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Seismology. Main earthquakes recorded

Sismologia. Principals terratrèmols registrats Catalonia. 2004
Date Hora d'origen (temps universal) Latitud nord (graus i minuts) Longitud est (graus i minuts) Profunditat del focus (km) Magnitud (escala Richter) Comarca
Gener
3 09:39 42.540 0.830 4 1.6 Alta Ribagorça
23 00:17 42.600 0.850 4 1.6 Alta Ribagorça
Febrer
03 21:16 42.580 0.840 4 3.2 Alta Ribagorça
15 01:36 42.760 0.880 10 2.2 Vall d'Aran
22 22:32 42.600 0.850 4 1.5 Alta Ribagorça
Març
2 04:14 42.270 2.530 4 1.7 Garrotxa
24 20:31 42.060 2.640 10 1.6 Garrotxa
26 04:26 41.990 2.630 10 1.7 La Selva
26 04:39 41.050 1.300 10 1.8 Costa Tarrag.
Abril
01 12:31 41.010 1.320 10 2.0 Costa Tarrag.
4 04:09 42.420 0.700 4 1.9 Alta Ribagorça
5 08:50 41.170 1.430 8 1.5 Tarragonès
13 12:32 41.450 2.340 28 1.7 Costa Maresme
30 12:17 41.830 2.770 4 1.6 La Selva
Maig
03 18:07 42.650 1.040 10 1.6 Pallars Sobirà
17 09:17 41.210 1.050 10 1.6 Baix Camp
18 09:52 42.360 3.200 6 1.5 Alt Empordà
Juny
1 16:50 42.300 2.230 8 3.5 Ripollès
1 17:13 42.300 2.250 8 1.6 Ripollès
1 17:35 42.290 2.230 7 1.6 Ripollès
2 13:05 42.300 2.240 8 1.8 Ripollès
3 08:35 42.300 2.240 8 1.5 Ripollès
4 04:57 42.290 2.230 8 3.0 Ripollès
4 16:23 42.300 2.230 8 1.6 Ripollès
4 17:19 42.310 2.260 7 1.5 Ripollès
22 01:54 41.830 2.760 10 1.5 La Selva
28 16:48 42.300 2.220 7 1.8 Ripollès
Juliol
06 20:06 41.850 2.640 7 2.0 La Selva
28 08:57 42.450 3.330 10 2.0 Costa Empordà
31 16:30 42.310 2.480 11 1.8 Garrotxa
Agost
09 08:43 40.320 1.290 10 1.9 Mediter. (SE Montsià)
17 09:22 42.300 2.210 9 1.7 Ripollès
22 10:13 40.910 1.580 8 3.0 Costa Tarrag.
22 11:43 40.940 1.570 4 1.7 Costa Tarrag.
25 09:16 41.150 1.690 10 1.5 Costa Garraf
25 11:13 42.400 2.320 4 1.6 Ripollès
25 14:48 40.960 1.590 10 1.6 Costa Tarrag.
27 23:20 41.190 1.760 6 1.6 Costa Garraf
Setembre
06 18:12 42.310 2.220 7 1.5 Ripollès
7 02:27 42.300 2.220 7 1.8 Ripollès
10 06:38 42.640 0.880 4 1.8 Vall d'Aran
15 20:25 41.850 2.650 10 1.5 La Selva
21 15:48 42.340 2.170 4 4.0 Ripollès
21 16:04 42.350 2.170 6 1.7 Ripollès
21 16:42 42.340 2.150 4 1.7 Ripollès
21 16:51 42.330 2.170 4 1.5 Ripollès
21 18:13 42.330 2.160 4 2.3 Ripollès
21 18:25 42.340 2.180 4 1.9 Ripollès
21 18:57 42.330 2.160 4 1.5 Ripollès
22 00:47 42.330 2.150 4 2.1 Ripollès
23 09:50 42.340 2.170 5 2.7 Ripollès
23 09:58 42.340 2.150 4 3.3 Ripollès
23 10:00 42.340 2.180 5 2.5 Ripollès
23 10:25 42.340 2.190 5 1.7 Ripollès
27 00:45 42.350 2.140 4 1.7 Ripollès
30 04:04 42.340 2.170 4 2.0 Ripollès
30 04:51 42.340 2.180 5 1.5 Ripollès
Octubre
04 18:07 41.580 2.550 5 2.4 Maresme
4 18:48 41.560 2.580 7 1.5 Maresme
24 00:39 42.330 2.140 4 2.0 Ripollès
28 17:58 42.340 2.140 4 2.0 Ripollès
30 08:13 40.520 0.870 5 2.2 Costa Montsià
Novembre
06 01:06 41.580 2.550 6 1.6 Maresme
21 21:57 42.180 2.380 10 1.5 Garrotxa
Desembre
02 18:11 41.580 2.550 6 2.6 Maresme
5 08:49 41.580 2.560 4 2.2 Maresme
6 08:25 42.270 2.110 10 1.5 Ripollès
21 04:43 42.330 2.150 4 2.8 Ripollès
28 10:25 41.670 0.930 7 1.5 Pla d'Urgell
Source: Institut Cartogràfic de Catalunya.
Note: Sismes amb magnitud superior a 1 a l'escala de Richter.

Last update: February 20, 2012.

Methodological note

Definition of concepts

Magnitude of an earthquake
Instrumental measure of its force. It is related with the energy transported by seismic waves. It is expressed in decimal figures in accordance with the Richter scale, whose highest value is 9.
Profundity of the focus of the earthquake
Distance from the point where the earthquake originated and the epicentre or point of vertical projection over the surface of the Earth. It is expressed in kilometres.
Earthquake
Set of shockwaves generated from a point within the Earth, called its focus or hypocentre, as result of which there is a sudden release of energy produced by a brusque movement between blocks of the crust and the mantle of the Earth. They are defined by the following: magnitude and depth of the focus.

Methodological aspects

The Western Mediterranean is located in a collusion zone between the European and African tectonic plates.

The Seismology Service was created in 1981 to study in detail the seismic activity in the territory, to monitor it closely, and to determine and characterise the seismic zones.

Since 1984, hypocentral determinations have been conducted in consideration of the Service's own data and that of other bodies: the Midi-Pyrénées Observatory, the Institute of Catalan Studies, the National Geographic Institute, the Ebro Observatory, the Fabra Observatory and the Detection and Geophysical Laboratory. Information on seismic activity in Catalonia and its neighbouring regions is released annually in the Seismic Bulletin published by the Geological Institute of Catalonia.

The criterion was to select all the seismic movements those that had an epicentre within the Catalan territory and were of a magnitude equal to or higher than 1.7 on the Richter scale.

Provisional data.