995 resultados para NOVA-SCOTIA


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Ledger containing accounts of smallpox inoculation by Dr. John Jeffries (1745-1819) at Rainsford Island Hospital in Boston, Massachusetts, from June to July 1775; at a West Boston smallpox hospital in July 1775; and in Halifax, Nova Scotia, between 1776 and 1779. The accounts include dates, names, ages and physical condition of patients, and details regarding the method of delivery. Among the patients he inoculated was his son, John, at Rainsford Island Hospital on 14 June 1775.

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Concerns the preparations for the reduction of Quebec.

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Ledger containing lists and charts of smallpox inoculation cases and patient case histories of Boston physician John Jeffries (1745-1819), recorded from November 1775 to June 1802. Descriptions include patients’ names, ages, and physical condition, method of inoculation and symptoms. The entries dated 1800-1802 are not in chronological order.

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This layer is a georeferenced raster image of the historic paper map entitled: Map of the European and North American Railway : showing its connection with the railways of the United States & Canada, [by] A.C. Morton, engineer. It was published in 1850 by Bowen & Co. Scale [ca. 1:1,625,000]. Covers New England, eastern New York, and the Maritime Provinces. The image inside the map neatline is georeferenced to the surface of the earth and fit to the USA Contiguous Albers Equal Area Conic projection (Meters). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, or other information associated with the principal map. This map shows features such as completed, in progress, and proposed railroads, selected towns, drainage, state boundaries, and more. Includes inset: Map showing the plan for shortening the transit between New York & London. This layer is part of a selection of digitally scanned and georeferenced historic maps of New England from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

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Fifty-seven white mica clasts were separated from five samples taken from near the bases of turbidites ranging in age from early Albian to middle Eocene. Twenty two (39%) of the micas have ages between 260 and 340 Ma and five (9%) have older ages (~400-600 Ma). The former age range is characteristic of the North American Alleghenian orogeny and the Iberian Variscan orogeny. The latter range is characteristic of the North American Acadian orogeny and older basement rocks in the Grand Banks and Newfoundland areas. Both age ranges are present in the middle Eocene sample, but only the younger range occurs in the middle Albian sample. This difference could be a sampling artifact. If this is not the case, then the most likely explanation is that the Acadian-aged micas within the Meguma Zone underlying the Grand Banks were totally reset by Alleghenian reactivation of the zone, a feature which occurs extensively in Nova Scotia. The addition of Acadian-aged micas in the middle Eocene sample may reflect a change in sediment provenance as drainage systems unrelated to rift topography developed. With the exception of one clast dated at 186 Ma, the 12 other micas obtained from the upper Paleocene sample yielded ages between 55 and 74 Ma, with 7 falling within ±2 m.y. of the 57-Ma age of the sample indicated by the biostratigraphic age-depth plot for Site 1276. This, together with the volcaniclastic content of the sample, indicates an input from near-contemporaneous volcanism. The nearest known occurrences of near-contemporaneous late Paleocene volcanism that could have produced white micas are in Greenland and Portugal, some 2000 and 1500 km distant, respectively, from Site 1276 during the Paleocene. However, ages of volcanism in these areas indicate that they could probably not be sources of micas younger than 60 m.y., which suggests some as-yet unknown volcanic source in the North Atlantic area. Accumulation in the Grand Banks area of airborne-transported volcaniclastic material from eruptions of slightly different ages, followed by a single resedimentation event, could account for the spread of dates obtained from the sample. White micas from the lowermost Albian sample show a spread of ages between 37 and 284 Ma that is completely different from the age distribution pattern of the middle Albian and middle Eocene samples. The sample location is between, and at least 25 m above and below, two igneous sills dated at 98 and 105 Ma. The sills have narrow thermal aureoles and ages older than the youngest detrital micas in the sample. It is unlikely, therefore, that the spread of mica ages in the sample is due to partial resetting of ages caused by thermal effects associated with the intrusion of the sills. The resetting may have been associated with a longer lived thermal event.

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p. [3]-64: A letter to the Right Honourable the Earl of Carnarvon, principal secretary of state for the colonies; p. 65-78: Report of resolutions adopted at a conference of delegates from the provinces of Canada, Nova Scotia and New Brunswick, and the colonies of Newfoundland and Prince Edward Island, held at the city of Quebec, 10th October, 1864, as the basis of a proposed confederation of those provinces and colonies

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The Gospel of John is included in this copy; the Gospels of Matthew and John have each a special t.-p. in Micmac, dated respectively 1871 and 1872.

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v. 1. Eastern Canada, including Nova Scotia, Prince Edward island, New Brunswick, Quebec and Ontario, by Wilfred Campbell.--v. 2. Western Canada, including Manitoba, Saskatchewan, Alberta, British Columbia, and portions of old Rupert's land and the Indian territories, by George Bryce.

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Title varies slightly.

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Report year ends July 31.

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Published earlier, Halifax, 1901, as v. 11 of Collections of the Nova Scotia historical society, under title: The war of 1812. Another edition, London, 1905, has title: How Canada was held for the empire.

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Vol. 1, p. 1-158, was first published from Chipman's manuscript by John C. Allen in 1849. Vol. 2 issued originally in parts.

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Mode of access: Internet.