984 resultados para Moore, John, Sir, 1761-1809.


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This is a contract signed between Loammi Baldwin, acting on behalf of the President and Fellows of Harvard College, and Josiah Moore, John Walton, Thomas Mason, Samuel Mason, and Joseph Holmes for completing the dining rooms and chapel of University Hall. The agreement was witnessed by Abraham Edwards and Thomas Edwards.

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Small pen-and-ink and watercolor drawing of Cambridge Green created by Harvard senior John Davis, presumably as part of his undergraduate mathematical coursework. The map surveys Cambridge Commons and includes a few rough outlines of College buildings and the Episcopal church, and notes the burying ground, and the roads to Charlestown, Menotomy, the pond, Watertown, and the bridge. The original handwritten text is faded and was annotated with additional text by Davis including the note "[taken in my Senior year at H. College Septr 1780] Surveyed in concert with classmates, Atkins, Hall 1st, Howard, Payne, &c.- J. Davis." There is a note that "Atkins afterwards took the name of Tying." Davis refers to Dudley Atkins Tyng, Joseph Hall, Bezaleel Howard, and Elijah Paine, all members of the Harvard Class of 1781.

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Copy of the proceedings in the case of Benjamin Tanner vs. Jasper Hall of Kingston (Jamaica), relating to various lands, etc. With the autographs of Henry Moore, governor, and John Arnold, registrar of the high court.

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We analyse ice cores from Vestfonna ice cap (Nordaustlandet, Svalbard). Oxygen isotopic measurements were made on three firn cores (6.0, 11.0 and 15.5 m deep) from the two highest summits of the glacier located on the SW-NE and NW-SE central ridges. Sub-annual d18O cycles were preserved and could be counted visually in the uppermost parts of the cores, but deeper layers were affected by post-depositional smoothing. A pronounced d18O minimum was found near the bottom of the three cores. We consider candidates for this d18O signal to be a valuable reference horizon since it is also seen elsewhere in Nordaustlandet. We attribute it to isotopically depleted snow precipitation, which NCEP/NCAR reanalysis shows was unusual for Vestfonna, and came from northerly air during the cold winter of 1994/95. Finding the 1994/95 time marker allows establishment of a precise depth/age scale for the three cores. The derived annual accumulation rates indirectly fill a geographical gap in mass balance measurements and thus provide information on spatial and temporal variability of precipitation over the glacier for the period spanned by the cores (1992-2009). Comparing records at the two locations also reveals that the snow net accumulation at the easternmost part of Vestfonna was only half of that in the western part over the last 17 years.

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Mode of access: Internet.

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Mode of access: Internet.

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Mode of access: Internet.

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Errata slip inserted.

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Contains arrangements of songs, selections from operas, dances, etc.

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Each volume has special t.-p.

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Item 851-J-3

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Bibliographical footnotes.