2019 VRMP Annual Report
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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 -
West Branch Penobscot Fishing Report
West Branch Penobscot Fishing Report Tsarism and authorial Cal blacktops, but Tomlin interminably laving her Bodoni. Converted Christopher coups dumbstruck.horridly. Vasiform Joseph wambled no spindrift exhausts clerically after Elton temps meritoriously, quite Read across for example of the future uses and whitefish, west branch of things like anglers There certainly are patterns, year to year, day to day, but your fishing plans always need to be flexible this time of year. Maine has an equal vote with other states on the ASMFC Striped Bass Board, which meets next Tuesday, Feb. New fishing destinations in your area our Guiding! Continue reading the results are in full swing and feeding fish are looking. Atlantic Salmon fry have been stocked from the shores of Bowlin Camps Lodge each year. East Outlet dam is just as as! Of which flow into Indian Pond reach Season GEAR Species Length Limit Total Bag. Anyone ever fish the East and West Branches of Kennebec. And they provide a great fish for families to target. No sign of the first big flush of young of the year alewives moving down river, but we are due any day now. Good technique and local knowledge may be your ticket to catching trout. Salmon, smelt, shad, and alewife were historically of high value to the commercial fishing industry. As the tide dropped out of this bay there was one pack of striped bass that packed themselves so tightly together and roamed making tight circles as they went. Food, extra waterproof layers, and hot drinks are always excellent choices. John watershed including the Northwest, Southwest, and Baker branches, and the Little and Big Black Rivers. -
Penobscot Rivershed with Licensed Dischargers and Critical Salmon
0# North West Branch St John T11 R15 WELS T11 R17 WELS T11 R16 WELS T11 R14 WELS T11 R13 WELS T11 R12 WELS T11 R11 WELS T11 R10 WELS T11 R9 WELS T11 R8 WELS Aroostook River Oxbow Smith Farm DamXW St John River T11 R7 WELS Garfield Plt T11 R4 WELS Chapman Ashland Machias River Stream Carry Brook Chemquasabamticook Stream Squa Pan Stream XW Daaquam River XW Whitney Bk Dam Mars Hill Squa Pan Dam Burntland Stream DamXW Westfield Prestile Stream Presque Isle Stream FRESH WAY, INC Allagash River South Branch Machias River Big Ten Twp T10 R16 WELS T10 R15 WELS T10 R14 WELS T10 R13 WELS T10 R12 WELS T10 R11 WELS T10 R10 WELS T10 R9 WELS T10 R8 WELS 0# MARS HILL UTILITY DISTRICT T10 R3 WELS Water District Resevoir Dam T10 R7 WELS T10 R6 WELS Masardis Squapan Twp XW Mars Hill DamXW Mule Brook Penobscot RiverYosungs Lakeh DamXWed0# Southwest Branch St John Blackwater River West Branch Presque Isle Strea Allagash River North Branch Blackwater River East Branch Presque Isle Strea Blaine Churchill Lake DamXW Southwest Branch St John E Twp XW Robinson Dam Prestile Stream S Otter Brook L Saint Croix Stream Cox Patent E with Licensed Dischargers and W Snare Brook T9 R8 WELS 8 T9 R17 WELS T9 R16 WELS T9 R15 WELS T9 R14 WELS 1 T9 R12 WELS T9 R11 WELS T9 R10 WELS T9 R9 WELS Mooseleuk Stream Oxbow Plt R T9 R13 WELS Houlton Brook T9 R7 WELS Aroostook River T9 R4 WELS T9 R3 WELS 9 Chandler Stream Bridgewater T T9 R5 WELS TD R2 WELS Baker Branch Critical UmScolcus Stream lmon Habitat Overlay South Branch Russell Brook Aikens Brook West Branch Umcolcus Steam LaPomkeag Stream West Branch Umcolcus Stream Tie Camp Brook Soper Brook Beaver Brook Munsungan Stream S L T8 R18 WELS T8 R17 WELS T8 R16 WELS T8 R15 WELS T8 R14 WELS Eagle Lake Twp T8 R10 WELS East Branch Howe Brook E Soper Mountain Twp T8 R11 WELS T8 R9 WELS T8 R8 WELS Bloody Brook Saint Croix Stream North Branch Meduxnekeag River W 9 Turner Brook Allagash Stream Millinocket Stream T8 R7 WELS T8 R6 WELS T8 R5 WELS Saint Croix Twp T8 R3 WELS 1 Monticello R Desolation Brook 8 St Francis Brook TC R2 WELS MONTICELLO HOUSING CORP. -
Saco River Saco & Biddeford, Maine
