Pecatonica River Rapid Watershed Assessment Document
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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. -
Scenic and Historic Illinois
917.73 BBls SCENIC AND== HISTORIC ILLINOIS With Abraham lincoln Sites and Monuments Black Hawk War Sites ! MADISON. WISCONSIN 5 1928 T»- ¥>it-. .5^.., WHm AUNOIS HISTORICAL SIISYIT 5 )cenic and Historic Illinois uic le to One TKousand Features of Scenic, Historic I and Curious Interest in Illinois w^itn ADraKam Lincoln Sites and Monuments Black Hawk War Sites Arranged by Cities and Villages CHARLES E. BROWN AutKor, Scenic and Historic Wisconsin Editor, TKe Wisconsin ArcKeologist The MusKroom Book First Edition Published by C. E. BROWN 201 1 CKadbourne Avenue Madison, Wisconsin Copyrighted, 1928 t' FOREWORD This booklet is issued with the expectation that prove of ready reference service to those who motor in Illinois. Detailed information of the Ian monuments, etc. listed may be obtained from th' cations of the Illinois Department of Conse Illinois State Historical Society, State Geological Chicago Association of Commerce, Chicago H. Society, Springfield Chamber of Commerce, an local sources. Tourists and other visitors are requested to re that all of the landmarks and monuments mentior many others not included in this publication, are lie heritage and under the protection of the state the citizens of the localities in which they occ the Indian mounds some are permanently pr' The preservation of others is encouraged. Tl ploration, when desirable, should be undertaken ganizations and institutions interested in and i equipped for such investigations. Too great a the States' archaeological history and to educat already resulted from the digging* in such an Indian landmarks by relic hunters. The mutile scenic and historic monuments all persons shoul in preventing. -
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. -
Illinois Snowmobile Trails
Connects To Wisconsin Trails East g g Dubuque g Warren L E G E N D 26 Richmond 173 78 Durand E State Grant Assisted Snowmobile Trails N Harvard O Galena O on private lands, open to the public. For B ILLINOIS’ SELF-FUNDED 75 E K detailed information on these trails, contact: A 173 L n 20 Capron n Illinois Association of Snowmobile Clubs, Inc. n P.O. Box 265 • Marseilles, IL 61341-0265 N O O P G e A McHenry Gurnee S c er B (815) 795-2021 • Fax (815) 795-6507 TRAIL SYSTEM Stockton N at iv E E onica R N H N Y e-mail: [email protected] P I R i i E W Woodstock N i T E S H website: www.ilsnowmobile.com C Freeport 20 M S S The State of Illinois has adopted, by legislative E Rockford Illinois Department of Natural Resources I 84 l V l A l D r Snowmobile Trails open to the public. e Belvidere JO v action, a system of funding whereby snowmobilers i R 90 k i i c Algonquin i themselves pay for the network of trails that criss-cross Ro 72 the northern 1/3 of the state. Monies are generated by Savanna Forreston Genoa 72 Illinois Department of Natural Resources 72 Snowmobile Trail Sites. See other side for detailed L L information on these trails. An advance call to the site 64 O Monroe snowmobile registration fees. These funds are administered by R 26 R E A L is recommended for trail conditions and suitability for C G O Center Elgin b b the Department of Natural Resources in cooperation with the snowmobile use. -
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. -
The Driftless Area – a Physiographic Setting (Dale K
