Magma transport in brittle rock occurs by diking. Understanding the dynamics of diking and
its observable consequences is essential to deciphering magma propagation in volcanic …

Forecasting eruptions is a fundamental goal of volcanology. However, difficulties in
identifying eruptive precursors, fragmented approaches and lack of resources make eruption …

Crust at many divergent plate boundaries forms primarily by the injection of vertical sheet-
like dykes, some tens of kilometres long. Previous models of rifting events indicate either …

More than 800 million people live in proximity to active volcanoes and could be directly
impacted by potential eruptions. Mitigation of future volcanic hazards requires adequate …

An existing magma chamber is normally a necessary condition for the generation of a large
volcanic edifice. Most magma chambers form through repeated magma injections …

Monogenetic basaltic volcanic fields occur worldwide in tectonic environments ranging from
extensional to convergent. Understanding similarities and differences between these fields …

We model the ascent and eruption of lunar mare basalt magmas with new data on crustal
thickness and density (GRAIL), magma properties, and surface topography, morphology and …

Twenty years of continuous Earth observation by satellite SAR have resulted in numerous
new insights into active volcanism, including a better understanding of subsurface magma …

Abstract The Cenozoic East African rift (EAR), Cameroon Volcanic Line (CVL), and Atlas
Mountains formed on the slow‐moving African continent, which last experienced orogeny …

When continents are stretched over a long period of time, deep elongated rift valleys form at
Earth's surface and zones of ponded magma, centred beneath the rift, form at the crust …