987 resultados para West Point Region (N.Y.)--Maps, Topographic.


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En este nuevo número de los Cuadernos del CILHA reunimos una serie de trabajos referidos a los temas de la literatura del Caribe y de la autoficción en América Latina. El conjunto de trabajos referidos a la literatura del Caribe constituye un esfuerzo que le debemos a Lancelot Cowie y Nina Bruni, ambos de la University of West Indies, de Trinidad y Tobago. Estos profesores, para mayores datos, han creado en la Universidad anglófona el Centre for Latin America and Caribbean (CENLAC), un centro de estudios de la cultura latinoamericana. El dossier del Caribe, entonces, presenta una serie de investigaciones que abordan nuevas problemáticas y autores poco conocidos en el Cono Sur, por no decir desconocidos debido a la escasa o nula circulación editorial; así como también el dossier contiene trabajos sobre autores consagrados, aunque en esta oportunidad se ofrecen nuevas y renovadas miradas. Los estudios literarios del área del Cono Sur presentan una marcada ausencia de investigaciones sobre la producción caribeña. Entre las razones de tal déficit se puede mencionar la secular incomunicación que existe entre las diversas naciones latinoamericanas, una problemática que abarca por lo menos todo el período republicano, y que se intensifica, en la actualidad, con ciertas políticas editoriales metropolitanas. Una segunda razón, derivada de lo anterior, es el escaso conocimiento del movimiento cultural del Caribe que se posee en el Cono Sur. El título de este dossier, “Voces del Caribe", es bastante elocuente respecto de su contenido, ya que ofrece un panorama a través de discursos polifónicos, plurales y heterogéneos. Ello es así en virtud de que tales características son las que mejor representan el abigarrado universo caribeño, que es además plurirracial, plurilingüístico y caótico, en el sentido que le dio Antonio Benítez Rojo al Caos en su ya clásico estudio sobre la cultura del Caribe, La isla que se repite. Esperamos que con este esfuerzo de los Cuadernos contribuyamos en algo al acercamiento entre el Caribe y el resto de América Latina. El segundo dossier de este número ha estado a cargo de Miriam Di Gerónimo, investigadora y docente de la Universidad Nacional de Cuyo, especialista en narrativa breve y en la obra de Julio Cortázar. La Dra. Di Gerónimo ha reunido un conjunto de investigadores de prestigio internacional para tratar el tema de la autoficción en la literatura de lengua hispana. Como ella misma dice en la introducción los autores

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La presente experiencia se desarrolló en el área Ciencias Naturales, en 1° año de la Educación Secundaria Básica del Colegio Nacional Rafael Hernández de la Universidad Nacional de La Plata, siguiendo el marco teórico referencial "La Enseñanza para la Comprensión". Esta presentación pretende dar a conocer la secuencia didáctica que se realizó, como parte de un proyecto institucional denominado Período de Síntesis, cuyo objetivo es que los alumnos sinteticen y demuestren la comprensión alcanzada a través de desempeños trabajados durante el año. Para diseñar la experiencia se tuvieron en cuenta las metas de comprensión irrenunciables en primer año y para el diseño de los desempeños de síntesis se utilizaron diferentes recursos didácticos, como power point, redes conceptuales y c--map. Como fortalezas de la propuesta, se valora la participación y predisposición de los alumnos así como la integración de los contenidos desarrollados durante el año. La experiencia proporcionó mayores conocimientos de cómo aprenden los estudiantes, y, en algunos casos, permitió a alumnos que no habían alcanzado las metas de comprensión seleccionadas, lograrlo. La realización de los desempeños de síntesis fue parte del modelo de evaluación continua en proceso, a partir de la cual se realizó la acreditación

