Waters of Change: the Great Miami River Flood of 1913 and Its Policy Consequences
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The Miami Slaughterhouse
The Miami Slaughterhouse In the 1780’s, a Squirrel could reach Cincinnati from Pittsburg and never touch the ground. In part because of this heavy tree canopy, the land between the Little Miami River and the Great Miami River was known to have some of the richest farm land ever seen. The land between the Miami’s was a special hunting ground for the Indians. They would not give it up without a fight. In 1966, while researching a high school term paper, I found a diary written by Mary Covalt called “Reminiscences of Early Days about the construction and defense of Covalt Station primarily set during the years 1789 until 1795. “ My story tonight is about ordinary men and women coming down the Ohio River to settle in the land between the Little Miami and Great Miami Rivers. The Covalts who came down the Ohio and built Covalt Station in the area now known as Terrace Park were my ancestors. Mary Covalt’s diary along with other letters and personal accounts gives us the chance to use a zoom lens to focus on how life was lived was during this period. This story takes place in the Old Northwest Territory, and more specifically in the Ohio Territory and very specifically in the land between the two Miami Rivers. Not many of us would want to personally experience the sacrifices made to develop this land. Innocently, these pioneers came to a place that would embroil them in a life and death struggle for the next five years. These five years in the Old Northwest Territory would settle once and for all if America’s future growth would be west of the Allegany Mountains. -
5.15 Water Pollution and Hydrologic Impacts 5.15.1 Chapter Index 5.15
Transportation Cost and Benefit Analysis II – Water Pollution Victoria Transport Policy Institute (www.vtpi.org) 5.15 Water Pollution and Hydrologic Impacts This chapter describes water pollution and hydrologic impacts caused by transport facilities and vehicle use. 5.15.1 Chapter Index 5.15 Water Pollution and Hydrologic Impacts ........................................................... 1 5.15.2 Definitions .............................................................................................. 1 5.15.3 Discussion ............................................................................................. 1 5.15.4 Estimates: .............................................................................................. 3 Summary Table ..................................................................................... 3 Water Pollution & Combined Estimates ................................................. 4 Storm Water, Hydrology and Wetlands ................................................. 6 5.15.5 Variability ............................................................................................... 7 5.15.6 Equity and Efficiency Issues .................................................................. 7 5.15.7 Conclusion ............................................................................................. 7 5.15.8 Information Resources .......................................................................... 9 5.15.2 Definitions Water pollution refers to harmful substances released into surface or ground water, -
NRSM 385 Syllabus for Watershed Hydrology V200114 Spring 2020
NRSM 385 Syllabus for Watershed Hydrology v200114 Spring 2020 NRSM (385) Watershed Hydrology Instructor: Teaching Assistant: Kevin Hyde Shea Coons CHCB 404 CHCB 404 [email protected] [email protected] Course Time & Location: Office Hours: (or by appointment) Tue/Thu 0800 – 0920h Kevin: Tue & Thu, 1500 – 1600h Natural Science 307 Shea: Wed & Fri, 1200 – 1300h Recommended course text: Physical Hydrology by SL Dingman, 2002 (2nd edition). Other readings as assigned. Additional course information and materials will be posted on Moodle: umonline.umt.edu Science of water resource management in the 21st Century: Sustainability of all life requires fundamental changes in hydrologic science and water resource management. Forty percent of the Earth’s ever-increasing population lives in areas of water scarcity, where the available supply cannot meet basic needs. Water pollution from human activities and increasing water withdrawals for human use impair and threaten entire ecosystems upon which human survival depends. Climate change increases environmental variability, exacerbating drought in some regions while leading to greater hydrologic hazards in others. Higher intensity and more frequent storms generate flooding that is especially destructive in densely developed areas of and where ecosystems are already compromised. Sustainable water resource management starts with scientifically sound management of forested landscapes. Eighty percent of fresh water supplies in the US originate on forested lands, providing over 60% of municipal drinking water. Forests also account for significant portions of biologically complex and vital ecosystems. Multiple land use activities including logging, agriculture, industry, mining, and urban development compromise forest ecosystems and threaten aquatic ecosystems and freshwater supplies. -
