Soil Survey of Powell County Area, Montana

Total Page:16

File Type:pdf, Size:1020Kb

Soil Survey of Powell County Area, Montana How to Use This Soil Survey Detailed Soil Maps The detailed soil maps can be useful in planning the use and management of small areas. To find information about your area of interest, you can locate the Section, Township, and Range by zooming in on the Index to Map Sheets, or you can go to the Web Soil Survey at (http://websoilsurvey.nrcs.usda.gov/app/). Note the map unit symbols that are in that area. The Contents lists the map units by symbol and name and shows the page where each map unit is described. See the Contents for sections of this publication that may address your specific needs. ii This soil survey is a publication of the National Cooperative Soil Survey, a joint effort of the United States Department of Agriculture and other Federal agencies, State agencies including the Agricultural Experiment Stations, and local agencies. The Natural Resources Conservation Service (formerly the Soil Conservation Service) has leadership for the Federal part of the National Cooperative Soil Survey. Major fieldwork for this soil survey was completed in 1989. Soil names and descriptions were approved in 1991. Unless otherwise indicated, statements in this publication refer to conditions in the survey area in 1991. This survey was made cooperatively by the Natural Resources Conservation Service and the Montana Agricultural Experiment Station. It is part of the technical assistance furnished to the Deer Lodge Valley and North Powell Conservation Districts. Financial assistance was provided by the Old West Regional Commission in cooperation with the Montana Department of State Lands and the Montana Association of Conservation Districts, the Board of County Commissioners, and Powell County. The most current official data are available through the NRCS Soil Data Mart website at http://soildatamart.nrcs.usda.gov. Soil maps in this survey may be copied without permission. Enlargement of these maps, however, could cause misunderstanding of the detail of mapping. If enlarged, maps do not show the small areas of contrasting soils that could have been shown at a larger scale. The United States Department of Agriculture (USDA) prohibits discrimination in all of its programs on the basis of race, color, national origin, gender, religion, age, disability, political beliefs, sexual orientation, and marital or family status. (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 the USDA’s TARGET Center at 202-720-2600 (voice or TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326W, Whitten Building, 14th and Independence Avenue SW, Washington, DC 20250-9410, or call 202-720-5964 (voice or TDD). USDA is an equal opportunity provider and employer. Cover: Deer Lodge Mountain and Mount Powell in southern Powell County Area. The lower elevation forested soils are mainly Worock gravelly loam, and the rangeland soils are mainly Roy- Shawmut-Danvers complex. Additional information about the Nation’s natural resources is available online from the Natural Resources Conservation Service at http://www.nrcs.usda.gov. iii Contents Part I 379E—Ambrant-Rochester-Rock outcrop complex, 15 to 35 percent slopes................ 30 How To Use This Soil Survey .................................. i 379F—Ambrant-Rochester-Rock outcrop Index to Taxonomic Units ................................... xiv complex, 35 to 60 percent slopes................ 31 Index to Map Units ............................................... xv Anaconda Series ............................................... 32 Summary of Tables .............................................xxiv 35B—Anaconda loam, 0 to 4 percent slopes .... 33 Foreword ............................................................ xxvii Aquents.............................................................. 33 Introduction ............................................................ 1 4—Aquents-Slickens complex, 0 to 2 percent General Nature of the Survey Area ..................... 1 slopes, occasionally flooded ....................... 33 History.................................................................. 1 Baggs Series ..................................................... 34 Industry, Transportation, and Recreation ............. 2 135B—Baggs sandy loam, 0 to 4 percent Physiography and Drainage................................. 2 slopes .......................................................... 35 Geologic History and Regional Geology ............. 3 135C—Baggs sandy loam, 4 to 8 percent Geologic Units ..................................................... 4 slopes .......................................................... 35 Mineral Resources ............................................... 5 135D—Baggs sandy loam, 8 to 15 percent Ground-Water Resources .................................... 6 slopes .......................................................... 35 Seismic Activity .................................................... 6 479B—Baggs sandy loam, cool, 0 to 4 Climate................................................................. 6 percent slopes ............................................. 36 How This Survey Was Made .................................... 7 Beaverell Series ................................................. 36 Formation and Classification of the Soils .......... 13 132B—Beaverell cobbly loam, 0 to 4 percent Formation of the Soils ........................................ 13 slopes .......................................................... 