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La presente experiencia se desarrolló en el área Ciencias Naturales, en 1° año de la Educación Secundaria Básica del Colegio Nacional Rafael Hernández de la Universidad Nacional de La Plata, siguiendo el marco teórico referencial "La Enseñanza para la Comprensión". Esta presentación pretende dar a conocer la secuencia didáctica que se realizó, como parte de un proyecto institucional denominado Período de Síntesis, cuyo objetivo es que los alumnos sinteticen y demuestren la comprensión alcanzada a través de desempeños trabajados durante el año. Para diseñar la experiencia se tuvieron en cuenta las metas de comprensión irrenunciables en primer año y para el diseño de los desempeños de síntesis se utilizaron diferentes recursos didácticos, como power point, redes conceptuales y c--map. Como fortalezas de la propuesta, se valora la participación y predisposición de los alumnos así como la integración de los contenidos desarrollados durante el año. La experiencia proporcionó mayores conocimientos de cómo aprenden los estudiantes, y, en algunos casos, permitió a alumnos que no habían alcanzado las metas de comprensión seleccionadas, lograrlo. La realización de los desempeños de síntesis fue parte del modelo de evaluación continua en proceso, a partir de la cual se realizó la acreditación

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La presente experiencia se desarrolló en el área Ciencias Naturales, en 1° año de la Educación Secundaria Básica del Colegio Nacional Rafael Hernández de la Universidad Nacional de La Plata, siguiendo el marco teórico referencial "La Enseñanza para la Comprensión". Esta presentación pretende dar a conocer la secuencia didáctica que se realizó, como parte de un proyecto institucional denominado Período de Síntesis, cuyo objetivo es que los alumnos sinteticen y demuestren la comprensión alcanzada a través de desempeños trabajados durante el año. Para diseñar la experiencia se tuvieron en cuenta las metas de comprensión irrenunciables en primer año y para el diseño de los desempeños de síntesis se utilizaron diferentes recursos didácticos, como power point, redes conceptuales y c--map. Como fortalezas de la propuesta, se valora la participación y predisposición de los alumnos así como la integración de los contenidos desarrollados durante el año. La experiencia proporcionó mayores conocimientos de cómo aprenden los estudiantes, y, en algunos casos, permitió a alumnos que no habían alcanzado las metas de comprensión seleccionadas, lograrlo. La realización de los desempeños de síntesis fue parte del modelo de evaluación continua en proceso, a partir de la cual se realizó la acreditación

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Lithobiostratigraphic data indicate that the double reflectors on the seismic profile through Ocean Drilling Program (ODP) Site 1148 represent two unconformities that coincide, respectively, with the lower/upper Oligocene boundary at ~488 mcd, and Oligocene-Miocene boundary at 460 mcd. Two other unconformities, at ~478 and 472 mcd, respectively, were also identified within the upper Oligocene section. Together they erased a sediment record of about 3 Ma from this locality in a period of very active seafloor spreading. The existence of 32.8 Ma marine sediment at the terminated depth (850 mcd) indicates that the initial breakup of the South China Sea (SCS) was probably during 34-33 Ma, close to the Eocene-Oligocene boundary. High sedimentation rates of 60-115 m/my from the much expanded, N350 m lower Oligocene section resulted from rifting and rapid subsidence between 33 and 29 Ma. The mid-Oligocene unconformity at ~28.5 Ma, which also occurred in many parts of the Indo-West Pacific region, was probably related to a significant uplift of the Himalayan-Tibetan Plateau to the west and the initial collision between Indonesia and Australia in the south. A narrowed Indonesian seaway may have accounted for the late Oligocene warming and chalk deposition in the northern South China Sea including the Site 1148 locality. The unconformities and slumps near the Oligocene-Miocene boundary indicate a very unstable tectonic regime, probably corresponding to changes in the rotation of different land blocks and the seafloor spreading ridge from nearly E-W to NE-SW, as recognized earlier at magnetic Anomaly 7. This 25 Ma event also saw the first New Guinea terrane docking at the northern Australian craton. The low sedimentation rate of ~15 m/my in the early to middle Miocene may correspond to another period of rapid seafloor spreading and rapid widespread subsidence that effectively caused sediment source areas to retreat with a rapidly rising sea level. The isostatic nature of these late Oligocene unconformities and slumps with several major collision-uplift events indicate that the rapid changes in the early evolutionary history of the South China Sea were mainly responding to regional tectonic reconfiguration including the uplift-driven southeast extrusion of the Indochina subcontinent.

