Julia's Unequivocal Nevada Klampout
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Jarbidge Mountains (Updated 2014)
Site Description Jarbidge Mountains (updated 2014) Geologic setting: The Jarbidge Mountains are located within the northeastern portion of Elko County, Nevada. The small mountain range is located between the Copper Mountains to the west and the Snake mountains to the east and southeast. Basement rocks of the Jarbidge quadrangle include schist, quartzite, hornfels, and limestones. These are intruded by a Cretaceous quartz monzonite stock. The basement rocks are displaced along pre-Cretaceous faults. Cambrian and Precambrian rocks are thrust over and upon Paleozoic sedimentary rocks. The early Tertiary volcanics and conglomerates are displaced along normal faults represented by the Copper Creek fault, which dips gently east. The Jarbidge Rhyolite (Miocene) and all older formations are displaced along three sets of faults that dip steeply: one set strikes northward, one northeast, and one northwest. These three sets of faults are locally mineralized (Smith, 1976). The oldest exposures are sedimentary deposits such as limestones and shale towards the western portion of the area (Scott, 1910). Geothermal features: Gray Rock Mine: The Great Basin Groundwater Geochemical Database lists a measurement of 26.7°C in an abandoned mineshaft well in the Gray Rock Mine (Sec. 24, T45N, R58E). Robinson Hole Hot Spring / Murphy Hot Spring / Kitties Hot Hole: (Sec. 29, T47N, R59E) The first acknowledged proprietor was Kittie Wilkins, who diverted river water to create the Kittie’s Hot Hole soaking pool (1885). Patrick Murphy developed a small resort on the property in the early 1900’s and renamed it Murphy Hot Spring, followed by Harry Showalter, who added a swimming pool and changing rooms. -
Mountain City, Ruby Mountains, and Jarbidge Combined Travel
Mountain City, Ruby Mountains and Jarbidge Ranger Districts Combined Travel Management Project Environmental Impact Statement Chapter 3. Affected Environment and Environmental Consequences 3.1. Introduction This chapter summarizes the physical, biological, social, and economic environments that are affected by the alternatives and the effects on that environment that would result from implementation of any of the alternatives. This chapter also presents the scientif ic and analyt ical basis for comparison of the alternatives presented in chapter 2. 3.1.1. Analysis Process Most of the data used in the following analysis are from the Humboldt-Toiyabe National Forest corporate GIS layers. There is a certain amount of error in the location and alignments included in this GIS data. For example, the road layer overlying the stream layer may show more stream crossings than actually exist on the ground because of the different sources from which the different layers were obtained. Some perennial streams may show up on the map as being intermittent. This may also create some inaccuracies as to the exact location and extent of riparian zones. The Forest is constantly working to improve map accuracies and the corporate GIS layers. For the purposes of this analysis, the best data that is available was used. The data in the tables below and in the project record depict with a reasonable amount of accuracy what would be occurring on the ground for each alternative, within the limitations described above. The changes between alternatives remain relative to each other. 3.1.2. Cumulative Effects According to the Council on Environmental Quality (CEQ) National Environmental Protection Ac t (NEPA) regulations, “cumulative impact” is the impact on the environment which results from the incremental impact of the action when added to other past, present, and reasonably foreseeable future actions regardless of what agency (federal or non-federal) or person undertakes such actions (40 CFR 1508.7). -
