Climate Change Vulnerability and Adaptation
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Porphyry and Other Molybdenum Deposits of Idaho and Montana
Porphyry and Other Molybdenum Deposits of Idaho and Montana Joseph E. Worthington Idaho Geological Survey University of Idaho Technical Report 07-3 Moscow, Idaho ISBN 1-55765-515-4 CONTENTS Introduction ................................................................................................ 1 Molybdenum Vein Deposits ...................................................................... 2 Tertiary Molybdenum Deposits ................................................................. 2 Little Falls—1 ............................................................................. 3 CUMO—2 .................................................................................. 3 Red Mountain Prospect—45 ...................................................... 3 Rocky Bar District—43 .............................................................. 3 West Eight Mile—37 .................................................................. 3 Devil’s Creek Prospect—46 ....................................................... 3 Walton—8 .................................................................................. 4 Ima—3 ........................................................................................ 4 Liver Peak (a.k.a. Goat Creek)—4 ............................................. 4 Bald Butte—5 ............................................................................. 5 Big Ben—6 ................................................................................. 6 Emigrant Gulch—7 ................................................................... -
Montana Forest Insect and Disease Conditions and Program Highlights
R1-16-17 03/20/2016 Forest Service Northern Region Montata Department of Natural Resources and Conservation Forestry Division In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. Additionally, program information may be made available in languages other than English. To file a program discrimination complaint, complete the USDA Program Discrimination Complaint Form, AD-3027, found online at http://www.ascr.usda.gov/complaint_filing_cust.html and at any USDA office or write a letter addressed to USDA and provide in the letter all of the information requested in the form. To request a copy of the complaint form, call (866) 632-9992. Submit your completed form or letter to USDA by: (1) mail: U.S. -
Idaho Mountain Goat Management Plan (2019-2024)
Idaho Mountain Goat Management Plan 2019-2024 Prepared by IDAHO DEPARTMENT OF FISH AND GAME June 2019 Recommended Citation: Idaho Mountain Goat Management Plan 2019-2024. Idaho Department of Fish and Game, Boise, USA. Team Members: Paul Atwood – Regional Wildlife Biologist Nathan Borg – Regional Wildlife Biologist Clay Hickey – Regional Wildlife Manager Michelle Kemner – Regional Wildlife Biologist Hollie Miyasaki– Wildlife Staff Biologist Morgan Pfander – Regional Wildlife Biologist Jake Powell – Regional Wildlife Biologist Bret Stansberry – Regional Wildlife Biologist Leona Svancara – GIS Analyst Laura Wolf – Team Leader & Regional Wildlife Biologist Contributors: Frances Cassirer – Wildlife Research Biologist Mark Drew – Wildlife Veterinarian Jon Rachael – Wildlife Game Manager Additional copies: Additional copies can be downloaded from the Idaho Department of Fish and Game website at fishandgame.idaho.gov Front Cover Photo: ©Hollie Miyasaki, IDFG Back Cover Photo: ©Laura Wolf, IDFG Idaho Department of Fish and Game (IDFG) adheres to all applicable state and federal laws and regulations related to discrimination on the basis of race, color, national origin, age, gender, disability or veteran’s status. If you feel you have been discriminated against in any program, activity, or facility of IDFG, or if you desire further information, please write to: Idaho Department of Fish and Game, P.O. Box 25, Boise, ID 83707 or U.S. Fish and Wildlife Service, Division of Federal Assistance, Mailstop: MBSP-4020, 4401 N. Fairfax Drive, Arlington, VA 22203, Telephone: (703) 358-2156. This publication will be made available in alternative formats upon request. Please contact IDFG for assistance. Costs associated with this publication are available from IDFG in accordance with Section 60-202, Idaho Code. -
