Black River Watershed Action Plan December 30, 2011
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
Lorain, Ohio: a Study in Urban Geography*
THE OHIO JOURNAL OF SCIENCE VOL. XXXV MAY, 1935 No. 3 LORAIN, OHIO: A STUDY IN URBAN GEOGRAPHY* R. B. FROST, Oberlin College TABLE OF CONTENTS PAGE INTRODUCTION 140 PART I. THE NATURAL ENVIRONMENT A. REGIONAL ASPECTS 1. Lake Erie and the Great Lakes Chain 142 2. The Lake Plain 143 (a) Geological Section 3. Appalachian Plateau 145 (a) Northern Glaciated Section (b) Unglaciated Section 4. Climate and Aboriginal Forest Cover 146 B. SITE CHARACTERISTICS 1. Black River and its Estuary 148 2. Lake Erie Shoreline 150 PART II. SEQUENT STAGES OF HUMAN OCCUPANCE (1755-1894) A. THE LANDSCAPE DURING THE INDIAN PERIOD 1. Indian Occupance 151 2. Indian Removal 152 B. THE LANDSCAPE DURING THE PIONEER PERIOD 1. Interim Period 153 2. Village Birth 154 3. Pioneer Developments 155 C. LANDSCAPE DURING THE PERIOD OF GROWTH 1. Agri-functional Character of the Village 158 2. Durand Survey 159 3. Village Extensions 160 4. Population Increase 160 D. A DECADENT VILLAGE 1. Effects of Railroad Expansion on Charleston 161 2. Decline of Population 162 3. Trade Decline 162 4. Persistence of Certain Industries 164 *Publication of this paper is made possible by a grant-in-aid from the trustees of the Research Fund of the Ohio Academy of Science. 139 140 R. B. FROST Vol. XXXV E. THE LANDSCAPE OF THE EARLY INDUSTRIAL PERIOD: A REVIVAL 1. Functional Changes 166 PART III. MODERN LANDSCAPE (1894-1932) A. RECENT GROWTH AND EXTENSION OF LORAIN 1. Landscape Characteristics 173 2. Present Plan 176 B. ELEMENTS OF THE CULTURAL LANDSCAPE 1. Heavy Industrial 182 2. -
Chapter 1. Natural History
CHAPTER 1. NATURAL HISTORY CHAPTER 1. NATURAL HISTORY —THE WILDERNESS THAT GREETED THE FIRST SETTLERS The land one sees today traveling through northern Ohio took gone. Thus, some 14,000 years ago as the last glacier receded millions of years to form. We can see evidence of tropical sea into the Lake Erie basin, the first Native Americans arrived and reefs on the Lake Erie Islands and deep ocean sediments here in began to utilize the natural resources that these natural processes the cliffs of the Black River. Ohio was just south of the equator had produced. at that time, some 350 million years ago, and over the millennia The natural history of Sheffield encompasses all those natural has migrated northward to its present position. Mountain features and processes of the environment that greeted the Native building to the east eventually raised the sea floor from under Americans, and later the pioneers, when they first arrived in the waves and erosion by streams, and later glacial ice, began Sheffield. To be sure, the landscape was a magnificent wilderness to sculpture the land. At the same time plants and animals were to the settlers, but it needed to be “tamed” in order to support evolving and began to populate the new land once the ice was the newcomers. Ice formation on the shale bluff of the Black River north of Garfield Bridge (2005). 1 BICENTENNIAL HISTORY OF SHEFFIELD TOPOGRAPHY Regional Physiography The topography of an area is the configuration of the land Physiography refers to the physical features or landforms of surface, including its relief [vertical differences in elevation of a region. -
Municipality of Tweed 2017 Gallery of Accomplishments Tweed Public Library
MUNICIPALITY OF TWEED 2017 GALLERY OF ACCOMPLISHMENTS TWEED PUBLIC LIBRARY The Tweed Public Library has had a very busy year! Our TD summer reading program was a great success with over 300 participants spread out across the 8 weeks of the program. We capped off the summer reading program with a well-attended magic show. In August the library was chosen by the Canada Post Community Foundation to receive a grant for $500 dollars, we used this money to launch our Building Imagination Lego Club. There were over 20 excited children in attendance for our first meeting in November. We have also held information seminars for the general public on topics such as estate planning and fraud prevention, as well as holding our weekly knitting group and monthly quilting groups which are quite popular. BLACK RIVER TRADING COMPANY ADDITIONALLY, WE HAVE RECENTLY ADDED A LOT OF INTERESTINGLY CARVED FURNITURE TO OUR OFFERING. This year we brought in a tremendous pile of pottery from Malaysia and Vietnam, put together a lot of shelving upon which to display it and redid the pottery section of the website. We know who and where the largest pottery outlets are in Ontario and we can now confidently say we have a more diverse and larger collection than anyone else in Ontario, and, by extension, (Ontario being the largest population base in Canada) we think we likely have the best and largest pottery offering in Canada. We have had the most extensive collection of sculpture in Canada for years and one of our goals has been to be able to add interestingly carved furniture to that "best collection you'll find" list. -
Enhanced Hydropower Database
