DOCSLIB.ORG

Soil Survey of Minnehaha County, South Dakota

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

United States In cooperation with South Department of Dakota Agricultural Agriculture Experiment Station at Soil Survey of South Dakota State Natural University Minnehaha Resources Conservation Service County, South Dakota NRCS Accessibility Statement The Natural Resources Conservation Service (NRCS) is committed to making its information accessible to all of its customers and employees. If you are experiencing accessibility issues and need assistance, please contact our Helpdesk by phone at 1-800-457-3642 or by e-mail at [email protected]. For assistance with publications that include maps, graphs, or similar forms of information, you may also wish to contact our State or local office. You can locate the correct office and phone number at http://offices.sc.egov.usda.gov/locator/app. 3 How To Use This Soil Survey General Soil Map The general soil map, which is a color map, shows the survey area divided into groups of associated soils called general soil map units. This map is useful in planning the use and management of large areas. To find information about your area of interest, locate that area on the map, identify the name of the map unit in the area on the color-coded map legend, then refer to the section General Soil Map Units for a general description of the soils in your area. 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, locate that area on the Index to Map Sheets. Note the number of the map sheet and turn to that sheet. Locate your area of interest on the map sheet. Note the map unit symbols that are in that area. Turn to the Contents, which lists the map units by symbol and name and shows the page where each map unit is described. The Contents shows which table has data on a specific land use for each detailed soil map unit. Also see the Contents for sections of this publication that may address your specific needs. 4 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 1994. Soil names and descriptions were approved in 1995. Unless otherwise indicated, statements in this publication refer to conditions in the survey area in 1995. This survey was made cooperatively by the Natural Resources Conservation Service and the South Dakota Agricultural Experiment Station at South Dakota State University. The survey is part of the technical assistance furnished to the Minnehaha County Conservation District. Financial assistance was furnished by the East Dakota Water Development District, Minnehaha County, and the City of Sioux Falls. 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: An area of Ihlen-Rock outcrop complex, 4 to 35 percent slopes, along the Big Sioux River at Sioux Falls. Additional information about the Nation’s natural resources is available on the Natural Resources Conservation Service homepage on the World Wide Web. The address is http://www.nrcs.usda.gov. 5 Contents How To Use This Soil Survey ................................. 3 Cb—Chancellor silty clay loam, 0 to 1 percent Foreword ................................................................. 9 slopes .......................................................... 38 General Nature of the County ................................. 11 Cc—Chancellor-Tetonka complex, 0 to 1 Climate ............................................................... 11 percent slopes ............................................. 39 Physiography, Relief, and Drainage .................... 12 Cd—Chaska loam, 0 to 2 percent slopes ........... 40 Settlement .......................................................... 12 Ch—Chaska loam, channeled ............................ 41 Farming .............................................................. 12 Cm—Clamo silty clay, 0 to 1 percent slopes ....... 42 Natural Resources ............................................. 13 CoB—Corson silty clay, 2 to 6 percent slopes .... 43 How This Survey Was Made ................................... 13 CoC—Corson silty clay, 6 to 9 percent General Soil Map Units ........................................ 15 slopes .......................................................... 44 1. Egan-Ethan-Trent Association .................... 15 CpC—Corson-Henkin complex, 6 to 9 percent 2. Egan-Wentworth-Trent Association ............ 17 slopes .......................................................... 45 3. Moody-Trent Association ............................ 17 CrD—Crofton-Nora complex, 9 to 15 percent 4. Moody-Nora Association ............................ 18 slopes .......................................................... 46 5. Nora-Crofton Association ........................... 18 CrE—Crofton-Nora complex, 15 to 25 percent 6. Splitrock-Trent Association ......................... 20 slopes .......................................................... 47 7. Houdek-Shindler Association ..................... 20 CsD—Crofton-Shindler complex, 9 to 15 8. Shindler-Steinauer Association .................. 21 percent slopes ............................................. 48 9. Grovena-Dobalt-Flandreau Association ..... 22 DcA—Davis loam, 0 to 2 percent slopes ............ 49 10. Flandreau-Thurman-Grovena DcB—Davis loam, 2 to 6 percent slopes ............ 49 Association ............................................... 22 DcC—Davis loam, 6 to 9 percent slopes ............ 50 11. Dempster-Graceville Association ............... 23 Dd—Davison-Crossplain clay loams, 0 to 2 12. Clamo-Chaska Association ........................ 24 percent slopes ............................................. 51 13. Bon-Davis-Chaska Association .................. 25 DeA—Delmont-Enet loams, 0 to 2 percent 14. Chaska-Davis-Bon Association .................. 26 slopes .......................................................... 52 15. Lamo-Graceville Association...................... 27 DeB—Delmont-Enet loams, 2 to 6 percent 16. Corson-Benclare Association..................... 27 slopes .......................................................... 53 Detailed Soil Map Units ........................................ 29 DgC—Delmont-Talmo complex, 6 to 9 percent AcA—Alcester silty clay loam, 0 to 2 percent slopes .......................................................... 54 slopes .......................................................... 30 DgD—Delmont-Talmo complex, 9 to 15 AcB—Alcester silty clay loam, 2 to 6 percent percent slopes ............................................. 55 slopes .......................................................... 30 DmA—Dempster silt loam, 0 to 2 percent Ar—Arlo loam, 0 to 1 percent slopes .................. 32 slopes .......................................................... 56 Ba—Baltic silty clay loam, 0 to 1 percent DmB—Dempster silt loam, 2 to 6 percent slopes .......................................................... 33 slopes .......................................................... 57 Bb—Baltic silty clay loam, ponded ...................... 33 DtB—Dempster-Talmo complex, 2 to 6 BcA—Benclare-Corson complex, 0 to 2 percent slopes ............................................. 58 percent slopes ............................................. 34 Dw—Dimo clay loam, 0 to 2 percent slopes ....... 59 BeE—Betts-Ethan loams, 15 to 40 percent DxB—Dobalt loam, 2 to 6 percent slopes ........... 60 slopes .......................................................... 35 DyA—Dobalt-Bonilla loams, 0 to 2 percent BfA—Blendon fine sandy loam, 0 to 2 percent slopes .......................................................... 60 slopes .......................................................... 36 EaB—Egan-Ethan complex, 2 to 6 percent BhB—Blendon-Henkin fine sandy loams, 2 to slopes .......................................................... 61 6 percent slopes .......................................... 37 EeB—Egan-Ethan-Trent complex, 1 to 6 Bo—Bon loam, 0 to 2 percent slopes ................. 38 percent slopes ............................................. 62 6 EfA—Egan-Trent silty clay loams, 0 to 2 Ja—Janude fine sandy loam, 0 to 2 percent percent slopes ............................................. 64 slopes .........................................................
Recommended publications
  • A Historical Geography of Lake Kampeska in the City of Watertown, South Dakota Joanita M

