History of Acadie, Penobscot Bay and River, with a More Particular
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Bay of Fundy (Canada)
Tides Bay of Fundy (Canada) Tides Measuring tides General description Physical mechanism Characteristics in different locations Tidal resonance and tidal bore Measuring tides Records of the position of sea surface with respect to a fixed level (a datum) tidal pole float tidal gauge Measuring tides Time series of sea surface height Hilo tide observations and predictions (PacIOOS) Measuring tides Examples of tidal time series General description Up and down motion of sea level Back and forth currents Periodic (~12 hours and 24 hours) Amplitude and timing vary from one location to another Propagating shallow-water wave of very long wavelength (~10,000km) Physical mechanism due to the gravitational attraction of Moon and Sun on Earth and its ocean and the rotation of Moon around Earth and the Earth-Moon system around the Sun Moon Sun Earth Physical mechanism due to the gravitational attraction of Moon and Sun on Earth and its ocean and the rotation of Moon around Earth and the Earth-Moon system around the Sun Moon Sun “It's complicated!” Earth Theory of equilibrium tides Simplified problem Earth-Moon system only No rotation of Earth around its own axis Earth covered with an ocean (no continents) No friction Theory of equilibrium tides Centrifugal Force (varies with r) r d Gravitational Force (varies with 1/d2) Theory of equilibrium tides Theory of equilibrium tides Theory of equilibrium tides Theory of equilibrium tides Theory of equilibrium tides Tidal Force Theory of equilibrium tides Tidal Force Theory of equilibrium -
MOG Biography
Dictionary of Canadian Biography MOG (Heracouansit, Warracansit, Warracunsit, Warrawcuset), a noted warrior, subchief, and orator of the Norridgewock (Caniba) division of the Abenakis, son of Mog, an Abenaki chief killed in 1677; b. c. 1663; killed 12 Aug. 1724 (O.S.) at Norridgewock (Narantsouak; now Old Point in south Madison, Me). In the La Chasse* census of 1708, Mog is listed under the name Heracouansit (in Abenaki, welákwansit, “one with small handsome heels”). During King William’s and Queen Anne’s Wars Mog took part in the numerous raids on English settlements by Abenakis and carried captives and scalps to Quebec. Following the peace of Utrecht in April 1713, Mog, Bomoseen, Moxus, Taxous, and other chiefs concluded a peace with New England at Portsmouth, N.H., on 11– 13 July. The Abenakis pledged allegiance to Anne, though “it is safe to say that they did not know what the words meant” (Parkman). They also admitted the right of the English to land occupied before the war. The English, on their side, promised that the Indians could settle any individual grievances with them in English courts. Mog and the others then sailed with six New England commissioners to Casco Bay, where the treaty and terms of submission were read to 30 chiefs, in the presence of 400 other Abenakis, on 18 July. “Young Mogg” was described as “a man about 50 years, a likely Magestick lookt Man who spake all was Said.” The Abenakis expressed surprise when told that the French had surrendered all the Abenaki lands to the English: “wee wonder how they would give it away without asking us, God having at first placed us there and They having nothing to do to give it away.” Father Sébastien RALE, the Jesuit missionary at Norridgewock, reported a month later that he had convinced the Indians the English were deceiving them with an ambiguous phrase, for England and France still disagreed about the limits of “Acadia.” Apparently the Indians remained disturbed, however, when the English offered to show them the official text of the European treaty in the presence of their missionaries. -
Kennebec Estuary Focus Areas of Statewide Ecological Significance Kennebec Estuary
