Wolf Conservation and Management 2015 Annual Report
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Alteration Petrology in the Potosi Mining District Tobacco Root Mountains Montana
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1975 Alteration petrology in the Potosi Mining District Tobacco Root Mountains Montana Michael James Burnside The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Burnside, Michael James, "Alteration petrology in the Potosi Mining District Tobacco Root Mountains Montana" (1975). Graduate Student Theses, Dissertations, & Professional Papers. 7724. https://scholarworks.umt.edu/etd/7724 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]. ALTERATION PETROLOGY IN THE POTOSI MINING DISTRICT, TOBACCO ROOT MOUNTAINS, MONTANA by Michael Burnside B.A., University of Montana, 1970 Presented in partial fulfillm ent of the requirements for the degree of Master of Science UNIVERSITY OF MONTANA 1975 Approved by: Chairman, Board o£/Examiners DeapC^ Graduate-^^hool ' Date Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. UMI Number: EP38525 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. -
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. -
MBMG 505-Jefferson-V2.FH10
GEOLOGIC MAP OF THE CENOZOIC DEPOSITS OF THE UPPER JEFFERSON VALLEY MBMG Open File Report 505 2004 Compiled and mapped by Susan M. Vuke, Walter W. Coppinger, and Bruce E. Cox This report has been reviewed for conformity with Montana Bureau of Mines and Geology’s technical and editorial standards. Partial support has been provided by the STATEMAP component of the National Cooperative Geology Mapping Program of the U.S. Geological Survey under contract Number 03HQAG0090. CENOZOIC DEPOSITS OF THE UPPER JEFFERSON VALLEY Cenozoic deposits are the focus of the Geologic Map of the upper Jefferson Valley. The map is largely a compilation of previous mapping with additional interpretations based on aerial photos and limited additional field work. Older rocks are included to show their relations to the Cenozoic deposits, but they are generalized on the map. Lithologic descriptions of the Cenozoic deposits are given in the map explanation (p. 17). References used for the map compilation are shown on p. 15. The northern and southern parts of the map are discussed separately. NORTHERN PART OF MAP AREA Quaternary deposits A variety of Quaternary deposits blanket much of the slope area of the Whitetail and Pipestone Creek valleys between the flanks of the Highland Mountains and Bull Mountain (Fig. 1). East and southeast of these Quaternary slope deposits are more isolated areas of partly cemented Pleistocene gravels on pediments. One of these gravel deposits near Red Hill (Fig. 1) yielded a late Pleistocene vertebrate assemblage including cheetah, horse, camel, and large mountain sheep. Radiocarbon dates from the lowest part of the sequence range between 10,000 and 9,000 14C yr. -
Edings of The
Proceedings of the FIRE HISTORYIISTORY WORKSHOP October 20-24, 1980 Tucson, Arizona General Technical Report RM.81 Rocky Mountain Forest and Range Experiment Station Forest Service U.S. Department of Agriculture Dedication The attendees of The Fire History Workshop wish to dedicate these proceedings to Mr. Harold Weaver in recognition of his early work in applying the science of dendrochronology in the determination of forest fire histories; for his pioneering leadership in the use of prescribed fire in ponderosa pine management; and for his continued interest in the effects of fire on various ecosystems. Stokes, Marvin A., and John H. Dieterich, tech. coord. 1980. Proceedings of the fire history workshop. October 20-24, 1980, Tucson, Arizona. USDA Forest Service General Technical Report RM-81, 142 p. Rocky Mountain Forest and Range Experiment Station, Fort Collins, Cob. The purpose of the workshop was to exchange information on sampling procedures, research methodologies, preparation and interpretation of specimen material, terminology, and the appli- cation and significance of findings, emphasizing the relationship of dendrochronology procedures to fire history interpretations. Proceedings of the FIRE HISTORY WORKSHOP October 20.24, 1980 Tucson, Arizona Marvin A. Stokes and John H. Dieterich Technical Coordinators Sponsored By: Rocky Mountain Forest and Range Experiment Station Forest Service, U.S. Department of Agriculture and Laboratory of Tree.Ring Research University of Arizona General Technical Report RM-81 Forest Service Rocky Mountain Forest and Range U.S. Department of Agriculture Experiment Station Fort Collins, Colorado Foreword the Fire has played a role in shaping many of the the process of identifying and describing plant communities found in the world today. -
