Abstract
Abstract Short-distance varve correlations across the Södertörn area have extended the continuous Swedish Time Scale back to about varve -1500 (about 10,400 B.P.). Varve -1073 (= 9,965 varves B.P.) is represented by a distinct drainage varve and a change from diatact to symict varves, recording the “drainage” of the Baltic Ice Lake at Billingen and the invasion of the sea into the Baltic. The varve chronology and the changes in the rate of ice recession provide new data for a firm correlation with the Finnish varve chronology.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
