Boletín de la Sociedad Geológica Mexicana

Volumen 72, núm. 1, 2020, p. 1-14

http://dx.doi.org/10.18268/BSGM2020v72n1a020919

 

 

Patrimonio geológico efímero: propuesta metodológica para el inventario y evaluación de las estructuras generadas por licuación de suelos durante sismos, San Juan-Argentina

 

Ephemeral geological heritage: methodological proposal for the inventory and evaluation of structures generated by soil liquefaction during earthquakes, San Juan-Argentina

 

Silvia Beatriz Palacios1,*, Laura Patricia Perucca2

1 Gabinete de Neotectónica y Geomorfología. INGEO. FCEFyN-UNSJ. Avda. Ignacio de la Roza 590 Oeste. Complejo Universitario Islas Malvinas. Departamento Rivadavia, 5402, San Juan, Argentina.

2 CONICET- CIGEOBIO. FCEFyN-UNSJ. Avda. Ignacio de la Roza 590 Oeste. Complejo Universitario Islas Malvinas. Departamento Rivadavia, 5402 San Juan, Argentina.

* Autor para correspondencia: (S. Palacios)

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Cómo citar este artículo: Palacios, S.B., Perucca, L.P., 2020, Patrimonio geológico efímero: propuesta metodológica para el inventario y evaluación de las estructuras generadas por licuación de suelos durante sismos, San Juan-Argen: Boletín de la Sociedad Geológica Mexicana, 72 (1), A020919. http://dx.doi.org/10.18268/BSGM2020v72n1a020919

  

Abstract

In this work, several features of liquefaction are valued as ephemeral heritage structures. These structures usually form during earthquakes of moderate to large magnitude and record important information about the characteristics of the seismic events. In this way, it is possible to act appropriately for their treatment and conservation at the time of its formation. The study of Ephemeral Geological Heritage is a recent research topic in geology that constitutes scientific and cultural resources. The 1894, 1944, 1952, and 1977 earthquakes with epicenters in the province of San Juan, Argentina induced liquefaction structures such as cracks, sand volcanoes, craters, and differential settlements, which caused serious damage to dwellings, and agro-industry in the region. There are several photographic records of such secondary effects. In this work, the analysis of these structures was limited to the distal portion of the Tulum valley, since these areas are susceptible to soil liquefaction. The objective of this study is to establish guidelines for preserving in situ liquefaction structures, considering the fragility of the material and the natural ephemeral time of preservation. Finally, we give some basic recommendations for a survey of liquefaction structures in situ so that in the future, a protocol may be established and accepted by the scientific community for designating ephemeral heritage structures.

Keywords: earthquake, liquefaction, ephemeral heritage, Tulum valley, Argentina.