During explosive eruption of low viscosity magmas, pyroclasts are cooled predominantly by
forced convection. Depending on the cooling efficiency relative to other timescales, a …

Volcanism on Earth and on other planets and satellites is dominated by the eruption of low
viscosity magmas. During explosive eruption, high melt temperatures and the inherent low …

Spatter is a common pyroclastic product of hawaiian fountaining, which typically forms vent-
proximal ramparts or cones. Based on textural characteristics and field relations of spatter …

High‐resolution investigations of Late Amazonian volcanic landforms provide previously
unrevealed insights into the dynamics of Martian volcanic eruptions. On Earth, the formation …

We present an in-situ analysis of the reflectance of Visible Near Infrared (VNIR) and the
petrologic texture of the surface of a relatively young lava flow at Jordan Craters, OR. Jordan …

Accurate classification of terrestrial and non-terrestrial volcanic landforms requires a robust
suite of morphometric parameters. The Small-volume Monogenetic Igneous Landforms and …

Spatter cones are a common mafic explosive volcanic feature observed on Earth associated
with Hawaiian and Strombolian-style lava fountaining. Across Mars there are numerous …

To investigate the thermal conditions of spatter eruptions on Earth, other planets, and moons
we measured and categorized the physical characteristics of clasts in spatter deposits in …

Abstract The Mesozoic Natash volcanics are rift-related monogenetic volcanic complex that
erupted in south Eastern Desert of Egypt. The architecture of their building has evolved …

Abstract The Pleistocene to Holocene Lanín composite volcano, in the Southern Volcanic
Zone of the Andes, has summit and flank eruptions of Holocene age. We present here a …