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Canyon Ferry Reservoir Camping Regulations and Information
Canyon Ferry Reservoir Camping Regulations and Information Welcome to Canyon Ferry Recreation Area. The Bureau of Reclamation invites you to come and experience the abundance of wildlife and fishing opportunities available on your public lands around Canyon Ferry Reservoir. There are many recreation areas around the reservoir which include overnight campgrounds, day use areas, and group use shelters. To enhance your enjoyment and the enjoyment of others, campground regulations have been established through 43 CFR Part 423. Remember to be safe and enjoy your stay. Finding a Reservations for camping and group use shelters are now available. Reservations may be made at www.recreation.gov or by calling the toll-free reservation line at1-877-444-6777 (10:00 AM Campsite - 10:00 PM MST). Reservations can be made up to six months prior to visit. Campsites unreserved are available on a first-come,first-serve for the unreserved date(s). Walk in campsites or campsites unreserved are available first-come, first-served basis and cannot be reserved. Camping is allowed in designated campsites only. To declare occupancy of a walk in campsite, you must have a tent, camper or camp trailer in the campsite. Within 30 minutes of choosing a campsite, fill out a fee envelope and deposit it in the fee tube. Place the completed envelope receipt in the clip on the numbered site post. Pay only for the nights you know you will be camping. No refunds are available. You must not attempt to reserve a campsite for future use by placing equipment or other items on the campsite, or by personal appearance, without camping on and paying the required fees for that campsite daily. -
Geology of Part of the Townsend Valley Broadwater and Jefferson
Geology of Part of the Townsend Valley Broadwater and Jefferson » Counties,x Montana GEOLOGICAL SURVEY BULLETIN 1042-N CONTRIBUTIONS TO ECONOMIC GEOLOGY GEOLOGY OF PART OF THE TOWNSEND VALLEY BROADWATER AND JEFFERSON COUNTIES, MONTANA By V. L. FREEMAN, E. T. RUPPEL, and M. R. KLEPPER ABSTRACT The Townsend Valley, a broad intermontane basin in west-central Montana, extends from Toston to Canyon Ferry. The area described in this report includes that part of the valley west of longitude 111° 30' W. and south of latitude 46° 30' N. and the low hills west and south of the valley. The Missouri River enters the area near Townsend and flows northward through the northern half of the area. Three perennial tributaries and a number of intermittent streams flow across the area and into the river from the west. The hilly parts of the area are underlain mainly by folded sedimentary rocks ranging in age from Precambrian to Cretaceous. The broad pediment in the southwestern part is underlain mainly by folded andesitic volcanic rocks of Upper Cretaceous age and a relatively thin sequence of gently deformed tuffaceous rocks of Tertiary age. The remainder of the area is underlain by a thick sequence of Tertiary tuffaceous rocks that is partly blanketed by late Tertiary and Quater nary unconsolidated deposits. Two units of Precambrian age, 13 of Paleozoic age, 7 of Mesozoic age, and several of Cenozoic tuffaceous rock and gravel were mapped. Rocks of the Belt series of Precambrian age comprise a thick sequence of silt- stone, sandstone, shale, and subordinate limestone divisible into the Greyson shale, the Spokane shale, and the basal part of the Empire shale, which was mapped with the underlying Spokane shale. -
Fall 2016 Golden Eagle Migration Survey Big Belt Mountains, Montana
1 Fall 2016 Golden Eagle Migration S urvey Big Belt Mountains, Montana Photo by Ronan Dugan Montana Audubon, Helena, Montana March 2017 2 Fall 2016 Golden Eagle Migration Survey Big Belt Mountains, Montana Report submitted to: Helena - Lewis & Clark National Forest ATTN: Denise Pengeroth, Forest Biologist 3425 Skyway Drive, Helena, MT 59602 Report prepared by: Jeff Grayum, Ronan Dugan, & Steve Hoffman Counts conducted by: Ronan Dugan & Jeff Grayum Project coordinated by : Montana Audubon, Inc. Project Coordinator: Steve Hoffman P.O. Box 595, Helena, MT 59624 (406) 443 - 3949 March 2017 3 Table of Contents List of Tables ................................ ................................ ................................ .............................. 3 List of Figures ................................ ................................ ................................ ............................. 4 Introduction ................................ ................................ ................................ ................................ 5 Study Site ................................ ................................ ................................ ................................ .... 6 Methods ................................ ................................ ................................ ................................ ...... 8 Results and Discussion ................................ ................................ ................................ ................ 9 Observ ation Effort and Weather Summary ............................... -
