989 resultados para University of North Carolina (1793-1962). Philanthropic Society


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This layer is a georeferenced raster image of the historic paper map entitled: To David Stone and Peter Brown, Esq. : this first actual survey of the state of North Carolina taken by the subscribers is respectfully dedicated by their humble servants, Jona. Price and John Strother ; engraved by W. H. Harrison. It was printed by C.P. Harrison in 1808. Scale [ca. 1:506,880]. This layer is image 1 of 3 total images of the three sheet source map, representing the western portion of the map.The image inside the map neatline is georeferenced to the surface of the earth and fit to the North Carolina State Plane NAD 1983 coordinate system (in Feet) (Fipszone 3200). 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, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, canals, cities and towns, selected public buildings (churches, inns), industry locations (e.g. mills, mines, etc.), selected private buildings with names of property owners, state and county boundaries, shoreline features, and more. Relief shown pictorially and by hachures.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

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This layer is a georeferenced raster image of the historic paper map entitled: To David Stone and Peter Brown, Esq. : this first actual survey of the state of North Carolina taken by the subscribers is respectfully dedicated by their humble servants, Jona. Price and John Strother ; engraved by W. H. Harrison. It was printed by C.P. Harrison in 1808. Scale [ca. 1:506,880]. This layer is image 2 of 3 total images of the three sheet source map, representing the central portion of the map.The image inside the map neatline is georeferenced to the surface of the earth and fit to the North Carolina State Plane NAD 1983 coordinate system (in Feet) (Fipszone 3200). 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, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, canals, cities and towns, selected public buildings (churches, inns), industry locations (e.g. mills, mines, etc.), selected private buildings with names of property owners, state and county boundaries, shoreline features, and more. Relief shown pictorially and by hachures.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

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This layer is a georeferenced raster image of the historic paper map entitled: To David Stone and Peter Brown, Esq. : this first actual survey of the state of North Carolina taken by the subscribers is respectfully dedicated by their humble servants, Jona. Price and John Strother ; engraved by W. H. Harrison. It was printed by C.P. Harrison in 1808. Scale [ca. 1:506,880]. This layer is image 3 of 3 total images of the three sheet source map, representing the eastern portion of the map.The image inside the map neatline is georeferenced to the surface of the earth and fit to the North Carolina State Plane NAD 1983 coordinate system (in Feet) (Fipszone 3200). 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, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, canals, cities and towns, selected public buildings (churches, inns), industry locations (e.g. mills, mines, etc.), selected private buildings with names of property owners, state and county boundaries, shoreline features, and more. Relief shown pictorially and by hachures.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

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Observations on the ecology and distribution of meiofauna occurring on the outer continental shelf and continental slope at depths from 50 to 2500 m in the region where the Blake Plateau cuts across the North Carolina slope are reported. Total numbers of meiofauna ranged from 151/100 cm**3 of sediment at 400 m to 1196/100 cm**3 of sediment at 250 m. Sediments of the upper region (50-500 m) consisted of medium-sized calcareous sands with relatively low organic carbon contents, while the deeper sediments (600-2500 m) consisted of sandy silts and silts with organic carbon contents 6-10 times that of the shallower sediments. Two basic faunas appear to be present in the areas investigated; a shallow-water fauna extending from 50 to 500 m and a deep-water fauna from 800 to 2500 m. The shallow-water fauna consists of nematodes (the dominant taxon) and relatively large numbers of harpactacoid copepods, ostracods, benthic foraminifera, polychaetes, gastrotrichs and several other groups, while below 500 m only nematodes and foraminifera are present in large numbers, the latter being especially abundant between 800 and 2000 m. A major change in the meiofauna occurs on the Blake Plateau between the depths of approximately 400-500 m and 600-750 m where the composition of the sediment changes from sand to silty sand. From 50 m to 400-500 m gastrotrichs, turbellaria, tardigrades, kinorhynchs, halicarids, hydrozoans, gnathostomulids, lamellibranchs and cumaceans are commonly encountered; these groups are absent below 500 m. In addition, there are significant reductions in the numbers of harpactacoids, ostracods, nemerteans and polychaetes below 500 m. Examination of the nematode population also show faunal differences between the shallower sediments (50-500 m) and the deeper sediments (600-2500 m). High indices of affinity exist among the faunas between 50 and 500 m and among the faunas between 800 and 2500 m; the fauna at 600-750 m represents a transition between these two regions, but it is more closely related to the deep-water fauna. Changes in the distribution of both the total meiofuna and also the nematodes are highly correlated with changes in sediments composition and bottom water temperatures. It is suggested that changes in grain size and accompanying changes in sources of nutrition, which are the results of Gulf Stream and other current activity, are the dominant environmental factors influencing the meiofauna of the area.