Tectonic Alteration of a Major Neogene River Drainage of the Basin and Range
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2016 TECTONIC ALTERATION OF A MAJOR NEOGENE RIVER DRAINAGE OF THE BASIN AND RANGE Stuart D. Parker Follow this and additional works at: https://scholarworks.umt.edu/etd Part of the Tectonics and Structure Commons Let us know how access to this document benefits ou.y Recommended Citation Parker, Stuart D., "TECTONIC ALTERATION OF A MAJOR NEOGENE RIVER DRAINAGE OF THE BASIN AND RANGE" (2016). Graduate Student Theses, Dissertations, & Professional Papers. 10637. https://scholarworks.umt.edu/etd/10637 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. TECTONIC ALTERATION OF A MAJOR NEOGENE RIVER DRAINAGE OF THE BASIN AND RANGE By STUART DOUGLAS PARKER Bachelor of Science, University of North Carolina-Asheville, Asheville, North Carolina, 2014 Thesis Presented in partial fulfillment of the requirements for the degree of Master of Science in Geology The University of Montana Missoula, MT May, 2016 Approved by: Scott Whittenburg, Dean of The Graduate School Graduate School James W. Sears, Committee Chair Department of Geosciences Rebecca Bendick Department of Geosciences Marc S. Hendrix Department of Geosciences Andrew Ware Department of Physics and Astronomy Parker, Stuart, M. S., May, 2016 Geology Tectonic alteration of a major Neogene river drainage of the Basin and Range Chairperson: James W. -
Seasonal Status of the American Pipit in Idaho
SEASONAL STATUS OF THE AMERICAN PIPIT IN IDAHO DANIEL M. TAYLOR, 244 N. 12th, Pocatello,Idaho 83201 In Idaho, the AmericanPipit (Antbus rubescens)has been considered primarilya migrant,either locally common but erratic (Larrison et al. 1967) or uncommonin springand commonin fall (Burleigh1972). Severalother writers(Merriam 1891, Merrill 1898, Newhouse1960, Levy 1962) consid- ered it an abundantfall migrantbut gaveno indicationof actualnumbers. The one (Larrisonet al. 1967) or two (Burleigh1972) winterrecords were from Lewiston.Larrison et al. (1967) suspectedthat pipitsmight breed on someof the state'shigh mountains,while Burleigh(1972) knew of only Merriam's(1891) statementthat they breedin the Salmon River Mountains and a report by L. B. McQueenof breedingin the upper Pahsimeroi drainagenear Borah Peak. This scantinessof breedingevidence may be why the mostrecent A.O.U. checklist(1983) statesthat the AmericanPipit breedslocally on mountaintopsin severalRocky Mountain states but does not specificallylist Idaho. In this paper I consolidateand enhancewhat is known aboutAmerican Pipit distributionin Idaho with reference to adjacent areas. I present evidenceof additionalbreeding, concentrations of thousandsof fall mi- grants,and the species'regular but erraticwintering in much of southern Idaho.I analyzeChristmas Bird Countdata for patternsin winterdistribu- tion relatedto differencesin weather,elevation, geography, and annual variability. METHODS I gatheredrecent American Pipit recordsfrom a literaturereview and my own fieldnotes for the last 15 years.All ChristmasBird Counts(CBCs) for Idahosince 1978 were included,as well as somefrom adjacentMontana and Washington.Long-term counts from southernIdaho were examined statisticallyin a mannersimilar to that of Lauranceand Yensen(1985) and Dunning and Brown (1982). Weather data were extracted from U.S. EnvironmentalData Servicemonthly reports from eachweather station in or closeto eachCBC. -
Ekstrom's L Diamond E Ranch
