Notice of Agency Rule-Making Adoption
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Assimilation Spawns Disunity --- Disunity Nurtures Assimilation
(submitted to June 2013 Wulustuk Times) Assimilation Spawns Disunity --- Disunity Nurtures Assimilation When Champlain visited Tadoussac in May, 1603 three First Nations had gathered together at St. Matthew’s Point near Tadoussac (in present day Quebec), a thousand of them, to celebrate a recent war victory over the Iroquois nation. The celebrations lasted for many days. These three victorious nations were the Etechemins, Algonquins and Montagnais. Most historians contend that the Etechemin nation was the name Champlain called the nation of the Wolastoqiyik whose territory extended from the St. John River watershed all the way to the St. Lawrence River. By uniting with their allied nations the Wolastoqiyik were able to defeat an enemy whose numbers were much greater than their own. When English captive John Gyles went hunting with the Wolastoqiyik in the late 1600s they took him up the Wolastoq to the Madawaska River and all the way to the Notre Dame Mountains along the St. Lawrence. There was plenty of game in those days and this region was their hunting and fishing grounds. Every year all of the families gathered at one place for the Grand Council meeting, Eqpahak Island above present day Fredericton being one such location. At that time families were assigned different hunting and fishing territories so that one area didn't get overharvested and the game depleted. This is how they survived for thousands of years working together as a united body. As late as the early 20th century some Wolastoqiyik families in New Brunswick and Maine were still hunting in their traditional family territories. -
Up and Up: River Herring in Eastern Maine
DOWNEAST FISHERIES PARTNERSHIP 2019 Up and up: River Herring in Eastern Maine PREPARED BY Anne Hayden, Medea Steinman, and Rachel Gorich This report is also available online at: downeastfisheries.org OUR PARTNERS coa.edu downeastinstitute.org mainesalmonrivers.org coastalfisheries.org mcht.org mainefarmlandtrust.org seagrant.umaine.edu manomet.org sunrisecounty.org wccog.net Contents 2 Introduction 2 Challenges for River Herring 4 What can be done? 5 What are River Herring? 6 Benefits of River Herring? 7 Managment 9 Status in 2018 11 Restoration Activities in Eastern Maine 14 Case Studies in River Herring Restoration 14 Bagaduce River 17 Patten Stream 17 Union River OUR PARTNERS 18 Narraguagus River 18 East Machias River 21 Orange River 21 Pennamaquan River 22 St. Croix River 23 Looking Ahead DOWNEAST FISHERIES parTNERSHIP / UP AND UP: RIVER HerrING IN EASTERN MAINE 1 Introduction River herring runs in eastern Maine are coming back! A string of successful projects, from the opening of the St. Croix fishway to the renewal of commercial fishing on Card Mill Stream in Franklin, have fueled growing momentum for restoration of rivers and streams, big and small. This report is an update on the status of river herring runs in eastern Maine. It describes the value of river herring and some of the many projects underway to allow river herring to swim upstream to their spawning habitat. Because river herring are a keystone species in freshwater and marine systems—and are so responsive to restoration efforts—they have become a focus of the Downeast Fisheries Partnership effort to restore fisheries in eastern Maine. -
Shellfish Harvesting Area Classification-Notification of Changes
S T A T E O F M A I N E D E P A R T M E N T O F M A R I N E R E S O U R C E S 2 1 S T A T E H O U S E S T A T I O N A U G U S T A, M A I N E 0 4 3 3 3 - 0 0 2 1 JANET T. MILLS PATRICK C. KELIHER GOVERNOR COMMISSIONER Shellfish Harvesting Area Classification-Notification of Changes October 18, 2020 This notice is in effect until repealed or replaced Ladies and Gentlemen: Under the authority of 12 M.R.S.A. § 6172; the Commissioner has made the following change to Area No. 500, Maine Coast Flood Closure: This notice reopens the Bagaduce River and from Eggemoggin Reach to Morgan Bay due to water quality returning to approved standards. Martin Pt (Friendship) to the Weskeag River, eastern Penobscot Bay, and from the Union River Bay to the Rt. 3 bridge in Trenton remain closed. All existing pollution and biotoxin closures remain in effect. The