The Northeastern Borderlands in an Age of Revolution, 1760-1820
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2.6 Settlement Along the Ottawa River
INTRODUCTION 76 2.6 Settlement Along the Ottawa River In spite of the 360‐metre drop of the Ottawa Figure 2.27 “The Great Kettle”, between its headwaters and its mouth, the river has Chaudiere Falls been a highway for human habitation for thousands of years. First Nations Peoples have lived and traded along the Ottawa for over 8000 years. In the 1600s, the fur trade sowed the seeds for European settlement along the river with its trading posts stationed between Montreal and Lake Temiskaming. Initially, French and British government policies discouraged settlement in the river valley and focused instead on the lucrative fur trade. As a result, settlement did not occur in earnest until the th th late 18 and 19 centuries. The arrival of Philemon Source: Archives Ontario of Wright to the Chaudiere Falls and the new British trend of importing settlers from the British Isles marked the beginning of the settlement era. Farming, forestry and canal building complemented each other and drew thousands of immigrants with the promise of a living wage. During this period, Irish, French Canadians and Scots arrived in the greatest numbers and had the most significant impact on the identity of the Ottawa Valley, reflected in local dialects and folk music and dancing. Settlement of the river valley has always been more intensive in its lower stretches, with little or no settlement upstream of Lake Temiskaming. As the fur trade gave way to farming, settlers cleared land and encroached on First Nations territory. To supplement meagre agricultural earnings, farmers turned to the lumber industry that fuelled the regional economy and attracted new waves of settlers. -
Dams and Reservoirs in the Lake Champlain Richelieu River Basin
JUST THE FACTS SERIES June 2019 DAMS AND RESERVOIRS IN THE LAKE CHAMPLAIN RICHELIEU RIVER BASIN MYTH Water released from tributary dams in the United States causes flooding in Lake Champlain and the Richelieu River. FACT Water levels in Lake Champlain and the Richelieu River Generally, mass releases of water from flood control are primarily affected by precipitation from rain or dams are avoided. In addition to compromising the snowmelt. structural integrity of the dams, mass releases would also endanger the very communities that these dams are built Because of its size, Lake Champlain can store a lot of to protect. water; the flood control dams and reservoirs in the basin, which are very small in comparison to the lake, do not When conditions force the release of more water than significantly change water levels of the lake and river as hydropower plants can handle, the increase in water they release water. levels immediately below the dam will be much greater than the increase on Lake Champlain. This is true even during high water and flooding events. Consider, for instance, when Lake Champlain and the Richelieu River experienced extreme flooding between April and June 2011, the additional releases flowing from Waterbury Reservoir—the largest flood control reservoir in the Vermont portion of the basin, contributed less than 2 centimetres (¾ inch) to the elevation of Lake Champlain and the upper Richelieu River. International Lake Champlain-Richelieu River Study Board FACT FACT Dams in the US portion of the basin are built for one of Waterbury Reservoir in Vermont is the largest reservoir two purposes: flood control or hydroelectric power. -
Atlantic Geoscience Society Abstracts 1995 Colloquium
