920 resultados para Carroll, Rory


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Nos últimos trinta anos, pesquisadores da área da saúde tem dado especial atenção ao tema da educação interprofissional (EIP), por esta estar relacionada com uma maior satisfação dos usuários e a oferta de uma assistência em saúde mais resolutiva e satisfatória. A necessidade de adotarmos a EIP como uma ferramenta para a formação de profissionais da saúde surge a partir do momento que percebemos que nosso sistema de saúde presta cuidados fragmentados e pouco resolutivos. Atualmente, estudos científicos comprovam que a prática colaborativa e um cuidado ofertado com qualidade é facilmente alcançável se os profissionais trabalharem em equipe com objetivos comuns, sendo imprenscindível o desenvolvimento de habilidades de comunicação interprofissional e prática colaborativa desde o início da graduação. Desta forma, este estudo tomou como objeto de investigação a educação interprofissional, no contexto da atenção primária a saúde e na perspectiva da integração do ensino com os serviços públicos de saúde, por meio do programa Pró PET-Saúde USP-Capital 2012/2014. A escolha do programa para o presente estudo foi devido a natureza interprofissional do projeto, visto que engloba estudantes, preceptores e tutores de diversos cursos da área da saúde e por este ter constituído um espaço privilegiado de aprendizado e aperfeiçoamento na formação em saúde, dando origem a outras iniciativas interprofissionais na Universidade de São Paulo (USP). A coleta de dados ocorreu de duas formas, sendo a primeira por meio de questionários individuais destinado aos profissionais de saúde (preceptores) e estudantes, com trechos da obra de Lewis Carroll \"As Aventuras de Alice no País das Maravilhas\", e por meio de um roteiro de entrevista destinado aos docentes (tutores) participantes do programa. Os dados obtidos foram analisados através da análise temática proposta por Minayo. Os resultados mostram que assim como a personagem Alice do livro de Carroll, muitas vezes ficamos confusos sobre quais opções escolher para aperfeiçoar a nossa formação em saúde. Se não soubermos onde queremos chegar, qualquer caminho se torna o certo, porém as evidências comprovam que a escolha por oportunidades de educação interprofissional na graduação e na pós graduação em saúde podem minimizar estereótipos e preconceitos formados pelos estudantes em relação as outras categorias profissionais e desenvolver habilidades de comunicação interprofissional e resolução de conflitos que contribuirá para uma prática colaborativa e a melhor assistência em saúde. Como produto do mestrado profissional foi elaborado um plano de aula destinado aos estudantes da USP com a finalidade de problematizar e permitir uma breve experiência da educação interprofissional.

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prepared under the direction of Carroll D. Wright ; for the use of the United States Department of Labor.

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Historical review of wages and prices. 1752-1860 -- Comparative wages, prices, and cost of living: Massachusetts and Great Britain. 1860-1883.

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This layer is a georeferenced raster image of the historic paper map entitled: Topographical map of the county of Penobscot Maine, from surveys under the direction of H.F. Walling; field work under the direction of L.H. Eaton. It was published by Lee & Marsh in 1859, Scale 1:80,000. This layer is image 2 of 2 total images, representing the northeast portion of the four sheet source map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Universal Transverse Mercator projection (UTM Zone 19N, meters, NAD1983). 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, public buildings, schools, churches, cemeteries, industry locations (e.g. mills, factories, mines, etc.), private buildings with names of property owners, town boundaries, and more. Relief shown by hachures. It includes many cadastral insets of individual county towns and villages. It also includes illustrations, business directories, and tables of statistics and distances.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 historic paper map entitled: New Hampshire by recent survey : made under the supreme authority and published according to law by Philip Carrigain ; J.J. Barralet, del. ; W. Harrison, sct., Philada. It was published by Philip Carrigain in 1816. Scale [ca. 1:200,000]. This layer is image 5 of 6 total images, representing the center west portion of the six sheet source map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the New Hampshire State Plane coordinate system (NAD 1983 in Feet) (Fipszone 2800). 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, public buildings, schools, churches, industry locations (e.g. mills, factories, mines, etc.), selected private buildings with names of property owners, town boundaries, land grants, and more. Relief shown pictorially and by hachures. Includes area notes, text, and table of population. Also includes illustrations: View of the Great Boars Head and Hampton Beach -- The Cap of the White Mountains -- View of the White Mountains from Shelburne; inset maps: States of the Union east of the Hudson with the adjacent British colonies. Scale [ca. 1:1,920,000] -- The middle, southern and western sections of the United States with the territories. Scale [ca. 1:4,900,000]. Includes: ms. additions with updated county boundary & township names.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 historic paper map entitled: New Hampshire by recent survey : made under the supreme authority and published according to law by Philip Carrigain ; J.J. Barralet, del. ; W. Harrison, sct., Philada. It was published by Philip Carrigain in 1816. Scale [ca. 1:200,000]. This layer is image 6 of 6 total images, representing the northwest portion of the six sheet source map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the New Hampshire State Plane coordinate system (NAD 1983 in Feet) (Fipszone 2800). 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, public buildings, schools, churches, industry locations (e.g. mills, factories, mines, etc.), selected private buildings with names of property owners, town boundaries, land grants, and more. Relief shown pictorially and by hachures. Includes area notes, text, and table of population. Also includes illustrations: View of the Great Boars Head and Hampton Beach -- The Cap of the White Mountains -- View of the White Mountains from Shelburne; inset maps: States of the Union east of the Hudson with the adjacent British colonies. Scale [ca. 1:1,920,000] -- The middle, southern and western sections of the United States with the territories. Scale [ca. 1:4,900,000]. Includes: ms. additions with updated county boundary & township names.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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'Reproduced with permission from Environmental Health Perspectives'

