Delaware's Water World
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Ecosystem Flow Recommendations for the Delaware River Basin
Ecosystem Flow Recommendations for the Delaware River Basin Report to the Delaware River Basin Commission Upper Delaware River © George Gress Submitted by The Nature Conservancy December 2013 THE NATURE CONSERVANCY Ecosystem Flow Recommendations for the Delaware River Basin December 2013 Report prepared by The Nature Conservancy Michele DePhilip Tara Moberg The Nature Conservancy 2101 N. Front St Building #1, Suite 200 Harrisburg, PA 17110 Phone: (717) 232‐6001 E‐mail: Michele DePhilip, [email protected] Suggested citation: DePhilip, M. and T. Moberg. 2013. Ecosystem flow recommendations for the Delaware River basin. The Nature Conservancy. Harrisburg, PA. Table of Contents Acknowledgments ................................................................................................................................. iii Project Summary ................................................................................................................................... iv Section 1: Introduction ........................................................................................................................ 1 1.1 Project Description and Goals ............................................................................................... 1 1.2 Project Approach ........................................................................................................................ 2 Section 2: Project Area and Basin Characteristics .................................................................... 6 2.1 Project Area ................................................................................................................................. -
Nanticoke Currents Summer 2017
Nanticoke June | 2017 currents CONSERVING THE NATUR AL, CULTURAL, AND RECREATIONAL RESOURCES OF THE NANTICOKE RI VER Homeowners Workshops Golden Nanticoke Creek Freaks Workshop Learn about rain gardens, Was there a fungus among The NWA offers educators an rain barrels, pollinator- us? Find out what caused a opportunity to learn about friendly gardening practices, golden sheen on the our local waterways and lawn fertilization, converting Nanticoke in May. learn activities they can lawns to meadows, and conduct with their students See pages 2 & 3 . more. inside and outside. See page 6. See page 5. C+ Grade for the Nanticoke Report Card The Nanticoke’s grades slipped a bit this year. Increased rainfall and higher levels of phosphorus are damaging the waterways. Learn more about the issues and what you can do. See page 7. Unusual Golden Sheen on the Nanticoke River Photo Credit: Tom Darby Written by Mike Pretl & Judith Stribling May 22 dawned as a normal though periodically rainy day for NWA’s Creekwatchers. Every other Monday from late March through early November – rain or shine -- our trained volunteers visit 36 sites on the river and its major tributaries, from Delaware down to Nanticoke. These citizen scientists collect water samples and partner labs analyze for total nitrogen, total phosphorus, chlorophyll a, and bacteria. Creekwatchers also measure dissolved oxygen, salinity, water temperature, water clarity, and total water depth directly. Lastly, Creekwatchers note and record on data sheets the temperature and weather conditions as well as any unusual phenomenon of the water or its surrounding habitat. That morning, our river waters displayed nothing abnormal, only an occasional, slight film of brownish algae, to be expected in the spring months. -
News Release Address: Email and Homepage: U.S
News Release Address: Email and Homepage: U.S. Department of the Interior Maryland-Delaware-D.C. District [email protected] U.S. Geological Survey 8987 Yellow Brick Road http://md.water.usgs.gov/ Baltimore, MD 21237 Release: Contact: Phone: Fax: January 4, 2002 Wendy S. McPherson (410) 238-4255 (410) 238-4210 Below Normal Rainfall and Warm Temperatures Lead to Record Low Water Levels in December Three months of above normal temperatures and four months of below normal rainfall have led to record low monthly streamflow and ground-water levels, according to hydrologists at the U.S. Geological Survey (USGS) in Baltimore, Maryland. Streamflow was below normal at 94 percent of the real-time USGS gaging stations and 83 percent of the USGS observation wells across Maryland and Delaware in December. Record low streamflow levels for December were set at Winters Run and Pocomoke River. Streamflow levels at Deer Creek and Winters Run in Harford County have frequently set new record daily lows for the last four months (see real-time graphs at http://md.water.usgs.gov/realtime/). Streamflow was also significantly below normal at Antietam Creek, Choptank River, Conococheague Creek, Nassawango Creek, Patapsco River, Gunpowder River, Patuxent River, Piscataway Creek, Monocacy River, and Potomac River in Maryland, and Christina River, St. Jones River, and White Clay Creek in Delaware. The monthly streamflow in the Potomac River near Washington, D.C. was 82 percent below normal in December and 54 percent below normal for 2001. Streamflow entering the Chesapeake Bay averaged 23.7 bgd (billion gallons per day), which is 54 percent below the long-term average for December. -