From Engineering Hydrology to Earth System Science: Milestones in the Transformation of Hydrologic Science
Hydrol. Earth Syst. Sci., 22, 1665–1693, 2018 https://doi.org/10.5194/hess-22-1665-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. From engineering hydrology to Earth system science: milestones in the transformation of hydrologic science Murugesu Sivapalan1,* 1Department of Civil and Environmental Engineering, Department of Geography and Geographic Information Science, University of Illinois at Urbana-Champaign, Urbana, Illinois 61801, USA * Invited contribution by Murugesu Sivapalan, recipient of the EGU Alfred Wegener Medal & Honorary Membership 2017. Correspondence: Murugesu Sivapalan ([email protected]) Received: 13 November 2017 – Discussion started: 15 November 2017 Revised: 2 February 2018 – Accepted: 5 February 2018 – Published: 7 March 2018 Abstract. Hydrology has undergone almost transformative hydrology to Earth system science, drawn from the work of changes over the past 50 years. Huge strides have been made several students and colleagues of mine, and discuss their im- in the transition from early empirical approaches to rigorous plication for hydrologic observations, theory development, approaches based on the fluid mechanics of water movement and predictions. on and below the land surface. However, progress has been hampered by problems posed by the presence of heterogene- ity, including subsurface heterogeneity present at all scales. எப்ெபாள் யார்யாரவாய் ் க் ேகட்ம் The inability to measure or map the heterogeneity every- அப்ெபாள் ெமய் ப்ெபாள் காண் ப த where prevented the development of balance equations and In whatever matter and from whomever heard, associated closure relations at the scales of interest, and has Wisdom will witness its true meaning. -
Hydrogeologic Characterization and Methods Used in the Investigation of Karst Hydrology
Hydrogeologic Characterization and Methods Used in the Investigation of Karst Hydrology By Charles J. Taylor and Earl A. Greene Chapter 3 of Field Techniques for Estimating Water Fluxes Between Surface Water and Ground Water Edited by Donald O. Rosenberry and James W. LaBaugh Techniques and Methods 4–D2 U.S. Department of the Interior U.S. Geological Survey Contents Introduction...................................................................................................................................................75 Hydrogeologic Characteristics of Karst ..........................................................................................77 Conduits and Springs .........................................................................................................................77 Karst Recharge....................................................................................................................................80 Karst Drainage Basins .......................................................................................................................81 Hydrogeologic Characterization ...............................................................................................................82 Area of the Karst Drainage Basin ....................................................................................................82 Allogenic Recharge and Conduit Carrying Capacity ....................................................................83 Matrix and Fracture System Hydraulic Conductivity ....................................................................83 -
Native Americans, Europeans, and the Raid on Pickawillany
ABSTRACT “THE LAND BELONGS TO NEITHER ONE”: NATIVE AMERICANS, EUROPEANS, AND THE RAID ON PICKAWILLANY In 1752, the Miami settlement at Pickawillany was attacked by a force of Ottawa and Chippewa warriors under the command of a métis soldier from Canada. This raid, and the events that precipitated it, is ideally suited to act as a case study of the role of Native American peoples in the Ohio Country during the first half of the eighteenth century. Natives negotiated their roles and borders with their British and French neighbors, and chose alliances with the European power that offered the greatest advantage. Europeans were alternately leaders, partners, conquerors and traders with the Natives, and exercised varying levels and types of control over the Ohio Country. Throughout the period, each of the three groups engaged in a struggle to define their roles in regards to each other, and to define the borders between them. Pickawillany offers insights into this negotiation. It demonstrates how Natives were not passive victims, but active, vital agents who acted in their own interest. The events of the raid feature a number of individuals who were cultural brokers, intermediaries between the groups who played a central, but tenuous, role in negotiations. It also exhibits the power of ritual violence, a discourse of torture and maiming that communicated meanings to friends and rivals alike, and whose implications shaped the history of the period and perceptions of Natives. Luke Aaron Fleeman Martinez May 2011 “THE LAND BELONGS TO NEITHER ONE”: -