boundary descriptions of the area are as follows (struck text is being removed and underlined text is being added): Effective immediately, because of pollution from heavy rainfall, it shall be unlawful to dig, take or possess any clams, quahogs, oysters, mussels, whole or roe-on scallops from the shores, flats and waters; East of a line beginning at Martin Point (Friendship) running south to the limits of Maine territorial waters; AND south of a line beginning at the southern tip of Spaulding Island (South Thomaston) running west to the mainland shore and running east to the southern tip of Greens Island (Vinalhaven) then running northeast to the southern tip of Lane’s Island (Vinalhaven): AND east of a line beginning at Telegraph Point (North Haven) running south to Calf Point (Vinalhaven); AND east of a line beginning at Pendleton Point (Islesboro) running southwest to Crabtree Point (North Haven); AND south of a line beginning at Turtle Head (Islesboro) running southeast to Sawyer Pt (Cape Rosier); AND west of the Deer Isle Bridge (Sargentville/Deer Isle); AND south of the N. -
Maine Open Water Fishing Laws Summary, 1975 Maine Department of Inland Fisheries and Game
Maine State Library Digital Maine Inland Fisheries and Wildlife Law Books Inland Fisheries and Wildlife 1-1-1975 Maine Open Water Fishing Laws Summary, 1975 Maine Department of Inland Fisheries and Game Follow this and additional works at: https://digitalmaine.com/ifw_law_books Recommended Citation Maine Department of Inland Fisheries and Game, "Maine Open Water Fishing Laws Summary, 1975" (1975). Inland Fisheries and Wildlife Law Books. 301. https://digitalmaine.com/ifw_law_books/301 This Text is brought to you for free and open access by the Inland Fisheries and Wildlife at Digital Maine. It has been accepted for inclusion in Inland Fisheries and Wildlife Law Books by an authorized administrator of Digital Maine. For more information, please contact [email protected]. Maine Open Water Fishing Laws Summary Maine Department of Inland Fisheries and Game 284 State Street, Augusta, Maine 04330 0££K) auie^M 'e+snSny '+994S 9+p+S VQZ FISHING LICENSES Commissioner of Indian Affairs stating that the person described is an awe0 pue sauaijsij pupguj jo juauupiedaQ auip^Aj Indian and a member of that tribe. For this purpose, an Indian shall RESIDENT NONRESIDENT be any member on tribal lists of the Penobscot and Passamaquoddy 16 years and older . $ 6.50 Season: age 16 and older $15.50 Tribes, or a person on the membership list of the Association of Combination ............. 10.50 12-15 years inclusive .. 2.50 Aroostook Indians and who has resided in Maine for at least 5 years. ‘ 3-day . ’ 6.50 15-day* “ ........................ 10.50 “ Leave or furlough . 2.50 7-day ................................. 7.50 3-day ................................ -
Geomorphological Processes and the Development of the Lower Saint John River Human Landscape
GEOMORPHOLOGICAL PROCESSES AND THE DEVELOPMENT OF THE LOWER SAINT JOHN RIVER HUMAN LANDSCAPE by Pamela Jeanne Dickinson Bachelor of Arts, University of New Brunswick, 1993 Master of Science, University of Maine, Orono, 2001 A Dissertation Submitted in Partial Fulfilment of the Requirements for the Degree of Doctorate of Philosophy in the Graduate Academic Unit of Geology Supervisor(s): Dr. B.E. Broster, Department of Geology, Chair Dr. D.W. Black, Department of Anthropology Examining Board: Dr. R. Miller, Department of Geology Dr. E.E. Hildebrand, Department of Civil Engineering Dr. P. Arpe, Department of Forestry External Examiner: Dr. T.J. Bell, Department of Geography, Memorial University This dissertation is accepted by the Dean of Graduate Studies THE UNIVERSITY OF NEW BRUNSWICK June 2008 © Pamela J. Dickinson, 2008 Library and Archives Bibliotheque et 1*1 Canada Archives Canada Published Heritage Direction du Branch Patrimoine de I'edition 395 Wellington Street 395, rue Wellington Ottawa ON K1A 0N4 OttawaONK1A0N4 Canada Canada Your file Votre reference ISBN: 978-0-494-69319-3 Our file Notre reference ISBN: 978-0-494-69319-3 NOTICE: AVIS: The author has granted a non L'auteur a accorde une licence non exclusive exclusive license allowing Library and permettant a la Bibliotheque et Archives Archives Canada to reproduce, Canada de reproduce, publier, archiver, publish, archive, preserve, conserve, sauvegarder, conserver, transmettre au public communicate to the public by par telecommunication ou par I'lnternet, preter, telecommunication or on the Internet, distribuer et vendre des theses partout dans le loan, distribute and sell theses monde, a des fins commerciales ou autres, sur worldwide, for commercial or non support microforme, papier, electronique et/ou commercial purposes, in microform, autres formats. -
