Mineral Resources of the Little Humboldt River Wilderness Study Area, Elko County, Nevada

Total Page:16

File Type:pdf, Size:1020Kb

Mineral Resources of the Little Humboldt River Wilderness Study Area, Elko County, Nevada Mineral Resources of the Little Humboldt River Wilderness Study Area, Elko County, Nevada U.S. GEOLOGICAL SURVEY BULLETIN 1732-B Chapter B Mineral Resources of the Little Humboldt River Wilderness Study Area, Elko County, Nevada By ALAN R. WALLACE, ROBERT L TURNER, V.J.S. GRAUCH, JOSEPH L. PLESHA, M. DENNIS KROHN, and JOSEPH S. DUVAL U.S. Geological Survey PETER N. GABBY U.S. Bureau of Mines U.S. GEOLOGICAL SURVEY BULLETIN 1732 MINERAL RESOURCES OF WILDERNESS STUDY AREAS LITTLE HUMBOLDT RIVER REGION, 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 Little Humboldt River wilderness study area, EIko County, Nevada. (U.S. Geological Survey bulletin ; 1732) (Mineral resources of wilderness study areas Little Humboldt River Region, Nevada ; ch. B) (Studies related to wilderness) Bibliography: p. Supt. of Docs, no.: I 19.3:1732-8 1. Mines and mineral resources Nevada Little Humboldt River Wilderness. 2. Little Humboldt River Wilderness (Nev.) I. Wallace, Alan R. II. Series. III. Series: Mineral resources of wilderness study areas Little Humboldt River Region, Nevada ; ch. B. IV. Series: Studies related to wilderness wilderness areas. QE75.B9 no. 1732-B 557.3 S [553'.09793'16] 87-600393 [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. Results must be made available to the public and be submitted to the President and the Congress. This report presents the results of a mineral survey of a part of the Little Humboldt River Wilderness Study Area (NV-010-132), Elko County, Nevada. CONTENTS Summary Bl Abstract Bl Character and setting Bl Resources Bl Introduction B3 Investigations by the U.S. Bureau of Mines B5 Investigations by the U^S. Geological Survey B5 Appraisal of identified resources B5 Mining and prospecting history B5 Mines, prospects, claims, and mineralized areas B6 CR claim group B6 Snow claim group B7 JMC and Red claim groups B7 Other metallic mineral occurrences B7 Diatomite occurrence B7 Zeolite occurrences B8 Recommendations for further work B8 Assessment of potential for undiscovered resources B8 Geologic setting B8 Volcanic and volcaniclastic rocks B9 Surficial deposits BIO Structure BIO Geochemistry BIO Methods BIO Geochemical results BIO Geophysics Bll Gravity and aeromagnetics Bll Remote sensing Bll Aerial gamma-ray spectroscopy B14 Mineral and energy resources B14 Disseminated gold deposits B14 Deposit characteristics B14 Resource potential B15 Brush Creek area B15 Snowstorm Creek area B15 Areas adjacent to the South Fork of the Little Humboldt River B17 Additional areas B17 Zeolites B18 Barite B18 Tin B18 Other metals B18 Geothermal energy B19 Oil and gas B19 Sand and gravel B19 Contents References cited B19 Appendix B21 PLATE [Plate is in pocket] 1. Mineral resource potential and geologic map of the Little Humboldt River Wilderness Study Area FIGURES 1. Summary map showing mineral resource potential of the Little Humboldt River Wilderness Study Area B2 2. Index map showing the location of the Little Humboldt River Wilderness Study Area B4 3. Complete Bouguer anomaly map of the Little Humboldt River Wilderness Study Area and vicinity B12 4. Total-field aeromagnetic map of the Little Humboldt River Wilderness Study Area and vicinity B13 5. Map showing areas of possible hydrothermally altered rocks outlined on the basis of spectral analysis of Landsat Thematic Mapper (TM) color-ratio com­ posite images, Little Humboldt River Wilderness Study Area B16 VI Contents MINERAL RESOURCES OF WILDERNESS STUDY AREAS- LITTLE HUMBOLDT RIVER REGION, NEVADA Mineral Resources of the Little Humboldt River Wilderness Study Area, Elko County, Nevada By Alan R. Wallace, Robert L Turner, V.J.S. Grauch, Joseph L Plesha, M. Dennis Krohn, and Joseph S. Duval U..S. Geological Survey Peter N. Gabby U.S. Bureau of Mines SUMMARY trending mountains that are separated by broad valleys filled with alluvium. In the transition zone between the two Abstract terranes, the volcanic rocks partly to completely cover the older rocks. The Little Humboldt River Wilderness Study Area The wilderness study area is underlain by a complex, (NV-010-132) in northern Nevada is underlain by faulted interlayered sequence of volcanic rocks that were erupted volcanic rocks. The study area has no identified mineral between about 10 