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BIG STONE LAKE State Park Management Plan April 1984
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.) BIG STONE LAKE State Park Management Plan April 1984 d STATE OF ~~~~©u~ DEPARTMENT OF NATURAl RESOURCES BOX , CENTENNIAL OFFICE BUILDING • ST. PAUL, MINNESOTA • 55155 DNR INFORMATION (612} 296-6157 FILE NO. _____ April 13, 1984 Dear Concerned Citizens: A draft management plan for Big Stone Lake State Park has been completed by the Department of Natural Resources, Park Planning Section. This plan was prepared under the authority of the Outdoor Recreation Act of 1975. Copies of this draft management plan are available for review at the Ortonville Public Library, Graceville Public Library, Big Stone State Park Office, and the DNR Regional Office in New Ulm. Any comments you have on the plan should be made in writing and addressed to: Dennis Thompson or Carol Braun Park Planning Section Box lOE, Centennial Building .St. Paul, MN 55155 t e 1 e : ( 61 2) 2 9 6-0 5 01 The Outdoor Reacreation Act of 1975 provides for a 30 day review period in which comments may be made by the public. A public open house will be held at the Ortonville National Guard Armory on Thursday, May 3, 1984, come anytime between 1:00-4:30 and 6:00-9:00 p.m. During this open house the park planning staff will be available to answer questions and discuss the plan. -
By Stephen J. Lawrence Water-Resources Investigations
WATER-RESOURCES APPRAISAL OP THE LAKE TRAVERSE INDIAN RESERVATION IN SOUTH DAKOTA By Stephen J. Lawrence U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 88-4031 Huron, South Dakota 1989 DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., 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 Books and Open-File Reports Rm. 408, Federal Bldg. Federal Center, Bldg. 810 200 4th St. SW Box 25425 Huron, SD 57350 Denver, CO 80225-0425 CONTENTS Page Abstract ................................ 1 Introduction .............................. 1 Physiography ........................... 2 Climate .............................. 2 Geology .............................. 6 Surface water .............................. 6 Surface-water quantity ....................... 15 Streams ............................ 15 Lakes ............................. 21 Surface-water quality ....................... 21 Streams ............................ 21 Lakes ............................. 27 Ground water .............................. 31 Hydrogeology ............................ 32 Ground-water quality ........................ 35 Needed additional studies ........................ 38 Summary ................................. 40 Selected references ........................... 41 ILLUSTRATIONS Page Figure 1. Map showing the location of the Lake Traverse Indian Reservation in South Dakota ................. 3 2. Map showing physiographic -
Quarrernary GEOLOGY of MINNESOTA and PARTS of ADJACENT STATES
UNITED STATES DEPARTMENT OF THE INTERIOR Ray Lyman ,Wilbur, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director P~ofessional Paper 161 . QUArrERNARY GEOLOGY OF MINNESOTA AND PARTS OF ADJACENT STATES BY FRANK LEVERETT WITH CONTRIBUTIONS BY FREDERICK w. SARDE;30N Investigations made in cooperation with the MINNESOTA GEOLOGICAL SURVEY UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON: 1932 ·For sale by the Superintendent of Documents, Washington, D. C. CONTENTS Page Page Abstract ________________________________________ _ 1 Wisconsin red drift-Continued. Introduction _____________________________________ _ 1 Weak moraines, etc.-Continued. Scope of field work ____________________________ _ 1 Beroun moraine _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 47 Earlier reports ________________________________ _ .2 Location__________ _ __ ____ _ _ __ ___ ______ 47 Glacial gathering grounds and ice lobes _________ _ 3 Topography___________________________ 47 Outline of the Pleistocene series of glacial deposits_ 3 Constitution of the drift in relation to rock The oldest or Nebraskan drift ______________ _ 5 outcrops____________________________ 48 Aftonian soil and Nebraskan gumbotiL ______ _ 5 Striae _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 48 Kansan drift _____________________________ _ 5 Ground moraine inside of Beroun moraine_ 48 Yarmouth beds and Kansan gumbotiL ______ _ 5 Mille Lacs morainic system_____________________ 48 Pre-Illinoian loess (Loveland loess) __________ _ 6 Location__________________________________ -
