Distribution and Abundance of Fishes and Invertebrates in North Atlantic Estuaries
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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). -
Maine's Recovery of Recreational Damages Due to Coastal Oil Spills Tanya Baker
The University of Maine DigitalCommons@UMaine Energy & the Environment Margaret Chase Smith Policy Center 2005 Maine's Recovery of Recreational Damages Due to Coastal Oil Spills Tanya Baker Kevin Boyle Deirdre Mageean Neil Pettigrew Jonathan Rubin See next page for additional authors Follow this and additional works at: https://digitalcommons.library.umaine.edu/ mcspc_energy_environ This Report is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Energy & the Environment by an authorized administrator of DigitalCommons@UMaine. For more information, please contact [email protected]. Authors Tanya Baker, Kevin Boyle, Deirdre Mageean, Neil Pettigrew, Jonathan Rubin, and Jennifer Ward Maine’s Recovery of Recreational Damages Due to Coastal Oil Spills August, 2005 Tanya Baker Kevin Boyle Deirdre Mageean Neal Pettigrew Jonathan Rubin Jennifer L. Ward Disclaimer This report has been funded in part by the Maine Oil Spill Advisory Committee (MOSAC). The opinions and conclusions state the views of the authors and do not necessarily reflect the views of MOSAC or any other individual or organization. Acknowledgements We thank the following individuals and organizations for their assistance with the research in this project. All errors and omissions are the responsibility of the authors. Contact Agency / Organization Charlene Daniels Maine Bureau of Parks & Lands Tom DesJardin Maine Bureau of Parks & Lands Natalie Springuel Marine Extension Associate, Maine Sea Grant Amy Kersteen -
Groundwater Aquifers
Water Resources - Town of Wells Comprehensive Plan Update Town of Wells 2021 Comprehensive Plan Update Chapter 3 Update – Natural Resource Policies and Strategies Appendix A Inventory and Analysis Section 2 Update – Water Resources How to Read this Document: The consultants hired to work with the Town of Wells are committed to a transparent planning process and aim to comply with the Town of Wells Chapter 12 Ordinance and other state requirements. To clearly show what has been updated from the 2005 Comprehensive Plan, “tracked changes” was used to show what has been deleted from the 2005 section, new information that has been added, and clarifying questions and comments. New language and data are shown in red. Deleted language is shown with a strikethrough in red. Old tables are shown with a red strikethrough and new tables of information were inserted. Questions and comments are shown in purple. Please note that the analysis sub-section at the end of each updated Appendix section will be reviewed again once all sections are updated. Cross- referencing sections will help the consultants better revise these analysis findings. Data Sources and References 1. Kennebunk-Kennebunkport Wells Water District 2. Beginning with Habitat Guidebook, 2012. (Maine Depart. of Inland Fisheries and Wildlife Beginning with Habitat Program) 3. Aquifers - Source is the Maine Geological Survey. 4. Center for Watershed Protection, 1997. "Impacts of Impervious Cover on Aquatic Systems" Watershed Protection Research Monograph No. 1. https://owl.cwp.org/mdocs-posts/impacts-of-impervious-cover-on-aquatic-systems- 2003/. 5. May, C., R. Horner, J. Karr, B. Mar and E. -
Maine Revised Statutes 38 §468
Presented below are water quality standards that are in effect for Clean Water Act purposes. EPA is posting these standards as a convenience to users and has made a reasonable effort to assure their accuracy. Additionally, EPA has made a reasonable effort to identify parts of the standards that are not approved, disapproved, or are otherwise not in effect for Clean Water Act purposes. Maine Revised Statutes 38 §468 Maine Revised Statutes Title 38: WATERS AND NAVIGATION Chapter 3: PROTECTION AND IMPROVEMENT OF WATERS Subchapter 1: ENVIRONMENTAL PROTECTION BOARD Article 4-A: WATER CLASSIFICATION PROGRAM §468. Classifications of minor drainages All surface waters lying within the boundaries of the State that are in basins having a drainage area less than 100 square miles that are not classified as lakes or ponds are classified in this section. [1989, c. 764, §20 (AMD).] 1. Cumberland County. Those waters draining directly or indirectly into tidal waters of Cumberland County, with the exception of the Androscoggin River Basin, the Presumpscot River Basin, the Royal River Basin and tributaries of the Androscoggin River Estuary and Merrymeeting Bay, entering above the Chops - Class B unless otherwise specified. A. Freeport. (1) Frost Gully Brook - Class A. [1989, c. 764, §21 (RPR).] A-1. Cape Elizabeth. (1) Trout Brook, those waters that form the town boundary with South Portland - Class C. [2009, c. 163, §13 (NEW).] B. Portland. (1) All minor drainages unless otherwise specified - Class C. (2) Stroudwater River from its origin to tidewater, including all tributaries - Class B. [2009, c. 163, §14 (AMD).] C. Scarborough. (1) All minor drainages - Class C unless otherwise specified. -