A Look Back at Driftless Area Science to Plan for Resiliency in an Uncertain Future th Special Publication of the 11 Annual Driftless Area Symposium 1 A Look Back at Driftless Area Science to Plan for Resiliency in an Uncertain Future Special Publication of the 11th Annual Driftless Area Symposium Radisson Hotel, La Crosse, Wisconsin February 5th-6th, 2019 Table of Contents: Preface: A Look Back at Driftless Area Science to Plan for Resiliency in an Uncertain Future (Daniel C. Dauwalter, Jeff Hastings, Marty Melchior, and J. “Duke” Welter) ........................................... 1 The Driftless Area – A Physiographic Setting (Dale K. Splinter) .......................................................... 5 Driftless Area Land Cover and Land Use (Bruce Vondracek)................................................................ 8 Hydrology of the Driftless Area (Kenneth W. Potter) ........................................................................... 15 Geology and Geomorphology of the Driftless Area (Marty Melchior) .............................................. 20 Stream Habitat Needs for Brown Trout and Brook Trout in the Driftless Area (Douglas J. Dieterman and Matthew G. Mitro) ............................................................................................................ 29 Non-Game Species and Their Habitat Needs in the Driftless Area (Jeff Hastings and Bob Hay) .... 45 Climate Change, Recent Floods, and an Uncertain Future (Daniel C. Dauwalter and Matthew G. Mitro) ......................................................................................................................................................... -
EAST SIDE REVITALIZATION Reducing the Impacts of Flooding and Floodway Regulations Freeport, IL
DECEMBER 2013 EAST SIDE REVITALIZATION Reducing the Impacts of Flooding and Floodway Regulations Freeport, IL INTRODUCTION HOW DO FLOODING AND FLOODWAY REGULATIONS EPA’s Superfund Redevelopment Initiative (SRI) IMPACT THE EAST SIDE? and EPA Region 5 sponsored a reuse planning process for the CMC Heartland Site and other The East Side is an African-American neighborhood located in the floodway of the Pecatonica River. Residents of the East Side share a strong sense of community and contaminated properties in the East Side deep affection for the neighborhood. Many families have lived in the neighborhood neighborhood of Freeport, Illinois. The project for generations. Long-time residents remember a time when the neighborhood connects site reuse with area-wide neighborhood supported quality housing and thriving businesses with neighborhood-oriented revitalization for this environmental justice amenities. community. This report summarizes outcomes The neighborhood’s economic vitality and housing quality have been impacted from a 12-month community planning process, negatively over time by the neighborhood’s location in the floodway. Residents including considerations for reducing the impacts contend with recurring major and minor flood events, and are subject to Federal of flooding and floodway regulations on the East Emergency Management Agency (FEMA) and State of Illinois floodway regulations, Side Neighborhood. which limit improvements on structures located in a floodway. These regulations, which were not in place when the neighborhood was built, make it challenging to COMMUNITY GOALS improve and expand both housing and neighborhood businesses. Over time, housing Neighborhood stakeholders identified two quality has severely declined and most commercial businesses have vacated the neighborhood. -
Unsuuseuracsbe
PLATTVILLE Pacific Hastings Red Agency Junction Malvern Emerson Chariton GARFIELD FRANKFORT CEDAR WAYNE GUILFORD TROY Albia MANTUA EIGHT MILE Oak RED POLK Ottumwa GLENWOOD CENTER SILVER INDIAN CREEK GROVE PLATTSMOUTH CREEK OAK CENTER D LINCOLN e AGENCY Plattsmouth s Melrose M Russell o in e MILLS Stanton Blakesburg s R MONTGOMERY ADAMS LUCAS MONROE iver WEST ROCK LYONS UNION CLARKE BLUFF WHITE DEER CREEK EAST WAPELLO WEST GRANT SCOTT Kent FRANKLIN MONROE URBANA RAWLES CLOUD NODAWAY JASPER MERCER Arispe BENTON WASHINGTON JACKSON Murray GRANT PLATTE GRANT PLEASANT DOYLE KNOX GREEN BAY FRANKLIN UNION WARREN MOUNT PLEASANT Villisca Nodaway SAND CREEK Derby ADAMS GREEN KEOKUK Coburg EAST ROCK Shannon City CASS BLUFF Tabor 109th Congress of the United States Moravia Randolph Weldon N Imogene Weeping Water Lenox E Le Roy CHARITON UNION Floris TAYLOR I RIVERSIDE MONROE TINGLEY Van Wert SOAP CREEK SALT NEHAWKA B GREEN PIERCE FREMONT DOUGLAS UNION MARION O NODAWAY INDEPENDENCE LICK CREEK CREEK SCOTT HOLT GROVE PLATTE LINCOLN JEFFERSON FRANKLIN GARDEN GROVE WRIGHT Rathbun Reservoir R UNION RICHLAND LONG CREEK Nehawka W Hepburn Tingley Humeston WASHINGTON Millerton LIBERTY A Union Thurman Essex Ellston RICHMAN AVOCA A Garden Grove Unionville S Grand River WALNUT Avoca K Rathbun DOUGLAS UDELL Drakesville A FREMONT Clearfield Diagonal Beaconsfield WALNUT Sharpsburg PERRY FOX RIVER DRAKESVILLE PRAIRIE Mystic Udell UNION GRANT TARKIO NEBRASKA WASHINGTON NODAWAY DALLAS MARSHALL GRANT CENTER BENTON CORYDON SOUTH FORK JOHNS GRANT WASHINGTON LIBERTY MONROE -
