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Preliminary Flood Insurance Study
VOLUME 4 OF 4 YORK COUNTY, MAINE (ALL JURISDICTIONS) COMMUNITY NAME NUMBER COMMUNITY NAME NUMBER ACTON, TOWN OF 230190 OGUNQUIT, TOWN OF 230632 ALFRED, TOWN OF 230191 OLD ORCHARD BEACH, TOWN OF 230153 ARUNDEL, TOWN Of 230192 PARSONSFIELD, TOWN OF 230154 BERWICK, TOWN OF 230144 SACO, CITY OF 230155 BIDDEFORD, CITY OF 230145 SANFORD, CITY OF 230156 BUXTON, TOWN OF 230146 SHAPLEIGH, TOWN OF 230198 CORNISH, TOWN OF 230147 SOUTH BERWICK, TOWN OF 230157 DAYTON, TOWN OF 230148 WATERBORO, TOWN OF 230199 ELIOT, TOWN OF 230149 WELLS, TOWN OF 230158 HOLLIS, TOWN OF 230150 YORK, TOWN OF 230159 KENNEBUNK, TOWN OF 230151 KENNEBUNKPORT, TOWN OF 230170 KITTERY, TOWN OF 230171 LEBANON, TOWN OF 230193 LIMERICK, TOWN OF 230194 LIMINGTON, TOWN OF 230152 LYMAN, TOWN OF 230195 NEWFIELD, TOWN OF 230196 NORTH BERWICK, TOWN OF 230197 EFFECTIVE: FLOOD INSURANCE STUDY NUMBER 23005CV004A Version Number 2.3.2.1 TABLE OF CONTENTS Volume 1 Page SECTION 1.0 – INTRODUCTION 1 1.1 The National Flood Insurance Program 1 1.2 Purpose of this Flood Insurance Study Report 2 1.3 Jurisdictions Included in the Flood Insurance Study Project 2 1.4 Considerations for using this Flood Insurance Study Report 20 SECTION 2.0 – FLOODPLAIN MANAGEMENT APPLICATIONS 31 2.1 Floodplain Boundaries 31 2.2 Floodways 43 2.3 Base Flood Elevations 44 2.4 Non-Encroachment Zones 44 2.5 Coastal Flood Hazard Areas 45 2.5.1 Water Elevations and the Effects of Waves 45 2.5.2 Floodplain Boundaries and BFEs for Coastal Areas 46 2.5.3 Coastal High Hazard Areas 47 2.5.4 Limit of Moderate Wave Action 48 SECTION -
Status of Conservation Planning for Watersheds of Southern Maine
watermark volume 26 issue 1 5 stewardship / conserving natural resources Status of Conservation Planning for Watersheds of Southern Maine The Wells Reserve has produced or assisted with every key conservation planning document prepared for What is a watershed? southern Maine watersheds over the past decade. Use this chart to learn which plans cover your town, then An area in which water, sediments, download the plan(s) from our website or read them at the Dorothy Fish Coastal Resource Library. and dissolved material drain to a To get involved in land or water protection in your area, contact the individuals or organizations named common outlet, such as a river, lake, in the plans. Key contacts for most towns and watersheds can also be found at swim.wellsreserve.org. If these bay, or ocean. avenues don’t work out, call the Wells Reserve stewardship coordinator, Tin Smith, at 646-1555 ext 119. U.S. Environmental Protection Agency Watershed A geographic area in which water flows on its way to a larger water body, such as a stream, river, estuary, lake, or Town Bridges Swamp Neddick River Cape River Works Great Josias River Kennebunk River Little River Mousam River Ogunquit River River Piscataqua River Salmon Falls Southside Brook Creek Spruce River Webhannet River York ocean. Coastal and ocean resources Acton 7 11 are affected not only by activities in Alfred 4 7 coastal areas but also by those in Arundel 4 7 upland watersheds. Berwick 2,3 2,11 U.S. Commission on Ocean Policy Eliot 2,11 2,11 2,13,14 2,16,17 Kennebunk 4 5,6 7 Kennebunkport 4 Why these watersheds? Kittery 11 11 0 13,14 16,17 The chart shows the Maine watersheds Lebanon 11 and towns that are included in the web- Lyman 4 7 based Seacoast Watershed Information North Berwick 2,3 2,11 Manager (swim.wellsreserve.org). -
Bay of Fundy (Canada)