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Mode of access: Internet.

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"Compilations from railroad returns are for year ending June 30, 1899-1908."

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Title varies slightly.

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Mode of access: Internet.

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Annually, the association publishes a journal, The Proceedings, which consists of papers presented at the annual meeting. Rev. Philip Mulkey, Pioneer Baptist Preacher in Upper South Carolina by Floyd Mulkey –Consolidated Book Publishers, Chicago, Ill. The South Carolina Ordnance Board, 1860-1861 by Frank E. Vandiver Some Events of the American Revolution in South Carolina as Recorded by the Rev. James Jenkins by George F. Scheer – The University of North Carolina Press

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Annually, the association publishes a journal, The Proceedings, which consists of papers presented at the annual meeting. Writing and Research in Southern History by Fletcher Melvin Green – University of North Carolina The South Carolina Constitution of 1865 as a Democratic Document by John Harold Wolfe – Appalachian State Teachers College William Porcher Miles, Progressive Mayor of Charleston, 1855-1857 by Clarence McKittrick Smith Jr. – Newberry College Salient Attributes of Bodin’s Theory of Sovereignty by Charles N. Sisson – Coker College Sources for South Carolina History in the Nation’s Capital by Maxcy Robson Dickson – The National Archives

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Annually, the association publishes a journal, The Proceedings, which consists of papers presented at the annual meeting. Writing and Research in Southern History by Fletcher Melvin Green – University of North Carolina The South Carolina Constitution of 1865 as a Democratic Document by John Harold Wolfe – Appalachian State Teachers College William Porcher Miles, Progressive Mayor of Charleston, 1855-1857 by Clarence McKittrick Smith Jr. – Newberry College Salient Attributes of Bodin’s Theory of Sovereignty by Charles N. Sission – Coker College Sources for South Carolina History in the Nation’s Capital by Maxcy Robson Dickson – The National Archives

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Annually, the association publishes a journal, The Proceedings, which consists of papers presented at the annual meeting. The Chinese Labor Issue in British Politics, 1904-1907 by E. B. Hannum – University of South Alabama A Statistical and Historical Analysis and Interpretation of British By-Elections, 1906-1909 by Michael C. Griffin Slavery and the Presence of Free Will by William F. Steirer Reconsideration: The University of South Carolina during Reconstruction by John Herbert Roper – University of North Carolina

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El terrorismo en la actualidad es considerado como uno de los conceptos más controversiales en los campos social, académico y político. El término se empieza a utilizar después de la Revolución Francesa, pero recientemente, a raíz de los atentados del 11 de septiembre de 2001, ha tomado suma relevancia y ha motivado numerosas investigaciones para tratar de entender qué es terrorismo. Aunque a la fecha existen varias revisiones sistemáticas, este trabajo tiene como propósito revisar, agrupar y concretar diferentes teorías y conceptos formulados por los autores que han trabajado sobre el concepto de “terrorismo” con el fin de entender las implicaciones de su utilización en el discurso, y cómo esto afecta la dinámica interna de las sociedades en relación con la violencia, las creencias, los estereotipos entre otros elementos. Para lograrlo, se revisaron 56 artículos, publicados entre los años 1985 y 2013; 10 fuentes secundarias entre noticias y artículos de periódicos correspondientes a los años 1995-2013 y 10 estudios estadísticos cuyos resultados nos aportan a la comprensión del tema en cuestión. La búsqueda se limitó al desarrollo histórico del terrorismo, sus diferentes dimensiones y el concepto social de la realidad de terrorismo. Los hallazgos demuestran que la palabra “terrorismo” constituye un concepto que como tal es un vehículo lingüístico que puede ser utilizado con fines, estratégicos movilizando al público conforme a través del discurso e intereses políticos, destacando la necesidad de estudiar las implicaciones psicológicas y sociales de su uso.

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El trabajo pretende brindar una aproximación crítica analítica a aquella propositiva histórica familiar dentro de la extensa literatura sobre los orígenes de la Guerra Fría. Reconociendo de antemano que el escenario de la Guerra Fría no fue necesariamente el efecto de una amenaza inminente.

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Las obras geográficas de Manuel Ancízar y Felipe Pérez dan cuenta de la manera en la que la élite intelectual neogranadina se apropió y representó el aspecto físico y humano de la nación al inicio y final de la Comisión Corográfica (1850-1859). Un análisis comparativo de las obras mostrará la manera en la que la narración literaria y la geográfica influyen en la elaboración de imaginarios territoriales para unificar la nación y consolidar la identidad nacional a partir de la apropiación territorial en la segunda mitad del siglo XIX