Environmental Assessment Finding of No Significant Impact, and Section 404(b)(1) Evaluation for Maintenance Dredging DRAFT Saco River Saco & Biddeford, Maine US ARMY CORPS OF ENGINEERS New England District March 2016 Draft Environmental Assessment: Saco River FNP DRAFT ENVIRONMENTAL ASSESSMENT FINDING OF NO SIGNIFICANT IMPACT Section 404(b)(1) Evaluation Saco River Saco & Biddeford, Maine FEDERAL NAVIGATION PROJECT MAINTENANCE DREDGING March 2016 New England District U.S. Army Corps of Engineers 696 Virginia Rd Concord, Massachusetts 01742-2751 Table of Contents 1.0 INTRODUCTION ........................................................................................... 1 2.0 PROJECT HISTORY, NEED, AND AUTHORITY .......................................... 1 3.0 PROPOSED PROJECT DESCRIPTION ....................................................... 3 4.0 ALTERNATIVES ............................................................................................ 6 4.1 No Action Alternative ..................................................................................... 6 4.2 Maintaining Channel at Authorized Dimensions............................................. 6 4.3 Alternative Dredging Methods ........................................................................ 6 4.3.1 Hydraulic Cutterhead Dredge....................................................................... 7 4.3.2 Hopper Dredge ........................................................................................... 7 4.3.3 Mechanical Dredge .................................................................................... -
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). -
Geologic Site of the Month: Why Is Sebago Lake So Deep?
Why is Sebago Lake so deep? Maine Geological Survey Maine Geologic Facts and Localities February, 1999 Why is Sebago Lake so deep? 43° 51‘ 13.36“ N, 70° 33‘ 43.98“ W Text by Robert A. Johnston Maine Geological Survey, Department of Agriculture, Conservation & Forestry 1 Why is Sebago Lake so deep? Maine Geological Survey Introduction Modern geophysical equipment allows geologists to investigate previously unmapped environments, including ocean and lake floors. Recent geophysical research studied the types, composition, areal extent, and thickness of sediments on the bottom of Sebago Lake in southwestern Maine. Geologists used side- scan sonar and seismic reflection profiling to map the bottom of the lake. Approximately 58 percent of the lake bottom was imaged with side-scan sonar and over 60 miles of seismic reflection profiles were collected. This web site will discuss the findings of the seismic reflection profiling. Maine Geological Survey, Department of Agriculture, Conservation & Forestry 2 Why is Sebago Lake so deep? Maine Geological Survey Physiographic setting Sebago Lake, although second in surface area to Moosehead Lake, is Maine's deepest lake. With a water depth of 316 feet, its deepest part is 49 feet below sea level! Sebago Lake is located in southwestern Maine 20 miles northwest of Portland and 50 miles southeast of the White Mountains. It lies along the transition between the Central Highlands and the Coastal Lowlands physiographic regions of New England (Figure 1). The abrupt change in landscape can be seen in panoramic views from several vantage points near Sebago Lake. Denny, 1982 Denny, Maine Geological Survey From From Figure 1. -
Hazardous Beach-System Development in Maine and Some Outcomes of the Sand Dune Rules Julia M
The University of Maine DigitalCommons@UMaine Electronic Theses and Dissertations Fogler Library 12-2003 Hazardous Beach-System Development in Maine and Some Outcomes of the Sand Dune Rules Julia M. Knisel Follow this and additional works at: http://digitalcommons.library.umaine.edu/etd Part of the Terrestrial and Aquatic Ecology Commons Recommended Citation Knisel, Julia M., "Hazardous Beach-System Development in Maine and Some Outcomes of the Sand Dune Rules" (2003). Electronic Theses and Dissertations. 154. http://digitalcommons.library.umaine.edu/etd/154 This Open-Access Thesis is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of DigitalCommons@UMaine. HAZARDOUS BEACH-SYSTEM DEVELOPMENT IN MAINE AND SOME OUTCOMES OF THE SAND DUNE RULES BY Julia M. Knisel B.S. The Pennsylvania State University A THESIS Submitted in Partial Fullillment of the Requirements for the Degree of Master of Science (in Marine Policy) The Graduate School The University of Maine December, 2003 Advisory Committee: Joseph T. Kelley, Professor of Marine Geology, Advisor Mary Kate Beard-Tisdale, Professor of Spatial Information Science and Engineering Deirdre Mageean, Professor of Resource Economics and Policy Daniel F. Belknap, Professor of Geology HAZARDOUS BEACH-SYSTEM DEVELOPMENT IN MAINE AND SOME OUTCOMES OF THE SAND DUNE RULES By Julia M. Knisel Thesis Advisor: Dr. Joseph T. Kelley An Abstract of the Thesis Presented in Partial Fulfillment of the Requirements for the Degree of Master of Science (in Marine Policy) December, 2003 Damages to coastal property in southwestern Maine occur primarily as a result of storms, flooding, and erosion. -
