Eastern Ontario

Coordinates: 45°N 75°W / 45°N 75°W / 45; -75
Source: Wikipedia, the free encyclopedia.
Eastern Ontario
Est de l'Ontario (
613/343

Eastern Ontario (census population 1,763,186 in 2016) (

Vaudreuil-Soulanges
region of Quebec to the east.

It includes the cities of

Lennox and Addington
.

Some sources may also include Hastings, Prince Edward, and occasionally Northumberland in the definition of Eastern Ontario, but others classify them as Central Ontario.

The region may also be referred to as Southeastern Ontario to differentiate it from the Northern Ontario secondary region of Northeastern Ontario.

History

French explorers and

fur traders were the first recorded Europeans to pass through this region. Samuel de Champlain, explorer, traversed the Ottawa River in 1615 on his way westward to the Great Lakes. The largest city in the region is the city of Ottawa, capital of Canada, which accounts for roughly 60% of Eastern Ontario's population. Kingston, itself once capital of the Province of Canada, is another city in the region outside of the National Capital Region
.

Much of the remainder of the region relies on agriculture and tourism. Heavier reliance on recreation and tourism exists in the more rugged Renfrew county in the northwest of Eastern Ontario.

Downtown Ottawa

Of all Ontario's regions, parts of Eastern Ontario are the most heavily influenced by the

United Empire Loyalists, American settlers who moved to Upper Canada out of loyalty to the British Crown during and after the American Revolutionary War
. The Loyalist influence has a presence in the counties of Stormont, Dundas, Leeds and Grenville, Frontenac, Hastings, and Prince Edward.

In Ottawa, Prescott and Russell, Glengarry, and Renfrew, Eastern Ontario is home to the largest

Franco-Ontarian
community within Ontario.

Extensive immigration by

lumber industry
.

Through the last century, newer immigrant groups, both Francophone and non-Francophone, have added to the cultural diversity, mostly in Ottawa. There are a large number of Francophones in Eastern Ontario, especially in Prescott and Russell United Counties. Following the

Second World War
, there was a massive influx of Dutch immigrants to Canada, with many settling in communities in Eastern Ontario, particularly in Dundas, Stormont, and Grenville.

Climate

The climate of Eastern Ontario is humid continental with large seasonal variation. Snow and ice are dominant during the winter season. Ottawa receives close to 250 cm (100 in) of snowfall over an average winter.

Winters are long and celebrated in Eastern Ontario. The average temperature in January is 21 °F (-6 °C). In recent years, there has been winters with snow free periods lasting into early January. However, in the winter months of 2008 and 2019, there were records levels of snow fall.

Ice storms are also relatively common, especially on lower terrain if compared with other parts of the country. One such large storm caused vast power outages and affected the local economy, known as the

Renfrew County
than further south along the Upper St. Lawrence River shoreline.

Summers are fairly hot and humid in the

St. Lawrence valleys
. The average July maximum temperature is 80 °F (27 °C). Temperatures occasionally exceed 35 °C (95 °F), and during periods of hot weather, high humidity is often an aggravating factor, pushing the temperature into the 100 °F (40 °C) with the humidex. Thunderstorms are on occasion severe, causing tree and property damage.

Spring and fall (especially spring) are changeable seasons, prone to extremes in temperature and unpredictable swings in conditions. Average annual precipitation is around 950 mm (37 in.).

Geography

Thousand Islands

The eastern section of Eastern Ontario, that is east and southeast of Ottawa, including the towns of Cornwall, Embrun and Hawkesbury is generally a flat plain, dotted with some extensive woodlots and boggy marshes, but is primarily farmland. Certain sections here are prone to low-lying flooding and spring ice jams, particularly on the banks of the South Nation River.

