The New Force in Dewatering the New 2600 Series from ITT Flygt Consistent Performance Over Time
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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. -
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. -
The Archean Geology of Montana
THE ARCHEAN GEOLOGY OF MONTANA David W. Mogk,1 Paul A. Mueller,2 and Darrell J. Henry3 1Department of Earth Sciences, Montana State University, Bozeman, Montana 2Department of Geological Sciences, University of Florida, Gainesville, Florida 3Department of Geology and Geophysics, Louisiana State University, Baton Rouge, Louisiana ABSTRACT in a subduction tectonic setting. Jackson (2005) char- acterized cratons as areas of thick, stable continental The Archean rocks in the northern Wyoming crust that have experienced little deformation over Province of Montana provide fundamental evidence long (Ga) periods of time. In the Wyoming Province, related to the evolution of the early Earth. This exten- the process of cratonization included the establishment sive record provides insight into some of the major, of a thick tectosphere (subcontinental mantle litho- unanswered questions of Earth history and Earth-sys- sphere). The thick, stable crust–lithosphere system tem processes: Crustal genesis—when and how did permitted deposition of mature, passive-margin-type the continental crust separate from the mantle? Crustal sediments immediately prior to and during a period of evolution—to what extent are Earth materials cycled tectonic quiescence from 3.1 to 2.9 Ga. These compo- from mantle to crust and back again? Continental sitionally mature sediments, together with subordinate growth—how do continents grow, vertically through mafi c rocks that could have been basaltic fl ows, char- magmatic accretion of plutons and volcanic rocks, acterize this period. A second major magmatic event laterally through tectonic accretion of crustal blocks generated the Beartooth–Bighorn magmatic zone assembled at continental margins, or both? Structural at ~2.9–2.8 Ga. -
Focus on Genetics Important Plant 2016 Plant Conservation Conference Areas for Montana by Peter Lesica, Clark Fork Chapter by Peter Lesica, Clark Fork Chapter
Volume 29 No. 3 | Spring 2016 elseyaNewsletter of the Montana Native Plant Society Kelseya uniflora K ill. by Bonnie Heidel Approved: Two More Focus on Genetics Important Plant 2016 Plant Conservation Conference Areas for Montana By Peter Lesica, Clark Fork Chapter By Peter Lesica, Clark Fork Chapter he Montana Native Plant Society, along with the U.S. Forest Service, the MONTANA NOW HAS TWO NEW University of Montana Division of Biological Sciences, the Montana Natural IMPORTANT PLANT AREAS (IPAs), THeritage Program and the Natural Resources Conservation Service, hosted the approved during the February Plant Ninth Montana Plant Conservation Conference at the University of Montana in mid- Conservation Conference, bringing the February. More than 100 people attended, about half being MNPS members. total number of state IPAs to nine. Both The first day was dedicated to learning about population genetics and how new locales are in the southwest part of our molecular-based methods can help inform plant conservation. The three talks in the state — one is above treeline and the morning were conceptual in nature. Fred Allendorf from UM provided a refresher course other in a valley bottom. Descriptions on population genetics that helped provide a context for later talks. Loreen Allphin from of the new new IPAs, as well as of the Brigham Young University followed Fred, focusing on the importance of genetic variation previously approved sites, can be found to rare plant conservation and how using on the Montana Native Plant Society molecular markers can inform these efforts. new molecular-based website (http://www.mtnativeplants.org/ Matt Lavin from MSU ended the morning methods can help inform Important_Plant_Areas). -
Southwest MONTANA
visitvisit SouthWest MONTANA 2017 OFFICIAL REGIONAL TRAVEL GUIDE SOUTHWESTMT.COM • 800-879-1159 Powwow (Lisa Wareham) Sawtooth Lake (Chuck Haney) Horses (Michael Flaherty) Bannack State Park (Donnie Sexton) SouthWest MONTANABetween Yellowstone National Park and Glacier National Park lies a landscape that encapsulates the best of what Montana’s about. Here, breathtaking crags pierce the bluest sky you’ve ever seen. Vast flocks of trumpeter swans splash down on the emerald waters of high mountain lakes. Quiet ghost towns beckon you back into history. Lively communities buzz with the welcoming vibe and creative energy of today’s frontier. Whether your passion is snowboarding or golfing, microbrews or monster trout, you’ll find endless riches in Southwest Montana. You’ll also find gems of places to enjoy a hearty meal or rest your head — from friendly roadside diners to lavish Western resorts. We look forward to sharing this Rexford Yaak Eureka Westby GLACIER Whitetail Babb Sweetgrass Four Flaxville NATIONAL Opheim Buttes Fortine Polebridge Sunburst Turner remarkable place with you. Trego St. Mary PARK Loring Whitewater Peerless Scobey Plentywood Lake Cut Bank Troy Apgar McDonald Browning Chinook Medicine Lake Libby West Glacier Columbia Shelby Falls Coram Rudyard Martin City Chester Froid Whitefish East Glacier Galata Havre Fort Hinsdale Saint Hungry Saco Lustre Horse Park Valier Box Belknap Marie Elder Dodson Vandalia Kalispell Essex Agency Heart Butte Malta Culbertson Kila Dupuyer Wolf Marion Bigfork Flathead River Glasgow Nashua Poplar Heron Big Sandy Point Somers Conrad Bainville Noxon Lakeside Rollins Bynum Brady Proctor Swan Lake Fort Fairview Trout Dayton Virgelle Peck Creek Elmo Fort Benton Loma Thompson Big Arm Choteau Landusky Zortman Sidney Falls Hot Springs Polson Lambert Crane Condon Fairfield Great Ronan Vaughn Haugan Falls Savage De Borgia Plains Charlo Augusta CONTENTS Paradise Winifred Bloomfield St. -
