Dioxin Monitoring Program
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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. -
Surface Water Supply of the United States 1915 Part I
DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director WATER-SUPPLY PAPER 401 SURFACE WATER SUPPLY OF THE UNITED STATES 1915 PART I. NORTH ATLANTIC SIOPE DRAINAGE BASINS NATHAN C. GROVES, Chief Hydraulic Engineer C. H. PIERCE, C. C. COVERT, and G. C. STEVENS. District Engineers Prepared in cooperation with the States of MAIXE, VERMONT, MASSACHUSETTS, and NEW YORK WASHINGTON GOVERNMENT FEINTING OFFICE 1917 DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Water-Supply Paper 401 SURFACE WATER SUPPLY OF THE UNITED STATES 1915 PART I. NORTH ATLANTIC SLOPE DRAINAGE BASINS NATHAN C. GROVER, Chief Hydraulic Engineer C. H. PIERCE, C. C. COVERT; and G. C. STEVENS, District Engineers Geological Prepared in cooperation with the States MAINE, VERMONT, MASSACHUSETTS^! N«\f Yd] WASHINGTON GOVERNMENT PRINTING OFFICE 1917 ADDITIONAL COPIES OF THIS PUBLICATION MAY BE PROCURED FROM THE SUPEBINTENDENT OF DOCUMENTS GOVERNMENT FEINTING OFFICE "WASHINGTON, D. C. AT 15 CENTS PER COPY V CONTENTS. Authorization and scope of work........................................... 7 Definition of terms....................................................... 8 Convenient equivalents.................................................... 9 Explanation of data...................................................... 11 Accuracy of field data and computed results................................ 12 Cooperation.............................................................. -
Introduction
Breaching of the Edwards Dam, July 1, 1999 The Kennebec River is the third largest river in Maine consolidating the flows from many large lakes in north-central Maine, then flowing south through agricultural areas and small towns and cities of the central part of the state to merge with the Androscoggin River at Merrymeeting Bay. Introduction Geography The Kennebec River originates at Moosehead Lake flowing 145 miles to Merrymeeting Bay where it joins the Androscoggin River, then to the Atlantic Ocean at Phippsburg and Georgetown. The upper Kennebec flows from Moosehead Lake about 4 miles before reaching Indian Pond, the first of many impoundments. Flowing out of Indian Pond through Harris Dam, a major hydroelectric station, its passes through the Kennebec gorge then runs south draining into Wyman Lake, and through Wyman Dam, another large hydroelectric impoundment. From there it passes through urban and industrial areas of Madison, Skowhegan, Waterville-Winslow, and, with the Biomonitoring Retrospective 78 Maine DEPLW1999-26 Dec. 1999 removal of the Edwards Dam in Augusta in July, 1999, the Kennebec head of tide now occurs between Augusta and Sidney. The river eventually empties into Merrymeeting Bay in Richmond. Six major tributaries enter the river: the Moose River is the major tributary of Moosehead Lake, Dead River, Sandy River, Sebasticook River, Messalonskee Stream and Cobbosseecontee Stream. The basin covers approximately 5,893 square miles with approximately 3,850 miles of rivers and streams. Basin Summary Statistics Biomonitoring -
Surface Water Supply of the United States 1914 Part I
U. 8, GFOL SURVEY H . HYO. RESEARCH ki A ^CITY, IOWA DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director WATER-SUPPLY PAPER 381 SURFACE WATER SUPPLY OF THE UNITED STATES 1914 PART I. NORTH ATLANTIC SLOPE DRAINAGE BASINS NATHAN C. GROVER, Chief Hydraulic Engineer C. C. COVERT, C. H. PIERCE, and G. C. STEVENS, District Engineers Prepared in cooperation with the States of MAINE, VERMONT, MASSACHUSETTS, and NEW YORK WASHINGTON GOVERNMENT PRINTING OFFICE 1916 u. A «tUU SURVEY C/0 IOWA INST. HYD, RESEARCH DEPARTMENT OF THE INTERIOR G1TY' I(WA FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Water-Supply Paper 381 SDRFACE WATER SUPPLY OF THE UNITED STATES^*1 Geolosicil Survey, 1014 Box /r^] |_ PART I. NORTH ATLMTIC SLOPE ' NATHAN C. GROVER, Chief Hydraulic Engineer C. C. COVERT, C. H. PIERCE, and G. C. STEVENS, District Engineers Prepared in cooperation with the States of MAINE, VERMONT, MASSACHUSETTS, and NEW YORK WASHINGTON GOVERNMENT PRINTING OFFICE 1916 ADDITIONAL COPIES OF THIS PUBLICATION MAY BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 15 CENTS PER COPY CONTENTS. Page. Authorization and scope of work........................................... 7 Definition of terms......................................................... 8 Convenient equivalents.................................................... 9 Explanation of data........................................................ 11 Accuracy -
