Glaciotectonics of Belarus

Different glaciotectonic structures and landforms occur in Ihc territory of Belarus: folded dislomtions, glacial depmsions, mfh and injective fcaturcs. The largest folded glaciodislocation is 30 !an long and 8-1 1 km wide, and glacial rafts are up to 1.5 krn long and 20-25 rn thick. Many gIaciotcctonicstructur~ are clearly expressed in landscape. Most large foldedglaciodislocations were formed during the Sozh (Warthian) Stagc of thc Dnicper GIaciation.