The Connection between the Precenting of Psalms on Cape Breton Island and in Colonial New England Churches

1962 ◽  
Vol 14 ◽  
pp. 155 ◽  
Author(s):  
Sidney Robertson Cowell
Keyword(s):  
New England ◽  
Cape Breton Island ◽  
Cape Breton ◽  
Colonial New England

Superposed Neoproterozoic and Silurian magmatic arcs in central Cape Breton Island, Canada: geochemical and geochronological constraints

2000 ◽  
Vol 137 (2) ◽  
pp. 137-153 ◽  
Author(s):  
J. D. KEPPIE ◽  
J. DOSTAL ◽  
R. D. DALLMEYER ◽  
R. DOIG
Keyword(s):  
New Brunswick ◽  
New England ◽  
Volcanic Rocks ◽  
Geochemical Data ◽  
Zircon Age ◽  
Cape Breton Island ◽  
Northern Margin ◽  
Element Abundances ◽  
Southern New England ◽  
Cape Breton

Isotopic and geochemical data indicate that intrusions in the eastern Creignish Hills of central Cape Breton Island, Canada represent the roots of arcs active at ∼ 540–585 Ma and ∼ 440 Ma. Times of intrusion are closely dated by (1) a nearly concordant U–Pb zircon age of 553±2 Ma in diorites of the Creignish Hills pluton; (2) a lower intercept U–Pb zircon age of 540±3 Ma that is within analytical error of 40Ar/39 Ar hornblende plateau isotope-correlation ages of 545 and 550±7 Ma in the River Denys diorite; and (3) an upper intercept U–Pb zircon age of 586±2 Ma in the Melford granitic stock. On the other hand, ∼ 441–455 Ma 40Ar/39 Ar muscovite plateau ages in the host rock adjacent to the Skye Mountain granite provide the best estimate of the time of intrusion, and are consistent with the presence of granitic dykes cutting the Skye Mountain gabbro–diorite previously dated at 438±2 Ma. All the intrusions are calc-alkaline; the Skye Mountain granite is peraluminous. Trace element abundances and Nb and Ti depletions of the intrusive rocks are characteristic of subduction-related rocks. The ∼ 540–585 Ma intrusions form part of an extensive belt running across central Cape Breton Island, and represent the youngest Neoproterozoic arc magmas in this part of Avalonia. Nearby, they are overlain by Middle Cambrian units containing rift-related volcanic rocks, which bracket the transition from convergence to extension between ∼ 540 and 505/520 Ma. This transition varies along the Avalon arc: 590 Ma in southern New England, 560–538 Ma in southern New Brunswick, and 570 Ma in eastern Newfoundland. The bi-directional diachronism in this transition is attributed to northwestward subduction of two mid-ocean ridges bordering an oceanic plate, and the migration of two ridge–trench–transform triple points. Following complete subduction of the ridges, remnant mantle upwelling along the subducted ridges produced uplift, gravitational collapse and the high-temperature/low-pressure metamorphism in the arc in both southern New Brunswick and central Cape Breton Island. The ∼ 440 Ma arc magmatism in the Creignish Hills extends through the Cape Breton Highlands and into southern Newfoundland, and has recently been attributed to northwesterly subduction along the northern margin of the Rheic Ocean.

Frank Campbell MacIntosh, 24 December 1909 - 11 September 1992

1994 ◽  
Vol 40 ◽  
pp. 253-264 ◽  
Keyword(s):  
Nova Scotia ◽  
New England ◽  
Prince Edward Island ◽  
United Church Of Canada ◽  
Cape Breton Island ◽  
North West ◽  
The North ◽  
Cape Breton ◽  
One Year ◽  
North West Territories

