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Critical Habitat
Biological valuation of Atlantic salmon habitat within the Gulf of Maine Distinct Population Segment Biological assessment of specific areas currently occupied by the species; and determination of whether critical habitat in specific areas outside the currently occupied range is deemed essential to the conservation of the species NOAA’s National Marine Fisheries Service Northeast Regional Office 1 Blackburn Drive Gloucester, MA. 01930 2009 Foreword: Atlantic salmon life history........................................................................................................... 3 Chapter 1: Methods and Procedures for Biological Valuation of Atlantic Salmon Habitat in the Gulf of Maine Distinct Population Segment (GOM DPS).......................................................................................... 6 1.1 Introduction .............................................................................................................................................. 6 1.2 Identifying the Geographical Area Occupied by the Species and Specific Areas within the Geographical Area ................................................................................................................................................................ 7 1.3 Specific areas outside the geographical area occupied by the species essential to the conservation of the species .......................................................................................................................................................... 11 1.4 Identify those “Physical -
High Peaks Region Recreation Plan
High Peaks Region Recreation Plan An overview and analysis of the recreation, possibilities, and issues facing the High Peaks Region of Maine Chris Colin, Jacob Deslauriers, Dr. Chris Beach Fall 2008 Maine Appalachian Trail Land Trust – High Peaks Initiative: The Maine Appalachian Trail Land Trust (MATLT) was formed in June 2002 by a group of Mainers dedicated to the preservation of the natural qualities of the lands surrounding the Appalachian Trail in Maine. Following its campaign to acquire Mount Abraham and a portion of Saddleback Mountain, MATLT is embarking on a new initiative to research and document the ecological qualities of the entire Western Maine High Peaks Region. The MATLT website describes the region as follows: “The Western Maine High Peaks Region is the 203,400 acres roughly bounded by the communities of Rangeley, Phillips, Kingfield and Stratton. In this region, there are about 21,000 acres above 2700 feet. It is one of only three areas in Maine where the mountains rise above 4000 feet. The other two are the Mahoosuc Range and Baxter Park. Eight (8) of the fourteen (14) highest mountains in Maine are in this region (Sugarloaf, Crocker, South Crocker, Saddleback, Abraham, The Horn, Spaulding and Redington Peak.) These are all above 4000 feet. If one adds the Bigelow Range, across Route 27/16 from Sugarloaf, the region hosts ten (10) of the highest mountains (Avery Peak and West Peak added)). This area is comparable in size to Baxter Park but has 40% more area above 2700 feet.” Table of Contents I. Introduction ............................................................................................................................................... 1 A. Purpose and Need for High Peaks Area Recreation Plan .................................................................... -
1982 Maine River Study Appendix J – Rivers with River Related Inland Fisheries
1982 Maine River Study Appendix J – Rivers with River Related Inland Fisheries Region River Segment Description County Length A Big Ossipee Saco River to NH Border Oxford, York 12.5 A Bog Brook Little Androscoggin River to headwaters Androscoggin, Oxford 9 A Branch Brook Tidewaters to headwaters York 13 A Collyer Brook Royal River to headwaters Cumberland 4 A Crooked River Songo River to Songo Road Oxford, Cumberland 48 A Little Androscoggin River South Paris Dam to headwaters Oxford 15 A Little Ossipee River Route 5 to Balch Pond York 14.5 A Little River Presumpscot River to headwaters Cumberland 16 A Nezinscot River Androscoggin River to headwaters Androscoggin, Oxford 13.5 A Northwest Pond Sebago Lake to Peabody Pond