THE BOWDOINHAM NEWS Volume 13, Issue 4 July & August 2015
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MAINE STATE LEGISLATURE The following document is provided by the LAW AND LEGISLATIVE DIGITAL LIBRARY at the Maine State Law and Legislative Reference Library http://legislature.maine.gov/lawlib Reproduced from scanned originals with text recognition applied (searchable text may contain some errors and/or omissions) ACTS AND RESOLVES AS PASSED BY THE Ninetieth and Ninety-first Legislatures OF THE STATE OF MAINE From April 26, 1941 to April 9, 1943 AND MISCELLANEOUS STATE PAPERS Published by the Revisor of Statutes in accordance with the Resolves of the Legislature approved June 28, 1820, March 18, 1840, March 16, 1842, and Acts approved August 6, 1930 and April 2, 193I. KENNEBEC JOURNAL AUGUSTA, MAINE 1943 PUBLIC LAWS OF THE STATE OF MAINE As Passed by the Ninety-first Legislature 1943 290 TO SIMPLIFY THE INLAND FISHING LAWS CHAP. 256 -Hte ~ ~ -Hte eOt:l:llty ffi' ft*; 4tet s.e]3t:l:ty tfl.a.t mry' ~ !;;llOWR ~ ~ ~ ~ "" hunting: ffi' ftshiRg: Hit;, ffi' "" Hit; ~ mry' ~ ~ ~, ~ ft*; eounty ~ ft8.t rett:l:rRes. ~ "" rC8:S0R8:B~e tffi:re ~ ft*; s.e]38:FtaFe, ~ ~ ffi" 5i:i'ffi 4tet s.e]3uty, ~ 5i:i'ffi ~ a-5 ~ 4eeme ReCCSS8:F)-, ~ ~ ~ ~ ~ ffi'i'El, 4aH ~ eRtitles. 4E; Fe8:50nable fee5 ffi'i'El, C!E]3C::lSCS ~ ft*; sen-ices ffi'i'El, ~ ft*; ffi4s, ~ ~ ~ ~ -Hte tFeasurcr ~ ~ eouRty. BefoFc tfte sffi4 ~ €of' ~ ~ 4ep i:tt;- ~ ffle.t:J:.p 8:s.aitional e1E]3cfisc itt -Hte eM, ~ -Hte ~ ~~' ~, ftc ~ ~ -Hte conseRt ~"" lIiajority ~ -Hte COt:l:fity COfi111'lissioReFs ~ -Hte 5a+4 coufity. Whenever it shall come to the attention of the commis sioner -
River Related Geologic/Hydrologic Features Abbott Brook
Maine River Study Appendix B - River Related Geologic/Hydrologic Features Significant Feature County(s) Location Link / Comments River Name Abbott Brook Abbot Brook Falls Oxford Lincoln Twp best guess location no exact location info Albany Brook Albany Brook Gorge Oxford Albany Twp https://www.mainememory.net/artifact/14676 Allagash River Allagash Falls Aroostook T15 R11 https://www.worldwaterfalldatabase.com/waterfall/Allagash-Falls-20408 Allagash Stream Little Allagash Falls Aroostook Eagle Lake Twp http://bangordailynews.com/2012/04/04/outdoors/shorter-allagash-adventures-worthwhile Austin Stream Austin Falls Somerset Moscow Twp http://www.newenglandwaterfalls.com/me-austinstreamfalls.html Bagaduce River Bagaduce Reversing Falls Hancock Brooksville https://www.worldwaterfalldatabase.com/waterfall/Bagaduce-Falls-20606 Mother Walker Falls Gorge Grafton Screw Auger Falls Gorge Grafton Bear River Moose Cave Gorge Oxford Grafton http://www.newenglandwaterfalls.com/me-screwaugerfalls-grafton.html Big Wilson Stream Big Wilson Falls Piscataquis Elliotsville Twp http://www.newenglandwaterfalls.com/me-bigwilsonfalls.html Big Wilson Stream Early Landing Falls Piscataquis Willimantic https://tinyurl.com/y7rlnap6 Big Wilson Stream Tobey Falls Piscataquis Willimantic http://www.newenglandwaterfalls.com/me-tobeyfalls.html Piscataquis River Black Stream Black Stream Esker Piscataquis to Branns Mill Pond very hard to discerne best guess location Carrabasset River North Anson Gorge Somerset Anson https://www.mindat.org/loc-239310.html Cascade Stream -
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.............................................................. -
Moose River Plains Wild Forest - South Anc D Little Moose Wilderness Owns
l r T s e d a Protect Yourself c s ^ ok Hiking trails can be rough and rugged a Bro • Moose River Plains Wild Forest - South anC d Little Moose Wilderness owns ! Br - they are not maintained as park Eighth Lake id E [J!j Sagamore c d walkways - wear boots or shoes See North Map Campground la a ! Lake P o e R designed for hiking. [J!(!G k Indian !9 ! " a ! !j L Lake ] - • Know the weather forecast; plan and e Sag k l am roo l Sugarloaf Fourth o [J!( st B i re Lo v Mtn prepare based on current and [J h Lake !0 R t d r forecasted conditions. !G o !S p N o B L U E R I D G E r • Pack a day pack with items like water, o e Inlet Sixth !0 L W I L D E R N E S S v [J i Lake e ! flashlight, extra clothing, etc. k ra R !0 e a Ko Lak ke Seveth L La • Sign in and out of all trail registers th Mohegan l h n i nth- t Wakely d eve ig Lake M ! that you encounter. a R S ly j! !( r E Pond ?g ke Wak r [J T a ely M Trl a W tn d Respect Others n e t M O O S E R I V E R !A iln k C k M o • Be courteous of all other users e P L A I N S W I L D ro ! im B (10) j! !(!G L F O R E S T ey [J regardless of their sport, speed or e dl ak ra Limekiln L ake L B Cellar Pd t[ skill level. -
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 -
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. -
The Design and Operation of a Picket Weir to Sample Brook Trout and Landlocked Salmon in Tributaries to Moosehead Lake