37 Classification of the Soils ................................... 14 132C—Beaverell cobbly loam, 4 to 8 percent Soil Series and Detailed Soil Map Units ............. 25 slopes .......................................................... 38 Ambrant Series .................................................. 26 332B—Beaverell loam, 0 to 4 percent slopes.... 38 79D—Ambrant-Rochester complex, cool, Bignell Series ..................................................... 38 4 to 15 percent slopes ................................. 27 99D—Bignell gravelly clay loam, 8 to 15 79E—Ambrant-Rochester complex, cool, percent slopes ............................................. 39 15 to 35 percent slopes ............................... 27 99E—Bignell gravelly clay loam, 15 to 35 79F—Ambrant-Rochester complex, cool, percent slopes ............................................. 40 35 to 60 percent slopes ............................... 28 99F—Bignell gravelly clay loam, 35 to 60 179E—Ambrant-Rochester complex, 15 to 35 percent slopes ............................................. 40 percent slopes ............................................. 28 199E—Bignell gravelly clay loam, cool, 179F—Ambrant-Rochester complex, 35 to 60 15 to 35 percent slopes ............................... 40 percent slopes ............................................. 29 199F—Bignell gravelly clay loam, cool, 279E—Ambrant, cool-Rochester, cool-Rock 35 to 60 percent slopes ............................... 41 outcrop complex, 15 to 35 percent 299E—Bignell-Yreka complex, 15 to 35 slopes .......................................................... 29 percent slopes ............................................. 41 279F—Ambrant, cool-Rochester, cool-Rock 299F—Bignell-Yreka complex, 35 to 60 outcrop complex, 35 to 60 percent slopes... 30 percent slopes ............................................. 41 iv 399E—Bignell-Yreka complex, cool, 15 to 35 242C—Braziel-Perma gravelly loams, 4 to 8 percent slopes ............................................. 42 percent slopes ............................................. 56 399F—Bignell-Yreka complex, cool, 35 to 60 242D—Braziel gravelly loam, 8 to 15 percent percent slopes ............................................. 42 slopes .......................................................... 56 499D—Bignell, cool-Yreka complex, 8 to 15 242E—Braziel gravelly loam, 15 to 35 percent percent slopes ............................................. 43 slopes .......................................................... 56 499E—Bignell, cool-Yreka complex, 15 to 35 342D—Braziel stony loam, 8 to 15 percent percent slopes ............................................. 43 slopes .......................................................... 57 499F—Bignell, cool-Yreka complex, 35 to 60 342E—Braziel stony loam, 15 to 35 percent percent slopes ............................................. 44 slopes .......................................................... 57 699D—Bignell gravelly loam, 8 to 15 percent 342F—Braziel stony loam, 35 to 60 percent slopes .......................................................... 44 slopes .......................................................... 58 699E—Bignell gravelly loam, 15 to 35 percent 442D—Braziel-Tolbert complex, 8 to 15 slopes .......................................................... 45 percent slopes ............................................. 58 699F—Bignell gravelly loam, 35 to 60 percent 442E—Braziel-Tolbert complex, 15 to 35 slopes .......................................................... 45 percent slopes ............................................. 58 799D—Bignell-Yreka-Crow complex, 8 to 15 442F—Braziel-Tolbert complex, 35 to 60 percent slopes ............................................. 46 percent slopes ............................................. 59 799E—Bignell-Yreka-Crow complex, 15 to 35 742E—Braziel-Perma-Water complex, 8 to 25 percent slopes ............................................
Recommended publications
  • Porphyry and Other Molybdenum Deposits of Idaho and Montana
    Porphyry and Other Molybdenum Deposits of Idaho and Montana Joseph E. Worthington Idaho Geological Survey University of Idaho Technical Report 07-3 Moscow, Idaho ISBN 1-55765-515-4 CONTENTS Introduction ................................................................................................ 1 Molybdenum Vein Deposits ...................................................................... 2 Tertiary Molybdenum Deposits ................................................................. 2 Little Falls—1 ............................................................................. 3 CUMO—2 .................................................................................. 3 Red Mountain Prospect—45 ...................................................... 3 Rocky Bar District—43 .............................................................. 3 West Eight Mile—37 .................................................................. 3 Devil’s Creek Prospect—46 ....................................................... 3 Walton—8 .................................................................................. 4 Ima—3 ........................................................................................ 4 Liver Peak (a.k.a. Goat Creek)—4 ............................................. 4 Bald Butte—5 ............................................................................. 5 Big Ben—6 ................................................................................. 6 Emigrant Gulch—7 ...................................................................
