The origin of the town of Andújar (figures 1 and 2), in southern Spain, is likely a Roman settlement, as suggested by certain archaeological evidence in its historical center (figure 2). Andújar was probably founded to control a significant strategic route on the edge of the Guadalquivir River and ending in Córdoba. The town was a flat settlement, without natural shelters, presumably defended in this epoch by a defensive wall or fortification, although no evidence remains of it.
The first clear reference to the defensive wall of Andújar is a request from the emir
Based on information gathered from various archaeological digs in the historical center of Andújar (figure 2), we propose the following construction stages in its walled compound.
As mentioned above, after the taifa-Almoravid improvement and enlargement of the defensive wall system, a moderate earthquake struck this region. In the most recent Spanish earthquake catalog , it is termed the 1169, Andújar (Jaén) earthquake, the most destructive shock known in the whole Iberian Peninsula until the 1396, Tavernes de Valldigna (Valencia) earthquake (VIII-IX, macroseismic
Although there is scarce information about the true effects of the earthquake, as we will see below, there is no doubt that there was a heavily damaging to destructive earthquake in Andújar. Moreover, in this paper we present what we consider to be the first archeological proof of this earthquake after interpreting the results obtained at an archeological site in the town. In archeoseismological studies, scientists must work bearing in mind the old rewrote saying: the presence of evidence is not evidence of presence. Considering contemporary documents of the event together with what we presume to be a recent archeoseismological result, we argue that in this case archeology supports the occurrence of this event.
This historical earthquake should be taken into account for future seismic hazard assessments in this region. If there is a moderate earthquake in an area, then there is a geological structure, known or unknown, that hosted it. Therefore, it is capable of being triggered again in future.
2. Contemporary written sources — Estimating effects and size
Three Arabic documents are the contemporary documentary evidence reporting the effects of this earthquake. They are two original manuscripts and a clear plagiarized summary of one of them providing no further information.
The best-known manuscript is that written by
This is the only text considered in the historical seismicity works including this shock in references [9,11,12]. In reference , authors place the epicenter at Córdoba, assigning it a felt intensity (MM scale) equal to X. In contrast, in reference  authors place the epicenter at Andújar, assigning it a felt intensity (MCS scale) equal to IX.
It is important to note, as he states in his manuscript, that
The second Arabic manuscript referring to this earthquake was written by
The manuscript by
There are only two known works written by
Further support as to the importance of this text and its chronicler, as stated in reference , is the fact that another contemporary historian,
Apart from these texts, there is no evidence of more reliable chronicles related to the event. A very short text (ms. number 4 in the Appendix) included in the so-called
Some researchers in the Spanish historic seismicity consider that this citation likely refers to the Andújar earthquake [7,16], inferring that the quoted date is just the date of the event. In fact, as mentioned, in the recent Spanish earthquake catalog it is identified as the 1169, Andújar earthquake. Although it is quite possible that the Andújar earthquake was felt in the center of the Iberian Peninsula, we cannot guarantee that this sole reference in the
Evidently, the scarce documentary sources of this earthquake are a real problem in accurately dating the event. This lack also prevents researches from estimating with greater detail effects on buildings and people, establishing the meisoseismal area, and determining its impact on the society.
In a recent and comprehensive work , used as a basic historic seismic catalog in seismicity and seismic hazard studies in Spain, it is catalogued with a maximum intensity equal to VIII-IX (EMS-98 scale, used henceforth; ). As mentioned, it appears that there was ground liquefaction, implying at least a degree of intensity VIII. Nonetheless, this value must be supported independently of other effects. The intensity IX is sustained by the presumed effects on buildings, the result of considering that many houses were destroyed or collapsed and that many people died. Using the EMS-98 scale, this implies that many buildings of vulnerability class A (masonry structures of rubble stone, fieldstone, or adobe) sustained damage of grade 5 (total or near-total collapse). Quoted effects concerning mosque minarets described by
Using the empirical relationship among intensity and surface magnitude for the Mediterranean area in  gives
An unpublished geophysical exploration test recently carried out by the authors in an alluvial terrace at the same level as Andújar using the H/V spectral ratio approach based on ambient vibrations, showed resonance frequencies in the range of 5-8 Hz, clearly related to very shallow structures, specifically a shallow sandy sedimentary layer. The potential amplification of earthquake motion by sediments in this area, using this or other approaches, must be explored in depth by future projects. Potential site effects in Andújar are expectable, increasing the seismic hazard in this location, but presumably decreasing the afore-mentioned expectable magnitude for the Andújar earthquake.
