2018 Amendment to the 2002 Gore Mountain Unit Management Plan and Final Generic Environmental Impact Statement
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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 -
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 .......................................... -
Mountain City, Ruby Mountains, and Jarbidge Combined Travel
Mountain City, Ruby Mountains and Jarbidge Ranger Districts Combined Travel Management Project Environmental Impact Statement Chapter 3. Affected Environment and Environmental Consequences 3.1. Introduction This chapter summarizes the physical, biological, social, and economic environments that are affected by the alternatives and the effects on that environment that would result from implementation of any of the alternatives. This chapter also presents the scientif ic and analyt ical basis for comparison of the alternatives presented in chapter 2. 3.1.1. Analysis Process Most of the data used in the following analysis are from the Humboldt-Toiyabe National Forest corporate GIS layers. There is a certain amount of error in the location and alignments included in this GIS data. For example, the road layer overlying the stream layer may show more stream crossings than actually exist on the ground because of the different sources from which the different layers were obtained. Some perennial streams may show up on the map as being intermittent. This may also create some inaccuracies as to the exact location and extent of riparian zones. The Forest is constantly working to improve map accuracies and the corporate GIS layers. For the purposes of this analysis, the best data that is available was used. The data in the tables below and in the project record depict with a reasonable amount of accuracy what would be occurring on the ground for each alternative, within the limitations described above. The changes between alternatives remain relative to each other. 3.1.2. Cumulative Effects According to the Council on Environmental Quality (CEQ) National Environmental Protection Ac t (NEPA) regulations, “cumulative impact” is the impact on the environment which results from the incremental impact of the action when added to other past, present, and reasonably foreseeable future actions regardless of what agency (federal or non-federal) or person undertakes such actions (40 CFR 1508.7). -
Southern Exposures
Searching for the Pliocene: Southern Exposures Robert E. Reynolds, editor California State University Desert Studies Center The 2012 Desert Research Symposium April 2012 Table of contents Searching for the Pliocene: Field trip guide to the southern exposures Field trip day 1 ���������������������������������������������������������������������������������������������������������������������������������������������� 5 Robert E. Reynolds, editor Field trip day 2 �������������������������������������������������������������������������������������������������������������������������������������������� 19 George T. Jefferson, David Lynch, L. K. Murray, and R. E. Reynolds Basin thickness variations at the junction of the Eastern California Shear Zone and the San Bernardino Mountains, California: how thick could the Pliocene section be? ��������������������������������������������������������������� 31 Victoria Langenheim, Tammy L. Surko, Phillip A. Armstrong, Jonathan C. Matti The morphology and anatomy of a Miocene long-runout landslide, Old Dad Mountain, California: implications for rock avalanche mechanics �������������������������������������������������������������������������������������������������� 38 Kim M. Bishop The discovery of the California Blue Mine ��������������������������������������������������������������������������������������������������� 44 Rick Kennedy Geomorphic evolution of the Morongo Valley, California ���������������������������������������������������������������������������� 45 Frank Jordan, Jr. New records -
Inactive Mines on Gallatin National Forest-Administered Land