Early History of Lake Agassiz in Southeast North Dakota
JOHN P. BLUEMLE North Dakota Geological Survey, University Station, Grand Forks, North Dakota 58201 Early History of Lake Agassiz in Southeast North Dakota Extensive accumulations of collapsed lake and shore sediment are present above the Herman level adjacent to the Agassiz lake plain in southeast North Dakota. The presence of these deposits indicates that ice-dammed lakes existed on top of stagnant glacial ice while Lake Agassiz was develop- ing. Lake Agassiz did not simply expand northward from its southern end; but rather, when the superglacial lakes coalesced, the resulting Lake Agassiz flooded areas along much of the length of the Herman Beach. INTRODUCTION The Herman Beach has long been considered to mark the earliest and uppermost level reached by glacial Lake Agassiz. Even though lake deposits at elevations slightly above Herman level have been described in association with Lake Agassiz, these have always been attributed to small, short-lived lakes. Upham (1895) Figure 1. Location map showing the Agassiz and Dakota lake plains (stippled areas), and the area (diagonally ruled) of high strandlines in southeast North Dakota. The high-level lakes drained through the spillway to glacial found evidence for pre-Herman strandlines Lake Dakota while at the Norma and Cuba strands, through Lake Traverse and Big Stone Lake to the glacial River in southeast North Dakota at elevations Warren (now the Minnesota River valley) while at the Fingal and Alice strands. The outlined area is shown on Fig- about 20 ft above the Herman level. He ures 3,4, and 5. reported evidence for the narrow Lake Milnor, the deposits of which cover about commonly bouldery as a result of having associated beach deposits. -
The Traverse County Comprehensive Local Water Plan
TRAVERSE COUNTY WATER PLAN UPDATE January 1, 2005- December 31, 2014 Prepared by: Sara Gronfeld, Traverse County Water Plan Coordinator Assistance Provided by the Bois de Sioux Watershed District and Other Local and Regional Agencies TABLE OF CONTENTS ____Page Number Local Water Management Council..........................................3 Traverse County Commissioners...........................................3 A. Executive Summary ............................................................4 Introduction............................................................4 Purpose ..................................................................4 Summary of Goals and Actions .........................................4 Description of Priority Concerns .......................................5 Erosion ...................................................................4 Flood Damage........................................................5 Contaminated Runoff............................................5 Groundwater Contamination................................6 Consistency with Other Plans..............................6 Recommendations to Other Plans & Controls....7 B. Priority Concerns Assessment of Priority Concerns................................ 9-20 Assessment of Erosion.......................................10 Assessment of Flood Damage ...........................13 Assessment of Contaminated Runoff................16 Assessment of Groundwater Contamination....18 C. Goals, Objectives, and Action items ........................ 21-27 Action Items, -
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. -
Bottom Sediments and Organic Geochemical Residues of Some Minnesota Lakes
MINNESOTA GEOLOGICAL SURVEY PRISCILLA C. GREW, Director BOTTOM SEDIMENTS AND ORGANIC GEOCHEMICAL RESIDUES OF SOME MINNESOTA LAKES EM. Swain Report of Investigations 41 ISSN 0076-9177 UNIVERSITY OF MINNESOTA Saint Paul - 1992 BOTTOM SEDIMENTS AND ORGANIC GEOCHEMICAL RESIDUES OF SOME MINNESOTA LAKES 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, color, creed, religion, national origin, sex, age, marital status, disability, public assistance status, veteran status, or sexual orientation. TABLE OF CONTENTS Page Foreword ........................................................................................ v Preface ........................................................................................... v Acknowledgments ............................... , ............................................. , v Abstract .......................................................................................... 1 Introduction .......................................... , .......................................... 2 Facies of Lake Sediments ...................................................................... 2 Clay Minerals .................................................................................. 42 Fossils ......................................................................................... 44 Carbohydrates ................................................................................. 44 Protein Amino Acids ........................................................................ -