Geologic Map of Ruby Dam Area Southwestern Montana
Geologic Map of Ruby Dam Area Southwestern Montana Compiled and Mapped by Zachary C. St. Jean and Deirdre R. Teeter Montana Bureau of Mines and Geology Open File Report MBMG 488 2004 This report has had preliminary reviews for conformity with Montana Bureau of Mines and Geology’s technical editorial standards. Partial support has been provided by the EDMAP component of the National Cooperative Geological Mapping Program of the U.S. Geological Survey under Contract Number 01HQAG0157. Introduction This project was funded by the EDMAP program of the U. S. Geological Survey. Field studies, including geologic mapping and a gravity and magnetic survey, were conducted during the 2001 field season. These studies were undertaken to gain a better understanding of the geologic structure of the Ruby basin in the area of Ruby Dam in southwest Montana (Figures 1 and 2). Ruby Dam, which impounds Ruby Reservoir, lies within a seismically active region known as the Intermountain Seismic Belt. Delineation and detailed mapping of the Tertiary and Quaternary sediments has helped to understand better the occurrence of Quaternary faulting in the basin. No new faults of Quaternary age were recognized within the field area. However, a fault that offsets Quaternary deposits was newly mapped by the authors in a gravel pit two miles north of the north map boundary. This fault may change previously calculated ground acceleration values at the dam site, and may indicate a greater susceptibility of the dam to seismic activity than previously thought. The geologic map in this report combines previous work that focused on the bedrock of the area with new mapping of the Tertiary and Quaternary deposits by the present authors. -
Idaho: Lewis Clark Byway Guide.Pdf
The Lewis and Clark Backcountry Byway AND ADVENTURE ROAD Tendoy, Idaho Meriwether Lewis’s journal entry on August 18, 1805 —American Philosophical Society The Lewis and Clark Back Country Byway AND ADVENTURE ROAD Tendoy, Idaho The Lewis and Clark Back Country Byway and Adventure Road is a 36 mile loop drive through a beautiful and historic landscape on the Lewis and Clark National Historic Trail and the Continental Divide National Scenic Trail. The mountains, evergreen forests, high desert canyons, and grassy foothills look much the same today as when the Lewis and Clark Expedition passed through in 1805. THE PUBLIC LANDS CENTER Salmon-Challis National Forest and BLM Salmon Field Office 1206 S. Challis Street / Salmon, ID 83467 / (208)756-5400 BLM/ID/GI-15/006+1220 Getting There The portal to the Byway is Tendoy, Idaho, which is nineteen miles south of Salmon on Idaho Highway 28. From Montana, exit from I-15 at Clark Canyon Reservoir south of Dillon onto Montana Highway 324. Drive west past Grant to an intersection at the Shoshone Ridge Overlook. If you’re pulling a trailer or driving an RV with a passenger vehicle in tow, it would be a good idea to leave your trailer or RV at the overlook, which has plenty of parking, a vault toilet, and interpretive signs. Travel road 3909 west 12 miles to Lemhi Pass. Please respect private property along the road and obey posted speed signs. Salmon, Idaho, and Dillon, Montana, are full- service communities. Limited services are available in Tendoy, Lemhi, and Leadore, Idaho and Grant, Montana. -
Volume 7 Number 7
Volume 8 Number 8 30 December 2020 The Taxonomic Report OF THE INTERNATIONAL LEPIDOPTERA SURVEY ISSN 2643-4776 (print) / ISSN 2643-4806 (online) Review of the Speyeria egleis complex in Montana, with the description of two new subspecies (Lepidoptera: Nymphalidae: Heliconiinae) Steve Kohler 2617 Glen Drive Missoula, MT 59804 ABSTRACT: Four phenotypically and geographically distinct sets of populations of Speyeria egleis are identified in Montana. Two new subspecies are named from northwestern and northcentral Montana. Two existing names are recognized (S. e. macdunnoughi from southwestern Montana, southeastern Idaho and northwestern Wyoming, and S. e. albrighti from central Montana. S. e. near macdunnoughi from Oregon and Washington is discussed. Additional key words: Island ranges, Sweet Grass Hills, Morrell Mountain, Highwood Mountains. ZooBank registration: urn:lsid:zoobank.org:pub:94D912CC-72BA-42EA-A14E-E0F51E1CD498 