[Pramāṇa](https://indike.org/pramana/) › [Studies](https://indike.org/pramana/ins) › [Reference works](https://indike.org/pramana/ins.reference) › [An Encyclopaedia of Indian Archaeology](https://indike.org/pramana/ins.reference.ghosh-1989) › v1.c14.s10.t1.6 # An Encyclopaedia of Indian Archaeology v1.c14.s10.t1.6 An Encyclopaedia of Indian Archaeology v1.c14.s10.t1.6 - **Language:** English ### [v1.c14.s10.t1.6](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s10.t1.6) The Quaternary climatic changes \[7.3\] have been recorded in the Indian river valleys in the form of massive alluvial cones (the BANGANGA-BEAS valleys), morainic deposits (the LIDDAR near Pahlgam, Kashmir basin), lake deposits (\*karewas\* in Kashmir) and cut-and-fill valleys \[9.9\] in the peninsular area, and with all of these river valleys are associated human settlements of different periods. - [Previous: v1.c14.s10.t1.5](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s10.t1.5) - [Next: v1.c14.s10.t1.7](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s10.t1.7) - [Up: v1.c14.s10.t1](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s10.t1) --- Source: [https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s10.t1.6](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s10.t1.6) · Pramāṇa