1.NO-ATL Cover
EXHIBIT 20 (AR L.29) NOAA's Estuarine Eutrophication Survey Volume 3: North Atlantic Region July 1997 Office of Ocean Resources Conservation and Assessment National Ocean Service National Oceanic and Atmospheric Administration U.S. Department of Commerce EXHIBIT 20 (AR L.29) The National Estuarine Inventory The National Estuarine Inventory (NEI) represents a series of activities conducted since the early 1980s by NOAA’s Office of Ocean Resources Conservation and Assessment (ORCA) to define the nation’s estuarine resource base and develop a national assessment capability. Over 120 estuaries are included (Appendix 3), representing over 90 percent of the estuarine surface water and freshwater inflow to the coastal regions of the contiguous United States. Each estuary is defined spatially by an estuarine drainage area (EDA)—the land and water area of a watershed that directly affects the estuary. The EDAs provide a framework for organizing information and for conducting analyses between and among systems. To date, ORCA has compiled a broad base of descriptive and analytical information for the NEI. Descriptive topics include physical and hydrologic characteristics, distribution and abundance of selected fishes and inver- tebrates, trends in human population, building permits, coastal recreation, coastal wetlands, classified shellfish growing waters, organic and inorganic pollutants in fish tissues and sediments, point and nonpoint pollution for selected parameters, and pesticide use. Analytical topics include relative susceptibility to nutrient discharges, structure and variability of salinity, habitat suitability modeling, and socioeconomic assessments. For a list of publications or more information about the NEI, contact C. John Klein, Chief, Physical Environ- ments Characterization Branch, at the address below. -
Survey of Hancock County, Maine Samuel Wasson
The University of Maine DigitalCommons@UMaine Maine History Documents Special Collections 1878 Survey of Hancock County, Maine Samuel Wasson Follow this and additional works at: https://digitalcommons.library.umaine.edu/mainehistory Part of the United States History Commons Repository Citation Wasson, Samuel, "Survey of Hancock County, Maine" (1878). Maine History Documents. 37. https://digitalcommons.library.umaine.edu/mainehistory/37 This Book is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Maine History Documents by an authorized administrator of DigitalCommons@UMaine. For more information, please contact [email protected]. SURVEY OF HANCOCK COUNTY. A SURVEY OF HANCOCK COUNTY, MAINE BY SAMIUEL WASSON. MEMBER OF STATE BOARD OK AGRICULTURE. AUGUSTA: SPRAGUE, OWEN A NASH, PRINTERS TO THE STATE. 1878. PREFACE. At the meeting of the Board of Agriculture held at Calais. a resolution was passed, urging the importance to our agri cultural literature of the publication of surveys of the differ ent counties in the State, giving brief notes of their history, industrial resources and agricultural capabilities ; and direct ing the Secretary to procure such contributions for the annual reports. In conformity with this resolution, and also as ear ning out the settled policy of the Board in this respect— evidences of which are found in the publication of similar reports in previous volumes—I give herewith a Survey of the County of Hancock, written by a gentleman who has been a member of the Board of Agriculture, uninterruptedly, from its first organization, and who is in every way well fitted for the work, which he has so well performed. -
Review of Circulation Studies and Modeling in Casco Bay Asa 2011-32
