Western Lake Erie Basin Collaborative Agreement
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Indiana Glaciers.PM6
How the Ice Age Shaped Indiana Jerry Wilson Published by Wilstar Media, www.wilstar.com Indianapolis, Indiana 1 Previiously published as The Topography of Indiana: Ice Age Legacy, © 1988 by Jerry Wilson. Second Edition Copyright © 2008 by Jerry Wilson ALL RIGHTS RESERVED 2 For Aaron and Shana and In Memory of Donna 3 Introduction During the time that I have been a science teacher I have tried to enlist in my students the desire to understand and the ability to reason. Logical reasoning is the surest way to overcome the unknown. The best aid to reasoning effectively is having the knowledge and an understanding of the things that have previ- ously been determined or discovered by others. Having an understanding of the reasons things are the way they are and how they got that way can help an individual to utilize his or her resources more effectively. I want my students to realize that changes that have taken place on the earth in the past have had an effect on them. Why are some towns in Indiana subject to flooding, whereas others are not? Why are cemeteries built on old beach fronts in Northwest Indiana? Why would it be easier to dig a basement in Valparaiso than in Bloomington? These things are a direct result of the glaciers that advanced southward over Indiana during the last Ice Age. The history of the land upon which we live is fascinating. Why are there large granite boulders nested in some of the fields of northern Indiana since Indiana has no granite bedrock? They are known as glacial erratics, or dropstones, and were formed in Canada or the upper Midwest hundreds of millions of years ago. -
Biological and Water Quality Study of the Blanchard River Putnam, Hancock, Seneca, Allen, Wyandot, and Hardin Counties, OH
State of Ohio Environmental Protection Agency Division of Surface Water Biological and Water Quality Study of the Blanchard River Putnam, Hancock, Seneca, Allen, Wyandot, and Hardin Counties, OH June 28, 2007 Ted Strickland, Governor Chris Korleski, Director EAS/2007-6-2 2005 Blanchard River Basin TSD June 28, 2007 Biological and Water Quality Study of the Blanchard River and Selected Tributaries 2005 Putnam, Hancock, Seneca, Allen, Wyandot, and Hardin Counties, OH June 28, 2007 OEPA Technical Report EAS/2007-6-2 Prepared by State of Ohio Environmental Protection Agency Division of Surface Water Lazarus Government Center 50 West Town Street, Columbus OH 43215 Mail to: P.O. Box 1049, Columbus OH 43216-1049 Ted Strickland, Governor, State of Ohio Chris Korleski Director, Ohio Environmental Protection Agency EAS/2007-6-2 2005 Blanchard River Basin TSD June 28, 2007 TABLE OF CONTENTS NOTICE TO USERS ........................................................................................................ i ACKNOWLEDGMENTS..................................................................................................iii FOREWORD...................................................................................................................iv MECHANISMS FOR WATER QUALITY IMPAIRMENT..................................................ix INTRODUCTION............................................................................................................. 1 SUMMARY..................................................................................................................... -
Moving Forward with Lake Erie's Impairment Designation
Moving Forward with Lake Erie’s Impairment Designation Since 2002, the Section 303(d) list of impaired waters in Ohio EPA’s biannual report to U.S. EPA (Integrated Report) has Policy Recommendations -Western Lake Erie Basin Impairment included many of the watersheds draining to the western basin. The agency’s past integrated reports have also listed the shore- line waters of the Lake Erie western basin and Lake Erie islands as well as the waters near the Toledo and Oregon municipal • To meet requirements under the Clean Water Act, TMACOG recommends that the U.S. EPA work collaboratively with the water intakes as impaired for all four beneficial uses (including for public drinking water due to harmful algal blooms). designated agencies of WLEB states – Ohio EPA, Michigan DEQ, and Indiana Office of Water Quality – to evaluate water However, an impairment designation for Ohio’s open waters of Lake Erie was withheld until 2018, when the Ohio EPA changed quality targets for open waters and set monitoring and assessment protocols that can be used to continue to evaluate the course and included the western basin’s open waters on the state’s 303(d) list of impaired waterbodies in the 2018 Integrated status for the four beneficial uses in the open waters of Lake Erie’s western basin. Report. This new impairment designation for the open waters adds recreational use impairment due to large algal blooms. In 2016, Michigan DEQ assigned an impaired designation to Michigan waters of Lake Erie due to algal blooms caused by excessive • If U.S. -
Biological and Water Quality Study of the Ashtabula River and Select Tributaries, 2011