The MacIntoshes were displaced from the Western Isles of Scotland by the Highland clearances at the end of the eighteenth century and like many of their compatriots moved to Nova Scotia. Around 1816 the Macintoshes were settled on a farm at Big Harbour Island on the Bras d’Or Lake of Cape Breton Island, that large detached part of Nova Scotia separated from the mainland by the narrow Straits of Canso - so narrow that they were frequently crossed by swimming deer. This part of Nova Scotia had a considerable resemblance to the old home in its landscape and its sea-tom ruggedness, which must have assuaged some of the pain of exile. Frank (who was always known as Hank) was born at Baddeck in Cape Breton on 24 December 1909, the son of the Reverend C.C. Macintosh, a well-known pastor of the United Church of Canada, who spoke and preached in Gaelic in the Canadian Maritimes and in New England. His mother Beenie Matheson, also of Scottish origin, came from Prince Edward Island. She had trained as a teacher and had moved to the north-west territories as a pioneer. As a child Hank frequently went visiting with his father in the horse and buggy. He was a precocious child and taught himself to read at the age of three - largely from the Encyclopedia Britannica - becoming especially interested in the geographical places described therein. At nine he was driving the family Model T. He was very proud of the fact that when he was just one year old, Alexander Graham Bell dandled him on his knee at his home in Beinn Bhreagh.

Culinary tourism on Cape Breton Island

2019 ◽  
Vol 6 (2) ◽  
Author(s):  
Erna MacLeod
Keyword(s):  
Tourism Destination ◽  
Cape Breton Island ◽  
Culinary Tourism ◽  
Economic Significance ◽  
Cape Breton ◽  
Local Stakeholders ◽  
Resilient Communities ◽  
World Class ◽  
Ecological Relations ◽  
Developed World

Cape Breton Island is a well-known North American tourism destination with long-standing attractions such as the Cabot Trail and more recently developed world-class offerings such as the Cabot Links Golf Course. Tourism contributes significantly to Cape Breton’s economy, particularly since the mid-20th century as traditional resource-based industries have declined. In the 21st century, culinary tourism has become increasingly important to expand the island’s tourism offerings and to provide “authentic” tourism experiences. This study examines local-food tourism in Cape Breton to illuminate its cultural and economic significance. I conducted interviews with food producers, restaurateurs, government representatives, and tourism executives. I also consulted websites and policy documents and compared local stakeholders’ experiences and perspectives with official tourism strategies. Promoting culinary tourism raises questions of power, autonomy, inclusion, and accountability. My study accentuates possibilities for aligning economic and ecological goals to create resilient communities, foster equitable social and ecological relations, and establish Cape Breton as a culinary tourism destination.

Cape Breton ruby, a new Canadian gemstone discovery, Cape Breton Island, Nova Scotia

2007 ◽  
Vol 30 (5) ◽  
pp. 279-286 ◽  
Author(s):  
David J. Mossman ◽  
James D. Duivenvoorden ◽  
Fenton M. Isenor
Keyword(s):  
Nova Scotia ◽  
Cape Breton Island ◽  
Cape Breton

Puritans and Race

2018 ◽  
Author(s):  
Richard A. Bailey
Keyword(s):  
New England ◽  
Colonial America ◽  
Colonial New England ◽  
Race And Religion

In scholarly discussions about “race” in the Americas, colonial New England often receives little attention. While race-based slavery perhaps never commanded the same attention in the northern colonies as in regions farther south, “race” factored into nearly every aspect of life in New England from the outset. This chapter not only discusses how scholars have approached this conversation but also investigates some of the ways in which New Englanders made sense of themselves and the peoples of varying ethnicities, relying at times on the specific theological context of New England puritanism. Focusing on the ways in which New Englanders wrestled with the dilemma of racial thinking within their theological system brings New England fully into the discussion of the intersections between “race” and religion in colonial America.

Literature & Theology in Colonial New England.

1951 ◽  
Vol 22 (4) ◽  
pp. 536
Author(s):  
Theodore Hornberger ◽  
Kenneth B. Murdock
Keyword(s):  
New England ◽  
Colonial New England
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