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0 Vol 6, No 3 |Ey SPRING 1993 Newslettar of the Llontana Natlve Plant Srclety
--'-'-- Kelseya uniflora cI 0 Vol 6, No 3 |ey SPRING 1993 Newslettar of the llontana Natlve Plant Srclety Type Localities and the Botanical Exploration of Montana - Peter Lesica lf you're a member of the Montana Native Plant Society, you're colfections of blanketflower (Gaillardia aristata), balsamroot probably getting usad to hearing plants referred to by their (Balsamorhiza sagittata), silvery lupine (Lupinus argenteusl and scientific name. Even though the/re often long and hard to mountain death-camas (Zgadenus elegans) - not bad for a da/s pronounce, perhaps you're even becoming convinced that they're work. Two weeks later he found scarlet globe-mallow useful. But where do these names come from, and how do (Sphaeralcea coccinea) near the Marias River in Toole County. taxonomists know what name clrrec.tly applies to which plant? Another early explorer in western Montana was Nathaniel When spotted knapweed first appeared in North America, how did Wyeth. He made a number of type collections from what he said taxonomists know that it was a European weed, Centaurea was the vicinity of the Flathead River. Among these were maculosa, instead of something else - perhaps an undescribed Columbia virgin's-bower (Clematis columbiana), low larkspur species? Taxonomy rests on a system of standards: for each (Delphinium bicololl and Wyeth's lupine (Luprnus wyethiil. He species that is described new to science, there is a type also made the first collections of white-head mule's-ears and specimen. This type specimen represents what the ta,ronomist northern mu le's-ears (Wy eth i a am pl e x i cau I i s artd W. -
Haystack Development
August 2, 2017 HAYSTACK DEVELOPMENT Moonlight Basin Overall Development Plan Wildlife Summary Report HAYSTACK DEVELOPMENT Wildlife Summary Report TABLE OF CONTENTS 1.0 INTRODUCTION ........................................................................................................................... 1 2.0 EXISTING WILDLIFE AND HABITAT ..................................................................................... 4 2.1 HABITAT ........................................................................................................................................ 4 2.2 FEDERALLY LISTED SPECIES ......................................................................................................... 6 2.2.1 Grizzly Bear .......................................................................................................................... 6 2.2.2 Canada Lynx ......................................................................................................................... 7 2.2.3 Wolverine ............................................................................................................................ 10 2.3 OTHER SPECIES OF REGIONAL SIGNIFICANCE ............................................................................ 10 2.3.1 Species of Greatest Conservation Need .............................................................................. 10 2.3.2 Migratory Birds ................................................................................................................... 13 2.3.3 Big Game Species -
Conservation in Yellowstone National Park Final Report on the COVER Wolverine Tracks in the Greater Yellowstone Ecosystem
Wolverine Conservation in Yellowstone National Park Final Report ON THE COVER Wolverine tracks in the Greater Yellowstone Ecosystem. Photo by Jason Wilmot. Wolverine Conservation in Yellowstone National Park Final Report Authors John Squires Kerry Murphy US Forest Service US Forest Service Rocky Mountain Research Station Jackson Ranger District 800 East Beckwith Avenue PO Box 25 Missoula, Montana 59801 Jackson, Wyoming 83001 [email protected] [email protected] (formerly Yellowstone Center for Resources, With contributions from Yellowstone National Park, Wyoming) Robert M. Inman Wildlife Conservation Society Jason Wilmot Wolverine Program Field Office Northern Rockies Conservation Cooperative 222 East Main Street PO Box 2705 Lone Elk 3B Jackson, Wyoming 83001 Ennis, Montana 59729 [email protected] [email protected] Jeff Copeland Mark L. Packila US Forest Service Wildlife Conservation Society Rocky Mountain Research Station Wolverine Program Field Office 800 East Beckwith Avenue 222 East Main Street Missoula, Montana 59801 Lone Elk 3B [email protected] Ennis, Montana 59729 [email protected] Dan Tyers US Forest Service Doug McWhirter Gardiner Ranger District Wyoming Game and Fish Regional Office PO Box 5 2820 State Highway 120 Gardiner, Montana 59030 Cody, Wyoming 82414 [email protected] National Park Service Yellowstone National Park Yellowstone Center for Resources Yellowstone National Park, Wyoming YCR-2011-02 March 2011 Suggested citation: Murphy, K., J. Wilmot, J. Copeland, D. Tyers, J. Squires, R. M. Inman, M. L. Packila, D. McWhirter. 