COASTAL MAINE S If R Nahraflve REPORT Jal^UARY - DECEMBER 1966 COASTAL MINE NATIONAL WILDLIFE REFUGE
7^ COASTAL MAINE S If R NAHRAflVE REPORT JAl^UARY - DECEMBER 1966 COASTAL MINE NATIONAL WILDLIFE REFUGE Newburyport, I-fes sachusett s NARRATIVE REPORT Jan. - Dec. 1966 REFUGE PERSONNEL During this period of initial acquisition, the Coastal Maine National Wildlife Refuge was administered "by personnel of the Parker River National Wildlife Refuge. NARRATIVE REPORT COASTAL MAINE NATIONAL WILDLIFE REFUGE Jan. - Dec. 1966 General On July 26, 1966 the MBCC authorized the acquisition of the three southern-most units of the Coastal Maine National Wildlife Refuge, specifically the Lower Wells Marsh, the Moody Beach Marsh, and the Brave Boat Harbor Marsh. The refuge was officially established on December 16, 1966 when the first land tract totaling l6 acres on the Lower Wells unit was acquired by the Government. The ultimate acreage to be acquired with duck stamp monies will form a National Wildlife Refuge of approximately 4,308 acres. Since no data was taken for this period, no weather information, wildlife population figures, or narrative report forms will be included in this report. However, an initial section on history, not ordinarily included in a narrative report, will be presented. The Coastal Maine National Wildlife Refuge, lying along the south ern coast of Maine will consist of ten units. All are located be tween Kittery Point and Portland, Maine along the Atlantic coast east of U.S. Route 1. The southern-most unit is 35 miles north of the Parker River National Wildlife Refuge and the northern-most unit is 235 miles southwest of the Moosehorn National Wildlife Refuge. The individual units are as follows: 1. -
Morphodynamics of Tidal Inlet Systems in Maine
Maine Geological Survey Studies in Maine Geology: Volume 5 1989 Morphodynamics of Tidal Inlet Systems in Maine 1 2 Duncan M. FitzGeraui, Jonathan M. Lincoln • 3 1 L. Kenneth Fink, Jr. , and Dabney W. Caldwel/ 1Departm ent of Geology Boston University Boston, Massachusetts 02215 2Department of Geological Sciencies Northwestern University Evanston, Illinois 60201 3Department of Geology University of Maine Orono, Maine 04469 ABSTRACT The occurrence of tidal inlets along the coast of Maine is tied closely to the structural geology and glacial history of this region. Most of the inlets are found along the southern arcuate-embayment shoreline where sand sources, consisting of glaciomarine sediments and other glacial deposits, were sufficient to build swash-aligned barriers between pronounced bedrock headlands. Along the peninsula coast of Maine, tidal inlets also occur at the mouths of the Kennebec and Sheepscot Rivers where large quantities of glaciofluvial sands were deposited during deglacia tion. The remainder of the southeastward facing coast was stripped of its preglacial sediment cover by the southerly moving glaciers. The thin tills that were left behind yield little sand and, thus, barriers and inlets are generally absent. Small to large-sized inlets (width= 50-200 m) in Maine are anchored next to bedrock outcrops and are bordered on their opposite sides by sandy spits. Despite the ubiquitous name "river inlet," they normally have little fresh water discharge compared to their salt water tidal prisms. The backbarriers of these inlets are expansive and would produce relatively large tidal prisms if high Spartina marshes had not filled most of the region, leaving little open water area. -
Piscataqua Area Place Names and History
