTENTS List of Figures ................................................................v List of Tables .................................................................v List of Appendixes ............................................................ vi CHAPTER 1. INTRODUCTION .................................................1 CHAPTER 2. ETHNOGRAPHIC OVERVIEW .....................................4 Northern Paiute ............................................................4 Habitation Patterns .......................................................8 Subsistence .............................................................9 Burial Practices ........................................................11 -
Schedule of Proposed Action (SOPA)
Schedule of Proposed Action (SOPA) 10/01/2017 to 12/31/2017 Humboldt-Toiyabe National Forest This report contains the best available information at the time of publication. Questions may be directed to the Project Contact. Expected Project Name Project Purpose Planning Status Decision Implementation Project Contact Projects Occurring in more than one Region (excluding Nationwide) Sierra Nevada Forest Plan - Land management planning Completed Actual: 09/17/2013 03/2014 Donald Yasuda Amendment (SNFPA) 09/13/2013 916-640-1168 EIS [email protected] *UPDATED* Description: Prepare a narrowly focused analysis to comply with two orders issued by the Eastern District Court of California on November 4, 2009. Correct the 2004 SNFPA Final SEIS to address range of alternatives and analytical consistency issues. Web Link: http://www.fs.fed.us/r5/snfpa/2010seis Location: UNIT - Eldorado National Forest All Units, Lassen National Forest All Units, Modoc National Forest All Units, Sequoia National Forest All Units, Tahoe National Forest All Units, Lake Tahoe Basin Mgt Unit, Carson Ranger District, Bridgeport Ranger District, Plumas National Forest All Units, Sierra National Forest All Units, Stanislaus National Forest All Units, Inyo National Forest All Units. STATE - California, Nevada. COUNTY - Alpine, Amador, Butte, Calaveras, El Dorado, Fresno, Inyo, Kern, Lassen, Madera, Mariposa, Modoc, Mono, Nevada, Placer, Plumas, Shasta, Sierra, Siskiyou, Tulare, Tuolumne, Yuba, Douglas, Esmeralda, Mineral. LEGAL - Along the Sierra Nevada Range, from the Oregon/California -
Central Nevada
University of Nevada Reno LATE CENOZOIC GEOLOGY AND TECTONICS OF STEWART AND MONTE CRISTO VALLEYS, WEST - CENTRAL NEVADA A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science .I by Mark Philip Molinari fit ; December, 1984 ii ABSTRACT Discontinuous right-normal-slip faults comprise the N30 0W trending, 45 kilometer long Stewart - Monte Cristo fault zone (SMCFZ). Initiation of the SMCFZ postdates the 15.5 to 11.0 m.y. Esmeralda Formation. Right-normal-slip >1 meter occurred on the southern segment of the SMCFZ during the 1932 Cedar Mountain earthquake (Ms= 7.2-7.3). Geomor- phic evidence supports at least three and possibly five or six surface faulting events on the southern segment during the latest Pleistocene and Holocene. Gentle folds in the Esmeralda Formation east of and sub-parallel to the SMCFZ are coeval with and genetically related to faulting. Structural development of the SMCFZ is similar to other right-lateral wrench faults and is consistent with labora- tory wrench fault models. The SMCFZ is the youngest and southeasternmost fault of a system of major late Cenozoic, left-stepping, en echelon right-slip faults in the central Walker Lane. - .~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ iii TABLE OF CONTENTS page ABSTRACT .................. S S ii INTRODUCTION . 0 0 1 0 * I Location and Extent of Study Area . S S S S 1 Regional Tectonic and Geologic Setting. S. S a * 0 1 Purpose and Scope ...... a a * a 5 Methodology . 6 Previous Work . 8 Physiography. 10 MESOZOIC STRATIGRAPHY. 13 Sedimentary Rocks . & 13 Mina Formation . 13 Luning Formation . 13 Plutonic Rocks . -
Hydrographic Basins Information