Focus Areas of Statewide Ecological Significance: Kennebec Estuary Focus Areas of Statewide Ecological Significance Kennebec Estuary WHY IS THIS AREA SIGNIFICANT? The Kennebec Estuary Focus Area contains more than 20 percent of Maine’s tidal marshes, a significant percentage of Maine’s sandy beach and associated dune Biophysical Region habitats, and globally rare pitch pine • Central Maine Embayment woodland communities. More than two • Cacso Bay Coast dozen rare plant species inhabit the area’s diverse natural communities. Numerous imperiled species of animals have been documented in the Focus Area, and it contains some of the state’s best habitat for bald eagles. OPPORTUNITIES FOR CONSERVATION » Work with willing landowners to permanently protect remaining undeveloped areas. » Encourage town planners to improve approaches to development that may impact Focus Area functions. » Educate recreational users about the ecological and economic benefits provided by the Focus Area. » Monitor invasive plants to detect problems early. » Find ways to mitigate past and future contamination of the watershed. For more conservation opportunities, visit the Beginning with Habitat Online Toolbox: www.beginningwithhabitat.org/ toolbox/about_toolbox.html. Rare Animals Rare Plants Natural Communities Bald Eagle Lilaeopsis Estuary Bur-marigold Coastal Dune-marsh Ecosystem Spotted Turtle Mudwort Long-leaved Bluet Maritime Spruce–Fir Forest Harlequin Duck Dwarf Bulrush Estuary Monkeyflower Pitch Pine Dune Woodland Tidewater Mucket Marsh Bulrush Smooth Sandwort -
A Review of Ice and Tide Observations in the Bay of Fundy
A tlantic Geology 195 A review of ice and tide observations in the Bay of Fundy ConDesplanque1 and David J. Mossman2 127 Harding Avenue, Amherst, Nova Scotia B4H 2A8, Canada departm ent of Physics, Engineering and Geoscience, Mount Allison University, 67 York Street, Sackville, New Brunswick E4L 1E6, Canada Date Received April 27, 1998 Date Accepted December 15,1998 Vigorous quasi-equilibrium conditions characterize interactions between land and sea in macrotidal regions. Ephemeral on the scale of geologic time, estuaries around the Bay of Fundy progressively infill with sediments as eustatic sea level rises, forcing fringing salt marshes to form and reform at successively higher levels. Although closely linked to a regime of tides with large amplitude and strong tidal currents, salt marshes near the Bay of Fundy rarely experience overflow. Built up to a level about 1.2 m lower than the highest astronomical tide, only very large tides are able to cover the marshes with a significant depth of water. Peak tides arrive in sets at periods of 7 months, 4.53 years and 18.03 years. Consequently, for months on end, no tidal flooding of the marshes occurs. Most salt marshes are raised to the level of the average tide of the 18-year cycle. The number of tides that can exceed a certain elevation in any given year depends on whether the three main tide-generating factors peak at the same time. Marigrams constructed for the Shubenacadie and Cornwallis river estuaries, Nova Scotia, illustrate how the estuarine tidal wave is reshaped over its course, to form bores, and varies in its sediment-carrying and erosional capacity as a result of changing water-surface gradients. -
American Eel Distribution and Dam Locations in the Merrymeeting Bay
Seboomook Lake American Eel Distribution and Dam Ripogenus Lake Locations in the Merrymeeting Bay Pittston Farm North East Carry Lobster Lake Watershed (Androscoggin and Canada Falls Lake Rainbow Lake Kennebec River Watersheds) Ragged Lake a d a n Androscoggin River Watershed (3,526 sq. miles) a C Upper section (1,363 sq. miles) South Twin Lake Rockwood Lower section (2,162 sq. miles) Kokadjo Turkey Tail Lake Kennebec River Watershed (6,001 sq. miles) Moosehead Lake Wood Pond Long Pond Long Pond Dead River (879 sq. miles) Upper Jo-Mary Lake Upper Section (1,586 sq. miles) Attean Pond Lower Section (3,446 sq. miles) Number Five Bog Lowelltown Lake Parlin Estuary (90 sq. miles) Round Pond Hydrology; 1:100,000 National Upper Wilson Pond Hydrography Dataset Greenville ! American eel locations from MDIFW electrofishing surveys Spencer Lake " Dams (US Army Corps and ME DEP) Johnson Bog Shirley Mills Brownville Junction Brownville " Monson Sebec Lake Milo Caratunk Eustis Flagstaff Lake Dover-Foxcroft Guilford Stratton Kennebago Lake Wyman Lake Carrabassett Aziscohos Lake Bingham Wellington " Dexter Exeter Corners Oquossoc Rangeley Harmony Kingfield Wilsons Mills Rangeley Lake Solon Embden Pond Lower Richardson Lake Corinna Salem Hartland Sebasticook Lake Newport Phillips Etna " Errol New Vineyard " Madison Umbagog Lake Pittsfield Skowhegan Byron Carlton Bog Upton Norridgewock Webb Lake Burnham e Hinckley Mercer r Farmington Dixmont i h s " Andover e p Clinton Unity Pond n i m a a Unity M H East Pond Wilton Fairfield w e Fowler Bog Mexico N Rumford -
