A splash in Earth gravity from the 2004 Sumatra Earthquake

Eos ◽  
2005 ◽  
Vol 86 (15) ◽  
pp. 149 ◽  
Author(s):  
Roberto Sabadini ◽  
Giorgio Dalla Via ◽  
Masja Hoogland ◽  
Abdelkrim Aoudia
2008 ◽  
Vol 1 (11) ◽  
pp. 777-781 ◽  
Author(s):  
Satish C. Singh ◽  
Hélène Carton ◽  
Paul Tapponnier ◽  
Nugroho D. Hananto ◽  
Ajay P. S. Chauhan ◽  
...  

2006 ◽  
Vol 14 (2) ◽  
pp. 193-205 ◽  
Author(s):  
A. RIBEIRO ◽  
L. MENDES-VICTOR ◽  
J. CABRAL ◽  
L. MATIAS ◽  
P. TERRINHA

The 1755 Lisbon earthquake and tsunami had one of the highest magnitudes in the history of Europe. The source mechanism requires generation at a subduction zone. Intensity distribution and tsunami modelling excludes the Gorringe Bank as a source area and suggests generation by the incipient convergence of the Atlantic with the Southwest Iberia and Morocco margin rather than at the less active Gulf of Cadiz Accretionary Prism. The comparison with the 2004 Sumatra earthquake and tsunami supports this interpretation. A tsunami warning alert system is urgent for the Atlantic.


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