18 resultados para Cilley, Jonathan, 1802-1838.

em Brock University, Canada


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The study area is situated in NE Newfoundland between Gander Lake and the north coast and on the boundary between the Gander and Botwood tectonostratigraphic zones (Williams et al., 1974). The area is underlain by three NE trending units; the Gander Group, the Gander River Ultramafic Belt (the GRUB) and the Davidsville Group. The easternmost Gander Group consists of a thick, psammitic unit composed predominantly of psammitic schist and a thinner, mixed unit of semipelitic and pelitic schist with minor psammite. The mixed unit may stratigraphically overlie the psammitic unit or be a lateral facies equivalent of the latter. No fossils have been recovered from the Gander Group. The GRUB is a terrain of mafic and ultramafic plutonic rocks with minor pillow lava and plagiogranite. It is interpreted to be a dismembered ophiolite in thrust contact with the Gander Group. The westernmost Davidsville Group consists of a basal conglomerate, believed deposited unconformably upon the GRUB from which it was derived, and an upper unit of greywacke and slate, mostly of turbidite origin, with minor limestone and calcareous sandstone. The limestone, which lies near the base of the unit, contains Upper Llanvirn to Lower Llandeilo fossils. The Gander and Davidsville Groups display distinctly different sedimentological , structural and metamorphic histories. The Gander Group consists of quartz-rich, relatively mature sediment. It has suffered three pre-Llanvirn deformations, of which the main deformation, Dp produced a major, NE-N-facing recumbent anticline in the southern part of the study area. Middle greenschist conditions existed from D^ to D- with growth of metamorphic minerals during each dynamic and static phase. In contrast, the mineralogically immature Davidsville Group sediment contains abundant mafic and ultramafic detritus which is absent from the Gander Group. The Davidsville Group displays the effects of a single penetrative deformation with localized D_ and D_ features, all of which can be shown to postdate D_ in the Gander Group. Rotation of the flat Gander S- into a subvertical orientation near the contact with the GRUB and the Davidsville Group is believed to be a Davidsville D^ feature. Regional metamorphism in the Davidsville Group is lower greenschist with a single growth phase, MS . These sedimentological, structural and metamorphic differences between the Gander and Davidsville Groups persist even where the GRUB is absent and the two units are in contact, indicating that the tectonic histories of the Gander and Davidsville Groups are distinctly different. Structural features in the GRUB, locally the result of multiple deformations, may be the result of Gander and/or Davidsville deformations. Metamorphism is in the greenschist facies. Geochemical analyses of the pillow lava suggest that these rocks were formed in a back-arc basin. Mafic intrusives in the Gander Group appear to be the result of magraatism separate from that producing the pillow lava. The Gander Group is interpreted to be a continental rise prism deposited on the eastern margin of the Late Precambrian-Lower Paleozoic lapetus Ocean. The GRUB, oceanic crust possibly formed in a marginal basin to the west, is believed to have been thrust eastward over the Gander Group, deforming the latter, during the pre-Llanvirnian, possibly Precambrian, Ganderian Orogeny. The Middle Ordovician and younger Davidsville Group was derived from, and deposited unconformably on, this deformed terrain. Deformation of the Davidsville Group occurred during the Middle Devonian Acadian Orogeny.

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Lt. Col. John Clark (1787-1862) was born in Kingston, Upper Canada. In 1801 Clark became a private in the 1st regiment of the Lincoln Militia, serving under Ralfe Clench. By June 1812 he was promoted to lieutenant by Maj. Gen. Sir Isaac Brock. During the War of 1812 he served as lieutenant and adjutant for the Lincoln Militia flank company on the Niagara frontier under Col. William Claus, and was present at the surrender of the enemy at the battle of Queenston Heights. By 1838 the Lincoln Militia was being re-organized and Lt. Col John Clark was requested to lead the 5th Regiment, made up of men from both Grantham and Louth townships in Lincoln County. He served in this capacity until his retirement in 1851?. Around this same time Clark bought from William May Jr. a house in Grantham Township. He was to call his home Walnut Dale Farm. John Clark also served as the customs collector for Port Dalhousie, and as a secretary in the Welland Canal Company. One hundred years later efforts by a local heritage group to save John Clark’s home failed, when the house was hit by arsonists. By this time the house had become known as the May-Clark-Seiler House. See RG 195 Anne Taylor Fonds for more information regarding the efforts of the heritage group to save this home. Clark died in 1862 at the age of 79 years and is buried in Victoria Lawn Cemetery. John Clark’s daughter Catherine (mentioned in the diary portion of the papers) was married to William Morgan Eccles.

