Rapid River Fishery Managment
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NH Trout Stocking - April 2018
NH Trout Stocking - April 2018 Town WaterBody 3/26‐3/30 4/02‐4/06 4/9‐4/13 4/16‐4/20 4/23‐4/27 4/30‐5/04 ACWORTH COLD RIVER 111 ALBANY IONA LAKE 1 ALLENSTOWN ARCHERY POND 1 ALLENSTOWN BEAR BROOK 1 ALLENSTOWN CATAMOUNT POND 1 ALSTEAD COLD RIVER 1 ALSTEAD NEWELL POND 1 ALSTEAD WARREN LAKE 1 ALTON BEAVER BROOK 1 ALTON COFFIN BROOK 1 ALTON HURD BROOK 1 ALTON WATSON BROOK 1 ALTON WEST ALTON BROOK 1 AMHERST SOUHEGAN RIVER 11 ANDOVER BLACKWATER RIVER 11 ANDOVER HIGHLAND LAKE 11 ANDOVER HOPKINS POND 11 ANTRIM WILLARD POND 1 AUBURN MASSABESIC LAKE 1 1 1 1 BARNSTEAD SUNCOOK LAKE 1 BARRINGTON ISINGLASS RIVER 1 BARRINGTON STONEHOUSE POND 1 BARTLETT THORNE POND 1 BELMONT POUT POND 1 BELMONT TIOGA RIVER 1 BELMONT WHITCHER BROOK 1 BENNINGTON WHITTEMORE LAKE 11 BENTON OLIVERIAN POND 1 BERLIN ANDROSCOGGIN RIVER 11 BRENTWOOD EXETER RIVER 1 1 BRISTOL DANFORTH BROOK 11 BRISTOL NEWFOUND LAKE 1 BRISTOL NEWFOUND RIVER 11 BRISTOL PEMIGEWASSET RIVER 11 BRISTOL SMITH RIVER 11 BROOKFIELD CHURCHILL BROOK 1 BROOKFIELD PIKE BROOK 1 BROOKLINE NISSITISSIT RIVER 11 CAMBRIDGE ANDROSCOGGIN RIVER 1 CAMPTON BOG POND 1 CAMPTON PERCH POND 11 CANAAN CANAAN STREET LAKE 11 CANAAN INDIAN RIVER 11 NH Trout Stocking - April 2018 Town WaterBody 3/26‐3/30 4/02‐4/06 4/9‐4/13 4/16‐4/20 4/23‐4/27 4/30‐5/04 CANAAN MASCOMA RIVER, UPPER 11 CANDIA TOWER HILL POND 1 CANTERBURY SPEEDWAY POND 1 CARROLL AMMONOOSUC RIVER 1 CARROLL SACO LAKE 1 CENTER HARBOR WINONA LAKE 1 CHATHAM BASIN POND 1 CHATHAM LOWER KIMBALL POND 1 CHESTER EXETER RIVER 1 CHESTERFIELD SPOFFORD LAKE 1 CHICHESTER SANBORN BROOK -
Section 5-2 Androscoggin River (Friends of Merrymeeting Bay)
Maine Department of Environmental Protection Androscoggin River (FOMB) 2018 Summary Data Report Section 5-2 Androscoggin River (Friends of Merrymeeting Bay) Androscoggin River The Androscoggin River is the third largest river in the state of Maine. It has a length of 177 miles and drainage area of 3,450 square miles (2,730 sq. mi. in Maine).1 The Androscoggin River’s headwaters are Umbagog Lake in Maine/New Hampshire. From there it flows into New Hampshire and then back into Maine through the towns of Gilead and Bethel. It continues flowing through the towns and cities of Rumford, Mexico, Dixfield, Jay, Livermore Falls, Lewiston, Auburn, Lisbon, Lisbon Falls, Durham, Brunswick, and Topsham where it joins the Kennebec River at Merrymeeting Bay. The Androscoggin River has a long history of industrial and municipal use over the last 200 years.1 Beginning in the early 1800s, many dams were constructed for mills, primarily in the lower part of the river. By the late 1800s, many textile and lumber mills were in operation, mostly from Lewiston to Brunswick. Pulp and paper mills that are still in operation today were established in the late 1800s in New Hampshire, Rumford, and Jay. Beginning in the late 1920s, Central Maine Power built hydroelectric dams that impounded much of the river from Lewiston to Livermore Falls. Some of these uses continue today. “Along its course to the sea, the river is repeatedly dammed. It receives discharges from industrial and municipal sources, as well as polluted runoff from a variety of sources.”2 Specific problems include mill discharges, combined sewer overflows (CSOs), dam impacts (28 dams exist), and historical sediment toxins. -
Fishery Interim Summary Report Series No. 08-04: Rapid River Fishery Management
FISHERY INTERIM SUMMARY REPORT SERIES NO. 08-04 RAPID RIVER FISHERY MANAGEMENT By David P. Boucher Maine Department of Inland Fisheries and Wildlife Division of Fisheries and Hatcheries Augusta, Maine December 2008 Job F-014 Interim Summary Report No. 4 (2007) Rapid River Fishery Management SUMMARY The Rapid River, located in Township C and Upton in Oxford County, has long been noted for its outstanding brook trout population. Brook trout in the Rapid River are sustained entirely by natural reproduction and support a popular, heavily utilized sport fishery of regional and statewide significance. Landlocked salmon are also present and provide an important ancillary fishery. During the 1980's, smallmouth bass were illegally introduced into Umbagog Lake, where they became well established and have since migrated to the Rapid River. A clerk creel survey was conducted in 2007 to monitor angler use, catch, and harvest subsequent to changes in fishing regulations and flow regimes, and to monitor the impacts of smallmouth bass. Creel survey data suggested