A t l a n t ic G eo l o g y 39 ATLANTIC GEOSCIENCE SOCIETY ABSTRACTS 1995 COLLOQUIUM AND ANNUAL GENERAL MEETING ANTIGONISH, NOVA SCOTIA The 1995 Colloquium of the Atlantic Geoscience Society was held in Antigonish, Nova Scotia, on February 3 to 4, 1995. On behalf of the Society, we thank Alan Anderson, Mike Melchin, Brendan Murphy, and all others involved in the organization of this excellent meeting. In the following pages we publish the abstracts of talks and poster sessions given at the Colloquium which included special sessions on "The Geological Evolution of the Magdalen Basin: ANatmap Project" and "Energy and Environmental Research in the Atlantic Provinces", as well as contri butions of a more general aspect. The Editors Atlantic Geology 31, 39-65 (1995) 0843-5561/95/010039-27S5.05/0 40 A b st r a c t s A study of carbonate rocks from the late Visean to Namurian Mabou Group, Cape Breton Island, Nova Scotia T.L. Allen Department o f Earth Sciences, Dalhousie University, Halifax, Nova Scotia B3H 3J5, Canada The Mabou Group, attaining a maximum thickness of7620 stituents of the lower Mabou Group. The types of carbonate m, lies conformably above the marine Windsor Group and rocks present include laminated lime boundstones (stromato unconformably below the fluviatile Cumberland Group. It com lites), floatstones, and grainstones. The stromatolites occur pre prises a lower grey lacustrine facies and an upper red fluviatile dominantly as planar laminated stratiform types and as later facies. The grey lacustrine facies consists predominantly of grey ally linked hemispheroids, some having a third order crenate siltstones and shales with interbedded sandstones, gypsum, and microstructure. -
The Mapping of Samuel De Champlain, 1603–1635 Conrad E
51 • The Mapping of Samuel de Champlain, 1603–1635 Conrad E. Heidenreich The cartography of Samuel de Champlain marks the be- roster of 1595 he was listed as a fourier (sergeant) and aide ginning of the detailed mapping of the Atlantic coast north to the maréchal de logis (quartermaster), apparently of Nantucket Sound, into the St. Lawrence River valley, reaching the rank of maréchal himself.4 The same pay ros- and, in a more cursory fashion, to the eastern Great Lakes. ter states that in 1595 he went on a secret mission for the Previous maps were based on rapid ship-board reconnais- king that was regarded to be of some importance. He also sance surveys made in the early to middle sixteenth cen- made a “special report” to Henri IV after his West Indian tury, particularly on the expeditions of Jacques Cartier and voyage (1601) and after the first two voyages to Canada Jean-François de La Rocque, sieur de Roberval (1534 – (1603 and 1607). These reports seem to indicate that 43). These maps conveyed little more than the presence of Champlain had a personal relationship with Henri IV, a stylized coastline. The immediate result of the Cartier- probably accounting for the pension the king awarded him Roberval expeditions was that France lost interest in sometime before 1603.5 After the war, Champlain joined North America, except for fishing off the northeast coast. his uncle’s ship, the 500-tun Saint-Julien, in Spanish The indigenous population was considered impoverished Caribbean service.6 In June 1601, Champlain was in and hostile, there were no quick riches, and the winters Cádiz where he was a witness to his dying uncle’s testa- were so brutal that the French wondered whether Euro- ment leaving him a large estate near La Rochelle as well as peans could live there. -
Annex VIII Casestudy0304 Ch
IEA Hydropower Implementing Agreement Annex VIII Hydropower Good Practices: Environmental Mitigation Measures and Benefits Case study 03-04: Fish Migration and River Navigation - Chambly Dam, Canada Key Issues: 3- Fish Migration and River Navigation Climate Zone: Cf: Temperate Subjects: - Fishway Effects: - Allow upstream migration of juvenile American eel ( Anguilla rostrata ) Project Name: Chambly Dam Country: Canada Implementing Party & Period - Project: Hydro-Québec 1965 - Good Practice: Hydro-Québec 1997 Key Words: American eel, ladder, fish migration, Chambly Dam Abstract: For 150 years, the Richelieu River (Québec, Canada) supported a sizable commercial silver American eel fishery. A sharp and constant decline of annual landings since 1981 has been at least partly related to the rebuilding, in 1965, of an old cribwork. In 1997, a ladder was retrofitted on the 270-m Chambly Dam to allow eel migration and enhance recruitment. 