and 15 m.y. (million years) ago. The resources (fig. 1). Numerous mining companies are actively oldest rocks are rhyolitic flows and tuffs and lesser amounts exploring for gold in and around the wilderness study area. of ash-rich sedimentary rocks and andesitic flows, dikes, Different parts of the area have a high, medium, or low and tuffs. These rocks were cut by steep faults that mineral resource potential for disseminated gold deposits produced a large, north-trending basin. Ash-flow tuffs were and zeolites. Some areas have an unknown mineral erupted into this basin as it developed, forming the resource potential for bedded barite and disseminated gold widespread tuff of the Little Humboldt River. Subsequently, in rocks beneath the volcanic cover. The entire study area widespread shallow lakes covered surrounding areas, and has a low resource potential for uranium and thorium, large volumes of crystal-rich rhyolitic flows were erupted just diatomite, tin, arsenic, antimony, silver, and mercury, oil and west of the wilderness study area. About 10 m.y. ago, basalt gas, geothermal energy, and sand and gravel. flows were erupted near the northeastern edge of the study area. Active faulting during volcanic activity produced a Character and Setting complex relation between volcanic units and various fault systems. The Little Humboldt River Wilderness Study Area includes 40,000 acres (66 square miles) in western Elko Resources County, northern Nevada (fig. 2). It occupies a broad, sage-covered upland basin surrounded on the west, south, Different parts of the study area have a high, medium, and east by ridges. The study area can be reached by good or low resource potential for disseminated gold deposits and to very poor dirt roads from the south, west, and north. for zeolites in tuffaceous sedimentary rocks (fig. 1). The Elevations range from 5,079 ft (feet) to 7,266 ft, and the study area does not have any identified mineral resources. South Fork of the Little Humboldt River has incised a narrow Altered and fractured rocks, numerous quartz veinlets, canyon that longitudinally bisects the wilderness study area. and geochemical anomalies indicate that some of the older The study area is between the predominantly volcanic volcanic rocks at the southeast end of the study area near Snake River Plain volcanic province to the north and the Brush Creek and along the western margin near Snowstorm structurally complex Basin and Range province to the south. Creek have a high resource potential for disseminated gold Faulted and deformed older sedimentary and igneous rocks deposits. An area along the South Fork of the Little in the Basin and Range province are exposed in north- Humboldt River was hydrothermally mineralized and has a Little Humboldt River Wilderness Study Area B1 117°00' 116°45' I To Paradise Valley RODEAR FLAT (38 miles) i*» M/B(2) APPROXIMATE BOUNDARY OF THE LITTLE HUMBOLDT RIVER WILDERNESS STUDY AREA (NV-010-132) L/C (1) PPROXIMATE v BOUNDARY OF SNOW CLAI GROUP APPROXIMATE BOUNDARY OF CR CLAIM GROUP 41° 15' (45 miles) Figure 1 (above and facing page). Summary map showing mineral resource potential of the Little Humboldt River Wilderness Study Area, Elko County, Nev. B2 Mineral Resources of Wilderness Study Areas Little Humboldt River Region, Nevada EXPLANATION The study area has a low resource potential for [Except for parts of study area designated below as having high or mod­ uranium and thorium, oil and gas, diatomite, tin, arsenic, erate potential for commodity 2. the study area has a low mineral resource silver, mercury, and antimony, geothermal energy, and sand potential for commodity 2 (certainty level D). Entire study area has a low and gravel. The underlying pre-volcanic sedimentary rocks mineral resource potential for tin, uranium and thorium, sand and gravel have an unknown resource potential for bedded sedimen­ and oil and gas (certainty level D) and for arsenic, antimony, mercury, tary barite deposits as well as carbonate-hosted dissemi­ silver, geothermal energy, and diatomite (certainty level C)] nated gold deposits. Geologic terrane having a high mineral re­ source potential for commodity 1 (cer­ tainty level C or D) or for commodity 2 (certainty level D) Commodity shown on INTRODUCTION figure by number in parentheses Geologic terrane having a moderate mineral That portion of the Little Humboldt River resource potential for commodity 1 (cer­ Wilderness Study Area (NV-010-132) evaluated for tainty level