Comparative Study of the Economic and Business Potential of Chouteau and Teton Counties
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Highwood Mountains Range Analysis Project Area on Those Resources Affected by Implementation
United States Department of Agriculture Environmental Forest Service Assessment 2015 Highwood Mountains Range Judith Ranger District, Lewis and Clark National Forest Cascade, Choteau and Judith Basin Counties, Montana For More Information Contact: Lewis and Clark National Forest Judith Ranger District Standford, Montana www.fs.fed.us/r1/lewisclark/projects 406-566-2292. The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or part of an individual’s income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at (202) 720-2600 (voice and TTY). To file a complaint of discrimination, write to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, SW., Washington, DC 20250-9410, or call (800) 795-3272 (voice) or (202) 720-6382 (TTY). USDA is an equal opportunity provider and employer. Environmental Assessment Table of Contents Introduction ...................................................................................................................................................4 Location of the Proposed Project Area ..........................................................................................................4 -
Description of the Fort Benton Quadrangle
DESCRIPTION OF THE FORT BENTON QUADRANGLE. INTRODUCTION. steeply inclined sides. In the center of the range of the throat of a volcano, the dikes which radiate heat and cold, varying greatly, of course, with the the limestones and other stratified rocks are hori from these centers of activity, and the loose mate altitude. The annual rainfall is from 13 to 20 General relations. The Fort Benton quad zontal, or nearly so, while on the flanks structure of rials and lava flows of which the cones Structure_. , of. inches, being greatest in the mountains; June and rangle extends in longitude from 110° to 111° of the mountains they are sharply BheuLMoun- were built. The sedimentary strata October are the rainy months. The snowfall is and in latitude from 47° to 48°. It is inclined and dip away from the moun through which the volcanoes broke up heavy and the mountain tracts are well watered. 69.25 miles Ions; from north to south. extent°ofan tains to the lower plains country. The horizontal and upon which their materials accumulated are, Agriculture is therefore confined to the foothills . quadrangle. 47.36 miles wide, and contains 3272.7 attitude is well shown in the rocks of Belt Park, over most of the area, nearly horizontal or inclined and stream bottoms, except where irrigation is square miles. It includes part of Choteau, the whereas farther north the mountain masses near gently to the north. These rocks belong entirely possible. northwest corner of Fergus, and the eastern part Monarch are formed of blocks of tilted limestones to the Cretaceous system, and denudation has Culture. -
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. -
Paleontology and Stratigraphy of Upper Coniacianemiddle
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- Published Research US Geological Survey 2005 Paleontology and stratigraphy of upper Coniacianemiddle Santonian ammonite zones and application to erosion surfaces and marine transgressive strata in Montana and Alberta W. A. Cobban U.S. Geological Survey T. S. Dyman U.S. Geological Survey, [email protected] K. W. Porter Montana Bureau of Mines and Geology Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Part of the Earth Sciences Commons Cobban, W. A.; Dyman, T. S.; and Porter, K. W., "Paleontology and stratigraphy of upper Coniacianemiddle Santonian ammonite zones and application to erosion surfaces and marine transgressive strata in Montana and Alberta" (2005). USGS Staff -- Published Research. 