The glacial legacy of the EISC during the Younger Dryas Stadial

• Main Authors: Hughes, Anna L.C., Greenwood, S. L., Winsborrow, Monica C.M.
• Other Authors: Palacios, David, Hughes, Philip D., García-Ruiz, José M., Andrés, Nuria
• Format: Book Part
• Language: English
• Published: Elsevier BV 2022
• Subjects: Fennoscandian Ice Sheet; ice-dammed lakes; Loch Lomond Stadial; Svalbard; Younger Dryas; Barents Sea; Loch Lomond; Fennoscandia; Fennoscandian; Ice Sheet
• Online Access: https://research.manchester.ac.uk/en/publications/c1562952-e7da-4a7f-8504-d403096c3446; https://doi.org/10.1016/B978-0-323-91899-2.00046-2; http://www.scopus.com/inward/record.url?scp=85143944381&partnerID=8YFLogxK; https://www.mendeley.com/catalogue/87ccfe44-9f45-36be-a11d-f50ac33a64ae/

The European Ice Sheet Complex (EISC) had already separated into independent ice masses of varying size before the start of the Younger Dryas (YD) Stadial (12.9–11.7ka), ceasing to exist as an integrated complex. Only Fennoscandia sustained an ice sheet at this point with much of the rest of the EIS...