George St School (1853) Appalachian mountains from Mount Carleton Provincial Park New Brunswick lies entirely within the Appalachian Mountain range All of the rivers of New Brunswick drain into the Gulf of Saint Lawrence to the east or the Bay of Fundy to the south These watersheds include lands in Quebec and Maine New Brunswick and the rest of the Maritime Peninsula was covered by thick layers of ice during the last glacial period (the Wisconsinian glaciation) it cut U-shaped valleys in the Saint John and Nepisiguit River valleys and pushed granite boulders from the Miramichi highlands south and east leaving them as erratics when the ice receded at the end of the Wisconsin glaciation along with deposits such as the eskers between Woodstock and St George today sources of sand and gravel Demographics, Perth 9 Culture Satellite image during late autumn. . . Hopewell Rocks are rock formations located at the upper reaches of the Bay of Fundy near Hopewell Cape Bedrock types range from 1 billion to 200 million years old. Much of the bedrock in the west and north derives from ocean deposits in the Ordovician that were subject to folding and igneous intrusion and that were eventually covered with lava during the Paleozoic peaking during the Acadian orogeny During the Carboniferous era about 340 million years ago New Brunswick was in the Maritimes Basin a sedimentary basin near the equator Sediments brought by rivers from surrounding highlands accumulated there; after being compressed they produced the Albert oil shales of southern New Brunswick Eventually sea water from the Panthalassic Ocean invaded the basin forming the Windsor Sea Once this receded conglomerates sandstones and shales accumulated the rust colour of these was caused by the oxidation of iron in the beds between wet and dry periods. Such late carboniferous rock formed the Hopewell Rocks which have been shaped by the extreme tidal range of the Bay of Fundy In the early Triassic as Pangea drifted north it was rent apart forming the rift valley that is the Bay of Fundy Magma pushed up through the cracks forming basalt columns on Grand Manan Topography.
; . Glendon College (Toronto) 1990 55 2008 Aboriginal 198,140 2.2% 3 History New City Hall Toronto 1 (8030180482).jpg 7.1 Federal politics. After the Rebellions the new governor Charles Poulett Thomson 1st Baron Sydenham proved an exemplary Utilitarian despite his aristocratic pretensions This combination of free trade and aristocratic pretensions needs to be underscored; although a liberal capitalist Sydenham was no radical democrat Sydenham approached the task of implementing those aspects of Durham's report that the colonial office approved of municipal reform and the union of the Canadas with a "campaign of state violence and coercive institutional innovation . empowered not just by the British state but also by his Benthamite certainties." Like governors Bond Head before him and Metcalfe after he was to turn to the Orange Order for often violent support it was Sydenham who played a critical role in transforming Compact Tories into Conservatives Sydenham introduced a vast expansion of the state apparatus through the introduction of municipal government Areas not already governed through civic corporations or police boards would be governed through centrally controlled District Councils with authority over roads schools and local policing a strengthened Executive Council would further usurp much of the elected assembly's legislative role leaving elected politician's to simply review the administration's legislative program and budgets Settlement.
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