Some Sioux Legends in Pictures
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The Rise and Fall of the Lake Pepin “Half-Breed Tract” Allison C. Bender
Valuable People: The Rise and Fall of the Lake Pepin “Half-Breed Tract” Allison C. Bender History 489: Research Seminar Fall Term 2016 Contents Abstract………...……….……………………………...…………………………………………iii Introduction and Historiography…………………………………………………………………..1 Race as a Social Construct.....……………………………………………………………………..5 Treaty of Prairie du Chien 1825…………………………………………………….......................7 Understanding the Treaty of Prairie du Chien 1830......................................................................10 The Lake Pepin “Half-Breed” Tract..............................................................................................16 Franklin Steele and the Fort Snelling Internment Camp...............................................................18 Call for Further Research………………………………………………………………………...22 Conclusion……………………………………………………………………………………….24 Works Cited.………………………………………………………………….………………….27 ii Abstract This paper focuses on the Dakota nation during the early nineteenth century while discussing the various tribes within the Midwest during that time. These tribes include the Ojibwe, confederated Sacs and Foxes, Ho-Chunk, Menominee, Ioway, Ottowa, and Potawatomi. As intertribal warfare disrupted the peace between these tribes, it also disrupted the plans of many European settlers who had wanted to live, farm, hunt, mineral mine, and trade in the Midwest. One can see evidence of this disruption by visiting treaties from the early nineteenth century as well as accounts from various Indian Agents from this time. Several treaties -
Ecological Regions of Minnesota: Level III and IV Maps and Descriptions Denis White March 2020
Ecological Regions of Minnesota: Level III and IV maps and descriptions Denis White March 2020 (Image NOAA, Landsat, Copernicus; Presentation Google Earth) A contribution to the corpus of materials created by James Omernik and colleagues on the Ecological Regions of the United States, North America, and South America The page size for this document is 9 inches horizontal by 12 inches vertical. Table of Contents Content Page 1. Introduction 1 2. Geographic patterns in Minnesota 1 Geographic location and notable features 1 Climate 1 Elevation and topographic form, and physiography 2 Geology 2 Soils 3 Presettlement vegetation 3 Land use and land cover 4 Lakes, rivers, and watersheds; water quality 4 Flora and fauna 4 3. Methods of geographic regionalization 5 4. Development of Level IV ecoregions 6 5. Descriptions of Level III and Level IV ecoregions 7 46. Northern Glaciated Plains 8 46e. Tewaukon/BigStone Stagnation Moraine 8 46k. Prairie Coteau 8 46l. Prairie Coteau Escarpment 8 46m. Big Sioux Basin 8 46o. Minnesota River Prairie 9 47. Western Corn Belt Plains 9 47a. Loess Prairies 9 47b. Des Moines Lobe 9 47c. Eastern Iowa and Minnesota Drift Plains 9 47g. Lower St. Croix and Vermillion Valleys 10 48. Lake Agassiz Plain 10 48a. Glacial Lake Agassiz Basin 10 48b. Beach Ridges and Sand Deltas 10 48d. Lake Agassiz Plains 10 49. Northern Minnesota Wetlands 11 49a. Peatlands 11 49b. Forested Lake Plains 11 50. Northern Lakes and Forests 11 50a. Lake Superior Clay Plain 12 50b. Minnesota/Wisconsin Upland Till Plain 12 50m. Mesabi Range 12 50n. Boundary Lakes and Hills 12 50o. -
To Prairie Preserves