Maine Revised Statutes 38 §467
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 §467 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 §467. Classification of major river basins All surface waters lying within the boundaries of the State that are in river basins having a drainage area greater than 100 square miles that are not classified as lakes or ponds are classified in this section. [1989, c. 764, §2 (AMD).] 1. Androscoggin River Basin. A. Androscoggin River, main stem, including all impoundments. (1) From the Maine-New Hampshire boundary to its confluence with the Ellis River - Class B. (2) From its confluence with the Ellis River to a line formed by the extension of the Bath-Brunswick boundary across Merrymeeting Bay in a northwesterly direction - Class C. [1989, c. 890, Pt. A, §40 (AFF); 1989, c. 890, Pt. B, §68 (AMD); MRSA T. 38, §467, sub-§1, ¶ A (AMD).] B. Little Androscoggin River Drainage. (1) Little Androscoggin River, main stem. (a) From the outlet of Bryant Pond to the Maine Central Railroad bridge in South Paris - Class A. (b) From the Maine Central Railroad bridge in South Paris to its confluence with the Androscoggin River - Class C. -
Atlantic Salmon EFH the Proposed EFH Designation for Atlantic Salmon
Atlantic salmon EFH The proposed EFH designation for Atlantic salmon includes the rivers, estuaries, and bays that are listed in Table 31 and shown in Map 105, which exhibit the environmental conditions defined in the text descriptions. Smaller tributaries not shown on the map are also EFH for one or more life stage as long as they conform to the proposed habitat descriptions. All EFH river systems form a direct connection to the sea, but EFH would not include portions of rivers above naturally occurring barriers to upstream migration or land-locked lakes and ponds. The oceanic component of EFH is to a distance of three miles from the mouth of each river. The new designation includes six new drainage systems not included in the original list of 26 rivers that were designated in 1998. All of them are in the Maine coastal sub-region (Chandler, Indian, Pleasant, St. George, Medomak, and Pemaquid rivers). All told, 30 river systems in nine New England sub-regions are designated for Atlantic salmon EFH. The new map includes a more continuous series of bays and areas adjacent to river mouths that are within three miles of the coast. Designated EFH in Long Island Sound has been reduced to small areas where the Connecticut and Pawcatuck Rivers empty into the sound, rather than taking up the entire sound. Also, there are a number of improvements in the text descriptions which make the habitat requirements for each life stage more specific and applicable to three separate juvenile life stages (fry, parr, and smolts). Text descriptions: Essential fish habitat for Atlantic salmon (Salmo salar) is designated as the rivers, estuaries, and bays that are listed in Table 31 and shown in Map 105. -
THE FLOODS of MARCH 1936 Part 1
If you do jno*-Be <l this report after it has served your purpose, please return it to the Geolocical -"" Survey, using the official mailing label at the end UNITED STATES DEPARTMENT OF THE INTERIOR THE FLOODS OF MARCH 1936 Part 1. NEW ENGLAND RIVERS Prepared in cooperation withihe FEDERAL EMERGENCY ADMINISTRATION OF PUBLIC WORKS GEOLOGICAL SURVEY WATER-SUPPLY PAPER 798 UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Water-Supply Paper 798 THS^LOODS OF MARCH 1936 PART 1. NEW ENGLAND RIVERS NATHAN C. GROVER Chief Hydraulic Engineer Prepared in cooperation with the FEDERAL EMERGENCY ADMINISTRATION OF PUBLIC WORKS UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1937 For sale by the Superintendent of Documents, Washington, D. C. Price 70 cents CONTENTS Page Abstract............................................................. 1 Introduction......................................................... 2 Authorization........................................................ 5 Administration and personnel......................................... 5 Acknowledgments...................................................... 6 General features of the storms....................................... 7 Floods of the New England rivers....................................o 12 Meteorologic and hydrologic conditions............................... 25 Precipitation records............................................ 25 General f>!-................................................... 25 Distr<* '-utlon -