    A Historical Geography of Lake Kampeska in the City of Watertown, South Dakota Joanita M

    South Dakota State University Open PRAIRIE: Open Public Research Access Institutional Repository and Information Exchange Geography Faculty Publications Department of Geography 2007 A Historical Geography of Lake Kampeska in the City of Watertown, South Dakota Joanita M. Kant South Dakota State University, [email protected] Follow this and additional works at: https://openprairie.sdstate.edu/geo_pubs Part of the Physical and Environmental Geography Commons Recommended Citation Kant, Joanita M., "A Historical Geography of Lake Kampeska in the City of Watertown, South Dakota" (2007). Geography Faculty Publications. 2. https://openprairie.sdstate.edu/geo_pubs/2 This Article is brought to you for free and open access by the Department of Geography at Open PRAIRIE: Open Public Research Access Institutional Repository and Information Exchange. It has been accepted for inclusion in Geography Faculty Publications by an authorized administrator of Open PRAIRIE: Open Public Research Access Institutional Repository and Information Exchange. For more information, please contact [email protected]. i A Historical Geography of Lake Kampeska in the City of Watertown, South Dakota 2007 by Joanita Kant copyright ii “Never forget that a small group of thoughtful, committed citizens can change the world. Indeed, it is the only thing that ever has.” Margaret Meade i ABSTRACT Many alterations in the hydrology of Lake Kampeska began with the arrival of masses of Anglo settlers in the 1870s. Why the lake has been altered is a complex issue linked to various natural physical processes which would have occurred even without the introduction of those settlers into the ecosystem. Those processes include weather, climate, sedimentation rates, lakebank erosion, chemical and mineral transport from soils, and flooding, among others.
  • Status of Mineral Resource Information for the Standing Rock Indian Reservation, North Dakota and South Dakota