367. https://digitalcommons.unl.edu/usgsstaffpub/367 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- Published Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Cretaceous Research 26 (2005) 429e449 www.elsevier.com/locate/CretRes Paleontology and stratigraphy of upper Coniacianemiddle Santonian ammonite zones and application to erosion surfaces and marine transgressive strata in Montana and Alberta W.A. Cobban a,1, T.S. Dyman b,*, K.W. Porter c a US Geological Survey, Denver, CO 80225, USA b US Geological Survey, Denver, CO 80225, USA c Montana Bureau of Mines and Geology, Butte, MT 59701, USA Received 28 September 2004; accepted in revised form 17 January 2005 Available online 21 June 2005 Abstract Erosional surfaces are present in middle and upper Coniacian rocks in Montana and Alberta, and probably at the base of the middle Santonian in the Western Interior of Canada. -
Postill Creek Ranch Geraldine, Montana
POSTILL CREEK RANCH GERALDINE, MONTANA $1,800,000 | 933± ACRES LISTING AGENT: TIM MURPHY 1227 NORTH 14TH AVENUE, SUITE 1 BOZEMAN, MONTANA 59715 P: 406.587.3090 M: 406.209.0644 [email protected] POSTILL CREEK RANCH GERALDINE, MONTANA $1,800,000 | 933± ACRES LISTING AGENT: TIM MURPHY 1227 NORTH 14TH AVENUE, SUITE 1 BOZEMAN, MONTANA 59715 P: 406.587.3090 M: 406.209.0644 [email protected] Land… that’s where it all begins. Whether it is ranch land or family retreats, working cattle ranches, plantations, farms, estancias, timber or recreational ranches for sale, it all starts with the land. Since 1946, Hall and Hall has specialized in serving the owners and prospective owners of quality rural real estate by providing mortgage loans, appraisals, land management, auction and brokerage services within a unique, integrated partnership structure. Our business began by cultivating long-term relationships built upon personal service and expert counsel. We have continued to grow today by being client-focused and results-oriented—because while it all starts with the land, we know it ends with you. WITH OFFICES IN: DENVER, COLORADO BOZEMAN, MONTANA EATON, COLORADO MISSOULA, MONTANA STEAMBOAT SPRINGS, COLORADO VALENTINE, NEBRASKA SUN VALLEY, IDAHO COLLEGE STATION, TEXAS TETON VALLEY, IDAHO LAREDO, TEXAS HUTCHINSON, KANSAS LUBBOCK, TEXAS BUFFALO, WYOMING MELISSA, TEXAS BILLINGS, MONTANA SOUTHEASTERN US SALES | AUCTIONS | FINANCE | APPRAISALS | MANAGEMENT © 2020 HALL AND HALL | WWW.HALLANDHALL.COM | [email protected] — 2 — EXECUTIVE SUMMARY Postill Creek Ranch is a 933± acre mountain retreat located on the northeastern flank of the Highwood Mountains in central Montana. The Highwood Mountains are an island mountain range rising above a prairie ecosystem with fertile farmlands to over 7,600 feet in elevation. -
University of Montana Commencement Program, 1975
University of Montana ScholarWorks at University of Montana University of Montana Commencement Programs, 1898-2020 Office of the Registrar 6-15-1975 University of Montana Commencement Program, 1975 University of Montana (Missoula, Mont. : 1965-1994). Office of the Registrar Follow this and additional works at: https://scholarworks.umt.edu/um_commencement_programs Let us know how access to this document benefits ou.y Recommended Citation University of Montana (Missoula, Mont. : 1965-1994). Office of the Registrar, "University of Montana Commencement Program, 1975" (1975). University of Montana Commencement Programs, 1898-2020. 78. https://scholarworks.umt.edu/um_commencement_programs/78 This Program is brought to you for free and open access by the Office of the Registrar at ScholarWorks at University of Montana. It has been accepted for inclusion in University of Montana Commencement Programs, 1898-2020 by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. SEVENTY-EIGHTH ANNUAL COMMENCEMENT UNIVERSITY OF MONTANA MISSOULA SUNDAY, JUNE THE FIFTEENTH NINETEEN HUNDRED AND SEVENTY-FIVE FIELD HOUSE AUDITORIUM THE MARSHALS James H. Lowe Chairman, Faculty Senate Associate Professor of Forestry Walter L. Brown R. Keith Osterheld Professor o f English Professor of Chemistry ORDER OF EXERCISES PROCESSIONAL BRASS ENSEMBLE AND ORGAN Lance Boyd, Director John Ellis, Organ PROCESSION Marshals, the Colors, Candidates for Degrees, the Faculty, Members of the Governing Boards, Guests of Honor, the President PRESENTATION OF COLORS NATIONAL ANTHEM The Star Spangled Banner O, say! can you see by the dawn’s early light, What so proudly we hailed at the twilight’s last gleaming, Whose broad stripes and bright stars, through the perilous flight O’er the ramparts we watched, were so gallantly streaming? And the rockets’ red glare, the bombs bursting in air, Gave proof through the night that our flag was still there. -
