{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,1,8]],"date-time":"2026-01-08T23:43:52Z","timestamp":1767915832565,"version":"3.49.0"},"reference-count":21,"publisher":"SAGE Publications","issue":"2","license":[{"start":{"date-parts":[[1995,6,1]],"date-time":"1995-06-01T00:00:00Z","timestamp":801964800000},"content-version":"tdm","delay-in-days":0,"URL":"https:\/\/journals.sagepub.com\/page\/policies\/text-and-data-mining-license"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["The Holocene"],"published-print":{"date-parts":[[1995,6]]},"abstract":"<jats:p> A description is given of a distinctive marine deposit at Boca do Rio on the Algarve coast of Portugal. It is proposed here that the sediment accumulation was deposited by the tsunami generated by the Lisbon earthquake of 1 November, AD 1755. The deposit exhibits sedimentary characteristics quite unlike other coastal sediment accumulations that are deposited by more moderate wave r\u00e9gimes. These include laterally continuous sand layers, chaotic pebble horizons, large amounts of gravel-sized shell debris and distinctive assemblages of marine microfossils. A preliminary attempt is made here to use the empirical field and laboratory data to define more clearly the processes of coastal sedimentation that characterize tsunami runup. The use of tsunami sediments as time synchronous marker horizons is also discussed. <\/jats:p>","DOI":"10.1177\/095968369500500208","type":"journal-article","created":{"date-parts":[[2007,11,26]],"date-time":"2007-11-26T22:55:20Z","timestamp":1196117720000},"page":"209-215","source":"Crossref","is-referenced-by-count":103,"title":["Tsunami sedimentation associated with the Lisbon earthquake of 1 November AD 1755: Boca do Rio, Algarve, Portugal"],"prefix":"10.1177","volume":"5","author":[{"given":"A.G.","family":"Dawson","sequence":"first","affiliation":[{"name":"Centre for Quaternary Science, Division of Geography, School of Natural and Environmental Sciences, Coventry University, Coventry CV1 5FB, UK"}]},{"given":"R.","family":"Hindson","sequence":"additional","affiliation":[{"name":"Centre for Quaternary Science, Division of Geography, School of Natural and Environmental Sciences, Coventry University, Coventry CV1 5FB, UK"}]},{"given":"C.","family":"Andrade","sequence":"additional","affiliation":[{"name":"Centro e Departamento de Geologia, Faculdade de Ci\u00eancias, Universidade de Lisboa, Edificio C2, Piso 5, Campo Grande, 1700 Lisboa, Portugal"}]},{"given":"C.","family":"Freitas","sequence":"additional","affiliation":[{"name":"Centro e Departamento de Geologia, Faculdade de Ci\u00eancias, Universidade de Lisboa, Edificio C2, Piso 5, Campo Grande, 1700 Lisboa, Portugal"}]},{"given":"R.","family":"Parish","sequence":"additional","affiliation":[{"name":"Geography Laboratory, University of Sussex, Falmer, Brighton BN1 9QN, UK"}]},{"given":"M.","family":"Bateman","sequence":"additional","affiliation":[{"name":"Geography Laboratory, University of Sussex, Falmer, Brighton BN1 9QN, UK"}]}],"member":"179","published-online":{"date-parts":[[1995,6,1]]},"reference":[{"key":"atypb1","first-page":"21","volume":"10","author":"Andrade, C.","year":"1992","journal-title":"Science of Tsunami Hazards"},{"key":"atypb2","doi-asserted-by":"publisher","DOI":"10.1016\/0040-1951(88)90031-5"},{"key":"atypb3","unstructured":"Cabral, J. 1993: Neotect\u00f3nica de Portugal Continental. 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