942 resultados para Moore, William, fl. 1662-1663.
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Mode of access: Internet.
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"April 1981."
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Mode of access: Internet.
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Advertisements: [4] p. at end.
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With reproduction of original t.p., dated 1600.
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Translation of two memoirs: Anatomisch physiologisch onderzoek over het fijnere zamenstel en de werking van het ruggemerg, published 1854, and Over het fijnere zamenstel en de werking van het verlangde ruggemerg en over de naaste oorzaak van epilepsie en hare rationele behandeling, published 1858.
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Mode of access: Internet.
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Mode of access: Internet.
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1879
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Mode of access: Internet.
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Mode of access: Internet.
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Indenture stating that David Secord of St. Davids, leased the sawmill water in St. Davids to Stroughton Moore of St. Davids for 50 pounds a year. This document was witnessed by Ezekiel and William Woodruff, July 22, 1824.
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In order to determine geochemical compositions of Late Cenozoic Arctic seawater, oxide fractions were chemically separated from 15 samples of hand-picked ferromanganese micronodules (50-300 mu m). The success of the chemical separation is indicated by the fact that >97% of the Sr in the oxide fraction is seawater-derived. Rare-earth element (REE) abundances of the Arctic micronodule oxide fractions are much lower than those of bulk Fe-Mn nodules from other ocean basins of the world (e.g., 33 vs. 145 ppm Nd), but the Arctic oxides are enriched in Ce relative to Nd (Ce-N/Nd-N=2.2+/-0.5) and have convex-upward, shale-normalized REE patterns (Nd-N/Gd-N=0.61+/-0.06, Gd-N/Yb-N = 1.5+/-0.2, Nd-N/Yb-N = 0.9+/-0.2), typical of other hydrogenous and diagenetic marine Fe-Mn-oxides. Bulk sediment samples from the central Arctic Ocean have REE abundances and patterns that are characteristic of those of post-Archean shale. Non-detrital fractions (calcite + oxide coatings) of Recent Arctic foraminifera have REE abundances and patterns similar to those of Recent foraminifera from the Atlantic Ocean. Electron microprobe analyses (n=178) of transition elements in 29 Arctic Fe-Mn micronodules from five different stratigraphic intervals of Late Cenozoic sediment indicate that oxide accretion occurred as a result of hydrogenetic and diagenetic processes close to the sediment-seawater interface. Transition element ratios suggest that no oxide accretion occurred during transitions from oxic to suboxic diagenetic conditions. Only K is correlated with Si and Al, and ratios of these elements suggest that they are associated with illite or phillipsite. Ca and Mg are correlated with Mn, which indicates variable substitution of these elements from seawater into the manganate phase. The geochemical characteristics of Arctic Fe-Mn micronodules indicate that the REEs of the oxide fractions were ultimately derived from seawater. However, because of minute contributions of Sr from siliciclastic detritus during diagenesis or during the chemical leaching procedure, Sr isotope compositions of the oxide fractions cannot be used to trace temporal changes in the Sr-87/Sr-86 ratio of Arctic seawater or to improve the chronostratigraphy.
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Two octavo-sized leaves containing a two-and-a-half-page handwritten letter from Winthrop to Bentley discussing Alexander Pope and mythology, and a brief criticism of John Moore's A view of society and manners.
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Two octavo-sized leaves with a two-and-a-half-page handwritten letter from William Winthrop to Bentley responding to a request to return a book, speculating about the identity of Harvard graduate Peter Cutler (Harvard AB 1698), and questioning Bentley about the interests of "F. Moore," likely referring to Francis Moore (1782-1856).