Biological and Water Quality Study of the Ashtabula River and Select Tributaries, 2011 Ashtabula County Ashtabula River at Benetka Road (RM 19.03) OHIO EPA Technical Report EAS/2014-01-01 Division of Surface Water December 19, 2014 EAS/2014-01-01 Ashtabula River and Select Tributaries TSD December 19, 2014 Biological and Water Quality Survey of the Ashtabula River and Select Tributaries 2011 Ashtabula County December 19, 2014 Ohio EPA Technical Report EAS/2014-01-01 Prepared by: Ohio Environmental Protection Agency Division of Surface Water Lazarus Government Center 50 West Town Street, Suite 700 Columbus, Ohio 43215 Ohio Environmental Protection Agency Ecological Assessment Section 4675 Homer Ohio Lane Groveport, Ohio 43125 and Ohio Environmental Protection Agency Northeast District Office 2110 East Aurora Road Twinsburg, Ohio 44087 Mail to: P.O. Box 1049, Columbus, Ohio 43216-1049 John R. Kasich, Governor, State of Ohio Craig W. Butler, Director, Ohio Environmental Protection Agency i EAS/2014-01-01 Ashtabula River and Select Tributaries TSD December 19, 2014 TABLE OF CONTENTS EXECUTIVE SUMMARY ............................................................................................................ 1 INTRODUCTION ...................................................................................................................... 12 STUDY AREA ........................................................................................................................... 13 RECOMMENDATIONS ............................................................................................................ -
2000 Lake Erie Lamp
Lake Erie LaMP 2000 L A K E E R I E L a M P 2 0 0 0 Preface One of the most significant environmental agreements in the history of the Great Lakes took place with the signing of the Great Lakes Water Quality Agreement of 1978 (GLWQA), between the United States and Canada. This historic agreement committed the U.S. and Canada (the Parties) to address the water quality issues of the Great Lakes in a coordinated, joint fashion. The purpose of the GLWQA is to “restore and maintain the chemical, physical, and biological integrity of the waters of the Great Lakes Basin Ecosystem.” In the revised GLWQA of 1978, as amended by Protocol signed November 18, 1987, the Parties agreed to develop and implement, in consultation with State and Provincial Governments, Lakewide Management Plans (LaMPs) for lake waters and Remedial Action Plans (RAPs) for Areas of Concern (AOCs). The LaMPs are intended to identify critical pollutants that impair beneficial uses and to develop strategies, recommendations and policy options to restore these beneficial uses. Moreover, the Specific Objectives Supplement to Annex 1 of the GLWQA requires the development of ecosystem objectives for the lakes as the state of knowledge permits. Annex 2 further indicates that the RAPs and LaMPS “shall embody a systematic and comprehensive ecosystem approach to restoring and protecting beneficial uses...they are to serve as an important step toward virtual elimination of persistent toxic substances...” The Great Lakes Water Quality Agreement specifies that the LaMPs are to be completed in four stages. These stages are: 1) when problem definition has been completed; 2) when the schedule of load reductions has been determined; 3) when P r e f a c e remedial measures are selected; and 4) when monitoring indicates that the contribution of i the critical pollutants to impairment of beneficial uses has been eliminated. -
Geomorphic and Sedimentological History of the Central Lake Agassiz Basin
Electronic Capture, 2008 The PDF file from which this document was printed was generated by scanning an original copy of the publication. Because the capture method used was 'Searchable Image (Exact)', it was not possible to proofread the resulting file to remove errors resulting from the capture process. Users should therefore verify critical information in an original copy of the publication. Recommended citation: J.T. Teller, L.H. Thorleifson, G. Matile and W.C. Brisbin, 1996. Sedimentology, Geomorphology and History of the Central Lake Agassiz Basin Field Trip Guidebook B2; Geological Association of CanadalMineralogical Association of Canada Annual Meeting, Winnipeg, Manitoba, May 27-29, 1996. © 1996: This book, orportions ofit, may not be reproduced in any form without written permission ofthe Geological Association ofCanada, Winnipeg Section. Additional copies can be purchased from the Geological Association of Canada, Winnipeg Section. Details are given on the back cover. SEDIMENTOLOGY, GEOMORPHOLOGY, AND HISTORY OF THE CENTRAL LAKE AGASSIZ BASIN TABLE OF CONTENTS The Winnipeg Area 1 General Introduction to Lake Agassiz 4 DAY 1: Winnipeg to Delta Marsh Field Station 6 STOP 1: Delta Marsh Field Station. ...................... .. 10 DAY2: Delta Marsh Field Station to Brandon to Bruxelles, Return En Route to Next Stop 14 STOP 2: Campbell Beach Ridge at Arden 14 En Route to Next Stop 18 STOP 3: Distal Sediments of Assiniboine Fan-Delta 18 En Route to Next Stop 19 STOP 4: Flood Gravels at Head of Assiniboine Fan-Delta 24 En Route to Next Stop 24 STOP 5: Stott Buffalo Jump and Assiniboine Spillway - LUNCH 28 En Route to Next Stop 28 STOP 6: Spruce Woods 29 En Route to Next Stop 31 STOP 7: Bruxelles Glaciotectonic Cut 34 STOP 8: Pembina Spillway View 34 DAY 3: Delta Marsh Field Station to Latimer Gully to Winnipeg En Route to Next Stop 36 STOP 9: Distal Fan Sediment , 36 STOP 10: Valley Fill Sediments (Latimer Gully) 36 STOP 11: Deep Basin Landforms of Lake Agassiz 42 References Cited 49 Appendix "Review of Lake Agassiz history" (L.H. -
