El Salvador - GFDRR
El Salvador - GFDRR
El Salvador - GFDRR
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I. DESCRIPTION OF THE EVENT | 17<br />
C. HOW UNUSUAL IS THIS EVENT? HISTORICAL EVIDENCE OF SIMILAR EVENTS<br />
With regard to the extreme rainfall, according to historical records and recorded landslides, and with<br />
respect to climate events that affect the country, this event is neither unusual nor infrequent. There is<br />
information on previous events and there are records from the last 100 years about various lahars with<br />
disastrous consequences in the San Vicente area. Most of them were the result of intense rains (lasting 5<br />
to 7 days straight, according to witnesses’ testimonies).<br />
BOX 1. THE SEVEREST LAHARS IN EL SALVADOR<br />
1774: Lahar on the northeastern slope of the volcano, affecting the city of San Vicente.<br />
1912: Lahar totally destroys Verapaz, causing numerous deaths both in Verapaz and in Agua Agria, a<br />
village higher up on the slope of the volcano.<br />
1934: Total destruction of Tepetitán by a lahar that originated in <strong>El</strong> Blanco creek, with numerous victims<br />
(for this reason, Nueva Tepetitán was founded). Likewise, Guadalupe was struck in 1934 by a<br />
lahar that originated in <strong>El</strong> Derrumbo creek, destroying various houses and causing victims.<br />
1996: On the southern slope of the volcano, a landslide blocked the main road between Tecoluca and<br />
Zacatecoluca.<br />
2001: Landslides caused by the February 13 th earthquake on the northern and northwestern slopes<br />
flowed toward the valley although they did not become lahars. However, the landslides deposited<br />
over 200,000 cubic meters of sediments in the channels that drain the volcano, and thus the<br />
instability of these sediments represents an increased risk for floods and lahars downstream<br />
toward Guadalupe, Verapaz and Tepetitán, as demonstrated in 2009.<br />
2001: On September 15 th , Guadalupe was struck by a lahar from <strong>El</strong> Derrumbo creek, triggered by rains.<br />
There was one victim and numerous houses were destroyed in approximately the same zone that<br />
was affected by the 1934 event.<br />
2005: Tropical Storm Stan produced several landslides on the eastern shore of Lake Ilopango.<br />
The period of return (recurrence) of situations with intensities similar to the current one is difficult to<br />
estimate due to the lack of continuous series of precipitation by hour per day. However, it may be stated<br />
that a critical factor was the 7-hour period of rain. The major damages caused by landslides appear to be<br />
associated with the presence of tropical storms lasting 3 to 4 days. If rains occur for periods of 5 to 10<br />
hours, with per-hour intensities over 30 to 50 mm in the final phase of a storm or depression, when the<br />
soil is saturated it is almost certain that a catastrophic event will occur.