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A cuarenta años del último Golpe de Estado en nuestro país se hace preciso recrear las lecturas que las manifestaciones artísticas del período de la post dictadura construyeron de su propia historia, particularmente desde el cine. Toda sociedad reflexiona sobre las causas profundas de sus conflictos y el cine, como manifestación artística, logra integrar lo icónico y lo lingüístico, imagen y sonido, convirtiéndose así, en uno de los medios más utilizados a la hora de denunciar determinados sucesos que contribuyen a reconstruir el entramado social desgarrado por la última dictadura. El cine abre nuevas perspectivas sobre lo que una sociedad confiesa de sí misma y también sobre lo que niega, este artículo intenta ser una invitación a revisitar el film La Historia Oficial (Puenzo, 1985) interpretando la trama que narra a partir del viaje de Alicia de Lewis Carroll. Para la Alicia de Carroll, atravesar el espejo implica traspasar el universo de la rutinaria y aburrida realidad a un mundo maravilloso, contrariamente, la Alicia de la película, habitó un mundo fantástico toda su vida y atravesar el espejo significará pasar del espacio privado al público. En ese recorrido, por ese "mundo extraño", descubrirá que el país de las maravillas que la albergaba, desapareció

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Polycyclic aromatic hydrocarbons (PAHs) are common environmental contaminants which can be derived from anthropogenic sources, such as combustion and discharges from extraction and transport, and natural processes, including leakage and erosion of fossil carbon. Natural PAH sources contribute, along with biological activities and terrestrial run-off, to the organic carbon content in sediments.The Barents Sea region is far from many anthropogenic sources of PAH, but production and trans-shipment of hydrocarbons is increasing. We present data for polycyclic aromatic hydrocarbon (PAH) concentrations in bottom sediments from 510 stations in the Barents and White Seas, and along the northern coast of Norway.

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A major trough ('Belgica Trough') eroded by a palaeo-ice stream crosses the continental shelf of the southern Bellingshausen Sea (West Antarctica) and is associated with a trough mouth fan ('Belgica TMF') on the adjacent continental slope. Previous marine geophysical and geological studies investigated the bathymetry and geomorphology of Belgica Trough and Belgica TMF, erosional and depositional processes associated with bedform formation, and the temporal and spatial changes in clay mineral provenance of subglacial and glaciomarine sediments. Here, we present multi-proxy data from sediment cores recovered from the shelf and uppermost slope in the southern Bellingshausen Sea and reconstruct the ice-sheet history since the last glacial maximum (LGM) in this poorly studied area of West Antarctica. We combined new data (physical properties, sedimentary structures, geochemical and grain-size data) with published data (shear strength, clay mineral assemblages) to refine a previous facies classification for the sediments. The multi-proxy approach allowed us to distinguish four main facies types and to assign them to the following depositional settings: 1) subglacial, 2) proximal grounding-line, 3) distal sub-ice shelf/subsea ice, and 4) seasonal open-marine. In the seasonal open-marine facies we found evidence for episodic current-induced winnowing of near-seabed sediments on the middle to outer shelf and at the uppermost slope during the late Holocene. In addition, we obtained data on excess 210Pb activity at three core sites and 44 AMS 14C dates from the acid-insoluble fraction of organic matter (AIO) and calcareous (micro-)fossils, respectively, at 12 sites. These chronological data enabled us to reconstruct, for the first time, the timing of the last advance and retreat of the West Antarctic Ice Sheet (WAIS) and the Antarctic Peninsula Ice Sheet (APIS) in the southern Bellingshausen Sea. We used the down-core variability in sediment provenance inferred from clay mineral changes to identify the most reliable AIO 14C ages for ice-sheet retreat. The palaeo-ice stream advanced through Belgica Trough after ~36.0 corrected 14C ka before present (B.P.). It retreated from the outer shelf at ~25.5 ka B.P., the middle shelf at ~19.8 ka B.P., the inner shelf in Eltanin Bay at ~12.3 ka B.P., and the inner shelf in Ronne Entrance at ~6.3 ka B.P.. The retreat of the WAIS and APIS occurred slowly and stepwise, and may still be in progress. This dynamical ice-sheet behaviour has to be taken into account for the interpretation of recent and the prediction of future mass-balance changes in the study area. The glacial history of the southern Bellingshausen Sea is unique when compared to other regions in West Antarctica, but some open questions regarding its chronology need to be addressed by future work.