Enhanced Hydropower Database Final Report | Report Number 18-34 | October 2018 NYSERDA’s Promise to New Yorkers: NYSERDA provides resources, expertise, and objective information so New Yorkers can make confident, informed energy decisions. Mission Statement: Advance innovative energy solutions in ways that improve New York’s economy and environment. Vision Statement: Serve as a catalyst – advancing energy innovation, technology, and investment; transforming New York’s economy; and empowering people to choose clean and efficient energy as part of their everyday lives. Enhanced Hydropower Database Final Report Prepared for: New York State Energy Research and Development Authority Albany, NY Prepared by: Gomez and Sullivan Engineers, D.P.C Utica, NY NYSERDA Report 18-34 NYSERDA Contract 104255 October 2018 Notice This report was prepared by Gomez and Sullivan Engineers, D.P.C. in the course of performing work contracted for and sponsored by the New York State Energy Research and Development Authority (hereafter “NYSERDA”). The opinions expressed in this report do not necessarily reflect those of NYSERDA or the State of New York, and reference to any specific product, service, process, or method does not constitute an implied or expressed recommendation or endorsement of it. Further, NYSERDA, the State of New York, and the contractor make no warranties or representations, expressed or implied, as to the fitness for particular purpose or merchantability of any product, apparatus, or service, or the usefulness, completeness, or accuracy of any processes, methods, or other information contained, described, disclosed, or referred to in this report. NYSERDA, the State of New York, and the contractor make no representation that the use of any product, apparatus, process, method, or other information will not infringe privately owned rights and will assume no liability for any loss, injury, or damage resulting from, or occurring in connection with, the use of information contained, described, disclosed, or referred to in this report. -
Late Devonian and Early Mississippian Distal Basin-Margin Sedimentation of Northern Ohio1
Late Devonian and Early Mississippian Distal Basin-Margin Sedimentation of Northern Ohio1 THOMAS L. LEWIS, Department of Geological Sciences, Cleveland State University, Cleveland, OH 44115 ABSTRACT. Clastic sediments, derived from southeastern, eastern and northeastern sources, prograded west- ward into a shallow basin at the northwestern margin of the Appalachian Basin in Late Devonian and Early Mississippian time. The western and northwestern boundary of the basin was the submerged Cincinnati Arch. The marine clastic wedges provided a northwest paleoslope and a distal, gentle shelf-edge margin that controlled directional emplacement of coarse elastics. Rising sea levels coupled with differences in sedimen- tation rates and localized soft-sediment deformation within the basin help explain some features of the Bedford and Berea Formations. The presence of sand-filled mudcracks and flat-topped symmetrical ripple marks in the Berea Formation attest to very shallow water deposition and local subaerial exposure at the time of emplacement of part of the formation. Absence of thick, channel-form deposits eastward suggests loss of section during emergence. OHIO J. SCI. 88 (1): 23-39, 1988 INTRODUCTION The Bedford Formation (Newberry 1870) is the most The Ohio Shale, Bedford, and Berea Formations of lithologically varied formation of the group. It is com- northern Ohio are clastic units which record prograda- prised of gray and red mudshales, siltstone, and very tional and transgressional events during Late Devonian fine-grained sandstone. The Bedford Formation thins and Early Mississippian time. The sequence of sediments both to the east and west and reaches its maximum is characterized by (1) gray mudshale, clayshale, siltstone, thickness in the Cleveland area. -
Black River Watershed Management Plan
Black River Watershed Management Plan MDEQ Tracking Codes 2002-0067 2005-0108 April 2005 Updated September 2009 Prepared by: Erin Fuller Black River Watershed Coordinator Van Buren Conservation District 1035 E. Michigan Avenue Paw Paw, MI 49079 (269) 657-4030 www.vanburencd.org i Table of Contents 1 Project Overview and Introduction ............................................................................................................... 1-1 2 Literature Review ............................................................................................................................................ 2-1 3 Watershed Description.................................................................................................................................... 3-1 3.1 Geographic Scope ....................................................................................................................................... 3-1 3.2 Topography ................................................................................................................................................. 3-4 3.3 Soils............................................................................................................................................................. 3-4 3.4 Ecosystem and Climate ............................................................................................................................... 3-5 3.5 Land Use and Land Cover.......................................................................................................................... -