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This paper presents an algorithm for generating scale-free networks with adjustable clustering coefficient. The algorithm is based on a random walk procedure combined with a triangle generation scheme which takes into account genetic factors; this way, preferential attachment and clustering control are implemented using only local information. Simulations are presented which support the validity of the scheme, characterizing its tuning capabilities.

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Este proyecto presenta un software para el análisis de imágenes dermatoscópicas correspondiente a lesiones melanocíticas, con el fin de clasificarlas entre lesiones benignas y melanoma. El sistema realiza una segmentación automática de la lesión y la procesa en varas etapas, extrayendo características de relevancia diagnóstica: asimetría, colores, irregularidad del borde, y la presencia de estructuras como redes pigmentadas atípicas o velo azul-blanquecino. Proporciona además una herramienta para el etiquetado manual de estructuras adicionales. La clasificación automática de las lesiones se realiza en base a los métodos de diagnóstico más comúnmente utilizados: las reglas ABCD, Menzies, 7-point checklist, CASH y CHAOS & CLUES. El sistema de clasificación se evalúa sobre una base de datos de imágenes dermatoscópicas, y se realiza una comparativa de los resultados obtenidos por cada método de diagnóstico. ABSTRACT. This project presents a software for the analysis of dermoscopic images of melanocytic lesions, and their classification into benign lesions and melanoma. The system performs automatic segmentation of the lesion and goes through several stages of extraction of certain characteristics relevant to the diagnosis, such as asymmetry, border irregularity, or presence of structures like atypical pigmented network or blue-whitish veil. Automatic classification of the lesions is accomplished by means of the most commonly used diagnostic methods, such as ABCD and Menzies's rules, the 7-point checklist, CASH, and CHAOS & CLUES. The classification system is evaluated by using a dermoscopic image database, and a comparison of the results yielded by the different diagnostic methods is performed.

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In the South West Pacific region, the striking geographical correlation between the frequency of α+-thalassemia and the endemicity of Plasmodium falciparum suggests that this hemoglobinopathy provides a selective advantage against malaria. In Vanuatu, paradoxically, α+-thalassemia increases the incidence of contracting mild malaria in the first 2 years of life, but severe disease was too uncommon to assess adequately. Therefore, we undertook a prospective case-control study of children with severe malaria on the north coast of Papua New Guinea, where malaria transmission is intense and α+-thalassemia affects more than 90% of the population. Compared with normal children, the risk of having severe malaria was 0.40 (95% confidence interval 0.22–0.74) in α+-thalassemia homozygotes and 0.66 (0.37–1.20) in heterozygotes. Unexpectedly, the risk of hospital admission with infections other than malaria also was reduced to a similar degree in homozygous (0.36; 95% confidence interval 0.22–0.60) and heterozygous (0.63; 0.38–1.07) children. This clinical study demonstrates that a malaria resistance gene protects against disease caused by infections other than malaria. The mechanism of the remarkable protective effect of α+-thalassemia against severe childhood disease remains unclear but must encompass the clear interaction between this hemoglobinopathy and both malarial and nonmalarial infections.

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This layer is a georeferenced raster image of the historic paper map entitled: Topographical map of the city of Providence showing proposed sewerage system together with sewers already constructed, compiled in the City Engineers Office. It was published Oct. 24, 1884 by the City Engineers Office, Sewer Dept. Scale [ca. 1:20,000]. Covers the city of Providence, Rhode Island and portions of the surrounding towns/cities. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Rhode Island State Plane Coordinate System (Feet) (FIPS 3800). 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 roads, railroads, topography, drainage, selected buildings, constructed and proposed sewer lines, town boundaries, city districts, and more. Relief shown by contours. 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 map purposes.

