Seismicity
Measure of earthquake activity at a given geographical location / From Wikipedia, the free encyclopedia
Seismicity is a measure encompassing earthquake occurrences, mechanisms, and magnitude at a given geographical location.[1] As such, it summarizes a region's seismic activity. The term was coined by Beno Gutenberg and Charles Francis Richter in 1941. Seismicity is studied by geophysicists.
This article provides insufficient context for those unfamiliar with the subject. (December 2016) |