C) or for commodity 2 (cer­ mineral resources and mineral resource potential, tainty level B) Commodity shown on figure hereafter referred to as the "wilderness study area"or by number in parentheses simply the "study area," covers 40,000 acres in western L/C Geologic terrane having a low mineral re­ Elko County, Nev. It is 50 mi (miles) northeast of source potential for commodity 1 (cer­ tainty level C) Commodity shown on figure Winnemucca, 50 mi north of Battle Mountain, and 5 mi by number in parentheses north of the small hamlet of Midas. Good to extremely poor dirt roads provide access to the north, west, and U/A Geologic terrane having an unknown mineral resource potential for commodity 1 (applies south sides; these roads connect with graded county to all parts of study area not designated as roads that lead west to Paradise Valley and south to having high, moderate, or low potential for Interstate Highway 80.
Recommended publications
  • Elko County Nevada Water Resource Management Plan 2017
    Elko County Nevada Water Resource Management Plan 2017 Echo Lake - Ruby Mountains Elko County Board of Commissioners Elko County Natural Resource Management Advisory Commission December 6, 2017 Executive Summary The Elko County Water Resource Management Plan has been prepared to guide the development, management and use of water resources in conjunction with land use management over the next twenty-five (25) years. Use by decision makers of information contained within this plan will help to ensure that the environment of the County is sustained while at the same time enabling the expansion and diversification of the local economy. Implementation of the Elko County Water Resource Management Plan will assist in maintaining the quality of life enjoyed by residents and visitors of Elko County now and in the future. Achievement of goals outlined in the plan will result in water resources found within Elko County being utilized in a manner beneficial to the residents of Elko County and the State of Nevada. The State of Nevada Water Plan represents that Elko County will endure a loss of population and agricultural lands over the next twenty-five years. Land use and development patterns prepared by Elko County do not agree with this estimated substantial loss of population and agricultural lands. The trends show that agricultural uses in Elko County are stable with minimal notable losses each year. Development patterns represent that private lands that are not currently utilized for agricultural are being developed in cooperation and conjunction with agricultural uses. In 2007, Elko County was the largest water user in the State of Nevada.
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Ground-Water Resources-Reconnaissance Series Report 20
    - STATE OF NEVADA ~~~..._.....,.,.~.:RVA=rl~ AND NA.I...U~ a:~~::~...... _ __,_ Carson City_ GROUND-WATER RESOURCES-RECONNAISSANCE SERIES REPORT 20 GROUND- WATER APPRAISAL OF THE BLACK ROCK DESERT AREA NORTHWESTERN NEVADA By WILLIAM C. SINCLAIR Geologist Price $1.00 PLEASE DO NOT REMO V~ f ROM T. ':'I S OFFICE ;:: '· '. ~- GROUND-WATER RESOURCES--RECONNAISSANCE SERIES .... Report 20 =· ... GROUND-WATER APPRAISAL OF THE BLACK ROCK OESER T AREA NORTHWESTERN NEVADA by William C. Sinclair Geologist ~··· ··. Prepared cooperatively by the Geological SUrvey, U. S. Department of Interior October, 1963 FOREWORD This reconnaissance apprais;;l of the ground~water resources of the Black Rock Desert area in northwestern Nevada is the ZOth in this series of reports. Under this program, which was initiated following legislative action • in 1960, reports on the ground-water resources of some 23 Nevada valleys have been made. The present report, entitled, "Ground-Water Appraisal of the Black Rock Desert Area, Northwe$tern Nevada", was prepared by William C. Sinclair, Geologist, U. s. Geological Survey. The Black Rock Desert area, as defined in this report, differs some~ what from the valleys discussed in previous reports. The area is very large with some 9 tributary basins adjoining the extensive playa of Black Rock Desert. The estimated combined annual recharge of all the tributary basins amounts to nearly 44,000 acre-feet, but recovery of much of this total may be difficult. Water which enters into the ground water under the central playa probably will be of poor quality for irrigation. The development of good produci1>g wells in the old lake sediments underlying the central playa appears doubtful.
