2012
DOI: 10.1193/1.4000033
|View full text |Cite
|
Sign up to set email alerts
|

Factors that Exacerbated or Reduced Impacts of the 27 February 2010 Chile Tsunami

Abstract: The 27 February 2010 Maule earthquake produced a significant tsunami that caused damage along over 600 kilometers of the Chilean coast. At least 124 of the confirmed 525 deaths were attributed to the tsunami. We examine factors that influenced losses from the tsunami. Chile's Servicio Hidrográfico y Oceanográ–fico de la Armada (SHOA) issued a tsunami warning about 11 minutes after the earthquake that was canceled shortly afterwards. Few coastal residents heard the warning or the cancelation due to widespread p… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
2
0

Year Published

2015
2015
2020
2020

Publication Types

Select...
5

Relationship

0
5

Authors

Journals

citations
Cited by 6 publications
(2 citation statements)
references
References 3 publications
0
2
0
Order By: Relevance
“…Long recurrence intervals involving disparate fault arrays on timescales of several 10 3 years can result in obliteration and overprinting of rupture traces, due to postseismic sedimentation, erosion [e.g., Scholz , ], and anthropogenic activity [e.g., Landgraf et al , ], rendering a rigorous determination of fault activity and hazard assessment difficult. As a result, damage and losses are often substantially higher than in plate boundary areas, where the higher frequency of earthquakes generally results in better preparedness [e.g., England and Jackson , ; Dengler et al , ]. This dilemma is furthermore exacerbated by rapid urbanization, growing population, and the concentration of economic values in many continental interiors that have been affected by infrequent earthquakes [e.g., Bilham , ].…”
Section: Introductionmentioning
confidence: 99%
“…Long recurrence intervals involving disparate fault arrays on timescales of several 10 3 years can result in obliteration and overprinting of rupture traces, due to postseismic sedimentation, erosion [e.g., Scholz , ], and anthropogenic activity [e.g., Landgraf et al , ], rendering a rigorous determination of fault activity and hazard assessment difficult. As a result, damage and losses are often substantially higher than in plate boundary areas, where the higher frequency of earthquakes generally results in better preparedness [e.g., England and Jackson , ; Dengler et al , ]. This dilemma is furthermore exacerbated by rapid urbanization, growing population, and the concentration of economic values in many continental interiors that have been affected by infrequent earthquakes [e.g., Bilham , ].…”
Section: Introductionmentioning
confidence: 99%
“…In the near field, the individual responses of coastal communities, based on self-evacuation following shaking of clearly exceptional intensity and duration, literally saved hundreds if not thousands of lives. Most of the tsunami fatalities involved individuals who became entrapped while camping on Orrego Island, in the estuary of the Maule River [97,98]. By contrast, the official governmental response was nothing short of inept: the President herself, on advice from the Chief of Staff of the Navy, issued a statement on national television barring any tsunami risk, about the time the first waves were reaching Valparaíso and after they had devastated the epicentral area; no warning was issued for the Juan Fernández Islands, 700 km west of the epicentre, when there would have been time to evacuate the village, later hit by waves running up 15 m, and causing 30 deaths [99].…”
Section: (A) Events From 2004 To 2010mentioning
confidence: 99%