1. Outline of the Project Chambly Dam is located on the Richelieu River, a tributary of the St. Lawrence near Montréal (Québec, Canada). It is a 270-m-long concrete overflow weir and the water head is approximately 5 m. It was built in 1965 to replace an old cribwork dam that was constructed in 1896. 2. Features of the Project Area The Richelieu River drains Lake Champlain, a large lake bordering New York and Vermont states (USA) and extending into Québec. Lake Champlain is connected to the Hudson River and to the Great Lakes by a network of locks and canals. The Richelieu River extends for 115 km between Lake Champlain and the St. Lawrence River. Figure 1 Location Map of the project From June to September, the average discharge is 271 m3/s (1937-1996) or about 3.5% of the St. -
17 Major Drainage Basins
HUC 8 HYDROLOGIC UNIT NAME CLINTON 04120101 Chautauqua-Conneaut FRANKLIN 04150409 CHAMPLAIN MASSENA FORT COVINGTON MOOERS ST LAWRENCE CLINTON 04120102 Cattaraugus BOMBAY WESTVILLE CONSTABLE CHATEAUGAY NYS Counties & BURKE LOUISVILLE 04120103 Buffalo-Eighteenmile BRASHER 04150308 CHAZY ALTONA ELLENBURG BANGOR WADDINGTON NORFOLK MOIRA 04120104 Niagara ESSEX MALONE DEC Regions JEFFERSON 6 04150307 BEEKMANTOWN MADRID 05010001 Upper Allegheny LAWRENCE BELLMONT STOCKHOLM DANNEMORA BRANDON DICKINSON PLATTSBURGH LEWIS OGDENSBURG CITY LISBON 05010002 Conewango 5 PLATTSBURGH CITY HAMILTON POTSDAM SCHUYLER FALLS SARANAC 05010004 French WARREN OSWEGATCHIE DUANE OSWEGO 04150306 PERU 04130001 Oak Orchard-Twelvemile CANTON PARISHVILLE ORLEANS WASHINGTON NIAGARA DE PEYSTER ONEIDA MORRISTOWN HOPKINTON WAVERLY PIERREPONT FRANKLIN 04140101 Irondequoit-Ninemile AUSABLE MONROE WAYNE BLACK BROOK FULTON SARATOGA DEKALB HERKIMER BRIGHTON GENESEE SANTA CLARA CHESTERFIELD 04140102 Salmon-Sandy ONONDAGA NYS Major 04150406 MACOMB 04150304 HAMMOND ONTARIO MADISON MONTGOMERY RUSSELL 04150102 Chaumont-Perch ERIE SENECA CAYUGA SCHENECTADY HERMON WILLSBORO ST ARMAND WILMINGTON JAY WYOMING GOUVERNEUR RENSSELAER ALEXANDRIA CLARE LIVINGSTON YATES 04130002 Upper Genesee OTSEGO ROSSIE COLTON CORTLAND ALBANY ORLEANS 04150301 04150404 SCHOHARIE ALEXANDRIA LEWIS 7 EDWARDS 04150408 CHENANGO FOWLER ESSEX 04130003 Lower Genesee 8 TOMPKINS CLAYTON SCHUYLER 9 4 THERESA 04150302 TUPPER LAKE HARRIETSTOWN NORTH ELBA CHAUTAUQUA CATTARAUGUS PIERCEFIELD 02050104 Tioga ALLEGANY STEUBEN -
Canadian Bee Journey
ECTD_051 TITLE: A Canadian bee journey SOURCE: Bee World 47: 55-65, 132-148 DATE: 1966 Reprinted from Bee World 41 : 55-65, 132-148 (1966) 55 CANADIAN BEE JOURNEY by EVA CRANE Bee Research Association, Hill House, Chalfont St. Peter, Gerrards Cross, Bucks., England 1. INTRODUCTION Three earlier visits to Canada from the United States (1954, 1957, 1964) had shown me that Canada ranks among the most progressive honey-producing countries of the world. It is also one of the most productive, on the basis of the honey yield per colony, and consistently shares with Australia the first world place for national average yield*. I had seen beekeeping in small sections of Ontario and British Columbia, and heard sporadic accounts of what was going on elsewhere; but Canada is 3 200 miles across and 2 900 miles from north to south [5 300, 4 800 km.], and I met very few Canadians who had seen the more remote areas. One such area, Peace River, seemed to be an El Dorado as far as beekeeping was concerned, but I had been able to get very little first-hand information about it. I was therefore very pleased to receive an invitation from the bee keepers of Canada to travel through their country from coast to coast in June 1965, when beekeeping activity would be at its height. I covered about 5 000 miles by road (and many more by air) attended a number of beekeepers' meetings and took part in various other programmes, and visited nearly all the scientific institutes where bee research is being done. -
