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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. -
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. _ _______________ -
2019 VRMP Annual Report
Volunteer River Monitoring Program 2019 Data Report VRMP March 2021 Contact: Kristin Feindel Phone: (207) 215-3461 MAINE DEPARTMENT OF ENVIRONMENTAL PROTECTION 17 State House Station Augusta, Maine 04330-0017 www.maine.gov/dep/index.html Maine Department of Environmental Protection VRMP 2019 Data Report Acknowledgements & Credits VRMP Staff Team (Maine DEP) Mary Ellen Dennis (retired 2019) Kristin Feindel Katie Goodwin (Americorps/Maine Conservation Corps) Tayelor Gosselin (Americorps/Maine Conservation Corps) Volunteer Coordinators and Data Managers Becky Secrest & Ferg Lea - Androscoggin River Watershed Council Ed Friedman - Friends of Merrymeeting Bay Greg Bither - Friends of Scarborough Marsh Toby Jacobs, Fred Dillion & Ben Libby - Presumpscot Regional Land Trust Bob Kennedy - Rockport Conservation Commission Jacob Aman - Wells National Estuarine Research Reserve Theo & Wes Pratt - Weskeag River Photograph Credits Photographs courtesy of Jeff Varricchione, Cynthia Montanez, Rich Obrey, Bob Kennedy, Mary Ellen Dennis and Kristin Feindel. Page 2 of 28 Maine Department of Environmental Protection VRMP 2019 Data Report Acknowledgements & Credits The VRMP would like to recognize the dedication and hard work of all the coordinators and volunteers who participated in the program. 2019 VRMP Volunteers Androscoggin River Watershed Council Androscoggin River (Upper River) Jane Andrews Tyler Ritter Janna Botka Peter Roberts Carol Gowing Becky Secrest Bob Kleckner Jeff Stern Friends of Merrymeeting Bay Androscoggin River (Lower River) Rebecca -
Directions to the Friends of Casco Bay Office 43 Slocum Drive South Portland, Maine 04106 (207) 799-8574
Directions to the Friends of Casco Bay Office 43 Slocum Drive South Portland, Maine 04106 (207) 799-8574 Our office is on the campus of Southern Maine Community College (SMCC) near Spring Point Lighthouse. If using GPS, use SMCC’s address 2 Fort RD, South Portland, ME 04106. From I-95 & I-295 . Take the exit 45 toward I-295/US-1/ME-114/Maine Mall Rd/Payne Rd . Merge onto Maine Turnpike Approach . Take the exit onto I-295 N toward Portland . Take exit 4 toward Casco Bay Br/Portland/Waterfront . Continue onto Veterans Memorial Bridge . Continue onto Fore River Pkwy . Continue onto W Commercial St . Turn left to merge onto Casco Bay Bridge / Route 77 S . Continue onto Broadway (straight through the lights at the end of the bridge) . Follow Broadway all the way to its dead end at Benjamin W. Pickett Street (about 1.3 miles) . Turn right onto Benjamin W. Pickett Street . Take the 2nd left onto Slocum Drive (it looks like you’re entering a parking lot in front of a big dormitory; if you get to the stop sign at Fort Road, you missed Slocum) . Our office is a small one-story building at 43 Slocum, toward the end of the road on the left. Look for a small blue sign that reads “Friends of Casco Bay” in front of our building. From the South via Route 1 . Follow Route 1 N to South Portland . At the intersection with Broadway, turn right onto Broadway. Continue for 1.9 miles. Just past the fire station, turn right to stay on Broadway/77 S. -
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. -
An Act to Change the Classification of Certain Waters of the State Be It Enacted by the People of the State of Maine As Follows: Sec
PUBLIC Law, Chapter 163 LD 330, item 1, 124th Maine State Legislature An Act To Change the Classification of Certain Waters of the State PLEASE NOTE: Legislative Information cannot perform research, provide legal advice, or interpret Maine law. For legal assistance, please contact a qualified attorney. An Act To Change the Classification of Certain Waters of the State Be it enacted by the People of the State of Maine as follows: Sec. 1. 38 MRSA §467, sub-§1, ¶C, as amended by PL 2003, c. 317, §2, is further amended to read: C. Androscoggin River, Upper Drainage; that portion within the State lying above the river's most upstream crossing of the Maine-New Hampshire boundary - Class A unless otherwise specified. (1) Cupsuptic River and its tributaries - Class AA. (2) Kennebago River and its tributaries except for the impoundment of the dam at Kennebago Falls - Class AA. (3) Rapid River, from a point located 1,000 feet downstream of Middle Dam to its confluence with Umbagog Lake - Class AA. (4) Magalloway River and tributaries above Aziscohos Lake in Lynchton Township, Parmachenee Township and Bowmantown Township - Class AA. (4-A) Abbott Brook and its tributaries in Lincoln Plantation - Class AA. (5) Little Magalloway River and tributaries in Parmachenee Township and Bowmantown Township - Class AA. (6) Long Pond Stream in Rangeley - Class AA. (7) Dodge Pond Stream in Rangeley - Class AA. Sec. 2. 38 MRSA §467, sub-§1, ¶D, as amended by PL 2003, c. 317, §3, is further amended to read: D. Androscoggin River, minor tributaries - Class B unless otherwise specified. -
