Luis Diego Morales

TL;DR: The Central Costa Rica volcanic range (CCRVR) as discussed by the authors contains thrust faults and related fault propagation folds, only partly covered by syntectonic and posttectonic volcanoclastic deposits.

TL;DR: In this article, the authors studied the relationship between the amount and distribution of the lava and the ground morphology in basaltic andesite lava flows and derived a velocity profile in the channel and the frontal zone.

TL;DR: In this article, a dynamic model for the activity of Poas Volcano, Costa Rica, is proposed, which leads to the assumption that the kinetic and thermal energies are proportional to the depth at which the mechanical equilibrium is disturbed.

TL;DR: The authors of as mentioned in this paper report that cinco sismos locales of magnitudes intermedias (5 < M ≤ 6.5) and foco superficial (h < 20 km) han afectado the zona with intensidades maximas (Mercali modificado) entre VII and IX grados.

TL;DR: In this paper, a geophysical and geochemical preliminar research has been carried out in the active caldera of Poas volcano during 1980-82, and the temperature increase from 92°C to 960°C in the N-E section of the lava dome seems to be related to the fracturing of the upper plug of the cooling magma body at depth.