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Northumberland Strait
46°05′N 63°35′W / 46.083°N 63.583°W
The Northumberland Strait (French: détroit de Northumberland) is a strait in the southern part of the Gulf of Saint Lawrence in eastern Canada. The strait is formed by Prince Edward Island and the gulf's eastern, southern, and western shores.
The western boundary of the strait is delineated by a line running between North Cape, Prince Edward Island and Point Escuminac, New Brunswick while the eastern boundary is delineated by a line running between East Point, Prince Edward Island and Inverness, Nova Scotia.
The Northumberland Strait varies in depth between 17 and 65 metres, with the deepest waters at either end. The tidal patterns are complex; the eastern end has the usual two tides per day, with a tidal range of 1.2 to 1.8 metres, while the western end effectively has only one tide per day.
The strait's shallow depths lend to warm water temperatures in summer months, with some areas reaching 25°C, or 77°F. Consequently, the strait is reportedly home to the warmest ocean water temperatures in Canada, and some of the warmest ocean water temperatures on the Atlantic coast north of Virginia.
There are many sandy beaches along both the northern and southern coasts of the strait. These beaches, found in New Brunswick, Prince Edward Island, and Nova Scotia, are very popular with tourists.
During the winter months between December and April, sea ice covers the entire strait and Gulf of St. Lawrence.
While the western shores of Cape Breton Island and northeastern shores of the Nova Scotia peninsula are dominated by granite, sedimentary rocks along the central and western parts of the strait, as well as the entire south shore of Prince Edward Island, consist of sandstone, lending to beautiful sandy beaches with minimal coastal development. The largest island in the strait is Pictou Island.
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Northumberland Strait
46°05′N 63°35′W / 46.083°N 63.583°W
The Northumberland Strait (French: détroit de Northumberland) is a strait in the southern part of the Gulf of Saint Lawrence in eastern Canada. The strait is formed by Prince Edward Island and the gulf's eastern, southern, and western shores.
The western boundary of the strait is delineated by a line running between North Cape, Prince Edward Island and Point Escuminac, New Brunswick while the eastern boundary is delineated by a line running between East Point, Prince Edward Island and Inverness, Nova Scotia.
The Northumberland Strait varies in depth between 17 and 65 metres, with the deepest waters at either end. The tidal patterns are complex; the eastern end has the usual two tides per day, with a tidal range of 1.2 to 1.8 metres, while the western end effectively has only one tide per day.
The strait's shallow depths lend to warm water temperatures in summer months, with some areas reaching 25°C, or 77°F. Consequently, the strait is reportedly home to the warmest ocean water temperatures in Canada, and some of the warmest ocean water temperatures on the Atlantic coast north of Virginia.
There are many sandy beaches along both the northern and southern coasts of the strait. These beaches, found in New Brunswick, Prince Edward Island, and Nova Scotia, are very popular with tourists.
During the winter months between December and April, sea ice covers the entire strait and Gulf of St. Lawrence.
While the western shores of Cape Breton Island and northeastern shores of the Nova Scotia peninsula are dominated by granite, sedimentary rocks along the central and western parts of the strait, as well as the entire south shore of Prince Edward Island, consist of sandstone, lending to beautiful sandy beaches with minimal coastal development. The largest island in the strait is Pictou Island.