Éditeur(s) : [S.l.] : L.G. Stahl
Siècle(s) traité(s) : 20
Droits : Domaine public
Provenance : Archives départementales de Guadeloupe
Permalien : http://www.manioc.org/patrimon/ADG18107
ADG18107

Éditeur(s) : Londres : John Stockolale
Siècle(s) traité(s) : 18
Droits : Domaine public
Provenance : Archives départementales de Guadeloupe
Permalien : http://www.manioc.org/patrimon/ADG17063
ADG17063

Éditeur(s) : London : Saunders and Otley
Description : History of the Caribs. Culture and way of life of Antiguans in the 18th and 19th Centuries.
Siècle(s) traité(s) : 18
Droits : Domaine public
Provenance : Ville de Pointe-à-Pitre. Réseau des bibliothèques
Permalien : http://www.manioc.org/patrimon/PAP11081
PAP11081

Éditeur(s) : HAL CCSD
Résumé : The strong earthquake (M = 6.3) occurred on 21st November 2004 in the DominicaPassage, between Guadeloupe and Dominica (Lesser Antilles), generated aweak tsunami with maximum amplitude 80 cm on neighbouring islands. Field surveyis conducted on November 27, 2004. Data of the field survey are described. Results ofthe numerical simulations in the framework of the shallow-water theory are in reasonableagreement with observed data.
European Geosciences Union - General Assembly 2005
Vienne, Austria

hal-00090423
https://hal.archives-ouvertes.fr/hal-00090423

Éditeur(s) : HAL CCSD The International Journal of the Tsunami Society
Résumé : http://library.lanl.gov/tsunami/231/pel.pdf
A strong earthquake (mb = 6.3; Ms = 6.1; Mw = 6.3) occurred on 21 November 2004 in the Dominica Passage separating Guadeloupe and Dominica, in the Lesser Antilles, and generated a weak tsunami with maximum amplitudes of +70 and -80 cm on neighbouring islands. We conducted field surveys on the islands of “Les Saintes”, in the immediate vicinity of the epicenter on November 27, 2004 and February 12, 2005, and report here on the resulting dataset.
ISSN: 8755-6839

hal-00095039
https://hal.archives-ouvertes.fr/hal-00095039

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : Coastal Quaternary deposits of western Oranie show typical soft-sediment deformations including sedimentary dykes, sand volcanoes, sismoslumps, thixotropic bowls, thixotropic wedges, diapir-like structures, and faults grading. Field observations indicate that these deformations exist at several levels of the studied deposits along the west Oranian coast. This study demonstrated that these structures are earthquakes-related, by analysis of potential trigger sources. Several arguments demonstrate the seismic origin: the depositional environment rich in water that located in an active tectonic region, the thixotropic nature of deformations and their large vertical and horizontal diffusion in the Quaternary series consistent with a seismic recurrence. This allows characterizing these Quaternary soft-sediment deformations as seismites that were triggered by earthquakes.
ISSN: 1383-4649

hal-01560975
https://hal.archives-ouvertes.fr/hal-01560975
DOI : 10.1007/s10950-016-9616-2