Astronuc said:
I was wondering about the swarm of earthquakes in Kumamoto. I don't remember seeing a swarm like that in Japan with other earthquakes. Usually there are a few aftershocks.
For others reading this...
There is a difference between a "swarm" and an "aftershock sequence"
1) a swarm refers to a set of events maybe 10's to a few 100 events where there is no significant main shock. Swarms would rarely contain events of higher magnitude ~M5.5 or greater. They would commonly consist of events in the M0 to M4.5 range ( A caveat ... event magnitude can actually go below M0 ... eg M0.5 ... swarm or otherwise)
2) An aftershock sequence follows a main shock. The mainshock can be small events say a M 4.5 and the aftershocks will be smaller than that M2's M3's etc.
The larger the main shock the more aftershocks there will be. A significant main shock, say a M6.5 could produce 100's of smaller aftershock events
An eg M7.5 or greater can often produce 10's of 1000's of recorded aftershock events particularly for shallow events ~30km or less.
The in general, deeper the main shock the main shock the smaller the number of aftershocks. Very deep main shocks may produce none to just a handful of recorded aftershocks.
A general rule for large main shocks, say around M7.0 and greater, an aftershock of up to 75% of the size of the main shock can be expected in the following 48 hours. Doesn't always happen, sometimes not at all, sometimes within the week following the main shock
Some sequences have foreshocks, then the main shock, then the aftershock sequence.
When foreshocks occur, it is not known if the event(s) is a foreshock or the main shock till some time has passed to see if a larger event occurs
This was apparent with the M6.2 ( original main shock this thread discussed) It was considered a main shock even after the M 6.0, the second largest event occurred but both those events were relegated to being foreshocks once the M7+ event occurred. That doesn't occur overly often and usually the foreshocks ( if any) are significantly smaller than the mainshock.
OK there's the seismology lesson for the nite, all the way from the East African Rift ( my current location)
cheers
Dave