<p>In this study, dendrogeomorphic techniques are employed to analyse the temporal frequency and spatial distribution of rockfalls on a talus slope of La Teta valley, located on the NW slopes of Cofre de Perote volcano at ~4000 m above sea level. Based on ...

<p>Coloumbo submarine volcano lies 6.5 km offshore the NE part ofthe Santorini island complex and exhibits high seismicity along with vigorous hydrothermal activity. This study models the local stress field around Coloumbo&rsquo;s magma chamber and investigates ...

<p>Over the past several years, the Mt. Amiata volcanogeothermal area has drawn the attention of the Italian scientific community for an environmental impact assessment concerning any interactions between the geothermal exploitation and the fresh water resources ...

Minimization differences on Cellular Automata approach to predict new inundated area of hot mudflow on LUSI mud eruption disaster which occurred in Sidoarjo area is proposed. There are three characteristics of hot mudflow that is unique such as surface material ...

Space borne differential synthetic aperture radar interferometry (DInSAR) has already proven its potential for mapping ground deformation phenomena, e.g. earthquakes, volcano dynamics, etc covering in continuity large areas. The innovative Persistent Scatterers ...

This paper describes the hot mud that has been gushing from the ground near a gas exploration well, in Sidoarjo, East Java, 35 kilometres south of Indonesia's second largest city, Surabaya.

This paper summarizes physical volcanological, geochemical, and time-volume characteristics of the Plio-Pleistocene part of the Southwestern Nevada Volcanic Field (SNVF) as an example of an extremely low volume-flux end member of basaltic fields.

Two volcanic eruptions in the Sumatra-Andaman arc that followed the disastrous M 9.3 earthquake of 26 December 2004 raise the question of whether these eruptions were triggered by the earthquake.In this paper are presented new evidence to suggest that earthquake-induced ...

Landslides from massive rock slope failure (MRSF) are a major geological hazard in many parts of the world. Hazard assessment is made difficult by a variety of complex initial failure processes and unpredictable post-failure behaviour, which includes transformation ...

In this paper is presented a new class of granular landslide models in which avalanches are simulated with large numbers of independent particles moving under the influence of topographically derivedgravitational and centripetal acceleration. This model is ...