Medway Estuary and Marshes
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Field Indicators of Hydric Soils
United States Department of Field Indicators of Agriculture Natural Resources Hydric Soils in the Conservation Service United States In cooperation with A Guide for Identifying and Delineating the National Technical Committee for Hydric Soils Hydric Soils, Version 8.2, 2018 Field Indicators of Hydric Soils in the United States A Guide for Identifying and Delineating Hydric Soils Version 8.2, 2018 (Including revisions to versions 8.0 and 8.1) United States Department of Agriculture, Natural Resources Conservation Service, in cooperation with the National Technical Committee for Hydric Soils Edited by L.M. Vasilas, Soil Scientist, NRCS, Washington, DC; G.W. Hurt, Soil Scientist, University of Florida, Gainesville, FL; and J.F. Berkowitz, Soil Scientist, USACE, Vicksburg, MS ii In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. -
South Fox Meadow Drainage Improvement Project
VILLAGE OF SCARSDALE WESTCHESTER COUNTY, NEW YORK COMPREHENSIVE STORM WATER MANAGEMENT SOUTH FOX MEADOW STORMWATER IMPROVEMENT PROJECT In association with WESTCHESTER COUNTY FLOOD MITIGATION PROGRAM Rob DeGiorgio, P.E., CPESC, CPSWQ The Bronx River Watershed Fox Meadow Brook Bronx River Watershed Area in Westchester 48.3 square miles (30,932 acres) 15 Sub-watersheds Percent of undeveloped land in the Watershed 3.3% (0.8 acres in Fox Meadow Brook (FMB) FMB watershed) 928 acres (5.7% of watershed) Bronx River Watershed Fox Meadow Brook George Field Park High School Duck Pond Project Philosophy and Goals •Provide flood mitigation within the Fox Meadow Brook Drainage Basin. •Reduce peak run off rates in the Bronx River Watershed through dry detention storage. •Rehabilitate and preserve natural landscapes and wetlands through invasive species management and re- construction. •Improve water quality. • Petition for and obtain County grant funding to subsidize the project. Village of Scarsdale Fox Meadow Brook Watershed SR-2 BR-4 SR-3 BR-7 BR-8 SR-5 Village of Scarsdale History •In 2009 the Village completed a Comprehensive Storm Water Management Plan. •Critical Bronx River sub drainage basin areas identified inclusive of Fox Meadow Brook (BR-4, BR-7, BR-8). •26 Capital Improvement Projects were identified, several of which comprise the Fox Meadow Detention Improvement Project. •Project included in Village’s Capital Budget. •Project has been reviewed by the NYS DEC. •NYS EFC has approved financing for the project granting Scarsdale a 50% subsidy for their local share of the costs. Village of Scarsdale Site Locations – 7 Segments 7 Project Segments 1. -
WATER-QUALITY SWALES Maria Cahill, Derek C
OREGON STATE UNIVERSITY EXTENSION SERVICE Photo: Clean Water Services LOW-IMPACT DEVELOPMENT FACT SHEET WATER-QUALITY SWALES Maria Cahill, Derek C. Godwin, and Jenna H. Tilt most Oregon jurisdictions have moved away from grass. hink of a water-quality swale as a rain garden Design elements may vary in several aspects, including in motion: It treats runoff while simultaneously function, vegetation type, and physical setting. Tmoving it from one place to another. The terms “rain garden” and “swale” are often used Water-quality swales (WQ swales) are linear, vegetat- interchangeably, but rain gardens hold runoff and treat ed, channeled depressions in the landscape that convey it, while swales treat runoff as it is conveyed. Depending and treat runoff from a variety of surfaces. Runoff may on the design, the resulting water-quality benefits can be piped or channeled, or it may flow overland to a differ greatly, but water-quality swales generally provide swale. As water passes through the swale, some runoff lower benefit than rain gardens or stormwater planters. may infiltrate, or seep, into the soil. Not all swales are WQ swales. Conveyance swales, Maria Cahill, principal, Green Girl Land Development Solutions; such as ditches, move water from one place to another. Derek Godwin, watershed management faculty, professor, But these are likely narrow channels with no vegetation biological and ecological engineering, College of Agricultural Sciences, Oregon State University; Jenna H. Tilt, assistant and little to no water-quality benefits. WQ swales may be professor (senior research), College of Earth, Ocean, and planted either with grass or landscape plants, although Atmospheric Sciences, Oregon State University EM 9209 June 2018 Site conditions The channel and linear design of swales make them suitable for roadside runoff capture, although residen- tial areas with frequent, closely spaced driveway cul- verts may not be ideal locations (Barr 2001). -
