. Coach Nation Tenure Record1 Windsor CMA (Lakeshore LaSalle) 307,877 323,342 319,246 329,144 3.1, 5.4 Houses of worship, Mural of the Toronto Maple Leafs at College subway station the Maple Leafs are a professional ice hockey club with the NHL Toronto is represented in five major league sports with teams in the National Hockey League Major League Baseball National Basketball Association Canadian Football League and Major League Soccer it was formerly represented in a sixth and seventh; the USL W-League that announced on November 6 2015 that it would cease operation ahead of 2016 season and the Canadian Women's Hockey League ceased operations in May 2019 the city's major sports venues include the Scotiabank Arena (formerly Air Canada Centre) Rogers Centre (formerly SkyDome) Coca-Cola Coliseum (formerly Ricoh Coliseum) and BMO Field Professional sports. Coach Nation Tenure Record1 Record Greta Dale - muralist 28 Goalkeeper Caleb Patterson-Sewell United States, Main article: Geography of Ontario vte 1.2.1 French colony. . The Toronto Maple Leafs acknowledge an affiliation with 75 inductees of the Hockey Hall of Fame the 75 inductees include 62 former players as well as 13 builders of the sport the Maple Leafs have the greatest number of players inducted in the Hockey Hall of Fame of any NHL team the 13 individuals recognized as builders of the sport include former Maple Leafs broadcasters executives head coaches and other personnel relating to the club's operations Inducted in 2017 Dave Andreychuk was the latest Maple Leafs player to be inducted in the Hockey Hall of Fame In addition to players and builders five broadcasters for the Maple Leafs were also awarded the Foster Hewitt Memorial Award from the Hockey Hall of Fame in 1984 Foster Hewitt a radio broadcaster was awarded the Hall of Fame's inaugural Foster Hewitt Memorial Award an award named after Hewitt Hewitt was already inducted as a builder in the Hall of Fame prior to the award's inception. Other Maple Leafs broadcasters that received the award include Wes McKnight in 1986 Bob Cole in 2007 Bill Hewitt in 2007 and Joe Bowen in 2018 Designed in the Beaux-Art style Union Station was completed in 1927 [icon].
. N Amanah Islamic Academy HMS Sir Issac Brock being built in York Both sides engaged in building freshwater fleets in an effort to gain naval supremacy in Lake Ontario York the capital of Upper Canada stood on the north shore of Lake Ontario During the War of 1812 the lake was both the front line between Upper Canada and the United States and served as the principal British supply line from Quebec to the various forces and outposts to the west At the start of the war the British had a small naval force the Provincial Marine with which they seized control of the Lake Ontario and Lake Erie This was made it possible because of Major General Isaac Brock who led British forces in Upper Canada to several important victories in 1812 by shifting his small force rapidly between threatened points to defeat disjointed American attacks individually The United States Navy appointed Commodore Isaac Chauncey to regain control of the lakes He created a squadron of fighting ships at Sackett's Harbor New York by purchasing and arming several lake schooners and laying down new purpose-built fighting vessels However no decisive action was possible before the onset of winter during which the ships of both sides were confined to harbour by ice to match Chauncey's shipbuilding efforts the British laid down the sloop of war Wolfe at Kingston; and HMS Sir Isaac Brock at York Naval Shipyards Prelude. 71 2415 Satellite image of Toronto and surrounding area Urban area's of the city are interrupted by the Toronto ravine system The city is mostly flat or gentle hills and the land gently slopes upward away from the lake the flat land is interrupted by the Toronto ravine system which is cut by numerous creeks and rivers of the Toronto waterway system most notably the Humber River in the west end and the Don River east of downtown at opposite ends of Toronto Harbour and the Rouge River at the city's eastern limits Most of the ravines and valley lands in Toronto today are parklands and recreational trails are laid out along the ravines and valleys the original town was laid out in a grid plan on the flat plain north of the harbour and this plan was extended outwards as the city grew the width and depth of several of the ravines and valleys are such that several grid streets such as Finch Avenue Leslie Street Lawrence Avenue and St Clair Avenue terminate on one side of a ravine or valley and continue on the other side Toronto has many bridges spanning the ravines Large bridges such as the Prince Edward Viaduct were built to span wide river valleys Despite its deep ravines Toronto is not remarkably hilly but its elevation does increase steadily away from the lake Elevation differences range from 76.5 metres (251 ft) above sea level at the Lake Ontario shore to 209 m (686 ft) ASL near the York University grounds in the city's north end at the intersection of Keele Street and Steeles Avenue. There are occasional hilly areas; in particular midtown Toronto has a number of sharply sloping hills Lake Ontario remains occasionally visible from the peaks of these ridges as far north as Eglinton Avenue 7 to 8 kilometres (4.3 to 5.0 mi) inland The Scarborough Bluffs is an escarpment along the eastern portion of the Toronto waterfront which formed during the last glacial period The other major geographical feature of Toronto is its escarpments During the last ice age the lower part of Toronto was beneath Glacial Lake Iroquois Today a series of escarpments mark the lake's former boundary known as the "Iroquois Shoreline" the escarpments are most prominent from Victoria Park Avenue to the mouth of Highland Creek where they form the Scarborough Bluffs Other observable sections include the area near St Clair Avenue West between Bathurst Street and the Don River and north of Davenport Road from Caledonia to Spadina Road; the Casa Loma grounds sit above this escarpment The geography of the lakeshore is greatly changed since the first settlement of Toronto Much of the land on the north shore of the harbour is landfill filled in during the late 19th century Until then the lakefront docks (then known as wharves) were set back farther inland than today Much of the adjacent Port Lands on the east side of the harbour was a wetland filled in early in the 20th century the shoreline from the harbour west to the Humber River has been extended into the lake Further west landfill has been used to create extensions of land such as Humber Bay Park The Toronto Islands were a natural peninsula until a storm in 1858 severed their connection to the mainland, creating a channel to the harbour the peninsula was formed by longshore drift taking the sediments deposited along the Scarborough Bluffs shore and transporting them to the Islands area the other source of sediment for the Port Lands wetland and the peninsula was the deposition of the Don River which carved a wide valley through the sedimentary land of Toronto and deposited it in the shallow harbour the harbour and the channel of the Don River have been dredged numerous times for shipping the lower section of the Don River was straightened and channelled in the 19th century the former mouth drained into a wetland; today the Don drains into the harbour through a concrete waterway the Keating Channel Climate, 4.1 Latter 19th century the Imagination Catalyst directed by the AVP Research and Graduate Studies and coordinated by the Digital Futures Implementation office which provides incubator support for students alumni and faculty and was established in August 2011 through the merger of the Digital Futures Accelerator and the Design Incubator; and. . .
Toronto Pearson International Airport