908 resultados para Boy scouts.


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Almanac containing a laid-in leaf and calendar pages with sporadic annotations of measurements, a note of the printer's markings on Winthrop and his wife's watches (January). The laid-in leaf includes personal entries about a measles outbreak (January), the death of his "negro man George" (May 13), the presence of bears in the area (September), the surrender of Quebec (October 16), the heights of Winthrop's son Jemmy and a "new negro boy" named Scipio, and deaths in the community including the burial and baptism statistics for Boston.

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In this deposition, Eliot describes Prince's anger at John Winthrop's selection as Hollis Professor of Mathematics and Natural Philosophy, which he believed was done "to vex and torture" him. Eliot claims that Prince said: "they have chosen that Boy Winthrop professor, I could teach him his A. B. C. in the Mathematicks, they want to get me away from College."

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The collection holds a heavily interleaved 1791 Triennial Catalogue annotated, in part, by Jeremy Belknap. A note by Harvard Librarian John Langdon Sibley, on the verso of the flyleaf, indicates a second annotator: "It should be observed that this catalogue is in the handwriting of two persons, Dr. Belknap & probably interlineations & additions by Rev. Dr. [John] Eliot. The interlineing part should not be too confidently relied on for accuracy. J. L. Sibley, April 14, 1848." The volume contains biographical notes, newspaper clippings, excerpts from manuscript and printed sources such as New England's First Fruits, the manuscript memoirs of Charles Chauncey, and John Winthrop's Journal, and a 1795 letter from Isaac Mansfield. In the letter, Mansfield references an item he believed to be written by his grandfather, Ames Cheever (Harvard AB 1707), and briefly describes his grandfather. A list of election sermon orators with dates is also pasted into the inside back cover, along with an obituary of the Rev. John Wales (Harvard AB 1728) from the Boston Post-Boy, March 4, 1765.

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Two account books containing entries noting patients visited, fees charged, and small accounts of Dr. William Aspinwall (1743-1823) in Boston and Brookline, Massachusetts, from 1776 to 1812. He includes sections for "Women's Accounts" with charges generally rendered to their husbands or other male relatives. There is also an entry charging the town of Cambridge, Massachusetts, four dollars and fifty cents for medicines and attendance to a boy who contracted smallpox.

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‘A bizarre phenomenon,’ Der Spiegel concluded, after trying to figure out why youngsters left Germany to become foreign fighters in Syria. The magazine painted a portrait of two thirty-somethings with similar background and the same hobby – martial arts. One became director of a martial arts school in Hamburg, the other became a terrorist poster boy in Syria.1

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‘A bizarre phenomenon,’ Der Spiegel concluded, after trying to figure out why young people left Germany to become foreign fighters in Syria. The magazine painted a portrait of two thirty-somethings with similar backgrounds and the same hobby – martial arts. One became director of a martial arts school in Hamburg, the other became a terrorist poster boy in Syria.2

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‘A bizarre phenomenon,’ Der Spiegel concluded, after trying to figure out why young people left Germany to become foreign fighters in Syria. The magazine painted a portrait of two thirty-somethings with similar backgrounds and the same hobby – martial arts. One became director of a martial arts school in Hamburg, the other became a terrorist poster boy in Syria.2

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Desde la perspectiva de la genética textual, en este trabajo observamos las representacionesdel personaje de Peter Pan en los textos de J. M. Barrie dedicados a este con respecto a sussemejanzas con el dios griego Pan, para ver de qué manera dialogan con los diferentes sentidosque el dios fue connotando a través de siglos. Analizamos la fotonovela The Boys Castawaysof Black Lake Island (1901); The Little White Bird (1902), novela en la que aparece en seiscapítulos; las "Fairy Notes" (1903) en borrador y el libreto inédito llamado Anon: a play de la obra teatral Peter Pan or The Boy Who Would Not Grow Up (estrenada en 1904); la novela Peter Pan in Kensington Gardens (1906), que consiste en esos seis capítulos de The LittleWhite Bird; la novela Peter and Wendy (1911), adaptación de la obra de teatro; un guion cinematográfico,Scenario for a Proposed Film of Peter Pan (c. 1918), que no se filmó; y ellibreto de la obra, finalmente publicado, con bastantes cambios, en 1928

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Desde la perspectiva de la genética textual, en este trabajo observamos las representacionesdel personaje de Peter Pan en los textos de J. M. Barrie dedicados a este con respecto a sussemejanzas con el dios griego Pan, para ver de qué manera dialogan con los diferentes sentidosque el dios fue connotando a través de siglos. Analizamos la fotonovela The Boys Castawaysof Black Lake Island (1901); The Little White Bird (1902), novela en la que aparece en seiscapítulos; las "Fairy Notes" (1903) en borrador y el libreto inédito llamado Anon: a play de la obra teatral Peter Pan or The Boy Who Would Not Grow Up (estrenada en 1904); la novela Peter Pan in Kensington Gardens (1906), que consiste en esos seis capítulos de The LittleWhite Bird; la novela Peter and Wendy (1911), adaptación de la obra de teatro; un guion cinematográfico,Scenario for a Proposed Film of Peter Pan (c. 1918), que no se filmó; y ellibreto de la obra, finalmente publicado, con bastantes cambios, en 1928