This document is made available electronically by the Minnesota Legislative Reference Library as part of an ongoing digital archiving project. http://www.leg.state.mn.us/lrl/lrl.asp (Funding for document digitization was provided, in part, by a grant from the Minnesota Historical & Cultural Heritage Program.) A GUIDE TO MINNESOTA PRAIRIES By Keith M. Wendt Maps By Judith M. Ja.cobi· Editorial Assistance By Karen A. Schmitz Art and Photo Credits:•Thorn_as ·Arter, p. 14 (bottom left); Kathy Bolin, ·p: 14 (top); Dan Metz, pp. 60, 62; Minnesota Departme'nt of Natural Resources, pp. '35 1 39, 65; U.S. Department of Agriculture, p. -47; Keith Wendt, cover, pp~ 14 (right), 32, 44; Vera Wohg, PP· 22, 43, 4a. · · ..·.' The Natural Heritage Program Minnesota Department of Natural Resources Box 6, Centennial Office Building . ,. St. Paul; MN 55155 ©Copyright 1984, State of Minnesota, Department of Natural Resource.s CONTENTS PREFACE .......................................... Page 3 INTRODUCTION .................................... Page 5 MINNESOTA PRAIRIE TYPES ........................... Page 6 PROTECTION STATUS OF MINNESOTA PRAIRIES ............ Page 12 DIRECTORY OF PRAIRIE PRESERVES BY REGION ............ Page 15 Blufflands . Page 18 Southern Oak Barrens . Page 22 Minnesota River Valley ............................. Page 26 Coteau des Prairies . Page 32 Blue Hills . Page 40 Mississippi River Sand Plains ......................... Page 44 Red River Valley . Page 48 Aspen Parkland ................................... Page 62 REFERENCES ..................................... Page 66 INDEX TO PRAIRIE PRESERVES ......................... Page 70 2 PREFACE innesota has established an outstanding system of tallgrass prairie preserves. No state M in the Upper Midwest surpasses Minnesota in terms of acreage and variety of tallgrass prairie protected. Over 45,000 acres of native prairie are protected on a wide variety of landforms that span the 400 mile length of the state from its southeast to northwest corner. -
Explore Minnesota S Prairies
Explore Minnesota s Prairies A guide to selected prairies around the state. By Peter Buesseler ECAUSE I'M the Depart- ment of Natural Re- sources state prairie biologist, people of- Bten ask me where they can go to see a prairie. Fortunately, Minnesota has established an outstanding system of prai- rie preserves. No state in the upper Midwest surpasses Minnesota in terms of acre- age and variety of tallgrass prairie protected. There is Among the prairies to explore are spectacular probably native prairie closer bluffland prairies located just a few hours south to you than you think. of the Twin Cities along the Mississippi River. When is the best time to visit a prairie? From the first pasque Read about the different prairie flowers and booming of prairie chick- regions and preserves described be- ens in April, to the last asters and low, then plan an outing with family bottle gentians in October, the prairie or friends. The most important thing is a kaleidoscope of color and change. is not when or where to go—just go! So don't worry. Every day is a good The following abbreviations are day to see prairie. used in the list of prairie sites: SNA 30 THE MINNESOTA VOLUNTEER means the prairie is a state scientific wildlife refuge. My personal favorites and natural area; TNC means the are marked with an asterisk (*). Have prairie is owned by The Nature Con- fun exploring your prairie heritage. servancy, a private, nonprofit conser- Red River Valley vation organization; WMA means the During the last ice age (10,000 to site is a state wildlife management 12,000 years ago), a great lake area; and NWR stands for national stretched from Wheaton, Minn., to the JULY-AUGUST 1990 31 Our Prairie Heritage sandy beach ridges of Glacial Lake Agassiz. -
Mississippi River Guide
see map on page 31 Mississippi River 815.3R Lock and Dam No. 2, U.S. Army Corps of Engineers lock on right 814.6R Lake Rebecca Municipal Park, City of Hastings 814.1R concrete plank ramp on lake, picnic area, trail, portable chemical toilet (across road) Lake Rebecca 814.3R Mississippi River - Hastings Public Access, MN DNR and City of Hastings concrete slab ramp Conley Lake 813.8L King’s Cove Marina, LLC, Private entrance at River Mile 812.7L, dockage, fuel, pumpouts, repair facilities, restrooms, service and canvas department, ship’s store, slips for rent, storage, brokerage (651) 437-6186, (651) 480-8900 fax (651) 480-8926 www.kingscove.com Mississippi River 815.3- Hastings