The Dirty History of Portland Harbor
Reprinted from a 1994 publication The Dirty History of Portland Harbor hen scientists began looking closely at the sediments and at W the bottom of Casco Bay beginning in the early 1980s, they confronted a pollution puzzle. Sediments taken from various locations throughout the Bay, and especially in Portland Harbor, held a wide variety of potentially toxic chemicals. Until we know more about how these heavy metals, pesticides and other compounds affect marine life, it’s hard to know what lasting impact the pollution in Casco Bay may have. But it was decided that the more we know about where those pollutants came from, the better chances we will have in preventing future problems. The Casco Bay Estuary Project (now Casco Bay Early industry was limited by natural energy sources, like this tidal mill at Estuary Partnership) commissioned environmental Stroudwater. (courtesy: Sullivan Train & Photo) historian Edward Hawes to do some detective work, hoping that he could turn up some puzzle pieces from the Casco Bay. Lead, cadmium and mercury concentrations were watersheds that feed the Bay. The industrial legacy he found comparatively high in Back Cove, as were lead and mercury was a surprise to almost anyone who thinks they know the in the inner Fore River. Lead was also relatively high in the Portland area. Presumpscot River estuary. Additional metals — nickel, silver, arsenic, chromium A Pollution Problem and zinc — were evident in lesser concentrations. This widespread contamination was a little mystifying. In this age hen investigators began sampling Casco Bay’s of environmental regulation, how could so much pollution sediments in the 1980s, levels of pollution have landed in the Bay? W were found that merited additional attention. -
A Dirty History of Casco Bay
University of Southern Maine USM Digital Commons Graphics, Maps, and Posters Casco Bay Estuary Partnership (CBEP) 2010 Portland Waterfront Sign: A Dirty History of Casco Bay Casco Bay Estuary Partnership Montgomery Designs Follow this and additional works at: https://digitalcommons.usm.maine.edu/cbep-graphics-maps-posters Recommended Citation Casco Bay Estuary Partnership and Montgomery Designs, "Portland Waterfront Sign: A Dirty History of Casco Bay" (2010). Graphics, Maps, and Posters. 6. https://digitalcommons.usm.maine.edu/cbep-graphics-maps-posters/6 This Book is brought to you for free and open access by the Casco Bay Estuary Partnership (CBEP) at USM Digital Commons. It has been accepted for inclusion in Graphics, Maps, and Posters by an authorized administrator of USM Digital Commons. For more information, please contact [email protected]. Custom H ouse 1 You are standing in the SAME PLACE SHOWN in 1 C this 1900 photo. Can you imagine the sounds and smells on OAL the day this picture was taken? RIGHT: This 1914 map shows R & M x the Randall & McAllister Coal Wharf located here, COAL A Dirty History of Casco Bay other industrial shipping piers, and railroad tracks. YOU BacK COVE C By the summer of 1866, Portland was the OAL ARE HERE 3 Randall & largest commercial shipping port in the nation. G The coal dust from the harbor M ALT WHA F R aine Steamship Co. Industries sprouted up everywhere. Much of their “ ANKLIN WHArf 2 PAINT FacTORIES like this one on Munjoy Hill (1899) used Eastern Steamship Co. was so thick we had to sweep up the M lead and mercury. -
Forest Avenue and Stevens Avenue Portland, Maine Historic Context
Forest Avenue and Stevens Avenue Portland, Maine Historic Context Scott T. Hanson Sutherland Conservation & Consulting August 2015 General context Development of Colonial Falmouth European settlement of the area that became the city of Portland, Maine, began with English settlers establishing homes on the islands of Casco Bay and on the peninsula known as Casco Neck in the early seventeenth century. As in much of Maine, early settlers were attracted by abundant natural resources, specifically fish and trees. Also like other early settlement efforts, those at Casco Bay and Casco Neck were tenuous and fitful, as British and French conflicts in Europe extended across the Atlantic to New England and both the French and their Native American allies frequently sought to limit British territorial claims in the lands between Massachusetts and Canada. Permanent settlement did not come to the area until the early eighteenth century and complete security against attacks from French and Native forces did not come until the fall of Quebec to the British in 1759. Until this historic event opened the interior to settlement in a significant way, the town on Casco Neck, named Falmouth, was primarily focused on the sea with minimal contact with the interior. Falmouth developed as a compact village in the vicinity of present day India Street. As it expanded, it grew primar- ily to the west along what would become Fore, Middle, and Congress streets. A second village developed at Stroudwater, several miles up the Fore River. Roads to the interior were limited and used primarily to move logs to the coast for sawing or use as ship’s masts. -
