Malecite-Passamaquoddy language in the context of "Saint John River (Bay of Fundy)"

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👉 Malecite-Passamaquoddy language in the context of Saint John River (Bay of Fundy)

The Saint John River (French: fleuve Saint-Jean; Maliseet-Passamaquoddy: Wolastoq) is a 673-kilometre-long (418 mi) river flowing within the Dawnland region from headwaters in the Notre Dame Mountains near the Maine-Quebec border through western New Brunswick to the northwest shore of the Bay of Fundy. Eastern Canada's longest river, its drainage basin is one of the largest on the east coast at about 55,000 square kilometres (21,000 sq mi). This “River of the Good Wave” and its tributary drainage basin formed the territorial countries of the Wolastoqiyik and Passamaquoddy First Nations (named Wolastokuk and Peskotomuhkatik, respectively) prior to European colonization, and it remains a cultural centre of the Wabanaki Confederacy to this day.

The Webster–Ashburton Treaty following the Aroostook War established a border between New Brunswick and Maine following 130 km (81 mi) of the river, while a tributary forms 55 km (34 mi) of the border between Quebec and Maine. Maine communities along the river include Fort Kent, Madawaska, and Van Buren. New Brunswick settlements through which it passes include, moving downstream, Edmundston, Fredericton, Oromocto, and Saint John.

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Malecite-Passamaquoddy language in the context of Eastern Algonquian languages

The Eastern Algonquian languages constitute a subgroup of the Algonquian languages. Prior to European contact, Eastern Algonquian consisted of at least 17 languages, whose speakers collectively occupied the Atlantic coast of North America and adjacent inland areas, from what are now the Maritimes of Canada to North Carolina. The available information about individual languages varies widely. Some are known only from one or two documents containing words and phrases collected by missionaries, explorers or settlers, and some documents contain fragmentary evidence about more than one language or dialect. Many of the Eastern Algonquian languages were greatly affected by colonization and dispossession. Miꞌkmaq and Malecite-Passamaquoddy have appreciable numbers of speakers, but Western Abenaki and Lenape (Delaware) are each reported to have fewer than 10 speakers after 2000.

Eastern Algonquian constitutes a separate genetic subgroup within Algonquian. Two other recognized groups of Algonquian languages, Plains Algonquian and Central Algonquian, are geographic but do not refer to genetic subgroupings.

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Malecite-Passamaquoddy language in the context of Bar Harbor, Maine

Bar Harbor (Malecite-Passamaquoddy: Man-es-ayd'ik or Ah-bays'auk) is a resort town on Mount Desert Island in Hancock County, Maine, United States. As of the 2020 census, its population is 5,089. The town is home to the College of the Atlantic, Jackson Laboratory, and MDI Biological Laboratory. During summer and fall seasons, it is a popular tourist destination.

Bar Harbor is also home to the largest parts of Acadia National Park, including Cadillac Mountain, the highest point within 25 miles (40 km) of the coastline of the Eastern United States.

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Malecite-Passamaquoddy language in the context of St. Croix River (Maine-New Brunswick)

The St. Croix River (French: Fleuve Sainte-Croix; Maliseet-Passamaquoddy: Skutik) is a river in northeastern North America, 71 miles (114 km) in length, that forms part of the Canada–United States border between Maine (U.S.) and New Brunswick (Canada). The river rises in the Chiputneticook Lakes and flows south and southeast, between Calais and St. Stephen. It discharges into Passamaquoddy Bay, in the Bay of Fundy.

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