Geology of Glacier National Park and the Flathead Region, Northwestern Montana

Total Page:16

File Type:pdf, Size:1020Kb

Geology of Glacier National Park and the Flathead Region, Northwestern Montana USGS: Geological Survey Professional Paper 296: Geology of Glacier National Park And the Flathead Region, Northwestern Montana Geological Survey Professional Paper 296 Geology of Glacier National Park And the Flathead Region, Northwestern Montana GEOLOGY OF GLACIER NATIONAL PARK AND THE FLATHEAD REGION, NORTHWESTERN MONTANA By Clyde P. Ross http://www.nps.gov/history/history/online_books/geology/publications/pp/296/index.htm[3/13/2014 5:25:22 PM] USGS: Geological Survey Professional Paper 296: Geology of Glacier National Park And the Flathead Region, Northwestern Montana GEOLOGICAL SURVEY PROFESSIONAL PAPER 296 1959 TABLE OF CONTENTS pp/296/index.htm Last Updated: 08-Jul-2008 http://www.nps.gov/history/history/online_books/geology/publications/pp/296/index.htm[3/13/2014 5:25:22 PM] USGS: Geological Survey Professional Paper 296 (Contents) Geological Survey Professional Paper 296 Geology of Glacier National Park And the Flathead Region, Northwestern Montana TABLE OF CONTENTS Cover Abstract Introduction Location Scope Acknowledgments Previous publications Geography Nomenclature of the ranges Drainage Relief Climate Transportation Resources General geology Stratigraphy Outline of major points Belt series (Precambrian) Classification Ravalli group Altyn limestone Appekunny argillite Grinnell argillite Piegan group Siyeh limestone Missoula group Correlations and divisions Main body Greenish calcareous argillite Purcell basalt Shepard formation Limestone Chemical composition of rocks of the Belt series Precambrian intrusive rocks Paleozoic strata Basis for divisions used http://www.nps.gov/history/history/online_books/geology/publications/pp/296/contents.htm[3/13/2014 5:25:23 PM] USGS: Geological Survey Professional Paper 296 (Contents) Cambrian rocks Devonian rocks Upper Paleozoic rocks Mesozoic rocks Jurassic rocks Cretaceous rocks Kootenai formation Colorado shale Montana group St. Mary River formation Undifferentiated Cretaceous deposits Cenozoic strata Old alluvium and associated deposits Terrace alluvium Glacial deposits Modern alluvium Landslide detritus Structure Structural highlights Broad flexures or warps Precambrian structural features Paleozoic structural features Mesozoic structural features Mountain-building structural features Lewis overthrust Thrusts in the eastern disturbed zone Folds of the disturbed zone Structural features in the overthrust block Steep master faults Steep minor faults Interpretation of the structure General structural features Erosion thrust concept Dates of deformation The concept of a sole Depth of fracture Uplift Displacement Structural features above the thrust Present shape of the Lewis thrust Adjustments after the thrusting Summary of structural interpretation Geomorphology General features of the geomorphology Effects of the early Tertiary uplift Concepts as to a summit peneplain Blackfoot erosional surface Post-Blackfoot erosional features Glacial features Recent erosional features Literature cited Index (omitted from the online edition) http://www.nps.gov/history/history/online_books/geology/publications/pp/296/contents.htm[3/13/2014 5:25:23 PM] USGS: Geological Survey Professional Paper 296 (Contents) ILLUSTRATIONS PLATE 1. Reconnaissance geologic map of Glacier National Park, northwestern Montana. (omitted from the online edition) 2. Reconnaissance geologic map of the Flathead region, northwestern Montana. (omitted from the online edition) 3. Map of part of northwestern Montana, showing principal topographic features and outlines of quadrangles topographically surveyed in and near Glacier National Park and the Flathead region. (omitted from the online edition) 4. Hypothetical