Magmatic lull (Volcanology 🌋)

A magmatic lull is a period of declined magmatic activity in volcanically active regions. They may occur as a result of underthrusting of hinterland lithosphere beneath a volcanic arc, changes in subduction parameters such as relative velocity, direction and slab dip, arc-arc collisions and subduction hinge advance. Individual magmatic lulls may last tens of millions of years between period...

https://en.wikipedia.org/wiki/Magmatic_lull

#MagmaticLull #Volcanology

Magmatic lull (Volcanology 🌋)

A magmatic lull is a period of declined magmatic activity in volcanically active regions. They may occur as a result of underthrusting of hinterland lithosphere beneath a volcanic arc, changes in subduction parameters such as relative velocity, direction and slab dip, arc-arc collisions and subduction hinge advance. Individual magmatic lulls may last tens of millions of years between period...

https://en.wikipedia.org/wiki/Magmatic_lull

#MagmaticLull #Volcanology