REVIEW OF CIRCULATION STUDIES AND MODELING IN CASCO BAY ASA 2011-32 PREPARED FOR: Casco Bay Estuarine Partnership (CBEP) University of Southern Maine, Muskie School PO Box 9300 34 Bedford St 228B Wishcamper Center Portland, ME 04104-9300 PREPARED BY: Malcolm L. Spaulding Applied Science Associates 55 Village Square Drive South Kingstown, RI 02880 DATE SUBMITTED July 11, 2011 1 EXECUTIVE SUMMARY Applied Science Associates (ASA) was contracted by the Casco Bay Estuary Partnership (CBEP) to prepare a report reviewing the state of knowledge of circulation in Casco Bay, discussing relevant hydrodynamic modeling approaches and supporting observation programs. A summary of the final report of this study (the present document) was presented at a two day, Casco Bay Circulation Modeling Workshop held on May 18-19, 2011 at the Eastland Park Hotel, Portland, Maine. At the conclusion of the workshop a brief consensus summary was prepared and provided in this report. The review identified four efforts focused on modeling the circulation of Casco Bay and the adjacent shelf waters. These included the following: Pearce et al (1996) application of the NOAA Model for Estuarine and Coastal Circulation Assessment (MECCA) model (Hess, 1998) (funded by CBEP); True and Manning’s (undated) application of the unstructured grid Finite Volume Coastal Ocean Model (FVCOM) model (Chen et al, 2003); McCay et al (2008) application of ASA’s Boundary Fitted Hydrodynamic Model (BFHYRDO), and Xue and Du(2010) application of the Princeton Ocean Model (POM) (Mellor, 2004). All models were applied in a three dimensional mode and featured higher resolution of the inner bay than of the adjacent shelf. -
Return the Tides Resource Book 1-1 Tidal Marsh Formation 1-2
Return the Tides Resource Book World Wide Web Version CONSERVATION LAW FOUNDATION by Erno R. Bonebakker, Portland ME with contributions by Peter Shelley, CLF, Rockland ME Kim Spectre, CLF, Rockland ME CREDITS AND ACKNOWLEDGEMENTS This resource book was developed during the Casco Bay “Return the Tides” pilot project in the summer of 1999. In large part, it is an adaptation and development of the marsh assessment manual developed by Rob Bryan of Maine Audubon and Michele Dionne of Wells NERR1 and the methods developed by the Parker River Clean Water Association in Newburyport, MA.2 Particular credit is due to Rob Bryan of Maine Audubon Society and Dr. Michele Dionne of the Wells Reserve for their guidance in the preparation of this manual. Rob’s unfailing support and advice has been a particular help. David Mountain and Tim Purinton of the Parker River Clean Water Association in Newburyport, MA were also critical in compiling their field methods handbook describing a simple way to develop and record useful inventory information using volunteers.. In addition, this book is the product of the thoughts and vision of a number of people who have dedicated themselves to estuaries: the science of estuary systems, the education of the public about the wonders of these systems, and the protection and restoration of these special places. They were completely generous in allowing us to borrow shamelessly from their writings and thinking and this effort in Maine would not have been possible without their gracious support. To that end, we would like to thank the following individuals and commend our readers to their efforts directly. -
Nonpoint Source Priority Watersheds List MARINE WATERS
Maine Department of Environmental Protection February 2019 Nonpoint Source Priority Watersheds List MARINE WATERS Impaired* Marine Waters Priority List (34 marine waters) Marine Water Area/Town Priority List Reasoning Anthoine Creek & Cove South Portland Negative Water Quality Indicators (FOCB) Broad Cove Cushing DMR/NPS Threat Bunganuc Creek Brunswick CBEP Priority Water Cape Neddick River York MS4 Priority Water Churches Rock So. Thomaston DMR/NPS Threat Egypt Bay Hancock/Franklin DMR/NPS Threat Goosefare Bay Kennebunkport MHB Priority Water, MS4 Priority Water Harpswell Cove Brunswick CBEP Priority Water Harraseeket River Freeport DMR/NPS Threat Hutchins Cove Bagaduce River / DMR/NPS Threat Northern Bay (Penobscot) Hyler Cove Cushing DMR/NPS Threat Kennebunk River Kennebunk MHB Priority Water Little River and Bay Freeport CBEP Priority Water Littlefield Cove Bagaduce River / DMR/NPS Threat Northern Bay (Penobscot) Maquoit Bay Brunswick CBEP Priority Water Martin Cove Lamoine DMR/NPS Threat Medomak River Estuary Waldoboro DMR/NPS Threat Mill Cove South Portland Negative Water Quality Indicators Mill Pond/Parker Head Phippsburg DMR/NPS Threat Mussell Cove Falmouth CBEP Priority Water, DMR/NPS Threat