Archaeomagnetic data are fundamental for our understanding of the evolution of Earth's
magnetic field on centennial to millennial timescales. From the earliest studies of the …

The aperiodic nature of geomagnetic field variations, both in intensity and direction, can aid
in dating archaeological artefacts, volcanic rocks, and sediment records that carry a …

This study presents 32 high-resolution geomagnetic intensity data points from Mesopotamia,
spanning the 3rd to the 1st millennia BCE. These data contribute to rectifying geographic …

Our understanding of geomagnetic field intensity prior to the era of direct instrumental
measurements relies on paleointensity analysis of rocks and archaeological materials that …

Variations of geomagnetic field in the Iberian Peninsula prior to Late Iron Age times are
poorly constrained. Here we report 14 directional and 10 palaeointensity results from an …

In this work, we present 16 directional and 27 intensity high‐quality values from Iberia.
Moreover, we have updated the Iberian archeomagnetic catalogue published more than 10 …

Paleomagnetic analysis of archaeological materials is crucial for understanding the
behavior of the geomagnetic field in the past. As it is often difficult to accurately date the …

Abstract Changes of the Earth's magnetic field have been observed with varying spatial and
temporal resolution since the middle ages by means of compasses, and later by refined …

The magnitude and origin of the Levantine Iron Age geomagnetic Anomaly (LIAA), which
spanned the first half of the first millennium before the common era, are not yet well …

Although a large number of magnetic declination and inclination measurements are
available for the historical period from 1400 to 1900 CE, even the evolution of the axial …