A. Clifford Edwards, Esquire
“WHY DO YOU HURT ME SO?” By: A. Clifford Edwards, Esquire THE INTERNATIONAL ACADEMY OF TRIAL LAWYERS DEAN’S ADDRESS APRIL 7, 2017 SAN DIEGO, CALIFORNIA A Publication of the International Academy of Trial Lawyers Why Do You Hurt Me So? Good morning Academy! The opinions, express or implied, in this Dean’s Address are solely my own; nothing more, nothing less. President Burbidge; soon-to-be President Noël; fellow officers; my sisters and brothers of our special Academy, guests and my Edwards’ family supporting me here today; Page | 1 Susan – my wife, of such beauty, both of spirit and appearance, my soulmate, as hand-in-hand we experience our lives together; My cherished sons Christopher and John, the proudest achievements of my life; my best friends and only law partners; Their wives, my Daughters-in-law, Kelly and Hollis, who have so enriched and enhanced our Edwards’ family; And, an unexpected bonus that came into my life with her mother Susan over a decade ago when she was just 12, my stepdaughter Alex. Now, we welcome her significant, Patrick Lopach. Then, our little shining family Beacons, – the Edwards’ grandchildren – Ellie Marie, Wright, A.C. and Bella! Now please, you four, sit. Be still! Grandpa’s going to be givin’ a speech. Mother Nature I posit the title of my Dean’s Address – “Why Do You Hurt Me So?” as a troubled query from our wounded Mother of this beautiful and bountiful planet we each absorb every day of our lives. Susan and I share an instilled love for Mother Nature from our Montana upbringings. -
Quaternary and Late Tertiary of Montana: Climate, Glaciation, Stratigraphy, and Vertebrate Fossils
QUATERNARY AND LATE TERTIARY OF MONTANA: CLIMATE, GLACIATION, STRATIGRAPHY, AND VERTEBRATE FOSSILS Larry N. Smith,1 Christopher L. Hill,2 and Jon Reiten3 1Department of Geological Engineering, Montana Tech, Butte, Montana 2Department of Geosciences and Department of Anthropology, Boise State University, Idaho 3Montana Bureau of Mines and Geology, Billings, Montana 1. INTRODUCTION by incision on timescales of <10 ka to ~2 Ma. Much of the response can be associated with Quaternary cli- The landscape of Montana displays the Quaternary mate changes, whereas tectonic tilting and uplift may record of multiple glaciations in the mountainous areas, be locally signifi cant. incursion of two continental ice sheets from the north and northeast, and stream incision in both the glaciated The landscape of Montana is a result of mountain and unglaciated terrain. Both mountain and continental and continental glaciation, fl uvial incision and sta- glaciers covered about one-third of the State during the bility, and hillslope retreat. The Quaternary geologic last glaciation, between about 21 ka* and 14 ka. Ages of history, deposits, and landforms of Montana were glacial advances into the State during the last glaciation dominated by glaciation in the mountains of western are sparse, but suggest that the continental glacier in and central Montana and across the northern part of the eastern part of the State may have advanced earlier the central and eastern Plains (fi gs. 1, 2). Fundamental and retreated later than in western Montana.* The pre- to the landscape were the valley glaciers and ice caps last glacial Quaternary stratigraphy of the intermontane in the western mountains and Yellowstone, and the valleys is less well known. -
Montana's "Boodlers"
MONTANA'S "BOODLERS": MONTANANS AND THE AFTERMATH OF THE 1899 SENATORIAL SCANDAL by WILLIAM J. YAEGER 'll*- Submitted in Partial Fulfillment of the Requirements for Graduation with Honors to the Department of History at Carroll College Helena, Montana March, 1983 3 5962 00083 098 Tv This thesis for honors recognition has been approved for the Department of History. Director x fko-. 1 . <1 Reader ^7^/ j>z /are Date ii CONTENTS PREFACE...................................................................................................... iv Chapter I. FACTORS CONTRIBUTING TO BRIBERY IN U.S. SENATORIAL ELECTIONS................................................................. 1 II. THE "WAR" THAT LED TO A SCANDAL.............................................. 6 III. THE BUYING OF A LEGISLATURE.................................................... 13 IV. THE CHANDLER HEARING: THE RESIGNATION AND REAPPOINTMENT OF W.A. CLARK................................................... 27 V. AFTERAFFECTS OF MONTANA'S SCANDAL OF 1899............................ 34 VI. CONCLUSIONS..................................................................................... 40 APPENDIX A. THE VALEDICTORY OF SENATOR FRED WHITESIDE........................ 44 B. THE EVERETT BILL......................................................................... 47 SOURCES CONSULTED................................................................................... 51 i i i PREFACE As a newsman, I have had to endure accusations at various times that I (meaning my profession) had fabricated -