PISCATAQUA AREA PLACE NAMES AND HISTORY by Sylvia Fitts Getchell Adams Point. Formerly known as Matthews Neck, q.v. Agamenticus. York. Originally the name applied by the Indians to what is now called York River. Early settlers used the term for the area about the river. [Used today only for Mount Agamenticus (in York)] Ambler’s Islands. Three small islands off Durham Point near the mouth of Oyster River. Ambush Rock. In Eliot. Where Maj. Chas. Frost was killed by Indians July 4, 1697 (about a mile N. of his garrison on his way home from Church at Great Works). Appledore Island. Named for a Parish in Northam, England. Early named Hog Island. Largest of the Isles of Shoals. Now in ME. [Name Appledore was used 1661-1679 for all the islands when they were briefly a township under Mass. Gov’t.] Arundel. See Cape Porpus. Acbenbedick River. Sometimes called the Little Newichawannock. Now known as Great Works River. First mills (saw mill and stamping mill) in New England using water power built here 1634 by carpenters sent to the colony by Mason. [Leader brothers took over the site (1651) for their mills. See also Great Works.] Ass Brook. Flows from Exeter into Taylor’s River. Atkinson’s Hill. In SW part of Back River District of Dover. Part in Dover, part in Madbury. Also known as Laighton’s Hill (Leighton’s). Back River. Tidal river W of Dover Neck. Back River District. Lands between Back River & Durham line from Cedar Point to Johnson’s Creek Bridge. Part now in Madbury, part in Dover. -
(72 Streams) Ream Town Priority List Reasoning
Maine Department of Environmental Protection February 2019 Nonpoint Source Priority Watersheds List STREAMS Impaired Streams Priority List (72 streams) ream Town Priority List Reasoning Adams Brook Berwick TMDL Arctic Brook Bangor TMDL, Highway Access-related Development Threat Barberry Creek South Portland TMDL Birch Stream Bangor TMDL, MS4 Priority Water Black Brook Windham TMDL Bond Brook Augusta Highway Access-related Development Threat, Development Threat Brackett Brook Palmyra TMDL Burnham Brook Garland TMDL Capehart Brook Bangor TMDL Capisic Brook Portland TMDL, MS4 Priority Water Card Brook Ellsworth TMDL Chamberlain Brook Whitefield TMDL Chandler River including East Pownal TMDL Branch Cold Stream Skowhegan High Growth Area Colley Wright Brook Windham TMDL Coloney Brook Fort Fairfield TMDL Concord Gully Freeport TMDL, Highway Access-related Development Threat, MS4 Priority Water Crooked Brook Corinth TMDL Dole Brook Portland TMDL Duck Brook Arundel Bacteria TMDL Dudley Brook Chapman TMDL Dyer River Newcastle Bacteria TMDL Everett Brook Fort Fairfield TMDL Fish Brook Fairfield TMDL French Stream Exeter TMDL Frost Gully Brook Freeport TMDL Goodall Brook Sanford TMDL Goosefare Brook Saco TMDL, Bacteria TMDL, Highway Access-related Development Threat Hart (Dill) Brook Lewiston TMDL, MS4 Priority Water Halfmoon Stream Thorndike TMDL Hobbs Brook Cumberland TMDL Page 1 of 6 MDEP NPS Priority Watersheds List - STREAMS February 2019 Inkhorn Brook Westbrook TMDL Jock Stream Wales TMDL Kennebunk River Arundel, Bacteria TMDL, MHB Priority -
Global Programme of Action Coalition for the Gulf of Maine (GPAC)
This working paper was prepared for the Secretariat of the Commission for Environmental Cooperation (CEC) and the Global Programme of Action Coalition for the Gulf of Maine (GPAC). The views contained herein do not necessarily reflect the views of the CEC, or governments of Canada, Mexico or the United States of America. Reproduction of this document in whole or in part and in any form for educational or non-profit purposes may be made without special permission from the CEC Secretariat, provided acknowledgement of the source is made. The CEC and the Wells National Estuarine Research Reserve would appreciate receiving a copy of any publication or material that uses this document as a source. Published by the Wells National Estuarine Research Reserve For more information about this report or to obtain additional copies contact: The Wells National Estuarine Research Reserve Research Department 342 Laudholm Farm Road Wells, ME 04090 Tel: (207) 646-1555vFax: (207) 646-2930 E-mail: [email protected] Internet: http://www.wellsreserve.org For information about this or other publications from the CEC, contact: Commission for Environmental Cooperation 393, rue St-Jacques Ouest, bureau 200 Montreal (Quebec) Canada H2Y 1N9 Tel: (514) 350-4300vFax: (514) 350-4314 E-mail: [email protected] Internet: http://www.cec.org Cover Photo Collage Background photo: mid-tide in an unaltered salt marsh (i.e., no tidal restrictions). Foreground photos clockwise from top right: wading birds foraging in a salt marsh panne; volunteer sampling vegetation on high marsh (orange color of grass indicates a fall rather than a summer sample date); road crossing with undersized culvert alters hydrology, functions and values of upstream marsh (photo taken at low tide in early spring); the mummichog (Fundulus heteroclitus) plays an important role in the marsh food web; Phragmites australis (commonly referred to as Phrag), a brackish marsh plant that can become invasive in salt marsh areas where elevations and/or hydrology have been altered. -
Coastal Water Access Priority Areas for Boating and Fishing
