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Dinosaur Provincial Park is a UNESCO World Heritage Site situated 220 kilometres (137 mi) east of Calgary, Alberta, Canada; or 48 kilometres (30 mi) northeast of Brooks.. The park is situated in the Red Deer River valley, which is noted for its striking badland topography, and abundance of dinosaur fossils.
The Dinosaur Trail continues northwest along the Red Deer River to the intersection of Highway 837/838 intersection, where it turns east onto Highway 838. It crosses the Red Deer River on the free, cable-operated Bleriot Ferry, which has been running since 1913 [ 4 ] and operates from late April to November. [ 2 ]
Dry Island Buffalo Jump Provincial Park is a provincial park in Central Alberta, Canada, located about 103 km (64 mi) southeast of Red Deer and 16 km (9.9 mi) northeast of Trochu, 1 mile north and 10 miles east of Huxley. The park is situated along the Red Deer River and features badlands topography.
Drumheller / d r ʌ m ˈ h ɛ l ər / is a town on the Red Deer River in the badlands of east-central Alberta, Canada. It is located 110 kilometres (68 mi) northeast of Calgary and 97 kilometres (60 mi) south of Stettler. The Drumheller portion of the Red Deer River valley, often referred to as Dinosaur Valley, has an approximate width of 2 ...
[2] [3] It takes its name from Horseshoe Canyon, an area of badlands near Drumheller. The Horseshoe Canyon Formation is part of the Edmonton Group . In its type section (Red Deer River Valley at Drumheller ), it is ~250 metres (820 ft) thick, but further west the formation is older and thicker, exceeding 500 metres (1,600 ft) near Calgary . [ 4 ]
The Vermilion Lakes are a series of lakes located immediately west of Banff, Alberta, in the Canadian Rocky Mountains. The three lakes are formed in the Bow River valley, in the Banff National Park, at the foot of Mount Norquay. They are located between the Trans-Canada Highway and the Canadian Pacific Railway tracks.
The Bare Range is a mountain range of the Canadian Rockies, located south of the Red Deer River valley in Banff National Park, Canada. The range is named for the "bareness" of or lack of trees on the gentle slopes of the range. [3] This range includes the following mountains and peaks:
As Johnston Creek approaches the Bow River, it flows through a large canyon formed by erosion over thousands of years. The creek has cut through the limestone rock to form sheer canyon walls, as well as waterfalls, tunnels, and pools. A popular hiking trail follows the canyon and leads to a meadow within the Johnston Valley above the canyon.