Ekstrom’s L Diamond E Ranch Clinton, MT 83 ± Acres $750,000 | 76 ± Acres | Land Only $795,000 | 7 ± Acres | Homestead 708 N. Rouse Bozeman, MT (406) 589-4160 westernranchbrokers.com If you’ve heard the water over rocks, if you’ve seen the Salmon Fly hatch, if you’ve set eyes on the verdant John Long and Sapphire Mountains then you already know. Homesteaded over 100 years ago by the Elliott family, the L Diamond E Ranch represents one of the last parcels of this size with this proximity to the Rock Creek area. The Blue Ribbon fishery of Rock Creek and the adjacent Clark Fork River both possess unparalleled beauty and unmatched fishing. Along with the elk, moose, and deer habitat this area represents a special place for outdoor enthusiasts. Fishing on nearby Rock Creek Rock Creek © 2019 Western Ranch Brokers || [email protected] ~2~ Summary The famed “L Diamond E Ranch” is a 83± acre historic homestead located near the Clark Fork and legendary Rock Creek, just outside of Missoula, MT. This renowned property comes complete with a spring creek, ponds, and irrigated hay fields. The historic barn, home as well as two cabins are well known for providing a comfortable base for travelers, guides, fishermen, and adventurers alike. This strategic location creates an excellent opportunity for commercial use as base for your own outfitting and lodging operation, real estate development opportunit, and/or private retreat. All water rights convey. Hunting and fishing outfitter permits also available. © 2019 Western Ranch Brokers || [email protected] ~3~ © 2019 Western Ranch Brokers || [email protected] ~4~ Location Located less than 30 minutes east of Missoula the L Diamond E is located at the exit for Rock Creek Road off Interstate 90 near the confluence of Rock Creek and the Clark Fork River. -
Effects of Winter Recreation on Wildlife of the Greater Yellowstone Area: a Literature Review and Assessment
EFFECTS OF WINTER RECREATION ON WILDLIFE OF THE GREATER YELLOWSTONE AREA: A LITERATURE REVIEW AND ASSESSMENT Greater Yellowstone Winter Wildlife Working Group Greater Yellowstone Coordinating Committee October 1999 DEPARTMENT OF AGRICULTURE EFFECTS OF WINTER RECREATION ON WILDLIFE OF THE GREATER YELLOWSTONE AREA: A LITERATURE REVIEW AND ASSESSMENT Greater Yellowstone Winter Wildlife Working Group October 1999 Suggested citation: Olliff, T., K. Legg, and B. Kaeding, editors. 1999. Effects of winter recreation on wildlife of the Greater Yellowstone Area: a literature review and assessment. Report to the Greater Yellowstone Coordinating Committee. Yellowstone National Park, Wyoming. 315 pages. Editors: Tom Olliff, Kristin Legg, and Beth Kaeding Layout: Tami Blackford Cover photo courtesy of the National Park Service. CONTENTS PREFACE ........................................................... v BIRDS Bald eagles (Haliaeetus leucocephalus) ACKNOWLEDGMENTS ........................................ vii J. T. Stangl ...................................... 103 Trumpeter swans (Cygnus buccinator) CONTRIBUTORS ................................................. ix Tom Olliff ....................................... 113 REVIEWERS ...................................................... xi HABITAT Effects of recreation on vegetation INTRODUCTION J. T. Stangl ...................................... 119 Tom Olliff ................................................. 1 ISSUES MAMMALS Effects of development on wildlife Bighorn sheep (Ovis canadensis) Wendy Clark -
Chronology, Stable Isotopes, and Glaciochemistry of Perennial Ice in Strickler Cavern, Idaho, USA
Investigation of perennial ice in Strickler Cavern, Idaho, USA Chronology, stable isotopes, and glaciochemistry of perennial ice in Strickler Cavern, Idaho, USA Jeffrey S. Munroe†, Samuel S. O’Keefe, and Andrew L. Gorin Geology Department, Middlebury College, Middlebury, Vermont 05753, USA ABSTRACT INTRODUCTION in successive layers of cave ice can provide a record of past changes in atmospheric circula- Cave ice is an understudied component The past several decades have witnessed a tion (Kern et al., 2011a). Alternating intervals of of the cryosphere that offers potentially sig- massive increase in research attention focused ice accumulation and ablation provide evidence nificant paleoclimate information for mid- on the cryosphere. Work that began in Antarc- of fluctuations in winter snowfall and summer latitude locations. This study investigated tica during the first International Geophysi- temperature