    [Show full text]
  • Thomas Stuart Homestead Site: Historic Context Report
    Thomas Stuart Homestead Historic Context Report Grant-Kohrs Ranch National Historic Site Avana Andrade Public Lands History Center at Colorado State University 2/1/2012 1 Thomas Stuart Homestead Site: Historic Context Report Grant-Kohrs Ranch National Historic Site in Deer Lodge Montana is currently developing plans for a new contact station. One potential location will affect the site of a late-nineteenth-century historic homestead. Accordingly, the National Park Service and the Montana State Historic Preservation Office need more information about the historic importance of the Thomas Stuart homestead site to determine future decisions concerning the contact station. The following report provides the historic contexts within which to assess the resource’s historic significance according to National Register of Historic Places guidelines. The report examines the site’s association with Thomas Stuart, a Deer Lodge pioneer, and the Menards, a French- Canadian family, and presents the wider historical context of the fur trade, Deer Lodge’s mixed cultural milieu, and the community’s transformation into a settled, agrarian town. Though only indications of foundations and other site features remain at the homestead, the report seeks to give the most complete picture of the site’s history. Site Significance and Integrity The Thomas Stuart homestead site is evaluated according to the National Register of Historic Places, a program designed in the 1960s to provide a comprehensive listing of the United States’ significant historic properties. Listing on the National Register officially verifies a site’s importance and requires park administrators or land managers to consider the significance of the property when planning federally funded projects.
    [Show full text]
  • Lord Ranch on Trout Creek Philipsburg, Montana
    Lord PHILIRanchPSBURG, on MONTANATrout Creek Lord Ranch on Trout Creek PHILIPSBURG, MONTANA Introduction: The Lord Ranch on Trout Creek enjoys exceptional trout fishing and elk, deer and bird hunting with access to national forest and close proximity to recreation. These 2,691.7 acres are an idyllic mix of pivot- NTRODUCTION I irrigated hay fields, brush-lined creek, riparian zone, rolling grass and timbered mountainside. Ranch improvements include five modern center pivot irrigation systems, two basic homes and assorted barns, RINGS RANCH sheds and outbuildings. Nearby recreational opportunities abound P with winter actives at Discovery Ski Area and summer pursuits at Georgetown Lake. ROCKING CHAIR S Craig Janssen, Montana Managing Broker Jack McInerney, Sales Associate Toll Free 866.734.6100 www.LiveWaterProperties.com Lord Ranch on Trout Creek- Excellent Fishing & Hunting Ranch Location: Located on the scenic byway, Skalkaho Highway, 10 minutes south of the charming mountain town of Philipsburg is the Lord Ranch on Trout Creek. The ranch borders the Deerlodge National Forest and is in the foothills of the Anaconda Mountain Range. Georgetown Lake lies less than a mile east. Philipsburg is the county seat of Granite County and is named for mining engineer Philip Deidesheimer, who platted the town site near gold and silver mines in 1867. Dining, shopping and everyday amenities are available in Phillipsburg. Riddick Field, a public airport with a paved 3,600 foot runway, is nearby for convenience. The cultural center of Missoula, home to the University of Montana, is an hour northwest. Butte, Montana, lies approximately 40 minutes to the east. Both of these communities have a rich history and offer shopping, fine dining and commercial air service.
