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Natural History
of Belfountain, Ontario, Canada
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To suggest an item,artefact or photo reflecting Belfountain's natural history, please visit here.

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Atlantic Salmon
The Atlantic salmon were once abundant in the West Credit River which flows through Belfountain. Salmo Salar (salmon the leaper) is threatened throughout its shrinking north Atlantic habitat. David Keith, Jeff Collins, Mark Heaton and Frank Entwisle are local volunteers with the Belfountain Fish Hatchery. There group's aim is to encourage a community effort that will support federal and provincial efforts to bring back Atlantic salmon to the Credit River. Construction on the Belfountain Hatchery began in 2001-2002 when volunteers managed to release 6,000 advanced fry. Demonstration tanks were set up in local schools so students could learn about Atlantic salmon through history, science and social studies programs.

 


Belfountain Conservation Area
Belfountain Conservation Area is part of the
Credit Valley Conservation. For hikers, a short trail loops around the pond, while the Trimble Trail, a side trail of the Bruce Trail, stretches 3 km downstream with lookouts on the Niagara Escarpment. Charles W. Mack, the inventor of the cushion-back rubber-stamp, purchased the land in 1908 and put stone masons to work on ideas he acquired while travelling. The waterfall is a miniature Niagara Falls. The cave is modelled after those of Yellowstone. The bell-shaped fountain was built to honour the village. From 1840- 1870 the area was mined for brownstone.
This stone was used in the construction of the provincial parliament buildings in Toronto. The Trimble Trail follows an old tramway used to carry the stone from the valley to the Forks of the Credit railway. The remains of his construction work bring many visitors to the park annually. Park hours and fees can be found
here.

The terrain includes soil, clay and bedrock surfaces with a series of boardwalks and bridges. The flora includes Cedar, Oak, Maple and Birch trees and an abundance of wildflowers. Visitors may catch a glimpse of the fauna which includes salamanders, turtles, mink, deer, songbirds, brook and brown trout. The Belfountain trail takes visitors around the pond and along the scenic right side of the river.

Members of the Caledon Hills Bruce Trail Club can provide more information about local hikes in the area.


Forks of the Credit Provincial Park
Located north of Belfountain, Forks of the Credit Provincial Park features the excitement of the Credit River, as it narrows and rushes through a deep gorge, plunging over a falls. Geological features that were deposited or carved out by retreating glaciers, such as kame hills and kettle lakes, surround the river. The park also includes some of the upland, rolling pasture land that is typical of much of southern Ontario.

Hiking and picnicking are favourite activities here. Visitors may fish but hunting is forbidden. Open year-round, the park is popular in winter for cross-country skiing and snowshoeing.

Directions: From Belfountain, take the Forks of the Credit Road east under the train trestle to McLaren Road. Turn left and follow McLaren Road north. From Caledon, take Charleston Sideroad west, turn left on McLaren Road and follow the signs south to the Park.

For more information on the Forks of the Credit Provincial Park phone the staff at Earl Rowe Provincial Park at 705-435-2498.

MORE info from OntarioParks.com


Jefferson Salamander
Jefferson Salamander (Ambystoma jeffersonianum) is a rare and endangered salamander found in the Belfountain area. They inhabit deciduous forests with suitable breeding areas like limestone sinkhole ponds, kettle ponds and other natural basins. The most likely cause of low numbers of this species in Canada is the limited amount of habitat (terrestrial and breeding ponds) that is considered suitable for the species. The habitat that does remain is very fragmented and under pressure from urban expansion. The Jefferson Salamander is protected under the federal Species at Risk Act (SARA). Details about the Jefferson Salamander monitoring program can be found here.


The Jefferson Salamander
(photo courtesy of the
Niagara Escarpment Commission)

Belfountain's Salamander Festival is named in honour of the Jefferson Salamander.


Niagara Escarpment
The Niagara Escarpment is recognized as one of the world's unique natural wonders. As a landform it is a ridge of rock several hundred metres high in some locations -- stretching 725 kilometres (450 miles) from Queenston on the Niagara River to Tobermory at the tip of the Bruce Peninsula. The Escarpment contains more than 100 sites of geological significance including some of the best exposures of rocks and fossils of the Silurian and Ordovician Periods to be found anywhere in the world.
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The Niagara Escarpment is home to 300 bird species, 53 mammals, 36 reptiles and amphibians, 90 fish and 100 varieties of special interest flora including 37 types of wild orchids. MORE...

UNESCO named Ontario's Escarpment a World Biosphere Reserve in 1990. This designation recognizes the Niagara Escarpment as an internationally significant ecosystem for its special environment and unique environmental plan. Learn more about the Niagara Escarpment Biosphere Reserve. MORE...

For more information about the management and protection of the Niagara Escarpment , please visit the Niagara Escarpment Commission.

According to a February 1989 presentation made to Ontario Members of Provincial Parliament by Mr. Elliot:
"That, in the opinion of this House, recognizing the importance of the Niagara Escarpment as a significant feature of Ontario's natural heritage, and that the varying uses of the escarpment lands for farming, tourism, housing and aggregate extraction have a significant impact on that land, the Ministry of Municipal Affairs should be directed to ensure that any development or use of Niagara Escarpment lands be environmentally sustainable development; and that the Ministry of Municipal Affairs be further directed to maintain heritage and environmental concerns as priorities when considering land use planning within the Niagara Escarpment boundaries. "
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