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Through Atlantic Ocean, Canada and North America

Geography

Extent

The Gulf of St. Lawrence is bounded on the north by the Labrador Peninsula and Quebec, on the east by Saint-Pierre and Newfoundland, on the south by the Nova Scotia peninsula and Cape Breton Island, and on the west by the Gaspé Peninsula, New Brunswick, and Quebec. The Gulf of St. Lawrence contains numerous islands, including Anticosti, Prince Edward, Saint Pierre, Cape Breton, Miquelon-Langlade, and the Îles-de-la-Madeleine archipelago.

Half of Canada's ten provinces adjoin the Gulf: New Brunswick, Nova Scotia, Prince Edward Island, Newfoundland and Labrador, and Quebec.

There is no consensus on the demarcation of the St Lawrence River from the Gulf, nor whether it is hydrographically a gulf or an estuary.

According to Commission of Toponymy Quebec, the St. Lawrence River becomes the gulf at Pointe des Monts on the Côte-Nord and Matane Bas-Saint-Laurent or Sainte-Anne-des-Monts La Haute-Gaspésie, the Estuary is upstream, the Gulf of St. Lawrence, much wider, downstream.

The International Hydrographic Organization defines the gulf's extent as follows:

On the Northeast: A line running from Cape Bauld (North point of Kirpon Island, 51°40′N 55°25′W / 51.667°N 55.417°W) to the East extreme of Belle Isle and on to the Northeast Ledge (52°02′N 55°15′W / 52.033°N 55.250°W). Thence a line joining this ledge with the East extreme of Cape St. Charles (52°13'N) in Labrador.
On the Southeast: A line from Cape Canso (45°20′N 61°0′W / 45.333°N 61.000°W) to Red Point (45°35′N 60°45′W / 45.583°N 60.750°W) in Cape Breton Island, through this Island to Cape Breton [45°57′N 59°47′W / 45.950°N 59.783°W] and on to Pointe Blanche (46°45′N 56°11′W / 46.750°N 56.183°W) in the Island of St. Pierre, and thence to the southwest point of Morgan Island (46°51′N 55°49′W / 46.850°N 55.817°W).
On the West: The meridian of 64°30'W from Pointe-Jaune (49°04′N 64°30′W / 49.06°N 64.5°W) to Magpie (50°19′N 64°30′W / 50.31°N 64.5°W), but the whole of Anticosti Island is included in the Gulf.

At Baie-Trinité, the Pointe-des-Monts Lighthouse, a National historic site of Canada, was built in 1829–1830 on a point that geographers throughout history, since as early as Samuel de Champlain (1567–1655), have classified as the demarcation point between the St. Lawrence River and the Gulf of St. Lawrence.

Fisheries and Oceans Canada's "Estuary and Gulf of St. Lawrence planning area" covers most of the Estuary and Gulf of St. Lawrence bioregion, an area with some of the warmest surface waters in Atlantic Canada during summer and the largest amount of sea ice during winter. The planning area is approximately 240,000 km².

Tributaries and nested bays

Besides the St. Lawrence itself, significant rivers emptying into the Gulf of St. Lawrence include the Miramichi, Natashquan, Romaine, Restigouche, Margaree, Humber and Mingan.

Branches of the Gulf include Chaleur Bay, Fortune Bay, Miramichi Bay, St. George's Bay, Bay St. George, Bay of Islands, and the Northumberland Strait.

Outlets

Around Anticosti Island and to flow into the Atlantic Ocean, the waters of the Gulf take the following straits:

  • Jacques Cartier Strait, between the shore of Côte-Nord region and the North of Anticosti Island.
  • Honguedo Strait, a wide passage between the Gaspé Peninsula and Anticosti Island.
  • Strait of Belle Isle between Labrador and Newfoundland: between 15 kilometres (9.3 miles) and 60 kilometres (37 miles) wide and 60 metres (200 feet) deep at its deepest.
  • Cabot Strait, about 56 miles wide, is the entrance to the Gulf of St. Lawrence between Cape Ray, Newfoundland, and Cape North, the NE point of Cape Breton Island.
  • Strait of Canso is located between Cape Breton Island and mainland Nova Scotia, it originally served as an outlet 1.0 km (0.6 mi) wide and 60 m (200 ft) deep at its deepest. Due to the construction of the Canso Causeway across the strait in 1955, the roadway no longer allows exchange of water between the Gulf of St. Lawrence and the Atlantic Ocean.

Undersea features

The Laurentian Channel is a feature of the floor of the Gulf that was formed during previous ice ages, when the Continental Shelf was eroded by the St. Lawrence River during the periods when the sea level plunged. The Laurentian Channel is about 290 m (950 ft) deep and about 1,250 km (780 mi) long from the Continental Shelf to the mouth of the St. Lawrence River. Deep waters with temperatures between 2 and 6.5 °C (36 and 44 °F) enter the Gulf at the continental slope and are slowly advected up the channel by estuariane circulation. Over the 20th century, the bottom waters of the end of the channel (i.e. in the St. Lawrence estuary) have become hypoxic.

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