That Granada continues to tremble after the magnitude 5 earthquake does not mean that it can be anticipated what will happen next.
The National Geographic Institute is explicit: there is currently no method capable of simultaneously predicting the time, place, and magnitude of an earthquake.
What the dozens of aftershocks mean
The aftershocks are earthquakes that occur after the main movement in its surroundings.
Civil Protection explains that they normally decrease both in intensity and frequency as time goes by.
The sequence in Granada fits so far with that general behavior: the large movement reached a magnitude of 5 and the subsequent earthquakes recorded by the IGN are substantially smaller. Among them stands out one of magnitude 3.3 recorded at 06:34 north of Gójar.
This allows describing what is happening, but not using it as a clock to know when it will end.
Do aftershocks release tension and prevent another earthquake?
It is one of the most widespread ideas, but it should not be interpreted in a simplistic way.
An earthquake releases energy accumulated in a zone of the crust, but it also modifies the tensions around the rupture. The subsequent evolution depends on the geometry of the faults and numerous factors that cannot be directly observed with sufficient precision to turn them into a prediction. The IGN itself attributes the difficulty of predicting earthquakes to the non-linear and chaotic behavior of the seismic process.
That is why a long succession of small movements is not a guarantee that all the available energy has already been released.
Granada is on an active fault system
The seismicity of the Vega has a known geological explanation.
Researchers from the University of Granada and the Andalusian Institute of Earth Sciences have characterized an extensional system of active faults in the Granada Basin. Among them is the Granada Fault, one of the most active structures in the system.
The researchers relate these normal faults to the frequent seismic activity of the metropolitan area and have identified an active zone at depth where several of these structures are rooted.
Another work from the CSIC also links the earthquakes in the area with active faults that delimit the basin and cross the Vega.
The swarm of 2021 does not allow predicting what will happen now
The memory of many Granadans has immediately gone back to 2021.
Then a long series of earthquakes occurred in the vicinity of Atarfe and Santa Fe. The IGN recorded thousands of movements during that episode.
But the fact that two sequences occur in the same region does not mean they have to evolve in the same way.
The pattern of 2021 helps to understand that Granada can register periods of prolonged seismic activity; it does not help to calculate how long the activity that started this August 15 will last or what the magnitude of the next earthquake will be.
What can be said this morning
There are three reasonable conclusions.
The first is that aftershocks following an earthquake like the one this morning are expected. The second is that most of the movements recorded after the 5.0 have been of clearly lower magnitude. The third is that the monitoring by the IGN must continue because the sequence remains active.