Roads and the Settlement of Minnesota
MINNESOTA HISTORY VOLUME 21 SEPTEMBER, 1940 NUMBER 3 ROADS A N D THE SETTLEMENT OF MINNESOTA IN THE STORY of settlement in America, the difficulty of travel in newly opened areas is a constantly recurring theme. As soon as the settlers of America moved inland from the coastal waters, their troubles began, for there were few roads, and it was no easy task to build them. Yet, the growth of the American nation hinged upon roads, for, un- til they were built and communication was improved, settle- ment was retarded. The problem of road building had to be faced anew by each generation of pioneers on the west- ward march, and by the time Minnesota was reached, the nation had almost a hundred and fifty years of experience in pioneering and road making. At the time of the organization of Minnesota Territory in 1849, there were fewer than five thousand white persons living in the whole area. Less than a decade later — in 1858 — the territory became a state with an estimated popu- lation of more than a hundred and fifty thousand. Each decade thereafter showed an astounding increase in popula- tion until, at the close of the nineteenth century, when the frontier had all but vanished, the state had a population of more than a million and three-quarters. In 1849, the popu- lation centers of Minnesota were at St. Paul, St. Anthony, and Stillwater. Together they had fewer than two thousand inhabitants, but that was more than forty per cent of the people then living in Minnesota. In 1860 the same com- munities had a combined population of well over eighteen thousand — only about ten per cent of the total state popu- 225 226 ARTHUR J. -
MAP -FPJN9NTA== South Dakota Wetland Inventory U.S. Fish And
South Dakota Wetland Inventory U.S . Fish and Wildlife Service 1:100,000 Map Narrative Report Milbank NE Pr-e- F)11~- (-C- +" 0 N-j MAP -FPJN9NTA== Contractor for this wetland inventory was the South Dakota Cooperative Fish and Wildlife Researt~ Unit, P .O . Box 2206, South Dakota State University, Brookirxgs, SD 57007 . Photointerpreters. were Howard Browers and Ross Blank-Libra . Preparation of this narrative report was ccupleted by Howard Browers . Regional Wetland Coordinator was Charles Elliott, U .S . Fish and Wildlife Service, Denver Federal Center, P.O. Box 25486, Denver, 00 80225 . Wetland delineation and classification for Milbank NE 1:100,000 quadrangle was done on 1 : 58, 000 color infrared aerial photographs taken in April and October 1984 . Photography covered 100% of the quadrangle . Classification of wetlands was done according to Cowardin et al . (1979) . National Wetlarxi Inventory Mapping Conventions were also used to assist in phatointerpretation. Field checking for the quadrangle was done on 4 and 5 April and 26 June 1988 . SPECIAL NAPPING PROBIEM Interpretation of this 1 :100,000 was originally to be done on NASA 1 :65,000 CIR. However, most (approximately 75%) of the NASA photos were taken in spring 1982 and exhibited depressed wetland conditions . The remaining 25% of the NASA was taken in spring 1979 and had nuch better wetland corx1itions . The NHAP used to replace the NASA was taken in spring and fall 1984 and generally had better wetland conditions. Both dates of NASA photos were used as collateral data while interpreting the NHAP . By using these photos as collateral data we were able to enhance the quality of the NHAP. -
Section 5.0 Detailed Analysis of Little Minnesota River Floodway and Toelle Coulee Flood Mitigation Alternatives
