937 resultados para Moore, George, 1852-1933.


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Mode of access: Internet.

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From the "Journal of the Academy of natural sciences of Philadelphia."

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"The poems of Moore have been printed according to the edition collected by himself."

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back row: manager Ernest Freeman, John Laun, Leo Gerber, Markham Coventry, William Williams, Avon Artz, ass't trainer John Brozovitch

front row: John Jewell, Harvey Chapman, Emerson Reid, coach J. Edward Lowrey, Keith Crossman, George David, John Sherf

not pictured, Cornelius Gabler

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Standing: coach Thomas Trueblood, Edwin Dayton, Lawrence Markham, John Fischer, coach Ray Courtright

Seated: Caroll F. Sweet, Alexander Jolly, George David

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Back Row: Herman Everhardus, Sylvester Shea, ? Rygg, Willis Ward, Tom Austin, Chuck Bernard, Francis Wistert, Donald McGuire, Harvey Chapman, Willard Hildebrand, John Viergiver, Russell Fuog, Wallace Frankowski, Fred Petoskey, Roy Semeyn, Robert Swanson, Gerald Ford

Middle Row: captain Stan Fay, William Renner, Henry Raymond, Hilton Ponto, Robert Wells, James Kidston, John Kowalik, Russ Oliver, Oscar Singer, Carl Savage, Chester Beard, John Regeczi, Herbert Schmidt, William Borgmann, Steve Remias

Front Row: George Rudness, Estel Tessmer, Lee Shaw, Louis Westover, Arthur Patchin, Lawrence Ratterman, Richard James, David Hunn, Eli Soodik, George Bolas, Antone Dauksza, Winfred Nelson, Herbert Paulson, Howard Triplehorn, D. King Lewis, ? Hall

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Publisher's catalog at end (16 p.)

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Includes index.

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"List of subscribers" ([15] p.) inserted between p. [iv] and v.

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New surveys were completed and data from the field sheets were kindly furnished by the U. S. Coast and Geodetic Survey to the Woods Hole Oceanographic Institution for use in dredging and coring operations. This field work, first reported in 1936, was continued from time to time until 1941 as new soundings became available. Rock dredging and coring has been carried out in every major canyon on the slope from Corsair Canyon at the tip of Georges Bank to Norfolk Canyon off the entrance to the Chesapeake. Numerous cores have also been taken from the areas in between; and while the whole slope from Georges to the Chesapeake has not been covered, it is believed that no significant areas have been missed. In the following report the tows and cores will be described by areas from Georges Bank southwards, as the same region was revisited in successive years. The various samples, however, will be referred to by number followed by the year in which they were taken. The material is in storage in the Woods Hole Oceanographic Institution and in the Museum of Comparative Zoology at Harvard University.

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Ferromanganese micronodules have been found on Georges Bank, off the U.S. northeast coast, distributed throughout the surficial sediments within an area about 125 km long and at least 12 km wide. These coarse, sand-sized concretions have precipitated from metal-rich interstitial waters and contain many of the textural and structural features common to other neritic nodules. Most of the nodules have accreted around detrital grains, and X-ray powder diffraction analyses indicate the presence of geothite and vernadite ( delta -MnO sub(2)) in the ferromanganese layers. Chemical analyses of the micronodules, when compared with similar data on deep-sea manganese nodules, reveal lower Mn/Fe ratios, significantly higher concentrations of V and As, comparable values of Mo, and an order of magnitude less of Co, Ni, Ce and most other, metals.

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Concentrations of tin in sea water decreased from estuarine and shelf (0.02-0.04 µg/kg) to surface Atlantic waters (0.009 µg/kg). Mean contents (ppm) in other materials included: ultramafic rocks, 0.8; basalts, 1.7; silicic rocks, 2.5; red clays, 3.4; amphibolites, 1.2. Oceanic ferromanganese deposits contained from 0.2 to 5.8 ppm; tin and cobalt contents were correlated.