    [Show full text]
  • The History of Water Law in Nevada Is
    Richard W. Harris, Esq. – Harris & Thompson he history of water law in Nevada is certificated water right can be lost through enough for mining activities. A dewatering closely tied to the state’s mining five years of non-use, but the Nevada operation of this magnitude poses several Thistory. Nevada’s first water law, in Supreme Court has held that there can be technical problems, including conflicts the form of custom and practice, arose in no forfeiture without a showing of intent with existing surface and groundwater conjunction with mining activities on the to abandon. rights, disposal of mine waters, and long- Comstock Lode and other gold and silver term environmental impacts. Curiously, although surface and camps. The doctrine of prior underground waters are both administered Mine dewatering and consumptive uses appropriation, or “first in time, first in by the same agency, there is a regulatory (such as dust control, evaporation from right,” became the guiding principle for disconnection between the two regimes. ponds, and loss of process fluids) can both surface water and groundwater. The Most of Nevada is divided into distinct have a substantial impact on existing customs of the miners, as well as hydrographic basins by its unique Basin users within the same hydrologic basin. ranchers, were formalized in the General and Range geology. There are few rivers The cone of depression can reach two Water Law Act of 1913 with the creation that flow continuously during the year, miles in diameter. The OSE is required of a permit system supervised by the and the water resources of most basins are by law to evaluate the impacts of these Office of the State Engineer (OSE).
    [Show full text]
  • AIR POLLUTION PROTECTION of LAKE TAHOE Construction
    CHAPTER 445 WATER CONTROLS; AIR POLLUTION PROTECTION OF LAKE TAHOE Construction Generally 445.010 Definitions. 445.011 "Breakwater" defined. __ 445.012 "Commercial construction" defined. 445.013 "Division" defined. 445.01-4 "Fills" defined. 445.015 "Lake Tahoe Watershed" defined. 445.016 "Pier" defined. 445.017 "Shoreline protection" defined. 445.018 "Single-family residence" defined. 445.019 Construction permit required. 4 45.020 Permits for construction of residences. 445.021 Permits for commercial or public construction. 445.022 Request for permit: information required. 445.023 Objections to permit. 445.024- Expiration, renewal of permit. 445.025 Inspection of the site* 445.026' Subdivision plans. 445.027 Land subdivided prior to 1949. 445.028 Shoreline and alteration appurtenances. 445.029 Minor repairs, alterations and protection of property, 445.030 Reference guides for construction. 445.031 Community water supply and sewage disposal. 445.032 Approval of installation of water supply and sewage disposal, systemsi. 445. 033", 3'P^c^b-jtteC'^^selUiil^i'i'.' 445.034 . Marineioilets. • 445.035;. Var^iaiiGes;.: ' Permits to Construct Piers, Breakwaters or Mooring: Buoys 44 5.040 . Definitions. 445.041 . "Breakwater" defined. 445.042 "Commercial use" defined. 445.043 \"Department" defined. 445.044 "Director" defined. 445.045 "Dredging" defined. 445.046 "Fill" defined. 445-i 445.047 "Floating dock or platform" defined. 445.048 "Industrial use" defined. " 445.049 "Littoral parcel" defined. 445.050 "Multiple use" defined. 445.051 "Navigational structure" defined. 445.052 "Permit" defined. 445.053 "Person" defined. 445.054 "Pier" defined. 445.055 "Salvage" defined. 445.056 Application for permit; duration of permit. 445.057 Purposes for which permits may be issued; types of permits.