that a decline in brook trout production documented earlier (from 2002 to 2004) was at least partially arrested, and that the vigorous expansion of smallmouth bass numbers slowed or declined by 2007. It's likely that increasingly restrictive fishing regulations, beginning in 2004, were partially responsible for the positive trend. Three consecutive years of unfavorable flows for bass spawning (2005- 2007), and the wet, cool conditions that prevailed during those years, were also important factors. By manipulating flows from Middle Dam, we'll maintain a high level of stress to smallmouth bass during their spawning, incubation, and early recruitment periods, and therefore maintain or improve conditions for trout survival. -
Friends of Merrymeeting Bay P.O
Friends of Merrymeeting Bay P.O. Box 233 Richmond, ME 04357 www.fomb.org To: Susanne Meidel, Water Quality Standards Coordinator Maine Department of Environmental Protection SHS 17 Augusta, ME 04333 207-441-3612 [email protected] From: Jennifer Brockway, Executive Director Friends of Merrymeeting Bay 207-666-1118 [email protected] E-Filed Subject: Water Re-Classification Proposal River/Sections: Androscoggin from Worumbo Dam to Merrymeeting Bay Proposed Upgrade: C to B Basis for Proposal: Actual conditions exceed those of present classification Documentation: Supporting data from FOMB monitoring program approved by Maine DEP and USEPA Data Collection Periods: DO-1999 to present; Coliform Bacteria-2006 to present Sampling Intervals: Monthly: April-October Proposal Date: November 29, 2017 Dear Ms. Meidel: Please consider this our formal upgrade proposal for the lower section of the Androscoggin River between Merrymeeting Bay at the line from Pleasant Point in Topsham to North Bath extending upriver to Worumbo Dam in Lisbon Falls. As our data show, while classified as C, this section has long been on the cusp of and now is actually meeting, Class B standards. We therefore propose it be upgraded from C to B. FOMB has the most complete set of classification data for the reaches in this proposal. We began our monitoring program in 1999 and continue to this day with over twenty sampling sites on the Androscoggin, Kennebec and around Merrymeeting Bay. FOMB joined the VRMP in 2009 to further support and substantiate water classification upgrades. Because the actual water quality of the lower Androscoggin sections described here exceeds that of their current classification, our request for a reclassification from C to B is supported by the State antidegradation policy as quoted below: 38 M.R.S.A. -
A Technical Characterization of Estuarine and Coastal New Hampshire New Hampshire Estuaries Project
AR-293 University of New Hampshire University of New Hampshire Scholars' Repository PREP Publications Piscataqua Region Estuaries Partnership 2000 A Technical Characterization of Estuarine and Coastal New Hampshire New Hampshire Estuaries Project Stephen H. Jones University of New Hampshire Follow this and additional works at: http://scholars.unh.edu/prep Part of the Marine Biology Commons Recommended Citation New Hampshire Estuaries Project and Jones, Stephen H., "A Technical Characterization of Estuarine and Coastal New Hampshire" (2000). PREP Publications. Paper 294. http://scholars.unh.edu/prep/294 This Report is brought to you for free and open access by the Piscataqua Region Estuaries Partnership at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in PREP Publications by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. A Technical Characterization of Estuarine and Coastal New Hampshire Published by the New Hampshire Estuaries Project Edited by Dr. Stephen H. Jones Jackson estuarine Laboratory, university of New Hampshire Durham, NH 2000 TABLE OF CONTENTS ACKNOWLEDGEMENTS TABLE OF CONTENTS ............................................................................................i LIST OF TABLES ....................................................................................................vi LIST OF FIGURES.................................................................................................viii -
Barker's Mill Hydroelectric Project