Tides Bay of Fundy (Canada) Tides Measuring tides General description Physical mechanism Characteristics in different locations Tidal resonance and tidal bore Measuring tides Records of the position of sea surface with respect to a fixed level (a datum) tidal pole float tidal gauge Measuring tides Time series of sea surface height Hilo tide observations and predictions (PacIOOS) Measuring tides Examples of tidal time series General description Up and down motion of sea level Back and forth currents Periodic (~12 hours and 24 hours) Amplitude and timing vary from one location to another Propagating shallow-water wave of very long wavelength (~10,000km) Physical mechanism due to the gravitational attraction of Moon and Sun on Earth and its ocean and the rotation of Moon around Earth and the Earth-Moon system around the Sun Moon Sun Earth Physical mechanism due to the gravitational attraction of Moon and Sun on Earth and its ocean and the rotation of Moon around Earth and the Earth-Moon system around the Sun Moon Sun “It's complicated!” Earth Theory of equilibrium tides Simplified problem Earth-Moon system only No rotation of Earth around its own axis Earth covered with an ocean (no continents) No friction Theory of equilibrium tides Centrifugal Force (varies with r) r d Gravitational Force (varies with 1/d2) Theory of equilibrium tides Theory of equilibrium tides Theory of equilibrium tides Theory of equilibrium tides Theory of equilibrium tides Tidal Force Theory of equilibrium tides Tidal Force Theory of equilibrium -
Town of Columbia Falls, Maine Comprehensive Plan 2019
TOWN OF COLUMBIA FALLS, MAINE COMPREHENSIVE PLAN 2019 Prepared by the Columbia Falls Comprehensive Plan Committee: Nancy Bagley Grace Falzarano Tony Santiago Philip Worcester Shelby Greene Jeff Greene David Perham Debi Beal Consultant: Washington County Council of Governments Table of Contents Chapter A. Executive Summary And Community Vision Chapter B. Public Opinion Survey Chapter C. Gis Mapping Chapter D. Historical And Archaeological Resources Chapter E. Population Chapter F. Natural Resources Chapter G. Employment And Economy Chapter H. Housing Chapter I. Public Facilities, Services, And Recreation Chapter J. Transportation Chapter K. Fiscal Capacity Chapter L. Regional Coordination Chapter M. Land Use Chapter N. Policies And Implementation Strategies Appendix A. Public Opinion Survey & Written Comments Appendix B. State Policies Appendix C. Evaluation Measures Appendix D. Maine’s Growth Management Legislation Appendix E. Affordable Housing And Elder Care Remedies Appendix F. 2002 Policies And Implementation Strategies CHAPTER A. VISION AND EXECUTIVE SUMMARY A. VISION AND EXECUTIVE SUMMARY Comprehensive planning demonstrates the importance of land use standards for Columbia Falls. Preserving and protecting the character of Columbia Falls is vital to the continued stability of the local economy and to the happiness and wellbeing of the townspeople. Consistent with the provisions of the Growth Management Legislation, Columbia Falls’ Comprehensive Plan has attempted to recognize the value of land use standards, to incorporate the desires of the community, and to preserve and protect the integrity of Columbia Falls. All of this is done so as to continue to make Columbia Falls a great place to live, work and vacation. The Town of Columbia Falls adopted its last Comprehensive Plan in 2002. -
Plan for Springs
Plan for Springs The population per square mile in Springs is approximately two to six times higher than any other Planning Area1 in East Hampton. Similarly, the number of housing units per square mile in Springs is 1.6 to 2 times higher than all the other Planning Areas. Springs has the lowest number of seasonal homes of all the Planning Areas. Furthermore, Springs contains the largest number of vacant single and separate lots one half acre or less in size of any East Hampton Planning Area. The total potential build-out of Springs is approximately the same as the East Hampton Planning Area, which is approximately three times the area of Springs. Except for Gardiner’s Island, there is no land zoned for A5 Residence and there is little A3 and A2 zoning compared to the other hamlets. Most of the land in Springs was divided during the time immediately following World War II or earlier, into small suburban and urban lots sizes. A few large blocks of undivided land remain