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The speciation of strongly chelated iron during the 22-day course of an iron enrichment experiment in the Atlantic sector of the Southern Ocean deviates strongly from ambient natural waters. Three iron additions (ferrous sulfate solution) were conducted, resulting in elevated dissolved iron concentrations (Nishioka, J., Takeda, S., de Baar, H.J.W., Croot, P.L., Boye, M., Laan, P., Timmermans, K.R., 2005, Changes in the concentration of iron in different size fractions during an iron enrichment experiment in the open Southern Ocean. Marine Chemistry, doi:10.1016/j.marchem.2004.06.040) and significant Fe(II) levels (Croot, P.L., Laan, P., Nishioka, J., Strass, V., Cisewski, B., Boye, M., Timmermans, K.R., Bellerby, R.G., Goldson, L., Nightingale, P., de Baar, H.J.W., 2005, Spatial and Temporal distribution of Fe(II) and H2O2 during EisenEx, an open ocean mescoscale iron enrichment. Marine Chemistry, doi:10.1016/j.marchem.2004.06.041). Repeated vertical profiles for dissolved (filtrate < 0.2 µm) Fe(III)-binding ligands indicated a production of chelators in the upper water column induced by iron fertilizations. Abiotic processes (chemical reactions) and an inductive biologically mediated mechanism were the likely sources of the dissolved ligands which existed either as inorganic amorphous phases and/or as strong organic chelators. Discrete analysis on ultra-filtered samples (< 200 kDa) suggested that the produced ligands would be principally colloidal in size (> 200 kDa-< 0.2 µm), as opposed to the soluble fraction (< 200 kDa) which dominated prior to the iron infusions. Yet these colloidal ligands would exist in a more transient nature than soluble ligands which may have a longer residence time. The production of dissolved Fe-chelators was generally smaller than the overall increase in dissolved iron in the surface infused mixed layer, leaving a fraction (about 13-40%) of dissolved Fe not bound by these dissolved Fe-chelators. It is suggested that this fraction would be inorganic colloids. The unexpected persistence of such high inorganic colloids concentrations above inorganic Fe-solubility limits illustrates the peculiar features of the chemical iron cycling in these waters. Obviously, the artificial about hundred-fold increase of overall Fe levels by addition of dissolved inorganic Fe(II) ions yields a major disruption of the natural physical-chemical abundances and reactivity of Fe in seawater. Hence the ensuing responses of the plankton ecosystem, while in itself significant, are not necessarily representative for a natural enrichment, for example by dry or wet deposition of aeolian dust. Ultimately, the temporal changes of the Fe(III)-binding ligand and iron concentrations were dominated by the mixing events that occurred during EISENEX, with storms leading to more than an order of magnitude dilution of the dissolved ligands and iron concentrations. This had strongest impact on the colloidal size class (> 200 kDa-< 0.2 µm) where a dramatic decrease of both the colloidal ligand and the colloidal iron levels (Nishioka, J., Takeda, S., de Baar, H.J.W., Croot, P.L., Boye, M., Laan, P., Timmermans, K.R., 2005, Changes in the concentration of iron in different size fractions during an iron enrichment experiment in the open Southern Ocean. Marine Chemistry, doi:10.1016/j.marchem.2004.06.040) was observed.

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Measurements of Fe(II) and H2O2 were carried out in the Atlantic sector of the Southern Ocean during EisenEx, an iron enrichment experiment. Iron was added on three separate occasions, approximately every 8 days, as a ferrous sulfate (FeSO4) solution. Vertical profiles of Fe(II) showed maxima consistent with the plume of the iron infusion. While H2O2 profiles revealed a corresponding minima showing the effect of oxidation of Fe(II) by H2O2, observations showed detectable Fe(II) concentrations existed for up to 8 days after an iron infusion. H2O2 concentrations increased at the depth of the chlorophyll maximum when iron concentrations returned to pre-infusion concentrations (<80 pM) possibly due to biological production related to iron reductase activity. In this work, Fe(II) and dissolved iron were used as tracers themselves for subsequent iron infusions when no further SF6 was added. EisenEx was subject to periods of weak and strong mixing. Slow mixing after the second infusion allowed significant concentrations of Fe(II) and Fe to exist for several days. During this time, dissolved and total iron in the infusion plume behaved almost conservatively as it was trapped between a relict mixed layer and a new rain-induced mixed layer. Using dissolved iron, a value for the vertical diffusion coefficient Kz=6.7±0.7 cm**2/s was obtained for this 2-day period. During a subsequent surface survey of the iron-enriched patch, elevated levels of Fe(II) were found in surface waters presumably from Fe(II) dissolved in the rainwater that was falling at this time. Model results suggest that the reaction between uncomplexed Fe(III) and O2? was a significant source of Fe(II) during EisenEx and helped to maintain high levels of Fe(II) in the water column. This phenomenon may occur in iron enrichment experiments when two conditions are met: (i) When Fe is added to a system already saturated with regard to organic complexation and (ii) when mixing processes are slow, thereby reducing the dispersion of iron into under-saturated waters.

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Top Row: Chuck Rogers, Brian Balaze, Pat Sullivan, Ace Adams, Mike DeCou, Bill Meyer

Middle Row: Mark Weber, John Lieneck, Reggie Ball, Dan Damiani, Dick Walterhouse, Tom Kettinger, Jim Kocoloski, bat boy Jones

Front Row: Mark Crane, Pete Ross, Chris Burak, John Lonchar, Craig Forhan, Pete Helt, Tom Joyce, coach Moby Benedict

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Ill. on lining paper.

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"AEC Category: Nuclear explosions - peaceful applications; Military distribution category 14."

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Mode of access: Internet.