over time (e.g., Luetscher et al., a recently discovered cave ice deposit in cal Year in the late 1950s (e.g., Summerhayes, 2005; Stoffel et al., 2009), and changes in cave Strickler Cavern, located in the Lost River 2008), increasingly collaborative efforts to ex- ice mass balances observed through long-term Range of Idaho, United States. Field and tract long ice cores from Antarctica (e.g., Jouzel monitoring have been linked to weather patterns laboratory analyses were combined to de- et al., 2007; Petit et al., 1999) and Greenland (Schöner et al., 2011; Colucci et al., 2016). Pol- termine the origin of the ice, to limit its age, (e.g., Grootes et al., 1993), satellite-based moni- len and other botanical evidence incorporated in to measure and interpret the stable isotope toring of glaciers (e.g., Wahr et al., 2000) and the ice can provide information about changes compositions (O and H) of the ice, and to sea-ice extent (e.g., Serreze et al., 2007), field in surface environments (Feurdean et al., 2011). -
MAP SHOWING LOCATIONS of MINES and PROSPECTS in the DILLON Lox 2° QUADRANGLE, IDAHO and MONTANA
DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY MAP SHOWING LOCATIONS OF MINES AND PROSPECTS IN THE DILLON lox 2° QUADRANGLE, IDAHO AND MONTANA By JeffreyS. Loen and Robert C. Pearson Pamphlet to accompany Miscellaneous Investigations Series Map I-1803-C Table !.--Recorded and estimated production of base and precious metals in mining districts and areas in the Dillon 1°x2° guadrangle, Idaho and Montana [Production of other commodities are listed in footnotes. All monetary values are given in dollars at time of production. Dashes indicate no information available. Numbers in parentheses are estimates by the authors or by those cited as sources of data in list that follows table 2. <,less than; s.t., short tons] District/area Years Ore Gold Silver Copper Lead Zinc Value Sources name (s. t.) (oz) (oz) (lb) (lb) (lb) (dollars) of data Idaho Carmen Creek 18 70's-190 1 (50,000) 141, 226 district 1902-1980 (unknown) Total (50,000) Eldorado 1870's-1911 17,500 (350 ,000) 123, 226 district 1912-1954 (13,000) (8,000) (300,000) Total (650,000) Eureka district 1880's-1956 (13 ,500) 12,366 (2,680,000) 57,994 (4,000) ( 4,000 ,000) 173 Total (4,000,000) Gibbonsville 1877-1893 (unknown) district 1894-1907 (83,500) (1,670,000) 123, 226 1908-1980 ( <10 ,000) 123 Total (2,000,000) Kirtley Creek 1870's-1890 2,000 40,500 173 district 1890's-1909 (<10,000) 1910-1918 24,300 (500 ,000) 123 1919-1931 (unknown) 1932-1947 2,146 (75 ,000) 173 Total (620,000) McDevitt district 1800's.-1980 (80,000) Total (80,000) North Fork area 1800's-1980 (unknown) Total ( <10 ,000) Pratt Creek 1870's-1900 (50 ,000) district Total (50,000) Sandy Creek 1800 's-1900 (unknown) district 1901-1954 19,613 4,055 4,433 71,359 166,179 (310,000) 17 3, 200 Total (310 ,000) Montana Anaconda Range 1880's-1980 (<100,000) area Total (<100,000) Argenta district 1864-1901 (1 ,500 ,000) 1902-1965 311,796 72,241 562,159 604,135 18,189,939 2,009,366 5,522,962 88 Total (7,000,000) Baldy Mtn. -
Lanners Ontana
Please Thank Our Sponsors MONTANA ASSOCIATION OF PLANNERS Planning in a Natural Resources State Conference Program 2014 MAP Conference September 15th -17th Hamilton, Montana 24 Notes Welcome to Ravalli County! 2014-2015 Montana Association of Ravalli County is a beautiful valley sandwiched Planners Board Members between the Sapphire Mountains to the East and the Bitterroot Mountains to the West. It is Charity Fechter referred to as the Bitterroot Valley. Madison County Planning Dept - Chair Ravalli County was created by the Montana Leg- Wyeth Friday islature in 1893 and named after Antony Ravalli, Billings-Yellowstone County Plan- a priest who arrived in the valley in 1845 and ning Dept. started the St. Mary’s Mission. The Mission, near the town of Stevensville, was the first per- Janet Cornish manent white settlement in Montana. Community Development Services of Montana, Butte - Treasurer The town of Hamilton was founded by Marcus Daly, one of the “Copper Kings” and founder of Brian Bender