There are four fluvial terraces and the present flood plain in the Andújar area, with elevations above the river channel on the order of 55, 25, 13, and 6 m, from oldest to youngest [19,20]. These terraces comprise alluvial sediments from the Guadalquivir River with thicknesses ranging from approximately 5 to 10 m. They show a conglomeratic lithology with a silty mud-matrix that becomes sandy mud-matrix at the top of each terrace level. In general, the lower part of the terraces portrays the channel infilling and bar bedform, and the upper part shows the alluvial flood plain. The ages of these terraces range from the Holocene to 600 ka.
3. Seismic and geological framework
The only shock that stands out in the area is the studied earthquake. Seismicity is very scarce near Andújar, which is characteristic of the northern Guadalquivir Basin. Even within the basin, only a few minor earthquakes (4.0 ≤
The work in reference , using the spatially smoothed seismicity approach, includes a model with the most significant earthquakes in the Iberian Peninsula over the last 300 years. On the other hand, the design acceleration considered in the Spanish building code was computed through a typical zonified method using a broad seismic zone including the whole Guadalquivir Basin. Neither of these two assessments properly included the 1170 Andújar earthquake.
The only instrumental shock in this region deserving of mention is the March 10th, 1951 Linares earthquake (
The presumed mesoseismal area of the Andújar earthquake (figures 1 and 3) involves three tectonic and geographic domains (figure 3). The first, just north of Andújar, is the Paleozoic Iberian Massif, structured during the Variscan orogeny. The Iberian Massif has a flat topography, with the exception of its southern edge, which has a smooth slope.
The second domain is the Guadalquivir Basin, which is a classic foreland basin  formed by the collision of the Internal Zones of the Betic Cordillera with the southern paleomargin of the Variscan Iberian Massif. The Andújar area is located on the north side of the basin, at the piedmont of Sierra Morena. This range, along the Variscan border, has recently been interpreted as a flexural fore-bulge formed by the overload of the Betic chains above the Iberian crust .
The third tectonic domain is the frontal thrust belt (Subbetic and Prebetic) of the Betic Cordillera, which delineates an evident mountain front 40 km south of Andújar, a result of the aforesaid continental collision.
The most active stage of the continental collision occurred in the region between 20 and 7 Ma ago (Burdigalian-Tortonian) . Nevertheless, there is clear evidence of recent tectonic activity along the Betic Mountain Front [29,30] that may account for its limited seismicity. This tectonic and regional seismic activity is probably related to the ongoing Africa-Iberia collision, with a convergence rate of 4-5 mm/year . However, the Andújar region and the Betic Mountain Front are relatively far from the current plate boundary. On the other hand, the Betic thrusts in the area are relatively shallow and detached from the Variscan Basement through the plastic Triassic materials (Keuper). Keuper sediments are rich in clay and gypsum, displaying very plastic behavior and lacking enough strength to accumulate a large amount of stress. Nevertheless, active Betic thrusts can account for small shallow earthquakes along the Betic Mountain Front .
Other tectonic structures near Andújar capable of accumulating enough stress to trigger moderate earthquakes, or at least displaying geomorphologic evidence of recent tectonic activity must also be considered. One possible source of the 1170 earthquake is the flexure of the entire lithosphere. It can cause moderate to strong earthquakes , but only from the beginning of the orogenic overload (Lower Miocene) until viscoelastic stress relaxation and equilibrium was reached, a few million years ago . However, the present intraplate compression could lead to the amplification of the initial flexural foreland loading [34,35] and consequently the reactivation of seismic faults.
