Coordinates: 43°04′38″N 79°04′32″W / 43.077305°N 79.07562°W
The Horseshoe Falls, also known as the Canadian Falls, as most of it lies in Canada, is part of Niagara Falls, on the Niagara River. Approximately 90% of the Niagara River, after diversions for hydropower generation, flows over Horseshoe Falls. The remaining 10% flows over the American Falls. It is located between Terrapin Point on Goat Island in the US state of New York, and Table Rock on the Ontario side of the falls. According to official U.S. Geological Survey maps (see References [7][8] below), approximately two-thirds of Horseshoe Falls is located in Ontario, Canada with the remaining one-third in New York, United States of America.
When the boundary line was determined in 1819 based on the Treaty of Ghent, the northeastern end of the Horseshoe Falls was in New York, United States, flowing around the Terrapin Rocks, which was once connected to Goat Island by a series of bridges. In 1955 the area between the rocks and Goat Island was filled in, creating Terrapin Point. In the early 1980s the United States Army Corps of Engineers filled in more land and built diversion dams and retaining walls to force the water away from Terrapin Point. Altogether 400 feet (120 m) of the Horseshoe Falls was eliminated. Constant erosion indicates the boundary line will alter into the future.
The Horseshoe Falls of South Africa are waterfalls that are located 4 km off the Old Lydenburg Road along the Sabie River in Mpumalanga. These unusual falls, although not very high, are horseshoe shaped and have been declared a national monument. While doing a short walk through the beautiful landscape that leads to the cascade-type falls, the opportunity to spot magnificent birdlife and other wildlife is not uncommon. Horseshoe Falls is also a popular venue for trout fishing. Although it is easy to navigate to, there is a small fee to get into the park to be able to enjoy this beautiful attraction.
The amphitheatre in the uKhahlamba Drakensberg Park, also in South Africa, has massive cliffs that are in the shape of a horseshoe that could be confused as horseshoe falls.
Coordinates: 25°7′50″S 30°41′41″E / 25.13056°S 30.69472°E
Horseshoe Falls is one of seven waterfalls on the Murtle River west of Murtle Lake in Wells Gray Provincial Park, east-central British Columbia, Canada. Horseshoe Falls has two steps, 100 m (328 ft) apart; the upper drop is 6 m (20 ft) high and the lower and much wider drop is 10 m (33 ft) high.
The waterfall was discovered by Joseph Hunter, a surveyor working for the future Canadian Pacific Railway, on May 26, 1874. Hunter did not name the falls, but he did name the Murtle River and Murtle Lake for his birthplace in Scotland, Milton of Murtle, near Aberdeen. Horseshoe Falls was named in 1914 by land surveyor Robert Henry Lee, who mapped homesteaders' lots along the south side of the Murtle River. The river is slow-moving between Horseshoe Falls and Meadow Falls, 4 km (2.5 mi) upstream, and Lee marked a "raft crossing" on his map.
Horseshoe Falls can be reached by a 14 km (8.7 mi) hiking trail from Pyramid Campground on Clearwater Valley Road. The trail passes volcanic Pyramid Mountain and Majerus Falls, and ends at Horseshoe Falls.
Horseshoe Falls is the Canadian portion of Niagara Falls on the Niagara River, also known as the Canadian Falls
Horseshoe Falls may also refer to:
Horseshoe Falls (grid reference SJ196433) is a weir on the River Dee near Llantysilio Hall in Denbighshire, Wales, about 5 kilometres (3 mi) north-west of the town of Llangollen.
The distinctively shaped weir, which is 460 feet (140 m) long, helps create a pool of water that can enter the Llangollen Canal (via an adjacent valve house and flow meter). The canal west of Pontcysyllte Aqueduct and the construction of the weir were authorised by an Act of Parliament obtained in 1804 by the Ellesmere Canal Company. The canal was a navigable feeder, which supplied water to the Ellesmere Canal beyond Pontcysyllte, and to the Chester Canal, to which it connected near Nantwich. Thomas Telford was the civil engineer responsible for the design, and the canal and feeder were completed in 1808.
The Horseshoe Falls, a tiered–cascade waterfall, is located in the Central Highlands region of Tasmania, Australia.
The Horseshoe Falls are situated in the Mount Field National Park, 100 metres (330 ft) upstream of Russell Falls, approximately 70 kilometres (43 mi) northwest of Hobart via the Brooker Highway to New Norfolk and are a popular tourist attraction. The waterfall descends over horizontal marine Permian siltstone benches, while the vertical faces of the falls are composed of resistant sandstone layers.
Horseshoe Falls
Horseshoe Falls
Horseshoe Falls
Horseshoe Falls