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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. -
Total Phosphorus Loads for Selected Tributaries to Sebago Lake, Maine
science for a changing world Total Phosphorus Loads for Selected Tributaries to Sebago Lake, Maine Water-Resources Investigations Report 01-4003 V Prepared in cooperation with the Portland Water District U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior U.S. Geological Survey By Glenn A. Hodgkins Water-Resources Investigations Report 01-4003 Prepared in cooperation with the Portland Water District Augusta, Maine 2001 U.S. DEPARTMENT OF THE INTERIOR GALE A. NORTON, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director The use of firm, trade, and brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Government. For additional information write to: Copies of this report can be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Branch of Information Services 26 Ganneston Dr. Box 25286, Federal Center Augusta, ME 04330 Denver, CO 80225 http://me.water.usgs.gov CONTENTS Abstract.................................................................................... 1 Introduction................................................................................. 2 Description of the study area.................................................................... 2 Data collection and analysis .................................................................... 2 Data-collection networks in the Sebago Lake Basin.......................................... 2 Adequacy of current stream-gaging network .............................................. -
The Maine Lake Science Center – Now a Reality by Peter Lowell LEA Board Votes to Buy the Science Center Property
Testing Buoy on Highland Lake The 2014 Milfoil Bill LEA Education Programs The buoy is large and yellow with solar More than a decade after the original are designed to create opportunities for panels mounted on it. There are two “Milfoil Bill” passed the Maine Legislature, life-long learning through place-based round mooring buoys near it that are a new bill will significantly modify a curricula offered in partnership with attached to anchors. long-standing funding inequity. local public schools and community Page 4 By Peter Lowell, Page 8 members. Page 10 Summer 2014 Free LEA Lake News The Maine Lake Science Center – Now a Reality by Peter Lowell LEA Board Votes to Buy the Science Center Property As kids growing up on Highland Lake, we never saw algae clouds that look like green cotton candy. The sand and gravel of the lake bottom was always clean and the rocks were clear of sediment. Unfortunately, these simple indicators of water quality decline are now widespread. Our work over 43 years has led us to conclude that Maine lakes are degrading because of continued watershed development and decline is being accelerated by climate change. All of our lakes have changed over the past few decades, and their future is certainly in doubt. For six years, LEA has studied the status of lake science and visiting lake centers around the country to learn their methods and establish relationships. LEA conducts more lake testing than anyone in Maine, and we feel that no one adequately understands the “tipping points” that lead to a decline in water quality. -
Maine Lakes Report 2012
Maine Lakes Report 2012 Dear Friends of Maine Lakes, This report on the health of Maine lakes reflects the effort of more than 1,000 volunteer citizen scientists who monitored several hundred lake basins throughout the State in 2012. Many of them have been doing so continuously for decades, and a few have been involved for most of the 42 years since the Maine Legislature officially authorized volunteer lake monitoring. Their work is a strong testimony to the level of public commitment in Maine to our clear, clean lakes, and it is probably not coincidental that our lakes have remained as healthy as they have under the watch of these individuals. The Maine Volunteer Lake Monitoring Program (VLMP) is believed to be the longest-standing statewide citizen lake monitoring program in America, having been formed at about the time of the passage of the historic Federal Clean Water Act. The Mission of the Maine Volunteer Lake Monitoring Program is to help protect Maine lakes through widespread citizen participation in the gathering and dissemination of credible scientific information pertaining to lake health. The VLMP trains, certifies and provides technical support to hundreds of volunteers who monitor a wide range of indicators of water quality, assess watershed health and function, and screen lakes for invasive aquatic plants and animals. In addition to being the primary source of lake data in the State of Maine, VLMP volunteers benefit their local lakes by playing key stewardship and leadership roles in their communities. Our primary partners are the Maine Department of Environmental Protection (DEP) and the US Environmental Protection Agency, which provide a wide range of financial, technical and management support to the program. -