Fisheries Division Report Series No. 18-2 The Design and Operation of a Picket Weir to Sample Brook Trout and Landlocked Salmon in Tributaries to Moosehead Lake Progress Report No. 1 By: Timothy Obrey and Jeffery Bagley Moosehead Lake Region July 2018 Maine Department of Inland Fisheries & Wildlife Fisheries and Hatcheries Division 1 Summary A picket weir was designed and fabricated for sampling wild Brook Trout and Landlocked Salmon on their spawning migrations in tributaries to Moosehead Lake. The weir was installed on Socatean Stream in 2009 then on the Roach River in 2010 and 2011. Staff utilized radio telemetry and Passive Integrated Transponder (PIT) tags to monitor movements and estimate mortality. A total of 132 fish were equipped with radio telemetry transmitters and 872 fish were implanted with PIT tags during the three years of sampling. Post-spawning mortality rates for wild male Brook Trout ranged from 44-63% during the study. Sixteen to twenty-five percent of surviving Brook Trout returned to spawn in a second consecutive year, while less than 3% of the Landlocked Salmon returned to the Roach River. The winter sanctuary areas established in the 1930s, 1950s, and 1960s to protect wild Brook Trout are still effective. Many of the tagged Brook Trout utilized these areas during the winter months and were therefore unavailable for angler harvest. The weir will be a valuable tool for fisheries managers in the Moosehead Lake Region and other areas of the state in future fisheries studies. KEYWORDS: BKT, LLS, AGE & GROWTH, AGE FREQUENCY, SIZE FREQUENCY, EXPLOITATION RATE, MIGRATION, MOVEMENTS, HOMING, REGULATIONS, SURVIVAL, TAGGING, MORTALITY, WEIR. -
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. -
Visitor's Guide to JACKMAN MAINE
Visitor’s Guide to JACKMAN MAINE Jackman-Moose River Region Chamber of Commerce On the Old Canada Road Scenic Byway 1-888-633-5225 [email protected] Jackmanmaine.org Sparkling pure lakes, tumbling streams, sweeping mountains, and the vast north woods... Four Seasons of Fun! Acknowledgements EVENTS: There is something We would like to thank those who happening here all year like the helped put this guide together and to Hunters Supper, horseshoe those who donated the beautiful photography of our region. tournaments, golf tournaments, Tamara Cowen Christmas tree lighting, or our 4th John Farnsworth of July parade and fireworks. You Marlene Griffin Nick Hamel can always find out what is Briana Harris planned on our events page: Annie Nielsen Jeffrey Rancourt Sadie Theriault Eric Winsor Jackmanmaine.org Copyright 2018 Jackman Moose River Region Chamber of Commerce. Sparkling pure lakes, tumbling streams, sweeping mountains, and the vast north woods... Four Seasons of Fun! Maine’s Hidden Treasure The Jackman-Moose River Region book; FALL with its spectacular palette Chamber of Commerce invites you to of colors ushers in the bird, bear, deer visit our world of scenic beauty and and moose hunting seasons. Shortly quiet splendor. Whatever season you thereafter, WINTER descends and the choose, there’s something for valley becomes a wonderland for cross everyone to enjoy. country skiing, SPRINGTIME offers some snowshoeing, ice of the best fishing to be fishing, and found in the northeast; snowmobiling on SUMMERTIME is delightful hundreds of miles of with moderate daytime scenic groomed trails. temperatures and Whether you’re evenings just right for sleeping after a looking for great recreation or peaceful day of boating, canoeing, kayaking, relaxation, what could be better than whitewater rafting, mountain biking, time in the great outdoors! ATV riding, or just enjoying a good WHERE TO STAY ALLEN’S FOUR SEASONS ACCOMMODATIONS 37 John's Street, Jackman, ME 04945; 207-668-7683, [email protected] Campground, Laundromat, public showers, rec. -
L a K E R E G I
MAINE | vAcAtIoN guIdE Moosehead Lake Region A lake region so vast, there’s enough room for everyone . where moose outnumber people three to one. www.mooseheadlake.org 1-888-876-27781-888-876-2778 | www.mooseheadlake.org 1 2 1-888-876-2778 | www.mooseheadlake.org Moosehead Area churches table of church of the open Bible contents Moosehead Lake Road, Greenville Services: Sun 10am & 6:30pm / Wed 7pm Air Tours ...........................21 Holy Family Roman catholic church All-Terrain Vehicle Riding ..39 Pritham Avenue, Greenville Area Map ...........................33 Services: Saturday 4pm / Sunday 8:00am Bird Watching ....................37 Monson community church Boating ...............................10 Main Street, Monson Churches ..............................5 Services: Sunday 10:30am Dining Out .........................14 Monson united church of christ Family Activities ..................17 North Guilford Road, Monson Fishing ................................18 Services: Sunday 10am Hiking ................................22 New Life church Historical Sights ..................25 Mayhew Manor, Greenville Hunting ..............................27 Services: Sunday 10am Moose Watching ...............34 People’s united Methodist church Scenic Drives ......................30 Pritham Avenue, Greenville Jct. Schedule of Events .............12 Services: Sunday 9 am Shopping ............................40 Pittston Farm chapel Snowmobiling ....................45 Pittston Farm The Steamship “Katahdin” ..29 Services: Sunday 10:30am Waterfalls ..........................24