The prealpine range of the eastern Southern Alps includes many high-elevation (up to 1900 m) massifs, whose northernslopes contain glacial deposits. On the northern side of the Chiampon-Cuel di Lanis ridge (Julian Prealps) five different mountain morainesystems are sited; these are related to local glaciers, which were independent from the major Tagliamento Glacier during the LastGlacial Maximum (LGM). Their length was slightly more than 3 km, with lateral moraines developed along the lower part of the deep valleys.Their terminal moraines occur from 490 m to 650 m a.s.l. Clast petrography of the carbonate-rich till clearly establishes a localprovenance, distinct from that of the Tagliamento catchment. Inferences from geomorphological parameters, such as elevations of thevalley floor and of the lateral moraines, as well as the extent of the accumulation area, indicate a thickness of the glaciers, ranging from130 to 230 m in the accumulation areas. Application of the Altitude x Area Balance-Ratio (AABR) formula provides an ELA estimate of1130 to 1200 m a.s.l. This is in agreement with the atmospheric circulation models of the LGM for the Eastern Alps, which indicate anELA depression, below 1300 m a.s.l., related to higher precipitation rates than the rest of the Alpine chain.