    [Show full text]
  • The Structural Geology and Tectonic History of the Northern Flint Creek
    The structural geology and tectonic history of the northern Flint Creek Range, western Montana by Jeffrey Frank Baken A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Science Montana State University © Copyright by Jeffrey Frank Baken (1984) Abstract: The Flint Creek Range of west-central Montana represents an important and rather atypical segment of the Cordilleran fold and thrust belt. The formation of opposing structural asymmetry in the range has not been satisfactorily explained. Field mapping and structural lab work have been incorporated with modern concepts of fold-and-thrust belt geometry to resolve this question. The range has been subdivided into three structural provinces based upon distinct structural geometries. The western province, which represents the eastern edge of the Sapphire allochthon, is characterized by "typical" eastward assymmetry; however, the eastern province displays "atypical" westward asymmetry. The northern province is represented by a change in structural trend (convex to the northeast) and opposing fold-plunges where the Flint Creek and Garnet Ranges meet across the Montana lineament. The kinematic sequence of deformation in the Flint Creek Range incorporates regional tectonic events and features. The Deer Lodge block, which occupies the Belt embayment, moved eastward along a major decollament as the result of combined east-west compression and intrusive wedging by the Idaho batholith (100 m.y. ago). Following development of this allochthon, the Boulder batholith initiated emplacement along the decollement with the Racetrack Creek pluton and the Elkhorn Mountains Volcanics (78-72 m.y. ago) as satellite effects. The "atypical" geometry of the eastern province was produced by the formation of a ramp interface beneath the Flint Creek Range.
    [Show full text]
  • Structural Geology Along Part of the Blackfoot Fault System Near Potomac Missoula County Montana
    University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1987 Structural geology along part of the Blackfoot fault system near Potomac Missoula County Montana Michael B. Thomas The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Thomas, Michael B., "Structural geology along part of the Blackfoot fault system near Potomac Missoula County Montana" (1987). Graduate Student Theses, Dissertations, & Professional Papers. 7524. https://scholarworks.umt.edu/etd/7524 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. COPYRIGHT ACT OF 1975 Th is is an unpublished manuscript in which copyright sub ­ s is t s . Any further r e p r in t in g of its contents must be approved BY THE AUTHOR. Mansfield Library U niversity of Montana D ate ; ____1 _______ Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. STRUCTURAL GEOLOGY ALONG PART OF THE BLACKFOOT FAULT SYSTEM NEAR POTOMAC, MISSOULA COUNTY. MONTANA By Michael B. Thomas 8. S., Central Washington University, 1982 Presented in partial fulfillment of the requirements for the degree of Master of Science University of Montana 1987 Approved by Chairman, Board of Examiners DeSrT, Graduate SchoÏÏ Date Reproduced with permission of the copyright owner.
    [Show full text]
  • Extension of the Anaconda Metamorphic Core Complex: 40Ar
    Extension of the Anaconda metamorphic core complex: 40Ar/39Ar thermochronology and implications for Eocene tectonics of the northern Rocky Mountains and the Boulder batholith David A. Foster1, Warren C. Grice Jr.1,*, and Thomas J. Kalakay2 1DEPARTMENT OF GEOLOGICAL SCIENCES, P.O. BOX 112120, UNIVERSITY OF FLORIDA, GAINESVILLE, FLORIDA 32611, USA 2DEPARTMENT OF GEOLOGY, ROCKY MOUNTAIN COLLEGE, 1511 POLY DRIVE, BILLINGS, MONTANA 59102, USA ABSTRACT Thermochronologic data defi ne the extension and exhumation history of the Anaconda metamorphic core complex and have implications for the Eocene tectonic setting of the northern Rocky Mountains. The 40Ar/ 39Ar data indicate that relatively rapid extension on the Anaconda detachment started at ca. 53 Ma and continued through ca. 39 Ma. Apatite fi ssion-track data reveal that faulting and exhumation of the foot- wall continued until ca. 27 Ma. The average displacement rate on the Anaconda detachment was on the order of 1 mm/yr between ca. 50 and 39 Ma based on the lateral gradient in mica 40Ar/39Ar ages in the direction of fault slip. The total displacement along the Anaconda detachment in Eocene and Oligocene times is estimated to be ≥25–28 km based on reconstruction of the Cretaceous Storm Lake Stock with its detached roof, which is now exposed in the Deer Lodge Valley. Extension exhumed crust from ~12 km depth and exposed middle-greenschist-facies mylonites in the easternmost part of the Anaconda complex footwall. On a regional scale, the Anaconda detachment dips east beneath the Cretaceous Boulder batholith, indicating that the batholith and the Butte mineralization were transported east in the hanging wall.
