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PYQ 1200 Q/A Part - 1
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Kerala PSC Indian History Book Study Materials Page 24
Book's First PageThe discovery and use of fire was very important to early man for several reasons. They discovered that most animals are afraid of fire. So a campfire gave some protection to the group or tribe. They could camp in better locations. The fire, which gave them protection, allowed them to choose places for camping. They no longer had to look for trees to climb into or rocks and cliffs to shelter under. It kept them warm. This goes with the second reason. They could move into colder climates and hunt the animals that lived there. They could then return to their campfire to warm up. It was a healthier way of life. Cooked food is less likely to carry disease. People began to cook their food consistently. As a result, it would have been easier for the young and the old to survive. It was a more social grouping. They could now gather in larger groups, feeling safer and more secure. This allowed them to exchange stories, and just talk to other people. What went on earlier and later is, of course, still unknown. By the time we reach the upper Paleolithic stage, their occurrences become more profuse and the tools more diverse and beautiful. Distribution and Characteristics of Mesolithic Cultures Transition between Pleistocene and Holocene Periods Towards the end of the geological period of Pleistocene (Ice Age) and the beginning of the geologically Holocene (Recent, Ice-free Age) period, and between the hunting-gathering upper Paleolithic and the Neolithic or a universal stage indicating the beginning of food-production and village-farming economy, the place of the Mesolithic as a distinct archeological level has been well acknowledged in archeology. In the Indian situation, on the one hand, we would assign this level to the preceding upper Paleolithic, and on the other, it should be earlier than the first manifestation of the village-farming economy in the regional context. Correspondingly, it should also be possible to ascribe it to a geological context of the late Pleistocene-early Holocene phase.