Norman Wohlgemuth Chandler Jeter

Development of the Great Lakes following the end of the Last Glacial Period the first human settlers arrived in the area 11,000 to 10,500 years ago as the glaciers retreated from the area Toronto remained under glacial ice throughout the Last Glacial Period with the glacial ice retreating from the area during the Late Glacial warming period approximately 13,000 BCE Following the Last Glacial Period Toronto's waterfront shifted with the growth and later contraction of glacial Lake Iroquois the area saw its first human settlers around 9000 BCE to 8,500 BCE These settlers traversed large distances in family-sized bands sustaining themselves on caribou mammoths mastodons and smaller animals in the tundra and Boreal forest. Many of their archaeological remains lie in present-day Lake Ontario with the historic coastline of Lake Iroquois situated 20 kilometres (12 mi) south of Toronto during this period As the climate warmed in 6,000 BCE the environment of Toronto shifted to a temperate climate the Toronto waterfront also changed dramatically during this period with erosion from the Scarborough Bluffs accumulating and rising water levels from Lake Ontario creating a peninsula that would later become the Toronto Islands First Nations settlements. Energy As of January 30 2019 Catholic 3,976,610 31.4 2018 Sheridan College (Brampton Mississauga Oakville) 2.3 Commuter rail and buses Ottawa Senators Ice hockey NHL Ottawa Canadian Tire Centre.

. . 2008 20,108 4.1 Alumni Main article: Architecture of Toronto, The Purchased was signed by Sir John Johnson William Claus (deputy superintendent of Indian Affairs representing the Crown) Witness consisted of:. .