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The Bay of Fundy (French: Baie de Fundy) is a bay between the Canadian provinces of New Brunswick and Nova Scotia, with a small portion touching the U.S. state of Maine. It is an arm of the Gulf of Maine. Its tidal range is the highest in the world. [1] The name is probably a corruption of the French word fendu, meaning 'split'. [2]
The world's largest mean tidal range of 11.7 metres (38.4 feet) occurs in the Bay of Fundy, Canada (more specificially, at Burntcoat Head, Nova Scotia). [ 4 ] [ 6 ] The next highest, of 9.75 metres (32.0 feet), is at Ungava Bay , also in Canada, [ 4 ] [ 7 ] and the next, of 9.60 metres (31.5 feet), in the Bristol Channel , between England and ...
The Dory Rips is a phenomenon involving extreme tidal agitation of waters located in the Bay of Fundy off the headland of Cape d'Or in Nova Scotia, Canada. The phenomenon occurs at the entrance to the Minas Basin , which is known for the globe's highest tides.
Burntcoat Head is located in Cobequid Bay, near the eastern end of the Bay of Fundy. Burntcoat Head had a public wharf that has been the location of a tide gauge since the 19th century. The tide gauge at Burntcoat Head was operated by the Canadian Hydrographic Service and has recorded the highest tidal range in the world.
South Florida is made up of a lot of low-lying areas near the water, and as the sea rises, king tides will reach farther and farther inland. It overwhelms storm drains, stops traffic routes and ...
Due to the extreme tidal range of the Bay of Fundy, the base of the formations are covered in water twice a day. It is possible to view the formations from ground level at low tide. The formations consist of red-brown sedimentary conglomerate, sandstone, and minor mudstone rock from the Carboniferous Hopewell Cape Formation, part of the Mabou ...
Surface runoff from heavy rainfall is the main cause of flooding, and can be exacerbated by ice jams, high tides, and rapid snowmelt. [15] Floods have been documented for more than 300 years. [ 16 ] Flooding has occurred in Edmundston, Grand Falls, Perth-Andover, Hartland, Woodstock, and most severely around Fredericton and Saint John.
The whirlpool is caused by local bathymetry and a 20-foot (6.1 m) tidal range [1] where waters exchange between Passamaquoddy Bay and the Bay of Fundy, combined with the topography of the location's sea floor at the confluence of the numerous local currents through channels and over small sea mounts.