    [Show full text]
  • Battle Mountain!
    Western hospitality at it s finest! Welcome to Battle Mountain, Nevada! Battle Mountain sits near the geographic center of the state, which also lies in Lander County. With access from the north, south, east and west, Battle Mountain provides a halfway point to just about everywhere you need to be in the state. Battle Mountain is in the heart of one of the world's richest gold-producing areas, and is home to several active gold mines. While the modern mining industry is important, holding equal prominence in the hearts and minds of residents is the history that made us great - the Western Shoshone Native Americans, Basque sheepherders and cattle ranchers have made their home in our area. Once famous for its quality turquoise mines, the battle Mountain areas still offers plenty of opportuni- ties for aspiring miners to discover a treasure trove of surprises. towards the small community of Austin. In late sum- Battle Mountain is the perfect access point to liter- mer, the town shifts gears with old time country flair, ally hundreds of miles of back-country roads and as the the Mountain Music Festival fills the air with trails. The area offers unlimited outdoor recreation bluegrass musicians from around the west, and the with year-round access to public lands. Visitors and town holds a country fair and harvest festival. residents alike enjoy fishing, hunting and 4-wheeling. Visitors to Battle Mountain will enjoy an area One of the highlights of the hunting season is the filled with Old West stories, wildlife, mountains, annual Chukar Tournament and feed.
    [Show full text]
  • NEVADA CALIF Ecogroup.Indd
    Eastern Sierra Eastern Sierra Humboldt-Toiyabe National Forest Scattered pieces of a national treasure where adventures come together H U M B O L D T - T O I Y A B E N A T I O N A L F O R E S T USDA Department of Agriculture • Forest Service Intermountain Region • Ogden, Utah Bridgeport Ranger District’s Hoover Wilderness in eastern California 23.260.419.01/01 Humboldt-Toiyabe National Forest WHERE ADVENTURES COME TOGETHER Santa Rosa Ranger District’s Santa Rosa Peak Spring Mountains National Recreation Area’s Mummy Mountain Hoover Wilderness he Humboldt-Toiyabe’s spectacular 6.3 million acres make up the largest national forest in the lower 48 states. TTen distinctive ranger districts are scat- tered like an intriguing puzzle across Nevada and a small portion of eastern California. Each piece contains its own unusual features, which offer unlimited rec- reation. The ranger districts vary from hardy “desert scapes” to snow-capped mountains with lush alpine meadows and timbered canyons. A world of discovery Indian Paintbrush awaits those who explore the Forest’s rich historic past. The following page displays the districts and lists numbers and web- sites. Bristlecone pine: one of the oldest known living tree species. Ruby Mountains Ranger District’s Echo Canyon Bridgeport Ranger District’s East Lake in the Hoover Wilderness Contacts . Scattered pieces of a national treasure: Humboldt Toiyabe Headquarters (Sparks) ................................ 775-355-5301 www.fs.fed.us/r4/htnf/ Carson Ranger District (Carson City) .................................. 775-882-2766 bringing it all together . Bridgeport Ranger District (Bridgeport, CA) .....................
    [Show full text]
  • Trends in Streamflow on the Humboldt River Between Elko and Imlay, Nevada, 1950–99
    Prepared in cooperation with the Nevada Department of Conservation and Natural Resources Trends in Streamflow on the Humboldt River between Elko and Imlay, Nevada, 1950–99 Scientific Investigations Report 2005-5199 U.S. Department of the Interior U.S. Geological Survey FRONT COVER: Photographs of Humboldt River at Blossom bridge near Valmy, Nevada, upstream of the streamflow gage at Comus. Top photograph is from the bridge looking downstream on June 9, 1999 during high flow. Bottom photograph is from the bridge looking downstream on October 18, 2001 during a period of no flow. Photographs taken by D.E. Prudic. Trends in Streamflow on the Humboldt River between Elko and Imlay, Nevada, 1950–99 By David E. Prudic, Richard G. Niswonger, and Russell W. Plume Prepared in cooperation with the NEVADA DEPARTMENT OF CONSERVATION AND NATURAL RESOURCES Scientific Investigations Report 2005–5199 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Carson City, Nevada: 2006 For sale by U.S. Geological Survey, Information Services Box 25286, Denver Federal Center Denver, CO 80225 For more information about the USGS and its products: Telephone: 1-888-ASK-USGS World Wide Web: http://www.usgs.gov/ Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report.