All About Maine Alewives
ALL ABOUT MAINE ALEWIVES... Alewives are anadromous (sea-run) fish that spend the majority of What are their life at sea but return to freshwater to spawn. Alewives have alewives? co-evolved and co-existed with other native fish and wildlife in Maine’s streams, rivers, ponds and lakes for thousands of years. Alewives are members of the herring family; their close cousins are shad and blueback herring. Alewives have slender bodies, and they normally grow to 10 – 11” in length, and weigh about half a pound. Repeat spawners can be as large as 14” and weigh a pound or more. Alewives are grayish green on their back, and silvery on their sides and belly. They’ve got a single black spot just behind their eye, and their tails are forked. The bad news is that many Mainers have never seen an alewife run Were alewives because Maine’s historically thriving alewife population has originally present plummeted during the last two centuries. Dams, pollution and overfishing have taken their toll. Southern Maine’s Alewife Brook, in our lakes? for example, no longer has alewives. But historians and scientists tell us that prior to Europeans settling this region, there was probably not a stream flowing out of a lake or pond anywhere in the Gulf of Maine that didn’t have an annual alewife migration, unless it was blocked by impassable waterfalls. One early historian said, “There can have been hardly an accessible pond in the whole State they did not visit.” Of all the Produced by: migratory fish that came up Maine Dept. -
4.0 Kennebec River Basin
4.0 Kennebec River Basin 4.1 Watershed Description The Kennebec River Basin occupies approximately 5,900 square miles of southwestern Maine. The headwaters of the river basin originate in the Appalachian Mountains on the international border with Canada. The upper two-thirds of the basin above Waterville are hilly and mountainous and the lower third of the basin has the gentle topography representative of a coastal drainage area. Major communities in this basin include Bingham, Anson, Madison, Norridgewock, Skowhegan, Waterville, Winslow, Augusta, Hallowell, and Gardiner. The Kennebec River originates at Moosehead Lake and flows south approximately 145 miles to Merrymeeting Bay. Table 27 presents the major tributaries to the Kennebec River along with their respective contributing area. The Kennebec River joins the Androscoggin River in Merrymeeting Bay before exiting to the ocean at Fort Popham. The Kennebec River is influenced by tidal process as far as Augusta, 25 miles above Abagadassett Point. Figure 10 illustrates the locations of major tributaries located within the Kennebec River basin. 4-1 October 2007 C:\Documents and Settings\swiding\Desktop\Maine River Basin Report _Final4.doc Table 27. Kennebec River, Tributaries from Upstream to Downstream and Drainage Areas Contributing Area Tributary (square miles) South Branch Moose River 70 Moose River (2) above Attean Pond 180 Moose River (3) at Long Pond 310 Brassua Lake 160 Moosehead Lake 550 Kennebec River (2) above The Forks 320 North Branch Dead River 200 South Branch Dead River 150 Flagstaff Lake 170 Dead River 360 Kennebec River (4) at Wyman Dam 160 Austin Stream 90 Kennebec River (6) 110 Carrabassett River 400 Sandy River 590 Kennebec River at Waterville Dam 410 Sebasticook River at Pittsfield 320 Sebasticook River (3) at Burnham 270 Sebasticook River (4) at Winslow 370 Messalonskee Stream 210 Cobbosseecontee Stream 220 Kennebec River at Merrymeeting Bay 320 Total 5,930 4-2 October 2007 C:\Documents and Settings\swiding\Desktop\Maine River Basin Report _Final4.doc Figure 10. -
Kennebec River Management Plan Diadromous Resources Amendment Prepared By
Kennebec River Management Plan Diadromous Resources Amendment Prepared By: Maine Department of Marine Resources December 2020* * Photo Credit: Sandy River holding pool with Atlantic salmon trucked by MDMR above four hydroelectric dams. Contents 1. Introduction ................................................................................................................................. 1 1.1 Purpose .................................................................................................................................. 1 1.2 Scope ..................................................................................................................................... 2 1.3 MDMR role ........................................................................................................................... 