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. -
Ichthyoplankton Density and Shovelnose Sturgeon Spawning
ICHTHYOPLANKTON DENSITY AND SHOVELNOSE STURGEON SPAWNING IN RELATION TO VARYING DISCHARGE TREATMENTS by Benjamin Joseph Goodman A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Fish and Wildlife Management MONTANA STATE UNIVERSITY Bozeman, Montana July 2009 © COPYRIGHT by Benjamin Joseph Goodman 2009 All Rights Reserved ii APPROVAL of a thesis submitted by Benjamin Joseph Goodman This thesis has been read by each member of the thesis committee and has been found to be satisfactory regarding content, English usage, format, citation, bibliographic style, and consistency, and is ready for submission to the Division of Graduate Education. Dr. Christopher S. Guy Approved for the Department of Ecology Dr. David W. Roberts Approved for the Division of Graduate Education Dr. Carl A. Fox iii STATEMENT OF PERMISSION TO USE In presenting this thesis in partial fulfillment of the requirements for a master’s degree at Montana State University, I agree that the Library shall make it available to borrowers under the rules of the Library. If I have indicated my intention to copyright this thesis by including a copyright notice page, copying is allowable only for scholarly purposes, consistent with “fair use” as prescribed in the U.S. Copyright Law. Requests for permission for extended quotation from or reproduction of this thesis in whole or in parts may be granted only by the copyright holder. Benjamin Joseph Goodman July 2009 iv ACKNOWLEDGMENTS I thank Nick Peterson and Jenn Ard for their superhuman efforts as technicians that made this study possible. Many thanks to Bill Gardner for contributing his indispensable Missouri River expertise to the design and implementation of this research. -
Dutton, MT 59433
Productive Teton County Farmland 0 4th Lane NE, Dutton, MT 59433 Offered at $575,000 Presented Exclusively by Trampus Corder, Broker Staci Corder, Broker 833-783-3224 toll free 406-622-3224 office [email protected] Property Information Acres: 400 Deeded (15.375 Grazing acres; 384.625 Fallow acres) Taxes: $970.42 (2020) Legal: S19, T24 N, R02 W, NE4; S13, T24 N, R03 W, E2SE; S24, T24 Utilities: Power on east side along county road Hunting District: 404 Executive Summary The smell of freshly turned black top-soil dense with nutrients beginsFort the Benton growing Farm season. There is nothing more satisfying than trudgingChouteau through County, thick,Montana, jade 1280.0 colored AC +/- winter wheat and watching the heads fill with protein-rich grain. The late summer months ripen the wheat to a beautiful gold that resembles waves of amber. These 400 acres of farm ground are 10 miles from Dutton, Montana and lie in the sacred Golden Triangle that stretches from Conrad to Havre and anchors in Great Falls. This region produces more wheat than most other regions in the entire country. Weather conditions, soil type, and soil nutrients all combine to form the ideal growing conditions for wheat, barley and other small grain crops. The property is in close proximity to grain elevators. The 100% base acres on the farm ground typically yield 76+ bushels per acre of winter wheat. Conservation remains an utmost priority and is demonstrated by the seller’s diligent dozer work to eradicate erosion. Power stretches alongside the county road on the eastern border of the property. -
Chouteau County, Tommy, 61 MT] 3Rd Printing, August 1974