Council Report Template
PW-12-2019-3 - Attachment B Bin Site Transition Plan Prepared for the Ministry of the Environment, Conservation and Parks DRAFT FOR DISCUSSION September 25, 2019 The District Municipality of Muskoka Engineering and Public Works Department 70 Pine Street, Second Floor Bracebridge, Ontario P1L 1N3 TABLE OF CONTENTS PART 1 – BACKGROUND .............................................................................................................. 1 1.1 INTRODUCTION ............................................................................................................ 1 1.2 MUSKOKA WASTE MANAGEMENT ............................................................................. 1 1.3 PROVINICIAL POLICY ................................................................................................... 2 1.3.1 Waste Sites and the Environmental Protection Act (EPA) .................................... 2 1.4 HISTORY OF THE “BIN SITE” ....................................................................................... 3 1.5 THE PROBLEM .............................................................................................................. 3 1.6 CURRENT BIN SITE NETWORK ................................................................................... 4 1.7 MUSKOKA’S WASTE MANGEMENT STRATEGY ........................................................ 5 PART 2 – CHANGE IMPACT ASSESSMENT ................................................................................ 6 2.1 ASSESSING IMPACT OF BIN SITE REMOVAL ........................................................... -
Southern Highways Program
Southern Highways Program 2017-2021 Ministry of Transportation TABLE OF CONTENTS SOUTHERN REGIONAL MAP ..................................................................................... 1 INTRODUCTION........................................................................................................ 2 SOUTHERN EXPANSION 2017 – 2021 ....................................................................... 3 SOUTHERN REHABILITATION 2017 – 2021 ............................................................... 8 PLANNING FOR THE FUTURE .................................................................................. 49 SOUTHERN REGIONAL MAP 1 SOUTHERN HIGHWAYS PROGRAM 2017-2021 INTRODUCTION Creating Jobs and Building a Stronger Ontario In 2017/18, the Ontario government will be investing more than $2.5 billion to repair and expand provincial highways and bridges. This includes almost $1.9 billion for Southern Ontario creating or sustaining approximately 13,300 direct and indirect jobs. Improving Ontario's transportation network is part of the government’s plan to strengthen the economy. 2017/18 Planned Accomplishments Southern Ontario 407 East Other Projects Total (Phase 2A) New highways (lane kms) 29 21 50 New bridges 10 10 Highways rehabilitated 317 317 (centreline kms) Bridges 121 121 rehabilitated The timing of projects in the following lists is subject to change based on funding, planning, design, environmental approval, property acquisition, and construction requirements. 2 SOUTHERN EXPANSION 2017 – 2021 WEST ONTARIO EXPANSION 2017-2021† -
Assessing the Petroleum Geology and Future Development of the Clendenin Gas Field in Kanawha County, West Virginia
Assessing the Petroleum Geology and Future Development of the Clendenin Gas Field in Kanawha County, West Virginia By: Jonathan Prevatte August 2020 Director of Thesis: Donald W. Neal Major Department: Geological Sciences Petroleum is one of the main sources for energy production in the US and is therefore important for the continuation of economic growth. Future development of petroleum resources in the US to meet supply demands is equally important. Understanding the controls on petroleum production will help in determining where and how to development these resources for maximum production. West Virginia is home to many gas fields and is underlain by one of the more prominent gas producing shales, the Marcellus Shale. The Clendenin Gas Field in Kanawha County is one of the historical gas producing areas found in West Virginia. This assessment is focused on the Devonian strata throughout the field including the Marcellus Shale. Using available geophysical logs, production data, and historic well records obtained from the West Virginia Geologic and Economic Survey (WVGES), cross-sections, isopach maps, and structure contour maps were created to give a visual representation of the subsurface geology across the field. Construction of the cross-sections and maps in conjunction with production and well record data aided in the identification of controls influencing production throughout the field. Applying the findings of this assessment to future production may reduce costs and improve yields of future petroleum wells. Results of this study indicate several options should be considered when planning for future production wells within the field. Target areas include the areas to the east of the field where formations tend to thicken. -
Marcellus Shale,” Hamilton Group [email protected] 2045 Morse Rd., Bldg