block diagrams illustrating steps in the development of the Lewis overthrust. (omitted from the online edition) FIGURE 1. View northwest from Bennie Hill Lookout in the Heart Butte quadrangle, Flathead region 2. Altyn limestone in the lower slopes of Appekunny Mountain, northeast of Many Glacier Hotel, Glacier National Park 3. Air view northeast from above Gunsight Pass toward the valley of St. Mary River, with Lake Ellen Wilson in the foreground 4. Grinnell argillite on Broken Leg Mountain, Nyack quadrangle, Flathead region 5. Grinnell argillite on Broken Leg Mountain, Nyack quadrangle, Flathead region 6. Photomicrographs of rocks of the Belt series 7. Molar-tooth structure in Siyeh limestone in roadcut along Going-to-the-Sun Highway, Glacier National Park 8. Irregular banding in Siyeh limestone in roadcut along Going-to-the-Sun Highway, Glacier National Park 9. Photomicrographs of rocks of the Belt series and associated igneous rocks 10. Conophyton in roadcut in Siyeh limestone above the big switchback on Going-to-the-Sun Highway, Glacier National Park 11. Stromatolite on Tongue Mountain, Nyack quadrangle, Flathead region 12. Argillite of the Missoula group with sand-filled mud cracks, Upper Twin Creek, Marias Pass quadrangle, Flathead region 13. Cusped ripple marks in argillite of the Missoula group, head of Grouse Creek, Marias Pass quadrangle, Flathead region 14. Clay spalls in argillite of the Missoula group below Mount Bradley, Marias Pass quadrangle, Flathead region http://www.nps.gov/history/history/online_books/geology/publications/pp/296/contents.htm[3/13/2014 5:25:23 PM] USGS: Geological Survey Professional Paper 296 (Contents) 15. Laminated argillite of the Missoula group with a small stromatolite, in railroad cut nearly opposite the mouth of Coal Creek Nyack quadrangle, Flathead region 16. View north from the head of Avalanche Basin, Glacier National Park 17. Closeup of Hannan limestone with chert layers, gorge of Gateway Creek, Heart Butte quadrangle, Flathead region 18. Contorted shale and limestone of the Ellis group on Badger Creek near the mouth of Red Poacher Creek, Marias Pass quadrangle, Flathead region 19. North side of the Middle Fork of the Flathead River showing exposure of beds of early Tertiary age 20. Sketch contours on the major surface of the Lewis overthrust near the eastern border of Glacier National Park 21. The trace of the Lewis overthrust as seen from Marias Pass looking north 22. View south from below Bennie Hill Lookout, Heart Butte quadrangle, Flathead region 23. Crooked Mountain, Heart Butte quadrangle, Flathead region 24. Irregular folds in limestone of Cambrian age south of Swift Reservoir, Heart Butte quadrangle, Flathead region 25. Contorted Grinnell argillite on the north wall of the cirque on the south slope of Mount Thompson, Glacier National Park 26. View northwest from Sperry Glacier showing part of the intensely folded rocks west of the major syncline 27. View southeast from near Fifty Mountain Camp, Glacier National Park showing the syncline that dominates the structure in the central part of the park 28. Overturned Grinnell argillite on McPartland Mountain, Glacier National Park, viewed from the northwest 29. Railroad cut along the Middle Fork of the Flathead River below the mouth of Coal Creek showing exposures of minor fractures in argillite of the Missoula group 30. View showing topography after the Blackfoot surface had formed in the area of Glacier National Park 31. View showing topography in the area of Glacier National Park at about the middle of Pleistocene time 32. View showing topography in Glacier National Park at the present time 33. Diagrammatic contour map of the Blackfoot surface in the region now occupied by Glacier National Park, with sections diagonally across the park A report on fieldwork and available data on the geology, structural, and