Another plausible seismic origin are the faults that fragmented the south Iberian crust during the Mesozoic, creating several blocks that produced swells and troughs in the marine paleomargin . These faults and their lateral ramps were tectonically inverted during the build-up of the Betic Cordillera (Miocene compression) and reutilized mainly as thrusts  until nowadays . Thus, they continue to comprise crustal weak zones locally focusing the present crustal stress to host moderate earthquakes . Most of these faults, seemingly with low slip rates, are now covered by the Guadalquivir Basin sediments (figures 1 and 3) and are difficult to recognize, even by geophysical exploration methods .
No Quaternary active faults have been described until now in the region and no clear limits can be traced at the lithospheric scale that could cluster the stress in the area. Nonetheless, any of the faults of these systems could explain a
4. Archeological evidence
A recent unfinished archeological survey in the south of Andújar, as previously mentioned, has revealed the ruins of a fortification that underwent rebuilding (figure 4). We presume that these repairs are related to the 1170 earthquake.
This archeological dig proves the existence of an early alcazar built in the 11th century, in the taifa-Almoravid stage, used approximately until the first half of the 12th century. In this epoch, it was replaced by a new alcazar located in the northern part of the town, built in the second half of the 12th and first half of the 13th centuries. After this, the early and obsolete alcazar was used only as a guard gate and control point of one of the main gateways (figure 5).
The defensive walls and towers of the early alcazar were built using a matrix of lime, sand, and small stones outside, and dirt and rubbish inside. This construction technique is unquestionably quick and cheap. However, although fillings of dirt and rubbish involve lower cost they also entail structural weakness, particularly for ground shaking during earthquakes. Two towers were excavated during the archeological survey, a small solid square tower to the north and another more complex one to the south (figure 5). This second tower had a room inside with a flat roof connecting the wall walks.
Inside the alcazar, there was a large courtyard or ward where a simple rectangular building was probably used as a storehouse and/or kitchen (figures 5 and 6). The fact that it is not decorated suggests that it was not a room belonging to a palace or a residence. This building, attached to the eastern rampart, is 6.15 m wide, with an ashlar wall 1 m wide parallel to the rampart. The total length of this building is not completely known at the moment because the ends have not yet been excavated. Inside the building were found adobe pillars in a central position, probably related to the inward division and the roof support. Also, a rubble bench attached to the ashlar wall. The building was likely a space without interior walls divided into two rooms separated only by central pillars. These pillars held up central beams forming part of a roof of wood and tiles.
The 1170 earthquake affected (figure 5) both the fortification and the attached building, as we show below.
The northern tower was heavily damaged. In fact, later reinforcement of its foundation can be observed (figure 7). The reinforcement was made by means of a wall of tamped dirt 0.4 m wide and 1.1 m high surrounding the tower at a distance of 1.6 m. The space between the tower and the wall was filled in with cobblestones, two layers of dirt, and another of adobe. At present, the reinforcement can be clearly seen only in the southern part of the tower, but it apparently bordered the entire tower. Thus, the final surface of the tower was quite extended.
The southern tower (figures 8 and 9) was also damaged. Specifically, its northwest corner was destroyed, likely the weakest part due to the opening of the gate. It was repaired, replacing the mud-wall by a tamped dirt wall, remodelling and decreasing the room inside it. The remodelled tower shows support with medium-sized rocks, barely preserved.
The rectangular building inside the alcazar underwent near-total collapse (figure 6). The archeological dig found that the unattached western wall (1 m wide) of this building toppled inwards, to the east, and the fallen blocks are aligned the length of the wall. Fallen rocks tumbled on the rubble bench attached to the wall and on the floor. After the collapse, instead of cleaning out the blocks to the original floor, only a shallow cleaning was made. Therefore, collapsed blocks were buried, raising the level for a new floor. Moreover, previous pillars, likely very damaged or collapsed, were replaced by a dividing wall parallel to the fortification and to the front. From this dividing wall, the room was partitioned into four compartments after its reconstruction.
