Los recursos visuales en el ordenamiento territorial : I- Potrerillos (Mendoza, Argentina)

Se presenta la primera etapa del relevamiento de los recursos paisajísticos de la provincia de Mendoza, con el ajuste metodológico efectuado mediante una prueba piloto desarrollada sobre la Ruta Nac. N° 7, desde el Acceso sur en Luján de Cuyo (límite este) hasta Potrerillos inclusive (límite oeste). Los límites norte y sur están abarcados por el horizonte observable desde la ruta que atraviesa el área en sentido este-oeste. Se seleccionaron los puntos representativos mediante dos tipos de muestreo: sistemático y discrecional. En base a la catalogación de los recursos visuales se diseña una zonificación referencial general con miras al ordenamiento territorial y uso del suelo en distintas actividades de desarrollo futuro: turístico, reservas, residencial, agrícola, industrial. Se valora la calidad estética del paisaje aplicando, además, índices valorativos de la vulnerabilidad de los espacios a las actividades humanas (Índice de Naturalidad e Índice de Fragilidad), para obtener valores de la Calidad Visual Vulnerable del paisaje. Estos valores se grafican en planos que representan las distintas calidades alcanzadas y se complementa con una descripción de los puntos analizados, recomendaciones para el mejoramiento paisajístico a través de introducción o conducción de vegetación y fotografías documentales de las vistas analizadas.

Geochemical parameters of bottom sediments from the Stromboli Canyon

In recent sediments of the Stromboli Canyon sides features of mineral and grain size compositions, redox conditions, behavior of Fe, Mn, organic carbon, Mo, and W in an environment of active input of pyroclastic material are considered. Differences in conditions of sedimentation and early diagenesis in the east and west sides of the canyon depending on position of the prevailing direction of drift and steepness of the slopes, as well as types of differentiation of detrital material in sediments under conditions of permanent vibrations are specified.

Documentation of sediment cores from the Great Meteor Seamount, North Atlantic

Sedimentological and biostratigraphic investigations of 15 cores (total length: 88 m) from the vicinity of Great Meteor seamount (about 30° N, 28° W) showed that the calcareous ooze are asymmetrically distributed around the seamount and vertically differentiated into two intervals. East and west of the seampunt, the upper "A"-interval is characterized by yellowish-brown sediment colors and bioturbation; ash layers and diatoms are restricted to the eastern cores. On both seamount flanks, the sediment of the lower "B"-interval are white and very rich in CaCO3 with a major fine silt (2-16 µ) mode (mainly coccoliths). Lamination, manganese micronodules, Tertiary foraminifera and discoasters, and small limestone and basalt fragments are typical of the "B"-interval of the eastern cores only. The sediments contain abundant displaced material which was reworked from the upper parts of the seamount. The sedimentation around the seamount is strongly influenced by the kind of displaced material and the intensity of its differentiated dispersal: the sedimentation rates are generally higher on the east than on the west flank /e.g. in "B": 0.9 cm/1000 y in the W; 3.1 cm/1000 y in the E), and lower for the "A" than for the "B"-interval. The lamination is explained by the combination of increased sedimentation rates with a strong input of material poor in organic carbon producing a hostile environment for benthic life. The CaCO3 content of the core is highly influenced by the proportion of displaced bigenous carbonate material (mainly coccoliths). The genuine in-situ conditions of the dissolution facies are only reflected by the minimum CaCO3 values of the cores (CCD = about 5,500 m; first bend in dissolution curve = 4,000 m; ACD = about 3,400 m). The preservation of the total foraminiferal association depends on the proportions of in-situ versus displaced specimens. In greater water depths (stronger dissolution), for example, the preservation can be improved by the admixture of relatively well preserved displaced foraminifera. Carbonate cementation and the formation of manganese micronodules are restricted to microenvironments with locally increased organic carbon contents (e.g. pellets; foraminifera). The ash layers consist of redeposited, silicic volcanic glass of trachytic composition and Mio-Pliocene age; possibly, they can be derived from the upper part of the seamount. Siliceous organisms, especially diatoms, are frequent close to the ash layers and probably also redeposited. Their preservation was favoured by the increase of the SiO2 content in the pore water caused by the silicic volcanic glass. The cores were biostraftsraphically subdivided with the aid of planktonic foraminifera and partly alsococcoliths. In most cases, the biostratigraphically determined cold- and warm sections could be correlated from core to core. Almost all cores do not penetrate the Late Pleistocene. All Tertiary fossils are reworked. In general, the warm/cold boundary W2/C2 corresponds with the lithostratigraphic A/B boundray. Benthonic foraminifera indicate the original site deposition of the displaced material (summit plateau or flanks of the seamount). The asymmetric distribution of the sediments around the seamount east and west of the NE-directed antarctic bottom current (AABW) is explained by the distortion of the streamlines by the Coriolis force; by this process the current velocity is increased west of the seamount and decreased east of it. The different proportion of displaced material within the "A" and "B" interval is explained by changes of the intensity of the oceanic circulation. At the time of "B" the flow of the AABW around the seamount was stronger than during "A"; this can be inferred from the presence of characteristic benthonic foraminifera. The increased oceanic circulation implies an enhanced differentiation of the current velocities, and by that, also of the sedimentation rates, and intensifies the winnowed sediment material was transported downslope by turbid layers into the deep-sea, incorporated into the current system of the AABW, and asymmetrically deposited around the seamount.