GEOLOGY and OIL and GAS PROSPECTS of the HUNTLEY FIELD, Montanj
GEOLOGY AND OIL AND GAS PROSPECTS OF THE HUNTLEY FIELD, MONTANj By E. T. HANCOCK. INTRODUCTION. The Huntley field is in Yellowstone and Big Horn counties, south- central Montana, and embraces an area of about 650 square miles, part of which lies northwest and part southeast of Yellowstone River. The field has railroad facilities that are exceptionally good for this general region, being traversed by the main lines of the Northern Pacific and the Chicago, Burlington & Quincy railroads. These roads furnish excellent shipping facilities at Huntley, Warden, Ballantine, Pompeys Pillar, and other points. Acknowledgments. In presenting this report the writer desires to express his thanks to David White for valuable suggestions and criticisms, to T. W. Stanton and F. H. Knowlton for the identifica tion of fossils, and to C. E. Dobbins for assistance in the detailed mapping. He also wishes to call attention to the public service rendered by oil and gas operators who have furnished records of deep borings and by individuals who have contributed in various ways to the success of the investigation. Earlier investigations. The Huntley field is in reality an ex tension of the Lake Basin field, which was mapped by the writer during the summer of 1916.1 The geologic investigation of the region including the Lake Basin and Huntley fields began with the Northern Transcontinental Survey of 1882. Prior to that time geologists had described certain struc tural features and the stratigraphic succession at points closely ad jacent to these fields, such as Judith Gap, the canyon of the North Fork of the- Musselshell, and the Bridger Range, but almost noth ing had been written concerning the geology of the area herein de scribed. -
Compilation of Reported Sapphire Occurrences in Montana
Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area .................................... -
Lazy J Brochure
LAZY J RANCH Offered Exclusively by TABLE OF CONTENTS INTRODUCTION 1 LOCATION & ACCESS 2 PHYSICAL & OPERATIONAL 3 ELEVATION, CLIMATE & PRECIPITATION 4 WATER RIGHTS & MINERAL RIGHTS 5 IMPROVEMENTS 7 ZONING & CONSERVATION EASEMENTS 8-9 FAMILY HISTORY 12 AREA HISTORY 13 RECREATION 14 UTILITIES & SERVICES AND TAXES 15 FENCES & BOUNDARY LINES 15 SUMMARY STATEMENT 16 OFFERING PRICE & CONDITIONS OF SALE 17 STATE OF MONTANA MAP 18 INTRODUCTION In the heart of Bridger Canyon in Southwest Montana, the Lazy J Ranch consists of approximately 5,665 deeded acres of alpine and mountain-meadow land. The Ranch is the largest remaining privately-held block of land in this pristine Rocky Mountain setting. Tucked against the famed Bridger Mountain Range, the Ranch possesses dramatic vistas of the Bridger Mountains and nearby Bangtail Range. It is a comfortable fifteen-minute drive on State Highway 86 (Bridger Canyon Road) to downtown Bozeman. The proximity of the Ranch to a commercial airport, private FBOs and interstate travel within a 25-minute drive make it readily accessible year-round. The secluded trout waters of Bridger Creek course through the core of the Ranch for nearly three miles. This quality alpine-fishing stream hosts healthy populations of brook and rainbow trout. The west side of the Ranch borders the Bridger Bowl Ski Resort and approximately three and a half miles of the Gallatin National Forest, providing unlimited hunting and recreational opportunities. The varied ecosystem of mountains, alpine meadows, and grassy creek bottoms offers prime habitat for an abundance of Rocky Mountain wildlife including elk, mule deer, whitetail deer, bear, mountain lion, moose, and upland game birds. -
High Elevation Cultural Use of the Big Belt Mountains: a Possible Mountain Tradition Connection