Sebago-Lake-Watershed-Newsletter
SUMMER 2017 Photo by John Stetson Portland Water District ● 225 Douglass Street ● Portland, Maine 04104-3553 ● 207.761.8310 ● www.pwd.org Recreational Believe It Water What’s Making Roger Lakes Like 3 Forecast 4or Not! 6 Watch 7 Waves? 8 Mosley 8 Less Lawn Silent Spring Comes to Sebago Lake By Paul Hunt You have likely heard of “Silent Sebago Lake. Fortunately for all of us that enjoy the lake today, the Maine Department of Inland Spring”, the 1962 book written in Fisheries and Wildlife (Maine IF&W) took Maine by Rachel Carson which decisive action to address the problem. alerted readers to the impact of is dramatic period in Sebago Lake’s history was described in a report entitled pesticides on the environment. “ e Sebago Lake Study.” Written by Stuart Maybe you have read it. DeRoche, a sheries biologist from Gorham, it was published in 1976 by the Maine IF&W According to Wikipedia: (then known as the Department of Fish and “Silent Spring was met with erce Game). According to the report, in 1957 the opposition by chemical companies, but average 4 year-old salmon in Sebago Lake it spurred a reversal in national pesticide was 19 inches long and weighed about 2 Stuart DeRoche stocking salmon in the Crooked River policy, led to a nationwide ban on DDT pounds. By 1963 there were far fewer salmon (Dichlorodiphenyltrichloroethane) being caught and the typical 4 year-old was concludes that the DDT wiped out the for agricultural uses, and inspired an just 15 inches long and weighed less than a minnows which starved out the salmon. -
Success on the Songo River and Brandy Pond!
Sediment Research MLSC - What’s up? Loons and Lead The mystery factor is climate change. The question is when LEA will move its While attacks from larger animals and Storms are intensifying and ice-out is offices to the new building. That will not boat strikes are sudden and obvious, lead coming much earlier, giving algae a longer happen since our year-round staff rely on poisoning is an insidious and deadly growing season. As we re-vamp our lake our Main Street building and its many killer. There are countless stories of loons protection standards ... Page 2 facilities. Page 5 dying... Page 10 Winter 2016 Free LEA Lake News Success on the Songo River and Brandy Pond! By Christian Oren After eleven summers of hard work, LEA is declaring victory in the battle against milfoil in the Songo River and Brandy Pond. When the project was first begun, huge patches of milfoil as big as football fields choked the entire length of the Songo. Now, boaters can pass through the river without ever seeing a single stalck of the plant. Never before has such a large and extensive invasive aquatic plant infestation been brought under control in the history of the State of Maine. The dozen or so infestations in Brandy Pond were also persistent, but seem to have been quelled by years of repeated harvesting. We declared victory on the Songo for two main reasons. First, the density of milfoil on the entire length of the river was much lower than we had seen in previous years. Even at the height of the growing season, there was only one plant for every 100 feet of shoreline, or less. -
Cumulative Impacts to Environmental Conditions on the Presumpscot River and Its Shorelands