the Anaconda Copper Company. Hamilton was Powell County Planning Dept - Sec- named after his employee James Hamilton, who retary platted the town in 1890. Christopher Scott Gallatin County Planning Dept The Bitterroot Valley has been predominately an agricultural and timber economy with retire- Allison Mouch ment and tourism becoming prominent in re- Planning Bureau Chief, MT Dept of cent years. It is also home to The Rocky Moun- Commerce tain Lab. The Lab is a Biosafety Level 4 Labora- tory which was constructed in 1928 as a result Andrew Hagemeier of research begun around 1900 to study Rocky Community Planner, Land Solutions Mountain spotted fever. -
Abandoned-Inactive Mines on Bitterroot National Forest-Administered Land
Abandoned-Inactive Mines on Bitterroot National Forest-Administered Land Map of the Curlew Mine by Rick Schmidt in MBMG mineral property files Open-File Report MBMG 484 Phyllis A. Hargrave Catherine McDonald Michael D. Kerschen John J. Metesh Robert Wintergerst Prepared for the U.S. Department of Agriculture Forest Service-Region 1 Abandoned-Inactive Mines on Bitterroot National Forest-Administered Land Open-File Report MBMG 484 October 2003 Phyllis A. Hargrave Catherine McDonald Michael D. Kerschen John J. Metesh Robert Wintergerst Prepared for the U.S. Department of Agriculture Forest Service-Region 1 CONTENTS Page LIST OF FIGURES ........................................................... iii LIST OF TABLES ............................................................ iii 1.0 INTRODUCTION ..........................................................1 1.1 Project Objectives ....................................................1 1.2 Abandoned and Inactive Mines Defined . 2 1.3 Health and Environmental Problems at Mines . 2 1.3.1 Acid Mine Drainage ...........................................3 1.3.2 Solubilities of Selected Metals ...................................3 1.3.3 The Use of pH and SC to Identify Problems . 5 1.4 Methodology ........................................................5 1.4.1 Data Sources .................................................5 1.4.2 Pre-Field Screening............................................6 1.4.3 Field Screening ...............................................7 1.4.4 Field Methods ................................................8 -
Level IV Ecoregions of Montana
DRAFT 2 15. Northern Rockies Ecoregion 15 is mountainous and rugged. Climate, trees, and understory species are characteristically maritime-influenced. Douglas-fir, subalpine fir, Englemann spruce, western larch, lodgepole pine, and ponderosa pine as well as Pacific indicators such as western redcedar, western hemlock, mountain Ecoregions of Montana hemlock, and grand fir occur. Pacific tree species are more numerous than in the Idaho Batholith (16) Second Edition and are never dominant in the Middle Rockies (17). Alpine areas occur but, as a whole, the region has lower elevations, less perennial snow and ice, and fewer glacial lakes than the adjacent Canadian Rockies (41). Metasedimentary rocks are common; granitic rocks and associated management problems are less extensive than in the Idaho Batholith (16). Thick volcanic ash deposits are more Widespread forests cover the Northern Elk commonly are found in high mountain Literature Cited: Rockies (15). Pacific Coast tree species are pastures during the summer and on lower, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and quantity of and Foothill Prairies (formerly Ecoregion 16) to another level III ecoregion, the Middle Rockies (17). The widespread than in Ecoregion 16. Logging and mining are common and have caused stream water Bailey, R.G., Avers, P.E., King, T., and McNab, W.H., eds., 1994, Ecoregions and subregions of the United States (map) (supplementary table of common locally. The ecoregion has been densely forested slopes during the winter. environmental resources; they are designed to serve as a spatial framework for the research, assessment, second edition also modifies a few level IV ecoregion lines along Montana's western border so that quality problems in the region.