Figure 12. Correlation of the ChRM declination and inclination magnitude variation in the sediments of the Belorussian lakes with the magnitudes of the respective PSV records obtained from historical data [Jackson et al., 2000], from archeomagnetic data [Daly and Le Goff, 1996], as well as from the records obtained in the Nautajarvi Lake [Ojala and Saarinen, 2002], in the West Eifel lakes (Germany) [Stockhausen, 1998], and in North Sweden lakes [Snowball and Sandgren, 2002].