Great Basin Tool-Stone Sources
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Historic Fire Lookouts? the View and the Solitude Can’T Be Beat
ince shortly after the turn of the century, ¢ government personnel have stood guard Bonus Points 25 S over western lands. In Klamath, Lake, W ant to spend more time in one of the area’s and Modoc Country, fire lookouts open to the historic fire lookouts? The view and the solitude can’t be beat. public offer breathtaking views from the top of • Bald Butte Lookout Rental - Many historic area lookouts HISTORIC the world as well as a chance to visit history . are being made available as rustic vacation rentals. Reservations are required. For Bald Butte Lookout Rental, arly fire lookouts were simply scaffolds, and outdoor recreation activities including skiing and FIRE E snowmobiling, contact the Paisley Ranger District, attached precariously to trees and offering 541-943-3114. Bald Butte Lookout is available little shelter to early fire observers. year-round. • Hager Mountain Lookout Rental - While a little more LOOKOUTS ost surviving fire lookout towers, built in difficult to get to, this lookout offers the adventurous a M the 20’s and 30’s, are 14' by 14' structures breathtaking view year-round from over 7,000 feet. On a assembled from pre-manufactured kits and clear day you might see as far north as Mt. Hood, and south to Mt. Shasta. Contact the Silver Lake Ranger packed up to mountain peaks by truck or even District, 541-576-2107, for information and reservations. mule train. Windows offered a 360-degree view Reservations also can be made for the Fremont Point Cabin of the area for the occupant. All the comforts of perched on the edge of the massive escarpment west of home were available: wood stove, bed and Summer Lake. -
Josie Pearl, Prospector on Nevada's Black Rock Desert
JUNE, 1962 40c • • • • . Author's car crossing the playa of Black Rock Desert in northwestern Nevada. On Black Rock Desert Trails When Dora Tucker and Nell Murbarger first began exploring the Black Rock country in northwestern Nevada they did not realize what a high, wide and wild country it was. On the Black Rock a hundred miles doesn't mean a thing. In the 10,000 square miles of this desert wasteland there isn't a foot of pavement nor a mile of railroad— neither gasoline station nor postoffice. Antelopes out-number human beings fifty to one. There's plenty of room here for exploring. By NELL MURBARGER Photographs by the author Map by Norton Allen S AN illustration of what the want to! Ain't nothin' there!" is known as "the Black Rock country," Black Rock country affords Thanking him, we accepted his re- the desert from which it derives its in the way of variety and con- port as a favorable omen and headed name actually is a stark white alkali trast, we made a J 50-mile loop trip out into the desert. Almost invariably playa, averaging a dozen miles in out of Gerlach last June. Our previous we find our best prowling in places width and stretching for 100 miles exploring of the region had been mostly where folks have told us there "ain't from Gerlach to Kings River. Merging in the northern and eastern sections, nothin'." imperceptibly with the Black Rock on so we hadn't the slightest idea of what Rising precipitously from the dead the southwest is the section known as we might find in the southern part. -
Lithic Raw Material Prospects in the Mojave Desert, California
UC Merced Journal of California and Great Basin Anthropology Title Lithic Raw Material Prospects in the Mojave Desert, California Permalink https://escholarship.org/uc/item/8np7g12w Journal Journal of California and Great Basin Anthropology, 11(2) ISSN 0191-3557 Authors Wilke, Philip J. Schroth, Adella B. Publication Date 1989-07-01 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Journal of California and Great Basin Anthropology Vol. 11, No. 2, pp. 146-174 (1989). Lithic Raw Material Prospects in the Mojave Desert, California PHILIP J. WILKE and ADELLA B. SCHROTH, Dept. of Anthropology, Univ. of California, Riverside, CA 92521. A HIS paper discusses lithic raw material THEORETICAL BACKGROUND prospects (or simply "prospects"), places where potentially flakeable tool stone was Acquisition of tool stone by aboriginal assayed or tested for quality. It characterizes peoples was an industry that in terms of scale this site type and contrasts it with quarries, varied greatly from one situation to another. places where stone was obtained consistently The large and well-known quarries of the and in quantity, and places where stone was western United States represent one end of picked up, used, and discarded with little the spectrum. These include the AUbates modification. We believe prospects represent silicified dolomite quarries, Texas; Spanish a major archaeological site type that has re Diggings quartzite quarries, Wyoming; ceived inadequate attention in the literature. Tosawihi opalite quarries, Nevada; and Casa We describe here a prospect site (CA- Diablo and Coso obsidian quarries, California, SBr-5872), characterize its assemblage, and to name a few. -