Abandoned-Inactive Mines on Gallatin National Forest-AdministeredLand Montana Bureau of Mines and Geology Abandoned-Inactive Mines Program Open-File Report MBMG 418 Phyllis A. Hargrave Michael D. Kerschen CatherineMcDonald JohnJ. Metesh PeterM. Norbeck RobertWintergerst Preparedfor the u.s. Departmentof Agriculture ForestService-Region 1 Abandoned-Inactive Mines on Gallatin National Forest-AdministeredLand Open-File Report 418 MBMG October 2000 Phyllis A. Hargrave Michael D. Kerschen Catherine McDonald John J. Metesh Peter M. Norbeck Robert Wintergerst for the U.S. Department of Agriculture Forest Service-Region I Prepared Contents List of Figures .V List of Tables . VI IntToduction 1 1.IProjectObjectives 1 1.2AbandonedandInactiveMinesDefined 2 1.3 Health and Environmental Problems at Mines. 3 1.3.1 Acid-Mine Drainage 3 1.3.2 Solubilities of SelectedMetals 4 1.3.3 The Use of pH and SC to Identify Problems. 5 1.4Methodology. 6 1.4.1 Data Sources : 6 1.4.2Pre-Field Screening. 6 1.4.3Field Screening. 7 1.4.3.1 Collection of Geologic Samples. 9 1.4.4 Field Methods ' 9 1.4.4.1 Selection of Sample Sites 9 1.4.4.2 Collection of Water and Soil Samples. 10 1.4.4.3 Marking and Labeling Sample Sites. 10 1.4.4.4ExistingData 11 1.4.5 Analytical Methods """"""""""""""""'" 11 1.4.6Standards. 12 1.4.6.1Soil Standards. 12 1.4.6.2Water-QualityStandards 13 1.4.7 Analytical Results 13 1.5 Gallatin National Forest 14 1.5.1 History of Mining 16 1.5.1.1 Production 17 1.5.1.2Milling 18 1.6SummaryoftheGallatinNationaIForestInvestigat~on 19 1.7 Mining Districts and Drainages 20 Gallatin National Forest Drainages 20 2.1 Geology "' ' '..' ,.""...' ""." 20 2.2 EconomicGeology. -
Fall 2003-Spring 2004)
David Korevaar, Helen and Peter Weil Professor of Piano 1 Updated: July 2018 David Korevaar University of Colorado at Boulder, College of Music 301 UCB, Boulder, CO 80309-0301 303-492-6256, [email protected] www.davidkorevaar.com http://spot.colorado.edu/~korevaar Curriculum Vitae Educational Background: Doctor of Musical Arts, Piano, The Juilliard School, 2000. Doctoral Document: “Ravel’s Mirrors.” DMA Document. New York: The Juilliard School, 2000. xi + 196 pp. Awarded Richard French prize for best DMA Document, The Juilliard School, 2000. Committee: L. Michael Griffel, Robert Bailey, Jerome Lowenthal. Piano studies with Abbey Simon. Related area studies with Jonathan Dawe, Jane Gottlieb, L. Michael Griffel, David Hamilton, Joel Sachs, Maynard Solomon, Claudio Spies. Master of Music, Piano, The Juilliard School, 1983. Bachelor of Music, Piano, The Juilliard School, 1982. Piano studies with Earl Wild. Composition studies with David Diamond. Chamber music studies with Claus Adam, Paul Doktor, Felix Galimir, Leonard Rose, Harvey Shapiro. Independent piano studies: Paul Doguereau (1985-1998). Earl Wild (1976-1984). Sherman Storr (1969-1976). Andrew Watts (2013) Richard Goode (2013) Summer programs: Johannesen International School of the Arts, Victoria, B. C. (1980). Piano studies with John Ogdon, Robin McCabe, Joseph Bloch, Bela Siki. Bowdoin Summer Music Program (1981). Piano studies with Martin Canin. Aspen (1985). Piano studies with Claude Frank. David Korevaar, Helen and Peter Weil Professor of Piano 2 Teaching Affiliations: Academic year appointments: Current: Professor of Piano at the University of Colorado at Boulder (2011-); Associate Professor with tenure (2006-2011); appointed as Assistant Professor in 2000. Former: University of Bridgeport, Bridgeport, Connecticut (Adjunct position, “Head of Piano Studies”; 1995-2000). -
2018 Gore Mountain UMP Amendment
Appendix 1 SEQRA Full Environmental Assessment Form Parts 1, 2 and 3 A-1 Full Environmental Assessment Form Part 1 - Project and Setting Instructions for Completing Part 1 Part 1 is to be completed by the applicant or project sponsor. Responses become part of the application for approval or funding, are subject to public review, and may be subject to further verification. Complete Part 1 based on information currently available. If additional research or investigation would be needed to fully respond to any item, please answer as thoroughly as possible based on current information; indicate whether missing information does not exist, or is not reasonably available to the sponsor; and, when possible, generally describe work or studies which would be necessary to update or fully develop that information. Applicants/sponsors must complete all items in Sections A & B. In Sections C, D & E, most items contain an initial question that must be answered either “Yes” or “No”. If the answer to the initial question is “Yes”, complete the sub-questions that follow. If the answer to the initial question is “No”, proceed to the next question. Section F allows the project sponsor to identify and attach any additional information. Section G requires the name and signature of the project sponsor to verify that the information contained in Part 1is accurate and complete. A. Project and Sponsor Information. Name of Action or Project: Gore Mountain Intensive Use Area 2017 Unit Management Plan (UMP) Amendment Project Location (describe, and attach a general -