    Status of Mineral Resource Information for the Standing Rock Indian Reservation, North Dakota and South Dakota

    STATUS OF MINERAL RESOURCE INFORMATION FOR THE STANDING ROCK INDIAN RESERVATION, NORTH DAKOTA AND SOUTH DAKOTA By Lee R. Rice Richard Bretz U.S. Bureau of Mines South Dakota Geological Survey Administrative Report BIA-41 1978 CONTENTS SUMMARY AND CONCLUSIONS ................................................. 1 INTRODUCTION ................................................................ 1 Previous Work ............................................................. 2 Land Status................................................................ 2 Map Coverage ............................................................. 3 Physiography .............................................................. 3 GEOLOGY ..................................................................... 4 General ................................................................... 4 Stratigraphy ............................................................... 4 Outcropping Rock Units ............................................... 4 Subsurface Rock Units ................................................. 5 Structure.................................................................. 5 GEOPHYSICS ................................................................... 6 MINERAL RESOURCES .......................................................... 6 General ................................................................... 6 Energy Resources........................................................... 6 Lignite ............................................................. 6 General
  • Fishes of South Dakota

    Fishes of South Dakota

    MISCELLANEOUS PUBLICATIONS MUSEUM OF ZOOLOGY, UNIVERSITY OF MICHIGAN, NO. 119 Fishes of South Dakota REEVE M. BAILEY AND MARVIN 0. ALLUM South Dakota State College ANN ARBOR MUSEUM OF ZOOLOGY, UNIVERSITY OF MICHIGAN JUNE 5, 1962 MISCELLANEOUS PUBLICATIONS MUSEUM OF ZOOLOGY, UNIVERSITY 01; MICHIGAN The publications of the Museum of Zoology, University of Michigan, consist of two series-the Occasional Papers and the Miscellaneous Publications. Both series were founded by Dr. Bryant Walker, Mr. Bradshaw H. Swales, and Dr. W. W. Newcomb. The Occasional Papers, publication of which was begun in 1913, serve as a medium for original studies based principally upon the collections in the Museum. They are issued separately. When a sufficient number of pages has been printed to make a volume, a title page, table of contents, and an index are supplied to libraries and indi- viduals on the mailing list for the series. The Miscellaneous Publications, which include papers on field and museum tech- niques, monographic studies, and other contributions not within the scope of the Occasional Papers, are published separately. It is not intended that they be grouped into volumes. Each number has a title page and, when necessary, a table of contents. A conlplete list of publications on Birds, Fishes, Insects, Mammals, Mollusks, and Reptiles and Amphibians is available. Address inquiries to the Director, Museum of Zoology, Ann Arbor, Michigan No. 13. Studies of the fishes of the order Cyprinodontes. By CARL L. HUBBS. (1924) 23 pp., 4 pls. ............................................. No. 15. A check-list of the fishes of the Great Lakes and tributary waters, with nomenclatorial notes and analytical keys.
  • Memorial to Edgar Paul Rothrock 1889-1977 DAVID P

