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Archaeological Heritage in Karnataka with Particular Reference to Geographical Setting

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Archaeological Heritage in Karnataka with Particular Reference to Geographical Setting Trans.Inst.Indian Geographers ISSN 0970-9851 Archaeological heritage in Karnataka with particular reference to Geographical setting Hema Thakur, Bangalore. Abstract Karnataka has given extremely rich evidence for archaeological remains. The landscape of Karnataka seems to have been suitable for human habitation from the pre-historic through the proto-historic and historic period as evidence for all the three phases is available almost all over the state. In this paper the geographical landscape of Karnataka has been discussed. The drainage of Karnataka is based on three notable rivers - Krishna on the north, the Kaveri on the south, the two Pennars (North Pennar and South Pennar) and the Palar on the east. The drainage of Karnataka is mentioned as settlements from the neolithic period onwards are located close to the rivers and rivers played a crucial role in sustaining human habitation. Similarly, Karnataka enjoys the benefit of numerous mountain ranges. Mountains are a source of economically viable rocks and minerals. There is evidence for the exploitation of metals and minerals since prehistoric period. Other important geographical aspects which may have had a bearing on the historical development such as soil types, flora and fauna, climate, etc. have been examined. Key words: landscape, rivers, mountains, metals and minerals The discipline of archaeology is extremely culture complex in Karnataka were first relevant for the Deccan, especially Karnataka noticed by Col. Colin Mackenzie. They were as this region has a rich assemblage of explored, excavated and analysed by amateur antiquities ranging from pre-historic through archaeologists and other scholars, prominent the proto-historic to early historic period. among them being Newbold, Cole, Knox The antiquities first attracted the attention of and Fawcett, Sewell, Longhurst, Captian the British officers in the nineteenth century Leonard Munn and Sir Leonard Woolley. who perhaps realized their significance A large number of megalithic monuments and thus brought to light a potentially rich were identified for the first time by British source for the reconstruction of the past. It officers in the course of explorations. They was Robert Bruce Foote who established not only faithfully recorded the details the presence of very large number of ground of megaliths and funerary appendage but stone axes in the Karnataka region, in the some of them like Colonel Meadows Taylor valley of the river Krishna and its tributaries. undertook their scientific investigation and Due to his efforts it has now become the best analysis. Furthermore, British officers were documented of the neolithic groups. Ash- perhaps the first to take note of some of the mounds, an integral feature of the neolithic finer aspects of human workmanship such Transactions | Vol. 39, No. 1, 2017 | 109 as paintings executed in rock-shelters. Some centuries of Christian era as the literary of the chance discoveries of the Britishers sources are few. A detailed review of proved to be of immense significance. For archaeological settlements is undertaken instance, C. Beadon, a mining engineer, specially with respect to the location, prospecting for gold in District Raichur, resource utilization, etc. The primary sources discovered at Maski, the famous Asokan used to closely study the geographical edict which mentioned the name Asoka as its setting are the District Gazetteers which author. Consequently the importance of the provide a very clear and detailed account. site was recognised and it attracted further The author also undertook a field-survey to archaeological attention. have first-hand account of the settlements and the immediate surrounding. Aim The aim of the paper is to discuss in detail Geographical Setting and Archaeological the geographic conditions in Karnataka and Settlements its possible link with the establishment and Karnataka shares border with more than sustenance of archaeological settlements. one state. The state of Maharashtra adjoins Karnataka has given rich evidence for northern Karnataka. Maharashtra stands out human habitation from the pre-historic, as a large but fairly homogeneous region through the proto-historic and early historic (15o 44’ - 21o 40’N and 73o 15’ - 80o 33’ E). period. Karnataka is immensely rich in Andhra Pradesh and east Karnataka share natural resources particularly perennial a common border. The Andhra Plateau rivers and their numerous tributaries, fertile (12o 14’ - 19o 54 N and 76o 50’ - 81o 50’ E) soils, rocks bearing minerals, forest cover, covering a major part of Andhra Pradesh, etc. There is sufficient evidence to show that is spread over 2,04,882 km2. Tamil Nadu these resources were being exploited since a and Kerela, on the south of Karnataka, are very long period. For instance, many ancient spread over an area of 74,254 km2. This metal