The field trip explores the Late Quaternary development of the Pinjaur Dun, an intermontane valley in the NW Himalayas. This valley, situated at the transition between the Kangra recess and the Nahan salient, features at least five levels of surfaces developed during the middle to late Pleistocene. The trip aims to observe the co-evolution of structures and landforms impacted by climate during the late Pleistocene. Participants will explore the evolution of Siwalik hills, which influence the local drainage patterns and sediment dynamics in the valley