Natural Vegetation of the Carolinas: Classification and Description of Plant Communities of the Lumber (Little Pee Dee) and Waccamaw Rivers
Natural vegetation of the Carolinas: Classification and Description of Plant Communities of the Lumber (Little Pee Dee) and Waccamaw Rivers A report prepared for the Ecosystem Enhancement Program, North Carolina Department of Environment and Natural Resources in partial fulfillments of contract D07042. By M. Forbes Boyle, Robert K. Peet, Thomas R. Wentworth, Michael P. Schafale, and Michael Lee Carolina Vegetation Survey Curriculum in Ecology, CB#3275 University of North Carolina Chapel Hill, NC 27599‐3275 Version 1. May 19, 2009 1 INTRODUCTION The riverine and associated vegetation of the Waccamaw, Lumber, and Little Pee Rivers of North and South Carolina are ecologically significant and floristically unique components of the southeastern Atlantic Coastal Plain. Stretching from northern Scotland County, NC to western Brunswick County, NC, the Lumber and northern Waccamaw Rivers influence a vast amount of landscape in the southeastern corner of NC. Not far south across the interstate border, the Lumber River meets the Little Pee Dee River, influencing a large portion of western Horry County and southern Marion County, SC before flowing into the Great Pee Dee River. The Waccamaw River, an oddity among Atlantic Coastal Plain rivers in that its significant flow direction is southwest rather that southeast, influences a significant portion of the eastern Horry and eastern Georgetown Counties, SC before draining into Winyah Bay along with the Great Pee Dee and several other SC blackwater rivers. The Waccamaw River originates from Lake Waccamaw in Columbus County, NC and flows ~225 km parallel to the ocean before abrubtly turning southeast in Georgetown County, SC and dumping into Winyah Bay. -
Data Collection Requirements and Procedures for Mapping Wetland, Deepwater, and Related Habitats of the United States (Version 3)
Data Collection Requirements and Procedures for Mapping Wetland, Deepwater, and Related Habitats of the United States (version 3) U.S. FISH & WILDLIFE SERVICE - ECOLOGICAL SERVICES DIVISION OF BUDGET AND TECHNICAL SUPPORT BRANCH OF GEOSPATIAL MAPPING AND TECHNICAL SUPPORT FALLS CHURCH, VA 2204 REVISED JULY 2020 1 Acknowledgements The authors would like to acknowledge the following individuals for their support and contributions: Bill Kirchner, USFWS, Region 1, Portland, OR; Elaine Blok, USFWS, Region 8, Portland, OR Brian Huberty, USFWS, Region 3, Twin Cities, MN; Ralph Tiner, USFWS, Region 5, Hadley, MA: Kevin Bon, USFWS, Region 6, Denver, CO; Jerry Tande, USFWS, Region 7, Anchorage, AK; Julie Michaelson, USFWS, Region 7, Anchorage, AK; Norm Mangrum, USFWS, St. Petersburg, FL; Dennis Fowler, USFWS, St. Petersburg, FL; Jim Terry, USFWS, St. Petersburg, FL; Martin Kodis, USFWS, Chief - Branch of Resources and Mapping Support, Washington, D.C. and David J. Stout, USFWS, Chief - Division of Habitat and Resource Conservation, Washington, D.C. Peer review was provided by the following subject matter experts: Dr. Shawna Dark and Danielle Bram, California State University - Northridge. Robb Macleod, Ducks Unlimited, Great Lakes and Atlantic Regional Office, Ann Arbor, MI; Michael Kjellson, Dept. Wildlife and Fisheries, South Dakota State University, Brookings, SD; and Deborah (Jane) Awl, Tennessee Valley Authority, Knoxville, TN. This document may be referenced as: Dahl, T.E., J. Dick, J. Swords, and B.O. Wilen. 2020. Data Collection Requirements and Procedures for Mapping Wetland, Deepwater and Related Habitats of the United States. Division of Habitat and Resource Conservation (version 3), National Wetlands Inventory, Madison, WI. 91 p. -