    [Show full text]
  • Geology of the Elliston Region, Powell and Lewis and Clark Counties, Montana
    Geology of the Elliston Region, Powell and Lewis and Clark Counties, Montana U.S. GEOLOGICAL SURVEY BULLETIN 2045 / Geology of the Elliston Region, Powell and Lewis and Clark Counties, Montana By R. G. SCHMIDT, J. S. LOEN, C. A. WALLACE, and H. H. MEHNERT U.S .. GEOLOGICAL SURVEY BULLETIN 2045 A description of rocks and structures in the region of the imbricate front of the Sapphire thrust plate, from a reconnaissance study UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director For sale by USGS Map Distribution Box 25286, Building 810 Denver Federal Center Denver, CO 80225 Any use of trade, product, or finn names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Library or Congress Cataloging-In-Publication Data Geology of the Elliston region, Powell and Lewis and Clark Counties, Montana : a de­ scription of rocks and structures in the region of the imbricate front of the Sapphire thrust plate, from a reconnaissance study I by R.G. Schmidt ... [et al.]. p. em. - (U.S. Geological Survey Bulletin; 2045) Includes bibliographical references. Supt. of Docs. no.: I 19.3:2045 1. Geology-Montana-Elliston Region. I. Schmidt, R.G., d. 1983. II. Series. QE75.B9 no. 2045 [QE134.E45] 557.3 s-dc20 92-42415 [557.86'615] CIP CONTENTS Abstract ................................................................................................................................ 1 Introduction..........................................................................................................................
    [Show full text]
  • Montana Gray Wolf Conservation and Management 2010 Annual Report
    Montana Gray Wolf Conservation and Management 2010 Annual Report A cooperative effort by Montana Fish, Wildlife & Parks, USDA Wildlife Services, Glacier National Park, Yellowstone National Park, Blackfeet Nation, and The Confederated Salish and Kootenai Tribes MFWP by photo Liz Bradley This report presents information on the status, distribution, and management of wolves in the State of Montana, from January 1, 2010 to December 31, 2010. It is also available at: www.fwp.mt.gov/wildthings/wolf This report may be copied in its original form and distributed as needed. Suggested Citation: Sime, Carolyn A., V. Asher, L. Bradley, N. Lance, K. Laudon, M. Ross, A. Nelson, and J. Steuber. 2011. Montana gray wolf conservation and management 2010 annual report. Montana Fish, Wildlife & Parks. Helena, Montana. 168 pp TABLE OF CONTENTS MONTANA EXECUTIVE SUMMARY ......................................................................... 1 INTRODUCTION AND BACKGROUND ..................................................................... 3 Delisting Efforts and Ligation in 2007 - 2010 ...................................................... 4 STATEWIDE PROGRAM OVERVIEW......................................................................... 8 Overview of Wolf Ecology in Montana ................................................................ 9 Population Estimation and Monitoring Methods .................................................. 11 Border Packs ........................................................................................................
    [Show full text]
  • National Register of Historic Places Registration Form
    NPS Form 10-9003 OMB No. 1024-0018 (Rev. 10-90) United States Department of the Interior National Park Service NATIONAL REGISTER OF HISTORIC PLACES REGISTRATION FORM 1. Name of Property Historic name: Grant-Kohrs Ranch/Warren Ranch Other name/site number: Grant-Kohrs Ranch National Historic Site, Grant-Kohrs Ranch National Historic Landmark, Grant Trading Post, John Grant Ranch, Kohrs & Bielenberg Home Ranch, Conrad Kohrs Company Ranch, CK Ranch, Warren Hereford Ranch 2. Location Street & number: Cattle Drive (no number), Grant-Kohrs Ranch NHS not for publication: n/a City/town: Deer Lodge vicinity: n/a state: Montana code: MT county: Powell code: 077 zip code: 59722 3. State/Federal Agency Certification As the designated authority under the National Historic Preservation Act of 1986, as amended I hereby certify that this^ nomination _ request for determination of eligibility meets the documenJaJieH-staadards for registering properties in the National Register of Historic Places and meets the procedural and professional requiremgpts'setforth in 36 Ct"R Part 60. In my opinion, the property j; meets _ does not meet the National Register Criteria. I recommend that this ppfSerty be considered signifpant _ nationally X statewide __ local.y. ( _ See continuation sheet for additional comments.) Signature~oTcertif^fig official/Title Nationll Park Service State or Federal agency or bureau In my* piniin, the property >C does not meet the National Register criteria Signati re rff comme/ffing or other official *~» 7>t-"7"£_ /-f-rf, T^c'/a-fC State or Federal agency and bureau 4. National Park Service Certification I, hereby certify that this property is: Date of Action entered in the National Register see continuation sheet determined eligible for the National Register w< ____ see continuation sheet determined not eligible for the National Register ____ see continuation sheet removed from the National Register ____ see continuation sheet other (explain) Grant-Kohrs Ranch/Warren Ranch Powell County.