SECTION 5.0 DETAILED ANALYSIS OF LITTLE MINNESOTA RIVER FLOODWAY AND TOELLE COULEE FLOOD MITIGATION ALTERNATIVES 5.1 LITTLE MINNESOTA AND TOELLE COULEE ALTERNATIVES Based upon the information presented within Section 4.0, Range of Flood Mitigation Alternatives Considered, discussions with the BVFMTF, and consultation with the UMRWD, the range of Little Minnesota River flood mitigation alternatives became reduced to: 1) a Little Minnesota River floodway; and, 2) storage, a floodway, a levee or some combination thereof for Toelle Coulee. This section provides descriptions, detailed information on the engineering design, and an assessment of hydraulic performance for each of the flood mitigation alternatives selected for evaluation. Section 7 provides the rationale for selection of the preferred floodway alternatives for the Little Minnesota River and the design for Toelle Coulee. 5.1.1 Little Minnesota River Floodway Alternatives Six different alignments and two inlet types (i.e., gate-controlled or “active” and fixed crest or “passive”) for a total of twelve different floodway alternatives were considered for the Little Minnesota River to provide flood protection for the City of Browns Valley. Floodway Option 3 was added by Houston Engineering, Inc. subsequent to the November 1, 2007 BVFMTF meeting. Option 3 is intended to better address potential concerns relative to maintaining the historic proportion of flow to Lake Traverse and concerns about modifying low flows through the City of Browns Valley. All floodway designs focused on containing the design discharge (plus 1-foot of freeboard) within the floodway channel, rather than using levees to provide additional capacity. Material from floodway construction will be placed in spoil banks adjacent to the floodway and used to reconstruct Roberts CR 24. -
Map of Minnesota River State Water Trail from Ortonville to Highway 40
Route Description, Minnesota River - RM 318 to 278 Route Description, Pomme de Terre River R and L represent sides of the river facing downstream. R and L represent sides of the river facing downstream 30.0 County Road 7 bridge. 318-304 Numerous log jams and snags exist in this 27.5 (L) Koosman carry-in launch. County Road 20 bridge. 24.6 185th Avenue bridge. area. 23.0 County Road 56 bridge. 317.9 Minnesota River enters from Big Stone 19.7 190th Avenue bridge. Lake. City of Ortonville. 19.1 (L) Pomme de Terre #1 carry-in access. Rest area and watercraft campsite. US Highway 12 bridge. 317.9 (L) Big Stone #8 trailer access and fishing pier. 16.6 (R) Confluence with Long Lake Creek. 317.7 Dam and railroad bridge. No portage. 14.8 (L) Larson carry-in access. County Road 36 bridge. 317.6 Ortonville Dam. No portage. Shorefishing 13.5 US Highway 59 bridge. site. 9.1 Hening Street bridge. City of Appleton. 8.9 (L) Veum Avenue bridge. 317.5 US Highway 12 bridge. Powerline crossing. 8.8 Appleton carry-in access and shorefishing. Munsterman Street/Highway 119 bridge. 316.8 Pedestrian bridge. 8.7 Railroad bridge. 316.8-303.4 Big Stone National Wildlife Refuge. 8.0 Railroad bridge. 5.0 County Road 51 bridge. 316.0 Powerline crossing. 2.3 County Road 51 bridge. 312.5 Bridge. 0.1 (R) Marsh Lake carry-in access. 307.9 (L) Confluence with Stony Run. 0-4 Lac qui Parle Wildlife Management Area. 0 to 10 CAUTION - numerous rapids an log jams in this area. -
Upper Minnesota River Watershed Five Year Strategic Plan
UPPER MINNESOTA RIVER WATERSHED FIVE YEAR STRATEGIC PLAN In Cooperation With: East Dakota Water Development District South Dakota Conservation Districts South Dakota Association of Conservation Districts South Dakota Department of Environment and Natural Resources USDA Natural Resources Conservation Service Date: August 2012 Prepared by: TABLE OF CONTENTS Executive Summary ...........................................................................................................6 Introduction ........................................................................................................................8 1.1 Project Background and Scope ........................................................................8 1.2 Upper Minnesota River Watershed History ...................................................10 1.3 Upper Minnesota River Watershed Water Quality Studies ..........................13 1.4 Goals of the Upper Minnesota River Basin Project .......................................15 2.0 Causes and Sources of Impairment .......................................................................15 2.0.1 Geography, Soils, and Land Use....................................................................15 2.0.2 Water Bodies Studies and Current Status .....................................................24 2.1.0 Description of the Impairments for 303(d) Water Body Listings in the Upper Minnesota River Basin ............................................................29 2.1.1 Temperature ...................................................................................................29