Flood Insurance Study
FLOOD INSURANCE STUDY CECIL COUNTY, MARYLAND AND INCORPORATED AREAS Cecil County Community Community Name Number ↓ CECIL COUNTY (UNINCORPORATED AREAS) 240019 *CECILTON, TOWN OF 240020 CHARLESTOWN, TOWN OF 240021 CHESAPEAKE CITY, TOWN OF 240099 ELKTON, TOWN OF 240022 NORTH EAST, TOWN OF 240023 PERRYVILLE, TOWN OF 240024 PORT DEPOSIT, TOWN OF 240025 RISING SUN, TOWN OF 240158 *No Special Flood Hazard Areas Identified Revised: May 4, 2015 Federal Emergency Management Agency FLOOD INSURANCE STUDY NUMBER 24015CV000B NOTICE TO FLOOD INSURANCE STUDY USERS Communities participating in the National Flood Insurance Program (NFIP) have established repositories of flood hazard data for floodplain management and flood insurance purposes. This Flood Insurance Study (FIS) report may not contain all data available within the Community Map Repository. Please contact the Community Map Repository for any additional data. Part or all of this FIS may be revised and republished at any time. In addition, part of the FIS may be revised by the Letter of Map Revision (LOMR) process, which does not involve republication or redistribution of the FIS. It is, therefore, the responsibility of the user to consult with community officials and to check the community repository to obtain the most current FIS components. Initial Countywide FIS Effective Date: July 8, 2013 Revised Countywide FIS Effective Date: May 4, 2015 TABLE OF CONTENTS Page 1.0 INTRODUCTION ............................................................................................................. -
Simulation of Streamflow and Water Quality in the Brandywine Creek Subbasin of the Christina River Basin, Pennsylvania and Delaware, 1994-98
U.S. Department of the Interior U.S. Geological Survey SIMULATION OF STREAMFLOW AND WATER QUALITY IN THE BRANDYWINE CREEK SUBBASIN OF THE CHRISTINA RIVER BASIN, PENNSYLVANIA AND DELAWARE, 1994-98 Water-Resources Investigations Report 02-4279 In cooperation with the DELAWARE RIVER BASIN COMMISSION, DELAWARE DEPARTMENT OF NATURAL RESOURCES AND ENVIRONMENTAL CONTROL, and the PENNSYLVANIA DEPARTMENT OF ENVIRONMENTAL PROTECTION U.S. Department of the Interior U.S. Geological Survey SIMULATION OF STREAMFLOW AND WATER QUALITY IN THE BRANDYWINE CREEK SUBBASIN OF THE CHRISTINA RIVER BASIN, PENNSYLVANIA AND DELAWARE, 1994-98 by Lisa A. Senior and Edward H. Koerkle Water-Resources Investigations Report 02-4279 In cooperation with the DELAWARE RIVER BASIN COMMISSION, DELAWARE DEPARTMENT OF NATURAL RESOURCES AND ENVIRONMENTAL CONTROL, and the PENNSYLVANIA DEPARTMENT OF ENVIRONMENTAL PROTECTION New Cumberland, Pennsylvania 2003 U.S. DEPARTMENT OF THE INTERIOR GALE A. NORTON, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director For additional information Copies of this report may be write to: purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Branch of Information Services 215 Limekiln Road Box 25286, Federal Center New Cumberland, Pennsylvania 17070-2424 Denver, Colorado 80225-0286 Email: [email protected] Telephone 1-888-ASK-USGS Internet address: http://pa.water.usgs.gov ii CONTENTS Page Abstract . 1 Introduction . 2 Purpose and scope . 4 Previous studies . 5 Acknowledgments . 5 Description of study area . 5 Physical setting . 5 Climate . 5 Geology . 6 Soils. 6 Hydrology . 6 Land use. 8 Water use . 8 Description of model . 8 Data for model input and calibration . 10 Model-input data . -
Landforms & Bodies of Water
Name Date Landforms & Bodies of Water - Vocab Cards hill noun a raised area of land smaller than a mountain. We rode our bikes up and down the grassy hill. Use this word in a sentence or give an example Draw this vocab word or an example of it: to show you understand its meaning: island noun a piece of land surrounded by water on all sides. Marissa's family took a vacation on an island in the middle of the Pacific Ocean. Use this word in a sentence or give an example Draw this vocab word or an example of it: to show you understand its meaning: 1 lake noun a large body of fresh or salt water that has land all around it. The lake freezes in the wintertime and we go ice skating on it. Use this word in a sentence or give an example Draw this vocab word or an example of it: to show you understand its meaning: landform noun any of the earth's physical features, such as a hill or valley, that have been formed by natural forces of movement or erosion. I love canyons and plains, but glaciers are my favorite landform. Use this word in a sentence or give an example Draw this vocab word or an example of it: to show you understand its meaning: 2 mountain noun a land mass with great height and steep sides. It is much higher than a hill. Someday I'm going to hike and climb that tall, steep mountain. Synonyms: peak Use this word in a sentence or give an example Draw this vocab word or an example of it: to show you understand its meaning: ocean noun a part of the large body of salt water that covers most of the earth's surface. -
To Middle Silurian) in Eastern Pennsylvania