4 Year Bridge Investment Plan : Includes $160M from "An Act to Keep Bridges Safe"
Maine State Library Digital Maine Transportation Documents Transportation 4-8-2008 4 Year Bridge Investment Plan : Includes $160M from "An Act to Keep Bridges Safe" Maine Department of Transportation Follow this and additional works at: https://digitalmaine.com/mdot_docs Recommended Citation Maine Department of Transportation, "4 Year Bridge Investment Plan : Includes $160M from "An Act to Keep Bridges Safe"" (2008). Transportation Documents. 127. https://digitalmaine.com/mdot_docs/127 This Text is brought to you for free and open access by the Transportation at Digital Maine. It has been accepted for inclusion in Transportation Documents by an authorized administrator of Digital Maine. For more information, please contact [email protected]. 4 Year Bridge Investment Plan Includes $160M from "An Act to Keep Bridges Safe" April 2008 ESTIMATED BRIDGE # TOWN/S BRIDGE NAME ROAD FEATURE UNDER COST 5657 Abbot Brown Black Road Brown Brook $300,000 3300 Acton - Newfield Balch Mills Acton Bridge Road Little Ossippee River $425,000 1271 Alfred Nutter's Back Road Littlefield River $450,000 5100 Alton Tannery Tannery Road Dead Stream $350,000 6247 Amherst West Branch Route 9 W. Branch 1/2 Mile Pond Brook $435,000 3726 Anson Ice House Route 201A Gilbert Brook $760,000 3948 Arundel Hutchins Log Cabin Road (SA 5) Goffs Mill Brook $100,000 0077 Auburn Royal River Old Danville Road Royal River $600,000 1465 Augusta I-95/New Belgrade SB I-95 SB Routes 8 - 11 & 27 $2,500,000 2719 Augusta Riggs Routes 100 & 201 Riggs Brook $2,000,000 3078 Augusta Father -
Shells of Maine: a Catalogue of the Land, Fresh-Water and Marine Mollusca of Maine
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Maine The University of Maine DigitalCommons@UMaine Maine History Documents Special Collections 1908 Shells of Maine: a Catalogue of the Land, Fresh-water and Marine Mollusca of Maine Norman Wallace Lermond Follow this and additional works at: https://digitalcommons.library.umaine.edu/mainehistory Part of the History Commons This Monograph is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Maine History Documents by an authorized administrator of DigitalCommons@UMaine. For more information, please contact [email protected]. Pamp 353 c. 2 Vickery SHELLS OF MAINE Norman Wallace Lermond Thomaston SHELLS OF MAINE. A Catalogue of the Land, Fresh-water and Marine Mollusca of Maine, by Norman Wallace Lermond. INTRODUCTORY. No general list of Maine shells—including land, fresh-water and marine species—-has been published since 1843, when Dr. J. W. Mighels’ list was printed in the Boston Journal of Natural History. Dr. Mighels may be called the “Pioneer” conchologist of Maine. By profession a physician, in his leisure hours he was a most enthusiastic collector and student of all forms of molluscan life. Enthusiasm such as his was “contagious” and he soon had gathered about him a little band of active students and collectors. Of these Capt. Walden of the U. S. Revenue Cutter “Morris” was dredging in deep water and exploring the eastern shores and among the islands, and “by his zeal procured many rare species;” Dr. -
Do the Rivers, Streams and Estuaries in the Casco Bay Watershed Meet State Water= Ouality Standards?
Do the Rivers, Streams and Estuaries in the Casco Bay Watershed Meet State Water= Ouality Standards? I Answer--: Overall, y~~, waters in the Casco Bay watershed meet State water quality standards. ere are some areas that do not meet State water quality standards. Which Waters Vo Not Meet Water Quality Standards? The table on page 42 lists the waters in the Casco Bay watershed that do not meet water quality stan dards and are required to have an improvement plan produced (known as a Total Maximum Daily Load or TMDL) by the Maine DEP. The Presumpscot River and Highland Lake (Duck Pond) in Windham, Falmouth and Westbrook also do not reach water quality standards but have completed TMDL plans. The New Meadows Lake and the Upper New Mead ows estuary do not meet water quality standards. Studies are being conducted with the coordination of the CBEP to determine if the source of the prob Why Are State Water Quality Standards lem is from flow restrictions or nonpoint pollution Important? sources. The map on the opposite page illustrates the waters that do not meet state standards, including ater quality standards help the State man the Presumpscot, Highland Lake (Duck Pond) and the age its waters. The State of Maine enacted New Meadows. W laws to comply with the Federal Clean Water Act of 1972 to manage its waters for specified "designated uses" such as swimming, fishing, boating, What Are the Trends? habitat for aquatic life, drinking water supply, naviga Overall the water quality in the watershed is good and tion, agriculture, hydropower, industrial process and has remained so over time.