The IGN has recorded numerous aftershocks in the metropolitan area during the night, with a movement of magnitude 3.1 in Armilla at 04:40 and another of 2.8 in Ogíjares at 06:27 this Sunday.
Granada has gone to sleep again attentive to any noise, vibration, or movement. The second night after the earthquake that shook the metropolitan area strongly has been very different from the previous one: no other major quake has occurred nor have new serious personal or structural damages been reported, but the aftershocks have continued practically until dawn.
The updated catalog of the National Geographic Institute shows that seismic activity remains concentrated south of Granada capital, around Ogíjares, Gójar, Armilla, Alhendín, and La Zubia. Between midnight and 06:30 hours this Sunday, numerous small magnitude earthquakes appear, several of them felt by the population.
The most significant one this morning occurred at 04:40 hours northwest of Armilla. It reached a magnitude of 3.1, was located seven kilometers deep, and was felt with intensity III.
The ground shook clearly again just before dawn. At 06:27 hours, the IGN recorded a quake of magnitude 2.8 southwest of Ogíjares, six kilometers deep. It was also felt by the population.
The aftershocks of the Granada earthquake during this morning
The sequence allows us to reconstruct a night in which there has not been a new major shock, but neither a disappearance of activity.
At 00:09 hours, a movement of magnitude 1.7 occurred northeast of Armilla. At 00:59, another of magnitude 2 to the west of Gójar.
Then came two earthquakes of magnitude 2.1, one east of Gójar at 01:16 and another southwest of La Zubia at 01:49. At 02:25, another movement was recorded in Ogíjares and at 02:50 one of magnitude 2.4 east of Gójar, felt with intensity III. (Ign)
Activity concentrated again during the second half of the morning. The IGN located movements at 03:23, 03:31, and 03:37 hours in the vicinity of Ogíjares before the earthquake of magnitude 3.1 recorded in Armilla at 04:40.
Nine minutes later, another tremor of 2.1 occurred north of Alhendín. At 05:25 there was one of magnitude 1.5 near Armilla and, after six, another of 1.9 next to Gójar before the movement of 2.8 recorded at 06:27 in Ogíjares.
The photograph from this Sunday morning is, therefore, quite clear: the aftershocks continue, but none have approached the magnitude of the main earthquake.
The IGN reviews the great earthquake: it now places it at magnitude 4.8
There is also a relevant novelty in the official data.
The earthquake that for much of Saturday was reported as magnitude 5 now appears in the updated catalog of the National Geographic Institute with a moment magnitude Mw of 4.8.
The movement occurred at 01:04 hours on Saturday, with an epicenter northeast of Alhendín, extremely shallow character, and maximum intensity V-VI. The IGN itself warns that the characteristics of the earthquakes may be modified as the instrumental analysis progresses.
The revision does not change the exceptional nature of the episode within the recent seismic history of Granada. Large surface movements of this intensity are very uncommon in the metropolitan area.
The immediate reference is found seven decades ago. In 1956, Albolote suffered an earthquake of magnitude 5 that caused 13 deaths, dozens of injuries, and severe damage to hundreds of homes. Since then, Granada had not experienced a comparable surface earthquake in its recent history.
More than a hundred aftershocks since the earthquake
The succession of small movements did not begin this morning. During Saturday, the National Seismic Network had already located almost a hundred aftershocks following the main earthquake, 13 of which were felt by the population and one of magnitude 3.3.
The Andalusian seismic network further expands the picture. The Andalusian Institute of Geophysics counted about 200 movements since this series began on Thursday, August 13, although the vast majority were so small that the population did not perceive them.
Experts had precisely anticipated the scenario that is occurring this morning. During the meeting of the Advisory Committee of the Seismic Plan, they pointed out that the aftershocks could continue for hours or days and even reach magnitudes of 3 or 4.
The Andalusian Institute of Geophysics has found similarities between the current behavior and the seismic series experienced in Granada in 2021, although there is still not enough basis to assert that both episodes will evolve in the same way.
Granada went from more than 500 calls to a second night without serious damage
The change compared to the first morning is significant.
The main earthquake generated more than half a thousand calls to the Andalusian Emergency service. Only in Granada capital were 445 incidents related to the earthquake and its consequences attended to, although inspections did not detect widespread structural damage.
There were falls of cornices and facades, cracks, damage to temples and homes, and numerous episodes of anxiety. Several buildings had to be reviewed by firefighters, municipal technicians, and architects.
The Alhambra delayed its opening to check the entire route before allowing the entry of visitors. The monumental complex was finally able to resume activity after inspections ruled out significant damage.
Five temples in Granada were closed preventively to check the damage caused by the movements, and the Junta continues to monitor the affected properties.
During this second early morning, until 07:30 hours, the official sources and emergency services consulted had not reported a new balance of serious personal or structural damage associated with the nighttime aftershocks.
Will Granada continue to shake this Sunday?
Specialists had already warned that the sequence may continue over the next few days, including movements of magnitude 3 or even 4. That does not mean that another earthquake like Saturday's will occur, nor does it allow for anticipating when a specific aftershock will arrive.
The director of the Andalusian Institute of Geophysics, Inmaculada Serrano, explained that what is expected is for the activity to gradually decrease both in the number of earthquakes and in their magnitude, although a seismic sequence does not necessarily evolve in a linear manner.
The most recent data available early this Sunday summarizes it well: at 06:27 hours the earth continued to move under the metropolitan area, with an earthquake of magnitude 2.8 near Ogíjares.