Cumulative Impacts to Environmental Conditions on the Presumpscot River and its Shorelands (DRAFT -- As distributed at the June 2002 Public Meetings) Title Page pictures Deleted due to large memory size. See separate file Prepared by the Presumpscot River Plan Steering Committee With Technical Assistance Provided by Land and Water Associates Hallowell, Maine And Funding and Assistance Provided by Casco Bay Estuary Project June 11, 2002 ADDENDUM April 18, 2003 Note on the Scope of Analysis for this Cumulative Impacts Report: The geographic scope of this analysis of cumulative impacts is the Presumpscot River from its outlet at Sebago Lake, including its tributaries and adjacent corridor lands, to and including the Casco Bay Estuary. This report addresses the impacts of the regulation of flows out of Sebago Lake at the Eel Weir Dam on the river and Casco Bay Estuary, since the flow regime on the river is almost entirely controlled by management of the Eel Weir Dam, and the Presumpscot River is the largest source of freshwater to Casco Bay. However, it does not include or address issues related to Sebago Lake levels. Comments received at the June 2002 public information meetings raised concerns about the impacts of flow regulation at the Eel Weir Dam on Sebago lake shorelands and wetlands. While it is acknowledged that the regulation of flows at the Eel Weir Dam has impacts not only on the river and estuary but also on Sebago Lake, these impacts are not addressed in this report, and there are no recommendations included in the report to change operations at the Eel Weir Dam. -
LEA Lake News
Special Issue! Diving In: A Deeper Understanding and Paddle Battle II Saturday July 7th Appreciation of Lakes Starting on Page 8 Details on Page 5 Summer 2018 Free LEA Lake News A Publication of the Lakes Environmental Association, Protecting Lakes Since 1970 Lake Courses Oer Something for Everyone Are you looking for a way to build your resume? Modern Environmental Monitoring is a three day Do you have an interest in micro-electronics? Do course that will cover the principles of freshwa- you want to learn how lakes work rst hand? is ter science both in the classroom and in the eld. summer, a series of fun and educational courses Days one and two cover on-the-lake sampling, is being oered at the Maine Lake Science Center including the basics of water column charac- in Bridgton. terization using everything from a Secchi disk We are hosting three new courses geared to- to advanced multi-parameter probes. Students ward students in college or late high school and will learn how to take surface and deep water interested adults looking to enhance their un- samples for nutrient and algae analysis and get derstanding of natural systems and scientic an overview of the lab work that nishes the pro- methodology. Participants in these courses will cess. Day three is a comprehensive overview of enjoy learning about environmental science in rivers and streams. is course will be taught a relaxed classroom environment and then get by LEA’s Sta Researcher, Education Director, a chance to collect samples in the eld and run Teacher/Naturalist, and Research Director. -
Maine Geological Survey Bottom Sediments of Sebago Lake
Bottom Sediments of Sebago Lake Maine Geological Survey Maine Geologic Facts and Localities September, 2001 Bottom Sediments of Sebago Lake 43° 51‘ 13.44“ N, 70° 33‘ 43.54“ W Text by Robert A. Johnston Maine Geological Survey, Department of Agriculture, Conservation & Forestry 1 Bottom Sediments of Sebago Lake 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 (Figure 1). This web site will discuss the findings of the side-scan sonar profiling. The seismic reflection profiles are described in the web page entitled Why is Sebago Lake so deep? Maine Geological Survey Figure by R. A. Johnston A. by R. Figure Figure 1. Side-scan sonar coverage map of Sebago Lake, Maine. Yellow areas show regions covered. Maine Geological Survey, Department of Agriculture, Conservation & Forestry 2 Bottom Sediments of Sebago Lake Maine Geological Survey Physiographic Setting and Methods Sebago Lake is located in southwestern Maine, 20 miles northwest of Portland. As Maine's second largest lake, it covers 47.5 square miles and is second in surface area to Moosehead Lake's 117 square miles. Sebago Lake is Maine's deepest lake with a water depth of 316 feet. -
Sebago Lake Milfoil Action Cooperative by Nate Whalen