A Study of Early Utah-Montana Trade, Transportation, and Communication, 1847-1881
Brigham Young University BYU ScholarsArchive Theses and Dissertations 1959 A Study of Early Utah-Montana Trade, Transportation, and Communication, 1847-1881 L. Kay Edrington Brigham Young University - Provo Follow this and additional works at: https://scholarsarchive.byu.edu/etd Part of the Mormon Studies Commons, and the United States History Commons BYU ScholarsArchive Citation Edrington, L. Kay, "A Study of Early Utah-Montana Trade, Transportation, and Communication, 1847-1881" (1959). Theses and Dissertations. 4662. https://scholarsarchive.byu.edu/etd/4662 This Thesis is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. A STUDY OF EARLY UTAH-MONTANA TRADE TRANSPORTATION, AND COMMUNICATION 1847-1881 A Thesis presented to the department of History Brigham young university provo, Utah in partial fulfillment of the Requirements for the degree Master of science by L. Kay Edrington June, 1959 This thesis, by L. Kay Edrington, is accepted In its present form by the Department of History of Brigham young University as Satisfying the thesis requirement for the degree of Master of Science. May 9, 1959 lywrnttt^w-^jmrnmr^^^^ The writer wishes to express appreciation to a few of those who made this thesis possible. Special acknowledge ments are due: Dr. leRoy R. Hafen, Chairman, Graduate Committee. Dr. Keith Melville, Committee member. Staffs of; History Department, Brigham young university. Brigham young university library. L.D.S. Church Historian's office. Utah Historical Society, Salt lake City. -
Citizens United, Caperton, and the War of the Copper Kings Larry Howell Alexander Blewett I I School of Law at the University of Montana, [email protected]
Alexander Blewett III School of Law at the University of Montana The Scholarly Forum @ Montana Law Faculty Law Review Articles Faculty Publications 2012 Once Upon a Time in the West: Citizens United, Caperton, and the War of the Copper Kings Larry Howell Alexander Blewett I I School of Law at the University of Montana, [email protected] Follow this and additional works at: http://scholarship.law.umt.edu/faculty_lawreviews Part of the Election Law Commons Recommended Citation Larry Howell, Once Upon a Time in the West: Citizens United, Caperton, and the War of the Copper Kings , 73 Mont. L. Rev. 25 (2012), Available at: http://scholarship.law.umt.edu/faculty_lawreviews/14 This Article is brought to you for free and open access by the Faculty Publications at The choS larly Forum @ Montana Law. It has been accepted for inclusion in Faculty Law Review Articles by an authorized administrator of The choS larly Forum @ Montana Law. ARTICLES ONCE UPON A TIME IN THE WEST: CITIZENS UNITED, CAPERTON, AND THE WAR OF THE COPPER KINGS Larry Howell* He is said to have bought legislaturesand judges as other men buy food and raiment. By his example he has so excused and so sweetened corruption that in Montana it no longer has an offensive smell. -Mark Twain' [T]he Copper Kings are a long time gone to their tombs. -District Judge Jeffrey Sherlock 2 I. INTRODUCTION Recognized by even its strong supporters as "one of the most divisive decisions" by the United States Supreme Court in years,3 Citizens United v. * Associate Professor, The University of Montana School of Law. -
Geologic Map of the Divide Area Southwestern Montana
GEOLOGIC MAP OF THE DIVIDE AREA SOUTHWESTERN MONTANA Mapped and compiled by Susan M. Vuke Montana Bureau of Mines and Geology Open File Report MBMG 502 2004 Paleontology Text Revised— 10/04 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 GEOLOGY OF THE DIVIDE AREA Introduction The narrow Cenozoic valley shown on the geologic map and in Figures 1, 2, and 3 is referred to as Divide Valley in this report. The Cenozoic deposits of the Divide Valley are the focus of this map. Older units are included to show the relations of Cenozoic structures to pre-existing structures, and were mapped only in some areas adjacent to Cenozoic deposits. In all other areas, they were compiled and generalized from previous mapping with some reinterpretation in places. Geologic maps by O’Neill and others (1996), Smedes (1967), and Zen (1988) provide detail not shown on this map for pre-Cenozoic rocks. A central horst divides the valley into three parts: the northern, central (horst), and southern segments of this report. Segmentation of the valley is reflected in offset of Cenozoic deposits, and in the present-day position of the Big Hole River. Late Neogene During the late Neogene, an ancestral river flowed through the entire Divide Valley. Its course and flow direction changed several times. The central segment horst exposes deposits of this ancestral river (QTal) that likely underlie the entire Divide Valley.