National Wetlands Inventory
3/23/2016 Wetlands Mapper National Wetlands Inventory Ecological Services ES Home About Us Species Wildlife and Habitat Conservation Development and Energy FWS Regions Library Newsroom NWI Menu Wetlands Mapper NWI Home The Wetlands Mapper integrates digital map data with other resource information to produce timely and relevant management and decision support tools. We recommend looking at the following prior to launching a map: Wetlands Data » Please read the Disclaimer, Data Limitations, Exclusions and Precautions, and Status and Trends » the Wetlands Geodatabase User Caution. Wetlands Layer » Refer to the following links for documentation and answers to frequently asked New: Wetland Mapping questions: Other Topics » Projects Mapper! Wetlands Mapper Documentation and Instructions Manual (PDF) Frequently Asked Questions: Wetlands Mapper (PDF) Click below to open the Mapper. National Wetlands Frequently Asked Questions web page Printing maps with the Wetlands Inventory Mapper (PDF) Mapper Introduction Contact Information » VIDEO: How to find and use the U.S Fish and Wildlife Service's Wetlands Mapper Help and Contacts Click Here to Open the Wetlands Mapper* (data last modified on October 1, 2015; best viewed by maximizing your browser window) To beta test our new HTML5 (nonFlash) mapper on your desktop, click here (FAQs). Frequently Asked Please note: Questions When in the wetlands mapper, you can change major geographic regions by using the "Zoom to: select" pull down menu located at the upper right side corner. For help with the new mobile mapper location function, please read this FAQ. Adobe Flash™ is required to access the Wetlands Mapper. Please visit the Adobe Flash Player website (http://www.adobe.com/products/flashplayer/) to download the latest version of the player. -
Destin Harbor, Joe's Bayou, and Indian Bayou Water Quality
FLORIDA RECIPIENT City of Destin, Florida Destin Harbor, Joe’s Bayou, and Indian AMOUNT $3,593,600 Bayou Water Quality Improvement LEVERAGE This project includes six projects in three focal areas included in the City of Destin’s $50,000 Master Stormwater Management plan to improve surface water quality in Destin LOCATION Harbor, Joe’s Bayou, and Indian Bayou that directly feed into the southwestern Okaloosa County, Florida portion of Choctawhatchee Bay. As part of the project, the City of Destin will establish roadside swale systems to provide treatment for shallow aquifer recharge ANNOUNCEMENT DATE November 2014 prior to discharge, construct exfiltration systems to provide stormwater treatment, and repair poorly performing culverts. Choctawhatchee Bay is a 27-mile-long estuary that PROGRESS UPDATE supports diverse aquatic and wetland habitats. No new or significant work to report. (April 2015) Submerged Aquatic Vegetation (SAV) habitat decline is a significant limiting factor for the overall productivity of the Choctawhatchee Bay, and efforts to improve water quality through the reduction of sediment input into the bay is anticipated to improve the viability of SAV in the western portions of the bay. Seagrass beds in Choctawhatchee Bay support diverse populations of fish and invertebrates, including many recreational and commercial species such as shrimp, eastern oysters, spotted seatrout, gulf menhaden, red drum, blue crab, gulf flounder and mullet. This work is complementary to additional stormwater treatment projects being supported through other oil spill settlement funds. The Gulf Environmental Benefit This suite of Fund, administered by the projects will National Fish and Wildlife complete the Foundation (NFWF), supports actions identified projects to remedy harm and in the City of eliminate or reduce the risk of Destin’s Master harm to Gulf Coast natural Stormwater resources affected by the 2010 Deepwater Horizon oil spill. -
Business Plan 2017-22
