Dispersal index (Volcanology 🌋)

Dispersal index is a parameter in volcanology. The dispersal index D {\displaystyle D} was defined by George P. L. Walker in 1973 as the surface area covered by an ash or tephra fall, where the thickness is equal or more than 1/100 of the thickness of the fall at the vent. An eruption with a low dispersal index leaves most of its products close to the vent, forming a cone; an ...

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

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Dispersal index - Wikipedia