Coastal Water Access Priority Areas for Boating and Fishing October 2000 Coastal Water Access Priority Areas for Boating and Fishing October 2000 This report was prepared by Paul Dest of the Maine Coastal Program/State Planning Office and Sue Inches of the Maine Department of Marine Resources. It was printed by the Maine Coastal Program with financial assistance provided by the Coastal Zone Management Act of 1972, as amended, which is administered by the National Oceanic and Atmospheric Administration. For more information, contact the Maine Coastal program/State Planning Office, 38 State House Station Augusta, ME 04333-0038, 207-287-3261 (www.mainecoastalprogram.org) Contents Introduction ............................................................................................................................ 1 Overview of Need.................................................................................................................. 3 Coastal Water Access Survey................................................................................................ 5 Types of Boat Access ...........................................................................................................7 Coastal Water Access Priority Areas ................................................................................... 9 Maps of Priority Areas.........................................................................................................13 Supplemental Recommendations...................................................................................... -
Gateway to Maine I V E Chamber of Commerce 22 Rustlewood Farm R Douglas Memorial Woods
Nature Preserves and Water Access Points of Southern Coastal Maine Kennebunk Plains 1 Bauneg Beg Mountain Conservation Area F ox Fa rm H i ll R Nature Preserves d. and Water Access Points Grover Herrick Preserve Sanford 95 2 of Southern Coastal Maine Wells Barrens Preserve Kennebunk Wire Rd. gatewaytomaineoutside.org F o r Bauneg d Q u Beg in t Pond R Fenderson Wildlife Commons d . N eg Little River ut aq u 109 e Boy 9A Rachel Carson National Wildlife Refuge/Carson Trail t l G e R d r R . e i v a t e 9 r W El Pond Hobbs o r Pond k s R i v Tilton Homestead Wildlife Commons North e Berwick r Diamond Hill Rd. Lake 4 Murdoch Wells Reserve at Laudholm Grant’s Meadow at Beaver Dam Heath Perkinstown Wildlife Commons 4 1 3 Keay Brook Preserve . d R e 5 Negutaquet Conservation Area Wells g Berwick id R 9 h . Webha c d nne e R t R e s iv B er od Boyd Rd. o Old Sanford Rd. 9 W ey hen 9B Finson Rd. C Beaver Dam Pond Tatnic Hills Preserve 95 Gre 6 Tatnic Woods at W o r . B k Rd s ell o 9 rr y u d T R h a 1 T ’s t i n v C o i e rn c r er R Rd. d . 8 Hilton-Winn Preserve 7 Orris Falls Conservation Area Kenyon Hill Preserve 9 11 Beach Plum Farm Knights 10 Ogunquit C Pond hi 4 ck s Youth Enrichment Center at Hilton-Winn Farm B Kimball Farm North ro 236 o k Desrochers Memorial Forest 14 Mount Agamenticus Conservation Region 12 Payeur Preserve . -
Prehistoric Archaeology and Evidence of Coastal Subsidence on the Coast of Maine
Maine Geological Survey Neotectonics of Maine 1989 Prehistoric Archaeology and Evidence of Coastal Subsidence on the Coast of Maine David Sanger and Douglas C. Kellogg Department of Anthropology and Institute for Quarternary Studies University of Maine Orono, Maine 04469 ABSTRACT Analysis of archaeological site locations can be used to help assess localized rates of sea-level rise provided certain conditions are met, and assumptions about the relationship between sea level and archaeological land surfaces are accurate. Provided it can be shown that marine-adapted peoples lived on contemporary shorelines, and that a particular stretch of shoreline exhibited equal potential for habitation, then differential preservation by age of site may be indicative of differential land erosion rates. This model is used to discuss the relative rates of sea-level rise for the Maine coast, divided into four shore zones. For each of the zones the archaeological evidence is reviewed together with an assessment of site loss due to sea-level rise and coastal erosion. It is concluded that the oldest coastal sites are found in the Penobscot Bay area, where 5000 year old sites are still relatively intact. The shortest record occurs in Passamaquoddy Bay where sites are no older than 2500 years. Erosion of sites, and perhaps rate of submergence, is clearly greater in Passamaquoddy Bay than elsewhere in the study area. In addition to documentation ofdifferential site preservation, archaeology can contribute to sea-level rise studies through the analysis of changing habitats resulting from drowned estuaries. Research on the oyster shell middens along the Damariscotta River indicates just over 1 meter of sea-level rise over the past 2500 years.