2011. Wolverine conservation in Yellowstone National Park: Final report. YCR-2011-02. National Park Service, Yellowstone National Park, Yellowstone Center for Resources, Yellowstone National Park, Wyoming. -
Table of Contents I. Foreword
TABLE OF CONTENTS I. FOREWORD................................................................................................................ 4 II. REGIONAL SETTING................................................................................................. 5 III. EXISTING LAND USES............................................................................................. 7 IV. DISTRICT HISTORY ................................................................................................. 9 A. THE BIG SKY, INC. "MASTER PLAN" ................................................ 11 B. 1972 GALLATIN CANYON STUDY..................................................... 11 V. POPULATION AND DEMOGRAPHICS ................................................................... 13 VI. INFRASTRUCTURE................................................................................................ 18 A. UTILITIES............................................................................................ 18 1. Wastewater Treatment.............................................................. 18 2. Water Distribution...................................................................... 19 3. Electric And Telephone Service ................................................ 19 B. TRANSPORTATION ........................................................................... 20 1. Streets And Highways............................................................... 20 2. Air Service................................................................................. 20 -
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. -
The 1898 Field Season of CD Walcott
Field work and fossils in southwestern Montana: the 1898 field season of C. D. Walcott Ellis L. Yochelson Research Associate, Department of Paleobiology, National Museum of Natural History, Washington, DC 20013-7012 G. Zieg Senior Geologist, Teck Cominco American Inc., East 15918 Euclid, Spokane, WA 99216 INTRODUCTION In 1879, Charles Doolittle Walcott (1850- 1927) (Yochelson, 1998) joined the new U. S. Geological Survey (USGS) and July 1, 1894, became the third director of the agency. Shortly before that time the USGS had several field parties starting to investigate mining dis- tricts in Montana and Idaho. There was no overall stratigraphic succession, nor clear cor- relation from one mining district to another. In 1895, Walcott took a first quick trip through the Belt Mountains. In the vicinity of Neihart, Montana, he collected Middle Cambrian fossils (Weed, 1900). These fossils established that Lower Cambrian rocks were absent from the area and thus the Belt strata (or Algonkian, as USGS Walcott called them) were pre-Cambrian in age The unhyphenated usage and the lack of capi- ABSTRACT talization of “formation” are relatively late de- velopments in stratigraphic nomenclature. The diary of Charles Doolittle Walcott pro- vides a brief daily account of his investigations For more than fifty years, Walcott used a small of Cambrian and Precambrian rocks, mainly in pocket diary and with his comments one can the Belt Mountains during one field season. trace his route and gain some notion of how These entries also give some notion of the tri- field work was conducted before the days of als of field work before the development of the rapid automobile transportation. -
Structural Geology of the Northern Snowcrest Range, Beaverhead and Madison Counties, Montana
Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 4-1984 Structural Geology of the Northern Snowcrest Range, Beaverhead and Madison Counties, Montana Mark Kenneth Sheedlo Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Sheedlo, Mark Kenneth, "Structural Geology of the Northern Snowcrest Range, Beaverhead and Madison Counties, Montana" (1984). Master's Theses. 1571. https://scholarworks.wmich.edu/masters_theses/1571 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. STRUCTURAL GEOLOGY OF THE NORTHERN SNOWCREST RANGE, BEAVERHEAD AND MADISON COUNTIES, MONTANA by Mark Kenneth Sheedlo A Thesis Submitted to the Faculty of The Graduate College in partial fu lfillm e n t of the requirements for the Degree of Master of Science Department of Geology Western Michigan University Kalamazoo, Michigan April 1984 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission STRUCTURAL GEOLOGY OF THE NORTHERN SNOWCREST RANGE, BEAVERHEAD AND MADISON COUNTIES, MONTANA Mark Kenneth Sheedlo, M.S. Western Michigan University, 1984 The Snowcrest Range was uplifted in Late Cretaceous and Early •Tertiary time as a consequence of thrusting in Precambrian basement and Phanerozoic cover rocks. The Snowcrest-Greenhorn thrust system is associated with large- scale overturned, eastward verging folds. Mean orientation of the thrust system is N.40°E., 35°N.W.. The trend of the thrust system and associated transverse faults appear to be controlled by earlier structures. -
THE 1959 HEBGEN LAKE, MONTANA, EARTHQUAKE: TWO GEOLOGIC POINTS of VIEW by Irving J
THE 1959 HEBGEN LAKE, MONTANA, EARTHQUAKE: TWO GEOLOGIC POINTS OF VIEW by Irving J. Witkind U.S. Geological Survey Denver, CO 80225 Some 16 years ago a major earth- quake, centered near Hebgen Lake, Montana, shook Yellowstone National Park, and abruptly brought to an end the bustling 1959 tourist season. That earthquake, formally known as "The Hebgen Lake, Montana, earthquake of August 17, 1959", was widely publi- cized, and as a result of the public's keen interest in the geologic features formed during the earthquake, the Forest Service set aside the area of major damage as an educational and the northeast edge of the Henrys Lake recreational area. Now, attractive ex- basin to end against the reactivated hibits and skilled naturalists explain the northwest-trending Hebgen and Red various geologic phenomena to the Canyon faults. They assume that the many tourists who annually pass Madison Range subsided along with through the area. the flanking basins, but not as much. Immediately after the earthquake Dual-basin concept.—A second the Geological Survey began a series of group of geologists concluded that the intensive geologic investigations of the deformational pattern involved two ba- epicentral area. It soon became ap- sins of subsidence, one on each side of a parent that geologists viewing the same tectonically stable Madison Range. phenomena interpreted them differ- Each of these basins slopes gently ently. Two major concepts evolved each northeastward to end against reacti- with its own adherents, and as the vated faults; the West Yellowstone Ba- field work continued it became obvious sin (east of the Range) ends against that a vexatious controversy had begun. -
Geology of Pre-Tertiary Rocks in the Northern Part of Yellowstone National Park, Wyon1ing by EDWARD T
GEOLOGY OF PRE- TERTIARY ROCKS IN THE NORTHERN PART OF YELLOWSTONE NATIONAL PARK, m WYOMING "* ,~ - DivMOri Coforado Distril'l r ih•." n' Geology of Pre-Tertiary Rocks in the Northern Part of Yellowstone National Park, Wyon1ing By EDWARD T. RUPPEL With a section on Tertiary laccoliths, sills, and stocks in and near the Gallatin Range, Yellowstone National Park GEOLOGY OF YELLOWSTONE NATIONAL PARK GEOLOGICAL SURVEY PROFESSIONAL PAPER 729-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 72-600268 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 2401-00242 Yellowstone National Park, the oldest of the areas set aside as part of the national park sys tem, lies amidst the Rocky Mountains in north western Wyoming and adjacent parts of Montana and Idaho. Embracing large, diverse, and complex geologic features, the park is in an area that is critical to the interpretation of many significant regional geologic problems. In order to provide basic data bearing on these problems, the U.S. Geological Survey in 1965 initiated a broad pro gram of comprehensive geologic and geophysical investigations within the park. This program was carried out with the cooperation of the National Park Service, and was also aided by the National Aeronautics and Space Administration, which supported the gathering of geologic information needed in testing and in interpreting results from various remote sensing devices. This professional paper chapter is one of a series of technical geo logic reports resulting from these investigations. -