today including the woodlands between Red Dirt Road and Accabonac Harbor (including the Town protected Jacob Farm property); the woodlands between Gardiner’s Bay and Springs Fireplace Road (including the Blue Bay Girl Scout Camp); the wetlands and meadows surrounding Accabonac Harbor; the woodlands between Springs Fireplace Rd., Abrahams Path and Accabonac Road.; and a few farm remnants. These areas contribute greatly to the area’s biological diversity by supporting species that would otherwise be absent from such a densely developed residential area. The smaller islands of woodland vegetation located near these large blocks also helps to protect species diversity. -
Contaminant Assessment of Coastal Bald Eagles at Maine Coastal Islands National Wildlife Refuge and Acadia National Park
SPECIAL PROJECT REPORT FY12‐MEFO‐2‐EC Maine Field Office – Ecological Services September 2013 Contaminant Assessment of Coastal Bald Eagles at Maine Coastal Islands National Wildlife Refuge and Acadia National Park Fish and Wildlife Service U.S. Department of the Interior Mission Statement U.S. Fish and Wildlife Service Our mission is working with others to conserve, protect, and enhance the nation’s fish and wildlife and their habitats for the continuing benefit of the American people. Suggested citation: Mierzykowski S.E., L.J. Welch, C.S. Todd, B. Connery and C.R. DeSorbo. 2013. Contaminant assessment of coastal bald eagles at Maine Coastal Islands National Wildlife Refuge and Acadia National Park. USFWS. Spec. Proj. Rep. FY12‐MEFO‐ 2‐EC. Maine Field Office. Orono, ME. 56 pp. U.S. Fish and Wildlife Service Maine Field Office Special Project Report: FY12‐MEFO‐2‐EC Contaminant Assessment of Coastal Bald Eagles at Maine Coastal Islands National Wildlife Refuge and Acadia National Park DEQ ID: 200950001.1 Region 5 ID: FF05E1ME00‐1261‐5N46 (filename: 1261‐5N46_FinalReport.pdf) by Steven E. Mierzykowski and Linda J. Welch, U.S. Fish and Wildlife Service Charles S. Todd, Maine Department of Inland Fisheries and Wildlife Bruce Connery, National Park Service and Christopher R. DeSorbo, Biodiversity Research Institute September 2013 Congressional Districts #1 and #2 1 Executive Summary Environmental contaminants including organochlorine compounds (e.g., polychlorinated biphenyls (PCBs), dichlorodiphenyldichloroethylene (DDE)), polybrominated diphenyl ether (PBDE), and mercury were measured in 16 non‐viable or abandoned bald eagle Haliaeetus leucocephalus eggs and 65 nestling blood samples collected between 2000 and 2012 from the Maine coast. -
State Historic Preservation Office Peter B
North Carolina Department of Cultural Resources State Historic Preservation Office Peter B. Sandbeck, Administrator Beverly Eaves Perdue, Governor Office of Archives and History Linda A. Carlisle, Secretary Division of Historical Resources Jeffrey J. Crow, Deputy Secretary David Brook, Director March 20, 2009 MEMORANDUM To: Mary Pope Furr Historic Architecture Group, HEU, PDEA NC Department of Transportation From: Peter Sandbeck Re: Mid-Cm-rituck Bridge Project, R-2576, Currituck and Dare Counties, CH 94-0809 We are in receipt of the March 11, 2009, letter from Courtney Foley, transmitting her Historic Architectural Resources Survey Report Addendum for the above referenced undertaking. Having reviewed the addendum, we offer the following comments. As noted in the report, the State Historic Preservation Office concurred on April 30, 2008 that the following properties are listed in or eligible for listing in the National Register of Historic Places. Girrituck Beach Light Station (CK1 — NR) Whalehead Club (CK5 — NR) Corolla Historic District (CK97 — DOE) Ellie and Blanton Saunders Decoy Workshop (CK99 — DOE) Dr. W. T. Griggs House (CK 103 — DOE) Currituck Sound Rural Historic District (DOE) Cle-01 09- Daniel Saunders House (DOE) (2,140 101 Samuel McHorney House (DOE) G4-00111 Coinjock Colored School (DOE) Oy_011,, On June 2, 2008, after further discussion with your staff, we also concurred that the Center Chapel A_ME Zion Church is eligible for the National Register. We also concur that the five properties in the subject addendum are eligible for listing in the National Register. They are: (Former) Grandy School (CK 40 — NR 1998) Jarvisburg Colored School (CK 55 — SL 1999) Dexter W. -
Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region. -
A Review of Ice and Tide Observations in the Bay of Fundy
A tlantic Geology 195 A review of ice and tide observations in the Bay of Fundy ConDesplanque1 and David J. Mossman2 127 Harding Avenue, Amherst, Nova Scotia B4H 2A8, Canada departm ent of Physics, Engineering and Geoscience, Mount Allison University, 67 York Street, Sackville, New Brunswick E4L 1E6, Canada Date Received April 27, 1998 Date Accepted December 15,1998 Vigorous quasi-equilibrium conditions characterize interactions between land and sea in macrotidal regions. Ephemeral on the scale of geologic time, estuaries around the Bay of Fundy progressively infill with sediments as eustatic sea level rises, forcing fringing salt marshes to form and reform at successively higher levels. Although closely linked to a regime of tides with large amplitude and strong tidal currents, salt marshes near the Bay of Fundy rarely experience overflow. Built up to a level about 1.2 m lower than the highest astronomical tide, only very large tides are able to cover the marshes with a significant depth of water. Peak tides arrive in sets at periods of 7 months, 4.53 years and 18.03 years. Consequently, for months on end, no tidal flooding of the marshes occurs. Most salt marshes are raised to the level of the average tide of the 18-year cycle. The number of tides that can exceed a certain elevation in any given year depends on whether the three main tide-generating factors peak at the same time. Marigrams constructed for the Shubenacadie and Cornwallis river estuaries, Nova Scotia, illustrate how the estuarine tidal wave is reshaped over its course, to form bores, and varies in its sediment-carrying and erosional capacity as a result of changing water-surface gradients. -
Type Your Frontispiece Or Quote Page Here (If Any)
A LATE MARITIME WOODLAND PESKOTOMUHKATI FISHERY FROM THE MAINLAND QUODDY REGION, SOUTHWESTERN NEW BRUNSWICK, CANADA by W. Jesse Webb B.A. (Hons.), Anthropology, 2009 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Arts in the Graduate Academic Unit of Anthropology Supervisors: Susan E. Blair, Ph.D, Anthropology, Chair Matthew W. Betts, Ph.D, Anthropology Examining Board: Darcy J. Dignam, M.A., Anthropology Richard A. Cunjak, Ph.D., Biology This thesis is accepted by the Dean of Graduate Studies THE UNIVERSITY OF NEW BRUNSWICK April 2018 © William Jesse Webb, 2018 ABSTRACT The nature of precontact Indigenous fisheries and their significance to subsistence economies, seasonal mobility, and diachronic cultural change remain underdeveloped in the archaeology of the Maritime Peninsula, northeastern North America. This thesis presents an analysis of a precontact fishery from BgDs-15, a small shell-bearing site located on the northern mainland of Passamaquoddy Bay, southwestern New Brunswick, Canada. Several hundred bones recovered during the 2004 field excavations and over 3,000 fish remains from midden column and bulk feature samples were examined. Most of these fish bones are attributable to Atlantic tomcod (Microgadus tomcod Walbaum, 1792) and unidentified, tomcod-sized gadids, with some herring (Clupeidae) present. Multiple lines of complementary evidence, including taxonomic composition, relative abundances, skeletal element frequency, seasonality, and the ethnohistoric record were examined to produce a high-resolution analysis of the BgDs-15 fishery and provide insight into ancestral Peskotomuhkati settlement-subsistence strategies during the Late Maritime Woodland period (ca. 1350–550 BP). ii ACKNOWLEDGMENTS The process of developing this thesis has, on the one hand, been the ideal of curiosity-driven academic research and, on the other, a Sisyphean personal struggle. -