    Memorial to Edgar Paul Rothrock 1889-1977 DAVID P

    Memorial to Edgar Paul Rothrock 1889-1977 DAVID P. ROTHROCK 10040 West 8th A venue, Lakewood, Colorado 80215 On 2 August 1977, Edgar Paul Rothrock was claimed by cancer. His death ended many years of public serv­ ice to the people of South Dakota. His association with the Geological Survey and the University at Ver­ million began in 1922 and was concurrent with the economic growth of the state. Dr. Rothrock was sixty-eight days older than the State of South Dakota and part of the pioneer generation who brought the state to its present economic development. Edgar was born on 26 August 1889, the eldest of three sons of a Congregational minister in Garretts- ville, Ohio. He graduated from Lincoln High School, Cleveland, in the class of “ naughty eight” (1908). Drawn by R. C. Moore Reading ability in Latin and Greek was a requirement in those days. As late as the 1970s, he took pleasure from his Greek copy of Xenophon. After a year at Western Reserve University, he entered Oberlin College and completed the A.B. in 1912, the M.A. in 1914. At Oberlin, Dr. George Hubbard encouraged him to enter the profession of geology. The Oberlin summer camps of 1912 and 1913 were good neophyte training because the New River Narrows country in Giles County, Virginia, has rough topography and is not overly generous with outcrops. The school year of 1914-1915 found Edgar at Kidder Institute, Kidder, Missouri. That job paid $800 for nine months work as “science” instructor teaching physics, geometry, algebra, and agriculture.
  • One Hundred Years of Geology and Hydrology Papers Published in the Proceedings of the South Dakota Academy of Science

    One Hundred Years of Geology and Hydrology Papers Published in the Proceedings of the South Dakota Academy of Science

    Proceedings of the South Dakota Academy of Science, Vol. 94 (2015) 85 ONE HUNDRED YEARS OF GEOLOGY AND HYDROLOGY PAPERS PUBLISHED IN THE PROCEEDINGS OF THE SOUTH DAKOTA ACADEMY OF SCIENCE Perry H. Rahn Department of Geology and Geological Engineering South Dakota School of Mines and Technology Rapid City, SD 57701 Corresponding author email: [email protected] ABSTRACT In 2015 The South Dakota Academy of Science celebrated one hundred years of publication of the Proceedings. This paper is written as part of the historic contributions to the Academy, focusing on the nearly two hundred papers deal- ing with geology and hydrology that have been published in the Proceedings. Emphasis in this paper is given to papers that are concerned with the Missouri River and the Homestake gold mine. Keywords Geology, hydrology, Missouri River, Homestake mine INTRODUCTION During the past 100 years there have been 180 full papers published in the Proceedings of the South Dakota Academy of Science that are primarily con- cerned with geology, paleontology, or hydrology. In addition, there are numerous abstracts published in the Proceedings that touch on these subjects. The purpose of this paper is to briefly review several of these papers and show how they have contributed to their respective disciplines. Since there have been so many papers published in the Proceedings that have been written about di- verse subjects within the general areas of geology and hydrology, it is not feasible to discuss all these references. Therefore, only a few citations are given in this paper, and two general themes are chosen that represent important works from both “East River” and “West River” within the State of South Dakota.
  • Pleistocene Geology of Eastern South Dakota

    Pleistocene Geology of Eastern South Dakota

    Pleistocene Geology of Eastern South Dakota GEOLOGICAL SURVEY PROFESSIONAL PAPER 262 Pleistocene Geology of Eastern South Dakota By RICHARD FOSTER FLINT GEOLOGICAL SURVEY PROFESSIONAL PAPER 262 Prepared as part of the program of the Department of the Interior *Jfor the development-L of*J the Missouri River basin UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1955 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $3 (paper cover) CONTENTS Page Page Abstract_ _ _____-_-_________________--_--____---__ 1 Pre- Wisconsin nonglacial deposits, ______________ 41 Scope and purpose of study._________________________ 2 Stratigraphic sequence in Nebraska and Iowa_ 42 Field work and acknowledgments._______-_____-_----_ 3 Stream deposits. _____________________ 42 Earlier studies____________________________________ 4 Loess sheets _ _ ______________________ 43 Geography.________________________________________ 5 Weathering profiles. __________________ 44 Topography and drainage______________________ 5 Stream deposits in South Dakota ___________ 45 Minnesota River-Red River lowland. _________ 5 Sand and gravel- _____________________ 45 Coteau des Prairies.________________________ 6 Distribution and thickness. ________ 45 Surface expression._____________________ 6 Physical character. _______________ 45 General geology._______________________ 7 Description by localities ___________ 46 Subdivisions. ________-___--_-_-_-______ 9 Conditions of deposition ___________ 50 James River lowland.__________-__-___-_--__ 9 Age and correlation_______________ 51 General features._________-____--_-__-__ 9 Clayey silt. __________________________ 52 Lake Dakota plain____________________ 10 Loveland loess in South Dakota. ___________ 52 James River highlands...-------.-.---.- 11 Weathering profiles and buried soils. ________ 53 Coteau du Missouri..___________--_-_-__-___ 12 Synthesis of pre- Wisconsin stratigraphy.
  • Hydrogeologic Framework for the Madison and Minnelusa Aquifers in the Black Hills Area