A p p e n d i x A - B a s i n 54 Crescent Valley Page 1 of 6 Basin 54 - Crescent Valley Crescent Valley is a semi-closed basin that is bounded on the west by the Shoshone Range, on the east by the Cortez Mountains, on the south by the Toiyabe Range, and on the north by the Dry Hills. The drainage basin is about 45 miles long, 20 miles wide, and includes an area of approximately 750 square miles. Water enters the basin primarily as precipitation and is discharged primarily through evaporation and transpiration. Relatively small quantities of water enter the basin as surface flow and ground water underflow from the adjacent Carico Lake Valley at Rocky Pass, where Cooks Creek enters the southwestern end of Crescent Valley. Ground water generally flows northeasterly along the axis of the basin. The natural flow of ground water from Crescent Valley discharges into the Humboldt River between Rose Ranch and Beowawe. It is estimated that the average annual net discharge rate is approximately 700 to 750 acre-feet annually. Many of the streams which drain snowmelt of rainfall from the mountains surrounding Crescent Valley do not reach the dry lake beds on the Valley floor: instead, they branch into smaller channels that eventually run dry. Runoff from Crescent Valley does not reach Humboldt River with the exception of Coyote Creek, an intermittent stream that flows north from the Malpais to the Humboldt River and several small ephemeral streams that flow north from the Dry Hills. Surface flow in the Carico Lake Valley coalesces into Cooks Creek, which enters Crescent Valley through Rocky Pass. -
Eocene–Early Miocene Paleotopography of the Sierra Nevada–Great Basin–Nevadaplano Based on Widespread Ash-Flow Tuffs and P
Origin and Evolution of the Sierra Nevada and Walker Lane themed issue Eocene–Early Miocene paleotopography of the Sierra Nevada–Great Basin–Nevadaplano based on widespread ash-fl ow tuffs and paleovalleys Christopher D. Henry1, Nicholas H. Hinz1, James E. Faulds1, Joseph P. Colgan2, David A. John2, Elwood R. Brooks3, Elizabeth J. Cassel4, Larry J. Garside1, David A. Davis1, and Steven B. Castor1 1Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada 89557, USA 2U.S. Geological Survey, Menlo Park, California 94025, USA 3California State University, Hayward, California 94542, USA 4Department of Earth and Environment, Franklin & Marshall College, Lancaster, Pennsylvania 17604, USA ABSTRACT the great volume of erupted tuff and its erup- eruption fl owed similar distances as the mid- tion after ~3 Ma of nearly continuous, major Cenozoic tuffs at average gradients of ~2.5–8 The distribution of Cenozoic ash-fl ow tuffs pyroclastic eruptions near its caldera that m/km. Extrapolated 200–300 km (pre-exten- in the Great Basin and the Sierra Nevada of probably fi lled in nearby topography. sion) from the Pacifi c Ocean to the central eastern California (United States) demon- Distribution of the tuff of Campbell Creek Nevada caldera belt, the lower gradient strates that the region, commonly referred and other ash-fl ow tuffs and continuity of would require elevations of only 0.5 km for to as the Nevadaplano, was an erosional paleovalleys demonstrates that (1) the Basin valley fl oors and 1.5 km for interfl uves. The highland that was drained by major west- and Range–Sierra Nevada structural and great eastward, upvalley fl ow is consistent and east-trending rivers, with a north-south topographic boundary did not exist before with recent stable isotope data that indicate paleodivide through eastern Nevada. -
Position Outreach Announcement
USDA FOREST SERVICE INTERMOUNTAIN REGION, R4 HUMBOLDT-TOIYABE NATIONAL FOREST AUSTIN/TONOPAH RANGER DISTRICTS Rangeland Management Specialist December 17, 2009 About thePosition… The Humboldt-Toiyabe National Forest will soon be filling a Rangeland Management Specialist position, GS-0454-5/7/9, located in Austin, Nevada on the Austin/Tonopah Ranger Districts. The Austin/Tonopah Ranger Districts administer grazing on 47 cattle allotments and 2 sheep allotments. The Districts also manage thirteen wild horse and burro territories. This position offers a variety of opportunities for individuals to develop skills and enjoy a variety of challenging experiences. Are you Interested? Interested applicants, or those desiring further information, should contact Steven Williams, Austin/Tonopah District Ranger, at (775) 964-2671 or email at: [email protected] ; or Heather Mobley 775-964-2671 or email at [email protected] For additional Forest and District information, check out the H-T website… http://www.fs.fed.us/htnf/ The Forest … At over 6.3 million acres, the Humboldt-Toiyabe National Forest is the largest National Forest in the contiguous United States. The Forest spans the entire state of Nevada, with one million acres of land in the eastern part of California, along the Eastern Sierra Front. The Districts … The Austin/Tonopah Ranger Districts have two offices one in Austin and the other in Tonopah, Nevada. The Districts are managed as one unit under one District Ranger, with employees working out of both offices. The Austin/Tonopah Ranger Districts are responsible for the management of approximately 2.2 million acres of National Forest System Lands. -
