The Humber River in Toronto
|District||Dufferin County, Regional Municipality of Peel, Simcoe County, Regional Municipality of York|
|Municipalities||Toronto, Adjala-Tosorontio, Brampton, Caledon, King, Mono, Vaughan|
|Source||Humber Springs Ponds|
|⁃ location||Mono, Dufferin County|
|⁃ elevation||421 m (1,381 ft)|
|Mouth||Humber Bay, Lake Ontario|
|74 m (243 ft)|
|Length||100 km (62 mi)|
|Basin size||903 km2 (349 sq mi)|
|Great Lakes Basin|
The Humber River is a river in Southern Ontario, Canada. It is in the Great Lakes Basin, is a tributary of Lake Ontario and is one of two major rivers on either side of the city of Toronto, the other being the Don River to the east. It was designated a Canadian Heritage River on September 24, 1999.
The Humber collects from about 750 creeks and tributaries in a fan-shaped area north of Toronto that encompasses portions of Dufferin County, the Regional Municipality of Peel, Simcoe County, and the Regional Municipality of York. The main branch runs for about 100 kilometres (60 mi) from the Niagara Escarpment in the northwest, while another major branch, known as the East Humber River, starts at Lake St. George in the Oak Ridges Moraine near Aurora to the northeast. They join north of Toronto and then flow in a generally southeasterly direction into Lake Ontario at what was once the far western portions of the city. The river mouth is flanked by Sir Casimir Gzowski Park and Humber Bay Park East.
The river was named "Cobechenonk", for "leave the canoes and go back", by the area's most recent native inhabitants, the Anishinaabe. A French map from 1688 called the river "passage de taronto", while Popple's map of 1733 shows the "Tanaovate River" beside the native settlement of Tejajagon.
The Humber has a long history of human settlement along its banks. Native settlement of the area is well documented archaeologically and occurred in three waves. The first settlers were the Palaeo-Indians who lived in the area from 10,000 to 7000 BC. The second wave, people of the Archaic period, settled the area between 7000 and 1000 BC and began to adopt seasonal migration patterns to take advantage of available plants, fish, and game. The third wave of native settlement was the Woodland period, which saw the introduction of the bow and arrow and the growing of crops which allowed for larger, more permanent villages. The Woodland period was also characterized by movement of native groups along what is known today as the Toronto Carrying-Place Trail, running from Lake Ontario up the Humber to Lake Simcoe and eventually to the northern Great Lakes.
It is believed that Étienne Brûlé was the first European to encounter the Humber while travelling the Toronto Carrying-Place Trail. Brûlé passed through the watershed in 1615 on a mission from Samuel de Champlain to build alliances with native peoples, but left no written record. The Trail became a convenient shortcut to the upper Great Lakes for traders, explorers, and missionaries. A major landmark on the northern end of the trail in Lake Simcoe was used to describe the trail as a whole, and eventually the southern end became known simply as "Toronto" to the Europeans. During the 1660s this was the site of Teiaiagon, a permanent settlement of the Seneca used for trading with the Europeans. Popple's map of 1733 shows a prominent river beside "Tejajagon" which is assumed to be the Humber.
During late-17th and 18th century, the portage along this river was frequently used by the French traders as a short cut to the upper Great Lakes and the area north of Toronto. In an attempt to secure the trade route from the British, the French established Magasin Royal, a trading post along the Humber River, near Baby Point. Completed in 1720, the trading post was abandoned shortly after the British fort in Oswego, New York was completed, as it diverted trade away from Magasin Royal.