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Survey map and description of Jonathan Clendenning's land created by The Welland Canal Company. Included is two written descriptions of the land along with two drawings of the land. Noteable features for the first (small) map include; line between the Clendennan and Sanderson properties, line between Clendennan and Steward properties, canal. Noteable features for map #2 (large map)include; numerous surrounding farms, roads. Surveyor notes are seen in pencil on both the maps. The deed for the land is dated August 23, 1826.Pages 49-51

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Survey map and description of Jonathan Silverthorn's land created by The Welland Canal Company. Included is a written description of the land along with a drawing of the land. The lands surveyed include lots 229 and 230. The land was first surveyed in 1830, then again in 1834, by George Keefer. The original survey only included the feeder and resevoir and wood land, whereas the second survey shows all lands owned by Silverthorn. The land totals 19.2 acres, 2 roads and 32 perches. The land is broken down as follows; 7.6 acres cleared land, canal and towpath, 6.6 acres reservoir - Michael Silverthorn, 5 acres woodland. Surveyor notes are seen in pencil and red pen on the map.See also page 138.

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An account of Jonathon Phillips, a settler in the Bay of Quinte region and a War of 1812 veteran. Printed at the Chronicle Office, Belleville

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The recipient of the letters is John Henry Dunn who was born on St. Helena (a British territory island of volcanic origin located in the South Atlantic Ocean) in 1792 to John Charles Dunn and Elizabeth Bazette. He was married to Charlotte Roberts on May 4th, 1820 and they had 6 sons and 2 daughters. He came to Canada in 1820 in which year he became the Receiver General for Canada. He held this position until 1841.Charlotte died in 1835. In 1822 he was named to the Province’s Legislative Council. He was president of the Welland Canal Company from 1825-1833. In 1836 he was named to the executive council of Upper Canada but resigned 3 weeks later with fellow counselors when lieutenant governor Sir Francis Bond refused the advice of the council. Dunn was made the Receiver General for the newly formed Province of Canada in 1841, and was elected to represent Toronto in the legislative assembly that year. He married his second wife on March 9th, 1842. Her name was Sophie-Louise Juchereau Duchsnay. They had a son and a daughter. In 1843 he resigned, and was not re-elected in 1844. He returned to England with his family and died in London on April 21, 1854. Dunn was a supporter of the Welland Canal, St. Lawrence Canals and other public improvements. Between the passage of the Canada Trade Act and the Act of the Union he had tried to insure that projects received funding despite financial constraints. He claimed that he has saved Upper Canada from bankruptcy. His son, Alexander Roberts Dunn received the Victoria Cross for his role in the Charge of the Light Brigade at Balaclava. Dunn Street in Niagara Falls is named after John Henry Dunn. The town and township of Dunnville were also named for him. Sources: http://biographi.ca/009004-119.01-e.php?id_nbr=3889 http://www.niagarafrontier.com/cityfalls.html

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A finding aid for collection RG 86. This archive contains materials relating to Niagara Falls and its development during the late 19th and early 20th century, with particular focus on power operations.

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Two newspaper clippings from the Montreal Herald of 1838 and an essay clipped from a book, handsewn into a booklet with paper cover and handwritten title and notes. The burning of the Caroline / Susanna Moodie -- The cutting out of the Caroline : a true story / by Francis W. Rowsell -- Juvenile courage and patriotism : instanced in Canada, during the disturbances at the close of the year 1837

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Message from the President of the United States transmitting a letter from the Marshal of the Northern District of the State of New York, respecting Disturbances on the Canadian Frontier.

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Message from the President of the United States transmitting the information required by a resolution of the House of Representatives of the 21st ultimo, respecting the Capture and Destruction of the Steamboat Caroline, on the night of the 29th December last.

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An invoice for goods bought in Port Robinson, 28, May 1838. The list of goods includes: Blue cloth, buttons & thread, high lace shoes etc. There is also a note which reads "To Mr. W. Cowen, Dear Sir, The above is the quantity of goods you wanted and as ---- the quality as may be. I hope they will suit him. I have not all the ------- for the vest & pant above, but have sent what I have. I could not procure a silk handkerchief of any kind. I think Mr. Donaldson will be up soon he is now at Toronto. Give my compliments to Mrs. Cowan & family no more at present" Robert Elliot

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Catherine (Lemon) Everingham was the widow of James Everingham, a private with the first Battalion of Colo Delancys Regt. of the Jersey Volunteers. He died in the American Revolutionary War in 1796, leaving his wife and two children settled on two hundred acres of land in the Township of Willoughby. No certificate had been awarded to James Everingham for this land. Catherine subsequently petitioned the government to grant her the land that she had settled on with her family.