INTRODUCTION At the present time, thirteen described subspecies of Speyeria egleis (Behr, 1862) are recognized in North America (Pelham 2020). Of these, two occur in Montana, S. e. macdunnoughi (Gunder, 1932) and S. e albrighti (Gunder, 1932). Historically, all Montana egleis populations with a brownish colored under hindwing disc have been assigned to macdunnoughi and all populations with an olive-green colored under hindwing disc have been assigned to albrighti (Ferris and Brown 1981; Kohler 1980). During the course of my study of Montana butterflies, I have identified at least four distinct sets of populations which can be phenotypically and geographically segregated. The purpose of this paper is to define the characters of these four distinctive populations and to describe two new subspecies. DISCUSSION In this study, the two current subspecies of S. -
MONTANA N7 4Qea
E 12, p( /F- o77 (r 2) Sf(jji PGJ/F-077(82) National Uranium Resource Evaluation 6 BOZEMAN QUADRANGLE 41 MONTANA n7 4QeA/ University of Montana Missoula, Montana and Montana State University Bozeman, Montana E2T oFi Issue Date August 1982 SATESO9 PREPARED FOR THE U.S. DEPARTMENT OF ENERGY Assistant Secretary for Nuclear Energy Grand Junction Area Office, Colorado rmetadc957781 Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed in this report, or represents that its use would not infringe privately owned rights. Reference therein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. This report is a result of work performed by the University of Montana and Montana State University, through a Bendix Field Engineering Corporation subcontract, as part of the National Uranium Resource Evaluation. NURE was a program of the U.S. Department of Energy's Grand Junction, Colorado, Office to acquire and compile geologic and other information with which to assess the magnitude and distribution of uranium resources and to determine areas favorable for the occurrence of uranium in the United States. Available from: Technical Library Bendix Field Engineering Corporation P.O. -
Stratigraphy and Structure of the Rock Creek Area, Beaverhead County, Montana by James Franklin Peters
AN ABSTRACT OF THE THESIS OF JAMES FRANKLIN PETERS for the Master of Science (Name) (Degree) in Geology presented on (Major) (Date) Title: STRATIGRAPHY AND STRUCTURE OF THE ROCK CREEK AREA, BEAVERHEAD COUNTY, MONTANA Abstract approved:Redacted for Privacy Dr. David A. Bostwick The Rock Creek area consists of 53 square miles located in the eastern foothills of the Pioneer Mountains, Beaverhead County, Montana. Approximately 8, 500 feet of late Paleozoic and early Mesozoic contact-metamorphosed sedimentary rocks and late Meso- zoic sedimentary rocks are exposed in the area of study. Most of the late Paleozoic and Mesozoic rocks were deposited along the eastern edge of the Cordilleran miogeosyncline.The old- est exposed rocks in the map area belong to the Amsden Formation of Late Mississippian to Early Pennsylvanian age.Other late Paleo- zoic rock units include the Quadrant Formation of Pennsylvanian age and the Phosphoria Formation of Permian age.Mesozoic forma- tions include the Dinwoody Formation of Triassic age and the Kootenai Formation and Colorado Group of Cretaceous age. The Tertiary is represented bybasin depositsand basaltic andesite extrusives.Unconsolidated Quaternary glacialand fluvial deposits complete the stratigraphicsuccession. Granodiorite intrusive rocksoccupy the southwestern corner of the area mapped andcompose part of the eastern margin of the Mount Torrey Batholith, whichis probably genetically relatedto the Boulder Batholith.Along the margin of the intrusive,contact meta- morphism has destroyed the originalsedimentary characteristics of the late Paleozoic and earlyMesozoic Formations. During the Late Cretaceous Laramideorogeny the sedimentary rocks were tilted and faulted. Thestructures in the area are related to the main episode of Laramidedeformation, emplacement of the Mount Torrey Batholith, and laterphases of structural adjustment. -
Montana Forest Insect and Disease Conditions and Program Highlights, 2006
