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 …

Aims. Cosmogenic isotopes provide the only quantitative proxy for analyzing the long-term
solar variability over a centennial timescale. While essential progress has been achieved in …

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

Geomagnetic field measurements from the past few centuries show heightened secular
variation activity in the southern hemisphere associated with the south Atlantic anomaly …

This review synthesizes field research, textual analysis, and archaeometric data to evaluate
different explanations for the spread of iron in the ancient Near East. Current evidence …

Earth's magnetic field, one of the most enigmatic physical phenomena of the planet, is
constantly changing on various time scales, from decades to millennia and longer. The …

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 …

The rich and extensively studied archaeological record of the Near East provides an
opportunity to develop a comprehensive archaeomagnetic dataset for exploring the …