Development of terminoglacial fan influence the kinematics of glaciotectonic folding.
The progradational sequence of fan indicates thickening and steepening of ice lobe margin.
Flexural slip and fold accommodation faults were analysed in terms of buckle folding.
Submarginal conditions for glaciotectonics were inferred from strong fold hinge migration.
Pattern of synfolding deposition of fan allowed to estimate the rate of ice lobe advance.