Development of a Benthic Macroinvertebrate In
Monitoring water quality of urban stormwater runoff to receiving river systems in Dayton, Ohio: Wet-weather sampling, site selection, and assessment of MS4 drainage areas By Kevin W. Custer, Eric B. Borth and Ryan W. McEwan Department of Biology University of Dayton 300 College Park Dr. Dayton, Ohio 45469 ___________________________________________ For The City of Dayton Department of Water Division of Environmental Management Final Report 31-December-2016 City of Dayton MS4 monitoring - 2016 1 Table of Contents EXECUTIVE SUMMARY .......................................................................................................... 5 1.0 BACKGROUND AND OBJECTIVES ................................................................................. 6 2.0 MATERIALS AND METHODS ........................................................................................... 7 2.1 WET-WEATHER SAMPLING DESIGN ......................................................................................... 7 2.2 WET-WEATHER SITES ............................................................................................................. 7 2.3 WATER SAMPLING .................................................................................................................. 8 2.4 PRECIPITATION ....................................................................................................................... 9 2.5 QA/QC .................................................................................................................................. 9 3.0 -
Taylorsville Metropark
Old Springfield Road PARK FEATURES TAYLORSVILLE BUCKEYE & NORTH METROPARK Buckeye & North COUNTRY TRAILS Country Trails S The Buckeye and North Country Trails join the Great u l l i Miami River Bikeway at Old Springfield Road and v a n follow it south through the park. The Buckeye Trail R o completely encircles Ohio and is more than 1,400 a d miles long. The North Country Scenic Trail extends into seven states and will be the longest continuous hiking trail in the United States when completed. Both trails provide long-distance hiking and link historical and scenic features of the state and surrounding areas. MIAMI-ERIE CANAL Running parallel to the Great Miami River through Taylorsville was the Miami-Erie Canal. This hand dug “big ditch,” completed in 1845, took 20 years to construct. A great achievement for its day, it opened the state for commerce by connecting the Ohio River at Cincinnati to Lake Erie at Toledo with a navigable channel. Remnants of the canal can still be found on the north and south sides of the dam. Five hundred Trails are open year-round, but during periods of high feet north of the dam stands the foundation of an water, trails along river may be muddy or impassable. aqueduct. These impressive structures were large, Visit metroparks.org/alerts for park closure information. water-filled bridges over rivers that allowed canal boats to cross. Color-Coded Hiking Trails TRAIL TADMOR white trail = 0.3 miles Follow the Great Miami River Bikeway north of the K E Y green trail = 0.4 miles dam about 1.25 miles to the site of Tadmor. -
Along the Ohio Trail
Along The Ohio Trail A Short History of Ohio Lands Dear Ohioan, Meet Simon, your trail guide through Ohio’s history! As the 17th state in the Union, Ohio has a unique history that I hope you will find interesting and worth exploring. As you read Along the Ohio Trail, you will learn about Ohio’s geography, what the first Ohioan’s were like, how Ohio was discovered, and other fun facts that made Ohio the place you call home. Enjoy the adventure in learning more about our great state! Sincerely, Keith Faber Ohio Auditor of State Along the Ohio Trail Table of Contents page Ohio Geography . .1 Prehistoric Ohio . .8 Native Americans, Explorers, and Traders . .17 Ohio Land Claims 1770-1785 . .27 The Northwest Ordinance of 1787 . .37 Settling the Ohio Lands 1787-1800 . .42 Ohio Statehood 1800-1812 . .61 Ohio and the Nation 1800-1900 . .73 Ohio’s Lands Today . .81 The Origin of Ohio’s County Names . .82 Bibliography . .85 Glossary . .86 Additional Reading . .88 Did you know that Ohio is Hi! I’m Simon and almost the same distance I’ll be your trail across as it is up and down guide as we learn (about 200 miles)? Our about the land we call Ohio. state is shaped in an unusual way. Some people think it looks like a flag waving in the wind. Others say it looks like a heart. The shape is mostly caused by the Ohio River on the east and south and Lake Erie in the north. It is the 35th largest state in the U.S. -
Runoff Hydrology 101