Decision-Support Tools for Conserving Greater Sage-Grouse During Fire and Fuels Management Projects in Pinyon and Juniper Woodla
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln JFSP Research Project Reports U.S. Joint Fire Science Program 2013 Decision-support tools for conserving Greater Sage-Grouse during fire and fuels management projects in pinyon and juniper woodlands Erica Fleishman University of California - Davis Jeanne C. Chambers USDA Forest Service, [email protected] David S. Dobkin High Desert Ecological Research Institute Brett .G Dickson Conservation Science Partners Follow this and additional works at: http://digitalcommons.unl.edu/jfspresearch Part of the Forest Biology Commons, Forest Management Commons, Natural Resources and Conservation Commons, Natural Resources Management and Policy Commons, Other Environmental Sciences Commons, Other Forestry and Forest Sciences Commons, Sustainability Commons, and the Wood Science and Pulp, Paper Technology Commons Fleishman, Erica; Chambers, Jeanne C.; Dobkin, David S.; and Dickson, Brett .,G "Decision-support tools for conserving Greater Sage-Grouse during fire and fuels management projects in pinyon and juniper woodlands" (2013). JFSP Research Project Reports. 46. http://digitalcommons.unl.edu/jfspresearch/46 This Article is brought to you for free and open access by the U.S. Joint Fire Science Program at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in JFSP Research Project Reports by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. FINAL REPORT Decision-support tools for conserving Greater Sage-Grouse during fire and fuels management projects in pinyon and juniper woodlands JFSP 09-1-08-4 Erica Fleishman, University of California, Davis (principal investigator) Jeanne C. Chambers, USDA Forest Service, Rocky Mountain Research Station, Reno, Nevada (co-principal investigator) David S. -
Geologic Map of the Tonopah 1° by 2° Quadrangle, Central Nevada
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP MF-1877-A U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE TONOPAH 1° BY 2° QUADRANGLE, CENTRAL NEVADA By Donald H. Whitebread and David A. John INTRODUCTION Qb Basalt of Lunar Crater area This map is part of a folio of maps of the (Quaternary) Lava flows and local Tonopah 1° by 2° quadrangle, Nevada, prepared cinders and dikes under the Conterminous United States Mineral Tba Basalt and andesite flows Assessment Program. (Tertiary) As mapped, probably includes some Quaternary lava flows in DESCRIPTION OF MAP UNITS Pancake Range. Includes trachyandesite of Red Mountain and trachyandesite of Thunder Mountain in San Antonio SURHCIAL DEPOSITS Mountains Qa Alluvial, lacustrine, and eolian Tr4 Rhyolitic rocks (Tertiary) Rhyolitic deposits (Quaternary) A s to dacitic flows, dikes, and small mapped, locally includes Tertiary gravel intrusive bodies. Includes Brougher QTIs Landslide deposits (Quaternary and Rhyolite of Bonham and Garside (1979) Tertiary) and Oddie Rhyolite 734 Andesitic rocks (Tertiary) Andesitic SEDIMENTARY ROCKS AND to latitic flows, volcanic breccia, and UNCONSOLIDATED DEPOSITS dikes Includes Gilbert Andesite, Mizpah Trachyte, and volcanics of Lime Ts4 Sedimentary rocks and bedded tuff Mountain of Bonham and Garside (Tertiary) Tuffaceous siltstone and (1979) sandstone, bedded tuff, and diatomite. Tas Andesitic rocks (Tertiary) Andesitic Includes Esmeralda and Siebert to latitic flows, flow breccias, sills, Formations. K-Ar ages about 11-13 Ma dikes, and plugs (Evernden and James, 1964; Evernden Tfs Rhyolitic rocks (Tertiary) Rhyolitic and others, 1964) for Esmeralda to dacitic flows, dikes, sills, and Formation and 13-17 Ma (Bonham and irregular small intrusive bodies Garside, 1979) for Siebert Formation Ta2 Andesitic rocks (Tertiary) Andesitic Ts3 Sedimentary rocks and bedded tuff to latitic flows, flow breccias, dikes, (Tertiary) Sandstone and siltstone, sills, and minor intrusive bodies commonly tuffaceous. -
F I N a L Mineral Assessment Report
