978 resultados para Oriskany, Battle of, N.Y., 1777.


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Later edition published in 1853 under title: The days of battle.

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Appendix: A. The fragment of this work preserved in the Book of Leinster. B. Chronology and genealogy of the kings of Munster and of Ireland, during the period of Scandinavian invasions. C. Maelseachlainn's description of the battle of Clontarf, from the Brussels ms. D. Genealogy of the Scandinavian chieftains named as leaders of the invasions of Ireland.

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Mode of access: Internet.

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title varies slightly

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Included in v. 2: Findings of the court, and opinion of Admiral Dewey; Rear-Admiral Schley's "Petition for relief from the findings and report of a court of inquiry, and accompanying papers"; The President's memorandum upon the appeal of Admiral Schley; Appendix, containing logs of the battle-ships, signals, etc.; Index prepared in the Office of the Superintendent of Documents.

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Contains New York at Gettysburg, by William F. Fox ; Dedication of the monuments erected in honor of the New York regiments at Gettysburg. Orations, addresses and regimental histories. Ed. by William F. Fox. Location, dimensions, construction and cost of each of the New York monuments at Gettysburg.

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En 1988, fue publicado por Siglo XXI México Filosofía y marxismo, un pequeño libro de entrevistas al filósofo marxista francés Louis Althusser realizadas por la profesora de filosofía mexicana Fernanda Navarro. En dicho volumen, Althusser retomaba varios de los aspectos fundamentales que habían caracterizado su intervención durante las décadas de 1960 y 1970 e introducía elementos absolutamente novedosos como las formulaciones alrededor del materialismo aleatorio y la filosofía del encuentro. La correspondencia mantenida entre Althusser y Navarro entre la entrevista de 1984 y la publicación de Filosofía y marxismo en 1988, habilita un horizonte interpretativo que permite integrar el vínculo establecido entre ambos filósofos en el marco más general del itinerario teórico-político de Althusser en Francia y de las proyecciones del althusserianismo hacia América Latina. Veremos de qué manera aquel encuentro entre Althusser y Navarro estuvo originado en un intercambio epistolar previo entre el filósofo francés y Mauricio Malamud, un comunista argentino difusor de la obra de Althusser en Argentina y por entonces exiliado en Morelia. Asimismo, la correspondencia entre Althusser y Navarro nos permite ver que el hecho de que el libro haya sido publicado únicamente en América Latina fue resultado de un interés específico de Althusser en los procesos políticos latinoamericanos. Finalmente, el intercambio permite captar el tenor filosófico del mencionado libro en el marco más general de la especificidad de la intervención althusseriana

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The phenomenon of B6-Y-DOM sex reversal arises when certain variants of the Mus domesticus Y chromosome are crossed onto the genetic background of the C57BL/6J (136) inbred mouse strain, which normally carries a Mus musculus-derived Y chromosome. While the sex reversal has been assumed to involve strain-specific variations in structure or expression of Sry, the actual cause has not been identified. Here we used in situ hybridization to study expression of Sry, and the critical downstream gene Sox9, in strains containing different chromosome combinations to investigate the cause of B6-Y-DOM sex reversal. Our findings establish that a delay of expression of Sry(DOM) relative to Sry(B6) underlies B6-Y-DOM sex reversal and provide the first molecular confirmation that Sry must act during a critical time window to appropriately activate Sox9 and effect male testis determination before the onset of the ovarian-determining pathway. (C) 2004 Elsevier Inc. All rights reserved.