St. Cloud State University theRepository at St. Cloud State Culminating Projects in Cultural Resource Management Department of Anthropology 5-2020 High Elevation Cultural Use of the Big Belt Mountains: A Possible Mountain Tradition Connection Arian Randall Follow this and additional works at: https://repository.stcloudstate.edu/crm_etds Recommended Citation Randall, Arian, "High Elevation Cultural Use of the Big Belt Mountains: A Possible Mountain Tradition Connection" (2020). Culminating Projects in Cultural Resource Management. 34. https://repository.stcloudstate.edu/crm_etds/34 This Thesis is brought to you for free and open access by the Department of Anthropology at theRepository at St. Cloud State. It has been accepted for inclusion in Culminating Projects in Cultural Resource Management by an authorized administrator of theRepository at St. Cloud State. For more information, please contact [email protected]. High Elevation Cultural Use of the Big Belt Mountains: A Possible Mountain Tradition Connection by Arian L. Randall A Thesis Submitted to the Graduate Faculty of St. Cloud State University in Partial Fulfillment of the Requirements for the Degree Master of Science in Cultural Resource Management, Archaeology May 6, 2020 Thesis Committee: Mark Muñiz, Chairperson Rob Mann Lauri Travis 2 Abstract The Sundog site (24LC2289) was first discovered in 2013 during a field school survey with Carroll College and the Helena-Lewis & Clark National Forest. This archaeological site is located at an elevation of 6,400ft above sea-level in the Northern Big Belt Mountains in Montana. The Sundog Site is a multi- component site with occupations from the Late Paleoindian period to the Late Prehistoric period. This site is significant due to its intact cultural deposits in a high-altitude park, in an elevational range that currently has a data gap. -
Spatial Variations in Snow Stability on Uniform Slopes
SPATIAL VARIATIONS IN SNOW STABILITY ON UNIFORM SLOPES: IMPLICATIONS FOR EXTRAPOLATION TO SURROUNDING TERRAIN by Christopher Cameron Landry A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences MONTANA STATE UNIVERSITY Bozeman, Montana April 2002 COPYRIGHT by Christopher Cameron Landry 2002 All Rights Reserved ERRATA The author, Christopher C. Landry, wishes to inform readers of the Master of Science thesis titled "Spatial variations in snow stability on uniform slopes: implications for extrapolation to surrounding terrain", published April 2002, of an error in the statistical analyses of project results. T-statistic tests were mistakenly performed at p < 0.10 rather than at p < 0.05. Nonetheless, re-performing the T-statistic analyses at p < 0.05 altered the results only marginally, and the conclusions of the research remain unchanged. Subsequent to the publication of the thesis, and the discovery of this error, a peer- reviewed article was submitted, using an alternative statistical approach, and published in Cold Regions Science and Technology. Readers of the original these are referred to the following article: Landry, C., K. Birkeland, K. Hansen, J. Borkowski, R. Brown and R. Aspinall. 2004. Variations in snow strength and stability on uniform slopes. Cold Regions Science & Technology, Vol. 39, p. 205-218. APPROVAL of a thesis submitted by Christopher Cameron Landry This thesis has been read by each member of the thesis committee and has been found to be satisfactory regarding content, English usage, format, citations, bibliographic style, and consistency, and is ready for submission to the College of Graduate Studies. -
Nonforested Terrestrial Ecosystems Report
Assessment Forest Plan Revision Final Nonforested Terrestrial Ecosystems Report Prepared by: Kim Reid Rangeland Management Specialist for: Custer Gallatin National Forest February 16, 2017 1 Custer Gallatin National Forest Assessment – Nonforested Terrestrial Ecosystems Contents Introduction .................................................................................................................................................. 1 Process, Methods and Existing Information Sources .................................................................................... 2 Scale .............................................................................................................................................................. 3 Current Forest Plan Direction ....................................................................................................................... 4 Custer Forest Plan ..................................................................................................................................... 4 Gallatin Forest Plan ................................................................................................................................... 7 Existing Condition ......................................................................................................................................... 7 Key Ecosystem Components ..................................................................................................................... 7 Structure and Composition .................................................................................................................. -