Matthew S. Erenpreiss Ohio Department of Natural Resources, Division of Geological Survey Mapping the Regional Organic Thickness of the “Marcellus Shale,” Hamilton Group [email protected] 2045 Morse Rd., Bldg. C-2, Columbus, OH 43229-6693 ABSTRACT • Regional and statewide isopach maps Shale” in each county and township, where available; this newly compiled data and observing the “Marcellus ASHTABULA REFERENCES WILLIAMS FULTON LUCAS OTTAWA LAKE GEAUGA WOOD Lash, G.G., and Engelder, Terry, 2011, Thickness HENRY TRUMBULL have been developed for the Middle Devonian “Marcellus this approach allowed for an even distribution of control Shale” upper and lower units, net organic thickness SANDUSKY CUYAHOGA DEFIANCE ERIE LORAIN trends and sequence stratigraphy of the Middle PORTAGE HURON SUMMIT Devonian Marcellus Formation, Appalachian Basin— PAULDING SENECA MEDINA Shale” for use in assessing Ohio’s shale gas potential. points and more consistent correlations. This correlation was calculated and contoured. Additional data was also PUTNAM HANCOCK MAHONING Implications for Acadian foreland basin evolution: VAN WERT WYANDOT CRAWFORD RICHLAND ASHLAND WAYNE AAPG Bulletin, v. 95, no. 1, p. 61–103. Existing stratigraphic analyses of Devonian shales in Ohio expansion of the Hamilton Group, “Marcellus Shale,” collected from the state geological surveys of New York, ALLEN STARK COLUMBIANA Ohio Division of Geological Survey, 1988, Analysis of HARDIN MERCER CARROLL stratigraphic and production relationships of Devonian MARION AUGLAIZE HOLMES MORROW TUSCARAWAS shale gas reservoirs in Ohio–Final report October were used as the starting dataset, which was expanded and Onondaga Limestone was based on U.S. Geological Pennsylvania, and West Virginia to create a new regional LOGAN KNOX SHELBY UNION JEFFERSON COSHOCTON HARRISON DELAWARE 1985–November 1988 (prepared for Gas Research DARKE A’ Institute): Ohio Department of Natural Resources, CHAMPAIGN LICKING with additional geophysical logs that span the “Marcellus Survey cross sections published in Bulletin 1909. -
Geology of Fairfield County, Ohio
This dissertation has been 61—5134 microfilmed exactly as received WOLFE, Edward Winslow, 1936- GEOLOGY OF FAIRFIELD COUNTY, OHIO. The Ohio State University, Ph.D., 1961 Geology University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY OF FAIRFIELD COUNTY, OHIO DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of the Ohio State University By Edward Winslow Wolfe, B. A. The Ohio State University 1961 Approved by Department of Geology ! ACKNOWLEDGMENTS Thanks are due Mr. R. J. Bernhagen, State Geologist, who suggest ed the need for an investigation of the geology of Fairfield County. The writer is particularly indebted to Dr. Aurele La Rooque who di rected the investigation and guided the writer throughout the prepara tion of this report. Many others gave freely of their time in dis cussing with the writer the geology of Fairfield County. Among these, special thanks are due Dr. Jane L. Forsyth of the Ohio Division of Geological Survey, Mr. George J. Franklin, who is presently completing a report on the geology of Licking County, and the writer's colleagues in the Department of Geology at the College of Wooster. The writer thanks several members of the Ohio Division of Geological Survey, in cluding Miss Pauline Smyth, Mr. Karl V. Hoover, and Mr. Harold J. Flint, for their valuable assistance. Most helpful, too, was the as sistance of Mr. Jon S. Galehouse during the summer of i960. The field work was sponsored and financed by the Ohio Division of Geological Survey. Additional financial aid, in the form of a William H. -
Lake Sturgeon (Acipenser Fulvescens) As Endangered Or Threatened Under the Endangered Species Act
Petition to List U.S. Populations of Lake Sturgeon (Acipenser fulvescens) as Endangered or Threatened under the Endangered Species Act May 14, 2018 NOTICE OF PETITION Submitted to U.S. Fish and Wildlife Service on May 14, 2018: Gary Frazer, USFWS Assistant Director, [email protected] Charles Traxler, Assistant Regional Director, Region 3, [email protected] Georgia Parham, Endangered Species, Region 3, [email protected] Mike Oetker, Deputy Regional Director, Region 4, [email protected] Allan Brown, Assistant Regional Director, Region 4, [email protected] Wendi Weber, Regional Director, Region 5, [email protected] Deborah Rocque, Deputy Regional Director, Region 5, [email protected] Noreen Walsh, Regional Director, Region 6, [email protected] Matt Hogan, Deputy Regional Director, Region 6, [email protected] Petitioner Center for Biological Diversity formally requests that the U.S. Fish and Wildlife Service (“USFWS”) list the lake sturgeon (Acipenser fulvescens) in the United States as a threatened species under the federal Endangered Species Act (“ESA”), 16 U.S.C. §§1531-1544. Alternatively, the Center requests that the USFWS define and list distinct population segments of lake sturgeon in the U.S. as threatened or endangered. Lake sturgeon populations in Minnesota, Lake Superior, Missouri River, Ohio River, Arkansas-White River and lower Mississippi River may warrant endangered status. Lake sturgeon populations in Lake Michigan and the upper Mississippi River basin may warrant threatened status. Lake sturgeon in the central and eastern Great Lakes (Lake Huron, Lake Erie, Lake Ontario and the St. Lawrence River basin) seem to be part of a larger population that is more widespread.