Designation of Critical Habitat for the Gulf of Maine, New York Bight, And
Federal Register / Vol. 81, No. 107 / Friday, June 3, 2016 / Proposed Rules 35701 the Act, including the factors identified Recovery and State Grants, Ecological Public hearings and public in this finding and explanation (see Services Program, U.S. Fish and information meetings: We will hold two Request for Information, above). Wildlife Service. public hearings and two public informational meetings on this proposed Conclusion Authority rule. We will hold a public On the basis of our evaluation of the The authority for these actions is the informational meeting from 2 to 4 p.m., information presented under section Endangered Species Act of 1973, as in Annapolis, Maryland on Wednesday, 4(b)(3)(A) of the Act, we have amended (16 U.S.C. 1531 et seq.). July 13 (see ADDRESSES). A second determined that the petition to remove Dated: May 25, 2016. public informational meeting will be the golden-cheeked warbler from the Stephen Guertin, held from 3 to 5 p.m., in Portland, List of Endangered and Threatened Maine on Monday, July 18 (see Wildlife does not present substantial Acting Director, U.S. Fish and Wildlife Service. ADDRESSES). We will hold two public scientific or commercial information [FR Doc. 2016–13120 Filed 6–2–16; 8:45 am] hearings, from 3 to 5 p.m. and 6 to 8 indicating that the requested action may p.m., in Gloucester, Massachusetts on BILLING CODE 4333–15–P be warranted. Therefore, we are not Thursday, July 21 (see ADDRESSES). initiating a status review for this ADDRESSES: You may submit comments, species. DEPARTMENT OF COMMERCE identified by the NOAA–NMFS–2015– We have further determined that the 0107, by either of the following petition to list the U.S. -
The Forks ATV Trails
Ragged Norcross Lake Mountain Tomhegan Pond p oo h L nc ra B th r o Big Spencer N Mountain d a o R o m e Spencer D Pond Lucky Lake Kokadjo Rockwood Black Brassua Brook Hill Lake d a o First Roach R Jackman o Pond L m o e Jackman ng n Little Po D d Loop Brassua Lake Little Big 668-2691 Wood Pond Moosehead Lake Long Pond Wood Pond Long Pond Mountain Attean Overlook d a o Lily Bay R Owls Head l Mountain t a i Moosehead p a Attean C Lily Bay Pond State Park Attean Mountain Burnham Pond Pa Prong Catheart rli Burnt Jacket n L o Pond Mountain o Mountain p Indian B-52 Crash Site Parlin Pond Mtn View Pond Pond Upper Road d ncer a Wilson Pond Spe o R Whipple y a Pond B Blue y l i Lower Ridge L d a Wilson Pond o Trout Pond R l a it Mountain p a Cold C Stream Falls Coburn Greenville Mountain d a o R Greenville Fish m Enchanted a Pond D s Pond i r r a H 911 West Forks RESCUE A Baker Pond 15 Mile Lodge & Outfitters 10 Spencer Moxie Falls Lake Lake RESCUE E Onawa King and Hawk’s Nest Lodge C.Moxie Gore Outfitters, Inc. Bartlett Lake 8 9 West Forks r Shi l e y R o a d Ledge Hill ake xie Ro Shirley Mills L Mo a d 911 RESCUE B Marshalls 7 Inn by the River 6 The Forks T r o RESCUE D u t d a l e Grand Falls Upper R o Eustis a Pierce Pond d RESCUE C Lake Basin 911 Monson Moxie Hebron Mountain Pond Northern Outdoors Lodge 5 Pleasant Pond Mountain Bald Mountain Pierce Blanchard Pond Fl a Pond Pleasant Kennebec River g s t Pond a Ice Jam Flagstaff f f Mountain R o a Spring Moosehorn d Flagstaff Lake Caratunk Lake Backcountry Expeditions 4 Moxie Mtn Balsamwoods -
Re-Membering Norridgewock Stories and Politics of a Place Multiple
RE-MEMBERING NORRIDGEWOCK STORIES AND POLITICS OF A PLACE MULTIPLE A Dissertation Presented to the Faculty of the Graduate School of Cornell University In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy by Ashley Elizabeth Smith December 2017 © 2017 Ashley Elizabeth Smith RE-MEMBERING NORRIDGEWOCK STORIES AND POLITICS OF A PLACE MULTIPLE Ashley Elizabeth Smith, Ph. D. Cornell University 2017 This dissertation is an ethnography of place-making at Norridgewock, the site of a famous Wabanaki village in western Maine that was destroyed by a British militia in 1724. I examine how this site is variously enacted as a place of Wabanaki survivance and erasure and ask, how is it that a particular place with a particular history can be mobilized in different and even contradictory ways? I apply Annemarie Mol’s (2002) analytic concept of the body multiple to place to examine how utilize practices of storytelling, remembering, gathering, producing knowledge, and negotiating relationships to variously enact Norridgewock as a place multiple. I consider the multiple, overlapping, coexistent, and contradictory enactments of place and engagements with knowledge that shape place-worlds in settler colonial nation-states. Rather than taking these different enactments of place to be different perspectives on or versions of place, I examine how these enactments are embedded in and shaped by hierarchies of power and politics that produce enactments of place that are at times parallel and at times contradictory. Place-making is especially political in the context of settler colonialism, where indigenous places, histories, and peoples are erased in order to be replaced (Wolfe 2006; O’Brien 2010). -
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. -
The Uncommon Enemy: First Nations and Empires in King William's War
The Uncommon Enemy: First Nations and Empires in King William's War By Steven Schwinghamer A Thesis Submitted to Saint Mary’s University, Halifax, Nova Scotia in Partial Fulfillment of the Requirements for the Degree of Master of Arts in History May 2007, Halifax, Nova Scotia Copyright Steven Schwinghamer, 2007 Dr Greg Marquis External Examiner Dr Michael Vance Reader Dr John Reid Supervisor Date: 4th May 2007 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Library and Bibliotheque et Archives Canada Archives Canada Published Heritage Direction du Branch Patrimoine de I'edition 395 Wellington Street 395, rue Wellington Ottawa ON K1A 0N4 Ottawa ON K1A 0N4 Canada Canada Your file Votre reference ISBN: 978-0-494-30278-1 Our file Notre reference ISBN: 978-0-494-30278-1 NOTICE: AVIS: The author has granted a non L'auteur a accorde une licence non exclusive exclusive license allowing Library permettant a la Bibliotheque et Archives and Archives Canada to reproduce,Canada de reproduire, 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 loan, distribute and sell theses le monde, a des fins commerciales ou autres, worldwide, for commercial or non sur support microforme, papier, electronique commercial purposes, in microform,et/ou autres formats. paper, electronic and/or any other formats. The author retains copyright L'auteur conserve la propriete du droit d'auteur ownership and moral rights in et des droits moraux qui protege cette these. -
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. -
People of the Dawnland and the Enduring Pursuit of a Native Atlantic World
UNIVERSITY OF OKLAHOMA GRADUATE COLLEGE “THE SEA OF TROUBLE WE ARE SWIMMING IN”: PEOPLE OF THE DAWNLAND AND THE ENDURING PURSUIT OF A NATIVE ATLANTIC WORLD A DISSERTATION SUBMITTED TO THE GRADUATE FACULTY in partial fulfillment of the requirements for the Degree of DOCTOR OF PHILOSOPHY By MATTHEW R. BAHAR Norman, Oklahoma 2012 “THE SEA OF TROUBLE WE ARE SWIMMING IN”: PEOPLE OF THE DAWNLAND AND THE ENDURING PURSUIT OF A NATIVE ATLANTIC WORLD A DISSERTATION APPROVED FOR THE DEPARTMENT OF HISTORY BY ______________________________ Dr. Joshua A. Piker, Chair ______________________________ Dr. Catherine E. Kelly ______________________________ Dr. James S. Hart, Jr. ______________________________ Dr. Gary C. Anderson ______________________________ Dr. Karl H. Offen © Copyright by MATTHEW R. BAHAR 2012 All Rights Reserved. For Allison Acknowledgements Crafting this dissertation, like the overall experience of graduate school, occasionally left me adrift at sea. At other times it saw me stuck in the doldrums. Periodically I was tossed around by tempestuous waves. But two beacons always pointed me to quiet harbors where I gained valuable insights, developed new perspectives, and acquired new momentum. My advisor and mentor, Josh Piker, has been incredibly generous with his time, ideas, advice, and encouragement. His constructive critique of my thoughts, methodology, and writing (I never realized I was prone to so many split infinitives and unclear antecedents) was a tremendous help to a graduate student beginning his career. In more ways than he probably knows, he remains for me an exemplar of the professional historian I hope to become. And as a barbecue connoisseur, he is particularly worthy of deference and emulation.