The Laurentian Highlands, which form a small section of the extensive Canadian Shield, cuts through the western section from the Upper Ottawa River valley southeast toward to the St. Lawrence River around Gananoque. Here sedimentary rock can be found folding over the Shield. This is also the portion where the greatest concentration of inland lakes are found. In Renfrew County, this higher terrain is called the 'Madawaska Highlands' after a major river that bisects these hills. Some highland peaks are over 400 m higher than the Ottawa River. The picturesque area of the St. Lawrence River bordering New York State is known as the Thousand Islands region reflected by its numerous small islands. The bulk of the Laurentian Upland is located just to the north of the Ottawa River in adjacent Quebec and covers a vastly larger area within that province.

Along the extreme western edge of Eastern Ontario is a continuation of the Laurentian Highlands, known as the Opeongo Hills, and they contain some of the highest elevations in Southern Ontario. They stretch into the northern portions of Central Ontario, near Algonquin Provincial Park.

Ottawa is at the confluence of the Rideau River and Ottawa River. A series of rugged rapids and waterfalls are found along these rivers in Ottawa. Most of the underlying rock in and around the city of Ottawa is limestone bedrock, also found in abundance farther south around Kingston. Limestone was used during the construction of the Rideau Canal, which connects Kingston and Ottawa by water and was also heavily used as the building blocks for many governmental and other buildings in both cities.

The Ottawa and St. Lawrence Rivers do not actually converge in Ontario. A small portion of

Vaudreuil-Soulanges
, lies between the Ontario-Quebec border and the river junction. The region has a land border with Ontario, but it is necessary to cross water to reach any other part of Quebec.

Geology

The Eastern Ontario region has a history of earthquakes. Several faults run through the region, and the area is near both the Western Quebec Seismic Zone and the Saint Lawrence rift system. Minor earthquakes occur in the region regularly, most of them too weak to be felt by people. More severe earthquakes, around 5–6 on the Richter magnitude scale, occur every sixty years, on average. The most recent of the earthquakes occurred in 2010. This earthquake, known as the 2010 Central Canada earthquake although it caused some power outages and minor damage to older buildings, did not cause significant damage because buildings in the area are required to be earthquake resistant by government regulations. The earthquake caused significant panic amongst the population, though: office buildings were evacuated in Ottawa, transit routes shut down, and in the minutes after the quake, cell phone service was down, as it was overloaded with calls made by panicked people attempting to talk to friends and relatives. Although the reaction was ridiculed by many, if buildings in the area were not designed to be earthquake-resistant, it would have caused significant damage. A similar earthquake in 1944 caused significant damage to buildings in Cornwall, as it was before earthquake-resistant architecture became common.

Education

Queens Theological Hall

The region is home to several

La Cité collégiale, and St. Lawrence College
.

Algonquin College has campuses in Ottawa, Perth, Pembroke, Hawkesbury, and Renfrew, while St. Lawrence College has campuses in Kingston, Cornwall, and Brockville.

Administrative divisions

Single-tier municipalities

Separated municipalities

Counties

  • Frontenac County
  • Lanark County
  • United Counties of Leeds and Grenville
  • Lennox and Addington County
  • United Counties of Prescott and Russell
  • Renfrew County
  • United Counties of Stormont, Dundas and Glengarry

Major urban areas

Name of Population Centre Population (2016)[1]
Ottawa 989,567
Kingston 117,660
Belleville 67,666
Cornwall 45,723
Brockville 21,854
Pembroke 15,940
Petawawa 13,701
Rockland 12,302
Carleton Place 11,936
Hawkesbury 11,715
Arnprior 10,426
Smiths Falls 8,885
Renfrew 8,152
Napanee 7,439
Embrun 6,918
Manotick Station 5,738
Perth 5,573
Gananoque 5,159
Almonte 5,039
Picton 4,702
Russel 4,464
Richmond 4,055
Prescott 3,965
Kemptville 3,911
Deep River 3,658
Casselman 3,563
Alexandria
2,924
Frankford 2,825
Osgoode 2,578

References

  1. ^ "Census Profile, 2016". Statistics Canada. 8 February 2017. Archived from the original on 2017-02-10.

External links

45°N 75°W / 45°N 75°W / 45; -75