AIDS NA REDE: UMA ABORDAGEM COMUNICACIONAL

O presente trabalho tem como objetivo geral investigar se um grupo de universitários da cidade de São Paulo tem comportamento sexual de risco em relação ao HIV, qual é o conhecimento que o grupo tem sobre HIV/AIDS e quais são as suas dúvidas mais freqüentes sobre o assunto. Além disso, tem como objetivo específico averiguar se o grupo usa a Internet para esclarecer suas dúvidas, quais as estratégias de busca utiliza e se considera que a informação obtida é confiável. Trata-se, portanto, de uma pesquisa exploratória e descritiva, de caráter qualitativo. Como instrumento de campo, construímos um questionário digital de coleta de dados, aplicado pela pesquisadora, usando um computador portátil tipo notebook a 400 estudantes na entrada de quatro unidades de ensino superior da cidade de São Paulo, sendo 100 informantes em cada uma e sendo cada unidade em uma região: Norte, Sul, Leste e Oeste. Além disso, temos ainda o Termo de Consentimento Livre e Esclarecido TCLEconforme determina a Resolução do Conselho Nacional de Saúde CNS 196/96. Para processar e analisar os dados e proceder ao cruzamento das variáveis foram usados procedimentos quantitativos. Para contextualizar nosso objeto, lançou-se um olhar sobre o panorama histórico da Comunicação e Saúde que se articula com a orientação metodológica da pesquisa bibliográfica e documental.

AIDS NA REDE: UMA ABORDAGEM COMUNICACIONAL

O presente trabalho tem como objetivo geral investigar se um grupo de universitários da cidade de São Paulo tem comportamento sexual de risco em relação ao HIV, qual é o conhecimento que o grupo tem sobre HIV/AIDS e quais são as suas dúvidas mais freqüentes sobre o assunto. Além disso, tem como objetivo específico averiguar se o grupo usa a Internet para esclarecer suas dúvidas, quais as estratégias de busca utiliza e se considera que a informação obtida é confiável. Trata-se, portanto, de uma pesquisa exploratória e descritiva, de caráter qualitativo. Como instrumento de campo, construímos um questionário digital de coleta de dados, aplicado pela pesquisadora, usando um computador portátil tipo notebook a 400 estudantes na entrada de quatro unidades de ensino superior da cidade de São Paulo, sendo 100 informantes em cada uma e sendo cada unidade em uma região: Norte, Sul, Leste e Oeste. Além disso, temos ainda o Termo de Consentimento Livre e Esclarecido TCLEconforme determina a Resolução do Conselho Nacional de Saúde CNS 196/96. Para processar e analisar os dados e proceder ao cruzamento das variáveis foram usados procedimentos quantitativos. Para contextualizar nosso objeto, lançou-se um olhar sobre o panorama histórico da Comunicação e Saúde que se articula com a orientação metodológica da pesquisa bibliográfica e documental.

London, England, 1822 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: A new map of London and its environs : from an original survey extending 8 miles east and west, 6 1/4 miles north & south, in which all new and intended buildings, improvements, &c. are carefully inserted, drawn by Mr. Thompson. It was published by Reeves & Hoare May 5, 1822. Scale [ca. 1:17,150]. The image inside the map neatline is georeferenced to the surface of the earth and fit to the British National Grid coordinate system (British National Grid, Airy Spheroid OSGB (1936) Datum). 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, selected buildings, built-up areas, parks, docks, city and borough boundaries, and more. Relief is shown by hachures. Includes "Explanation of Colours". 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.

Radiocarbon ages from Novaya Zemlya, Russia

Recent observations on postglacial emergence and past glacier extent for one of the least accessible areas in the Arctic, northern Novaya Zemlya are here united. The postglacial marine limit formed 5 to 6 ka is registered on the east and west coasts of the north island at 10 ± 1 and 18 ± 2 m aht, respectively. This modest and late isostatic response along with deglacial ages of >9.2 ka on adjacent marine cores from the northern Barents Sea indicate either early (>13 ka) deglaciation or modest ice sheet loading (<1500 m thick ice sheet) of Novaya Zemlya. Older and higher (up to 50 m aht) raised beaches were identified beneath a discontinuous glacial drift. Shells from the drift and underlying sublittoral sediments yield minimum limiting 14C ages of 26 to 30 ka on an earlier deglacial event(s). The only moraines identified are within 4 km of present glacier margins and reflect at least three neoglacial advances in the past 2.4 ka.

Hekija shōgen.

Mode of access: Internet.

John Strange Winter; a volume of personal record,

Mode of access: Internet.

Tōzai bunmei no chōwa /

Mode of access: Internet.

The bread of the eucharist,

The uses of the church before the schism of East and West.--The controversy between East and West.--England.--The Eastern churches (with certain documents)

Letters from a Chinese official : being an Eastern view of Western civilization.

Originally published in 1901 under title: Letters from John Chinaman.

Rackham Blg. [Building] construction

View toward north. Scaffolding in place on both east and west ends of building. Stonework on second floor near completion. No. 26 of chronological series of construction photographs, numbered 1 to 32. Smith, Hinchman & Grylls, architects. W.B. Wood Co., construction

Central Campus, University of Michigan

An aerial panorama of the buildings of the Central Campus area shows Burton Tower, Rackham Graduate School, East and West Engineering, the Cook Law Quadrangle, Harlan Hatcher Graduate Library and many other buildings.