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The vegetation of the New England and Maritime Appalachian Highlands is similar throughout the Nova Scotia highlands including the Cobequid Hills and the Pictou-Antigonish Highlands on the mainland and the Cape Breton Highlands, the Chaleur Uplands of New Brunswick, the New England Uplands, the White Mountains and Mont Mégantic on the New ...
The Confederacy covered roughly most of present-day Maine in the United States, and New Brunswick, mainland Nova Scotia, Cape Breton Island, Prince Edward Island and some of Quebec south of the St. Lawrence River in Canada. The Western Abenaki live on lands in New Hampshire, Vermont, and Massachusetts of the United States. [10]
Atlantic Canada, also called the Atlantic provinces (French: provinces de l'Atlantique), is the region of Eastern Canada comprising four provinces: New Brunswick, Newfoundland and Labrador, Nova Scotia, and Prince Edward Island.
As with many regional networks, this creates a balancing act where local stories in one community or province are of little interest in another area of CTV Atlantic's coverage area, and viewers in each province feel the news division focuses too much on either New Brunswick or Nova Scotia, along with a lesser focus on Prince Edward Island.
By the 1800s most Mi'kmaw had left the area to live on the Reserve in Bear River, while still returning for fishing, hunting, trade and ceremony throughout the year. It was named "Clare" by then Lieutenant Governor of Nova Scotia, Michael Francklin. The name comes from the County Clare in Ireland. [3]
The Chedabucto Fault is a fault that divides Mainland Nova Scotia from the Minas Basin in the west to Chedabucto Bay in the east into the Avalon zone in the north and the Meguma Zone in the south. The Avalon and Meguma Zones are different because they belonged to different land masses that were widely separated from one another.
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The Meguma terrane, also known as Megumia, is a terrane exposed in southern Nova Scotia, that became joined to the present North American landmass as part of the Appalachian orogeny. The exposed part of the Meguma terrane, the Meguma Group , is largely composed of c. 10 km (6.2 mi) thick Cambrian to Ordovician turbidites that have been ...