[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.t2.5 # An Encyclopaedia of Indian Archaeology v1.c14.s10.t2.5 An Encyclopaedia of Indian Archaeology v1.c14.s10.t2.5 - **Language:** English ### [v1.c14.s10.t2.5](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s10.t2.5) Much of the above is conjectural (and largely based on the find of the so-called Yamuna sand in the borings of the dry bed of the Ghaggar; there is strong literary evidence that during the Vedic times both the Sarasvatī and Yamuna flowed independently, \*Ṛgveda-saṁhitā\*, 10.76.7), but the corresponding archaeological facts are solid. Another example of the Yamuna changing its course also comes from the Bharatpur region where we have not only a concentration of PGW sites but the ox-bow lakes and a modern canal—the Gobardhan drain system (Gupta \*et al.\*, 1976). - [Previous: v1.c14.s10.t2.4](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s10.t2.4) - [Next: v1.c14.s10.t2.6](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s10.t2.6) - [Up: v1.c14.s10.t2](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s10.t2) ## Cites (1) - [Ṛgvedasaṃhitā](https://indike.org/pramana/in.veda.samhita.rg.10.76.7) — Sanskrit --- Source: [https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s10.t2.5](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s10.t2.5) · Pramāṇa