A Traditional Use Study of the Hagerman
A TRADITIONAL USE STUDY OF THE I HAGERMAN FOSSIL BEDS NATIONAL MONUMENT L.: AND OTHER AREAS IN SOUTHERN IDAHO Submitted to: Columbia Cascade System Support Office National Park Service Seattle, Washington Submitted by: L. Daniel Myers, Ph.D. Epochs· Past .Tracys Landing, Maryland September, 1998 PLEASE RETURN TO: TECHNICAL INFORMATION CENTER DENVER SERViCE CENTER NATIONAL PARK SERVICE TABLE OF CONTENTS Table of Contents ii List of Figures and Tables iv Abstract v CHAPTER ONE: INTRODUCTION l OBJECTIVES l FRAMEWORK OF STUDY 2 STUDY AREAS 4 STUDY POPULATIONS 5 DESIGN OF SUCCEEDING CHAPTERS 5 CHAPTER TWO: PROTOCOL AND STRATEGIES. 7 OBJECTIVES 7 CONTACT WITH POTENTIAL CONSULTANTS 7 SCHEDULING AND APPOINTMENTS 8 QUESTIONNAIRE 8 INTERVIEW SPECIFICS 10 CHAPTER THREE: INTERVIEW DETAILS 12 OBJECTIVES 12 SELF, FAMILY, AND ANCESTORS 12 TRIBAL DISTRIBUTIONS AND FOOD-NAMED GROUPS 13 SETTLEMENT AND SUBSISTENCE 13 FOOD RESOURCES . 14 MANUFACTURE GOODS 15 INDIAN DOCTORS, MEDICINE, AND HEALTH 15 STORIES, STORYTELLING, AND SACRED PLACES 15 CONTEMPORARY PROBLEMS AND ISSUES 16 CHAPTER FOUR: COMMUNITY SUMMARIES OF THE FIRST TIER STUDY AREAS 17 OBJECTIVES 17 DUCK VALLEY INDIAN RESERVATION 17 FORT HALL INDIAN RESERVATION 22 NORTHWESTERN BAND OF SHOSHONI NATION 23 CHAPTER FIVE: COMMUNITY SUMMARIES OF THE SECOND TIER STUDY AREAS 25 OBJECTIVES 25 DUCK VALLEY INDIAN RESERVATION 25 ii TABLE OF CONTENTS Craters of the Moon 25 City of Rocks National Reserve and Bear River Massacre . 25 FORT HALL INDIAN RESERVATION 26 Craters of the Moon 26 City of Rocks . 28 Bear River Massacre ·28 NORTHWESTERN BAND OF SHOSHONI NATION 29 Craters of the Moon 29 City of Rocks . 29 Bear River Massacre 30 CHAPTER SIX: ASSESSMENT AND RECOMMENDATIONS 31 OBJECTIVES 31 SUMMARY REVIEW 31 STUDY AREAS REVIEW 3 3 RECOMMENDATIONS 3 5 REFERENCES CITED 38 ACKNOWLEDGEMENTS 41 APPENDIX A 43 APPENDIX B 48 APPENDIX C 51 iii LIST OF FIGURES AND TABLES Figure 1: Map of Southern Idaho showing Study Areas 3 Figure 2. -
Campgrounds BOUNDARY CO
CANADA o o South-Central Idaho Southwestern Idaho Northern Idaho Eastern Idaho o 117 116 49 o 49 Burley Area Bruneau Area Coeur d’Alene Area Challis Area Every Kid in the Park «¬ Castle Rocks State Park (SP) Bruneau Sand Dunes SP Beauty Bay Bayhorse 1 CS 29 61 BS £ ¤95 Hidden K CR City of Rocks SP 1 Poison Creek Picnic Site 30 Blackwell Island 62 Challis Bridge o Idaho Parks, Destinations Lake o t e n Upper a LW Lake Wolcott SP Greater Boise Area 31 Blue Creek Bay 63 Cottonwood i Priest Lake 119 Lud Drexler Reservoir Bonneville Point 32 Blue Creek Trail 64 Deadman Hole 2 and Campgrounds BOUNDARY CO R 120 McClendon Spring Celebration Park CM Coeur d' Alene Old Mission 65 East Fork i ver 18 Harrison Campground Priest ! Lake £2 Lake Bonners ¤ 3 Clay Peak 33 Crater Lake 66 Garden Creek Milner Historic Ferry 121 PL Recreation Area 19 Cove (CJ Strike Reservoir) 34 Crater Peak 67 Herd Lake Campsite ¤£95 122 Snake River Vista 20 Dedication Point FG Farragut 68 Herd Lake Overlook Twin Falls Area EI Eagle Island SP 35 Gamlin Lake YF Land of the Yankee Fork SP Chase Lake 123 Big Cottonwood 4 8th Street Trail HB Heyburn SP «¬57 69 Jimmy Smith BONNER CO 124 Bruneau Canyon Overlook 5 Lower Hulls Gulch 36 Huckleberry Campground Trailhead Kootenai Joe T. Fallini at ! 125 Bruneau River Launch Site 6 Upper Hulls Gulch 38 Killarney Lake Boat Launch 70 Blue Sandpoint System Trail Mackay Lake ! 126 Bruneau River Take-Out 7 Miller Gulch Ridge to Rivers 39 Killarney Lake Picnic Site Priest ¤£2 71 Little Boulder P 35 end River O 127 Cedar Creek Reservoir 21 -