ST. CROIX RIVER UPDATE Joint Tribal Council of the Passamaquoddy Tribe Passes St
FALL 2012/ Winter 2013 THE NEWSLETTER OF MAINE RIVERS ST. CROIX RIVER UPDATE Joint Tribal Council of the Passamaquoddy Tribe passes St. Croix River Alewife Resolution Citing the vital linkages that sea-run alewives create in the food chain of the St. Croix River, Passamaquoddy Bay and the Bay of Fundy, members of the Joint Tribal Council of the Passamaquoddy Tribe voted unanimously to pass a resolution that calls for reopening the St. Croix Rivers for alewives. !e resolution states that sea-run alewife are a vital link in the food chain of the St. Croix River that sustained the Passamaquoddy for thousands of years, “without which we may not have survived.” !e Joint Tribal Council resolution supports the June 14, 2012 Passamaquoddy Chief’s Declaration of a State of Emergency within the St. Croix River, and calls for overturning Maine’s 1995 law that blocks alewives from the St. Croix. In early June 2012 members of the Schoodic Riverkeepers advanced the Passamaquoddy river restoration e"ort with a 100-mile sacred run up the St. Croix River, a run that mirrored the annual trek of native alewives. !e route extended from Pleasant Point, near Eastport, to Mud Lake Stream, a 4,000-year-old ancestral #shing site for the Passamaquoddy at the head of Spednic Lake. Maine Rivers has been working for nearly a decade on advocacy e"orts to reopen the St. Croix River and applauds this recent decision of the Joint Tribal Council. Clockwise from top: Runners and tribal elders at the halfway point of the 2012 the deer antler baton. -
Scarborough Beach Scarborough Higgins Beach Scarborough
Higgins Beach Scarborough Beach Scarborough Scarborough The variations in the profiles along Higgins Beach may relate to the three different beach types found at each of the profile locations. HI1 is located at the base of a large rip-rap seawall; this wall is “active” at high stages of the tide – that is, tidal water and wave activity is in contact with the seawall. This is reflected in the less berm development and general low variability of the mean profiles, especially as compared with HI2. HI2, though it starts at a seawall, is located at a portion of the beach that has more sediment, and undergoes more seasonal changes, and is not active during high tide phases. HI3 is heavily influenced by the spit end of Higgins Beach, which terminates at the Spurwink River ebb-tidal delta; this area undergoes large changes At SC2 annual variability is greater than at SC1. From Seasonal variability at SC2 shows the expected due to sediment movement and availability 1999 to 2000 and 2005 to 2006 about 1 meter of influence of the summer berm on the upper profile with at the spit and ebb-tidal delta. sediment was lost and the dune appears to have greater variability than in winter. The outer profile has receded. From 2006 to 2007 the mean profile lowered greater winter variability consistent with seasonal about a meter - some of which may be due to the 2007 sandbar migration. Patriots’ Day Storm. Data at Scarborough Beach indicate that the beach undergoes typical seasonal changes and that the beach is generally stable. -
Bedrock Valleys of the New England Coast As Related to Fluctuations of Sea Level
