[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.c34.212 # An Encyclopaedia of Indian Archaeology v2.c34.212 An Encyclopaedia of Indian Archaeology v2.c34.212 - **Language:** English ### [v2.c34.212](https://indike.org/pramana/ins.reference.ghosh-1989.v2.c34.212) \*\*Ghod valley.\*\* The Ghod (18°22'; 73°14') originates about 75 km n.-w. of Pune at an elevation of about 1000 m above mean sea level on the e. slopes of the W. Ghats and flows over the Deccan plateau in e.-s.-e. direction for about 160 km before meeting the river Bhima, a n. tributary of the Krishna. The solid geology of the area is represented by the varieties of basalts and intrusive dolerite dykes of the Cretaceous-Eocene Age. The present climate of the area is predominantly semi-arid. - [Previous: v2.c34.211](https://indike.org/pramana/ins.reference.ghosh-1989.v2.c34.211) - [Next: v2.c34.213](https://indike.org/pramana/ins.reference.ghosh-1989.v2.c34.213) - [Up: v2.c34](https://indike.org/pramana/ins.reference.ghosh-1989.v2.c34) --- Source: [https://indike.org/pramana/ins.reference.ghosh-1989.v2.c34.212](https://indike.org/pramana/ins.reference.ghosh-1989.v2.c34.212) · Pramāṇa