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The Belgica Trough and the adjacent Belgica Trough Mouth Fan in the southern Bellingshausen Sea (Pacific sector of the Southern Ocean) mark the location of a major outlet for the West Antarctic Ice Sheet during the Late Quaternary. The drainage basin of an ice stream that advanced through Belgica Trough across the shelf during the last glacial period comprised an area exceeding 200,000 km**2 in the West Antarctic hinterland. Previous studies, mainly based on marine-geophysical data from the continental shelf and slope, focused on the bathymetry and seafloor bedforms, and the reconstruction of associated depositional processes and ice- drainage patterns. In contrast, there was only sparse information from seabed sediments recovered by coring. In this paper, we present lithological and clay mineralogical data of 21 sediment cores collected from the shelf and slope of the southern Bellingshausen Sea. Most cores recovered three lithological units, which can be attributed to facies types deposited under glacial, transitional and seasonally open-marine conditions. The clay mineral assemblages document coinciding changes in provenance. The relationship between the clay mineral assemblages in the subglacial and proglacial sediments on the shelf and the glacial diamictons on the slope confirms that a grounded ice stream advanced through Belgica Trough to the shelf break during the past, thereby depositing detritus eroded in the West Antarctic hinterland as soft till on the shelf and as glaciogenic debris flows on the slope. The thinness of the transitional and seasonally open-marine sediments in the cores suggests that this ice advance occurred during the last glacial period. Clay mineralogical, acoustic sub-bottom and seismic data furthermore demonstrate that the palaeo-ice stream probably reworked old sedimentary strata, including older tills, on the shelf and incorporated this debris into its till bed. The geographical heterogeneity of the clay mineral assemblages in the sub- and proglacial diamictons and gravelly deposits indicates that they were eroded from underlying sedimentary strata of different ages. These strata may have been deposited during either different phases of the last glacial period or different glacial and interglacial periods. Additionally, the clay mineralogical heterogeneity of the soft tills recovered on the shelf suggests that the drainage area of the palaeo-ice stream flowing through Belgica Trough changed through time.

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Back Row: Trainer Mike Willie, Assistant coaches Frank Maloney, Jerry Hanlon, George Mans, Tirrel Burton, Gary Moeller, Dick Hunter, Chuck Stobart, Jim Young, Larry Smith, Manager Neil Hiller, Head Trainer Lindsy McLean

5th Row: Tom Ferchau, John Pighee, Greg Ellis, Bob Mogulich, Tony Smith, Tom Poplawski, Mark Duffy, Bill Moran, Bill Haslett, Don Eaton, Carroll Damron, Bob Swan, Coach Bo Schembechler

4th Row: Bill Ross, Gary Coakley, Bob Rosema, Mike Smith, John Cilluffo, Randy Logan, Tom Kee, Bill Hart, Tom Coyle, Jack McBride, Jerry Schumacher, Jim Coode, Bo Rather, John Daniels

3rd Row: Frank Gusich, Bruce Elliott, Butch Carpenter, Tom Beckman, Mike Oldham, Reggie McKenzie, Fritz Seyferth, Dana Coin, Tom Huiskens, Jim Brandstatter, Dave Zuccarelli, Preston Henry, Paul Seymour, Scott Hulke

2nd Row: Greg Harrison, Bill Berutti, Ed Baldwin, Tom Nieman, Lance Scheffler, Jerry Dutcher, Fred Grambau, Tom Darden, Glenn Doughty, Guy Murdock, Mike Keller, Bill Taylor, Mike Taylor, John Wolff

Front Row: Marty Huff, Pete Newell, Ed Moore, Dan Dierdorf, Tim Killian, Jack Harpring, Co-captain Henry Hill, Co-captain Don Moorhead, Paul Staroba, Werner Hall, Dick McCoy, Bill Harris, Phil Seymour, Jim Betts.

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[L-R: tom Stiles, Todd Carlile, Pat Goff, Bill Brauer, John Bjorkman, Dan Carroll, Dan Goff]

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Federal Railroad Administration, Office of Research and Development, Washington, D.C.