DRAFT ENVIRONMENTAL ASSESSMENT FOR HYDROPOWER LICENSE Barker’s Mill Hydroelectric Project FERC Project No. 2808-017 Maine Federal Energy Regulatory Commission Office of Energy Projects Division of Hydropower Licensing 888 First Street, NE Washington, DC 20426 September 2018 TABLE OF CONTENTS TABLE OF CONTENTS .................................................................................................... ii LIST OF FIGURES ............................................................................................................ iv LIST OF TABLES.............................................................................................................. iv ACRONYMS AND ABBREVIATIONS.......................................................................... vii 1.0 INTRODUCTION ................................................................................................ 1 1.1 APPLICATION .................................................................................................... 1 1.2 PURPOSE OF ACTION AND NEED FOR POWER ......................................... 1 1.2.1 Purpose of Action .......................................................................................... 1 1.2.2 Need for Power .............................................................................................. 3 1.3 STATUTORY AND REGULATORY REQUIREMENTS ................................. 3 1.3.1 Federal Power Act ......................................................................................... 4 1.3.2 Clean Water Act ........................................................................................... -
Rapid River Fishery Management (PDF)
FISHERY INTERIM SUMMARY REPORT SERIES NO. 11-03 RAPID RIVER FISHERY MANAGEMENT By David P. Boucher Maine Department of Inland Fisheries and Wildlife Division of Fisheries and Hatcheries Augusta, Maine December 2011 Job F-014 Interim Summary Report No. 5 (2008-2010) Rapid River Fishery Management SUMMARY The Rapid River, located in Township C and Upton in Oxford County, has long been noted for its outstanding brook trout population. Brook trout in the Rapid River are sustained entirely by natural reproduction and support a popular, heavily utilized sport fishery of regional and statewide significance. Landlocked salmon are present also and they provide an important ancillary fishery. During the 1980’s, smallmouth bass were illegally introduced into Umbagog Lake, where they became well established and have since migrated to the Rapid River. Intensive creel surveys have been conducted periodically since 1994 to monitor this important fishery. The most recent creel surveys, including in 2010, were intended to monitor angler use, catch, and harvest subsequent to changes in fishing regulations and flow regimes, and to assess the impacts of smallmouth bass on the river’s brook trout and salmon fisheries. Creel survey data suggested that a decline in brook trout production documented earlier (from 2002 to 2004) was at least partially arrested, and that the vigorous expansion of smallmouth bass numbers slowed or declined. We attributed this to improved protection of brook trout provided by more restrictive fishing regulations, beginning in 2004; to wet, cool environmental conditions that prevailed during several years from 2005 to 2010; and to unfavorable river flows for bass spawning and early recruitment during the same period. -
Whitewater Boating Program
Whitewater Boating Program 2020 Annual Warden Corporal Steve Allarie Report Whitewater Boating Specialist Whitewater Boating Program 2020 Annual Report on: Maine Warden Service Whitewater Boating Program Commercial Rafting Industry 130th Legislature – First Regular Session Dated: January 1, 2021 • In Maine, there are approximately 20 licensed Commercial Whitewater Outfitters providing whitewater boating trips among our6 Rapidly Flowing Rivers. The rivers include stretches of the upper Kennebec River, West Branch of the Penobscot River, South Branch of the Penobscot River, Dead River, Rapid River and the Magalloway River. • In Maine, the commercial whitewater industry provided professional services to approximately 24,639 commercial rafting passengers during the 2020 rafting season (January 1, 2020 to December 31, 2020). The low numbers reflect COVID-19 pandemic concerns and restrictions in early spring. The Commercial industry did not receive state approval to operate until the first week in June. The outfitters reported significant cancelations in the spring, which affected commercial numbers throughout the season. • The commercial whitewater rafting industry continues to be a tremendous economic asset to the State of Maine. The industry is complex and requires a significant investment of time by the Department to fulfill the responsibilities required by the State. In 1999, the Department hired a full-time Game Warden to work as a Whitewater Boating Specialist to enforce whitewater rafting rules and regulations and manage the administrative duties associated with the whitewater rafting industry. • Title 12, section 10259-B; states that all money from the Whitewater Rafting Fund shall be expended solely for purposes related to river recreation, with primary emphasis on those activities that relate to whitewater trips, including, but not limited to, administration, regulation, safety education, enforcement, mitigation of environmental and safety problems and mitigation of any adverse effect on competing use of the river. -
