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of 24
pro vyhledávání: '"Walter S. Newman"'
Autor:
Walter S. Newman
Publikováno v:
Annals of the New York Academy of Sciences. 288:545-570
Publikováno v:
Radiocarbon. 26:412-430
The following list includes radiocarbon analyses of samples related to studies of Holocene sea levels completed since the publication of the last list (R, 1980, v 22, p 1073–1083). Sample preparation and counting for liquid scintillation samples re
Autor:
Walter S. Newman, Cecile Baeteman
Publikováno v:
Progress in Oceanography. 18:287-322
Computer-assisted analyses of more than 600 radiocarbon-dated sea-level indicators from northwestern Europe, concentrated around the North Sea margin, indicate that vertical crustal movements are more important that eustatic sea-level change in deter
Autor:
Rhodes W. Fairbridge, Walter S. Newman
Publikováno v:
Progress in Oceanography. 18:61-78
This proposal builds a high-speed inter-urban express between Jerusalem and Tel Aviv, generates 1500 megawatts of hydroelectric energy, curtails littoral erosion, builds a port along the Israeli Mediterranean coast and demands peaceful cooperation on
Publikováno v:
Marine Geology. 2:100-120
At least 500 sections of surface replicas prepared from 45 sand grains collected along the Atlantic shore of Long Island, New York, between Montauk Point and East Hampton were examined by electron microscopy at magnifications of about × 5,000. The s
Autor:
Craig A Munsart, Walter S. Newman
Publikováno v:
Marine Geology. 6:81-105
The Wachapreague lagoon and the barrier islands defending the lagoon have been in existence for at least 5,500 years. Submergence, continuing at a decreasing rate, has controlled the evolution of the barrier islands and lagoon during the last 4,400 y
Publikováno v:
Transactions of the New York Academy of Sciences. 31:548-570
Autor:
Bert Salwen, Walter S. Newman
Publikováno v:
American Antiquity. 43:313-315
Autor:
Walter S. Newman, Rhodes W. Fairbridge
Publikováno v:
Nature. 320:319-321
Man can regulate the hydrological cycle by diverting ocean-bound fresh water into reservoirs, subsurface storage and interior basins, and by diverting sea water into continental depressions. Between 1957 and 1982, human intervention stored as much as