geomorphic studies of the rocks, ranging from Precambrian to Recent in age, in two adjacent mountainous regions of Montana. http://www.nps.gov/history/history/online_books/geology/publications/pp/296/contents.htm[3/13/2014 5:25:23 PM] USGS: Geological Survey Professional Paper 296 (Contents) UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U. S. Geological Survey Library has cataloged this publication as follows: Ross, Clyde Polhemus, 1891— Geology of Glacier National Park and the Flathead region, northwestern Montana. Washington, U. S. Govt. Print. Off., 1959. iv, 125 p. illus., maps (part col.) diagrs., tables, 30 cm. (U. S. Geological Survey. Professional paper 296) Three colored maps and colored diagr. in pocket. Bibliography: p. 118-121. 1. Glacier National Park. 2. Geology—Montana—Flathead region. (Series) GE75.P9 no. 296 557.868 G S 58-174 ___ _______ Copy 2. QE133.R57 <<< Previous <<< Contents >>> Next >>> pp/296/contents.htm Last Updated: 08-Jul-2008 http://www.nps.gov/history/history/online_books/geology/publications/pp/296/contents.htm[3/13/2014 5:25:23 PM] USGS: Geological Survey Professional Paper 296 (Abstract) Geological Survey Professional Paper 296 Geology of Glacier National Park And the Flathead Region, Northwestern Montana ABSTRACT GEOLOGY OF GLACIER NATIONAL PARK AND THE FLATHEAD REGION NORTHWESTERN MONTANA By CLYDE P. ROSS This report summarizes available data on two adjacent and partly overlapping regions in northwestern Montana. The first of these is Glacier National Park plus small areas east and west of the park. The second is here called, for convenience, the Flathead region; it embraces the mountains from the southern tip of Glacier Park to latitude 48° north and between the Great Plains on the east and Flathead Valley on the west. The fieldwork under the direction of the writer was done in 1948, 1949, 1950, and 1951, with some work in 1952 and 1953. The two regions together include parts of the Swan, Flathead,
Recommended publications
  • Montana Official 2018-2019 Visitor Guide
    KALISPELL MONTANA OFFICIAL 2018-2019 VISITOR GUIDE #DISCOVERKALISPELL 888-888-2308 DISCOVERKALISPELL.COM DISCOVER KALISPELL TABLE OF CONTENTS 4 DISCOVER KALISPELL 6 GETTING HERE 7 GLACIER NATIONAL PARK 10 DAY HIKES 11 SCENIC DRIVES 12 WILD & SCENIC 14 QUICK PICKS 23 FAMILY TIME 24 FLATHEAD LAKE 25 EVENTS 26 LODGING 28 EAT & DRINK 32 LOCAL FLAVOR 35 CULTURE 37 SHOPPING 39 PLAN A MEETING 41 COMMUNITY 44 RESOURCES CONNECTING WITH KALISPELL To help with your trip planning or to answer questions during your visit: Kalispell Visitor Information Center Photo: Tom Robertson, Foys To Blacktail Trails Robertson, Foys To Photo: Tom 15 Depot Park, Kalispell, MT 59901 406-758-2811or 888-888-2308 DiscoverKalispellMontana @visit_Kalispell DiscoverKalispellMontana Discover Kalispell View mobile friendly guide or request a mailed copy at: WWW.DISCOVERKALISPELL.COM Cover Photo: Tyrel Johnson, Glacier Park Boat Company’s Morning Eagle on Lake Josephine www.discoverkalispell.com | 888-888-2308 3 DISCOVER KALISPELL WELCOME TO KALISPELL Photos: Tom Robertson, Kalispell Chamber, Mike Chilcoat Robertson, Kalispell Chamber, Photos: Tom here the spirit of Northwest Montana lives. Where the mighty mountains of the Crown of the Continent soar. Where the cold, clear Flathead River snakes from wild lands in Glacier National Park and the Bob WMarshall Wilderness to the largest freshwater lake in the west. Where you can plan ahead for a trip of wonder—or let each new moment lead your adventures. Follow the open road to see what’s at the very end. Lay out the map and chart a course to its furthest corner. Or explore the galleries, museums, and shops in historic downtown Kalispell—and maybe let the bakery tempt you into an unexpected sweet treat.
    [Show full text]
  • 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.