Geologic Maps of the Grand View-Bruneau Area, Owyhee County, Idaho
Geologic Map of the Grand View-Bruneau Area, Owyhee County, Idaho Margaret D. Jenks Bill Bonnichsen Martha M. Godchaux Idaho Geological Survey Technical Report 98- 1 University of Idaho December 1998 Moscow, Idaho 83844-3014 Contents Introduction ............................................................... 1 Location ................................................................ 2 General Geologic Setting ........................................................ 2 Structure ................................................................ 5 Hotsprings ............................................................... 6 Acknowledgments ........................................................... 7 References ............................................................... 7 DescriptionofUnits .......................................................... 9 SedimentqUnits .......................................................... 9 Younger Unconsolidated Sediments ............................................... 9 Qal Alluvium (Holocene) .................................................. 9 Qil Intermittent lake sediments (Holocene) ......................................... 9 Qfs Fresh, unvegetated dune sand (Holocene) ....................................... 9 Qaf Alluvial fan deposits (Holocene and Pleistocene) ........................ :.............. 9 Qds Vegetated dune sand (Holocene and Pleistocene) ................................... 9 Qls Landslide deposits (Holocene and Pleistocene) .................................... 9 Qbf Bonneville -
Jarbidge River Distinct Population Segment of Bull Trout (Salvelinus Confluentus) Cover Illustration by Kendal Morris, U.S
U.S. Fish & Wildlife Service Draft Recovery Plan for the Jarbidge River Distinct Population Segment of Bull Trout (Salvelinus confluentus) Cover illustration by Kendal Morris, U.S. Fish and Wildlife Service; used with permission. Draft Recovery Plan for the Jarbidge River Distinct Population Segment of Bull Trout (Salvelinus confluentus) (May 2004) Region 1 U.S. Fish and Wildlife Service Portland, Oregon Approved: XXXXXXXXXXXXXXXXXXXXXXXXXXXXX Manager, California/Nevada Operations Office U.S. Fish and Wildlife Service Date: XXXXXXXXXXXXXXXXXXXXXXXXXXXXX Draft Recovery Plan for the Jarbidge River Distinct Population Segment of Bull Trout DISCLAIMER Recovery plans delineate reasonable actions which are believed to be required to recover and/or protect listed species. Plans are published by the U.S. Fish and Wildlife Service, and, in this case, with the assistance of recovery teams, State, Federal, and Tribal agencies, and others. Objectives will be attained and any necessary funds made available subject to budgetary and other constraints affecting the parties involved, as well as the need to address other priorities. Recovery plans do not necessarily represent the views or the official positions or approval of any individuals or agencies involved in the plan formulation, other than the U.S. Fish and Wildlife Service. Recovery plans represent the official position of the U.S. Fish and Wildlife Service only after they have been signed by the Director, Regional Director, or Manager, as approved. Approved recovery plans are subject to modification as dictated by new findings, changes in species status, and the completion of recovery actions. Literature citation of this document should read as follows: U.S. -
How Safe Is Idaho's Pipeline Network?