Geologic Map of the Sedan Quadrangle, Gallatin And
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY GEOLOGIC INVESTIGATIONS SERIES I–2634 Version 2.1 A 25 20 35 35 80 rocks generally fall in the range of 3.2–2.7 Ga. (James and Hedge, 1980; Mueller and others, 1985; Mogk and Henry, Pierce, K.L., and Morgan, L.A., 1992, The track of the Yellowstone hot spot—Volcanism, faulting, and uplift, in Link, 30 5 25 CORRELATION OF MAP UNITS 10 30 Kbc Billman Creek Formation—Grayish-red, grayish-green and gray, volcaniclastic mudstone and siltstone ၤ Phosphoria and Quadrant Formations; Amsden, Snowcrest Range and Madison Groups; and Three Overturned 45 20 10 30 20 P r 1988; Wooden and others, 1988; Mogk and others, 1992), although zircons have been dated as old as 3.96 Ga from P.K., Kuntz, M.A., and Platt, L.B., eds., Regional geology of eastern Idaho and western Wyoming: Geological 40 Ksms 45 Kh interbedded with minor volcanic sandstone and conglomerate and vitric tuff. Unit is chiefly 30 30 25 45 45 Forks Formation, Jefferson Dolomite, Maywood Formation, Snowy Range Formation, Pilgrim Ksl 5 15 50 SURFICIAL DEPOSITS quartzites in the Beartooth Mountains (Mueller and others, 1992). The metamorphic fabric of these basement rocks has Society of America Memoir 179, p. 1–53. 15 20 15 Kbc volcaniclastic mudstone and siltstone that are gray and green in lower 213 m and grayish red above; Estimated 40 Qc 5 15 Qoa Limestone, Park Shale, Meagher Limestone, Wolsey Shale, and Flathead Sandstone, undivided in some cases exerted a strong control on the geometry of subsequent Proterozoic and Phanerozoic structures, Piombino, Joseph, 1979, Depositional environments and petrology of the Fort Union Formation near Livingston, 15 25 Ksa 50 calcareous, containing common carbonaceous material and common yellowish-brown-weathering 60 40 20 15 15 (Permian, Pennsylvanian, Mississippian, Devonian, Ordovician, and Cambrian)—Limestone, Ksa 20 10 10 45 particularly Laramide folds (Miller and Lageson, 1993). -
Inactive Mines on Gallatin National Forest-Administered Land
Abandoned-Inactive Mines on Gallatin National Forest-AdministeredLand Montana Bureau of Mines and Geology Abandoned-Inactive Mines Program Open-File Report MBMG 418 Phyllis A. Hargrave Michael D. Kerschen CatherineMcDonald JohnJ. Metesh PeterM. Norbeck RobertWintergerst Preparedfor the u.s. Departmentof Agriculture ForestService-Region 1 Abandoned-Inactive Mines on Gallatin National Forest-AdministeredLand Open-File Report 418 MBMG October 2000 Phyllis A. Hargrave Michael D. Kerschen Catherine McDonald John J. Metesh Peter M. Norbeck Robert Wintergerst for the U.S. Department of Agriculture Forest Service-Region I Prepared Contents List of Figures .V List of Tables . VI IntToduction 1 1.IProjectObjectives 1 1.2AbandonedandInactiveMinesDefined 2 1.3 Health and Environmental Problems at Mines. 3 1.3.1 Acid-Mine Drainage 3 1.3.2 Solubilities of SelectedMetals 4 1.3.3 The Use of pH and SC to Identify Problems. 5 1.4Methodology. 6 1.4.1 Data Sources : 6 1.4.2Pre-Field Screening. 6 1.4.3Field Screening. 7 1.4.3.1 Collection of Geologic Samples. 9 1.4.4 Field Methods ' 9 1.4.4.1 Selection of Sample Sites 9 1.4.4.2 Collection of Water and Soil Samples. 10 1.4.4.3 Marking and Labeling Sample Sites. 10 1.4.4.4ExistingData 11 1.4.5 Analytical Methods """"""""""""""""'" 11 1.4.6Standards. 12 1.4.6.1Soil Standards. 12 1.4.6.2Water-QualityStandards 13 1.4.7 Analytical Results 13 1.5 Gallatin National Forest 14 1.5.1 History of Mining 16 1.5.1.1 Production 17 1.5.1.2Milling 18 1.6SummaryoftheGallatinNationaIForestInvestigat~on 19 1.7 Mining Districts and Drainages 20 Gallatin National Forest Drainages 20 2.1 Geology "' ' '..' ,.""...' ""." 20 2.2 EconomicGeology. -
Proposed Action–Revised Forest Plan, Custer Gallatin National Forest
United States Department of Agriculture Proposed Action–Revised Forest Plan, Custer Gallatin National Forest Forest Service January 2018 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 (for example, 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.