Mining, Geology, and Geological History of Garnet at the Barton Garnet Mine, Gore Mountain, New York William Kelly
6: RARE EARTH ELEMENT AND YTTRIUM MINERAL OCCURENCES IN THE ADIRONDACK MOUNTAINS 7 MINING, GEOLOGY, AND GEOLOGICAL HISTORY OF GARNET AT THE BARTON GARNET MINE, GORE MOUNTAIN, NEW YORK WILLIAM KELLY New York State Geologist, Emeritus, Division of Research and Collections, New York State Museum, Albany, NY 12230, [email protected] KEYWORDS: Garnet, Mining, Gore Mountain, Metamorphism, Lyon Mountain Granite ABSTRACT Garnet megacrysts commonly 30 centimters (cm) ranging up to 1 meter (m) in diameter occur at the summit of Gore Mountain, Adirondacks, NY and were mined there for abrasives for more than a century. The mine, owned by Barton Mines Co., LLC, is roughly 2 km x 150 m and is located in a hornblende-rich garnet amphibolite at the southern boundary of a metamorphosed olivine gabbro body that is in fault contact with charnockite. Barton supplies garnet, a chemically homogeneous pyrope-almandine, to the waterjet cutting, lapping, and abrasive coatings industries. The garnet megacrysts are reliably dated at 1049 ± 5 Ma. The growth of the garnet megacrysts was facilitated by an influx of hydrothermal fluid emanating from the ore body’s southern boundary fault. The fluids were most probably associated with the intrusion of the Lyon Mountain Granite (1049.9 ± 10 Ma) and/or associated pegmatitic rocks late in the tectonic history of the Adirondacks. INTRODUCTION The Adirondack Mountains in upstate New York are a small outlier of a larger body of rocks of similar age and geologic history that is located to the north in Canada. The Adirondack region can be loosely divided into amphibolite metamorphic facies Lowlands, in the northwest, and the granulite facies Central Highlands, which are 86 THE ADIRONDACK JOURNAL OF ENVIRONMENTAL STUDIES VOLUME 21 87 7: MINING, GEOLOGY, AND GEOLOGICAL HISTORY OF GARNET AT THE BARTON GARNET MINE, GORE MOUNTAIN, NEW YORK separated by a very large, northwest-dipping fault zone. -
Relevance of a Major Scarp and Two Associated Landslides in The
GEOLOGICA BELGICA (2018) 21/3-4: 101-110 Seismotectonic activity in East Belgium: relevance of a major scarp and two associated landslides in the region of Malmedy Anne-Sophie MREYEN1*, Alain DEMOULIN² & Hans-Balder HAVENITH1 1 University of Liege, Department of Geology, Allée du six Août 14, B18, 4000 Liege, Belgium. ² University of Liege, Department of Physical Geography, Clos Mercator 3, B11, 4000 Liege, Belgium. *corresponding author: [email protected]. ABSTRACT. Geomorphological markers such as scarps, river diversions and slope failures can be used as proxy indicators for the seismotectonic activity of a region. This study concentrates on the Malmedy-Bévercé area, E-Belgium, where formerly unknown geomorphological features have been recently discovered in the frame of a new regional geological mapping campaign. The area is characterised by gentle to locally very steep slopes along the Warche valley crossing the Stavelot Massif and the Malmedy Graben. Coupled with a LiDAR-DEM and UAV imagery analysis, field mapping has revealed a steep scarp extending near two landslides on the southern hillslopes of the Warche valley at Bévercé. These slope failures developed in the Permian conglomerates of the Malmedy Formation (also known as the Poudingue de Malmedy), which represent the infill of the Malmedy Graben. Roughly perpendicular to the graben axis, the scarp has a N330°E orientation similar to that of the seismotectonically active Hockai Fault Zone that crosses the Malmedy region in this area. In this paper, we present the geological and geomorphological context of the Bévercé scarp and of the largest landslide. Furthermore, we demonstrate the results of a geophysical reconnaissance survey of the structures (seismic refraction and electrical resistivity profiling). -
On the Design of Rockfall Protection Galleries
