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|Title:||Earthquakes, subaerial and submarine landslides, tsunamis and volcanoes in Aysen Fjord, Chile|
Calafat, Antonio M.
Hermanns, Reginald L.
Sepulveda, Sergio A.
|Keywords:||Earthquakes -- Chile|
Landslides -- Chile
Landslides -- Risk assessment
Submarine geology -- Research
Submarine topography -- Chile
Tsunamis -- Research
Tsunamis -- Chile -- Aysen Fjord
Volcanic eruptions -- Chile -- Aysen Fjord
|Publisher:||University of Barcelona|
|Citation:||Lastras, G., Amblas, D., Calafat, A., Canals, M., Frigola, J., Hermanns, R. L.,... Rayo, X. (2014). Earthquakes, subaerial and submarine landslides, tsunamis and volcanoes in Aysén Fjord, Chile.|
|Abstract:||The Aysén fjord, 65 km long and east-west oriented, is located at 45.4ºS and 73.2ºW in Chilean Patagonia. It has a maximum water depth of 345 m. It collects the inputs of Aysén, Pescado, Condor and Cuervo rivers, which drain the surrounding Patagonian Andes. The fjord is crossed by the Liquiñe-Ofqui Fault Zone, a seismically active trench parallel intra-arc fault system. On 21 April 2007, an Mw 6.2 earthquake triggered numerous subaerial and submarine landslides along the fjord flanks. Some of the subaerial landslides reached the water mass, generating tsunami-like displacement waves that flooded the adjacent coastlines, withlocal >50 m high run-ups, causing ten fatalities and damage to salmon farms. The research cruise DETSUFA on board BIO Hespérides in March 2013, aiming to characterise the landslides and their effects, mapped with great detail the submerged morphology of the fjord. Multibeam data display deformation structures created by the impact of the landslides in the inner fjord floor. Landslide material descended and accelerated down the highly sloping fjord flanks, and reached the fjord floor at 200 m water depth generating large, 10-m-deep impact depressions. Fjord floor sediment was pushed and piled up in arcuate deformation areas formed by 15-m-high compressional ridges, block fields and a narrow frontal depression. Up to six >1.5 km2 of these structures have been identified. In addition, the cruise mapped the outer fjord floor beyond the Cuervo ridge. This ridge, previously interpreted as a volcanic transverse structure, most probably acted as a limit for grounding ice in the past, as suggested by the presence of a melt-water channel. The fjord smoothens and deepens to more than 330 m forming an enclosed basin, before turning SW across a field of streamlined hills of glacial origin. Three volcanic cones, one of them forming Isla Colorada and the other two totally submerged and previously unknown, have been mapped in the outer fjord. The largest one is 160 m high, 1.3 km in diameter and tops at 67 m water depth. This high-resolution data set illustrates a wide set of geohazards in the recent lively geological history of Aysén fjord.|
|Appears in Collections:||Scholarly Works - FacSciGeo|
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