[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.c12.s4.2 # An Encyclopaedia of Indian Archaeology v1.c12.s4.2 An Encyclopaedia of Indian Archaeology v1.c12.s4.2 - **Language:** English ### [v1.c12.s4.2](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c12.s4.2) In Kashmir pollen studies of lower \*karewa\* lake deposits, dating from the Pliocene/early Pleistocene \[9.8.2\] times, have indicated significant changes of climate ranging from cool, moist temperate through cool dry temperate to cool, moist temperate conditions, but it has not yet been possible to relate these changes to any stratigraphically significant horizons indicating major glacial and interglacial periods \[7.3\]. - [Previous: v1.c12.s4.1](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c12.s4.1) - [Next: v1.c12.s4.3](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c12.s4.3) - [Up: v1.c12.s4](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c12.s4) --- Source: [https://indike.org/pramana/ins.reference.ghosh-1989.v1.c12.s4.2](https://indike.org/pramana/ins.reference.ghosh-1989.v1.c12.s4.2) · Pramāṇa