    Hydrogeologic Framework for the Madison and Minnelusa Aquifers in the Black Hills Area

    Hydrogeologic Framework for the Madison and Minnelusa Aquifers in the Black Hills Area by Jonathan D.R.G. McKaskey A thesis submitted to the Graduate Division in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE IN GEOLOGICAL ENGINEERING SOUTH DAKOTA SCHOOL OF MINES AND TECHNOLOGY RAPID CITY, SOUTH DAKOTA 2013 Prepared by: _____________________________________ Jonathan D.R.G McKaskey, Degree Candidate Approved by: _____________________________________ Dr. Arden Davis, Major Professor _____________________________________ Dr. Jennifer Benning, Graduate Division Representative _____________________________________ Dr. Kurt Katzenstein, Committee Member _____________________________________ Dr. Andrew Long, Committee Member _____________________________________ Dr. Laurie Anderson, Head of Department of Geology and Geological Engineering _____________________________________ Dr. Douglas Wells, Dean of Graduate Education i Abstract More than 50 percent of the public drinking water systems and more than 90 percent of the population in South Dakota rely solely on groundwater. This dependence on groundwater raises important questions regarding the Madison and Minnelusa aquifers in and near the Black Hills of South Dakota, including groundwater availability, the effects of water use or drought, mixing of regional flow and local recharge, and the effects of capture zones of springs and wells on the groundwater-flow system. These questions are best addressed with a three-dimensional numerical groundwater-flow model that
  • Publications of the South Dakota Geological Survey

    Publications of the South Dakota Geological Survey

    STATE OF SOUTH DAKOTA M. Michael Rounds, Governor DEPARTMENT OF ENVIRONMENT AND NATURAL RESOURCES Steven M. Pirner, Secretary DIVISION OF FINANCIAL AND TECHNICAL ASSISTANCE David Templeton, Director GEOLOGICAL SURVEY PROGRAM Derric L. Iles, State Geologist PUBLICATIONS OF THE SOUTH DAKOTA GEOLOGICAL SURVEY Akeley-Lawrence Science Center University of South Dakota Vermillion, South Dakota REVISION DATE: JUNE 29, 2009 GEOLOGICAL SURVEY PROGRAM DEPARTMENT OF ENVIRONMENT AND NATURAL RESOURCES AKELEY-LAWRENCE SCIENCE CENTER, USD 414 EAST CLARK STREET VERMILLION, SOUTH DAKOTA 57069-2390 (605) 677-5227 Derric L. Iles, M.S., C.P.G. State Geologist Sarah A. Chadima, M.S. Senior Geologist Timothy C. Cowman, M.S. Natural Resources Administrator Brian A. Fagnan, M.S. Senior Geologist Dragan Filipovic, M.S. Senior Hydrologist Thomas N. Haggar, B.S. Senior Geologist Ann R. Jensen, B.S. Senior Geologist Matthew T. Noonan, B.S. Hydrologist Thomas B. Rich, M.S. Senior Hydrologist Layne D. Schulz, B.S. Senior Geologist Dennis D. Iverson Civil Engineering Technician Scott W. Jensen Civil Engineering Technician Ted R. Miller, B.S. Civil Engineering Technician Colleen K. Odenbrett Word Processing Supervisor Jeffrey J. Puthoff, B.A. Natural Resources Technician Lori L. Roinstad Cartographer Priscilla E. Young, B.S. Senior Secretary RAPID CITY REGIONAL OFFICE 2050 WEST MAIN, SUITE 1 RAPID CITY, SOUTH DAKOTA 57702-2493 (605) 394-2229 Mark D. Fahrenbach, Ph.D. Senior Geologist Kelli A. McCormick, Ph.D. Senior Geologist Joanne M. Noyes, M.S., P.E. Senior Hydrologist CONTENTS Page THE SOUTH DAKOTA GEOLOGICAL SURVEY ................................................................ 1 HOW TO OBTAIN PUBLICATIONS AND MAP PRODUCTS .......................................... 1 BASIC-DATA REPORT SERIES ................................................................................................
  • Jewel Cave National Monument Historic Resource Study