Updated Site Characterization Data Inventory
INL/MIS-16-38127-D DE-EE0007159 Rev. 1 Updated Site Characterization Data Inventory May 2016 DISCLAIMER This information was prepared as an account of work sponsored by an agency of the U.S. Government. Neither the U.S. Government nor any agency thereof, nor any of their employees, makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness, of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. References herein to any specific commercial product, process, or service by trade name, trade mark, manufacturer, or otherwise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the U.S. Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the U.S. Government or any agency thereof. INL/MIS-16-38127-D Rev. 1 Updated Site Characterization Data Inventory May 2016 Snake River Geothermal Consortium Hosted by Idaho National Laboratory Idaho Falls, Idaho www.snakerivergeothermal.org Prepared for the U.S. Department of Energy Office of Energy Efficiency and Renewable Energy Under DOE Idaho Operations Office Contract DE-AC07-05ID14517 CONTENTS ACRONYMS ............................................................................................................................................... ix 1. DATA MADE AVAILABLE THROUGH THE GEOTHERMAL DATA REPOSITORY ARCHIVE ......................................................................................................................................... -
Ra Ising the Ba R
12 Ra ising the Ba r Lithic Analysis and Archaeological Research in the Southeast William Andrefsky Jr. When I was asked to provide comments on the collection of lithic analysis pa- pers presented at the Southeastern Archaeological Conference (included within this volume), I did not realize the extent to which lithic tools and debitage had been overlooked in the region as a medium for interpreting past aboriginal practices and behaviors. According to the session abstract, the goal of the lithic symposium and this volume is to highlight contemporary methods and theory in lithic analysis to encourage researchers in the Southeast to integrate lithic data into their site interpretations. After a quick perusal of the literature for the region, it was apparent that very few Southeast lithics-related publications have appeared in the national peer-reviewed literature (Daniel2001; Shott and Ballenger 2007); slightly more lithic research occurs in regional journal venues (Carr and Bradbury 2000; Franklin and Simek 2008; Peacock 2004); and other contributions are found in edited volumes not necessarily focused specifically on lithics in the region (Anderson and Sassaman 1996; Carr 1994a; Henry and Odell1989; Johnson and Morrow 1987). Similar to the case of Mesoamerica and the American Southwest, there is a relatively low proportion of lithics- based research relative to ceramics and architecture. Such a trend comes as a surprise to me. However, I have been hooked on stone tool technology since the sixth grade when I first began looking at Louis Leakey's Oldowan pebble tools and wondering whether the broken cobbles in my local creek could have been made by Australopithecus. -
Geologic Map of the Twin Falls 30 X 60 Minute Quadrangle, Idaho
Geologic Map of the Twin Falls 30 x 60 Minute Quadrangle, Idaho Compiled and Mapped by Kurt L. Othberg, John D. Kauffman, Virginia S. Gillerman, and Dean L. Garwood 2012 Idaho Geological Survey Third Floor, Morrill Hall University of Idaho Geologic Map 49 Moscow, Idaho 83843-3014 2012 Geologic Map of the Twin Falls 30 x 60 Minute Quadrangle, Idaho Compiled and Mapped by Kurt L. Othberg, John D. Kauffman, Virginia S. Gillerman, and Dean L. Garwood INTRODUCTION 43˚ 115˚ The geology in the 1:100,000-scale Twin Falls 30 x 23 13 18 7 8 25 60 minute quadrangle is based on field work conduct- ed by the authors from 2002 through 2005, previous 24 17 14 16 19 20 26 1:24,000-scale maps published by the Idaho Geological Survey, mapping by other researchers, and compilation 11 10 from previous work. Mapping sources are identified 9 15 12 6 in Figures 1 and 2. The geologic mapping was funded in part by the STATEMAP and EDMAP components 5 1 2 22 21 of the U.S. Geological Survey’s National Cooperative 4 3 42˚ 30' Geologic Mapping Program (Figure 1). We recognize 114˚ that small map units in the Snake River Canyon are dif- 1. Bonnichsen and Godchaux, 1995a 15. Kauffman and Othberg, 2005a ficult to identify at this map scale and we direct readers 2. Bonnichsen and Godchaux, 16. Kauffman and Othberg, 2005b to the 1:24,000-scale geologic maps shown in Figure 1. 1995b; Othberg and others, 2005 17. Kauffman and others, 2005a 3. -
