UNIVERSITY of NEVADA-RENO Nevada Bureau of Mines and Geology Un~Vrrsiryof Nevada-8.Eno Reno, Nevada 89557-0088 (702) 784-6691 FAX: (7G2j 784-1709
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Rartioter Vol
rartioter Vol. XII, No. 1 WINTER 1 9 7 9 BLACK DOME IN 1924 The Catskill Mountains have been known to white men for three hundred years and their valleys have been settled more than a cen- tury. It would seem as if all their summits ought by this time to be easily accessible by well known trails. Yet there are a dozen or more of the higher ones, above 3500 feet, which have no trails to their summits and which are climbed only by the exploring hiker, or perhaps a bear hunter in winter. I recently found another trackless peak, Black Dome, just under 4000 feet--3990 according to the Durham sheet of the United States Geological Survey--on a week-end climb in the northern Catskills. There is no trail over it, and the only paths that reach its flanks are faded out logging roads in the valleys north and south, attain- ing heights 1500 feet below its highest point. Black Dome is the central and highest of the three peaks that make up the Blackhead Mountains, running east and west, Black Head being the easternmost, then Black Dome and the last Thomas Cole. The other two are about fifty feet lower than the Dome. South of them is the valley of the East Kill, north that of Batavia Kill. North of Black Head runs a long ridge to Acra Point, then turning west to Windham High Peak. South this ridge runs through North Mountain and Stoppel Mountain to Kaaterskill Clove. Black Head is accessible by a good trail. -
Ecoregions of Nevada Ecoregion 5 Is a Mountainous, Deeply Dissected, and Westerly Tilting Fault Block
5 . S i e r r a N e v a d a Ecoregions of Nevada Ecoregion 5 is a mountainous, deeply dissected, and westerly tilting fault block. It is largely composed of granitic rocks that are lithologically distinct from the sedimentary rocks of the Klamath Mountains (78) and the volcanic rocks of the Cascades (4). A Ecoregions denote areas of general similarity in ecosystems and in the type, quality, Vegas, Reno, and Carson City areas. Most of the state is internally drained and lies Literature Cited: high fault scarp divides the Sierra Nevada (5) from the Northern Basin and Range (80) and Central Basin and Range (13) to the 2 2 . A r i z o n a / N e w M e x i c o P l a t e a u east. Near this eastern fault scarp, the Sierra Nevada (5) reaches its highest elevations. Here, moraines, cirques, and small lakes and quantity of environmental resources. They are designed to serve as a spatial within the Great Basin; rivers in the southeast are part of the Colorado River system Bailey, R.G., Avers, P.E., King, T., and McNab, W.H., eds., 1994, Ecoregions and subregions of the Ecoregion 22 is a high dissected plateau underlain by horizontal beds of limestone, sandstone, and shale, cut by canyons, and United States (map): Washington, D.C., USFS, scale 1:7,500,000. are especially common and are products of Pleistocene alpine glaciation. Large areas are above timberline, including Mt. Whitney framework for the research, assessment, management, and monitoring of ecosystems and those in the northeast drain to the Snake River. -
ALBANY CHAPTER of the ADIRONDACK MOUNTAIN CLUB
The Cloudsplitter Vol. 79 No. 3 July-September 2016 published by the ALBANY CHAPTER of the ADIRONDACK MOUNTAIN CLUB The Cloudsplitter is published quarterly by the Albany Chapter of the Adirondack Mountain Club and is distributed to the membership. All issues (January, April, July, and October) feature activities schedules, trip reports, and other articles of interest to the outdoor enthusiast. All outings should now be entered on the web site www.adk-albany.org. Echoes should be entered on the web site www.adk-albany.org with your login information. The Albany Chapter may be Please send your address and For Club orders & membership For Cloudsplitter related issues, reached at: phone number changes to: call (800) 395-8080 or contact the Editor at: Albany Chapter ADK Adirondack Mountain Club e-mail: [email protected] The Cloudsplitter Empire State Plaza 814 Goggins Road home page: www.adk.org c/o Karen Ross P.O. Box 2116 Lake George, NY 12845-4117 7 Bird Road Albany, NY 12220 phone: (518) 668-4447 Lebanon Spgs., NY 12125 home page: fax: (518) 668-3746 e-mail: [email protected] www.adk-albany.org Submission deadline for the next issue of The Cloudsplitter is August 15, 2016 and will be for the months of October, November and December, 2016. Many thanks to Gail Carr for her cover sketch. September 7 (1st Wednesdays) Business Meeting of Chapter Officers and Committees 6:00 p.m. at Little’s Lake in Menands Chapter members are encouraged to attend - please call James Slavin at 434-4393 There are no Chapter Meetings held during July, August, or September MESSAGE FROM THE CHAIRMAN It has been my honor and pleasure to serve as Chapter Chair, along with Frank Dirolf as Vice Chair, for the last two years. -
Mineral Resources of the Clan Alpine Mountains Wilderness Study Area, Churchill County, Nevada
Mineral Resources of the Clan Alpine Mountains Wilderness Study Area, Churchill County, Nevada U.S. GEOLOGICAL SURVEY BULLETIN 1727-B 1- J Chapter B Mineral Resources of the Clan Alpine Mountains Wilderness Study Area, Churchill County, Nevada By RICHARD F. HARDYMAN, WILLIAM E. BROOKS, MICHAEL J. BLASKOWSKI, HARLAN N. BARTON, and DAVID A. PONCE U.S. Geological Survey JERRY E. OLSON U.S. Bureau of Mines U.S. GEOLOGICAL SURVEY BULLETIN 1727 MINERAL RESOURCES OF WILDERNESS STUDY AREAS WEST-CENTRAL 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 Mineral resources of the Clan Alpine Mountains Wilderness Study Area, Churchill County, Nevada. (Mineral resources of wilderness study areas west-central Nevada ; ch. B) (U.S. Geological Survey bulletin ; 1727-B) Bibliography: p. Supt. of Docs, no.: I 19.3:1727-6 1. Mines and mineral resources Nevada Clan Alpine Mountains Wilderness. 2. Clan Alpine Mountains Wilderness (Nev.) I. Hardyman, Richard F. II. Series. III. Series: U.S. Geological Survey bulletin ; 1727-B. QE75.B9 no. 1727-B 557.3 s [553'.09793'52] 87-600445 [TN24.N3] 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. -
Idaho Roadless Areas FEIS
United States Roadless Area Conservation Department of Agriculture National Forest System Lands in Idaho Forest Service Final Environmental Impact Statement Idaho National Forests August 2008 Appendix C—Idaho Roadless Areas Volume 5: Caribou, Challis, Salmon, and Targhee National Forests The U.S. 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, or 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 (202) 720-2600 (voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326-W, Whitten Building, 1400 Independence Avenue, SW, Washington, DC 20250-9410 or call (202) 720-5964 (voice and TDD). USDA is an equal opportunity provider and employer. Roadless Area Conservation; National Forest System Lands in Idaho FEIS Idaho Roadless Areas TABLE OF CONTENTS APPENDIX C. IDAHO ROADLESS AREAS............ C5-1 Diamond Peak #601..................................... C5-155 Greylock #007............................................... C5-161 CARIBOU NATIONAL FOREST Grouse Peak #010 ........................................ C5-165 Bear Creek #615 ............................................... C5-3 Hanson Lakes #915 see Sawtooth National Bonneville -
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 -
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. -
Burning Man Geology Black Rock Desert.Pdf
GEOLOGY OF THE BLACK ROCK DESERT By Cathy Busby Professor of Geology University of California Santa Barbara http://www.geol.ucsb.edu/faculty/busby BURNING MAN EARTH GUARDIANS PAVILION 2012 LEAVE NO TRACE Please come find me and Iʼll give you a personal tour of the posters! You are here! In one of the most amazing geologic wonderlands in the world! Fantastic rock exposure, spectacular geomorphic features, and a long history, including: 1. PreCambrian loss of our Australian neighbors by continental rifting, * 2. Paleozoic accretion of island volcanic chains like Japan (twice!), 3. Mesozoic compression and emplacement of a batholith, 4. Cenozoic stretching and volcanism, plus a mantle plume torching the base of the continent! Let’s start with what you can see on the playa and from the playa: the Neogene to Recent geology, which is the past ~23 million years (= Ma). Note: Recent = past 15,000 years http://www.terragalleria.com Then we’ll “build” the terrane you are standing on, beginning with a BILLION years ago, moving through the Paleozoic (old life, ~540-253 Ma), Mesozoic (age of dinosaurs, ~253-65 