<!-- Pramāṇa, a library of Indian primary sources · https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s9.6 -->

[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.s9.6

# An Encyclopaedia of Indian Archaeology v1.c14.s9.6

An Encyclopaedia of Indian Archaeology v1.c14.s9.6

- **Language:** English

### [v1.c14.s9.6](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s9.6)

In the peninsula terraces are formed due to climatic changes although the effect of a mild tectonic activity cannot be ruled out. These river terraces are of the cut-and-fill type.

- [Previous: v1.c14.s9.5](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s9.5)
- [Next: v1.c14.s9.7](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s9.7)
- [Up: v1.c14.s9](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s9)

---
Source: [https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s9.6](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s9.6) · Pramāṇa