area 812.0R food, lodging Dakota County Sheriff emergency 911 or non-emergency (651) 438-4771 814.2L Hub’s Landing and Marina, Private concrete slab ramp (fee), transient slips, overnight parking available (651) 437-4358 www.hubslanding.com 813.3R Hastings Marina, Inc., Private concrete slab ramp (fee), fuel, pumpouts, restrooms, showers, snacks, water & pop (651) 437-9621, fax (651) 438-9924 St. Croix River 0.4- Prescott area 810.8L food, lodging away from river www.saintcroixriver.com Pierce County Sheriff emergency 911 or all other services (715) 273-5051 28 St. Croix River Continued 0.5L Prescott Public Beach, City of Prescott beach 0.3R Point Douglas, Washington County Parks fishing pier, picnicking, restrooms, swimming beach (651) 430-8240 www.co.washington.mn.us/parks 0.1L Prescott City, Courtesy Dock temporary docking (fee) Mississippi River 811.5- Prescott area 810.8L food, lodging www.saintcroixriver.com Pierce County Sheriff emergency 911 or all other services (715) 273-5051 811.4L Leo’s Landing, Private temporary dockage, fuel, full service marina, pumpouts, restrooms (715) 262-5998, fax (651) 770-8870 e-mail: [email protected] 811.4L Point St. -
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. -
S`Jt≈J`§≈J`§ ¢`§Mnln”D: the EVERCHANGING PIPESTONE QUARRIES
The Everchanging Pipestone Quarries Sioux Cultural Landscapes and Ethnobotany of Pipestone National Monument, Minnesota Item Type Report Authors Toupal, Rebecca; Stoffle, Richard, W.; O'Meara, Nathan; Dumbauld, Jill Publisher Bureau of Applied Research in Anthropology, University of Arizona Download date 05/10/2021 14:10:29 Link to Item http://hdl.handle.net/10150/292658 S`jt≈j`§≈j`§ ¢`§mnln”d: THE EVERCHANGING PIPESTONE QUARRIES SIOUX CULTURAL LANDSCAPES AND ETHNOBOTANY OF PIPESTONE NATIONAL MONUMENT, MINNESOTA Final Report June 30, 2004 Rebecca S. Toupal Richard W. Stoffle Nathan O’Meara Jill Dumbauld BUREAU OF APPLIED RESEARCH IN ANTHROPOLOGY THE UNIVERSITY OF ARIZONA S`jt≈j`§≈j`§ ¢`§mnln”d: THE EVERCHANGING PIPESTONE QUARRIES SIOUX CULTURAL LANDSCAPES AND ETHNOBOTANY OF PIPESTONE NATIONAL MONUMENT, MINNESOTA Final Report Prepared by Rebecca S. Toupal Richard W. Stoffle Nathan O’Meara and Jill Dumbauld Prepared for National Park Service Midwest Region Under Task Agreement 27 of Cooperative Agreement H8601010007 R.W. Stoffle and M. N. Zedeño, Principal Investigators Bureau of Applied Research in Anthropology University of Arizona Tucson, AZ 86721 June 30, 2004 TABLE OF CONTENTS PREFACE................................................................................................................................ iv ACKNOWLEDGEMENTS..................................................................................................... vi STUDY OVERVIEW................................................................................................................1 -
Earth Sciences: Two-Ice-Lobe Model for Kansan Glaciation James S
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Transactions of the Nebraska Academy of Sciences Nebraska Academy of Sciences and Affiliated Societies 1982 Earth Sciences: Two-Ice-Lobe Model For Kansan Glaciation James S. Aber Emporia State University Follow this and additional works at: http://digitalcommons.unl.edu/tnas Aber, James S., "Earth Sciences: Two-Ice-Lobe Model For Kansan Glaciation" (1982). Transactions of the Nebraska Academy of Sciences and Affiliated Societies. 490. http://digitalcommons.unl.edu/tnas/490 This Article is brought to you for free and open access by the Nebraska Academy of Sciences at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Transactions of the Nebraska Academy of Sciences and Affiliated Societies by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. 