    [Show full text]
  • Coram Experimental Forest
    United States Department of Agriculture Coram Experimental Forest Service Forest: 50 Years of Rocky Mountain Research Station General Technical Research in a Western Report RMRS-GTR-37 September 1999 Larch Forest Raymond C. Shearer Madelyn M. Kempf Abstract Shearer, Raymond C.; Kempf, Madelyn M. 1999. Coram Experimental Forest: 50 years of research in a western larch forest. Gen. Tech. Rep. RMRS-GTR-37. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 66 p. This publication will enrich public understanding about the important contributions to science made at this and other outdoor laboratories. Coram, and other long-range research sites, provide scientific knowledge to assist resource professionals with the development of sound land management principles. This knowledge ensures healthy, sustainable, and productive ecosystems while meeting social and economic needs. Major research at Coram includes the regeneration of young forests and the interaction of flora, fauna, and water to a wide range of forest treatments. Ongoing studies include: • cone and seed development and dispersal • natural and artificial regeneration after harvest cuttings • effects of stand culture treatment on forest development • insect and disease interactions • effects of the amount of wood harvest on site productivity • influence of silvicultural practices on watershed, esthetics, and wildlife values The Coram Experimental Forest is used cooperatively by Federal, university, and private scientists. About 340 ha of the forest are designated as the Coram Research Natural Area where virgin conditions are permanently maintained for research and monitoring. Coram, designated a Biosphere Reserve in 1976, is part of an international network that is devoted to the conservation of nature and scientific research in the service of humans.
    [Show full text]
  • Going-To-The-Sun Road Historic District, Glacier National Park
    National Park Service Cultural Landscapes Inventory 2002 Going-to-the-Sun Road Historic District Glacier National Park Table of Contents Inventory Unit Summary & Site Plan Concurrence Status Geographic Information and Location Map Management Information National Register Information Chronology & Physical History Analysis & Evaluation of Integrity Condition Treatment Bibliography & Supplemental Information Going-to-the-Sun Road Historic District Glacier National Park Inventory Unit Summary & Site Plan Inventory Summary The Cultural Landscapes Inventory Overview: CLI General Information: Purpose and Goals of the CLI The Cultural Landscapes Inventory (CLI), a comprehensive inventory of all cultural landscapes in the national park system, is one of the most ambitious initiatives of the National Park Service (NPS) Park Cultural Landscapes Program. The CLI is an evaluated inventory of all landscapes having historical significance that are listed on or eligible for listing on the National Register of Historic Places, or are otherwise managed as cultural resources through a public planning process and in which the NPS has or plans to acquire any legal interest. The CLI identifies and documents each landscape’s location, size, physical development, condition, landscape characteristics, character-defining features, as well as other valuable information useful to park management. Cultural landscapes become approved CLIs when concurrence with the findings is obtained from the park superintendent and all required data fields are entered into a national
    [Show full text]
  • National Register of Historic Places Registration Form
    NPS Form 10-900 OMB No. 1024-0018 (Rev. Oct. 1990) United States Department of the Interior National Park Service NATIONAL REGISTER OF HISTORIC PLACES REGISTRATION FORM 1. Name of Property historic name: Dearborn River High Bridge other name/site number: 24LC130 2. Location street & number: Fifteen Miles Southwest of Augusta on Bean Lake Road not for publication: n/a vicinity: X city/town: Augusta state: Montana code: MT county: Lewis & Clark code: 049 zip code: 59410 3. State/Federal Agency Certification As the designated authority under the National Historic Preservation Act of 1986, as amended, I hereby certify that this _X_ nomination _ request for detenj ination of eligibility meets the documentation standards for registering properties in the National Register of Historic Places and meets the proc urf I and professional requirements set forth in 36 CFR Part 60. In my opinion, the property X_ meets _ does not meet the National Register Criterfi commend thatthis oroperty be considered significant _ nationally X statewide X locafly. Signa jre of oertifying officialn itle Date Montana State Historic Preservation Office State or Federal agency or bureau (_ See continuation sheet for additional comments. In my opinion, the property _ meets _ does not meet the National Register criteria. Signature of commenting or other official Date State or Federal agency and bureau 4. National Park Service Certification , he/eby certify that this property is: 'entered in the National Register _ see continuation sheet _ determined eligible for the National Register _ see continuation sheet _ determined not eligible for the National Register_ _ see continuation sheet _ removed from the National Register _see continuation sheet _ other (explain): _________________ Dearborn River High Bridge Lewis & Clark County.
