Toronto Ontario Canada Business directory Metrolinx 2 History Toronto is home to several sports venues most notably the Rogers Centre the Scotiabank Arena and BMO Field which are all current venues the Maple Leaf Gardens is perhaps Toronto's best known former sporting venue as it was the home of the Toronto Maple Leafs of the National Hockey League (NHL) for much of said team's history the Gardens were later converted to a grocery and liquor store for the first two floors respectively as well as clothing on the second floor and its upper floor a smaller arena the Mattamy Athletic Centre for the Ryerson Rams hockey team as well as for basketball matches in the 2015 Pan American Games Other sports venues in Toronto include the Coca-Cola Coliseum (formerly known as the Ricoh Coliseum) The Golden Horseshoe (including Toronto) saw construction of new venues for the 2015 Pan American Games and the 2015 Parapan American Games as well as renovations to existing venues Permanent venues constructed for the Pan American Games include Toronto Pan Am Sports Centre and the York Lions Stadium at York University Transportation architecture. Stony Point Light Markham Green tick Green tick, 10 Canada West The Toronto District School Board (TDSB; known as English-language Public District School Board No 12 prior to 1999) is the English-language public-secular school board for Toronto Ontario Canada the minority public-secular francophone (Conseil scolaire Viamonde) public-separate anglophone (Toronto Catholic District School Board) and public-separate francophone (Conseil scolaire catholique MonAvenir) communities of Toronto also have their own publicly funded school boards and schools that operate in the same area but which are independent of the TDSB Its headquarters are in the district of North York The TDSB was founded on January 20 1953 as the Metropolitan Toronto School Board (MTSB) as a "super-ordinate umbrella board" to coordinate activities and to apportion tax revenues equitably across the six anglophone and later a francophone school boards within Metro Toronto the MTSB was reorganized and replaced on January 1 1998 when the six anglophone metro school boards and MTSB merged to form the Toronto District School Board the francophone school board of MTSB was amalgamated with several other Francophone school boards in the region to form Conseil scolaire Viamonde Today the TDSB is Canada's largest school board and the fourth largest school board in North America Contents; Other Christians 1,224,300 9.7 Hospitality & Tourism Management General manager Ali Curtis. Charlotte-Genesee Lighthouse 3.2 Line 6 Finch West 5.2.3 Ryerson and the Methodists Louisa St School (1852). .
. . 2011 12,851,821 +5.7% Withrow Park: Beavers Britch Gang Graphic Gang (Rogers refers to at least 4 other unnamed gangs in this area), History western part of Whitchurch 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. Lake Ontario is the easternmost of the Great Lakes and the smallest in surface area (7,340 sq mi 18,960 km2), although it exceeds Lake Erie in volume (393 cu mi 1,639 km3) It is the 13th largest lake in the world When its islands are included the lake's shoreline is 712 miles (1,146 km) long As the last lake in the Great Lakes' hydrologic chain Lake Ontario has the lowest mean surface elevation of the lakes at 243 feet (74 m) above sea level; 326 feet (99 m) lower than its neighbor upstream Its maximum length is 193 statute miles (311 kilometres; 168 nautical miles) and its maximum width is 53 statute miles (85 km; 46 nmi) the lake's average depth is 47 fathoms 1 foot (283 ft; 86 m) with a maximum depth of 133 fathoms 4 feet (802 ft; 244 m) the lake's primary source is the Niagara River draining Lake Erie with the St Lawrence River serving as the outlet the drainage basin covers 24,720 square miles (64,030 km2) as with all the Great Lakes water levels change both within the year (owing to seasonal changes in water input) and among years (owing to longer term trends in precipitation) These water level fluctuations are an integral part of lake ecology and produce and maintain extensive wetlands the lake also has an important freshwater fishery although it has been negatively affected by factors including over-fishing water pollution and invasive species Baymouth bars built by prevailing winds and currents have created a significant number of lagoons and sheltered harbors mostly near (but not limited to) Prince Edward County Ontario and the easternmost shores Perhaps the best-known example is Toronto Bay chosen as the site of the Upper Canada (Ontario) capital for its strategic harbour Other prominent examples include Hamilton Harbour Irondequoit Bay Presqu'ile Bay and Sodus Bay the bars themselves are the sites of long beaches such as Sandbanks Provincial Park and Sandy Island Beach State Park These sand bars are often associated with large wetlands which support large numbers of plant and animal species as well as providing important rest areas for migratory birds. Presqu'ile on the north shore of Lake Ontario is particularly significant in this regard One unique feature of the lake is the Z-shaped Bay of Quinte which separates Prince Edward County from the Ontario mainland save for a 2-mile (3.2 km) isthmus near Trenton; this feature also supports many wetlands and aquatic plants as well as associated fisheries Major rivers draining into Lake Ontario include the Niagara River Don River Humber River Trent River Cataraqui River Genesee River Oswego River Black River Little Salmon River and the Salmon River Geology. .
Greenblatt, Pierce, Funt and Flores