    Jewel Cave National Monument Historic Resource Study

    PLACE OF PASSAGES: JEWEL CAVE NATIONAL MONUMENT HISTORIC RESOURCE STUDY 2006 by Gail Evans-Hatch and Michael Evans-Hatch Evans-Hatch & Associates Published by Midwestern Region National Park Service Omaha, Nebraska _________________________________ i _________________________________ ii _________________________________ iii _________________________________ iv Table of Contents Introduction 1 Chapter 1: First Residents 7 Introduction Paleo-Indian Archaic Protohistoric Europeans Rock Art Lakota Lakota Spiritual Connection to the Black Hills Chapter 2: Exploration and Gold Discovery 33 Introduction The First Europeans United States Exploration The Lure of Gold Gold Attracts Euro-Americans to Sioux Land Creation of the Great Sioux Reservation Pressure Mounts for Euro-American Entry Economic Depression Heightens Clamor for Gold Custer’s 1874 Expedition Gordon Party & Gold-Seekers Arrive in Black Hills Chapter 3: Euro-Americans Come To Stay: Indians Dispossessed 59 Introduction Prospector Felix Michaud Arrives in the Black Hills Birth of Custer and Other Mining Camps Negotiating a New Treaty with the Sioux Gold Rush Bust Social and Cultural Landscape of Custer City and County Geographic Patterns of Early Mining Settlements Roads into the Black Hills Chapter 4: Establishing Roots: Harvesting Resources 93 Introduction Milling Lumber for Homes, Mines, and Farms Farming Railroads Arrive in the Black Hills Fluctuating Cycles in Agriculture Ranching Rancher Felix Michaud Harvesting Timber Fires in the Forest Landscapes of Diversifying Uses _________________________________ v Chapter 5: Jewel Cave: Discovery and Development 117 Introduction Conservation Policies Reach the Black Hills Jewel Cave Discovered Jewel Cave Development The Legal Environment Developing Jewel Cave to Attract Visitors The Wind Cave Example Michauds’ Continued Struggle Chapter 6: Jewel Cave Under the U.S.
  • Dreams and Dust in the Black Hills: Race, Place, and National Identity in America's "Land of Promise" Elaine Marie Nelson

    Dreams and Dust in the Black Hills: Race, Place, and National Identity in America's "Land of Promise" Elaine Marie Nelson