    [Show full text]
  • Moving Forward in the Humboldt River Basin
    UPDATE ON PROGRAMS AND ACTIVITIES OF THE HUMBOLDT RIVER BASIN WATER AUTHORITY Nevada Legislature’s Interim Committee on Public Lands July 26, 2018 Jeff Fontaine Executive Director Humboldt River Basin Water Authority AGENDA ITEM XIII - LANDS Meeting Date: 07-26-18 Overview of Humboldt River Basin Water Authority Established in 1995 by Elko, Eureka, Lander, Humboldt and Pershing Counties Organized to Oppose Proposal to Export in Excess of 300,000 acre feet of Groundwater from the Upper Humboldt River Basin to the Lower Carson River Basin (EcoVision Project) EcoVision Water Right Applications Denied By Nevada State Engineer As Speculative In Nature Fifteen-member Board of Directors; 3 appointed by each member county commission; includes at least one county commissioner from each member county; NMA representative appointed as non-voting member For Past 22 Years 15-Member HRBWA Board of Directors Have Continued to Meet Quarterly to Address Water Resource Issues of Concern 2 Major Roles and Responsibilities Recognize and protect all existing decreed and certificated water rights Identify and seek to resolve inter-county water allocation and management issues Formulate positions for presentation to relevant local, state, and federal agencies Monitor water supply and demand within the Basin Monitor the extent to which proposals to develop and export Humboldt River Basin water may adversely affect the water balance for member counties within the Authority Recommend appropriate federal and state legislation for the management of surface
    [Show full text]
  • 1969 Annual Report of the Chief of Engineers on Civil Works Activities
    DEs -Nor CnUAJI N~eF ~)1A 1969 Annual Report of The Chief of Engineers on Civil Works Activities Department of the Army '.Corps of Engineers Volume H forL4 INDEX FISCAL YEAR 1969 PROPERTY o U. s. Agg I[RT4 INDEX The following abbreviations are used in the index: BERH Board of Engineers for Rivers and Harbors NPP Portland, Oreg., District CDC California Debris Commission NPS Seattle, Wash., District CERC Coastal Engineering Research Center NPW Walla Walla, Wash., District LMK Vicksburg, Miss., District ORD Ohio River Division LMM Memphis, Tenn., District ORH Huntington, W. Va., District LMN New Orleans, La., District ORL Louisville, Ky., District LMS St. Louis, Mo., District ORN Nashville, Tenn., District MR&T Mississippi River and Tributaries Project ORP Pittsburgh, Pa., District MRK Kansas City, Mo., District POD Pacific Ocean Division MRO Omaha, Nebr., District SAJ Jacksonville, Fla., District NAB Baltimore, Md., District SAM Mobile, Ala., District NAN New York, N.Y., District SAN Charleston, S.C., District NAO Norfolk, Va., District SAS Savannah, Ga., District NAP Philadelphia, Pa., District SAW Wilmington, N.C., District NCB Buffalo, N.Y., District SPK Sacramento, Calif., District NCC Chicago, Ill., District SPL Los Angeles, Calif., District NCE Detroit, Mich., District SPN San Francisco, Calif., District NCL U.S. Lake Survey SWA Albuquerque, N. Mex., District NCR Rock Island, Ill., District SWG Galveston, Tex., District NCS St. Paul, Minn., District SWL Little Rock, Ark., District NED New England Division SWT Tulsa, Okla., District NPA Alaska District A Algoma Harbor, Wis. (NCC) 908 Alhambra Creek, Calif. (SPN) 1057 Abbapoola Creek, S.C. (SAN) 287 Alhambra Wash, Calif.
    [Show full text]