Surficial Geology Map for the Freeport East 7.5 Minute Quadrangle, Stephenson County, Illinois
Surficial Geology Map for the Freeport East 7.5 Minute Quadrangle, Stephenson County, Illinois Surficial Geology Map for the Freeport East 2013 7.5 Minute Quadrangle, Stephenson County, Illinois Cheyenne Morgan, Eric Peterson, Robert Nelson, 89 94 Qg 0 Qpr 0 0 Og Qg 0 0 94 9 Kathryn Schroeder, Dave Malone 8 7 Og 0 Qg Og 9 0 00 Qpr 4 Qg Qg Qpr Department of Geology-Geography, Illinois State University 8 Qpr 0 5 Qc Qpr 9 93 2013 940 0 92 Qg 0 Qg Qg 0 Quaternary System Qpr 2 9 950 9 2 Qg 890 0 Qpr89 0 0 Og 4 94 Og Qpr 9 0 8 Qg 3 9 0 Og Floodplain 4 910 0 95Og0 930 Qg 9 Qpr 2 950 0 Alluvium Qg 9 0 96 4 1 9 Qpr Qpr Not much is known of the large-scale geology of Stephenson County. Though numerous wells 0 0 9 30 Qg 950 9 9 have been drilled within the Freeport East Quadrangle, the geologic data provided from these wells 6 20 930 Og 0 Floodplain have not been collected, organized, and analyzed. The principal focus of this project will be to Og Qg Qg 9 Og 0 create a surficial geologic map of the Quaternary and overlying units within the region. The 2 92 930 0 8 Alluvium 8 80 surficial geology map is needed to understand the local geology and will assist in future geologic 8 Qpr Qpr Qg 0 Og 0 91 and hydrogeologic investigations within the Freeport area. Due to the composition of the partially 0 Qc Qpr 7 8 9 6 3 8 0 0 Cahokia Alluvium buried bedrock valley and the current downcutting of the Pecatonica into the surrounding geology 91 0 0 92 0 3 Qpr there is a need to assess both shallow and deep aquifer sensitivity within the region. -
Rock River Basin: Historical Background, Iepa Targeted Watersheds, and Resource-Rich Areas
ROCK RIVER BASIN: HISTORICAL BACKGROUND, IEPA TARGETED WATERSHEDS, AND RESOURCE-RICH AREAS by Robert A. Sinclair Office of Surface Water Resources: Systems, Information & GIS Illinois State Water Survey Hydrology Division Champaign, Illinois A Division of the Illinois Department of Natural Resources April 1996 CONTENTS Page Introduction 1 Acknowledgments 1 Historical Perspective of the Basin 3 Basin Physiography and Geology 3 Land Use 5 Basin Soils 5 Streams in the Basin 5 Streamflow and Sediment Quality 8 Streamflow 8 Sediment Quality 8 Surface Water Quality 13 IEPA Stream Assessment Criteria 13 IEPA Surface Water Quality Assessment 14 Ground-Water Resources and Quality 16 Ground-Water Resources 16 Ground-Water Quality 17 IEPA Targeted Watershed Approach 19 Major Watershed Areas 19 Criteria for Selecting Targeted Watersheds 19 TWA Program Activities 19 TWA for the Rock River Basin 20 References 23 INTRODUCTION Conservation 2000, a program to improve natural ecosystems, visualizes resource-rich areas, and promotes ecosystem projects and development of procedures to integrate economic and recreational development with natural resource stewardship. The Rock River basin is one of the areas identified for such projects. This report briefly characterizes the water resources of the basin and provides other relevant information. The Rock River originates in the Horicon Marsh in Dodge County, Wisconsin, and flows in a generally southerly direction until it enters Illinois just south of Beloit. Then it flows in a southwesterly direction until it joins the Mississippi River at Rock Island. The river flows for about 163 miles in Illinois, and its total length from head to mouth is about 318 miles.