The volcanic explosivity index (commonly shortened VEI) is a scale, from 0 to 8, for measuring the strength of eruptions. It is used by the Smithsonian Institution's Global Volcanism Program to assess historic and prehistoric lava flows. It works in a way similar to the Richter scale for earthquakes: each interval in value is a tenfold increase in magnitude (it is logarithmic). Most volcanic eruptions are of VEIs between 0 and 2.