Azores, Portugal
20 March 2022
They do not know if magmatic forces are part of the swarm earthquake that just occurred in the Azores, but it might be a possibility, situation which in some ways reminds a little bit of LaPalma. In order words; let’s keep an eye on what is going on here…
PS: The translation comes via iPad’s / Apple’s translation engine (i am on an iPad now after my computer totally crashed, so I still have to figure out if DeepL on this platform works for me in a workflow or makes it more difficult. Since working on an iPad with a lot of “windows” back and forth isn’t exactly straight forward)
(
Translated from Vulkanet.net)
Swarm quake on Azores island São Jorge
Date: 03/20/22 | Time: 03:43:02 UTC | Location: 38.68 N ; 28.20 W | Depth: 8 km | Ml 3.5
The Azores island of São Jorge has been shaken by a swarm quake since last night. Until now, the EMSC has detected 18 quakes with magnitudes between 2.5 and 3.5, although there have also been numerous weaker earthquakes that are not displayed at EMSC. A total of over 40 earthquakes were detected. The hypocentres are flat, more accurate, at depths between 1-13 km. For an earthquake swarm, the magnitudes are relatively large. Some of the shocks had an intensity of III and were felt by the population. However, no damage has occurred so far.
At a greater distance from the islands, there have also been several moderately strong earthquakes in recent days. The strongest brought it on the 15th. March to a magnitude of Mb 4.7.
The Azores are of volcanic origin and partly associated with the Mid-Atlantic Ridge. However, most of the islands were formed along a leaf shift, the Azores-Gibraltar Ridge. While Europe and North America drift apart on the Mid-Atlantic Ridge, Africa and Europe glide past the Azores gibraltar Ridge. Much of the magma that created the 9 major Azores Islands rose along this seam. Only the two western islands consist of lava, whose magma rose along the Mid-Atlantic Ridge.
Earthquake strip volcanic ridge near Manadas
The most dominant volcanic structure on São Jorge is the volcano Manadas. Strictly speaking, it is a nameless volcanic ridge that strikes the island towards the main fracture zone of the Azores-Gibraltar Ridge and thus runs towards NW-SE. Numerous slag cones line up along the back. The highest is the Pico da Esperança, which last erupted in 1808. The situation is reminiscent of the Cumbre Vieja on La Palma, which kept us in suspense last autumn.
The volcanic ridge on São Jorge is predominantly located in the southeastern part of the island, and only a few earthquake clusters are located directly below the volcanic area, northwest of the Pico da Esperança, which is the only slag cone named on google maps. At the moment it is not yet clear whether the earthquakes are tectonic or vulkanotectonic in nature. Since there have been no earthquakes at greater depths before, which indicated that a magma body rises from the asthenosphere and penetrates the earth's crust, I suspect that these are tectonic shocks. We will only know more precisely after further scientific investigations and until then it cannot be ruled out that Magma has its fingers in the game.