Monogenetic basaltic volcanoes are the most common volcanic landforms on the continents.
They encompass a range of morphologies from small pyroclastic constructs to larger shields …

The breaking apart of magma into fragments is intimately related to the eruptive style and
thus the nature and footprint of volcanic hazards. The size and shape distributions of the …

Se presenta una revisión de la información disponible sobre historia glacial, cambios en los
niveles lacustres y datos sobre paleovegetación del Pleistoceno tardío de varios volcanes y …

La mayor parte de los grandes volcanes de nuestro país se encuentran ubicados en la parte
frontal de la Faja Volcánica Transmexicana y en otras zonas volcánicas aisladas. En este …

The most viscous volcanic melts and the largest explosive eruptions on our planet consist of
calcalkaline rhyolites,. These eruptions have the potential to influence global climate. The …

Water chemistry of crater lakes, maars and water reservoirs linked to some Mexican
volcanoes within and outside the Mexican Volcanic Belt has been determined for several …

Based on the stratigraphic record of the deposits, analysis of previous works, historic
archives, and eyewitness accounts the 1913 eruption of Volcán de Colima was …

The Ochre Pumice (OP) Plinian fallout was produced by Popocatépetl volcano in central
Mexico, during a major Plinian eruption that occurred 4965±6514C yr BP (3700 BC). The OP …

Abstract The White Pumice (WP) is one of the thickest and most voluminous Plinian fallouts
produced by Popocatépetl volcano in central Mexico during the Late Pleistocene-Holocene …

The probabilistic analysis of volcanic eruption time series is an essential step for the
assessment of volcanic hazard and risk. Such series describe complex processes involving …