Glaciotectonics of Belar

• Autorzy: Karabanov A.
• Języki publikacji: EN

Abstrakty

EN

Different glaciotectonic structures and landforms occur in the territory of Belarus: folded dislocations, glacial depressions, rafts and injective features. The largest folded glaciodislocation is 30 km long and 8-11 km wide, and glacial rafts are up to 1.5 km long and 20-25 m thick. Many glaciotectonic structures are clearly expressed in landscape. Most large folded glaciodislocations were formed during the Sozh (Warthe) Stage of the Dnieper Glaciation.

Słowa kluczowe

EN

Belarus; Quaternary; glaciation; glaciotectonic; glaciodislocation

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2000
• Tom: Vol. 44, Nr 1
• Strony: 1--7
• Opis fizyczny: fot. rys., bibliogr. 41 poz.

Twórcy

autor

Karabanov A.

• National Academy of Sciences of Belarus, Institute of Geological Sciences, Kuprevich 7, 220141 Minsk, Belarus;,