<abstract xmlns="http://www.w3.org/1999/xhtml">

A set of brick samples from 26 historical buildings in SE Poland was taken for archeomagnetic study. As a result of this study, the secular variations of inclination of the geomagnetic field from 1200 to 1800 AD were defined for SE Poland. The course of them is approximately the same as obtained in other parts of Europe. The only remarkable difference is a more rapid and deeper drop of inclination noted in SE Poland at the end of the 18th century. The regional curve of secular variations of inclination for SE Poland differs substantially from the coeval curve defined earlier for N Poland (Gdańsk) in their segments dated at the first half of the 18th century, where a deep minimum of inclination was disclosed in the bricks from N Poland only. The reuse of medieval bricks for the construction of objects giving this minimum or later secondary heating of original bricks can be a reason for the difference observed. Further archeomagnetic studies of the bricks of the last millennium are necessary in SE Poland to eliminate the gaps and uncertainties in the regional curve of secular variations of inclination.
</abstract>

A set of brick samples from 26 historical buildings in SE Poland was taken for archeomagnetic study. As a result of this study, the secular variations of inclination of the geomagnetic field from 1200 to 1800 AD were defined for SE Poland. The course of them is approximately the same as obtained in other parts of Europe. The only remarkable difference is a more rapid and deeper drop of inclination noted in SE Poland at the end of the 18th century. The regional curve of secular variations of inclination for SE Poland differs substantially from the coeval curve defined earlier for N Poland (Gdańsk) in their segments dated at the first half of the 18th century, where a deep minimum of inclination was disclosed in the bricks from N Poland only. The reuse of medieval bricks for the construction of objects giving this minimum or later secondary heating of original bricks can be a reason for the difference observed. Further archeomagnetic studies of the bricks of the last millennium are necessary in SE Poland to eliminate the gaps and uncertainties in the regional curve of secular variations of inclination.

Secular Variations of Inclination of the Geomagnetic Field in SE Poland Between 1200 and 1800 AD

Faculty of Earth Sciences and Spatial Management

Department of Magnetism, Institute of Geophysics

Geochronometria

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

A set of brick samples from 26 historical buildings in SE Poland was taken for archeomagnetic study. As a result of this study, the secular variations of...

Secular Variations of Inclination of the Geomagnetic Field in SE Poland Between 1200 and 1800 AD

Publicado en línea: 08 jul 2021

Páginas: 95 - 104

Recibido: 18 mar 2020

Aceptado: 07 dic 2020

DOI: https://doi.org/10.2478/geochr-2020-0031

Palabras clave
archeomagnetism, bricks, last millennium, SE Poland

© 2021 Jerzy Nawrocki et al., published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Secular Variations of Inclination of the Geomagnetic Field in SE Poland Between 1200 and 1800 AD

Publicado en línea: 08 jul 2021

Páginas: 95 - 104

Recibido: 18 mar 2020

Aceptado: 07 dic 2020

DOI: https://doi.org/10.2478/geochr-2020-0031

Palabras clavearcheomagnetism, bricks, last millennium, SE Poland

© 2021 Jerzy Nawrocki et al., published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Palabras clave
archeomagnetism, bricks, last millennium, SE Poland