Ma)) and Cenozoic (age of mammals, ~65 -0 Ma). Neogene to Recent geology Black Rock Playa extends 100 miles, from Gerlach to the Jackson Mountains. The Black Rock Desert is divided into two arms by the Black Rock Range, and covers 1,000 square miles. Empire (south of Gerlach)has the U.S. Gypsum mine and drywall factory (brand name “Sheetrock”), and thereʼs an opal mine at base of Calico Mtns. Neogene to Recent geology BRP = The largest playa in North America “Playa” = a flat-bottomed depression, usually a dry lake bed 3,500ʼ asl in SW, 4,000ʼ asl in N Land speed record: 1997 - supersonic car, 766 MPH Runoff mainly from the Quinn River, which heads in Oregon ~150 miles north. -
C:\A Projects\AAA IBLA Decs\061IBLA\L370-375.Wpd
CHURCHILL COUNTY BOARD OF COMMISSIONERS IBLA 81-539 Decided February 17, 1982 Appeal from a decision of the Nevada State Director, Bureau of Land Management, denying a protest of wilderness study area designations. 8500 (N-932.6). Affirmed. 1. Federal Land Policy and Management Act of 1976: Wilderness--Wilderness Act--Words and Phrases. "Roadless." H.R. Rep. No. 94-1163, 94th Cong., 2d Sess. 17 (1976), provides a definition of "roadless" adopted by the Bureau of Land Management in its Wilderness Inventory Handbook. The word "roadless" refers to the absence of roads which have been improved and maintained by mechanical means to insure relatively regular and continuous use. A way maintained solely by the passage of vehicles does not constitute a road. 2. Federal Land Policy and Management Act of 1976: Wilderness--Wilderness Act Sights and sounds outside a wilderness study area will be considered during the study phase of the wilderness review process absent a finding by BLM during the inventory phase that such impacts are adjacent to the unit and are so extremely imposing that they cannot be ignored, and and if not considered, reasonable application of inventory guidelines would be questioned. 3. Federal Land Policy and Management Act of 1976: Wilderness--Wilderness Act The requirement in section 2(c) of the Wilderness Act of 1964, 16 U.S.C. § 1131(c) (1976), that a wilderness possess, inter alia, outstanding opportunities for solitude or a primitive and unconfined type of 61 IBLA 370 IBLA 81-539 recreation is properly construed to require outstanding opportunities for either solitude or a primitive and unconfined type of recreation; both need not be present in an inventory unit to allow the unit to enter the study phase of the wilderness review process. -
DOE/ET /27010-2 MC Coy AREA, NEVADA Geothermal Reservoir
t -- DOE/ET /27010-2 MC COy AREA, NEVADA Geothermal Reservo ir Assessment Case History Northern Basin and Range ANNUAL REPORT January 1980 - 31 December 1980 H. D. PILKINGTON August 1981 WORK PERFORMED UNDER CONTRACT DE AC 08-79 ET 27010 At-1AX EXPLORATION, INC. 7100 West 44th Ave. Wheat Rid~~t CO 80033 r TABLE OF CONTENTS Page ABSTRACT INTRODUCTION 2 EXPLORATION HISTORY 4 Geological Studies 4 Geochemical Studies . 6 Geophys i ca 1 Studies. 10 Exploration Drilling 13 \. TAB LE OF ILLUSTRATIONS Page Figure 1. Location map for the McCoy geothermal prospect 3 Figure 2. Geologic map of the McCoy geothermal prospect, Nevada (after Adams, Moore and Struhsacker, 1980) 5 Figure 3 Geologic cross-sections through well 14-7 (top) and well 66-8 (bottom) after Pilkington, 1980. 7 Figure 4 Location map of drill holes used on geochemical study of drill cuttings. 9 Figure 5 Contour map of mercury in drill cuttings from 120-160 foot interval at McCoy (Pilkington, 1980) . 11 Figure 6 Gravity profile with automatic interpretation for density (top) compared wi th geologic cross-section (bottom) 12 Figure 7 Resistivity at 5km depth from 10 magnetotelluric inve·rsion (Te mode) and location of survey lines 14 and stations Figure 8 MT section (Te mode, 10 inversion) along line C-C' compared with geologic section (after Lange, 1980) . 15 Figure 9 Survey location map of the McCoy prospect, after Wilt etal, 1980 . 16 Figure 10 MT section (Te mode 10 inversion) along line A-A" compared with EM data, after Lange, 1980 17 Page Table I Chemical analyses of McCoy Mine well and Well 66-8 waters 8 ABSTRACT The McCoy geothermal prospect is located at the junction of the Augusta Mountains, Clan Alpine Mountains and the New Pass Range. -
Riders- Thomas Flynn, B. Riley) (Kansas St. Hist. Soc.
