Explosive volcanic eruptions constitute a major class of natural hazard with potentially
profound economic and societal consequences. Although such eruptions cannot be …

The origin of silicic rocks in the Michoacán-Guanajuato volcanic field (MGVF) has been
understudied since the volcanic field attracted the attention of researchers. Using …

The 163 ky history as well as the chemical and 46 km3 volumetric evolution of Volcán
Parinacota are described in detail by new mapping, stratigraphy, and 57 40Ar/39Ar ages …

Determining the state of magma reservoirs is essential to mitigate volcanic hazards.
However, geophysical methods lack the spatial resolution to quantify the volume of eruptible …

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 …

Explosive eruptions that occur with little or no precursory unrest (less than a month) pose the
greatest hazards from volcanoes to nearby populations. Here we focus on the preeruptive …

Plagioclase crystals from the 8 km3 10· 5 ka Upper Toluca Pumice (UTP) eruption from
Nevado de Toluca provide a detailed temporal record of pre-eruptive magmatic processes …

Abstract The Tancítaro–Nueva Italia region (∼ 4400 km2) is located within the west-central
Mexican volcanic belt and spans∼ 80 km of arc length along the volcanic front. On the basis …

The formation of highly evolved, dacitic magmas has been attributed to various processes,
including crystal fractionation, partial melting of overlying crust, and/or assimilation of crustal …

Nevado de Toluca is a stratovolcano in the densely populated Mexican Highland and the
source of three late Pleistocene Plinian eruptions. While the characterization of the …