US Naval Plans for War with the United Kingdom in the 1890S: a Compromise Between Pragmatism and Theory
US Naval Plans for War with the United Kingdom in the 1890s: A Compromise between Pragmatism and Theory Michael J. Crawford En 1890, Alfred Thayer Mahan a élaboré un plan de guerre en cas d’hostilités envers les Britanniques; pour leur part, les classes du Naval War College des États-Unis ont mis sur pied des plans semblables en 1894 et 1895. Ces plans portaient notamment sur le nord-est des États-Unis et sa frontière avec le Canada. Faisant partie des premiers exercices formels de planification de mesures de guerre de la marine américaine, ces plans représentent un compromis entre la nouvelle vision stratégique de la profession navale américaine et une conception pragmatique des limites de la flotte américaine. In 1890, a small group of US naval professionals drew up plans for war in case of hostilities with the United Kingdom, and a few years later the Naval War College classes of 1894 and 1895, as their Problem in the Art of War, a new annual exercise, elaborated plans for war with the British.1 The plans that resulted from these efforts, 1 Versions of this essay were delivered at “From Enemies to Allies: An International Conference on the War of 1812 and Its Aftermath,” Annapolis, Maryland, 14 June 2013, and the 83rd annual meeting of the Society for Military History, in Ottawa, Ontario, 16 April 2016. The author thanks the commentators and audience at these conferences whose helpful comments contributed to revisions. Ronald Spector, Professors of War: The Naval War College and the Development of the Naval Profession (Newport, R.I.: Naval War College Press, 1977), 71-73; Alfred Thayer Mahan, Contingency Plan of Operations in Case of War with Great Britain, December 1890, in Letters and Papers of Alfred Thayer Mahan, edited by Robert Seager and Doris Maguire, 3 vols. -
Sitios Arqueológicos De Ponce
Sitios Arqueológicos de Ponce RESUMEN ARQUEOLÓGICO DEL MUNICIPIO DE PONCE La Perla del Sur o Ciudad Señorial, como popularmente se le conoce a Ponce, tiene un área de aproximadamente 115 kilómetros cuadrados. Colinda por el oeste con Peñuelas, por el este con Juana Díaz, al noroeste con Adjuntas y Utuado, y al norte con Jayuya. Pertenece al Llano Costanero del Sur y su norte a la Cordillera Central. Ponce cuenta con treinta y un barrios, de los cuales doce componen su zona urbana: Canas Urbano, Machuelo Abajo, Magueyes Urbano, Playa, Portugués Urbano, San Antón, Primero, Segundo, Tercero, Cuarto, Quinto y Sexto, estos últimos seis barrios son parte del casco histórico de Ponce. Por esta zona urbana corren los ríos Bucaná, Portugués, Canas, Pastillo y Matilde. En su zona rural, los barrios que la componen son: Anón, Bucaná, Canas, Capitanejo, Cerrillos, Coto Laurel, Guaraguao, Machuelo Arriba, Magueyes, Maragüez, Marueño, Monte Llanos, Portugués, Quebrada Limón, Real, Sabanetas, San Patricio, Tibes y Vallas. Ponce cuenta con un rico ajuar arquitectónico, que se debe en parte al asentamiento de extranjeros en la época en que se formaba la ciudad y la influencia que aportaron a la construcción de las estructuras del casco urbano. Su arquitectura junto con los yacimientos arqueológicos que se han descubierto en el municipio, son parte del Inventario de Recursos Culturales de Ponce. Esta arquitectura se puede apreciar en las casas que fueron parte de personajes importantes de la historia de Ponce como la Casa Paoli (PO-180), Casa Salazar (PO-182) y Casa Rosaly (PO-183), entre otras. Se puede ver también en las escuelas construidas a principios del siglo XX: Ponce High School (PO-128), Escuela McKinley (PO-131), José Celso Barbosa (PO-129) y la escuela Federico Degetau (PO-130), en sus iglesias, la Iglesia Metodista Unida (PO-126) y la Catedral Nuestra Señora de Guadalupe (PO-127) construida en el siglo XIX.