Photo by Rich Antinarelli Photo by Rich SPRING 2016 Portland Water District ● 225 Douglass Street ● Portland, Maine 04104-3553 ● 207.761.8310 ● www.pwd.org 10 Year Rain Events What’s Making Watershed Sebago 3 Anniversary 4Gardens 5 2016 6 Waves? 7 Prioritization 8 Lakescaping Sebago Lake Milfoil Action Cooperative By Nate Whalen Can milfoil be eliminated in Sebago Lake? With the cooperation of homeowners, local town governments, and lake protection groups such as the Maine Volunteer Lake Monitoring Program (VLMP), the Lakes Environmental Association, Raymond Waterways Protective Association, the Portland Top: LEA crew deploying a benthic barrier. Photo: LEA Water District (PWD) and the Maine Left: Variable leaf milfoil. Photo: LEA Department of Environmental Protection working together as the Sebago Lake Milfoil Action fragments are set adrift to possibly infest areas. Infestations can affect Cooperative, the answer is new lakeshore areas. recreational opportunities such as it’s possible. The good news is that much of the swimming and fishing, and can have Variable leaf milfoil was first lake shore around Sebago Lake is rocky a negative impact on property values discovered in Sebago Lake in the and sandy, which is not ideal for aquatic for homeowners. early 1970s. This aquatic plant is vegetation. Milfoil prefers back water In 2002, the Maine Department not native to New England and coves that have soft mucky bottoms. The of Environmental Protection (DEP) is considered “invasive” because bad news is that some of these backwater it lacks natural enemies to keep places on Sebago Lake are already Continued on page 2 its growth in check, allowing it to heavily infested out-compete other aquatic plants. -
Water Budget for Sebago Lake, Maine, 1996-99
U.S DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Water Budget for Sebago Lake, Maine, 1996-99 Water-Resources Investigations Report 01-4235 U.S. GEOLOGICAL SURVEY Prepared in cooperation with the PORTLAND WATER DISTRICT, TOWN OF WINDHAM, MAINE DEPARTMENT OF HEALTH, AND MAINE GEOLOGICAL SURVEY U.S. GEOLOGICAL SURVEY Cover Photograph. Gage at Sebago Lake (photo courtesy Robert Johnston). Water Budget for Sebago Lake, Maine, 1996-99 By Robert W. Dudley, Glenn A. Hodgkins, and Joseph P. Nielsen U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 01-4235 In cooperation with the PORTLAND WATER DISTRICT TOWN OF WINDHAM MAINE DEPARTMENT OF HEALTH MAINE GEOLOGICAL SURVEY Augusta, Maine 2001 U.S. DEPARTMENT OF THE INTERIOR GALE A. NORTON, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director The use of firm, trade, and brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Government. For additional information write to: Copies of this report can be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Branch of Information Services 26 Ganneston Drive Box 25286 Augusta, ME 04330 Federal Center http://me.water.usgs.gov Denver, CO 80225 CONTENTS Abstract . .. .. .1 Introduction . .. .. .1 Purpose and Scope . .. .. 4 Description of the Study Area . .4 . Physiography and Geology . .4 . Climate . .. .. .5 Surface-Water Hydrology . .5 . Data Compilation and Analysis. .. .. 5 Precipitation . .. .. .5 Evaporation . .. .. .5 Surface-Water Inflows and Outflows . .6 . Withdrawals and Lake Storage . .9 . Water Budget for Sebago Lake . .. .. 10 Uncertainties of Water-Budget Components. .14 . Precipitation . .. .. .14 Surface-Water Inflows. -
Eel Weir FERC Environmental Assessment Supplement 2014
Document Accession #: 20140408-3044 Filed Date: 04/08/2014 UNITED STATES OF AMERICA FEDERAL ENERGY REGULATORY COMMISSION S.D. Warren Company Project No. 2984-042 NOTICE OF AVAILABILITY OF SUPPLEMENTAL ENVIRONMENTAL ASSESSMENT (April 8, 2014) In accordance with the National Environmental Policy Act of 1969 and the Federal Energy Regulatory Commission’s (Commission) regulations, 18 CFR Part 380 (Order No. 486, 52 FR 47897), the Office of Energy Projects has reviewed the application for new license for the Eel Weir Project, located at the outlet of Sebago Lake on the Presumpscot River, in Cumberland County, Maine, and has prepared a supplemental Environmental Assessment (supplemental EA) for the project. The supplemental EA contains the staff’s analysis of the potential environmental impacts of the project and concludes that licensing the project, with appropriate environmental protective measures, would not constitute a major federal action that would significantly affect the quality of the human environment. A copy of the supplemental EA is available for review at the Commission in the Public Reference Room or may be viewed on the Commission’s website at http://www.ferc.gov using the “eLibrary” link. Enter the docket number excluding the last three digits in the docket number field to access the document. For assistance, contact FERC Online Support at [email protected], at (866) 208-3676 (toll free), or (202) 502-8659 (TTY). You may also register online at http://www.ferc.gov/docs-filing/esubscription.asp to be notified via e-mail of new filings and issuances related to this or other pending projects. For assistance, contact FERC Online Support.