List of waterfalls by flow rate

Canadian side of the Niagara Falls. Horseshoe Falls as viewed from Skylon Tower
Aerial view of the Iguazu Falls from a helicopter
Victoria Falls

This list of waterfalls by flow rate in the world includes waterfalls that have a flow rate of more than 1000 m³/s. This list is sorted by mean annual flow rate of the waterfall by default, but can also be sorted by other criteria, such as width, power, etc.

Extant and submerged waterfalls

WaterfallMean annual flow rate (m³/s)Tallest single drop (m)Width (m)Power (GW)RiverCountries
Boyoma Falls17,000[1] (estm)5[1]1372[1]0.83LualabaDemocratic Republic of the Congo
Guaíra Falls (submerged)13,300[2]405.22ParanaParaguay and Brazil
Khone Phapheng Falls11,610[1]21 [1]10783[1]2.39MekongLaos
Celilo Falls (submerged)5415[1]7[1]3219[1]0.37ColumbiaUnited States
Niagara Falls2407[1]51[1]1203[1]1.20NiagaraCanada and the United States
Iguazú Falls1746[1]82[1]2700[1]1.40IguazúArgentina and Brazil
Victoria1088 [1]108[1]1708[1]1.15ZambeziZimbabwe and Zambia

The first five waterfalls by power (Guaíra, Khone Phapheng, Iguazú, Niagara and Victoria) are called the Great Five Waterfalls.[3][4]

Prehistoric waterfalls

WaterfallMaximum daily flow rate (m³/s)Tallest single drop (m)Width (m)RiverCountries
Dry Falls1,906,000[5]3504828ColumbiaUnited States
Bosphorus (Black Sea deluge hypothesis)482,407[6]80Bosphorus StraitTurkey

See also

References

  1. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 World Waterfalls Website accessed 15 November 2013
  2. "Guaíra, Salto del at the World Waterfall Database". Archived from the original on 2013-03-15. Retrieved 2011-01-29.
  3. Г. Т. Арсеев. Водопады. — М.: Мысль, 1987. — С. 14. — 127 с.
  4. В. И. Задорожный, К. В. Зворыкин. Методология и региональные физико-географические исследования. — М.: Географическое общество СССР, 1975. — С. 60. — 78 с.
  5. The Channeled Scablands of Eastern Washington, United States Geological Survey, retrieved 2012-03-15
  6. Ryan, W.B.F.; Pitman III, W.C., et al. 1997. An abrupt drowning of the Black Sea shelf. Marine Geology, 138: 119–126.
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