Examining Recreation Potential of the Little Androscoggin River Through the FERC Relicensing of the Lower Barker Dam in Auburn, Maine Nina Doonan
Bates College SCARAB Community Engaged Research Reports Environmental Studies Fall 12-2015 Examining Recreation Potential of the Little Androscoggin River through the FERC Relicensing of the Lower Barker Dam in Auburn, Maine Nina Doonan William Hilton Max Millslagle Sarah Stanley Follow this and additional works at: http://scarab.bates.edu/community_engaged_research Recommended Citation Doonan, Nina; Hilton, William; Millslagle, Max; and Stanley, Sarah, "Examining Recreation Potential of the Little Androscoggin River through the FERC Relicensing of the Lower Barker Dam in Auburn, Maine" (2015). Community Engaged Research Reports. 28. http://scarab.bates.edu/community_engaged_research/28 This Article is brought to you for free and open access by the Environmental Studies at SCARAB. It has been accepted for inclusion in Community Engaged Research Reports by an authorized administrator of SCARAB. For more information, please contact [email protected]. Examining Recreation Potential of the Little Androscoggin River through the FERC Relicensing of the Lower Barker Dam in Auburn, Maine ENVR 417 - Community Engaged Research Bates College Nina Doonan, William Hilton, Max Millslagle, Sarah Stanley Fall 2015 Acknowledgements: We would like to thank our professors Jane Costlow and Tom Wenzel for providing clear and thoughtful suggestions throughout the duration of this project. We also express our gratitude to our community partners, the Mayor of Auburn, Jonathan LaBonte and the Auburn Deputy Director of Planning and Development, Eric Cousens, for their vision and commitment to improving the community’s rivers and recreation opportunities. FERC "2 Table of Contents: I. Executive Summary..…………………………………………………………..….4 II. Summary of FERC Process.………………………………………………………5 III. Comparable Communities.……………………………………………………….7 IV. Interested Community Stakeholders.………………………………………….….9 V. -
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. -
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 -
Deglaciation of the Upper Androscoggin River Valley and Northeastern White Mountains, Maine and New Hampshire
Maine Geological Survey Studies in Maine Geology: Volume 6 1989 Deglaciation of the Upper Androscoggin River Valley and Northeastern White Mountains, Maine and New Hampshire Woodrow B. Thompson Maine Geological Survey State House Station 22 Augusta, Maine 04333 Brian K. Fowler Dunn Geoscience Corporation P.O. Box 7078, Village West Laconia, New Hampshire 03246 ABSTRACT The mode of deglaciation of the White Mountains of northern New Hampshire and adjacent Maine has been a controversial topic since the late 1800's. Recent workers have generally favored regional stagnation and down wastage as the principal means by which the late Wisconsinan ice sheet disappeared from this area. However, the results of the present investigation show that active ice persisted in the upper Androscoggin River valley during late-glacial time. An ice stream flowed eastward along the narrow part of the Androscoggin Valley between the Carter and Mahoosuc Ranges, and deposited a cluster of end-moraine ridges in the vicinity of the Maine-New Hampshire border. We have named these deposits the" Androscoggin Moraine." This moraine system includes several ridges originally described by G. H. Stone in 1880, as well as other moraine segments discovered during our field work. The ridges are bouldery, sharp-crested, and up to 30 m high. They are composed of glacial diamictons, including flowtills, with interbedded silt, sand, and gravel. Stone counts show that most of the rock debris comprising the Androscoggin Moraine was derived locally, although differences in provenance may exist between moraine segments on opposite sides of the valley. Meltwater channels and deposits of ice-contact stratified drift indicate that the margin of the last ice sheet receded northwestward.