A Survey of Distribution Patterns in the Montana Alpine Flora
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1965 A survey of distribution patterns in the Montana alpine flora Richard H. Pemble 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 Pemble, Richard H., "A survey of distribution patterns in the Montana alpine flora" (1965). Graduate Student Theses, Dissertations, & Professional Papers. 6680. https://scholarworks.umt.edu/etd/6680 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]. A SURVEY OF DISTRIBUTION PATTERNS IN THE MONTANA ALPINE FLORA by RICHARD HOPPE PEMBLE B.A. Simpson College, 196j Presented in partial fulfillment of the requirements for the degree of Master of Arts UNIVERSITY OF MONTANA 1965 Approved by: Chairman, Bracrd of Examiners\ Dean, Graduate School AUG ' *• Date Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. UMI Number: EP37481 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. UMT Ois»artation Publishing UMI EP37481 Published by ProQuest LLG (2013). -
Geologic Map of the Central Madison Valley (Ennis Area) Southwestern Montana
GEOLOGIC MAP OF THE CENTRAL MADISON VALLEY (ENNIS AREA) SOUTHWESTERN MONTANA MBMG Open File Report 543 2007 Karl S. Kellogg1, Chester A. Ruleman1, and Susan M. Vuke2 1 U.S. Geological Survey 2 Montana Bureau of Mines and Geology This report has been reviewed for conformity with Montana Bureau of Mines and Geology 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 05HQAG0093. GEOLOGY OF THE CENTRAL MADISON VALLEY (ENNIS AREA) Introduction The geologic map of Cenozoic deposits of the central Madison Valley is one of a series of 1:50,000-scale intermontane valley maps prepared by the Montana Bureau of Mines and Geology as part of the U.S. Geological Survey STATEMAP program (Fig. 1). The western Montana valley maps were individually proposed by the STATEMAP Advisory Board primarily because they are areas where development is occurring or is anticipated. The maps emphasize the geology of the Cenozoic deposits. The central Madison Valley map adjoins a 1:50,000-scale geologic map to the north, of the lower Jefferson Valley (Vuke, 2006). The Central Madison Valley map is based on a series of 1:24,000-scale geologic maps by Karl S. Kellogg (1992, 1993a, 1993b, 1994, and 1995) and part of a 1:100,000-scale geologic map of the Ennis 30’x 60’ quadrangle by Karl S. Kellogg and Van S. Williams (2000) that incorporates much new mapping with previous mapping in the area. In addition, the Central Madison Valley map includes subsequent mapping by Chester S. -
Yellowstone Paleontological Survey
Yellowstone Paleontological Survey Introduction Stratigraphy Fossil Chronology Taxonomy Localities Vincent L. Santucci Interpretation Paleontological Resource Management Research Collections and Curation Paleontological Resources Near Yellowstone [email protected] Bibliography Yellowstone Center for Resources Appendix A: Yellowstone Paleontological Survey Proposal National Park Service Yellowstone National Park, Wyoming Appendix B: Yellowstone Paleo-Species List YCR-NR-98-1 1998 Appendix C: RMP Paleontological Project Statements Appendix D: Paleontology Researchers at Yellowstone Appendix E: Fossil Specimens in Park Collections Appendix F: Yellowstone Fossils in Outside Repositories Appendix G: GIS Stratigraphy Maps http://www2.nature.nps.gov/geology/paleontology/surveys/yell_survey/index.htm[5/28/2013 2:13:48 PM] Yellowstone Paleo Survey: Introduction Introduction A survey of Yellowstone's fossil resources was initiated in the same spirit of discovery demonstrated by Captain William Raynolds, Henry Washburn, and Ferdinand Hayden. Rumors of marine reptiles, trilobite mass death assemblages, and even dinosaurs in Yellowstone have lured a team of paleontologists in the same way that the legends of "Colter's Hell" and Jim Bridger's "Tall Tales" have attracted many before. Compared to other natural resources at Yellowstone National Park, fossils have received little attention. Except for the research conducted on the petrified forests, Yellowstone's fossils have remained a relative "paleo-incognita" more than 125 years after the park's establishment. As this survey demonstrates, the lack of paleontological research is not due to a lack of significant fossils. Perhaps historian Aubrey Haines provided the best explanation in his comment, "Past administrations preferred that resources not in the public's eye be left alone" (pers.