Exploring Idaho one step, cast, curve and vista at a time. Changes are in the works as IOJ ex- pands its coverage Winter studies The Clearwater and distribution track wolverine and Country has a lot across the state. human behavior. to offer visitors. page3 page5 page9 Volume 1. No. 8 MAY 2012 FREE A look inside STATE How safe is Idaho’s pipeline network? Idaho Biking News will By Mike McLaskey According to PHMSA, provide Idaho’s active biking “the nation’s pipelines are a community with news and BOISE — There is a vast transportation system,” and information about biking and little known-about net- this complex network “deliv- activities across the state. work of natural gas and ers trillions of cubic feet of PAGE 3 petroleum pipelines that run natural gas and hundreds of Ashton Dam repair update. throughout the country. billions of ton/miles (a unit To postpone the draw down, Over two million miles of of freight transportation as some have suggested, pipeline carry crude oil and equivalent to a ton of freight would push the work into natural gas 24 hours a day, moved one mile) of liquid next year, requiring yet seven days a week all over petroleum products each year.” another draw down. the country and Idaho has This network is essential PAGE 4 70,000 miles in that network. because the country’s vast Panhandle trout decisions Regulation and upkeep size makes any other means loom and it was standing of these pipelines is in the of distributing these energy room only at the Coeur hands of the Pipeline and resources cost-prohibitive. -
Bruneau River
Bruneau River General Information The headwaters of the Bruneau River are in northeast Nevada on the Humbolt National Forest. The river flows northward into Idaho and eventually confluences with the Snake River. The study area includes two river reaches and is associated with U.S. Geological Survey gaging station (13161500), which is located about 0.5 mi. upstream from Rowland, Nevada. The site is at an elevation of about 4,500 ft. The drainage area upstream of the gage is 382 mi2 and the geology of the watershed is mixed with the dominant material being sedimentary and volcanic extrusive. Streamflow records are available from June 1, 1913 to September 30, 1918 and October 1, 1966 to present (Water Year 2012). Sediment transport measurements are available for water years 1998, 1999, 2000 and 2002. Additional information collected includes a 1998 survey of a stream reach and pebble counts of the surface bed material in 1998 and 2000. Figures 1 and 2 show photographs of the reach surveyed in 1998. Figure 1. Bruneau River looking upstream from the downstream end of the surveyed reach. Figure 2. Bruneau River looking downstream from the upstream end of the surveyed reach. Streamflow records are available for 52 complete water years. The average 3 annual streamflow (Qa) for the period of record is 110 ft /s (3.8 in). During the period of record, daily mean discharges ranged from 1.7 ft3/s to 2,070 ft3/s. The highest instantaneous discharge recorded was 2,140 ft3/s on May 14, 1984. Page |2 Channel Profile and Cross-Section The surveyed river segment is about 890 ft. -
Jarbidge River Watershed Analysis
JARBIDGE RIVER WATERSHED ANALYSIS JARBIDGE RANGER DISTRICT HUMBOLDT-TOIYABE NATIONAL FORESTS ANALYSIS CORE TEAM: MICHAEL E. MCNEILL, TEAM LEADER JAY FREDERICK, BIOLOGIST BONNIE WHALEN, GIS SUPPORT SPECIALIST TEAMMEMBERS: Chris Butler, Hydrologist Fred Frampton, Archaeologist Kathy Ramsey, Fish Biologist· Additional Inputprovided by: Gary Johnson, Nevada Division of Wildlife, Region II Jim K1ott, Jarbidge Resource Area, Idaho .BLM Bruce ZoeUick,Idaho State BLM JARBIDGE CANYON WATERSHED ANALYSIS TABLE OF CONTENTS CHAPTER ONE - CHARACTERIZATION OF THE WATERSHED Introduction . Page 1-1 Physical Setting Page 1-2 Geology Page 1-3 Soils Page 1-4 Disturbance Page 1-5 Biological Processes and Human Influence Page 1-5 CHAPTER TWO - /DENT/FICA T/ON OF ISSUES AND KEY QUESTIONS Key Questions Page 2-1 CHAPTER THREE - DESCRIPTION OF CURRENT CONDITIONS Stream Order Page 3-1 Hydrologic Regime Page 3-1 Headwater Morphology Page 3-1 Valley Bottom Morphology Page 3-1 Channel Morphology Page 3-2 Substrate Page Width/Depth Ratio Page 3-5 Pools and large Wood 3-5 Water Quality· Page 3-7 Heavy Metals Page 3-7 Temperature Page 3-7 Other Water Quality Concerns Page 3-10 Soils Page 3-10 Vegetation Page 3-10 Riparian Vegetation Page 3-12 Macros Page 3-12 CHAPTER FOUR - DESCRIPTION OF REFERENCE CONDITIONS Biological Processes and Human Influence . Page 4-1 Beaver Page 4-1 Livestock Page 4-2 Mining Page 4-5 Mining and Water quality Page 4-5 Temperature Page 4-6 Roads Page 4-6 Vegetation Page 4-7 Channel Morphology Page 4-8 CHAPTER FIVE - SYNTHESIS AND INTERPRETATION OF INFORMATION Summary Page 5.1 CHAPTER SIX - RECOMMENDATIONS Recommendations Page 6.1 Data Shortcomings Page 6.2 DATA CHARTS AND GIS OVERLAYS Data Charts: Geologic Formations Figure 1.2' Valley Boltom Gradient Figure 3.1 Stream Reach. -
