Opasquia Provincial Park | |
---|---|
Location | Ontario, Canada |
Coordinates | 53°32′N93°05′W / 53.533°N 93.083°W Coordinates: 53°32′N93°05′W / 53.533°N 93.083°W |
Area | 473,000 ha (1,170,000 acres) |
Established | 1983 [1] |
www |
The Opasquia Provincial Park is located in Northwest Ontario, Canada. Situated alongside the Manitoba boundary, this remote park is approximately 473,000 hectares (1,170,000 acres) in size. The Opasquia park is home to many different species of plants and animals.
Located approximately 245 kilometres (152 mi) north of Red Lake, Ontario, the Opasquia has no road access, even during the winter highway season. The park is accessible by float plane only. Hundreds of lakes and dozens of rivers flow northwest through this 473,000-hectare (1,170,000-acre) park. The northwestern water flow is considered an anomaly[ according to whom? ] due to the fact all other bodies of water in Ontario flow northeast[ citation needed ] towards Hudson Bay and James Bay. This can be attributed to the Cocos Plateau formed from glaciers during the last ice age.
The reason the Opasquia Park has been protected as a wilderness park has more to do with its distinctive geology. A ridge of glacial till two kilometres wide rises 100 metres above its surroundings here. This is called the Opasquia Moraine. On the sides of the moraine, wave-cut terraces and segments of raised shoreline indicate the former limit of glacial Lake Agassiz. [2]
The wolverine population is what makes this park unique. Opasquia Provincial Park supports one of the largest concentration of wolverines in North America. The park also has large numbers of moose, bear, eagles, otters, beavers, and wolves. Hundreds of others species of birds have been identified, and northern pike and walleye dominate the fisheries in this park. Whitefish and perch have also been found in its waters.
This park is a non-operating park, which means it does not have any visitors’ facilities. There is one known fly-in tourist operation located within the park named Big Hook Wilderness Camps . The resort caters to fisherman and nature lovers.
Lake Abitibi is a shallow lake in northeastern Ontario and western Quebec, Canada. The lake, which lies within the vast Clay Belt, is separated in two distinct portions by a short narrows, making it actually 2 lakes. Its total area is 931 square kilometres (359 sq mi), and net area 903 square kilometres (349 sq mi). The lake is shallow and studded with islands. Its shores and vicinity are covered with small timber.
The Oak Ridges Moraine is an ecologically important geological landform in the Mixedwood Plains of south-central Ontario, Canada. The moraine covers a geographic area of 1,900 square kilometres (730 sq mi) between Caledon and Rice Lake, near Peterborough. One of the most significant landforms in southern Ontario, the moraine gets its name from the rolling hills and river valleys extending 160 km (99 mi) from the Niagara Escarpment east to Rice Lake. It was formed 12,000 years ago by advancing and retreating glaciers. The moraine is a contested site in Ontario, since it stands in the path of major urban development.
A kettle is a depression/hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased friction. The ice becomes buried in the sediment and when the ice melts, a depression is left called a kettle hole, creating a dimpled appearance on the outwash plain. Lakes often fill these kettles; these are called kettle hole lakes. Another source is the sudden drainage of an ice-dammed lake. When the block melts, the hole it leaves behind is a kettle. As the ice melts, ramparts can form around the edge of the kettle hole. The lakes that fill these holes are seldom more than 10 m (33 ft) deep and eventually fill with sediment. In acid conditions, a kettle bog may form but in alkaline conditions, it will be kettle peatland.
The Ogoki River is a river in the Thunder Bay and Cochrane Districts of Ontario. It springs from the wilderness just east of Savant Lake, flowing north of Lake Nipigon to Ogoki, where it joins the Albany River which empties into James Bay. The river is 480 kilometres (300 mi) long.
The Amable du Fond River is a river in Nipissing District, in Northern Ontario, Canada.
The Southern Laurentian Channel is an ancient underground river in southern Ontario, Canada. The river predates the recent ice ages. The river valley was filled with glacial debris. Water still flows down this old valley—underground. The source of the aquifer is the Georgian Bay, approximately 200 kilometres (120 mi) away.
Wabakimi Provincial Park is a wilderness park located to the northwest of Lake Nipigon and northwest of Armstrong Station in the province of Ontario, Canada. The park contains a vast and interconnected network of more than 2,000 kilometres of lakes and rivers. The park covers an area of 8,920 square kilometres (3,440 sq mi) and became the second largest park in Ontario and one of the world's largest boreal forest reserves following a major expansion in 1997. A number of local citizen groups and residents, including Bruce Hyer have been instrumental in the creation, expansion, and preservation of this region.