Bird Wise North Kent – Business Plan 2017-2022 1 Contents Contents ......................................................................... 1 Introduction .................................................................... 2 Vision and Objectives ..................................................... 3 Year 1 - Implementation 2017/18 .................................. 4 Year 2 - Delivery 2018/19 ............................................... 6 Continuation of Projects 2019-22 ................................ 10 Budget .......................................................................... 12 Bird Wise North Kent – Business Plan 2017-2022 2 Introduction The north Kent coastal habitat from Gravesend to Whitstable plays home to thousands of wading birds and waterfowl. For this reason, the Thames, Medway and Swale estuaries and marshes comprise of three Special Protection Areas (SPAs). All of these are also listed as Ramsar sites due to the international significance of the wetland habitats. Significant development is planned for north Kent with growing demand for new homes to accommodate the increasing population in the administrative areas of Canterbury, Dartford, Gravesham, Medway and Swale. With additional homes, the number of recreational visitors to the coastal areas will increase. Research has shown that the increasing numbers of visitors will have a negative impact on designated bird species. A strategic approach is required to deliver measures to mitigate any disturbance to birds caused by increased recreational activity. The -
04 174 09 Jbc Low Res Proof
walking cover:Layout 1 24/4/09 11:52 Page 1 Over 100 walks exploring countryside, coast and towns May to June 2009 North Kent Walking Festival 2009 It's time to get out and explore the great outdoors and enjoy some fresh air and fantastic views and find out more about the amazing variety of places to visit in north Kent. There's lots to discover on your doorstep. This year's festival builds on the success of events in previous years, and has expanded to cover the whole of north Kent, from Dartford to Faversham. The walking festival has linked to the Gravesham Heritage Festival in late May, so there are six weeks of walks to enjoy. There are over a hundred walks to choose from, starting in mid May and leading up to the end of June. There are a couple of extra ones squeezed into July too. With guided walks exploring our north Kent towns, coast and countryside, there is something for everyone. You may like to join a guided walk learning about the history of the area (in some cases with costumed walks leaders too). There are walks introducing people to the area's wildlife and landscapes. Walks are a great and economical way to get some exercise and socialise at the same time. The walking festival is delivered by many organisations and groups that want to share in celebrating the great heritage and environment that we have in north Kent. It has been sup- ported this year by Greening the Gateway Kent and Medway, an initiative to promote and improve the quality of the environment for people and wildlife in north Kent. -
Biodiversity Opportunity Area Statement Name: North Kent Marshes
Biodiversity Opportunity Area Statement Name: North Kent Marshes Description: The North Kent Marshes are designated, almost in their entirety, as SSSI, SPA and/or Ramsar, and are of national and international importance for breeding and overwintering bird populations. The area includes three areas recommended to be Marine Conservation Zones: the Thames Estuary rMCZ, (on hold) which provides critical spawning and nursery grounds for fish, the Medway Estuary MCZ, designated for a range of estuarine habitats as well as for the tentacled lagoon worm and The Swale Estuary rMCZ (under consultation), supporting seagrass and mussel beds and rich muddy gravels. The opportunity area also includes a few LWSs such as the Diggs and Sheppey Court Marshes near Queenborough, Graveney Dykes and Pasture, Minster Marshes and Minster Cliffs. Much of this Biodiversity Opportunity Area is included in the Greater Thames Estuary Nature Improvement Area. National Character Area(s): Greater Thames Estuary Kent Landscape Character Area(s): Eastern Thames Marshes, Hoo Peninsula, Medway Marshes, Swale Marshes, North