Some authors have used ordered fallen blocks as seismic-related kinematic indicators [40,41], among others effects, in order to determine, for example, the direction of seismic wave propagation or the degree of seismic shaking. In our case, the occurrence of just one episode unfortunately does not allow any conclusions to be inferred.
Since that time, this defensive complex likely had other functions, mainly as dwellings with rooms, kitchens, stables, and so on, as inferred from the archeological material found. This new use is supported by the fact that in the Almohad epoch, as noted previously, the alcazar was relocated to the northern part of the town, in a more strategic site .
Until now, these damages, reconstructions, and reinforcements could not be accurately dated. In any case, the fact that they occurred during the The
5. Summary and conclusions
In this paper we have presented a case study in seismic archeology that we believe to be the first likely archeological evidence of the 1170 Andújar earthquake. This case concerns one of the thorniest aspects of archeoseismology: to ascribe to historical attested earthquakes observed damages or effects in archaeological digs.
For this shock in southern Spain, only historical/documentary records have been available until now. Initially, a review of the scarce contemporary manuscripts was done, estimating some effects and justifying the presumed size. Then, damaged archeological structures and different repairs and reinforcements revealed in an archeological survey are proposed as true earthquake-related damages. In this case, in addition to the observed reinforcements and damages, there is the supporting evidence  of the historical record. We are confident that repairs and reinforcements in the two discovered and excavated towers, as well as the remodelling of a building attached to the rampart, including tumbled blocks along the length of its wall, are archeoseismological evidence. But it is still not possible from these effects to derive a better earthquake intensity estimate than that from contemporary manuscripts. In any case, we expect further results in future surveys, trusting that the site preserves additional traces of seismic activity in the ground.
The question still remains as to which geological structure hosted this shock. As discussed above, with no more plausible candidates, we suggest hidden faults bordering blocks of the basement as the most likely hypothesis.
Evidently, additional historical, archeological, and geological studies must be undertaken to estimate the size, effects and future implications of this earthquake.
Manuscript number 1
transcription: reference 
Anyone who saw with his own eyes the earthquake which occurred at Córdoba in the year 566 [September 14th, 1170 - September 3th, 1171] has received confirmation [of the Aristotelian theory of earthquakes]. I was not at Córdoba at the time, and when I arrived, I heard the rumble which preceded the earthquake; people thought the rumble came from the west. I saw the earthquake being generated by the progressive movement of west winds. These earthquakes persisted at Córdoba throughout the year, and only ceased after about three years. The first earthquake caused great destruction and killed many people; it was said that at a place near Córdoba called Andujira [Andújar], the earthquake caused the earth to split open and something similar to ashes and sand came out of the fissure. To the east of Córdoba the effects were even more violent, whereas they were slighter to the west.
Manuscript number 2
source: History of the Almohad Caliphate. Manuscript number 433. Bodleian Library. Oxford University
used transcription and translation: reference 
In the same year, the rain for the laid fields in al-Andalus was delayed until the Christian month of December, 1169, and [then] it rained and people sown. In this year big earthquakes happened at dawn and when noon declined in the month of
Manuscript number 3
used transcription and translation: reference 
In this year, a big earthquake happened, at dawn and at the end of the month of
Manuscript number 4
source: vanished codex
used transcription: reference 
Toledo was shaken on February XVIII, MCCVII [February 18th, 1169] [The quoted data in the text concern to the Spanish or Hispanic era, or Era of the Caesars, beginning in the year 38 B.C.].
This work was mainly supported by the Seismic Hazard and Microzonation Spanish research group. The authors are grateful to Emanuela Guidoboni for their constructive comments in an early version of this manuscript.
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