Surface Waters of Vermont
DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Water-Supply Paper 424 SURFACE WATERS OF VERMONT BY C. H. PIERCE Prepared in cooperation with the STATE OF VERMONT WASHINGTON GOVEENMENT PBINTING OFFICE 1917 ADDITIONAL COPIES OF THIS PUBLICATION MAY BK PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 25 CENTS PER COPY CONTENTS. Introduction.............................................................. 5 Cooperation................................................................ 8 Division of work.......................................................... 8 Definition of terms......................................................... 9 Explanation of data........................................................ 9 Accuracy of field data and computed results................................ 11 Gaging stations maintained in Vermont..................................... 12 St. Lawrence River basin................................................. 13 Lake Champlain drainage basin......................................... 13 General features................................................... 13 Gaging-station records.............................................. 14 Lake Champlain at Burlington, Vt.............................. 14 Lake Champlain outlet (Richelieu River) at Chambly, Province of Quebec.1................................................. 20 Poultney Eiver near Fair Haven, Vt............................ 25 Otter Creek at Middlebury, -
Cultural Assets of Nova Scotia African Nova Scotian Tourism Guide 2 Come Visit the Birthplace of Canada’S Black Community
Cultural Assets of NovA scotiA African Nova scotian tourism Guide 2 Come visit the birthplace of Canada’s Black community. Situated on the east coast of this beautiful country, Nova Scotia is home to approximately 20,000 residents of African descent. Our presence in this province traces back to the 1600s, and we were recorded as being present in the provincial capital during its founding in 1749. Come walk the lands that were settled by African Americans who came to the Maritimes—as enslaved labour for the New England Planters in the 1760s, Black Loyalists between 1782 and 1784, Jamaican Maroons who were exiled from their home lands in 1796, Black refugees of the War of 1812, and Caribbean immigrants to Cape Breton in the 1890s. The descendants of these groups are recognized as the indigenous African Nova Scotian population. We came to this land as enslaved and free persons: labourers, sailors, farmers, merchants, skilled craftspersons, weavers, coopers, basket-makers, and more. We brought with us the remnants of our cultural identities as we put down roots in our new home and over time, we forged the two together and created our own unique cultural identity. Today, some 300 years later, there are festivals and gatherings throughout the year that acknowledge and celebrate the vibrant, rich African Nova Scotian culture. We will always be here, remembering and honouring the past, living in the present, and looking towards the future. 1 table of contents Halifax Metro region 6 SoutH SHore and YarMoutH & acadian SHoreS regionS 20 BaY of fundY & annapoliS ValleY region 29 nortHuMBerland SHore region 40 eaStern SHore region 46 cape Breton iSland region 50 See page 64 for detailed map. -
Canada Archives Canada Published Heritage Direction Du Branch Patrimoine De I'edition