1982. Transactions a/the Nebraska Academy a/Sciences, X:25-29. EARTH SCIENCES TWO-ICE-LOBE MODEL FOR KANSAN GLACIATION James S. Aber Geoscience Department Emporia State University Emporia, Kansas 66801 The Kansan glaciation should be representative of Early Pleisto western source area, the so-called Keewatin Center, in the cene glaciations in the Kansas-Nebraska-Iowa-Missouri region. It is region west of Hudson Bay. Frye and Leonard (1952: 11) often assumed the Kansan ice-sheet advanced as a single, broad lobe supported this concept on the basis of distribution of the coming from somewhere in Canada. This simple view contrasts with the known complexities of the younger Wisconsin glaciation, and indeed Sioux Quartzite, a common erratic derived mainly from east there is much evidence that the Kansan glaciation was equally complex. -
Restoring the Upper Mississippi River at Lake Pepin: Phase 1
Lessard-Sams Outdoor Heritage Council HRE 12 Fiscal Year 2020 / ML 2019 Request for Funding Date: May 31, 2018 Program or Project Title: Restoring the Upper Mississippi River at Lake Pepin: Phase 1 Fund s Req uested : $750,000 Manager's Name: Rylee Main T itle: Executive Director Organization: Lake Pepin Legacy Alliance Ad d ress: P.O. Box 392 C ity: Red Wing, MN 55066 Office Number: 630-806-9909 Mobile Number: 630-806-9909 Email: [email protected] Web site: www.lakepepinlegacyalliance.org County Locations: Goodhue Regions in which work will take place: Southeast Forest Activity types: Restore Enhance Priority resources addressed by activity: Wetlands Forest Habitat Abstract: This project leverages more than $10 million in federal funds to begin implementation of a system-wide effort to improve game fish and waterfowl production in the Upper Mississippi River by improving 100 acres of floodplain forest and up to 1,000 acres of aquatic and wetland habitat at the upper end of Lake Pepin. Local partners are working with the U.S. Army Corps of Engineers to mitigate habitat degradation caused by turbidity and excess sediment accumulating at the head of the lake. Project construction is anticipated to begin in 2020. Design and scope of work: The Upper Mississippi River is impaired for turbidity (fine sediments) from the confluence with the Minnesota River to Lake Pepin. Continued deposition of these Minnesota sourced suspended solids has resulted in a lack of aquatic vegetation, poor invertebrate production, and reduced abundance of fish and wildlife. Deep protected aquatic areas that would serve as habitat for bluegill and other species, including walleye and sauger, is lacking in both the backwaters and within large open water areas of upper Lake Pepin. -
Recurrence of Hexagenia Mayflies Demonstrates Improved Water Quality in Pool 2 and Lake Pepin, Upper Mississippi River
OpenRiver Cal Fremling Papers Cal Fremling Archive 1990 Recurrence of hexagenia mayflies demonstrates improved water quality in Pool 2 and Lake Pepin, Upper Mississippi River Cal R. Fremling Winona State University Follow this and additional works at: https://openriver.winona.edu/calfremlingpapers Recommended Citation Fremling, Cal R., "Recurrence of hexagenia mayflies demonstrates improved water quality in Pool 2 and Lake Pepin, Upper Mississippi River" (1990). Cal Fremling Papers. 35. https://openriver.winona.edu/calfremlingpapers/35 This Book is brought to you for free and open access by the Cal Fremling Archive at OpenRiver. It has been accepted for inclusion in Cal Fremling Papers by an authorized administrator of OpenRiver. For more information, please contact [email protected]. i\ ooj>. at RECURRENCE OF HEXAGENIA MAYFLIES DEMONSTRATES IMPROVED WATER QUALITY IN POOL 2 AND LAKE PEPIN, UPPER MISSISSIPPI RIVER Calvin R. Fremling1 and D. Kent Johnson2 1 Biology Department, Winona State University, Winona, Minnesota, 55987, USA 2Metropolitan Waste Control Commission, St. Paul, Minnesota, 55101, USA ABSTRACT Hexagenia mayflies are good indicators of general water quality because they have long life cycles and because their burrowing nymphs, which are unable to tolerate anaerobic conditions or swim long distances, live in sediments where toxins tend to accumulate. While chemical tests only describe water quality in terms of specific parameters and times, Hexagenia distribution indicates synergistic effects of many toxins, anoxia and other stresses throughout the year. Over 1,400 collections of imagoes and subimagoes along the Upper Mississippi River in 1957-1968,1976 showed that most of the 29 navigation pools supported large populations, as did impoundments upstream of Minneapolis-St.Paul. -