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Shale-normalised rare earth element and yttrium (REE + Y) patterns for siderite-jasper couples in a banded iron formation of the 3.45 Ga Panorama Formation, Warrawoona Group, eastern Pilbara Craton, display distinct positive Y and Eu anomalies and weak positive La and Gd anomalies, combined with depleted light REE relative to middle and heavy REE. Ambient seawater and hydrothermal fluids are identified as major sources of REE + Y for the BIF. In the case of siderites, strong correlations between incompatible trace elements and trace element ratios diagnostic of seawater indicate variable input from a terrigenous source (e.g. volcanic ash). We propose a volcanic caldera setting as a likely depositional environment where jasper and siderite precipitated as alternating bands in response to episodic changes in ambient water chemistry. The episodicity was either driven by fluctuations in the intensity of hydrothermal activity or changes in magma chamber activity, which in turn controlled relative sea level. In this context, precipitation of jasper probably reflects background conditions during which seawater was saturated in silica due to evaporative conditions, while siderites were deposited most likely during intermittent periods of enhanced volcanic activity when seawater was more acidic due to the release of exhalative phases (e.g. CO2). © 2005 Elsevier B.V. All rights reserved.

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A conexão que se estabelece entre a publicidade veiculada na mídia impressa revista e os jovens da chamada Geração Y é o principal foco deste trabalho. Estes jovens, nascidos entre 1980 e meados da década de 90, no século XX, se desenvolveram juntamente com as novas tecnologias da comunicação, cresceram com um computador ligado ao mundo pela internet, com o telefone celular e jogos interativos, mas continuam sendo assediados pelas revistas. Com o objetivo de conhecer melhor esta conexão, saber como a Geração Y se comporta diante das mensagens publicitárias e verificar se existe um padrão de consumo entre estes jovens foram realizadas investigações exploratórias em fontes primárias e secundárias complementada por um estudo conclusivo descritivo. Depois de uma revisão da literatura que trata dos conceitos de geração até o perfil da Geração Y, e de uma análise histórica da mídia revista, a realização de pesquisas aplicadas em forma de grupos focais e de um estudo descritivo, nos permitiu concluir que existe uma sobrevida para a mídia impressa revista, e ainda por muito tempo. Aspectos como a tangibilidade, portabilidade e a tradição são os pilares que garantem às revistas uma sólida confiabilidade por parte dos jovens da Geração Y, sobrepondo-se à mídia eletrônica, volátil e pouco confiável para eles.

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Mineralogical investigations have determined the sites of u and Th associated with two radioelement-enriched granites from different geological settings. In the Ririwai ring complex, Nigeria, the u- and Th-bearing accessories have been greatly affected by post-magmatic alteration of the biotite granite. Primary thorite, zircon and monazite were altered to Zr(±Y)-rich thorite, partially metamict zircon (enriched in Th, U, Y, P, Fe, Mn, Ca) and an unidentified LREE-phase respectively, by pervasive fluids which later precipitated Zr-rich coffinite. More intense, localised alteration and albitisation completely remobilised primary accessories and gave rise to a distinctive generation of haematite- and uranothorite-enriched zircon with clear, Hi-enriched rims and xenotime overgrowths. In the Ririwai lode, microclinisation and later greisenisation locally remobilised or altered zircon and deposited Y-ricl1 coffinite and Y(±Zr)-rich thorite which was overgrown by traces of xenotime and LREE-phase(s) of complex and variable composition. Compositions indicating extensive solid-solution among thorite, coffinite, xenotime and altered zircon are probably metastable and formed at low temperatures. The widespread occurrence of REE-rich fluorite suggests that F-complexing aided the mobility of REE, Y, U, Th and Zr during late-magmatic to post-magmatic alteration, while uranyl-carbonate complexing may have occurred during albitisation. The Caledonian, Helmsdale granite in northern Scotland has undergone pervasive and localised hydrothermal alteration associated with U enrichment. Zircon xenocrysts, primary sphene and apatite contain a small.proportion of this U which is largely adsorbed on to secondary iron-oxide, TiOand phyllosilicates.Additional sites for U in the overlying, Lower Devonian Ousdale arkose include coffinite, secondary uranyl phosphates, hydrocarbon and traces of xenotime and unidentified LREE-phases. U may have been leached from the granite and deposited in the arkose, along channelways associated with the Helmsdale fault, by convecting, hydrothermal fluids

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2000 Mathematics Subject Classification: 60J80.