The Roberts Mountains Formation, a Regional Stratigraphic Study with Emphasis on Rugose Coral Distribution
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ANTC Environmental Assessment
U.S. Department of the Interior Bureau of Land Management Environmental Assessment DOI-BLM-NV-B010-2013-0024-EA Telecommunication Facilities at Kingston, Dyer, and Hickison Summit July 2013 Applicant: Arizona Nevada Tower Corporation 6220 McLeod Drive Ste. 100 Las Vegas, Nevada 89120 Battle Mountain District Bureau of Land Management 50 Bastian Road Battle Mountain, Nevada 89820 Table of Contents Page Chapter 1 Introduction 1 1.1 Introduction 1 1.2 Background 1 1.3 Identifying Information 2 1.4 Location of Proposed Action 2 1.5 Preparing Office 2 1.6 Case File Numbers 2 1.7 Applicant 2 1.8 Proposed Action Summary 3 1.9 Conformance 3 1.10 Purpose & Need 3 1.11 Scoping, Public Involvement & Issues 4 Chapter 2 Proposed Action & Alternatives 11 2.1 Proposed Action 11 2.1.1 Best Management Practices 13 2.2 No Action Alternative 13 2.3 Alternatives Considered but Eliminated from Detailed Analysis 14 Chapter 3 Affected Environment & Environmental Consequences 15 3.1 Project Site Descriptions 15 3.2 Issues 16 3.2.1 Air Quality 18 3.2.1.1 Affected Environment 18 3.2.1.2 Environmental Consequences 18 3.2.2 Cultural/Historical Resources 18 3.2.2.1 Affected Environment 18 3.2.2.2 Environmental Consequences 18 3.2.3 Noxious Weeds/Invasive Non-native Plants 19 3.2.3.1 Affected Environment 19 3.2.3.2 Environmental Consequences 20 3.2.4 Native American Religious Concerns 20 3.2.4.1 Affected Environment 20 3.2.4.2 Environmental Consequences 20 3.2.5 Migratory Birds 21 3.2.5.1 Affected Environment 21 3.2.5.2 Environmental Consequences 22 3.2.6 Solid/Hazardous -
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 -
Quaternary Fault and Fold Database of the United States
Jump to Navigation Quaternary Fault and Fold Database of the United States As of January 12, 2017, the USGS maintains a limited number of metadata fields that characterize the Quaternary faults and folds of the United States. For the most up-to-date information, please refer to the interactive fault map. Diamond Valley fault (Class A) No. 1161 Last Review Date: 2000-06-06 citation for this record: Anderson, R.E., compiler, 2000, Fault number 1161, Diamond Valley fault, in Quaternary fault and fold database of the United States: U.S. Geological Survey website, https://earthquakes.usgs.gov/hazards/qfaults, accessed 12/14/2020 02:17 PM. Synopsis The Diamond Valley fault is along the precipitous east-facing bedrock escarpment of the Sulphur Spring Range adjacent to Diamond Valley near the southeastern corner of the Winnemucca 1:250,000 map. It includes a subparallel 6-km-long fault along the east margin of Union Mountain in Elko County. The Sulphur Spring Range is an east-tilted structural block similar to many ranges in the region. The range is also a north-trending horst, and the Diamond Valley fault is the east-bounding structure of the horst. The precipitous, convex-eastward bedrock escarpment along the fault is little incised by transverse drainages, and generally lacks the faceted spurs and wineglass valleys that tend to characterize the geomorphology of major active range blocks. The fault probably juxtaposes Quaternary alluvium against bedrock, but fault scarps and (or) lineaments on Quaternary surficial deposits or erosion surfaces are apparently lacking. Name Modified from dePolo (1998 #2845), who applied the name comments Diamond Valley fault zone to a single-trace north-striking fault mapped by Dohrenwend and Moring (1991 #282) at the base of the precipitous east-facing bedrock escarpment of the Sulphur Spring Range adjacent to Diamond Valley. -
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. -
Paleozoic Rocks Antelope Valley Eureka and Nye Counties Nevada
:It k 'I! ' Paleozoic Rocks Antelope Valley Eureka and Nye Counties Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 423 Paleozoic Rocks of Antelope Valley Eureka and Nye Counties Nevada By CHARLES W. MERRIAM GEOLOGICAL SURVEY PROFESSIONAL PAPER 423 P,rinciples of stratigraphy applied in descriptive study of the Central Great Basin Paleozoic column UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Page Silurian system ____________________________________ _ Abstract------------------------------------------- 1 36 Introduction. _____________________________________ _ 2 General features-------------------------------- 36 Geologic setting ______________ ------ ___ --------- 2 Roberts Mountains formation ___________________ _ 37 History of investigation ________________________ _ 5 Lone Mountain dolomite ______ ---_-------------- 39 Purpose and scope _____________ -- ______ ------ --- 6 Devonian system ______________ ---- __ - _- ___ - _------- 41 Acknowledgments ______________________________ _ 6 General features _____________ - ___________ -_----- 41 Geologic structure as related to stratigraphy __________ _ 6 Western Helderberg age limestones of the Monitor Paleontologic studies ______ ..:. _______ ~ ________________ _ 9 · Range ______ - _.- ___ --------------------------- 42 The Paleozoic column at Antelope Valley -