The Shawangunk Formation (Upper OrdovicianC?) to Middle Silurian) in Eastern Pennsylvania GEOLOGICAL SURVEY PROFESSIONAL PAPER 744 Work done in cooperation with the Pennsylvania Depa rtm ent of Enviro nm ental Resources^ Bureau of Topographic and Geological Survey The Shawangunk Formation (Upper Ordovician (?) to Middle Silurian) in Eastern Pennsylvania By JACK B. EPSTEIN and ANITA G. EPSTEIN GEOLOGICAL SURVEY PROFESSIONAL PAPER 744 Work done in cooperation with the Pennsylvania Department of Environmental Resources, Bureau of Topographic and Geological Survey Statigraphy, petrography, sedimentology, and a discussion of the age of a lower Paleozoic fluvial and transitional marine clastic sequence in eastern Pennsylvania UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 74-189667 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 65 cents (paper cover) Stock Number 2401-2098 CONTENTS Page Abstract _____________________________________________ 1 Introduction __________________________________________ 1 Shawangunk Formation ___________________________________ 1 Weiders Member __________ ________________________ 2 Minsi Member ___________________________________ 5 Lizard Creek Member _________________________________ 7 Tammany Member _______________________________-_ 12 Age of the Shawangunk Formation _______ __________-___ 14 Depositional environments and paleogeography _______________ 16 Measured sections ______________________________________ 23 References cited ________________________________________ 42 ILLUSTRATIONS Page FIGURE 1. Generalized geologic map showing outcrop belt of the Shawangunk Formation in eastern Pennsylvania and northwestern New Jersey ___________________-_ 3 2. Stratigraphic section of the Shawangunk Formation in the report area ___ 3 3-21. Photographs showing 3. Conglomerate and quartzite, Weiders Member, Lehigh Gap ____ 4 4. -
Classifying Rivers - Three Stages of River Development
Classifying Rivers - Three Stages of River Development River Characteristics - Sediment Transport - River Velocity - Terminology The illustrations below represent the 3 general classifications into which rivers are placed according to specific characteristics. These categories are: Youthful, Mature and Old Age. A Rejuvenated River, one with a gradient that is raised by the earth's movement, can be an old age river that returns to a Youthful State, and which repeats the cycle of stages once again. A brief overview of each stage of river development begins after the images. A list of pertinent vocabulary appears at the bottom of this document. You may wish to consult it so that you will be aware of terminology used in the descriptive text that follows. Characteristics found in the 3 Stages of River Development: L. Immoor 2006 Geoteach.com 1 Youthful River: Perhaps the most dynamic of all rivers is a Youthful River. Rafters seeking an exciting ride will surely gravitate towards a young river for their recreational thrills. Characteristically youthful rivers are found at higher elevations, in mountainous areas, where the slope of the land is steeper. Water that flows over such a landscape will flow very fast. Youthful rivers can be a tributary of a larger and older river, hundreds of miles away and, in fact, they may be close to the headwaters (the beginning) of that larger river. Upon observation of a Youthful River, here is what one might see: 1. The river flowing down a steep gradient (slope). 2. The channel is deeper than it is wide and V-shaped due to downcutting rather than lateral (side-to-side) erosion. -
Maryland Stream Waders 10 Year Report
MARYLAND STREAM WADERS TEN YEAR (2000-2009) REPORT October 2012 Maryland Stream Waders Ten Year (2000-2009) Report Prepared for: Maryland Department of Natural Resources Monitoring and Non-tidal Assessment Division 580 Taylor Avenue; C-2 Annapolis, Maryland 21401 1-877-620-8DNR (x8623) [email protected] Prepared by: Daniel Boward1 Sara Weglein1 Erik W. Leppo2 1 Maryland Department of Natural Resources Monitoring and Non-tidal Assessment Division 580 Taylor Avenue; C-2 Annapolis, Maryland 21401 2 Tetra Tech, Inc. Center for Ecological Studies 400 Red Brook Boulevard, Suite 200 Owings Mills, Maryland 21117 October 2012 This page intentionally blank. Foreword This document reports on the firstt en years (2000-2009) of sampling and results for the Maryland Stream Waders (MSW) statewide volunteer stream monitoring program managed by the Maryland Department of Natural Resources’ (DNR) Monitoring and Non-tidal Assessment Division (MANTA). Stream Waders data are intended to supplementt hose collected for the Maryland Biological Stream Survey (MBSS) by DNR and University of Maryland biologists. This report provides an overview oft he Program and summarizes results from the firstt en years of sampling. Acknowledgments We wish to acknowledge, first and foremost, the dedicated volunteers who collected data for this report (Appendix A): Thanks also to the following individuals for helping to make the Program a success. • The DNR Benthic Macroinvertebrate Lab staffof Neal Dziepak, Ellen Friedman, and Kerry Tebbs, for their countless hours in -
New York State Canal Corporation Flood Warning and Optimization System