Cumberland 8 A Pleasant River Presumpscot River to headwaters Cumberland 12.5 A Pleasant River Androscoggin River to headwaters Oxford 3 A Saco River Bonney Eagle Dam to NH border Oxford, York 54 A Wild River Androscoggin River NH border Oxford 4.5 B Belgrade Stream Route 27 to Wings Mill Kennebec 6.5 B Cobbosseecontee Headtide to Cobbosseecontee Lake Kennebec 17 B Ducktrap River Headtide to Tilden Pod Waldo 9 B Jock Stream /Dilnow Brook Cobbosseecontee Lake to headwaters Androscoggin, Kennebec 10.5 B Kennebec River Augusta to Skowhegan Kennebec, Somerset 32 B Messalonskee Stream Kennebec River to Messalonskee Lake Kennebec 5 B Oyster River Headtide to headwaters Knox 7.5 B Sebasticook River Benton Falls to Burnham Lake Kennebec 15.5 B Sheepscot River Headtide to Sheepscot Lake Lincoln 23 B St George River Tidewater to -
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 ..................................................................... -
Report of the Commissioners of Inland Fisheries and Game, 1914
TJWra Report of the Commit m sioners of »■— « . INLAND FISHERIES AND GAME State of flbaine 1914 REPORT OF T H E COMMISSIONERS INLAND FISHERIES AND GAME FOR T H E STATE OF MAINE FOR THE YEAR 1914 W ATERVILEE SENTINEL PUBLISHING COMPANY STATE OF MAINE. To His Excellency, William T. Haines, Governor of Maine: The Commissioners of Inland Fisheries and Game have the honor to present to Your Excellency their report for the year ending December 31, 1914, as required by section 19 of chapter 32 of the Revised Statutes, as amended by chapter 206 of the Public laws of 1913. HARRY B. AUSTIN, Chairman, W A LT ER I. N EA L, B L A IN E S. V IL E S, Commissioners of Inland Fisheries and Game. Since the last annual report of this department was issued our fish and game resources have not suffered material reduc tion, yet the time has come when, in order to conserve them, further restrictive legislation seems to us to be necessary. r e v i s i o n OE 1913. Experience has shown that private and special legislation is not usually so effective a means of conservation as are laws applicable to larger sections of the State rather than to the smaller units of a particular lake or town, and the general re vision of our fish and game laws in 1913 was based upon this principle and upon the idea that shorter open season and smaller bag limits would be easier of enforcement, and thus tend towards better conservation, than the former idea of private and special legislation covering the multitude of our inland waters and hunting grounds. -
Index to River Surveys Made by The
If you no lon~rer need this publication write to the Geological Survey in Washington for an official mailing label to use in returning it UNITED STATES DEPARTMENT OF THE INTERIOR • INDEX TO RIVER SURVEYS MADE BY THE I• UNITED STATES GEOLOGICAL SURVEY AND OTHER AGENCIES REVISED TO JULY 1, 1947 GEOLOGICAL SURVEY WATER-SUPPLY PAPER 995 UNITED STATES DEPARTMENT OF THE INTERIOR J. A. Krug, Secretary GEOLOGICAL SURVEY W. E. •Wrather, Director Water-Supply Paper 995 INDEX TO RIVER SURVEYS MADE BY THR UNITED STATES GEOLOGICAL SURVEY AND OTHER AGENCIES REVISED TO JULY 1, 1947 BY _BENJAMIN E. JONES and RANDOLPH 0. HELLAND UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1948 Ji', r s'lle bv the Superintendent of Documents, U. S. Government Printing Office, Washinglnu 25, D. C. Pr-ice 75 cents CONTENTS Page Introduction _____________________________________________________ _ 1 Alabama---------------------------------------------------------Alaska __________________________________________________________ _ 4 4 Arizona--------------------------------------------------------- 5 Arkansas-------------------------------------------------------- 11 12 California--------------------------------------------------------Colorado ________________________________________________________ _ 23 Connecticut------------------------------------------------------- 30 I>elaware ________________________________________________________ _ 30 I>istrict of Columbia ______________________________________________ _ 30 Florida __________________________________________________________ -
Catostomus Commersonii) in Maine Megan A
