[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) › v2.c46.118 # An Encyclopaedia of Indian Archaeology v2.c46.118 An Encyclopaedia of Indian Archaeology v2.c46.118 - **Language:** English ### [v2.c46.118](https://indike.org/pramana/ins.reference.ghosh-1989.v2.c46.118) The presence of hot springs and regional lineaments in the source regions of the Aner, a n. tributary of the Tapti, and deeply entrenched rejuvenated course of the modern Tapti indicate tectonic instability in the region. - [Previous: v2.c46.117](https://indike.org/pramana/ins.reference.ghosh-1989.v2.c46.117) - [Next: v2.c46.119](https://indike.org/pramana/ins.reference.ghosh-1989.v2.c46.119) - [Up: v2.c46](https://indike.org/pramana/ins.reference.ghosh-1989.v2.c46) --- Source: [https://indike.org/pramana/ins.reference.ghosh-1989.v2.c46.118](https://indike.org/pramana/ins.reference.ghosh-1989.v2.c46.118) · Pramāṇa