    [Show full text]
  • Montana Oil and Mining Journal (Great Falls, Mont.), 1937-06-26, [P
    B V; W-* PP|jl ■ - , W- Wfæ ’ : ■' ■ ml ■BHBR8BR SATURDAY, J UN* 26. 1637. PAGE FOU» MONTANA OIL AND MININO JOURNAL member that King Solomon used to "Use Just been bit by a dog and ‘T «ent my husband to the hos­ P take his pick and go to bed.” I’se worried. I hear whenever a pital because cd bis knee.” L dog bits yon, whatever the dog has, “Did he hare -water on H?” • • • • • . “No; his private secretary.” For Sale—Pure Bred Milking you got.” /-Aonla 'Journal shorthorn ball. Ready for service. "Boy, then you have a right to • • • • • —Owendboro (Ky.) paper. worry.” "Last night my boyfriend gave me Sap He’s got something Giere. "Why?” a quarter for every kiss I gave him.” «ESTABLISHED 1921 PUBLISHED WEEKLY • • • • "That dog Just bad eleven pups!” "Why are yon telling us?” s I Bat» all kind Nature doth bestow, • • • • • “I thlought maybe you could tell Owned and published by the Montana Oil Journal, a Montana corporation. me where I can buy a yacht.” it will amalgamate below. "What dreadful language your Address all communications to 618 First National Bank Building, K the mind says so, it shall be so parrot uses.” • •••••• I But If you once begin to doubt Great Falls. Montana. O. I. DeSCHON. publisher "Yes. My husband bought the Son: Daddy, what Is the différ­ The gastric Juice will find it out. ence between seduction and nape? • • • • • bird in town and drove It home In SUBSCRIPTION RATES: bis car. He had three blowouts, Daddy: It’s salesmanship, son.
    [Show full text]
  • 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 ....................................
    [Show full text]
  • Status of Mineral Resource Information for the Blackfeet Indian Reservation, Montana
    STATUS OF MINERAL RESOURCE INFORMATION FOR THE BLACKFEET INDIAN RESERVATION, MONTANA By C. A. Balster Michael Sokaski Billings, Montana George McIntyre R. B. Berg U.S. Bureau of Mines H. G. McClernan Miller Hansen Montana Bureau of Mines and Geology Administrative Report BIA-24 1976 CONTENTS SUMMARY AND CONCLUSIONS ................................................. 1 INTRODUCTION ................................................................ 1 General ................................................................... 1 Geography ................................................................ 1 Physiography .............................................................. 2 GEOLOGY ..................................................................... 3 Stratigraphy ............................................................... 3 Structure.................................................................. 5 MINERAL RESOURCES .......................................................... 6 Energy Resources........................................................... 6 Petroleum and Natural Gas ............................................. 6 General ....................................................... 6 Production and Reserves ......................................... 7 Cut Bank Oil and Gas Field ................................. 7 Reagan Oil and Gas Field .................................. 9 Blackfoot Oil Field ...................................... 10 Red Creek Oil Field ...................................... 12 Graben Coulee Oil Field .................................
    [Show full text]
  • Comparison of Geodetic and Glaciological Mass Budgets for White Glacier, Axel Heiberg Island, Canada
    Journal of Glaciology (2016), Page 1 of 12 doi: 10.1017/jog.2016.112 © The Author(s) 2016. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. Comparison of geodetic and glaciological mass budgets for White Glacier, Axel Heiberg Island, Canada LAURA I. THOMSON,1 MICHAEL ZEMP,2 LUKE COPLAND,1 J. GRAHAM COGLEY,3 MILES A. ECCLESTONE3 1Department of Geography, Environment and Geomatics, University of Ottawa, Ottawa, Ontario K1N 6N5, Canada 2Department of Geography, University of Zurich, Winterthurerstrasse 190, 8057 Zurich, CH, Switzerland 3Department of Geography, Trent University, Peterborough, Ontario, K9J 7B8, Canada Correspondence: Laura I. Thomson <[email protected]> ABSTRACT. This study presents the first reanalysis of a long-term glacier mass-balance record in the Canadian Arctic. The reanalysis is accomplished through comparison of the 1960–2014 glaciological mass-balance record of White Glacier, Axel Heiberg Island, Nunavut, with a geodetically derived mass change over the same period. The corrections applied to homogenize the two datasets, including adjusting for changes in hypsometry over the period of record and the generic differences between methods, are discussed along with the associated systematic and random errors of the two forms of mass-balance measurement. Statistical comparison of the two datasets reveals that within the error margin there is no significant difference between the average annual glaciological balance (–213 ± 28 − − mm w.e. a 1) and geodetic balance (–178 ± 16 mm w.e.