99. Camp Floyd: Hutchings' California Magazine July 1860 . (riders - Thomas Flynn, B. Riley) (Kansas St. Hist. Soc.) ( General Road Agent: W.W. Finney) (agents: Hamilton, Ruffin) (stations: St. Joseph, Kennekuk, 3rd Station, Marysville, 5th Station, Little Blue, Up Little Blue, Ft. Kearney, Plum Creek, Cottonwood, Crossing South Platte, Ash Hollow, Rush Creek, Larence Fork, Chimney Rock, Scott's Bluff, Horse Creek, Ft. Laramie, Horse-Shoe Creek, Deer Creek, Platte Bridge, 1st Crossing Sweetwater, 3rd Crossing Sweetwater, Last Crossing Sweetwater, South Pass, Dry Sandy, Little Sandy, Big Sandy, Green River, Ham's Fork, Miller's Fork, Ft. Bridger, Bear River, Weber River/mouth of Echo Canyon, Salt Lake City, Hot Springs, Camp Floyd, Rush Valley, Simpson's Springs, Dug Way (Well) Desert, Fish Springs, Pleasant Valley, Schell Creek, Thousand Spring valley, Ruby Valley, Two Springs, Next Station, Willow Creek, Antelope Creek, Mouth of Canyon, Cold Springs, Reese's River, Willow Creek, Sink of Carson River, Walker's River, Up Walker's River, Carson River, Miller ' s Station, Carson River, Miller's Station, Carson City, Placerville, Sacramento City, San Francisco) [SJM] U.S. Senate, Exec. Doc. 46th Congress, 3rd session, I, No 21 p. 7-8 "Contract with Overland Mail Co, 11 & "Route 10773 " (stations: St. Joseph, Troy, Lewis, Kinnekuk, Goteschall, Log Chain, Seneca, Gautard's, Marysville, Cottonwood, Rock House, Rock Creek/Lodi P.O., Virginia City, Big Sandy, Milllersville, Kiowa Station, Liberty Farm, Thirty-two Mile Creek, Sand Hill, Kearney Station, Fort Kearney, Platt's Station, Garden, Plum Creek, Willow Island, Midway, Gilman's, Cottonwood Springs, Cold Springs, Fremont Springs, Dansey's Station, Gills, Diamond Springs, Frontz Station, Julesburg, Nine Mile Station, Pole Creek No. -
Washington State's Scenic Byways & Road Trips
waShington State’S Scenic BywayS & Road tRipS inSide: Road Maps & Scenic drives planning tips points of interest 2 taBLe of contentS waShington State’S Scenic BywayS & Road tRipS introduction 3 Washington State’s Scenic Byways & Road Trips guide has been made possible State Map overview of Scenic Byways 4 through funding from the Federal Highway Administration’s National Scenic Byways Program, Washington State Department of Transportation and aLL aMeRican RoadS Washington State Tourism. waShington State depaRtMent of coMMeRce Chinook Pass Scenic Byway 9 director, Rogers Weed International Selkirk Loop 15 waShington State touRiSM executive director, Marsha Massey nationaL Scenic BywayS Marketing Manager, Betsy Gabel product development Manager, Michelle Campbell Coulee Corridor 21 waShington State depaRtMent of tRanSpoRtation Mountains to Sound Greenway 25 Secretary of transportation, Paula Hammond director, highways and Local programs, Kathleen Davis Stevens Pass Greenway 29 Scenic Byways coordinator, Ed Spilker Strait of Juan de Fuca - Highway 112 33 Byway leaders and an interagency advisory group with representatives from the White Pass Scenic Byway 37 Washington State Department of Transportation, Washington State Department of Agriculture, Washington State Department of Fish & Wildlife, Washington State Tourism, Washington State Parks and Recreation Commission and State Scenic BywayS Audubon Washington were also instrumental in the creation of this guide. Cape Flattery Tribal Scenic Byway 40 puBLiShing SeRviceS pRovided By deStination