Sheppey and Eastern Swale Marshes. Landscape Character: An open and remote landscape characterised by grazing marsh associated with wetlands. Fields are bounded by creeks and ditches – many of which have a long history, creating a distinctive pattern. These landscape features support salt marsh and intertidal mudflats stretching from the River Thames estuary in the west to the Swale Estuary in the east. Settlements and roads are limited in this area, low but prominent hills typically with settlements or copses of trees. Saltmarsh extends inland along creeks and drainage dykes and in places grazing marsh has been converted to arable cultivation. -
A GROUP of MOUNDS on SEASALTER LEVEL, NEAR WHITSTABLE, and the MEDIEVAL IMBANKING in THIS AREA by M
Archaeologia Cantiana Vol. 70 1956 A GROUP OF MOUNDS ON SEASALTER LEVEL, NEAR WHITSTABLE, AND THE MEDIEVAL IMBANKING IN THIS AREA By M. W. THOMPSON THE origin of the mounds that are so commonly found on the marshes around the British Isles has always been a perplexing problem. The Essex Archaeological Society, it will be remembered, after several seasons' excavation on the Red Hills in the Essex marshes were unable to decide what activity had caused their accumulation, and it was only ten years later that Mr. R. A. Smith1 by the use of convincing Conti- nental parallels was able to show beyond reasonable doubt that they were the remains of salt works, where sea-water had been evaporated by an unfamiliar method. A few years later other members of this Society excavated further mounds, taller than the Red Hills, without briquetage and of Medieval date.2 They concluded they were salt works also, a view lent some support by the enclosures adjoining them. In the mounds we shall discuss below there was practically no briquetage and very little red earth; the mounds were clearly Medieval in date and not Roman or Iron Age like the Red Hills; and on Sheppey (within sight three miles away) the dialect word " coterells,"3 apparently of ancient origin, suggested that the mounds there may have been thrown up as refuges for cattle and sheep during tidal flooding. For these reasons we were reluctant to regard these mounds as salt works until the bulldozing of further intact mounds showed such frequent traces of burning that the conclusion became unavoidable that some industrial activity was involved. -
Age, Extent and Carbon Storage of the Central Congo Basin Peatland Complex Greta C
LETTER doi:10.1038/nature21048 Age, extent and carbon storage of the central Congo Basin peatland complex Greta C. Dargie1,2*, Simon L. Lewis1,2*, Ian T. Lawson3, Edward T. A. Mitchard4, Susan E. Page5, Yannick E. Bocko6 & Suspense A. Ifo6 Peatlands are carbon-rich ecosystems that cover just three per We combined a digital elevation model (DEM; from the Shuttle cent of Earth’s land surface1, but store one-third of soil carbon2. Radar Topography Mission, SRTM) to exclude high ground and Peat soils are formed by the build-up of partially decomposed steep slopes, radar backscatter (from the Advanced Land Observation organic matter under waterlogged anoxic conditions. Most peat is Satellite Phased Array type L-band Synthetic Aperture Radar, found in cool climatic regions where unimpeded decomposition ALOS PALSAR) to detect standing surface water under forest, and is slower, but deposits are also found under some tropical swamp optical data (from Landsat Enhanced Thematic Mapper, ETM+ ) to forests2,3. Here we present field measurements from one of the categorize likely swamp vegetation, to identify areas to prospect for world’s most extensive regions of swamp forest, the Cuvette peat (Extended Data Table 1). We identified nine transects (2.5–20 km Centrale depression in the central Congo Basin4. We find extensive long) within an approximately 40,000 km2 area of northern Republic peat deposits beneath the swamp forest vegetation (peat defined of the Congo (ROC), each traversing more than one vegetation type as material with an organic matter content of at least 65 per cent within waterlogged regions, and collectively spanning the range of non- to a depth of at least 0.3 metres).