[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.s8.t4.3 # An Encyclopaedia of Indian Archaeology v1.c14.s8.t4.3 An Encyclopaedia of Indian Archaeology v1.c14.s8.t4.3 - **Language:** English ### [v1.c14.s8.t4.3](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s8.t4.3) In India the glaciations were confined to the higher reaches of the Himalayas. Not all of them descended even down to the Kashmir valley. To draw a Pleistocene—Holocene boundary in India is therefore a hazardous job, particularly when there is very little scope for adjusting the marginal errors. - [Previous: v1.c14.s8.t4.2](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s8.t4.2) - [Next: v1.c14.s8.t4.4](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s8.t4.4) - [Up: v1.c14.s8.t4](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s8.t4) --- Source: [https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s8.t4.3](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c14.s8.t4.3) · Pramāṇa