President of the United States
.ME’SS.hGE PRESIDENT OF THE UNITED STATES, TRANSMITTIP;G A RmEPORT OF THE SECRETARY OF AGRICULTURE IN KEI,ATIOI\‘ TO THE l~ORESTS, lZI\‘lSltS, AND MOUNTAlNS OF THE SOlYl’HF,RN APPALACHIAN REGION. WASHINGTON: GOVERNMENT PRINTING OFFICE. 1902. 5% th,r SL')Lcttr and I-lonfW ofR~~~/,~~~sc)ltltli,'eS: I transmit herewith a report of the Secretary of Agriculture, pre- pared in collaboration with the Department of the Interior, upon the forests, rivers, and mountains; of the Southern L4ppalachian region, and upon its agricultural situation as affected by t’lem. The report of the Secretary presents t#he final results of an investigation authorized by the last Congress. Its conclusions point unmistakably, in the judg- ment of the Secretary and in my own, to the creation of a national forest reserve in certain lyarts of the Southern States. The facts ascer- tained and here presented deserve the careful consideration of the Congress; they have already received the full attention of the scientist and the lumberman. They set forth an economic need of prime impor- tance to the welfare of the South, and hence to that of the nation as a whole, and they point to the necessity of protecting t,hrough wise use a mountain region whose influence flows far beyond its borders with the waters of the rivers to which it gives rise. Among the elevations of the eastern half of t.he United States the Southern ;Lppalachians are of paramount interest for geographic, hydrographic, and forest reasons, and, as a consequence, for economic reasons as well. -
GEOLOGICAL SURVEY RESEARCH 1972 Chapter B
GEOLOGICAL SURVEY RESEARCH 1972 Chapter B GEOLOGICAL SURVEY PROFESSIONAL PAPER 800-8 Scientific notes and summaries of investigations in geology, hydrology, and related fields UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director For sale by the Superintendent of Documents, U.S. Qovernment Printing Office, Washington, D.C., 20402 - Price $2.26 CONTENTS GEOLOGIC STUDIES Marine geology Page Structural features of the continental margin, northeastern Gulf of Mexico, by R. G. Martin, Jr. Marine geology of Yakutat Bay, Alaska, by F. F. Wright . Paleontology and stratigraphy Leiosphaeridio (Acritarcha) in the Mesozoic oil shales of northern Alaska, by R. F. Boneham and I. L. Tailleur . Quartzsand-bearing zone and Early Silurian age of upper part of the Hanson Creek Formation in Eureka County, Nev., by T. E. MullensandF.G.Poole ................................................................................... Trend-surface analysis of the thickness of the High Bridge Group (Middle Ordovician) of central Kentucky and its bearing on the nature of the post-Knox unconformity, by D. E. Wolcott, E. R. Cressman, and J. J. Connor . Glacial geology The Ingraham esker, Chazy, N.Y ., by C. S. Denny . Economic geology High-purity veins of soda-niter, NaN03, and associated saline minerals in the Chilean nitrate deposits, by G. E. Ericksen and M. E. Mrose ................................................................................................. Thorium distribution in a ganite stock near Bull Canyon, Lemhi County, Idaho, by M. H. Staatz, C. M. Bunker, and C. A. Bush . White clay deposits of Centre, Blair, Huntingdon, and Bedford Counties, Pa., by J. W. Hosterman . Reconnaissance geology and mineral potential of Thomas, Keg, and Desert calderas, central Juab County, Utah, by D. -
Paleozoic Geology of the Dobbin Summit-Clear Creek Area, Monitor
AN ABSTRACT OF THE THESIS OF DIANE CAROL WISE for the degree of MASTER OF SCIENCE in Geology presented on August 13, 1976 Title: PALEOZOIC GEOLOGY OF THE DOBBIN SUMMIT- CLEAR CREEK AREA, MONITOR RANGE, NYiE COUNTY, NEVADA Abstract approved: Redacted for Privacy son Paleozoic limestones, dolomites, quartz arenites, and other clastic rocks were mapped in the vicinity of Dobbin Summit and Clear Creek in the central Monitor Range. Sedimentary rock units present in this area represent the shallow-shelf eastern assemblage and basin and also the basin-slope facies of the traditional limestone- clastic assemblage. The four oldest, Ordovician, units were deposited in shallow shelf environments. The Lower Ordovician Goodwin Formation is composed of about 1200 feet of calcareous shales and thin-bedded limestones. The overlying Antelope Valley Limestone is about 500 feet thick and consists of wackestones, packstones, and rare algal grainstones.The Copenhagen Formation (135 feet thick) is the highest regressive deposit of sandstone, siltstone, and limestone below the transgressive Eureka Quartzite.The Eureka is a quartz arenite 181 feet thick, with an intercalated shallow marine dolomite member. The transition from shallow to deep water conditions can be seen in the change from algal boundstones to laminated lime mud- stones in the Hanson Creek Formation (190 feet thick).The super- jacent Roberts Mountains Formation (285 feet thick) is composed of lime mudstones and allodapic beds deposited in basinal, deep water conditions.During earliest Devonian -
