Abstract
We present characteristics of tectonic landform in Gelephu in southern Bhutan. First attempt of photo-interpretation related to tectonic geomorphology leads that active faults are distributed densely in southern Bhutan Himalaya. Fieldwork in Gelephu where typical tectonic landform are recognized by photo-interpretation provides us that 1) active fault has deformed landform and deposit in the late Quaternary (125 ka to present), 2) active fault has moved on same trace during the late Quaternary.