Geologic History of Minnesota Rivers
GEOLOGIC HISTORY OF MINNESOTA RIVERS Minnesota Geological Survey Ed ucational Series - 7 Minnesota Geological Survey Priscilla C. Grew, Director Educational Series 7 GEOLOGIC HISTORY OF MINNESOTA RIVERS by H.E. Wright, Jr. Regents' Professor of Geology, Ecology, and Botany (Emeritus), University of Minnesota 'r J: \ I' , U " 1. L I!"> t) J' T II I ~ !oo J', t ' I' " I \ . University of Minnesota St. Paul, 1990 Cover: An early ponrayal of St. Anthony Falls on the Mississippi River In Minneapolis. The engraving of a drawing by Captain E. Eastman of Fan Snelling was first published In 1853; It Is here reproduced from the Second Final Report of the Geological and Natural History Survey of Minnesota, 1888. Several other early views of Minnesota rivers reproduced In this volume are from David Dale Owen's Report of a Geological Survey of Wisconsin, Iowa, and Minnesota; and Incidentally of a portion of Nebraska Territory, which was published In 1852 by Lippincott, Grambo & Company of Philadelphia. ISSN 0544-3083 1 The University of Minnesota is committed to the policy that all persons shall have equal access to its programs, facilities, and employment without regard to race, religion, color, sex, national origin, handicap, age, veteran status, or sexual orientation. 1-' \ J. I,."l n 1 ~ r 1'11.1: I: I \ 1"" CONTENTS 1 .... INTRODUCTION 1. PREGLACIAL RIVERS 5 .... GLACIAL RIVERS 17 ... POSTGLACIAL RIVERS 19 . RIVER HISTORY AND FUTURE 20 . ... REFERENCES CITED iii GEOLOGIC HISTORY OF MINNESOTA RIVERS H.E. Wright, Jr. A GLANCE at a glacial map of the Great Lakes region (Fig. 1) reveals that all of Minnesota was glaciated at some time, and all but the southeastern and southwestern corners were covered by the last ice sheet, which culminated about 20,000 years ago. -
Town of Pepin Comprehensive Plan Page 1 of 73 General Characteristics
Town of Pepin Pepin County Wisconsin Comprehensive Plan Public Hearing: September 15, 2009 Plan Committee Members: Andrea Myklebust Alice Auth Jim Reeser Jim Sterry Carol Inderion Bruce Peterson Gary Samuelson Rob Meyer Mark Johnson Robert Bjerstedt Lou Seyffer Betty Bergmark Dennis Wolfe Table of Contents General Characteristics Page 2 History of Town of Pepin Page 3 General Planning Goals Page 6 Elements Section Issues and Opportunities Page 7 Transportation Page 13 Housing Page 17 Utilities and Community Facilities Page 22 Agricultural, Natural, Cultural Resources Agricultural Page 26 Natural Page 30 Cultural Page 34 Intergovernmental Cooperation Page 36 Economic Development Page 39 Land Use Page 45 Implementation Page 52 Appendix Appendix I Survey letter and form Page 59 Appendix II Maps Page 63 1. Bluffland & Slope Areas 2. Floodplain 3. Surface Waters/Wetlands 4. Groundwater Flow and Nitrates 5. Land Use Appendix III Cultural/Historic Sites Page 68 August 27, 2009 Town of Pepin Comprehensive Plan Page 1 of 73 General Characteristics The Town of Pepin is located in Pepin County in West Central Wisconsin. Lake Pepin, a wide part of the Mississippi River, forms a southern border. The Chippewa River borders the eastern boundary. To the north Frankfort Township of Pepin County and Maiden Rock Township of Pierce County are found on the map. Stockholm Township forms a western border. Pierce and Dunn County are located to the west and north and Buffalo County is located across the Chippewa River as our eastern neighbor. The land survey system designates the Town of Pepin at Townships 23 and 24 North, Ranges 14 and 15 West of the 4th Prime Meridian.