North Atlantic Press Gangs: Impressment and Naval-Civilian Relations in Nova Scotia and Newfoundland, 1749-1815 by Keith Mercer Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at Dalhousie University Halifax, Nova Scotia August 2008 © Copyright by Keith Mercer, 2008 Library and Bibliotheque et 1*1 Archives Canada Archives Canada Published Heritage Direction du Branch Patrimoine de I'edition 395 Wellington Street 395, rue Wellington Ottawa ON K1A0N4 Ottawa ON K1A0N4 Canada Canada Your file Votre reference ISBN: 978-0-494-43931-9 Our file Notre reference ISBN: 978-0-494-43931-9 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 Plntemet, prefer, 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. this thesis. Neither the thesis Ni la these ni des extraits substantiels de nor substantial extracts from it celle-ci ne doivent etre imprimes ou autrement may be printed or otherwise reproduits sans son autorisation. -
They Planted Well: New England Planters in Maritime Canada
They Planted Well: New England Planters in Maritime Canada. PLACES Acadia University, Wolfville, Nova Scotia, 9, 10, 12 Amherst Township, Nova Scotia, 124 Amherst, Nova Scotia, 38, 39, 304, 316 Andover, Maryland 65 Annapolis River, Nova Scotia, 22 Annapolis Township, Nova Scotia, 23, 122-123 Annapolis Valley, Nova Scotia, 10, 14-15, 107, 178 Annapolis County, Nova Scotia, 20, 24-26, 28-29, 155, 258 Annapolis Gut, Nova Scotia, 43 Annapolis Basin, Nova Scotia, 25 Annapolis-Royal (Port Royal-Annapolis), 36, 46, 103, 244, 251, 298 Atwell House, King's County, Nova Scotia, 253, 258-259 Aulac River, New Brunswick, 38 Avon River, Nova Scotia, 21, 27 Baie Verte, Fort, (Fort Lawrence) New Brunswick, 38 Barrington Township, Nova Scotia, 124, 168, 299, 315, Beaubassin, New Brunswick (Cumberland Basin), 36 Beausejour, Fort, (Fort Cumberland) New Brunswick, 17, 22, 36-37, 45, 154, 264, 277, 281 Beaver River, Nova Scotia, 197 Bedford Basin, Nova Scotia, 100 Belleisle, Annapolis County, Nova Scotia, 313 Biggs House, Gaspreau, Nova Scotia, 244-245 Blomidon, Cape, Nova Scotia, 21, 27 Boston, Massachusetts, 18, 30-31, 50, 66, 69, 76, 78, 81-82, 84, 86, 89, 99, 121, 141, 172, 176, 215, 265 Boudreau's Bank, (Starr's Point) Nova Scotia, 27 Bridgetown, Nova Scotia, 196, 316 Buckram (Ship), 48 Bucks Harbor, Maine, 174 Burton, New Brunswick, 33 Calkin House, Kings County, 250, 252, 259 Camphill (Rout), 43-45, 48, 52 Canning, Nova Scotia, 236, 240 Canso, Nova Scotia, 23 Cape Breton, Nova Scotia, 40, 114, 119, 134, 138, 140, 143-144 2 Cape Cod-Style House, 223 -
Newer Chelsea, As Distinct from Old Chelsea
/ A TALE OF TWO CHELSEAS The following pages are about the newer Chelsea, as distinct from Old Chelsea. The area covered is the road between the two Chelseas (once designated as High Street), and along the highway (11/105" ) between Mile Hill to the Chelsea Pioneer Cemetery. Also included are some offshoot roads where there are farms and other habitations of historic interest. 'For the purpose of this tale the highway from Hull to Maniwaki is shown as 11/105. This highway was known for many years as No. 11, but is currently No. 105 73 - The Road From Wright's Town (Hull) to Chelsea Joseph Bouchette in his book "A Topographical Dictionary of the Province of Lower Canada", published in London in 1832, describes Philemon Wright's method of road construction. "This road is called Britannia [now Aylmer] Road and extends seven miles. Being the first road made in this township, the mode of forming it may be interesting as well as useful; Mr. Wright first marked it out as far as the lake [Deschenes], then ploughed it on each side and threw the earth to the centre to form the top into low places, built bridges and paved the road, where necessary, with broken stones; he also built stores at each end for the deposit of different kinds of goods for the accommodation of the upper country. From Columbia Farm two roads branch off in different directions. One, passing along the edge of Columbia Pond [now Leamy Lake], leads to the Gatineau Farm, remarkable as being the spot selected by Mr.