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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]
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 ...
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.
The waters of Minas Bay exchange with the main part of the Bay of Fundy through the Minas Channel which flows between Cape Split and Cape Sharp, creating extremely strong tidal currents. Near Cape d'Or, the turbulent collision of currents is known as the Dory Rips .
Fundy National Park is a national park of Canada located on the Bay of Fundy, near the village of Alma, New Brunswick. It was created on April 10, 1946 and officially opened on July 29, 1950. The park showcases a rugged coastline which rises up to the Canadian Highlands, the highest tides in the world and more than 25 waterfalls.
The Reversing Falls are a series of rapids on the Saint John River, located in Saint John, New Brunswick, Canada, where the river runs through a narrow gorge before emptying into the Bay of Fundy. The semidiurnal tides of the bay force the flow of water to reverse against the prevailing current when the tide is high.
Erected in 1829 by the provincial government, its purpose was to aid navigation for ships in the Bay of Fundy. While West Quoddy Light stands at the mouth of the narrows around Lubec, Maine, East Quoddy was built on the north side of Campobello, on a small tidal islet connected to the primary landmass, guiding entry into Passamaquoddy Bay ...
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.