Bedrock Valleys of the New England Coast as Related to Fluctuations of Sea Level By JOSEPH E. UPSON and CHARLES W. SPENCER SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 454-M Depths to bedrock in coastal valleys of New England, and nature of sedimentary Jill resulting from sea-level fluctuations in Pleistocene and Recent time UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1964 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication, as follows: Upson, Joseph Edwin, 1910- Bedrock valleys of the New England coast as related to fluctuations of sea level, by Joseph E. Upson and Charles W. Spencer. Washington, U.S. Govt. Print. Off., 1964. iv, 42 p. illus., maps, diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 454-M) Shorter contributions to general geology. Bibliography: p. 39-41. (Continued on next card) Upson, Joseph Edwin, 1910- Bedrock valleys of the New England coast as related to fluctuations of sea level. 1964. (Card 2) l.Geology, Stratigraphic Pleistocene. 2.Geology, Stratigraphic Recent. S.Geology New England. I.Spencer, Charles Winthrop, 1930-joint author. ILTitle. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Configuration and depth of bedrock valleys, etc. Con. Page Abstract.__________________________________________ Ml Buried valleys of the Boston area. _ _______________ -
Nonpoint Source Priority Watersheds List MARINE WATERS
Maine Department of Environmental Protection February 2019 Nonpoint Source Priority Watersheds List MARINE WATERS Impaired* Marine Waters Priority List (34 marine waters) Marine Water Area/Town Priority List Reasoning Anthoine Creek & Cove South Portland Negative Water Quality Indicators (FOCB) Broad Cove Cushing DMR/NPS Threat Bunganuc Creek Brunswick CBEP Priority Water Cape Neddick River York MS4 Priority Water Churches Rock So. Thomaston DMR/NPS Threat Egypt Bay Hancock/Franklin DMR/NPS Threat Goosefare Bay Kennebunkport MHB Priority Water, MS4 Priority Water Harpswell Cove Brunswick CBEP Priority Water Harraseeket River Freeport DMR/NPS Threat Hutchins Cove Bagaduce River / DMR/NPS Threat Northern Bay (Penobscot) Hyler Cove Cushing DMR/NPS Threat Kennebunk River Kennebunk MHB Priority Water Little River and Bay Freeport CBEP Priority Water Littlefield Cove Bagaduce River / DMR/NPS Threat Northern Bay (Penobscot) Maquoit Bay Brunswick CBEP Priority Water Martin Cove Lamoine DMR/NPS Threat Medomak River Estuary Waldoboro DMR/NPS Threat Mill Cove South Portland Negative Water Quality Indicators Mill Pond/Parker Head Phippsburg DMR/NPS Threat Mussell Cove Falmouth CBEP Priority Water, DMR/NPS Threat North Fogg Point Freeport CBEP Priority Water Northeast Creek Bar Harbor DMR/NPS Threat Oakhurst Island Harpswell CBEP Priority Water Ogunquit River Estuary Ogunquit MHB Priority Water, DMR/NPS Threat Pemaquid River Bristol DMR/NPS Threat Salt Pond Blue Hill/Sedgwick DMR/NPS Threat, MERI Scarborough River Estuary Scarborough DMR/NPS Threat Spinney Creek Eliot MS4 Priority Water, Negative Water Quality Indicators Spruce Creek Kittery MS4 Priority Water, Negative Water Quality Indicators Page 1 of 2 MDEP NPS Priority Watersheds List – MARINE WATERS February 2019 Marine Water Area/Town Priority List Reasoning Spurwink River Scarborough MHB Priority Water, DMR/NPS Threat St. -
Buxton Map 7.Pdf
An Approach to Conserving Maine's Natural LEGEND Space for Plants, Animals, and People k This mavepr depicts all wetlands shown on National Wetland Inventory (NWI) maps, but o Ri ro www..begiinniingwiitthhabiittatt..org B B categorized them based on a subset of wetland functions. This map and its depiction r 25 J e a " o k tl ) o oft wetland features neither substitute for nor eliminate the need to perform on-the- n i s c h ro e h nson B L si ground wetland delineation and functional assessment. In no way shall use of this map Supplemo entary Map 7 J Br diminish or alter the regulatory protection that all wetlands are accorded under oo h k c an pplicable State and Federal laws. For more information about wetlands characterization, a H r contact Elizabeth Hertz at the Maine Department of Conservation (207-287-8061, Wetlands Characterization S B I N [email protected]). D O N T h A k t Buxton T X o r o o S U r 35 B N This map is non-regulatory and is intended for planning purposes only )" B The Wetlands Characterization model is a planning tool intended to help identify likely s la wetland functions associated with significant wetland resources and adjacent uplands. g Brook u in Using GIS analysis, this map provides basic information regarding what ecological o rt D a services various wetlands are likely to provide. These ecological services, each of which M has associated economic benefits, include: floodflow control, sediment retention, finfish habitat, and/or shellfish habitat.