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  • B.P.) and, since about 6500 B.P., the present regressive Baltic Sea. (P. A. Pirazzoli).
  • transgressions (Littorina, reaching a maximum altitude of 11-12 m) can be identified. (P. A. Pirazzoli).
  • Synthèse sur les changements de l'environnement quaternaire sur la bordure californienne au cours des derniers 128 000 ans, avec quelques indications de présence humaine antérieurement à 8 000 ans B. P. (P. A. Pirazzoli).
  • Sea level has risen at least 5 m since 5000 B.C., when the population of this Neolithic village was forced to abandon the settlement due to rapid accumulation of sand. (P. A. Pirazzoli).
  • The Late Pleistocene and Holocene coastal deposits are interpreted according to the assumption that the bulk of the deposits on the coastal plain of Israel originated in the continental shelf. (P.A. Pirazzoli).
  • Submarine bogs and artifacts indicate that large submerged areas of the strait between the Island of Zealand (Denmark) and South Sweden were habitable and suitable for settlement by man during the Boreal period (7000-6000 B.C.). (P. A. Pirazzoli).
  • A computer-assisted analysis of 3,700 radiocarbon dates related to sea level shows that the shape of the earth has changed significantly through time. The lack of a stable datum prevents to measure absolute eustatic fluctuations. (P. A. Pirazzoli).
  • The Holocene warping of the continental shelf in central and northern Queensland is interpreted as due to differential hydro-isostatic effects, possibly enhanced by a regional tectonic downwarping of the Halifax basin. (P. A. Pirazzoli).
  • earliest and rebounded first. As deglaciation progressed, the zone of rapid isostatic uplift migrated and was accompanied by forebulge effects. (P. A. Pirazzoli).