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Geography of New Brunswick

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Geography of New Brunswick

New Brunswick (French: Nouveau-Brunswick) is one of Canada's three Maritime provinces. While New Brunswick is one of Canada's Maritime Provinces, it differs from its neighbours both ethnoculturally and physiographically. Both Nova Scotia and Prince Edward Island are either wholly or nearly surrounded by water and the ocean, therefore, tends to define their climate, economy and culture. New Brunswick, on the other hand, although having a significant seacoast, is sheltered from the Atlantic Ocean proper and has a large interior that is removed from oceanic effects. New Brunswick, therefore, tends to be defined by its rivers rather than its seacoast.

New Brunswick is bounded on the north by Quebec's Gaspé Peninsula and Bay of Chaleur and on the east by the Gulf of Saint Lawrence and Northumberland Strait. In the southeast, the Isthmus of Chignecto connects it to Nova Scotia. On its west, the province borders the American state of Maine.

The total land and water area of the province is 72,908 square kilometres.

The major river systems in the province include the Saint John River, Petitcodiac River, Miramichi River, St. Croix River and the Restigouche River. The Saint John River is thought to be the second-longest river on the North American eastern seaboard between the St. Lawrence River and the Mississippi River.

The northern seacoast, along Miramichi Bay, the Gulf of St. Lawrence and the Bay of Chaleur is called the North Shore, a region predominately Francophone, but with sizable English-speaking communities

New Brunswick lies entirely within the Appalachian Mountain range, a chain of ancient, eroded mountains which have created river valleys and low, gently rolling hills throughout large parts of the province. Zones of the province include:

The majority of western New Brunswick is drained by the Saint John River system. The river, which rises in northern Maine, empties into the Bay of Fundy in Saint John. Notable tributaries within the province include the Madawaska River, Tobique River, Meduxnekeag River, Nashwaak River, Oromocto River, Nerepis River and Kennebecasis River. Other water bodies within the Saint John River system are Grand Lake (which itself is fed by the Salmon River), Washademoak Lake (fed by the Canaan River), and Belleisle Bay. The high tides of the Bay of Fundy often cause the Saint John River to flow upstream, an effect most pronounced at the Reversing Falls in Saint John.

The Petitcodiac River, Shepody River, Tantramar River, and Memramcook River empty into Chignecto Bay at the head of the Bay of Fundy. Like the Saint John River, the Bay of Fundy tides causes another upstream phenomenon, known as a tidal bore. The construction of a causeway on the river at Moncton, approximately 50 kilometres upstream, has lessened the tidal bore's effect and changed the river's ecosystem.

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