Physiographic Divisions of Illinois
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Upper Mississippi River Conservation Opportunity Area Wildlife Action Plan
Version 3 Summer 2012 UPPER MISSISSIPPI RIVER CONSERVATION OPPORTUNITY AREA WILDLIFE ACTION PLAN Daniel Moorehouse Mississippi River Pool 19 A cooperative, inter-agency partnership for the implementation of the Illinois Wildlife Action Plan in the Upper Mississippi River Conservation Opportunity Area Prepared by: Angella Moorehouse Illinois Nature Preserves Commission Elliot Brinkman Prairie Rivers Network We gratefully acknowledge the Grand Victoria Foundation's financial support for the preparation of this plan. Table of Contents List of Figures .............................................................................................................................. ii Acronym List .............................................................................................................................. iii I. Introduction to Conservation Opportunity Areas ....................................................................1 II. Upper Mississippi River COA ..................................................................................................3 COAs Embedded within Upper Mississippi River COA ..............................................................5 III. Plan Organization .................................................................................................................7 IV. Vision Statement ..................................................................................................................8 V. Climate Change .......................................................................................................................9 -
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. -
Pecatonica River: Targeting Conservation Practices in a Watershed to Improve Water Quality
Pecatonica River: Targeting conservation practices in a watershed to improve water quality Madison 151 Partners discuss new stream crossing on the Judd farm. © TNC Pleasant Valley Watershed One of the challenges facing landowners and managers in Wisconsin and nationwide is keeping sediment and phosphorus on the land and out of streams. Too much phosphorus leads to excessive algae growth, which consumes oxygen in the water and can contaminate The group tested this approach in the Pecatonica River drinking water. watershed in southwest Wisconsin, and the results are in. Farmers working with the project cut their estimated Since 2009, farmers and conservation groups in average phosphorus runoff and erosion almost in half, Wisconsin have worked together to test whether it is keeping an estimated average 4,400 pounds of phosphorus possible to target efforts to improve water quality to and 1,300 tons of sediment out of the water each year. have the greatest impact at the lowest possible cost. Just one year after fully implementing targeted changes The idea was to use science to target conservation to agricultural practices on approximately one third practices on those fields and pastures with the greatest of the crop and pasture acres in the watershed, water potential for contributing nutrients to streams. quality has improved. Launching a Pilot Project in Driftless Area Bypassed by the glaciers, the Driftless Area in southwest Wisconsin is characterized by steep- sided ridges and miles of rivers and smaller tributary streams that eventually drain into the Mississippi River. The pilot project took place in two sub-watersheds Changing crop rotations to increase cover on fields in winter gives the Kellers to the Pecatonica River: Pleasant Valley Branch another source of feed for some of their herd. -
Lake of the Ozarks Regional Housing Study Acknowledgments
LAKE OF THE OZARKS REGIONAL HOUSING STUDY ACKNOWLEDGMENTS The project team would like to acknowledge the contributions of the residents of the Lake Region, who gave their time, ideas, and exper- tise for the creation of this plan. It is only with their assistance and direction the plan gained the depth necessary to truly represent the spirit of the Lake Region and it is with their commitment that the plan will be implemented. We would also like to thank the partner organizations, Lake of the Ozarks Regional Economic Development Council who financially sup- ported this study and provided their leadership. A special thanks to everyone involved. Project Manager LOREDC BOARD Roger Corbin Tim Jacobsen Jeana Woods COMMITTEE Jacob Neusche Kim Willey Corey ten Bensel Linda Conner Brent Depeé Colleen Richey Debbie Hurr Russell Clay Jeff Hancock Cary Patterson Lori Hoelscher Vicki Devine Dennis Croxton Vicki Brown Kevin McRoberts Stan Schultz Roger Corbin CONSULTING TEAM RDG Planning & Design Omaha and Des Moines www.RDGUSA.com CHAPTER 1: INTRODUCTION 7 CHAPTER 2: PROFILE OF THE REGION 11 CHAPTER 3: CAMDEN COUNTY 49 CHAPTER 4: MORGAN COUNTY 79 CHAPTER 5: MILLER COUNTY 103 CHAPTER 6: LACLEDE COUNTY 127 CHAPTER 7: DEFINING HOUSING ISSUES / DIRECTIONS FORWARD 153 CHAPTER 1: Introduction 1 LAKE OF THE OZARKS REGIONAL HOUSING STUDY | Introduction INTRODUCTION The Lake of the Ozarks Regional Housing Study represents an in-depth study of the housing conditions of the three counties that constitute the Lake of the Ozarks Regional Economic Development Council (LOREDC). This includes the counties of Camden, Miller, and Morgan and the commercial centers of Camdenton, Eldon, Lake Ozark, Osage Beach, and Versailles. -
