The 2004 earthquake left several traces of coseismic land deformation and tsunami deposits, both on the islands along the plate boundary and distant shores of the Indian Ocean rim countries. Researchers are now exploring these sites to develop a chronology of past events. Where the coastal regions are also inundated by storm surges, there is an additional challenge to discriminate between the deposits formed by these two processes. Paleo-tsunami research relies largely on finding deposits where preservation potential is high and storm surge origin can be excluded. During the past decade of our work along the Andaman and Nicobar Islands and the east coast of India, we have observed that the 2004 tsunami deposits are best preserved in lagoons...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The 2004 earthquake left several traces of coseismic land deformation and tsunami deposits, both on ...
Where historical records are short and/or fragmentary, geological evidence is an important tool to r...
The 2004 Indian Ocean Tsunami (IOT), generated by an exceptionally strong rupture of the Sunda Arc, ...
Tsunamis are low amplitude, large wavelength waves that can significantly impact coastal regions. Al...
The 2004 Sumatra-Andaman tsunami emphasized the catastrophic nature of such disasters and exposed ou...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The 2004 earthquake left several traces of coseismic land deformation and tsunami deposits, both on ...
Where historical records are short and/or fragmentary, geological evidence is an important tool to r...
The 2004 Indian Ocean Tsunami (IOT), generated by an exceptionally strong rupture of the Sunda Arc, ...
Tsunamis are low amplitude, large wavelength waves that can significantly impact coastal regions. Al...
The 2004 Sumatra-Andaman tsunami emphasized the catastrophic nature of such disasters and exposed ou...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...
The identification of paleotsunamis in the coastal geological record requires modern analogues to al...