    [Show full text]
  • ENVIRONMENTAL ASSESSMENT for SAINT MARY SCENIC OVERLOOK and BLACKFEET INTERPRETIVE LOOP
    ENVIRONMENTAL ASSESSMENT for SAINT MARY SCENIC OVERLOOK and BLACKFEET INTERPRETIVE LOOP BLACKFEET TRANSPORTATION PLANNING DEPARTMENT BLACKFEET INDIAN RESERVATION GLACIER COUNTY, MONTANA Prepared for: U.S. Department of the Interior Bureau of Indian Affairs Blackfeet Agency Browning, Montana Prepared by: Blackfeet Environmental Office and Rocky Mountain Botany Consulting and Donna Jo Pridmore, Hydrogeologist February 2014 TABLE OF CONTENTS ADMINISTRATIVE SUMMARY ................................................................................................. 1 I. PURPOSE AND NEED FOR ACTION ........................................................ 2 II. ALTERNATIVES .......................................................................................... 4 A. Alternative A: Proposed action. ..................................................................................................... 4 B. Alternative B: No action. ................................................................................................................ 4 III. DESCRIPTION OF THE AFFECTED ENVIRONMENT ..................... 4 A. LAND RESOURCES ..................................................................................................................... 5 1. Topography ................................................................................................................................ 5 2. Soils ............................................................................................................................................. 7 3. Geologic
    [Show full text]
  • Hydrogeologic Framework of the Upper Clark Fork River Area: Deer Lodge, Granite, Powell, and Silver Bow Counties R15W R14W R13W R12W By
    Montana Bureau of Mines and Geology Montana Groundwater Assessment Atlas No. 5, Part B, Map 2 A Department of Montana Tech of The University of Montana July 2009 Open-File Version Hydrogeologic Framework of the Upper Clark Fork River Area: Deer Lodge, Granite, Powell, and Silver Bow Counties R15W R14W R13W R12W by S Qsf w Qsf Yb Larry N. Smith a n T21N Qsf Yb T21N R Authors Note: This map is part of the Montana Bureau of Mines and Geology (MBMG) a n Pz Pz Groundwater Assessment Atlas for the Upper Clark Fork River Area groundwater Philipsburg ValleyUpper Flint Creek g e Pz Qsf characterization. It is intended to stand alone and describe a single hydrogeologic aspect of the study area, although many of the areas hydrogeologic features are The town of Philipsburg is the largest population center in the valley between the Qsc interrelated. For an integrated view of the hydrogeology of the Upper Clark Fork Area Flint Creek Range and the John Long Mountains. The Philipsburg Valley contains 47o30 the reader is referred to Part A (descriptive overview) and Part B (maps) of the Montana 040 ft of Quaternary alluvial sediment deposited along streams cut into Tertiary 47o30 Groundwater Assessment Atlas 5. sedimentary rocks of unknown thickness. The east-side valley margin was glaciated . T20N Yb t R during the last glaciation, producing ice-sculpted topography and rolling hills in side oo B kf l Ovando c INTRODUCTION drainages on the west slopes of the Flint Creek Range. Prominent benches between ac la kf k B Blac oo N F T20N tributaries to Flint Creek are mostly underlain by Tertiary sedimentary rocks.
    [Show full text]
  • Summits on the Air – ARM for the USA (W7A
    Summits on the Air – ARM for the U.S.A (W7A - Arizona) Summits on the Air U.S.A. (W7A - Arizona) Association Reference Manual Document Reference S53.1 Issue number 5.0 Date of issue 31-October 2020 Participation start date 01-Aug 2010 Authorized Date: 31-October 2020 Association Manager Pete Scola, WA7JTM Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Document S53.1 Page 1 of 15 Summits on the Air – ARM for the U.S.A (W7A - Arizona) TABLE OF CONTENTS CHANGE CONTROL....................................................................................................................................... 3 DISCLAIMER................................................................................................................................................. 4 1 ASSOCIATION REFERENCE DATA ........................................................................................................... 5 1.1 Program Derivation ...................................................................................................................................................................................... 6 1.2 General Information ..................................................................................................................................................................................... 6 1.3 Final Ascent
    [Show full text]