Runoff Hydrology 101 Hydrology 101 Runoff Hydrology 101 Legislation (c) The agency shall develop performance standards, design standards, or other tools to enable and promote the implementation of low-impact development and other stormwater management techniques. For the purposes of this section, "low-impact development" means an approach to storm water management that mimics a site's natural hydrology as the landscape is developed. Using the low-impact development approach, storm water is managed on-site and the rate and volume of predevelopment storm water reaching receiving waters is unchanged. The calculation of predevelopment hydrology is based on native soil and vegetation. Minnesota Statutes 2009, section 115.03, subdivision 5c Runoff Hydrology 101 The Water Cycle Hanson, 1994 Runoff Hydrology 101 Development Impacts on the Water Cycle Runoff Hydrology 101 Runoff Hydrology 101 Rate Impacts of Development 1 Existing Hydrograph 2 Developed, conventional CN, no controls Vegetation Removal Pre-development Soil Compaction Peak Runoff Volume Rate Q Drainage Alteration 2 Impervious Areas 1 Area under the curve = Volume T Runoff Hydrology 101 Hydrograph Scenarios Rate 1 Existing 2 Developed, conventional CN, no control. 3 Developed, conventional CN and control. MIDS Pre-development 4 Peak Runoff Volume Rate Q 3 2 1 4 T Runoff Hydrology 101 Factors Affecting Q Runoff • Precipitation • Antecedent moisture • Soil permeability • Watershed area • Ground cover • Storage in watershed • Time parameters Runoff Hydrology 101 Runoff Equations Runoff Hydrology 101 Runoff Curve Numbers Commonly used approach to determine runoff Based on land cover and soils Simple regression model that is useful for quickly assessing stormwater management practices and assessing impacts of land use changes Runoff Hydrology 101 Hydrological Soil Group: Soil groups which are classified according to their drainage potential. -
Henry Larcom Abbot 1831-1927
NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA BIOGRAPHICAL MEMOIRS VOLUME XIII FIRST MEMOIR BIOGRAPHICAL MEMOIR OF HENRY LARCOM ABBOT 1831-1927 BY CHARLES GREELEY ABBOT PRESENTED TO THE ACADEMY AT THE ANNUAL MEETING, 1929 HENRY LARCOM ABBOT 1831-1927 BY CHARGES GREKLEY ABBOT Chapter I Ancestry Henry Larcom Abbot, Brigadier General, Corps of Engi- neers, U. S. Army, member of the National Academy of Sciences, was born at Beverly, Essex County, Massachusetts, August 13, 1831. He died on October 1, 1927, at Cambridge, Massachusetts, aged 96 years. He traced his descent in the male line from George Abbot, said to be a native of Yorkshire, England, who settled at Andover, Massachusetts, in the year 1642. Through early intermarriage, this line is closely con- nected with that of the descendants of George Abbott of Row- ley, Essex County, Massachusetts. The Abbots of Andover were farmers, highly respected by their townsmen, and often intrusted with elective office in town, church, and school affairs. In the fifth generation, de- scended through John, eldest son of George Abbot of An- dover,1 Abiel Abbot, a great-grandfather of General Abbot, removed from Andover to settle in Wilton, Hillsborough County, New Hampshire, in the year 1763. He made his farm from the wilderness on "Abbot Hill" in the southern part of the township. Having cleared two acres and built a two-story house and barn, he married Dorcas Abbot and moved into the house with his bride before the doors were hung, in November, 1764. They had thirteen children, of whom the fourth, Ezra Abbot, born February 8, 1772, was grandfather to our propo- s^tus. -
Shelby County Natural Hazards Mitigation Plan
Shelby County Natural Hazards Mitigation Plan Prepared for Shelby County, Ohio February, 2005 Shelby County- Countywide All Natural Hazards Mitigation Plan Draft TABLE OF CONTENTS EXECUTIVE SUMMARY.............................................................................................................iii LIST OF ACRONYMS .................................................................................................................iv 1.0 INTRODUCTION .................................................................................................................1-1 1.1 Planning Approach .......................................................................................................1-2 1.2 Participating Communities ............................................................................................1-3 2.0 COMMUNITY INFORMATION ............................................................................................2-1 2.1 County Profile ...............................................................................................................2-1 2.2 County History ..............................................................................................................2-1 2.3 Jurisdictions ..................................................................................................................2-2 2.4 Census Information.......................................................................................................2-9 2.5 County Land Use and Future Land Use .....................................................................2-11