BLM F I N A L MINERAL ASSESSMENT REPORT Battle Mountain District Office - Nevada J A N U A R Y 2 0 1 2 This page intentionally left blank Bureau of Land Management Mineral Assessment Report SUMMARY The Bureau of Land Management (BLM) Battle Mountain District Office (BMDO) is in the process of revising the district’s Resource Management Plan (RMP). As part of the RMP revision process, the BLM is required to prepare a Mineral Assessment Report providing information regarding mineral occurrences and potential within the BMDO Planning Area (planning area). This report provides an intermediate level of detail for mineral assessment as prescribed in BLM Manual 3060 (BLM 1994). Information presented in this report will be summarized and incorporated into an Environmental Impact Statement (EIS) for the proposed RMP and into the final RMP. The geologic history of central and southern Nevada and the planning area is very complex and includes two major cycles of sedimentation (western and eastern facies sources), episodic thrust faulting, mountain building, and associated intrusive and igneous activity. More recent geologic history includes a period of crustal extension that was accompanied by bimodal (rhyolite-basalt) volcanism, large volume caldera volcanism, and basin and range block-faulting resulting in high-levels of shallow crustal heat flow. The regional and local geologic setting has been instrumental in the location of and potential for numerous economic metallic mineral deposits in the planning area, as well as development of economic geothermal resources. MINING AND MINERAL ACTIVITY IN NEVADA Mineral exploration, particularly for gold, is an ongoing enterprise in Nevada by both operators of existing mines and by other exploration companies. -
Paleozoic Tectonic Domains of Nevada: an Interpretive Discussion to Accompany the Geologic Map of Nevada
Paleozoic tectonic domains of Nevada: An interpretive discussion to accompany the geologic map of Nevada A. Elizabeth Jones Crafford GeoLogic, 9501 Nettleton Drive, Anchorage, Alaska 99507, USA ABSTRACT contain rocks unlike those from the adjacent tectonic domains is to help characterize and dis- margin or other terranes and suggest they are tinguish groups of rocks by the distinct tectonic The Paleozoic geologic history of Nevada far traveled. A change in the plate boundary histories that have (or have not) impacted them. can be viewed in terms of tectonic domains confi guration in the Middle Pennsylvanian Traditional interpretations of Paleozoic tec- derived from the newly interpreted digi- led to the development of a new margin that tonic events in Nevada have primarily relied tal geologic map of Nevada. These domains refl ected the effects of a new plate boundary on pre-plate tectonic or early plate tectonic reveal that Paleozoic tectonic events were farther to the west. Accretion to the margin ideas of displacement of the Earth’s crust that shaped by complex interactions between the of upper Paleozoic oceanic terranes at the do not necessarily address the complexity of continental margin in Nevada and accreted close of the Paleozoic redefi ned the margin structural and stratigraphic evidence that has terranes outboard of the margin. once again as it changed from a transpres- been observed since they were fi rst proposed Ten domains are described. They include sive accretion regime to a true backarc plate (Brueckner and Snyder, 1985; Burchfi el and lower Paleozoic domains based on paleogeo- tectonic setting in the Mesozoic. -
Potential Formation of a New Fire District
I Fire Department Funding and Governance Analysis Tooele County January 2021 Fire Department Funding and Governance Analysis Tooele County TABLE OF CONTENTS ACKNOWLEDGEMENTS .................................................................................................................. 3 SECTION I: EXECUTIVE SUMMARY ................................................................................................ 4 SECTION II: METHODOLOGY .......................................................................................................... 6 Kick-Off Meeting ................................................................................................................................... 6 Stakeholder Interviews .......................................................................................................................... 6 Data Collection ...................................................................................................................................... 6 Background Research .......................................................................................................................... 7 SECTION III: BACKGROUND ........................................................................................................... 8 Tooele County Geography and Population ........................................................................................... 8 Study Objectives ..................................................................................................................................