    University of New Mexico UNM Digital Repository History ETDs Electronic Theses and Dissertations 8-19-2011 Dreams and Dust in the Black Hills: Race, Place, and National Identity in America's "Land of Promise" Elaine Marie Nelson Follow this and additional works at: https://digitalrepository.unm.edu/hist_etds Part of the History Commons Recommended Citation Nelson, Elaine Marie. "Dreams and Dust in the Black Hills: Race, Place, and National Identity in America's "Land of Promise"." (2011). https://digitalrepository.unm.edu/hist_etds/58 This Dissertation is brought to you for free and open access by the Electronic Theses and Dissertations at UNM Digital Repository. It has been accepted for inclusion in History ETDs by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. i ii ©2011, Elaine Marie Nelson iii DEDICATION I wish to dedicate this to my parents—and their parents—for instilling in me a deep affection for family, tradition, history, and home. iv ACKNOWLEDGMENTS I do not remember our first family vacation. My sisters and I were so used to packing up and hitting the road in the family station wagon (later a minivan), that our childhood trips blur together. Oftentimes we visited our paternal grandparents in Sidney, Nebraska, or our maternal grandparents in Lincoln, Nebraska. But on special occasions we would take lengthy road trips that ended with destinations in the Appalachian Mountains, the Gulf of Mexico, Yellowstone National Park, and Myrtle Beach. As an ―East River‖ South Dakotan, driving six hours west to visit the Black Hills was hardly as exciting as going to the beach.
  • Geology of the Flint Hill Quadrangle, Fall River County, South Dakota

    Geology of the Flint Hill Quadrangle, Fall River County, South Dakota

    GeologyCJm/ of the Flint Hill Quadrangle, Fall River County, South Dakota_^^^ = GEOLOGICAL SURVEY BULLETIN 1063-M a | Prepared on behalf of the * U.S. Atomic Energy Commission Geology of the Flint Hill Quadrangle, Fall River County, South Dakota By HENRY BELL III and EDWIN V. POST GEOLOGY AND URANIUM DEPOSITS OF THE SOUTHERN BLACK HILLS GEOLOGICAL SURVEY BULLETIN 1063-M Prepared on behalf of the U.S. Atomic Energy Commission A description of the stratigraphy and structure in the quadrangle, with emphasis on the rocks of the Inyan Kara Group of Early Cretaceous age UNITED STATES GOVERNMENT PRINTING. OFFICE, WASHINGTON : 1971 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY W. A. Radlinski, Acting Director Library of Congress catalog-card No. 72-172970 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 2401-1124 CONTENTS Page Abstract__________________-___-___________-__--__-..------------ M505 Introduction. _____________________________________________________ 506 Regional stratigraphic setting.______________________________________ 508 Jurassic rocks.________-___-_-_-______-_______-___-___-__-___---_-- 509 Sundance Formation..__________________________________________ 509 Lak Member____________________________________________ 510 Redwater Shale Member._____________.___-___-.______._--_ 510 Unkpapa Sandstone.__-_-_-__________________-__--_-__---__--- 510 Morrison Formation.__________________________________________ 513 Cretaceous rocks-_____________-__________________-__--_--__--._--_ 516 Lower Cretaceous rocks._______________________________________ 516 Inyan Kara Group.________________._-___-___-__-__---.--_ 516 History of stratigraphic nomenclature.______-_____-__--__ 516 Lakota Formation________________.____________________ 518 Chilson Member_________________________________ 518 Unit l__--_-______-________-___________-_--_- 518 Unit 2_______________________________________ 527 Interpretation of environments--.-.----.-------- 532 Minnewaste Limestone Member.
  • South Dakota's Railroads

    South Dakota's Railroads

    South Dakota’s Railroads South Dakota State Historic Preservation Office South Dakota’s Railroads: An Historic Context Prepared for: South Dakota State Historic Preservation Office 900 Governors Drive Pierre, South Dakota 57501 Prepared by: Mark Hufstetler and Michael Bedeau Renewable Technologies, Inc. 511 Metals Bank Bldg. Butte, Montana 59701 July 1998 Revised, December 2007 TABLE OF CONTENTS 1. Introduction.................................................................................................................................2 A. Purpose of this Document..............................................................................................2 B. Methodology ..................................................................................................................3 2. The Importance of Railroads to South Dakota ...........................................................................4 3. The History of Railroading in South Dakota..............................................................................5 A. Geographical Background .............................................................................................5 B. Establishment and Expansion: South Dakota Railroads in the Nineteenth Century......6 1. Beginnings (1851-1868) .....................................................................................6 2. The Little Dakota Boom and the First Railroads (1868-1873)...........................8 3. Railway Expansion During the Great Dakota Boom (1878-1887).....................9 4. The Impact and