North Fogg Point Freeport CBEP Priority Water Northeast Creek Bar Harbor DMR/NPS Threat Oakhurst Island Harpswell CBEP Priority Water Ogunquit River Estuary Ogunquit MHB Priority Water, DMR/NPS Threat Pemaquid River Bristol DMR/NPS Threat Salt Pond Blue Hill/Sedgwick DMR/NPS Threat, MERI Scarborough River Estuary Scarborough DMR/NPS Threat Spinney Creek Eliot MS4 Priority Water, Negative Water Quality Indicators Spruce Creek Kittery MS4 Priority Water, Negative Water Quality Indicators Page 1 of 2 MDEP NPS Priority Watersheds List – MARINE WATERS February 2019 Marine Water Area/Town Priority List Reasoning Spurwink River Scarborough MHB Priority Water, DMR/NPS Threat St. -
Dynamics of Larval Fish Abundance in Penobscot Bay, Maine
81 Abstract–Biweekly ichthyoplankton Dynamics of larval fi sh abundance surveys were conducted in Penobscot Bay, Maine, during the spring and early in Penobscot Bay, Maine summer of 1997 and 1998. Larvae from demersal eggs dominated the catch from late winter through spring, but Mark A. Lazzari not in early summer collections. Larval Maine Department of Marine Resources fi sh assemblages varied with tempera- P.O. Box 8 ture, and to a lesser extent, plankton West Boothbay Harbor, Maine 04575 volume, and salinity, among months. E-mail address: [email protected] Temporal patterns of larval fi sh abun- dance corresponded with seasonality of reproduction. Larvae of taxa that spawn from late winter through early spring, such as sculpins (Myoxocepha- lus spp.), sand lance (Ammodytes sp.), and rock gunnel (Pholis gunnellus) For most fi sh, the greatest mortality tial variation in species diver sity and were dominant in Penobscot Bay in occurs during early life stages (Hjort, abundance, and 3) to relate these vari- March and April. Larvae of spring to early summer spawners such as 1914; Cushing, 1975; Leggett and Deb- ations to differences in location and en- winter fl ounder (Pleuronectes america- lois, 1994). Therefore, it is essential that vironmental variables. nus) Atlantic seasnail (Liparis atlan- fi sh eggs and larvae develop in favorable ticus), and radiated shanny (Ulvaria habitats that maximize the probability subbifurcata) were more abundant in of survival. Bigelow (1926) recognized Materials and methods May and June. Penobscot Bay appears the signifi cance of the coastal shelf for to be a nursery for many fi shes; there- the production of fi sh larvae within the Field methods fore any degradation of water quality Gulf of Maine, noting that most larvae during the vernal period would have were found within the 200-m contour. -
Seafloor Features and Characteristics of the Black Ledges Area, Penobscot Bay, Maine, USA
Journal of Coastal Research SI 36 333-339 (ICS 2002 Proceedings) Northern Ireland ISSN 0749-0208 Seafloor Features and Characteristics of the Black Ledges Area, Penobscot Bay, Maine, USA. Allen M. Gontz, Daniel F. Belknap and Joseph T. Kelley Department of Geological Sciences, 111 Bryand Global Science Center, University of Maine, Orono, Maine, USA04469-5790. [email protected], [email protected], [email protected] ABSTRACT The Black Ledges, a series of islands, shoals, and ledges in East Penobscot Bay, Maine, was mapped with digital sidescan sonar and shallow marine seismic reflection equipmentA total of 38 km2 of sidescan and 600 km of seismic data was collected during four cruises in 2000-2001. The sidescan sonar reveals a surficial geology dominated by muddy sediments with frequent, patchy outcrops of gravel and minor amounts of bedrock. There are seven large concentrations of pockmarks with populations totaling over 3500 in the areas of muddy sediments. Generally circular, pockmarks range in size from five to 75 meters in diameter and up to eight meters deep. Calculations show over 2 x 106 m3 of muddy sediment and pore water were removed from the system during pockmark formation. Seismic data reveal a simple stratigraphy of modern mud overlying late Pleistocene glaciomarine sediment, till and Paleozoic bedrock. Seismic data indicate areas of gas-rich sediments and gas- enhanced reflectors in close association with pockmarks, suggesting methane seepage as a cause of pockmark formation. Pockmarks are alsorecognized in areas lacking evidence of subsurface methane accumulations adding further validity to the late stage of development for the field.