2 1.4 Existing Comprehensive Plans ............................................................................................. 3 1.5 Background of diadromous fish in the Kennebec River watershed ...................................... 5 2. Description of the watershed ...................................................................................................... 5 2.1 Land use and development.................................................................................................... 6 2.2 Hydropower projects ............................................................................................................. 6 2.3 Status of fish passage at hydropower projects ..................................................................... -
Diadromous Fish Habitat Protection and Restoration Projects in Maine
DIADROMOUS FISH HABITAT PROTECTION AND RESTORATION PROJECTS IN MAINE Supported by USFWS GULF OF MAINE COASTAL PROGRAM in cooperation with other federal, state and NGO partners, 1998 – 2007 Photo credit: S. Lary, USFWS Photo credit: D. W at ts Photo credit: USFWS This briefing includes projects supported by the following USFWS-linked funding sources: NFWF Maine Habitat Restoration Partnership Grant NFWF Maine Atlantic Salmon Conservation Fund USFWS Region 5 Challenge Grant Program funds USFWS Region 5 Ecological Services funds Recovery Land Acquisition Grants North American Wetland Conservation Act Grants National Coastal Wetland Conservation Act Grants 1124 funding to support Gulf of Maine Coastal Program staff 1124 funding to provide project funds compiled by USFWS Gulf of Maine Coastal Program July, 2007 TAKE-HOME MESSAGES: 1. Gulf of Maine Coastal Program (GOMCP) is collaborating with conservation partners to implement cooperative conservation projects and to protect and restore priority diadromous fish habitat in Maine. • GOMCP completes all of its diadromous fish protection and restoration work by working in close coordination with many conservation partners (i.e. state agencies, NGOs, private landowners, corporate interests). • Two of six permanent employees at GOMCP direct significant time toward protecting riparian habitat and improving river connectivity for all 12 species of native diadromous fish. One employee offers technical expertise in GIS, fluvial geomorphology and riverine functions on priority Atlantic salmon rivers, while the other employee offers technical expertise in diadromous fisheries ecology and coastal riverine restoration for Maine’s diverse diadromous fish assemblage. Both biologists are well-known and respected amongst all of the key diadromous fish partners statewide; they both work with diverse partners to ensure effective prioritization and coordination of diadromous fish habitat efforts. -
Chapter 3 Existing Environment
Chapter 3 Dan Salas, Cardno JFNew Dan Salas, Cardno View of Carlton Pond Existing Environment • Introduction • Physical Landscape • Refuge and WPA Biological Resources • Cultural Landscape Setting and Land Use History • Socioeconomic Environment • Refuge and WPA Administration • Refuge and WPA Public Use • Archaeological and Historical Resources Introduction Introduction This chapter describes the current and historic physical, biological, and socioeconomic landscape of Carlton Pond WPA and the three units comprising Sunkhaze Meadows NWR (Sunkhaze Meadows, Benton, and Sandy Stream Units). Included are descriptions of the physical landscape, the regional context and its history, and the refuge environment, including its history, current administration, programs, and specific refuge resources. The 11,484-acre Sunkhaze Meadows Unit is located in the town of Milford, Penobscot County, approximately 14 miles northeast of Bangor, Maine. The refuge is about 3 miles east of the Penobscot River and roughly bounded on the west by Dudley Brook, on the south and east by County Road, and on the north and east by Stud Mill Road. Sunkhaze Stream bisects the refuge along a northeast to southwest orientation and, along with its six tributaries, creates a diversity of wetland communities. The bogs and stream wetlands, adjacent uplands and associated transition zones, provide important habitat for many wildlife species. The wetland complex consists primarily of wet meadows, shrub thickets, cedar swamps, extensive red and silver maple floodplain forests and open freshwater stream habitats, along with plant communities associated with peatlands, such as shrub heaths and cedar and spruce bogs. The 334-acre Benton Unit is in the town of Benton, Kennebec County, about 5 miles northeast of Waterville, Maine.