Nevada Hunter Information Sheet
Nevada Hunter Information Sheet CALIFORNIA BIGHORN SHEEP Unit 031 LOCATION: Unit 031 is located northwest of the town of Winnemucca. The unit is bounded on the north by the Oregon state line: the east by Unit 051, the south by Unit 035, and on the west by Unit 032. ELEVATION: The elevations range from 8,500' at the top of the Trout Creek Range to 4,100' along the Quinn River. TERRAIN: The unit is bounded on the west by the Bilk Creek Range, the north by the Trout Creek Range, the east by the Montana Mountains and the Double H Mountains. The Kings River Valley, a highly developed agricultural area, is situated among the ranges listed above. The Bilk Creek Range and the Trout Creek Range are mountainous with moderately sloped drainages. The Montana Mountains and the Double H Mountains are high table plateaus, rising sharply on their west faces, and sloping gradually to the east. The west slopes are short and deep; canyons draining to the east are long with deep precipitous gorges in their upper reaches. VEGETATION: The majority of the basins and slopes up to 6,500' elevation are dominated by sagebrush. Sites above those elevations typically have aspen in the drainages, islands of mahogany, and a mixed variety of shrubs and grasses. WEATHER AND CLIMATE: The precipitation varies from 7-18+ inches from the valley floor to the upper peaks. Rain and snow can cause travel problems from September through November. LAND STATUS: Approximately 85% of the unit is BLM land. Private land is mostly associated with agriculture or mining. -
Evolution of Deformation in the Buck Mountain Fault Damage Zone, Cambrian Flathead Sandstone, Teton Range, Wyoming Stephanie R
Pan-American Current Research on Fluid Inclusions Rice University, Houston, Texas, U.S.A., June 12-14, 2018, Abstract Volume Evolution of deformation in the Buck Mountain Fault damage zone, Cambrian Flathead Sandstone, Teton Range, Wyoming Stephanie R. FORSTNER, Stephen E. LAUBACH, András FALL Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas, U.S.A. E-mail: [email protected] The Teton Range is a normal fault block that contains older reverse faults (Love et al., 1992). Although generally considered to be Late Cretaceous to early Tertiary structures, the timing, kinematic style, and history of these faults is conjectural. Faults include the Forellen Peak Fault to the north, the Buck Mountain Reverse Fault (BMRF) to the west and south, and the Teton normal fault to the east (Love et al., 1992). The BMRF is rooted in Precambrian crystalline rocks and dips steeply to the east about 60°. The fractured Cambrian Flathead sandstone, an orthoquartzite (90%+ quartz), rests nonconformably on the Precambrian. Its stratigraphic position and relative isotropic mineralogy make the Flathead an ideal horizon for studying brittle deformation. Oriented Flathead hand samples were collected from the footwall of the BMRF along a partially overturned syncline (Figure 1). Continuous SEM-Cathodoluminescence (SEM-CL) scanlines of these samples allow for a systematic kinematic analysis of the cemented opening-mode fractures. We quantify attributes such as; geometry, spacing, orientation, and cross-cutting relationships. In isotropic rock, mode-I fractures primarily propagate along the plane perpendicular to Shmin; therefore, microfractures can be used to indicate paleostress trajectories, strain, and relative fracture timing (Anders et al., 2014; Hooker et al. -
Lahontan Cutthroat Trout Species Management Plan for the Upper Humboldt River Drainage Basin