NATURAL RESOURCES (Updated Excerpt from Jo Daviess Comprehensive Plan Baseline Data)
ATTACHMENT F: NATURAL RESOURCES (Updated excerpt from Jo Daviess Comprehensive Plan Baseline Data) The natural resources in Jo Daviess County are unique relative to the rest of the state and much of the mid-west because the county is part of the Wisconsin Driftless Region bypassed by continental glaciers of the Ice Age. This region covers parts of southern Minnesota and Wisconsin, Northwestern Illinois and Northeastern Iowa. Glaciated areas were leveled, strewn with glacial debris or "drift" and dotted with lakes and ponds. The driftless areas, on the other hand, have bedrock close to the surface into which deep valleys have been carved by millions of years of weather and erosion. In Jo Daviess County, streams are numerous and the only two lakes are man-made. The relief from the higher ridges to the valley floors is typically 300 feet or more creating a rugged and scenic landscape. Ecosystems can be found in this landscape that are older than those found in glaciated areas. Geology The topography of Jo Daviess County is characterized by rugged relief unique to most of Illinois. Our county, located in the far northwestern corner of the state, is in an area spared by the major glaciations of the last two million years. It is, accordingly, called the "Driftless Area" by geologists, the term "drift" referring to material deposited by glacial activity. The visible landscape that we see today began during the Paleozoic Era (570 to 245 million years ago) when shallow seas repeatedly inundated the interior of the continent. Shells of marine animals, along with muds, silts and sands from eroding highlands, were periodically deposited in those sea bottoms. -
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. -
ST. CHARLES 7.5' QUADRANGLE Qslt 0 5 4 ST
90°22'30"W 90°30'00"W 90°27'30"W 90°25'00"W R 5 E R 6 E 38°52'30"N 38°52'30"N 31 32 33 34 35 36 31 35 SURFICIAL MATERIAL GEOLOGIC MAP OF THE ST. CHARLES 7.5' QUADRANGLE Qslt 0 5 4 ST. CHARLES AND ST. LOUIS COUNTIES, MISSOURI 0 45 Qslt 2 Geology and Digital Compilation by 0 45 Qtd David A. Gaunt and Bradley A. Mitchell Qcly «¬94 3 5 6 5 4 2011 Qslt Qtd Qtd Qtd 1 Graus «¬94 Lake OFM-11-593-GS 6 «¬H Qtd 6 Croche 9 10 MISSOURI DEPARTMENT OF NATURAL RESOURCES 8 7 s DIVISION OF GEOLOGY AND LAND SURVEY ai ar 7 M GEOLOGICAL SURVEY PROGRAM Qslt Qtd P.O. BOX 250, ROLLA MO 65402-0250 12 www.dnr.mo.gov/geology B «¬ Qslt 573-368-2100 7 13 THIS MAP WAS PRODUCED UNDER A COOPERATIVE 0 5 AGREEMENT WITH THE UNITED STATES GEOLOGICAL 4 18 38°50'00"N 38°50'00"N SURVEY Qtd Permission must be obtained to visit privately owned land Qslt Qslt PHYSIOGRAPHY 0 5 4 St. Charles County D St. Louis County The St. Charles quadrangle includes part of the large floodplain of the Missouri River and loess covered uplands. N 500 550 A L The floodplain is up to five miles wide in this area. The quadrangle lies within the Dissected Till Plains Section 50 S 5 I 45 6 0 0 0 of the Central Lowland Province of the Interior Plains Physiographic Division. -
Tunnel Hill 100 MILE RUN & 50 MILE RUN
Tunnel Hill 100 MILE RUN & 50 MILE RUN NOVEMBER 13, 2016 TUNNEL HILL STATE TRAIL Vienna, Illinois IN THE HEART OF JOHNSON COUNTY The citizens of Johnson County WOULD LIKE TO WELCOME YOU We encourage you to take advantage of all that Johnson County has to offer during your stay with us. Below is just a short list of attractions. Throughout this booklet you will find local restaurants, shops, and tourist destinations. We hope you enjoy your time and look forward to seeing you again! Shawnee National Forest 1-800-MY-WOODS Ferne Clyffe State Park South of Goreville, IL, (618) 995-2411 Paul Powell Home (Museum) Rt. 146 and Vine, Vienna, IL 62995 Vienna Depot Welcome Center Vienna City Park, Vienna, IL 62995, (618) 658-8547 Shawnee Hills Wine Trail (618) 967-4006, shawneewinetrail.com Cache River Wetlands Center THE JOHNSON COUNTY 8885 Rt. 37 S, Cypress, IL, (618) 657-2064 BOARD OF Johnson County’s Courthouse COMMISSIONERS and Carnegie Public Library ERNIE HENSHAW, PHIL STEWART Vienna, IL, both on the AND FRED MEYER National Registry of Historic Buildings Tunnel Hill 100/50 Mile Run - 2 SCHEDULE OF EVENTS FRIDAY NOVEMBER 12, 2016 Packet Pick up – 4 p.m. – 8 p.m. Pasta Dinner - 6 p.m. – 7:30 p.m. Vienna High School – 601 N 1st St, Vienna, IL 62995 SATURDAY NOVEMBER 13, 2016 Late packet pick up 6:30 – 7:30 a.m. Start – 100 mile and 50 mile 8:00 a.m. Finish – 100 & 50 mi. – Sun. Nov. 15 2 p.m. Vienna City Park – 298 E. -
