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 magnetic recordings preserved in calcite speleothems and the nature of their
constituent magnetic minerals hold enormous potential for paleomagnetic and …

The selection of paleointensity data is a challenging, but essential step for establishing data
reliability. There is, however, no consensus as to how best to quantify paleointensity data …

This paper presents the results of the 2009 excavations at Site 30 in the Timna Valley, Israel.
The results, coupled with a suite of 11 new radiocarbon dates, fix the chronology of the site …

The Moon possesses strong magnetic anomalies that are enigmatic given the weak
magnetism of lunar rocks. We show that the most prominent grouping of anomalies can be …

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

The intensity of the geomagnetic field varies over different time scales. Yet, constraints on
the maximum intensity of the field as well as for its maximum rate of change are inadequate …

Thellier‐type experiments are a method used to estimate the intensity of the ancient
geomagnetic field from samples carrying thermoremanent magnetization. The analysis of …

Site 34 (“Slaves' Hill”) is a large copper smelting camp located on a flat mesa at the center of
the Timna Valley. The first excavations at the site focused on the main slag mounds, related …

Geomagnetic models based on direct observations since the 1830s show that the averaged
relative change in field intensity on Earth's surface over the past 170 years is less than 4.8 …