Trails, Trials and Tributes, 3rd printing Family, 69 Trails, Trials and Tributes. James & Violet, 69 Compiled by The Egly Country Club (Home Thomas & Etta, 69 Demonstration Club), 1958. [Chouteau County, Tommy, 61 MT] 3rd Printing, August 1974. Throughout the ARTHURS book, pages containing photos were labeled with John, 23 an “a” designation, (example, 62a) in order to ASHMOOR-GENOU SECTION, 34, 53 index those pages. Five unnumbered pages at the ATKINSON back (homestead sections) were labeled 104a- Edith, 28 104f, for the purpose of indexing. The use of this AYERS index is permitted so long as it is not Mr. & Mrs., 22 commercially sold. JT, 07.31.2009. Store, 22 AZNOE, 53 ABERNATHY A., 104d, 104e BAKER G., 104e Joseph A., 8 J., 104d Myrtle, Miss (teacher), 67 John, 104d BALLARD ABRAMS C., 104d Del, Mrs., 80 BANNACK, 5 ADAMS BARBED WIRE ROUNDUP, 18, 20, 24, 28, R., 104c 100 ALBERS BARBER John, 82 R., 104b ALLEN Roy, 10, 77, 78 Marian, 63, 89 BARKER ALLISON Mines, 7 Mary, 63 BARNES AMERICAN FUR COMPANY, 5 J., 104a AMOS, 10 J. J., & Mrs., 91-92 O., 104b Jim, 104a AMES Joe, 92, 104a C., 104a R., 104b Charley, 101, & Lena J. Michels, 41-42 Roy, 10 Family, 40a Wesley, 92 Howard, 42 BARTLETT W., 104a Bill, 73 AMMERMAN E. J., (Bud), 40a, 104c, & Margaret A., 104a (Maggie), 70, 73 M., 104a Gladys, 40a, 70 ANDERS Irving, 47 R., 104e Mayme, 69-70 ANDERSON Oscar, Mrs., 38, 40a A. 104d Oscar, 90, 104c, & Mayme, 56, 69-71, C., 104d 91 H., 104a School, 56 Jack, acknowledgements W., 104c ARCHER BARTLEY Neal, 58 H. -
Investigators' Annual Reports Yellowstone
1999 INVESTIGATORS’ ANNUAL REPORTS YELLOWSTONE NATIONAL PARK YELLOWSTONE NATIONAL PARK ABS u89 AR O GE K A im J R RAN on A y Dome Mountain ee n N a C G nk a Y E LATIN OTO Ranch Corwin Springs GAL GALLATIN NATIONAL FOREST Gardiner Hellroaring McLaren Deckard Flats Mountain Mine Site ing Cr. r. Electric Peak Cr. ar Cooke City hC ro alo g ll ff Silver Gate Mammoth u e Slou G H B a rd Ga n Swan Rive er ll tin r Camp a Lake reek Ri Bunsen SHOSHO Roosevelt Buffalo C ve Peak e r Ranch tt lCr. u Tower B sta da ry So C AB Mt. NE NATIO SA ver Holmes Ri R e O Co ton La KA ug Canyon ws m NAL ar ar C Ye l l o R r e Norris Ri A GALLATIN NATIONAL FOREST ek v N e G Madiso r FOREST E Hay er k Vall iv e nR Madison de e er r West iv ey n Gibbo n R C . n Yellowstone Cr Fishing ca t eli er e Creek u P c o ez Per Bridge iv N Tr R Lake ole ireh F Cody To Old Faithful Yellowstone Lake Mt. Doane West AB Shoshone Mt. SA Lake Thumb Stevenson R Grant O K A Lewis k R e Eagle Y A re Lake el Heart lo N C iver Peak l w G e R r Lake st z E e er u o iv hl Mt. n O c e R e B s Sheridan eCreek s R wi iv Bechler u e o r Meadows Le Gr ke na R Thor TARGHEE NATIONAL FOREST S iver ofare Cr. -
Highwood Mountains, Montana
Bulletin No. 237 Series j ft ?e?criPtlv« Gwl°^ 43 , 90 \ D, Petrography and Mineralogy, 29 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR PETROGRAPHY AND GEOLOGY OF THE IGNEOUS ROCKS OF THE HIGHWOOD MOUNTAINS, MONTANA BY LOUIS VALENTINE PIRSSO1ST WASHINGTON GOVERNMENT PRINTING OFFICE 1905 CONTENTS. Page. Letter of transmittal. .......................^............................ 11 Introduction__._.._._.____..--.-----_--.------..--.---...---- .-.------ 13 Bibliography ___.._______. __.__._____..---.._..-------.--.-..----..-..- 14 Chapter I. Geography and history ........----.-....-..--...-.----..----- 14 Location ..__._.._.._____..---..._------- --------------------. 14 Bibliography .. ...-.-...-..----.-_.._. ...... ....................:...... 15 Topography and geography .......................:.-.------.------.- 15 History................................................................. 16 Chapter II. Geology of the igneous stocks ................................ 20 Introductory ................................................... ------ 20 Highwood Peak stock....-.-.-..........-._.....--...-.---_.-.--._... 20 Character of the border contact.-..-.-.-..-..-.--...-----..-.--.- 22 Middle Peak stock.................................................. 23 Contact phenomena. -..---.......---------. -..-..-..--------.-.-- 23 Endomorphic contact phenomena ..........^..................... 24 East Peak stock....................................................... 24 Shonkin stock ...................... ....-'---.--...--".-...-.---.-.---.-