Final Report
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. Dobkin, High Desert Ecological Research Institute, Bend, Oregon (co-principal investigator) Brett G. Dickson, Conservation Science Partners, Truckee, California (co-principal investigator) ABSTRACT Prescribed fire and other fuels management treatments have been suggested as mechanisms to slow expansion of pinyon and juniper woodlands while minimizing potential expansion of cheatgrass (Bromus tectorum) and increasing habitat quality and quantity for Greater Sage- Grouse (Centrocercus urophasianus). These treatments also may reduce the probability of severe wildfires, which can have undesirable effects on social, economic, cultural, and ecological values. However, achieving long-term goals related to fire and fuels may conflict with short-term goals related to survival and viability of native species. Fire can fragment high-quality habitat for species associated with woodlands, including more than 20 native species of breeding birds. Additionally, expansion of pinyon and juniper woodlands may have been patchy but common and natural before European settlement of the Great Basin. Evaluation of spatial and temporal trade-offs of actions to reduce probability of wildfire, maintain sagebrush steppe, and conserve native species, including rare or endangered species, can identify strategies that are either consistent or incompatible with achieving these and other objectives simultaneously. We monitored use by Greater Sage-Grouse of areas treated with fire or proposed for treatment. -
A History of the Tonopah Area and Adjacent Region of Central Nevada, 1827-1941
A History of the Tonopah Area and Adjacent Region of Central Nevada, 1827-1941 A History of the Tonopah Area and Adjacent Region of Central Nevada, 1827-1941 A thesis presented to the Faculty of the Department of History UNIVERSITY OF NEVADA In partial fulfillment of the requirements for the degree MASTER OF ARTS by Lucile Rae Berg MAY 1942 with an introduction by Robert D. McCracken Nye County Press TONOPAH, NEVADA Published in 2011 by Nye County Press P.O. Box 153 Tonopah, Nevada 89049 Copyright © 2011 by Nye County Press All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording, or any information storage or retrieval system, without permission in writing from the publisher. ISBN 978-1-878138-04-0 DESIGN BY JANE RAESE Text set in ii-point Adobe Caslon Pro Frontispiece: Lucile Berg in her twenties, circa 1937. Courtesy Lucile R. Berg. Printed in the United States of America Contents Editor's Introduction Acknowledgments Map of South Central Nevada 1 General Description of Big Smoky, Reese River, Monitor, and Ralston Valleys Special Points of Interest Hot Springs Blue Spring Elephant Rock Diana's Bowl or Devil's Punch Bowl Northumberland Caves 2 Early Expeditions Through the Region Fremont's Third Expedition, 1845 Jedediah Smith, 1827 Captain J. H. Simpson, 1859 3 Early Mining Camps in the Region, 1860-1880: Northern Section Ione Ophir Canyon Last Chance, Hercules, and Summit Canyons Kingston Canyon Santé Fe Northumberland 4 -
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. -
STRATIGRAPHY and STRUCTURE of the SOUTHERN SULPHUR SPRING RANGE, EUREKA COUNTY, NEVADA Redacted for Privacy Abstract Approved: U G
AN ABSTRACT OF THE THESES OF Joseph T. Lipka IC for the degree ofMaster of Sciencein Geology presented on April 17, 1987 Title:STRATIGRAPHY AND STRUCTURE OF THE SOUTHERN SULPHUR SPRING RANGE, EUREKA COUNTY, NEVADA Redacted for Privacy Abstract approved: U G. Johnson Early Paleozoic limestones and dolomites of the shallow shelf transitional facies belt were mapped in the southern Sulphur Spring Range, Eureka County, Nevada.The four youngest units in the map area are in fault contact with the Lower Devonian rocks and wereprobably transported westward, along a low-angle normal fault. The minoirlal dolomites of the Hanson Creek Formation, dated as latest Ordovician in the map area, were deposited in a low-energy lagoon.Overlying the Hanson Creek Formation, with a gradational contact, is the lower member ofthe Lone Mountain Dolomite, a probable reef complex.The exposed thickness of the lower Lone Mountain Dolomite is estimated to be 250 feet.The Lower Devonian Old Whalen Member of the Lone Mountain Dolomite is composed of well-bedded, alternating brown and gray dolomites.The repetition of rock types in the Old Whalen Member indicates recurring shallow marine environments on a broad carbonate platform.The Old Whalen is estimated to be 1400 feet thick.Directly overlying the Old Whalen Member, is the Kobeh Member of the Mc Colley Canyon Formation.Rocks of the Mc Colley Canyon Formation were deposited on a shallow shelf under normal marine conditions.The mid-Lower Devonian Kobeh Member is sparsely to abundantly fosciliferous and varies from a peloidal wackestone to a peloidal sandy wackestone to a sandy peloidal packstone.The thickness is 276 feet.Overlying the Kobeh Member are the abundantly fossiliferous beds of the lower part of the Bartine.