The Maumee River Watershed and Algal Blooms in Lake Erie1 2
SESYNC Case Study The Maumee River Watershed and Algal Blooms in Lake Erie1 2 Ramiro Berardo3 & Ajay Singh4. Summary: The decay of Lake Erie’s environmental health and its impacts on local communities, including public health and the environment, was one of the focal events motivating the passage of the Clean Water Act in 1972. Despite the considerable improvement in water quality in the 1970s and 1980s because of implementation of agricultural best management practices to address soil erosion, seasonal algal blooms returned to Western Lake Erie. Potential causes of algal blooms may be a mixture of agricultural and urban practices that threaten ecological stability and public health for millions dependent on the lake for drinking water, tourism, and fisheries. For instance, in fall, 2014, national attention turned to the city of Toledo, Ohio as the city’s residents experienced disruption to city services such as access to potable water and certain medical services including child birth and surgery. For this case study we will study the relationship between human behavior and water quality impairments which lead to toxic algal blooms in the Western Lake Erie Basin, and in particular, the Maumee River Watershed. We will also review prior management and policy efforts of different stakeholders to improve water quality as well as issues surrounding the development of proposed policy and management changes. Multiple stakeholders from multiple states and Canadian provinces are involved in seeking solutions to the ongoing pollution problems. This case study will be ideal to examine how cooperation unfolds in the presence of collective action problems, and the interrelationships between human behavior and environmental outcomes. -
Status and Trends in Suspended-Sediment Discharges, Soil Erosion, and Conservation Tillage in the Maumee River Basin–Ohio, Michigan, and Indiana
In cooperation with the U.S. Army Corps of Engineers and the U.S. Department of Agriculture, Natural Resources Conservation Service Status and Trends in Suspended-Sediment Discharges, Soil Erosion, and Conservation Tillage in the Maumee River Basin–Ohio, Michigan, and Indiana U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior U.S. Geological Survey Status and Trends in Suspended-Sediment Discharges, Soil Erosion, and Conservation Tillage in the Maumee River Basin—Ohio, Michigan, and Indiana By Donna N. Myers and Kevin D. Metzker, U.S. Geological Survey, and Steven Davis, U.S. Department of Agriculture, Natural Resources Conservation Service Water-Resources Investigations Report 00-4091 In cooperation with the U.S. Army Corps of Engineers and the U.S. Department of Agriculture, Natural Resources Conservation Service U.S. Department of the Interior BRUCE BABBITT, Secretary U.S. Geological Survey Charles G. Groat, Director Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. For additional information write to: District Chief U.S. Geological Survey 6480 Doubletree Avenue Columbus, OH 43229-1111 Copies of this report can be purchased from: U.S.Geological Survey Branch of Information Services Box 25286 Denver, CO 80225-0286 2000 CONTENTS Abstract ................................................................................................................................................................................. 1 Introduction -
Indiana's Great Lakes Water Quality Agreement (GLWQA) Domestic Action Plan (DAP) for the Western Lake Erie Basin (WLEB)
Indiana’s Great Lakes Water Quality Agreement (GLWQA) DOMESTIC ACTION PLAN (DAP) for the WESTERN LAKE ERIE BASIN (WLEB) February 2018 INDIANA’S GREAT LAKES WATER QUALITY AGREEMENT DOMESTIC ACTION PLAN for the WESTERN LAKE ERIE BASIN Table of Contents FOREWORD .................................................................................................................................................................... 2 BACKGROUND ............................................................................................................................................................... 4 GOALS ............................................................................................................................................................................ 6 Timeframe to meet load reduction goals ........................................................................................................ 7 INDIANA’S PORTION OF THE WLEB ............................................................................................................................... 8 Land Use in the WLEB and Major Sources of Phosphorous ............................................................................ 8 WATERSHED PRIORITIZATION ..................................................................................................................................... 11 GUIDING PRINCIPLES FOR ACHIEVING WATER QUALITY IMPROVEMENTS ................................................................. 14 Point Sources/Regulated .............................................................................................................................. -