The University of Maine DigitalCommons@UMaine Electronic Theses and Dissertations Fogler Library 11-2016 Understanding the Impact of Commercial Harvest on White Suckers (Catostomus commersonii) in Maine Megan A. Begley University of Maine - Main, [email protected] Follow this and additional works at: http://digitalcommons.library.umaine.edu/etd Part of the Aquaculture and Fisheries Commons, Population Biology Commons, Terrestrial and Aquatic Ecology Commons, and the Zoology Commons Recommended Citation Begley, Megan A., "Understanding the Impact of Commercial Harvest on White Suckers (Catostomus commersonii) in Maine" (2016). Electronic Theses and Dissertations. 2553. http://digitalcommons.library.umaine.edu/etd/2553 This Open-Access Thesis is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of DigitalCommons@UMaine. UNDERSTANDING THE IMPACT OF COMMERCIAL HARVEST ON WHITE SUCKERS (CATOSTOMUS COMMERSONII) IN MAINE By Meg Begley B.S. University of Maine at Machias 2009 A THESIS Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science (in Wildlife Ecology) The Graduate School The University of Maine December 2016 Advisor Committee: Joseph Zydlewski, Professor of Fisheries Science, Co-Advisor Stephen M. Coghlan Jr., Associate Professor of Freshwater Fisheries Ecology, Co-Advisor Michael T. Kinnison, Professor of Evolutionary Applications UNDERSTANDING THE IMPACT OF COMMERCIAL HARVEST ON WHITE SUCKERS (CATOSTOMUS COMMERSONII) IN MAINE By Meg Begley Thesis Co-Advisors: Dr. Joseph Zydlewski and Dr. Stephen Coghlan, Jr. An Abstract of the Thesis Presented in Partial Fulfillment of the Requirements for the Degree of Master of Science (in Wildlife Ecology) December 2016 The State of Maine issues an unlimited number of commercial permits for the harvest of White Suckers Catostomus commersonii in Maine’s inland waters. -
Geologic Map of the Kenneabago Lake Quadrangle, Franklin County, Maine
DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-2058 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE KENNEABAGO LAKE QUADRANGLE, FRANKLIN COUNTY, MAINE By Eugene L. Boudette INTRODUCTION phased rocks as Early to Middle Proterozoic remains valid and the Jim Pond is older than the Ammonoosuc (see also Baudette, 1982, Previous work and Baudette and Boone, 1976). The earliest reconnaissance geologic investigations in this part of Silurian rocks older than those of the Moose River synclinorium Maine were by Jackson (1837, 1839), Holmes and Hitchcock occur in the quadrangle. A northwest-trending marine onlap during (1861, 1862), Hitchcock and Huntington (1874), and Hitchcock the Silurian was established (U.S. Geological Survey, 1965). (1877, 1878). Other early studies included the granitic plutons by Harwood and Berry (1967) determined a Middle Ordovician age Dale (1907), the Rangeley Conglomerate by Smith (1923), and for rocks in the Cupsuptic quadrangle (fig. 1) on regional strike with the bedrock geology by Keith (1933). a unit in the southwestern corner of the Kennebago Lake quad Studies related to mineral occurrences in the region were rangle. Moench (1969) defined and mapped the Upper Ordovi reported by Pratt and Allen (1949) on agricultural limestone, and cian(?) and Quimby and Greenvale Cove Formations in the by Wing and Dawson (1949) and Wing (1951a,b) on asbestos, Rangeley quadrangle. The Rangeley Formation and Perry Moun serpentinite, and greenstone. Many independent mining compa tain Formations were revised and defined by Osberg and others nies actively studied base-metal deposits during the period from (1968) in their description of the Kearsarge-central Maine syncli 1950 to 1968. -
Appendix G - Scenic Rivers
Maine River Study Appendix G - Scenic Rivers Length Segment Description County(s) Miles River Name Allagash River St John River to Telos Lake Aroostook /Piscataquis 102 Aroostook River Caribou to Sheridan Aroostook 31 Bear River Confluence Androscoggin River to headwaters Oxford 11 Wight Brook Bear River to headwaters Oxford n/a Big Wilson Stream Sebec Lake to Lower Wilson Pond Piscataquis 14 Little Wilson Stream Confluence with Big Wilson Stream to headwaters Piscataquis 8 Crooked River Sebago Lake to headwaters Cumberland/Oxford 45 Damaiscotta River Foster Point to headwaters Lincoln/Knox 45 Dead River Kennebec River to Flagstaff Lake Somerset 22 Enchanted Stream Dead River to headwaters Somerset 9 Spencer Stream Dead River