Cape Breton in the context of "Strait of Canso"

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⭐ Core Definition: Cape Breton

Cape Breton Island (French: île du Cap-Breton, formerly île Royale; Scottish Gaelic: Ceap Breatainn or Eilean Cheap Bhreatainn; Mi'kmaq: Unama'ki) is a rugged and irregularly shaped island on the Atlantic coast of North America and part of the province of Nova Scotia, Canada.

The 10,311 km (3,981 sq mi) island accounts for 18.7% of Nova Scotia's total area. Although the island is physically separated from the Nova Scotia peninsula by the Strait of Canso, the 1,385 m (4,544 ft) long Canso Causeway connects it to mainland Nova Scotia. The island is east-northeast of the mainland with its northern and western coasts fronting on the Gulf of Saint Lawrence with its western coast forming the eastern limits of the Northumberland Strait. The eastern and southern coasts front the Atlantic Ocean with its eastern coast also forming the western limits of the Cabot Strait. Its landmass slopes upward from south to north, culminating in the highlands of its northern cape. A large body of saltwater, the Bras d'Or ("Golden Arm" in French), dominates the island's centre.

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Cape Breton in the context of Terre-Neuve (New France)

Terre-Neuve (French pronunciation: [tɛʁ nœv] , "Newfoundland") was a colony in New France that existed from 1655 to 1713, and which consisted of the southern portion of Newfoundland island (the northern portion being claimed by England). The most, and sometimes only, populated region was Placentia, called "Plaisance" in French. Because of Placentia's geographic position, its main economic activity was fishing, and the settlement could serve as a pit stop for ships traveling to and from France and other New France colonies like Canada or Acadia. Terre-Neuve ceased to exist in 1713, when France evacuated its settlers and transplanted them to Cape Breton. But, France regained the Saint Pierre and Miquelon islands of this colony in 1763, and still has possession over them today.

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Cape Breton in the context of Atlantic Canadian English

Atlantic Canadian English is a class of Canadian English dialects spoken in Atlantic Canada that is notably distinct from Standard Canadian English. It is composed of Maritime English (or Maritimer English) and Newfoundland English. It was mostly influenced by British and Irish English, Irish and Scottish Gaelic, and some Acadian French. Atlantic Canada is the easternmost region of Canada, comprising four provinces located on the Atlantic coast: Newfoundland and Labrador, plus the three Maritime provinces of Nova Scotia, New Brunswick, and Prince Edward Island.

Areas like Miramichi and Cape Breton feature a diverse array of unique phrases and vocabulary that are rarely heard outside their regions. Additionally, the English accent exhibits considerable variation across different population centres.

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Cape Breton in the context of Dalhousie University

Dalhousie University is a large public research university in Nova Scotia, Canada, with three campuses in Halifax, a fourth in Bible Hill, and two satellite medical school campuses, in Saint John, New Brunswick and in Cape Breton. Dalhousie offers over 200 degree programs in 13 undergraduate, graduate, and professional faculties. The university is a member of the U15, a group of research-intensive universities in Canada.

The institution was established as Dalhousie College, a nonsectarian institution established in 1818 by the eponymous Lieutenant Governor of Nova Scotia, George Ramsay, 9th Earl of Dalhousie, with education reformer Thomas McCulloch as its first principal. However, the college did not hold its first class until 1838, with operations remaining sporadic due to financial difficulties. The college was reorganized in 1863 and renamed The Governors of Dalhousie College and University. The university formally changed its name to Dalhousie University in 1997 through the same provincial legislation that merged the institution with the Technical University of Nova Scotia.

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Cape Breton in the context of Dome (geology)

A dome is a feature in structural geology where a circular part of the Earth's surface has been pushed upward, tilting the pre-existing layers of earth away from the center. In technical terms, it consists of symmetrical anticlines that intersect each other at their respective apices. Intact, domes are distinct, rounded, spherical-to-ellipsoidal-shaped protrusions on the Earth's surface. A slice parallel to Earth's surface of a dome features concentric rings of strata. If the top of a dome has been eroded flat, the resulting structure in plan view appears as a bullseye, with the youngest rock layers at the outside, and each ring growing progressively older moving inwards. These strata would have been horizontal at the time of deposition, then later deformed by the uplift associated with dome formation.

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