North Ridge Scenic Byway Geology
GUIDE TO THE NORTH RIDGE SCENIC BYWAY GEOLOGY LANDFORMS The North Ridge Scenic Byway corridor lies in the Erie Lake Plain landform of the Central Lowlands Physiographic Province of the United States (Fenneman 1938; Brockman 2002). The Lake Plain consists of wide expanses of level or nearly level land interrupted only by sandy ridges that are remnants of glacial-lake beaches and by river valleys carved into Paleozoic bedrock. With the exception of the sandy ridges, much of the Lake Plain in Avon and Sheffeld was a dense swamp forest prior to settlement. The North Ridge Scenic Byway follows the northernmost ancient beach ridge as it traverses Sheffeld and Avon at an elevation ranging from 675 to 690 feet above sea level, some 105 to 120 feet above modern Lake Erie. Topography of Sheffeld and Avon Townships as surveyed in 1901, showing North Ridge near the center of the map (courtesy of U.S. Geological Survey, Oberlin, Ohio Quadrangle 1903). 2 GEOLOGY FORMATION OF NORTH RIDGE Approximately 18,000 years ago, the last The chronology of lake stages in the Lake continental glacier blanketed northern Ohio as Erie basin relates a fascinating story of glacial it pushed down from the north to its maximum action, movements of the earth’s crust and southern thrust. The ice sheet reached as far erosion by waves to form the body of water south as Cincinnati, Ohio, then it began to we see today. The story begins nearly 15,000 melt back. As the glacier paused in its retreat, years ago as the last glacier [known as the piles of rock and clay debris [known as end Wisconsinan ice sheet] temporarily halted to moraines] were built up at the ice margins. -
Natural Resource Amendment
Natural Resource Amendment to the Fulton County Comprehensive Development Plan Of 1998 Prepared By Fulton County Regional Planning Commission Steven Brown, Director Leitha Sackmann, Planner & GIS Director Seth Brehm, Planner Adopted April 27, 2004 Revision Adopted June 28, 2011 by the Fulton County Regional Planning Commission Adopted June 28, 2004 Revision Adopted August 4, 2011 by the Fulton County Commissioners TABLE OF CONTENTS List of Maps ............................................................................................................................................................... iii Executive Summary ................................................................................................................................................... iv Acknowledgements .....................................................................................................................................................v Task Force Members ................................................................................................................................................. vi Chapter 1: INTRODUCTION ...................................................................................................................................... 1 BACKGROUND ..................................................................................................................................................... 1 Comprehensive Development Plan Update ....................................................................................................... -
The Fresh-Water Naiades of Auglaize County, Ohio
THE FRESH-WATER NAIADES OF AUGLAIZE COUNTY, OHIO CLARENCE F. CLARK, Ohio Division of Conservation and Natural Resources, St. Marys, Ohio This paper deals with 30 collections of mussels taken at 24 stations (Fig. 1) in the drainage systems of Auglaize County during the past four years, 1938-42. The materials are of interest because: (1) no other naiad records have been pub- lished for this area; (2) rapid changes in stream ecology necessarily alter the mussel fauna; and (3) the proximity of headwater streams of the Ohio and Lake Erie drainages produce interesting distribution patterns for comparison. In the general vicinity, Goodrich (1914) reported on naiades from the Wabash River in Mercer County; Clark and Wilson (1912) surveyed the Maumee and Auglaize Rivers of Defiance County; Kirsch (1894) investigated the Maumee Basin; Ortmann (1919) reported on mussels from the St. Marys River, Beaver Creek, and Lake St. Marys in Mercer County, the Maumee River in Defiance County, the Scioto River in Hardin County, and Indian Lake in Logan County. These collections have been made in counties to the west, north and east of the region considered at present. Records of Sterki (1907) and those from the Carnegie Museum of Pitts- burgh list specimens from the Great Miami drainage to the south. This paper presents data on the origin of the naiades of Auglaize County, the species involved, their distribution and ecology, together with a brief discussion on the future of naiades in the county. Acknowledgements are due Dr. Henry van der Schalie for assistance in the identification of the specimens used in this study and in the preparation of this paper, and Dr.