Geoid change indications along the Brazilian coast during the last 7,000 years in Proceedings. Volume 3. Symposia and seminars.
Differences between Holocene sea-level curves obtained in several coastal sectors are ascribed to recent changes in the geoid shape. In the State of Bahia, where the coastline is parallel to the isobases of present geoidal height, no shift can
symposium on Late Quaternary sea-level changes and coastal evolution. Mar del Plata, 30 September-3 October 1984.
Wave-induced longshore currents and sea level changes during the last 7 000 years played an important role in the construction of the Quaternary coastal plains adjacent to the present Paraiba do Sul river mouth. The river acted as a hydraulic groin