Research Collection Doctoral Thesis On the design of rockfall protection galleries Author(s): Schellenberg, Kristian Publication Date: 2008 Permanent Link: https://doi.org/10.3929/ethz-a-005711071 Rights / License: In Copyright - Non-Commercial Use Permitted This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library DISS. ETH NO. 17924 ON THE DESIGN OF ROCKFALL PROTECTION GALLERIES A dissertation submitted to ETH ZURICH for the degree of Doctor of Sciences presented by KRISTIAN SCHELLENBERG Dipl. Bauingenieur ETH born 18.07.1978 citizen of Winkel ZH accepted on the recommendation of Prof. Thomas Vogel, examiner Prof. Dr. Norimitsu Kishi, co-examiner 2008 Dedicated to my father Jorge Hugo Schellenberg “El hombre es lo que su alma trae, su voluntad modifica, o su dejadez acentúa.”. Table of contents Summary .................................................................................................................................. 3 Zusammenfassung ................................................................................................................... 4 Resumen ................................................................................................................................... 5 1. Introduction ..................................................................................................................... 7 1.1. Existing structures .................................................................................................... -
Geological Survey
WASHINGTON . GEOLOGICAL SURVEY. HENRY LANDES, STA TE GEOLOGIST. VOLUME I. ANNUAL REPORT FOR 1901. OLYMPIA, WA.Sa: GWIN HICKS, . STATE PRINTER, 1902. (} • BOARD OF GEOLOGICAL SURVEY. HENRY McBRIDE, Preaident. Governor of Washington. C. w. MAYNA.RD, Secretary. Treasurer of Washington. F. P. GRAVES, President of the University of Washington. E. A. BRYAN, President of the Washington Agrtoultural College and School of Soienoe. STA.FF OF GEOLOGICAL SURVEY. HENRY LANDES, • . State Geologist. Professor of Geology, University of Washington. SOLON SHEDD, • Geologist. Professor of Geology, Washington Agrioultural College and Sohool of Soienoe. w. s. THYNG, . Geol<Jg-ist. Professor of Mining Engineering, Washington Agrtoultural College and School of Science. D. A. LYON, Geol<Jgist. Late Professor ot Mining Engineering and Metallurgy, University of Washington. • LETTER OF TRANSMITTAL. To His Excellency, HENRY McBRIDE, Governor of the State of Washing ton and President of the Board of Geological Survey: Srn-I have the honor to present herewith the annual report of the State Geological Survey for the year 1901. It embraces a preliminary account of the geology and mineral resources of the state, to which is added a bibliography of the literature re ferring to Washington geology. It is hoped that this report, while very general in its nature, may serve as a basis for more elaborate and detailed reports in future years. Very respectfully, HENRY LANDES, State Geologist. UNIVEBSITY OF W ASBING'l'ON, SJIIATTLE, March, 1902. CONTENTS. PART I. PAGEi, CREATION OF A STATE GEOLOGICAL SURVEY,, BY HENRY LANDES, 3 Introduction . • . 3 The:La.w Establishing the Survey. 4 Organization of the Board of Geological Survey. -
Downscaling of Climate Change Scenarios for a High Resolution, Site
https://doi.org/10.5194/esd-2021-9 Preprint. Discussion started: 31 March 2021 c Author(s) 2021. CC BY 4.0 License. Downscaling of climate change scenarios for a high resolution, site– specific assessment of drought stress risk for two viticultural regions with heterogeneous landscapes Marco Hofmann 1, Claudia Volosciuk 2, Martin Dubrovský 3,4 , Douglas Maraun 5 and Hans R. Schultz 1 5 1Department of General and Organic Viticulture, Hochschule Geisenheim University, Geisenheim, 65366, Germany 2Science and Innovation Department, World Meteorological Organization, Geneva, CH-1211, Switzerland 3Institute of Atmospheric Physics, The Czech Academy of Sciences, Prague, 141 00, Czech Republic 4Global Change Research Institute, The Czech Academy of Sciences, Brno, 603 00, Czech Republic 5Wegener Center for Climate and Global Change, University of Graz, Graz, 8010, Austria 10 Correspondence to : Marco Hofmann ([email protected]) Abstract. Extended periods without precipitation observed for example in Central Europe including Germany during the seasons from 2018 to 2020, can lead to water deficit and yield and quality losses for grape and wine production. However, irrigation infrastructure is largely non–existent. Regional climate models project changes of precipitation amounts and patterns, indicating an increase in frequency of occurrence of comparable situations in the future. In order to assess possible impacts of 15 climate change on the water budget of grapevines, a water balance model was developed, which accounts for the large heterogeneity of vineyards with respect to their soil water storage capacity, evapotranspiration as a function of slope and aspect, and viticultural management practices. The model was fed with data from soil maps (soil type and plant available water capacity), a digital elevation model, the European Union (EU) vineyard–register, observed weather data and future weather data provided by regional climate models and a stochastic weather generator.