    [Show full text]
  • U.S. Department of the Interior U.S. Geological
    U.S. DEPARTMENT OF THE INTERIOR MINERAL INVESTIGATIONS U.S. GEOLOGICAL SURVEY RESOURCES MAP MR-96 PAMPHLET MAP SHOWING THE LOCATION OF PRODUCTIVE LODE AND PLACER GOLD MINES IN MONTANA By David Frishman, I.E. Elliott, E.E. Foord, R.C. Pearson, and W.H. Raymond INTRODUCTION mines that ceased production long ago, the list of commodities present is likely incomplete. For lode This pamphlet contains tabular information keyed mines having recorded production, not all the to the accompanying map. Table 1 lists site names commodities listed were necessarily recovered some numerically keyed to the map; sites are organized by may be minor elements that are listed because they county and numbered consecutively by mining district record the geochemical signature of the deposit. within each county. Site numbers were assigned Industrial commodities, however (like silicon or abrasive geographically by county with the intention of making it sand), are listed only when they were produced. Silver as easy as possible to find a particular number on the is listed as a commodity along with gold for aT placer map after the site name and number have been mines because we are confident that silver was produced identified in table 1. The site name listed is the one and, eventually, refined, even from those placer deposits that seemed to be most commonly used and is usually whose gold was of high fineness. the name of a mine (for lodes) or a creek or gulch (for Host rock type as given in table 1 is that from placers). In some cases, the name is that of a claim, a which the gold or gold-bearing minerals were ertracted group of claims, or, rarely, an exploration project.
    [Show full text]
  • Helena, Montana August 1993 U.S
    HYDROLOGY AND WATER CHEMISTRY OF SHALLOW AQUIFERS ALONG THE UPPER CLARK FORK, WESTERN MONTANA By David A. Nimick U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 93-4052 Prepared in cooperation with the MONTANA BUREAU OF MINES AND GEOLOGY Helena, Montana August 1993 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. Geological Survey DALLAS L. PECK, Director For additional information Copies of this report can write to: be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Earth Science Information Center 428 Federal Building Open-File Reports Section Drawer 10076 Box 25286, MS 517 301 South Park Denver Federal Center Helena, MT 59626-0076 Denver, CO 80225 CONTENTS Page Abstract. .................................. 1 Introduction. ................................ 1 Purpose and scope ............................. 2 Previous investigations .......................... 2 Quality assurance ............................. 4 Systems for specifying geographic locations ................ 5 Acknowledgments .............................. 6 Description of study area .......................... 6 Drainage and physiography ......................... 6 Climate .................................. 6 General geology .............................. 7 Hydrology and water chemistry of shallow aquifers .............. 9 Quaternary deposits ............................ 10 Aquifer characteristics ......................... 10 Water chemistry ............................. 13 Major ions. .............................. 13 Trace
    [Show full text]
  • Geology of the Wasa Mining Area Granite County Montana
    University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1956 Geology of the Wasa mining area Granite County Montana Kenneth Keith Smallwood The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Smallwood, Kenneth Keith, "Geology of the Wasa mining area Granite County Montana" (1956). Graduate Student Theses, Dissertations, & Professional Papers. 7108. https://scholarworks.umt.edu/etd/7108 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. GEOLOGY OF THE WA3A MINING AREA GRANITE COUNTY, MONTANA by Kenneth K. Smallwood B.S. Montana State University, 1949 Presented in partial fulfillment of the requirements for the degree of Master of Science MONTANA STATE UNIVERSITY 1956 Approved by: J j<J- Cljfl^man^^oarci oi* Examiners Üatï UMI Number: EP37909 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMT OisMftAtK^ FHiblishing UMI EP37909 Published by ProQuest LLC (2013). Copyright in the Dissertation held by the Author.
    [Show full text]