Evaluation of Eastern Redcedar Infestations in the Northern Kansas Flint Hills Author(S): Clenton E
Society for Range Management Evaluation of Eastern Redcedar Infestations in the Northern Kansas Flint Hills Author(s): Clenton E. Owensby, Kenneth R. Blan, B. J. Eaton, O. G. Russ Reviewed work(s): Source: Journal of Range Management, Vol. 26, No. 4 (Jul., 1973), pp. 256-260 Published by: Allen Press and Society for Range Management Stable URL: http://www.jstor.org/stable/3896570 . Accessed: 20/12/2011 14:12 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Allen Press and Society for Range Management are collaborating with JSTOR to digitize, preserve and extend access to Journal of Range Management. http://www.jstor.org Arizona ranchers are enthusiastic about the potential ways and Public Works. 19(12):3-7. application of horizontal well drilling in remote and rough Root, A. W. 1955. Horizontal drill, Calif. Highways and Public Works. country. 34(3): 26-29. Stanton, T. E. 1948. Hydrauger method. Calif. Highways and Public LiteratureCited Works. 27(1):6-10). Tripp, Vollie. 1963. Not how deep but how long says this driller. Water Hellesoe, G. F. 1941. Los Gatos-Santa Cruz highway slipout. Calif. High- Well J. 17(5):21, 36-38. -
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. -
The 1951 Kansas - Missouri Floods
The 1951 Kansas - Missouri Floods ... Have We Forgotten? Introduction - This report was originally written as NWS Technical Attachment 81-11 in 1981, the thirtieth anniversary of this devastating flood. The co-authors of the original report were Robert Cox, Ernest Kary, Lee Larson, Billy Olsen, and Craig Warren, all hydrologists at the Missouri Basin River Forecast Center at that time. Although most of the original report remains accurate today, Robert Cox has updated portions of the report in light of occurrences over the past twenty years. Comparisons of the 1951 flood to the events of 1993 as well as many other parenthetic remarks are examples of these revisions. The Storms of 1951 - Fifty years ago, the stage was being set for one of the greatest natural disasters ever to hit the Midwest. May, June and July of 1951 saw record rainfalls over most of Kansas and Missouri, resulting in record flooding on the Kansas, Osage, Neosho, Verdigris and Missouri Rivers. Twenty-eight lives were lost and damage totaled nearly 1 billion dollars. (Please note that monetary damages mentioned in this report are in 1951 dollars, unless otherwise stated. 1951 dollars can be equated to 2001 dollars using a factor of 6.83. The total damage would be $6.4 billion today.) More than 150 communities were devastated by the floods including two state capitals, Topeka and Jefferson City, as well as both Kansas Cities. Most of Kansas and Missouri as well as large portions of Nebraska and Oklahoma had monthly precipitation totaling 200 percent of normal in May, 300 percent in June, and 400 percent in July of 1951. -
Ouachita Mountains Ecoregional Assessment December 2003
Ouachita Mountains Ecoregional Assessment December 2003 Ouachita Ecoregional Assessment Team Arkansas Field Office 601 North University Ave. Little Rock, AR 72205 Oklahoma Field Office 2727 East 21st Street Tulsa, OK 74114 Ouachita Mountains Ecoregional Assessment ii 12/2003 Table of Contents Ouachita Mountains Ecoregional Assessment............................................................................................................................i Table of Contents ........................................................................................................................................................................iii EXECUTIVE SUMMARY..............................................................................................................1 INTRODUCTION..........................................................................................................................3 BACKGROUND ...........................................................................................................................4 Ecoregional Boundary Delineation.............................................................................................................................................4 Geology..........................................................................................................................................................................................5 Soils................................................................................................................................................................................................6