archaeomagnetic dating problems
From these records, the geomagnetic field variation throughout recent time is well-understood. The Earth's magnetic field is characterised by three measurable parameters: declination, inclination and intensity. There are a number of limitations, however. It is composed of archaeomagnetic and palaeomagnetic information from locations across the world, and includes over 13, directional measurements, and measurements of the intensity of the geomagnetic field Korte and Constable 3. In this study, we tried to date a Holocene monogenetic volcano located in the Kazbeki Volcanic Province by means of a paleomagnetic age determination using the SHA. However, the material was not in situ. It covers an area of approximately km 2 in the upper Tergi basin.
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