STATE OF NEVADA DEPARTMENT OF WILDLIFE LAHONTAN CUTTHROAT TROUT SPECIES MANAGEMENT PLAN FOR THE UPPER HUMBOLDT RIVER DRAINAGE BASIN Prepared by John Elliott SPECIES MANAGEMENT PLAN December 2004 LAHONTAN CUTTHROAT TROUT SPECIES MANAGEMENT PLAN FOR THE UPPER HUMBOLDT RIVER DRAINAGE BASIN SUBMITTED BY: _______________________________________ __________ John Elliott, Supervising Fisheries Biologist Date Nevada Department of Wildlife, Eastern Region APPROVED BY: _______________________________________ __________ Richard L. Haskins II, Fisheries Bureau Chief Date Nevada Department of Wildlife _______________________________________ __________ Kenneth E. Mayer, Director Date Nevada Department of Wildlife REVIEWED BY: _______________________________________ __________ Robert Williams, Field Supervisor Date Nevada Fish and Wildlife Office U.S.D.I. Fish and Wildlife Service _______________________________________ __________ Ron Wenker, State Director Date U.S.D.I. Bureau of Land Management _______________________________________ __________ Edward C. Monnig, Forest Supervisor Date Humboldt-Toiyabe National Forest U.S.D.A. Forest Service TABLE OF CONTENTS Contents EXECUTIVE SUMMARY ……………………………………………………………………..1 INTRODUCTION……………………………………………………………………………….…2 AGENCY RESPONSIBILITIES……………………………………………………………….…4 CURRENT STATUS……………………………………………………………………………..6 RECOVERY OBJECTIVES……………………………………………………………………19 RECOVERY ACTIONS…………………………………………………………………………21 RECOVERY ACTION PRIORITIES BY SUBBASIN………………………………………….33 IMPLEMENTATION SCHEDULE……………………………………………………………..47 -
Nevada Department of Wildlife
Nevada Department of Wildlife BBIIGG GGAAMMEE RREELLEEAASSEE PPLLAANN For FISCAL YEARS 2014 AND 2015 (August 2013 – June 2015) August 2013 FY 2012 and 2013 BIG GAME RELEASE PLAN SUMMARY OF ACCOMPLISHMENTS Number Species Date Location County Type Released Desert Bighorn 10/29/11 Excelsior Mountains Mineral A 20 10/30 & Virginia Range Storey R 42 11/3/11 10/30/11 Gold Buttes Clark A 17 10/30 Delamar Mountains Lincoln A 35 &10/31/11 11/1/11 Meadow Valley Mtns Lincoln A 24 11/2/11 South Pahroc Range Lincoln A 25 4/30 & Virginia Range Storey A 11 5/2/12 5/22/12 Excelsior Mountains Mineral A 7 11/3/12 Excelsior Mountains Mineral A 25 California 11/5/11 Calico Mtn/Capitol Pk Humboldt A 25 Bighorn 11/7/11 Martin Creek, Santa Rosas Humboldt A 27 2/2 & Massacre Rim Washoe A 29 2/3/12 11/6/12 Jackson Mountains Humboldt A 23 1/15/13 Hays Canyon Range Washoe A 30 Santa Rosa Range (Peterman 1/16/13 Humboldt A 25 Creek) Rocky Mountain 2/6/12 Ruby Mountains Elko A 11 2/14/13 East Humboldt Range Elko A 20 1 FY 2014 and 2015 DESERT BIGHORN SHEEP PROPOSED RELEASE SUMMARY Location County Type Number Agency Candelaria Hills Mineral Augmentation 50 BLM - Stillwater Excelsior Mineral Augmentation 30 BLM - Stillwater Mountains Sonoma Range Humboldt Augmentation 50 BLM – Humboldt River Boulder Canyon, Delamar Lincoln Augmentation 30 BLM - Caliente Mountains Virginia Range Storey Augmentation 30 Private Gold Buttes Clark Augmentation 15 BLM – Southern Nevada Proposed source populations: Bare Mountains, Monte Cristo Range, Lone Mountain, River Mountains, Muddy Mountains, -
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. -
Thacker Pass Lithium Mine Final EIS, Appendix B, Mining Plan Of
Final Environmental Impact Statement Thacker Pass Lithium Mine Project Appendix B Mining Plan of Operations This page intentionally left blank. Appendix B – Mining Plan of Operations APPENDIX B. MINING PLAN OF OPERATIONS Thacker Pass Lithium Mine Project B-1 Final Environmental Impact Statement Appendix B – Mining Plan of Operations This page intentionally left blank. B-2 Thacker Pass Lithium Mine Project Final Environmental Impact Statement Thacker Pass Project Proposed Plan of Operations and Reclamation Plan Permit Application July 2019 October 2019 - Revised Submitted to: Bureau of Land Management Nevada Division of Environmental Protection Winnemucca District Bureau of Mining Regulation and Reclamation Humboldt River Field Office 901 S Stewart Street, Suite 4001 5100 East Winnemucca Boulevard Carson City, Nevada 89701 Winnemucca, Nevada 89445 Submitted by: LithiumNevada Lithium Nevada Corp. 3685 Lakeside Drive Reno, Nevada 89509 Contact: Edward (Ted) Grandy, VP Legal and Regulatory Affairs Thacker Pass Project – Plan of Operations and Reclamation Plan LithiumNevada Summary Lithium Nevada Corp. (LNC), a wholly owned subsidiary of Lithium Americas Corp. (LAC), proposes to construct, operate, reclaim, and close an open pit lithium mining and processing operation, the Thacker Pass Project (Project), located on public lands in northern Humboldt County, Nevada. The surface and subsurface mineral estates associated with the Project are located on public lands administered by the Bureau of Land Management (BLM), Winnemucca District, and controlled by federal unpatented lode mining claims owned by LNC. LNC is submitting this Plan of Operations and Reclamation Plan (Plan) to develop the Project in accordance with BLM Surface Management Regulations under 43 Code of Federal Regulations (CFR) 3809, Surface Occupancy regulations under 43 CFR 3715, and Nevada reclamation regulations under Nevada Administrative Code (NAC) 519A.