Montana United States Forest Insect and Disease Conditions Department of Agriculture and Program Forest Service Highlights Northern Region Forest Health Protection 2006 Montana Department of Natural Resources Trees killed by bark beetles and Conservation Forestry Division Assessing decay in fire-killed western larch MOONNTTAANNAA M FFoorreesstt IInnsseecctt aanndd DDiisseeaassee CCoonnddiittiioonnss aanndd PPrrooggrraamm HHiigghhlliigghhttss -- 22000066 Report 06-1 2007 Compiled By: Amy Gannon, Montana Department of Natural Resources and Conservation, Forestry Division Scott Sontag and Kjerstin Skov, USDA Forest Service, Northern Region, State and Private Forestry, Forest Health Protection Contributors: Leah Aquino, Gregg DeNitto, Ken Gibson, Marcus Jackson, Blakey Lockman, Kjerstin Skov, Nancy Sturdevant, USDA Forest Service, Northern Region, State and Private Forestry, Forest Health Protection; Brennan Ferguson, Amy Gannon, Montana Department of Natural Resources and Conservation, Forestry Division Data Summary and Map Production: Jim Fears, USDA Forest Service, Northern Region, State and Private Forestry, Forest Health Protection Cover Photo: Trees killed by bark beetles, courtesy of Ken Gibson, USDA Forest Service. Assessing decay in fire-killed larch, courtesy of Marcus Jackson, USDA Forest Service. i TABLE OF CONTENTS ABBREVIATIONS ..................................................................................................................... 1 INTRODUCTION ...................................................................................................................... -
NEZ PERCE ...Through the Big Hole, Horse Prairie and Lemhi Valleys -1877
Auto Tour the plight op The NEZ PERCE ...through the Big Hole, Horse Prairie and Lemhi Valleys -1877 United States Forest Beaverhead-Deerlodge Department of Service National Agriculture Forest n August 1877, the tranquility of the Big Hole Valley was shattered by the sound of gunfire as a battle erupted between J five bands of Nez Perce Indians and U.S. military forces along the banks of the Big Hole River. For valley settlers, anxiety turned to fear and concern as nearly 800 Nez Perce men, woman and children gathered their wounded and fled southward towards Skinner Meadows and the country beyond. Today, you can retrace the route used by the Nez Perce and their military pursuers. This brochure describes the Nez Perce (Nee- Me-Poo) National Historic Trail between Big Hole National Batttlefield, Montana and Leadore, Idaho. The map shows the auto tour route in detail. Auto Tour Route - This designated auto route stays on all-weather roads and allows you to experience the Nez Perce Trail from a distance. The auto tour route is passable for all types of vehicles. An alternative route exists from Lost Trail Pass on the Montana/Idaho border south to Salmon and Leadore, Idaho along Hwy. 93 and 28. Adventure Route - For those seeking the most authentic historic route, a rough two lane road, connects Jackson, Montana and the Horse Prairie Valley. Examine the map carefully and watch for signs. You may want to take a more detailed Forest Map. The adventure route is usually passable from July to October. It is not recommended for motor homes or vehicles towing trailers. -
Papilio Series) 2006
(NEW April 28 PAPILIO SERIES) 2006 TAXONOMIC STUDIES AND NEW TAXA OF NORTH AMERICAN BUTTERFLIES by James A. Scott (also editor), Michael S. Fisher, Norbert G. Kondla, Steve Kohler, Crispin S. Guppy, Stephen M. Spomer, and B. Chris Schmidt Abstract. New diversity is reported and discussed among North American butterflies. Several dozen new taxa are named. A new "sibling" species has been found to occur throughout the Rocky Mts., introducing a new butterfly species to most states in western U.S. and to southern Alberta and BC. Several taxa of Colias, Euphydryas, Lycaena, and Plebejus are raised to species status. Many nam.e changes are made, and many taxa are switched between species to create several dozen new combinations. The relevance of species concepts to difficult groups of butterflies is explored. Introduction This paper consists of miscellaneous taxonomic studies on North American butterflies, some in the northeast, but mostly in the west. Most of the diversity of butterfly fauna in North America is in the western mountainous areas, where the human population is lower, so it has taken longer to study western butterflies, and a lot more study is needed. We have made new findings on many wes.tern butterflies, and this progress is reported below. And Scott recently moved his collection out of old dermestid-infested drawers into fine very-tight ones that those beetles cannot enter, and in the process of resorting them found a dozen unnamed subspecies, which are named below. As we study our butterflies and learn more and more about them, a disturbing pattern has emerged.