K19-10283720JGM New York State Canal Corporation Flood Warning and Optimization System SCOPE OF SERVICES K19-10283720JGM Contents 1 Background of the Project........................................................................................................... 3 2 Existing FWOS features ............................................................................................................... 5 2.1 Data Import Interfaces ............................................................................................................ 5 2.2 Numeric Models ...................................................................................................................... 5 2.2.1 Hydrologic Model............................................................................................................. 6 2.2.2 Hydraulic Model .............................................................................................................. 6 2.3 Data Dissemination Interfaces .................................................................................................. 6 3 Technical Landscape ................................................................................................................... 7 3.1 Software ................................................................................................................................. 7 3.1.1 Systems......................................................................................................................... 7 3.1.2 FWOS Software .............................................................................................................. -
Monopoly and Monopsony Power in a Market for Mud
Monopoly and Monopsony Power in a Market for Mud This article describes an unusual market I use in my intermediate microeconomics courses to illustrate characteristics of monopoly and monopsony power. For over sixty years the Lena Blackburne Rubbing Mud (LBRM) company has been the sole supplier of mud taken from a Delaware River tributary that is applied to all baseballs used by Major League Baseball (MLB) teams. The unique quality of the mud removes the shine and slickness of new baseballs. Students must explain why LBRM is or is not a monopoly and recognize the source of MLB’s monopsony power. Edward Scahill† †University of Scranton © 2020 Journal of Economics Teaching. All rights reserved. Scahill / Journal of Economics Teaching (2020) 1. Introduction A monopoly is an enterprise that is the only seller of a good or service… Before and during the period of the classical economics (roughly 1776–1850), most people believed that… [the] only monopolies that could persist… were those that got the government to exclude rivals… Even today, most important enduring monopolies or near monopolies in the United States rest on government policies…Monopolies that exist independent of government support are likely to be due to smallness of markets (the only druggist in town) or to rest on temporary leadership in innovation…(Stigler) Although most students in my intermediate economics courses understand the graphical analysis of monopoly and the impact of monopoly power on economic welfare, it is a challenge to find actual examples of monopoly power that engage their interest.1 Although dominant firms in many markets have some degree of monopoly power, the number of “pure” monopolies – sole providers of a good or service that have no close substitutes - are rare. -
The Effect of Different Confluence Confirmation Strategies on the Obturation of Vertucci Type II Canal: Micro-CT Analysis
Restor Dent Endod. 2021 Feb;46(1):e12 https://doi.org/10.5395/rde.2021.46.e12 pISSN 2234-7658·eISSN 2234-7666 Research Article The effect of different confluence confirmation strategies on the obturation of Vertucci type II canal: micro-CT analysis Seungjae Do , Min-Seock Seo * Department of Conservative Dentistry, Wonkwang University Daejeon Dental Hospital, Daejeon, Korea Received: Apr 8, 2020 Revised: Jun 7, 2020 ABSTRACT Accepted: Jun 17, 2020 Objectives: The present study aims to compare the obturation quality of 2 confluence Do S, Seo MS confirmation techniques in artificial maxillary first premolars showing Vertucci type II root canal configuration. *Correspondence to Min-Seock Seo, DDS, PhD Materials and Methods: Thirty artificial maxillary premolars having Vertucci type II root Associate Professor, Department of canal configuration were made. They were divided into 3 groups according to the confluence Conservative Dentistry, Wonkwang University confirmation technique as follows. Gutta-percha indentation (GPI) group (confluence Daejeon Dental Hospital, 77 Dunsan-ro, Seo- confirmation using a gutta-percha cone and a K file); electronic apex locator (EAL) group gu, Daejeon 35233, Korea. (confluence confirmation using K files and EAL); and no confluence detection (NCD) E-mail: [email protected] group. In the GPI group and the EAL group, shaping and obturation were performed with Copyright © 2021. The Korean Academy of the modified working length (WL). In the NCD group, shaping was performed without WL Conservative Dentistry adjustment and obturation was carried out with an adjusted master cone. Micro-computed This is an Open Access article distributed tomography was used before preparation and after obturation to calculate the percentage under the terms of the Creative Commons of gutta-percha occupied volume (%GPv) and the volume increase in the apical 4 mm.