Owyhee Monument Proposal Legacy Landscape
Legacy Landscape O v e r v i e w Preface here the remote corners of Idaho, Oregon and Nevada come together lies one of the most unique and spectacular high desert areas remaining in the continental United WStates. This region, known as the Owyhee - Bruneau Canyonlands, represents one of the last best examples of the wide-open country which once characterized the American West. Consisting of high sagebrush and grassland plateaus incised by deep, sheer-walled river canyons and mountains dominated by juniper woodlands, the Owyhee-Bruneau Canyonlands stretch across an area twice the size of Yellowstone National Park. Home to some of the nation’s rarest fish, wildlife, and plant species, scientific assessments have rated the region one of the most bio- logically rich and diverse high deserts in the country. Humans have been part of the Owyhee country for over 15,000 years—resulting in the richest concentration of archaeological sites in Idaho. It is also one of the greatest contiguous landscapes of historical and cultural significance in the West. The unique geologic, biologic, and historic resources of the Owyhee-Bruneau Canyonlands lend the region to protection as a national monument under the Antiquities Act. This docu- ment was prepared to compile the wide range of scientific information identifying the national- ly significant values of this land and to put forth the argument for monument designation. Focusing on the geology, paleontology, landscape ecology, biology, archaeology, history, and cul- ture of the Owyhee-Bruneau Canyonlands, this document also presents a picture of the threats posed to these values and the landscape as a whole. -
Snake River Basin, Idaho
DEPAETMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIBECTOB WATER-SUPPLY PAPER 347 PROFILE SURVEYS IN SNAKE RIVER BASIN, IDAHO PREPARED UNDER THE DIRECTION OF R. B. MARSHALL, CHIEF GEOGRAPHER WASHINGTON GOVERNMENT PRINTING OFFICE 1914 CONTENTS. Page. General features of Snake River basin....................................... 5 Gaging stations............................................................ 7 Publications.............................................................. 12 ILLUSTRATIONS. PLATE I. A-S, Plan and profile of Snake River from Enterprise to Minidoka, Idaho............................................ At end of volume. II. A-L, Plan and profile of Salmon River from Salmon to Riggins and Little Salmon River from Riggins to Meadows, Idaho. At end of volume. III. A-F, Plan and profile of Salmon River from Riggins to Snake River, Idaho ............................................ At end of volume. 3 PROFILE SURVEYS IK SNAKE RIYER BASIN, IDAHO. Prepared under the direction of R. B. MARSHALL, Chief Geographer. GENERAL FEATURES OP SNAKE RIVER BASIN. Snake River, the largest tributary of the Columbia, rises among the high peaks of the Rocky Mountains in Yellowstone National Park, heading in the divide from which streams flow northward and eastward into the Missouri, southward to the Colorado and the lakes of the Great Basin, and westward to the Columbia. From the head water region, including Shoshone, Lewis, and Heart lakes, in Yellow- stone National Park, the river flows southward, broadening into -
Distribution and Movement of Bull Trout in the Upper Jarbidge River Watershed, Nevada
Prepared in cooperation with the U.S. Fish and Wildlife Service Distribution and Movement of Bull Trout in the Upper Jarbidge River Watershed, Nevada Open-File Report 2010-1033 U.S. Department of the Interior U.S. Geological Survey Distribution and Movement of Bull Trout in the Upper Jarbidge River Watershed, Nevada By M. Brady Allen, Patrick J. Connolly, Matthew G. Mesa, Jodi Charrier, and Chris Dixon Prepared in cooperation with the U.S. Fish and Wildlife Service Open-File Report 2010–1033 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2010 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Suggested citation: Allen, M.B., Connolly, P.J., Mesa, M.G., Charrier, Jodi, and Dixon, Chris, 2010, Distribution and movement of bull trout in the upper Jarbidge River watershed, Nevada: U.S. Geological Survey Open-File Report 2010-1033, 80 p. Any use of trade, product, or firm names 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.