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<dc:creator>García Redondo, Natalia</dc:creator>
<dc:creator>Calvo Rathert, Manuel</dc:creator>
<dc:creator>Carrancho Alonso, Ángel</dc:creator>
<dc:creator>Goguitchaichvili, Avto</dc:creator>
<dc:creator>Iriarte Avilés, Eneko</dc:creator>
<dc:creator>Blanco González, A.</dc:creator>
<dc:creator>Dekkers, M. J.</dc:creator>
<dc:creator>Morales Contreras, Juan J.</dc:creator>
<dc:creator>Alario García, C.</dc:creator>
<dc:creator>Macarro Alcalde, C.</dc:creator>
<dc:date>2021-09</dc:date>
<dc:description>We report an archeomagnetic study from the Early Iron Age archeological site of Cerro de&#xd;
San Vicente (Salamanca, Spain). The studied materials were sampled from one roundhouse and its central&#xd;
fireplace, a surrounding burnt floor, and slags with a twofold objective. First, to archeomagnetically&#xd;
determine the last use of the central fireplace, because dating with other methods was imprecise.&#xd;
Second, to retrieve information about the Earth's magnetic field in Western Europe from a period&#xd;
when the Levantine Iron Age Anomaly (LIAA) has been occasionally reported. This study includes&#xd;
mineralogical, archeomagnetic directional analyses, and multimethod archeointensity determinations.&#xd;
Paleomagnetic analyses of the central fireplace yield a mean direction: declination D = 15.1°, inclination&#xd;
I = 52.5°; k = 477.1, and α95 = 5.6°. Archeointensity determinations yield a mean anisotropy-corrected&#xd;
archeointensity of 72.4 ± 2.0 μT (74.7 ± 4.3 μT if a pTRM-check correction is applied) on the central&#xd;
fireplace and 48.2 ± 2.0 μT on slags. A full-vector archeomagnetic dating was performed with the SHA.&#xd;
DIF.4k geomagnetic field model which yielded an age interval of last use of the central fireplace between&#xd;
644 and 575 BCE (654–575 BCE with the pTRM-check corrected data) at 95% confidence level. This date&#xd;
agrees with the archeological context. Results allows to place the high paleointensity obtained near the&#xd;
maximum observed in Iberia at this age, confirming the existence of this peak related to the LIAA in&#xd;
Western Europe where records of this feature are still scarce.</dc:description>
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<dc:language>eng</dc:language>
<dc:publisher>Wiley</dc:publisher>
<dc:title>Further Evidence of High Intensity During the Levantine Iron Age Anomaly in Southwestern Europe: Full Vector Archeomagnetic Dating of an Early Iron Age Dwelling From Western Spain</dc:title>
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