Many scientists who have worked on active lava flows or attempted to model lava flows have
recognized the importance of rheology in understanding flow dynamics. Numerous attempts …

Abstract The Andean Southern Volcanic Zone (SVZ) concentrates many of the most active
volcanoes of the Andean continental arc, as well as the region's most recent and impactful …

Transport properties of natural silicate melts at super-liquidus temperatures are reasonably
well understood. However, migration and transport of silicate melts in the Earth's crust and at …

Abstract Villarrica or Rukapillan (35.9° S; 2,847 m asl) is one of the most active volcanoes in
South America and is the highest-risk volcano in Chile. It has an open conduit with a …

Since the late-18th Century, eye-witness accounts have documented a wide-spectrum of
eruptive activity sourced from Volcán Calbuco located in northwest Patagonia. Despite these …

Given the high eruption recurrence in the Michoacán-Guanajuato volcanic field (MGVF) in
central Mexico, the birth of a new monogenetic volcano can be expected in the future. It is …

The stabilized channel is a crucial element of an 'a 'ā flow system, delivering lava to forward
extending zones of dispersed flow. However, the term stable implies that channel …

Volcano morphology has been traditionally studied from a descriptive point of view, but in
this work we took a different more quantitative perspective. Here we used volcano …

Propagation of a lava flow is governed by slope topography, magma rheology, heat
exchange with the atmosphere and the underlying terrain, and the rate of the eruption …

To examine whether there was any physical or thermal interaction between trees and lava
when a lava flow inundates a forest, we studied the Kīlauea's July 1974 lava flow. We …