The Albany River is a river in Northern Ontario, Canada, which flows northeast from Lake St. Joseph in Northwestern Ontario and empties into James Bay. It is 982 kilometres (610 mi) long to the head of the Cat River, tying it with the Severn River for the title of longest river in Ontario. Major tributaries include the Kenogami River and Ogoki River.
Awenda Provincial Park is a provincial park in Tiny Township, Simcoe County in Central Ontario, Canada, located on a peninsula jutting into Georgian Bay north of Penetanguishene. The park occupies an area of 2,915 hectares and was established in 1975. It is classified as a Natural Environment Park and therefore all land is protected.
The Waterloo Moraine is a landform and sediment body that was created as a moraine in the Regional Municipality of Waterloo, in Ontario, Canada. It covers a large portion of the cities of Waterloo and Kitchener and the township of Wilmot, and some parts of the townships of Wellesley and North Dumfries. About 90% of the water supply of the Regional Municipality of Waterloo is derived from groundwater of the Waterloo Moraine aquifer system.
Ontario Parks is the Ontario government agency in Ontario, Canada, that protects significant natural and cultural resources in a system of parks and protected areas that is sustainable and provides opportunities for inspiration, enjoyment and education. The Ontario Parks system covers over 78,000 square kilometres (30,000 sq mi), which is about 10 percent of the province's surface area or the equivalent of an area approximately equal to Nova Scotia. It falls under the responsibility and mandate of the province's Ministry of the Environment, Conservation and Parks. It was formerly under the mandate of the Ministry of Natural Resources and Forestry.
The White River is a tributary of Lake Superior in Thunder Bay District, Ontario, Canada. It starts at Negwazu Lake and flows in a predominantly western direction to Lake Superior, passing through the Township of White River.
Rouge National Urban Park is a national urban park in Ontario, Canada. The park is centred around the Rouge River and its tributaries in the Greater Toronto Area. The southern portion of the park is situated around the mouth of river, in Scarborough, and extends northwards into Markham, Pickering, Uxbridge, and Whitchurch-Stouffville.
The Obabika River Provincial Park is a provincial park in Ontario, Canada, straddling across the boundaries of the Sudbury, Nipissing, and Timiskaming Districts. While it is named after and includes the Obabika River, the bulk of the park extends north of Obabika Lake to the eastern boundary of Lady Evelyn-Smoothwater Provincial Park.
Hamilton is located on the western end of the Niagara Peninsula and wraps around the westernmost part of the Lake Ontario. Most of the city including the downtown section lies along the south shore. Situated in the geographic centre of the Golden Horseshoe, it lies roughly midway between Toronto and Buffalo. The two major physical features are Hamilton Harbour marking the northern limit of the city and the Niagara Escarpment running through the middle of the city across its entire breadth, bisecting the city into 'upper' and 'lower' parts.
The Toronto ravine system is a distinctive feature of the city's geography, consisting of a network of deep ravines, which forms a large urban forest that runs through most of Toronto. The ravine system is the largest in any city in the world, with the Ravine and Natural Feature Protection Bylaw protecting approximately 110 square kilometres (42 sq mi) of public and privately-owned land. The ravine system has been presented as a central characteristic of the city, with the size of the ravine system leading Toronto to be described as "a city within a park".
The Temagami River, formerly spelled as Timagami River, is a river in the Nipissing District of Ontario, Canada, in the Temagami region. Its source is Lake Temagami and flows through Cross Lake and Red Cedar Lake. It flows into the Sturgeon River at the community of River Valley.
The Toronto waterway system comprises a series of natural and man-made watercourses in the Canadian city of Toronto. The city is dominated by a large river system spanning most of the city including the Don River, Etobicoke Creek, Highland Creek, Humber River, Mimico Creek and Rouge River.
Mira River Provincial Park is a provincial park situated on the Mira River in Cape Breton County, 22 kilometres (14 mi) from Sydney and 17 kilometres (11 mi) kilometres from the Fortress of Louisbourg National Historic Site of Canada. Opened in 1967, the 87.49 hectares property offers camping sites and a range opportunities for outdoor recreation including picnicking, swimming, canoeing, kayaking, biking, front-country hiking, walking, boat ramp, fishing, cross-country skiing, snowshoeing, and geocaching. Lands were initially acquired for the park in 1962, with major acquisitions occurring in 1968 and 1973. The property was designated under the Provincial Parks Act by Order in Council on 12 June 1984.
Carden Alvar Provincial Park is a provincial park located in the Kawartha Lakes in Central Ontario, Canada. Alvars are globally rare ecosystems found exclusively in Northern Europe and the Great Lakes region of North America. The park is classified as a non-operating, natural environment park and was established in 2014. Natural environment parks protect outstanding landscapes, ecosystems and other elements of the province's wilderness to provide high quality recreational and educational experiences for visitors.