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The height of the falls is so great that before getting anywhere near the ground, the water is atomized by the strong winds and turned into mist. The mist can be felt a mile away. The base of the falls feeds into the Kerep River (alternatively known as the Río Gauya), which flows into the Churun River, a tributary of the Carrao River.
The height figure 3,212 feet (979 m) mostly consists of the main plunge but also includes about 0.25 miles (400 m) of shallowly sloped cascades and rapids below the drop and a 100-foot (30 m) high plunge downstream of the talus rapids. While the main plunge is undoubtedly the highest single drop in the world, including the lower cascades somewhat stretches the criteria for the measurement of waterfalls. Some other waterfalls, such as Yosemite Falls in North America, also include intermediary cascades in their height figures, but, in the case of Yosemite Falls, the middle cascades are much steeper and have less run than those of Angel Falls.
In the indigenous Pemon language Kerepakupai merú means 'waterfall of the deepest place'. The falls are sometimes referred to as Churún-merú, an error, since that name corresponds to another waterfall in the Canaima National Park. Churún in the Pemon language means "thunder".
Angel Falls (Kerepakupai merú) is one of Venezuela's top tourist attractions, but, even today, a trip to the falls is a complicated affair. The falls are located in an isolated jungle region of Venezuela, and a flight from Caracas or Ciudad Bolívar is required to reach Canaima camp, the starting point for river trips to the base of the falls. River trips generally take place from June to December, when the rivers are deep enough for the wooden curiaras used by the Pemon guides. During the dry season (December to March) there is less water seen than in the other months.
An alternative possibility is to purchase a package that includes an aerial flyby of the falls. However, since the falls cannot be seen on cloudy days, there is no guarantee visitors will see them from the air.
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