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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 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 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.
With the water flow in the spring being six times the average rate, the valley has always been prone to flooding in the spring. 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]
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 ...
A 100-mile-long bloom of red tide is floating off Southwest Florida, prompting warnings about respiratory irritation and potential fish kills on area beaches. Experts say weather could be helping ...
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 .
The maximum displacement of the amphidrome from the centre coincides with spring tides, whereas the minimum occurs at neaps. During spring tides, more energy is absorbed from the tidal wave compared to neap tides. As a result, the reflection coefficient α is smaller and the displacement of the amphidromic point from the centre is larger.