In 1750, the French built another fort near the mouth of the Humber River, with the intention of diverting aboriginals using the Toronto Carrying-Place Trail from proceeding to the British in Fort Oswego. Known as Fort Toronto, the fort saw immediate success, with demand outstripping the supply of goods the Fort was able to provide. The success of the fort persuaded the Governor General of New France, Jacques-Pierre de Taffanel de la Jonquière, Marquis de la Jonquière to order the construction of a larger fort, with more trading capacity and military potential, in an effort to consolidate its hold of the region, and its trade routes. Fort Rouillé, located in present-day Exhibition Place (east of the Humber River), was completed in the spring of 1751. The fort continued to operate until 1759, during the Seven Years' War. The fort's garrison was instructed to evacuate and burn Fort Rouille should Fort Niagara be captured. Following the French defeat at Fort Niagara in July 1759, the garrison at Fort Rouille burnt down the fort, and withdrew to Montreal.
However, no permanent European settlement occurred until the arrival of Jean-Baptiste Rousseau in the late 18th century. Rousseau piloted John Graves Simcoe's ship into Toronto Bay to officially begin the British era of control in 1793. Most of the British attention was focussed to the east of the Humber, around the protected Toronto Bay closer to the Don River. Settlement was scattered until after the War of 1812 when many loyalists moved to the area, who were joined by immigrants from Ireland and Scotland who chose to remain in British lands.
Upon his arrival in York, Simcoe was keenly aware of the need for a lumber mill and grist mill in the area. He had constructed a sawmill on the west bank of the river near present-day Bloor Street in 1793, which was operated by John Wilson. In 1797 Simcoe managed to get a grist mill established on the Humber River. It was owned and operated by John Lawrence. Over the years, numerous mills have been operated along the river by such men as William Cooper, W. P. Howland, Thomas Fisher, John Scarlett, William Gamble and Joseph Rowntree. The last grist mill on the Humber, Hayhoe Mills in Woodbridge, closed in 2007.
By 1860 the Humber Valley was extensively deforested. This decreased the stability of the river banks and increased damages done by periodic flooding. In 1878 a disastrous flood destroyed the remaining water powered mills. As the Toronto area grew, the lands around the Humber became important farming areas; in addition, some areas of the river's flood plain were developed as residential. This led to serious runoff problems in the 1940s, which the Humber Valley Conservation Authority was established to address. But in 1954, Hurricane Hazel raised the river to devastating flood levels, destroying buildings and bridges; on Raymore Drive, 60 homes were destroyed and 35 people were killed.
The Metropolitan Toronto and Region Conservation Authority (MTRCA later TRCA) succeeded the Humber Valley authority in 1957 (the word "Metropolitan" was dropped in 1998). More recently, a task force within the Authority was formed to further clear the Humber as a part of the Great Lakes 2000 Cleanup Fund.
The Humber River begins at Humber Springs Ponds on the Niagara Escarpment in Mono, Dufferin County and reaches its mouth at Humber Bay on Lake Ontario in the city of Toronto. The West Humber River goes through the Claireville Conservation Area, joining the east branch at Summerlea Park.
The Humber watershed is a hydrological feature of south-central Ontario, Canada, principally in north and west Toronto. It has an area of 903 square kilometres (349 sq mi), flowing through numerous physio-graphic regions, including the Oak Ridges Moraine and the Niagara Escarpment. The watershed is bounded on the west by the Credit River, Etobicoke Creek and Mimico Creek watersheds, and on the east by the Garrison Creek, Don River and Rouge River watersheds, all six of which empty into Lake Ontario; on the north by the Nottawasaga River which empties into Lake Huron; and on the northeast by the Holland River, which empties into Lake Simcoe.
Unlike the Don to the east, the Humber remained relatively free from industrialization as Toronto grew. Since the flooding of Hurricane Hazel, it has been largely developed or redeveloped as parkland, with the extensive and important wetlands on its southern end remaining unmolested. Whereas the mouth of the Don is often clogged with flotsam and is obstructed by low bridges, the Humber is navigable and used for recreation and fishing.
Today the majority of the Toronto portion of the Humber is parkland, with paved trails running from the lake shore all the way to the northern border of the city some 30 km away. Trails following the various branches of the river form some 50 km of bicycling trails, much of which are in decent condition. Similar trails on the Don tend to be narrower and in somewhat worse condition, but the complete set of trails is connected along the lake shore, for some 100 km of off-road paved trails.
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