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Volume 8, Issue 10 (Suppl)

J Earth Sci Clim Change, an open access

ISSN: 2157-7617

Climate Change 2017

October 19-21, 2017

CLIMATE CHANGE

October 19-21, 2017 | Rome, Italy

4

th

World Conference on

Geomorphological changes and tsunami risk in a coastal wetland post-earthquake in south-central

Chile

Carolina Martinez

1,3

and

Rafael Aranguiz

2,3

1

Pontifical Catholic University of Chile, Chile

2

Catholic University of the Most Holy Conception, Chile.

3

National Research Center for the Integrated Management of Natural Disasters, Chile

I

n the central Chilean region (33°-38.6°S), the Mw=8.8 earthquake of February 27, 2010, and the associated tsunami generated

widespread devastation along 600 km of shoreline. This event caused strong morphologic, environmental and social changes.

Coastal uplift larger than 2 m on the west coast of Arauco Peninsula (37°-37.7°S) produced the outcropping of shore platforms,

changes in the intertidal zone, and the drying of wetlands. One of the most affected coastal wetlands was the Tubul-Raqui

where important geomorphological, ecological and socio-territorial changes were generated. Here, the uplift magnitude was

1.4m. In the 1960s, a group of fishermen and algae (gracilariachilensis) gatherers was organized, forming a settlement of

about 2000 residents. This was severely affected by the tsunami of February 27, 2010. In this context, the inundation risk due

to tsunami in Tubul, Arauco Gulf was evaluated. The risk of tsunami inundation is analyzed for an extreme event in the town

of Tubul (37°S), Bio-Bio Region. Three scenarios were identified for risk assessment, in all of which numerical simulation was

applied. Two of the three scenarios were local tsunamis, the events of 1835 and 2010, and the event of 1877 was included to

determine the effects of a far field tsunami. The tsunami of 1835 was determined as an extreme event, which gave inundation

heights of 10m and run-up of 10m. Vulnerability was analyzed from physical, socioeconomic and educational points of views.

Two levels of vulnerability were defined, namely medium and high. These levels were selected based on the poor housing

materials, the vulnerable socioeconomic profiles of the population, low educational levels and the population´s reactions to

these tsunami events. The results show that natural risk is obtained at the high level in the whole town. These results were also

compared with the current reconstruction plan.

Biography

Carolina Martinez is a PhD in Geography. She is a Professor at the Geography Institute at the Pontificia Universidad Católica de Chile (PUC). Her area of research

is geomorphology and costal environment dynamics, coastal and natural risk management. Her recent works are focused on analyzing factors of change on tectonic

coasts that are recently affected by natural disturbances such as earthquakes, tsunamis and swells. She also studies the socio-territorial effects on costal locations.

camartinezr@uc.cl

Carolina Martinez et al., J Earth Sci Clim Change 2017, 8:10(Suppl)

DOI: 10.4172/2157-7617-C1-036