to headwaters Somerset 18 Kibby Stream Spencer Stream to headwaters Somerset /Franklin 11 North Branch Dead River Flagstaff Lake to headwaters of Chain of Lakes Franklin 31 South Branch Dead River Flagstaff Lake to headwaters of Saddleback Lake Franklin 23 Dennys River Dennysville Station to Meddybemps Lake Washington 25 Ducktrap River Ocean to headwaters (Tilden Pond) Waldo 8 West Branch Ellis River Ellis River to headwaters including Frye Brook & Dunn Notch Oxford 10 Fish River Eagle Lake to headwaters Aroostook 38 Red River St Froid Lake to headwaters Aroostook 14 Rocky Brook Red River to headwaters Aroostook 9 Fox Brook Fish River to headwaters Aroostook 15 Smith Brook Fish River Lake to headwaters Aroostook 6 Kennebago River Cupsuptic Lake to Big Island Pond Oxford /Franklin 25 Kennebec River Bay Point to Bath -
The Lithologic and Structural Controls on the Geomorphology of the Mountainous Areas in North-Central Maine
Maine Geological Survey Studies in Maine Geology: Volume 5 1989 The Lithologic and Structural Controls on the Geomorphology of the Mountainous Areas in North-Central Maine Lindley S. Hanson Department of Geological Sciences Salem State College Salem, Massachusetts 01970 Dabney W. Caldwell Department of Geology Boston University Boston, Massachusetts 02215 ABSTRACT In the mountainous areas of north-central Maine, the highest peaks are commonly formed in hornfelsic rocks which surround Acadian plutons. Quartzites and felsic volcanic rocks form ridges and steep-sided mountains. The only summit supported by granitic rock is Mount Katahdin, which has a resistant cap of granophyre that overlies the weaker granular-textured granite. Lowlands are underlain by platonic rock, of both granitic and gabbroic composition, and by pervasively cleaved pelitic rocks. In Maine, the area of greatest relief occurs in a northeast-trending belt, referred to here as the Central Highlands. High peaks that exceed 4000 feet (1220 m) are most abundant in the Rangeley area, western Maine. The highlands continue into New Hampshire to the even higher peaks of the Presidential Range. In the center of the belt, near Greenville, there are no peaks that rise above 4000 feet (1220 m). All other high elevations are associated with the Katahdin massif, near the northeastern terminus of this mountainous region. The rugged topography of the Central Highlands has formed from the erosion of the Acadian orogen, which was either originally higher toward the southwest or has been differentially uplifted by one or more subsequent thermal events. Trellis drainage systems are best developed in areas of low-grade, regionally metamorphosed sandstones and petites. -
Maine River Study Appendix F - Rivers with Undeveloped Corridors
Maine River Study Appendix F - Rivers with Undeveloped Corridors Average Length Segment Description Development County(s) Miles Pts/Mile River Name Allagash River St John River to Telos Lake 9 Aroostook /Piscataquis 102 Musquacook Stream Allagash River to Clear Lake 4 Aroostook /Piscataquis 27 Chemquasabamticook Stream Long Lake to Ross Lake 7 Aroostook /Piscataquis 21 Allagash Stream Chamberlain Lake to headwaters 1 Piscataquis 23 Aroostook River Sheridan to Washburn 28 Aroostook 17 Aroostook River Masardis to Millinocket Stream 5 Aroostook 32 Millinocket Stream Confluence with Aroostook River to Millinocket Lake 6 Aroostook 5 Munsungan Stream Confluence with Aroostook River to Munsungan Lake 4 Aroostook 6 Machias River Aroostook River to headwaters of Big Machias Lake 7 Aroostook 40 Big Wilson Stream Sebec Lake to Lower Wilson Pond 14 Piscataquis 19 Little Wilson Stream Confluence with Big Wilson Stream to headwaters 3 Piscataquis 8 Chandler River Deep Hole Point to headwaters 21 Washington 15 Cupsuptic River Cupsuptic Lake to headwaters 7 Oxford 20 Dead River Kennebec River to Flagstaff Lake 19 Somerset 24 Enchanted Stream Dead River to headwaters 1 Somerset 9 Spencer Stream Dead River to headwaters 9 Somerset 18 Little Spencer Stream Spencer Stream to Spencer Lake 1 Somerset 6 Kibby Stream Spencer Stream to headwaters 9 Somerset /Franklin 9 North Branch Dead River Tim Brook to headwaters of Chain of Lakes 17 Franklin 20 Tim Brook North Branch Dead River to headwaters 8 Franklin n/a South Branch Dead River Flagstaff Lake to headwaters