Abstract During the Younger Dryas cold event, the Scandinavian ice sheet readvanced in
southwest Sweden and formed the Middle Swedish end-moraine zone (MSEMZ). Recent
highway construction near Skara has created an exposure through the prominent ridge at
Ledsjö. Through sketching and measurement of structural information, we have documented
the internal character of the Ledsjö moraine. The moraine consists predominantly of clay
with numerous sand pods and lenses, which show undeformed, brittle deformed, or fluidized …