workings have been located which region occupies a significant position as it is testify to the fact that mineral ore was being a connecting link between the Western coast sourced. How far did the local environment and Coromandal coast ((Singh:1971:698, facilitate human habitation? Did the local 821, 851). Though these neighbouring resource base fulfill the basic subsistence states share some common features with needs of various settlements? What bearing Karnataka, it is the rivers which tie them did the local geographical lay-out have on more closely to each other as some of the the over-all socio-economic conditions? important rivers originate in neighbouring These are some of the issues which the states and flow in Karnataka or vice-versa. author has tried to examine in this paper. The drainage of Karnataka is based on three notable rivers - Krishna on the north, the Methodology Kaveri on the south, the two Pennars (North Pennar and South Pennar) and the Palar on Archaeological data is the primary evidence the east. Along with the three great river for the history of Karnataka till the early systems, Godavari and its tributeres also 110 | Transactions | Vol. 39, No. 1, 2017 flow through the state in the north. Few is about 600 mt. with broad flat bottomed streams unite in the Sharavati and flowing valleys, ranging upto 450 mt. Southern half down the Ghats in the falls of Gersoppa join of the area lies on Peninsular gneiss with the Arabian sea. NNW-SSE belts of Dharwar Schists. To the The region of Karnataka can be divided north of Dharwar and Peninsular gneisses, between the forested Malnad in the west and sedimentary rocks such as sandstone, the more open country of the Maidan in the limestone and mudstone of Cuddapah east. Maidan can be further divided between formations are found in a continuous line in North Maidan and South Maidan. Karnataka the west and Kurnool formations in the east. plateau with its Malnad rim and Maidan The remaining area is capped with Deccan character is diversified by the Krishna and trap. South Maidan is a plateau region Cauvery river systems, rainfall variability studded with bare granitic boulders and hills. resulting in varying patterns of land use The region has a relatively moderate climate and settlements. The vast Maidan, so named with greater variability of rainfall, the drier after its relatively low and subdued relief, is parts lie around Chitradurga, in the extreme divided into north and south, largely owing east near Kolar and around Srirangapatam. to cultural differentiations, the former is The region is very rich in mineral deposits, mostly drained by the Krishna and the latter particularly in iron ore, manganese, gold, by the Cauvery system. Malnad in Kannada etc. (Singh:1971: 817, 819). means “hilly country” as Male stands for “hill” and Nadu for country. The Malnad 1. North Maidan - The region of North stretches in a continuous belt trending Maidan has emerged as probably richest in NNW-SSE. The topographical features of the remains of the neolithic period. In North the Malnad also vary greatly from North Maidan there appears to be a concentration of to South. In the North, it attains a height neolithic sites on the banks of river Krishna of 450 mt. to 600 mt. and south of this it and its tributaries, notably the Bhima, the descends and is just an upraised part above Tungabhadra and the Malaprabha. The the general level of the plateau. The South important excavated neolithic settlements attains a height of 900 mt. - 1200 mt. in a that are situated on river banks are Maski (on large tract, especially along the western rim Maski nullah, a tributary of Tungabhadra), just above the coastal plain. Some of the Hallur (on Tungabhadra), as well as a large parts of this area attain considerable height number of explored sites. Proximity to as the Bababudan hills (1,913 mts.). This the rivers must have fulfilled not only the part serves as watershed for the two different basic needs of man concerning subsistence drainage systems and the rivers have, finely but would have facilitated traffic as well. dissected the area giving a picturesque hill- Along with fertile plains drained by rivers and-valley terrain (Singh:1971:794, 814). neolithic man inhabited granitoid hills. North Maidan is a landscape of Notable settlements such as Tekkalakota, monotonous seemingly endless plateau Piklihal, are located on terraces at different covered with rich black cotton soil, of large levels of the hillocks or at the foot of hills. open treeless fields. The general elevation The large number of sites and extensive Transactions | Vol. 39, No. 1, 2017 | 111 pottery suggest that neolithic settlements There are several indications that small were perhaps thickly populated. A crucial scale horticulture rather than agriculture factor that was probably responsible for was practised. The fertile plains drained by sustaining the large population was the rivers were ideal for agricultural activity. resource base that man could effectively The fact that agriculture, even though on a exploit as per his needs.
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