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This layer is a georeferenced raster image of the United States Geological Survey sheet map entitled: Philadelphia County, Pennsylvania, produced by the United States Geological Survey ; Commonwealth of Pennsylvania, Department of Environmental Resources, Topographic and Geologic Survey. It was published in 1983. Scale 1:50,000. Compiled from USGS 1:24,000-scale topographic maps. Planimetry revised from aerial photographs taken in 1981 and other source data. Revised information not field checked. Map edited 1982. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Pennsylvania South State Plane Coordinate System NAD27 (in Feet) (Fipszone 3702). 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. USGS maps are typical topographic maps portraying both natural and manmade features. They show and name works of nature, such as mountains, valleys, lakes, rivers, vegetation, etc. They also identify the principal works of humans, such as roads, railroads, boundaries, transmission lines, major buildings, etc. Relief is shown with standard contour intervals of 20 feet and spot heights. Please pay close attention to map collar information on projections, spheroid, sources, dates, and keys to grid numbering and other numbers which appear inside the neatline. Includes notes, index to 1:24,000-scale maps, and location map. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

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This layer is a georeferenced raster image of the historic paper map entitled: Topographical map of the District of Columbia and a portion of Virginia, compiled under the direction of Major G.J. Lydecker, Corps of Engineers, Engineer Commissioner D.C., by Captain F.V. Greene, Corps of Engineers ; drawn by W.T.O. Bruff. It was published in 1884. Scale [1:15,840]. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Maryland State Plane Coordinate System Meters NAD83 (Fipszone 1900). 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, railroads, drainage, selected public buildings, selected private residences and names of landowners, built-up areas, parks, and more. Relief shown by contours. Depths shown by soundings. Includes source materials note. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

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This layer is a georeferenced raster image of the historic paper map entitled: Topographical map of the original District of Columbia and environs showing the fortifications around the city of Washington, by E.G. Arnold C.E. It was published by G. Woolworth Colton in 1862. Scale [ca. 1:31,680]. Covers also adjacent portions of Virginia and Maryland. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Maryland State Plane Coordinate System Meters NAD83 (Fipszone 1900). 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, railroads, bridges, canals, drainage, cities and towns, forts, selected public buildings and places of interest, hospitals, schools, Washington, D.C. school districts, selected private residences with names of landowners, and more. Relief is shown by hachures. Includes text and population tables. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

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This layer is a georeferenced raster image of the historic paper map entitled: New Orleans and vicinity, Louisiana. It was published by the Geological Survey in 1956. Scale 1:24,000. Covers also adjacent portions of Jefferson, St. Bernard, and Plaquemines Parishes. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Louisiana State Plane Coordinate System, South NAD27 (in Feet) (Fipszone 1702). 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 is a topographic map showing features such as roads, railroads, canals, levees, drainage, selected public and industrial buildings, cemeteries, Parish boundaries, ferry routes, and more. Relief shown by contours and spot heights. Depths shown by soundings. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

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This layer is a georeferenced raster image of the historic paper map entitled: Regional plan map of Cincinnati, Ohio, prepared by City Planning Commission, Technical Advisory Corporation Consulting Engineers. It was published by Technical Advisory Corp. in 1925. Scale 1:62,500. Covers also a portion of Northern Kentucky. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Ohio South State Plane NAD 1983 coordinate system (in Feet) (Fipszone 3402). 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 is a typical topographic map portraying both natural and manmade features. It shows and names works of nature, such as mountains, valleys, lakes, rivers, vegetation, etc. It also identify the principal works of humans, such as roads, railroads, boundaries, transmission lines, major buildings, etc. Relief is shown with standard contour intervals of 20 feet. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

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This layer is a georeferenced raster image of the historic, topographic paper map entitled: Cleveland and vicinity, Ohio. It was published by The Survey in 1956. Scale 1:24,000. Compiled from 1:24,000 scale maps of the Mayfield Heights 1953, East Cleveland 1953, Cleveland North 1953, Lakewood 1953, Cleveland South 1953, Shaker Heights 1953, and Chagrin Falls 1953 7.5 minute quadrangles. Hydrography from U.S. Lake Survey Charts 35 (1:80,000) and 354 (1:10,000). The image inside the map neatline is georeferenced to the surface of the earth and fit to the Ohio North State Plane NAD 1927 coordinate system (in Feet) (Fipszone 3401). 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 is a typical topographic map portraying both natural and manmade features. It shows and names works of nature, such as mountains, valleys, lakes, rivers, vegetation, etc. It also identify the principal works of humans, such as roads, railroads, boundaries, transmission lines, major buildings, etc. Relief is shown with standard contour intervals of 5 and 10 feet. Depths are shown with bathymetric isolines and soundings. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.