Chapter H the Sites, Their Ecological Setting and Cultural Sequence

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Chapter H the Sites, Their Ecological Setting and Cultural Sequence Chapter H The Sites, Their Ecological Setting and Cultural Sequence Fig. 2.1. Map showing Chalcolithic site* referred in the text, A M H If (; M' 0 ft<' c ADIUA pnAOESH V N /P f~ GUJAMAT ( > - - ^_ 1. - OIIULE ^) 1 y , \ \ AMnAVAU •r'-X .9 ) ARAI I • 1 'f !., •\, NTOPUH ;.»'"" JAIOAOH nUlRAMA \ r .'"'• JWAIUMIA',^ / 1 \ ) --' NA5HIK "i _< ,- 1 1 AKOIA • i ' 'AVnAMOARAO 1 VAIMAl , ^.f^ 1 6 M\ A ..^ M^' A-,, n A (S H,/ T n X >' y IHAME ^V'' " 3 4'"5-v, > ! ^~--^ - f • • •'-/—, ( PAnBMAItl / •;-.• -,^^ AMMAD'MOAn > .-J ; cnt/MrJUU <-' ] '"•', ./" / \ \ \-- ' BIO ( 1 f HANDED*' N \ - i"; \ 6 \ iMANAOAOVJ /^ ANOHMA PMADESM 1 .,_ ', lAiun j L , SOlAPUn lAIARA lnoniH ' VlAINACiini / SAimii ' ' -> 1 ) ( ) \ '• iiAPun, -^ s 1 <•. " KM \tMIAKA y' \ 5ii(0l|u lunoj v -^ ") 1( \ * \ J 1 - • 1. Kaothe, Z. Nasik, 3. Daiiabad, 4. Nevasa. 5. Apegaon, 6. UaltTi, 7. lna«lgaon, 8, Tuljapu^ Garhi and 9. Ada'k. 12 THE SITES, THEIR ECOLOGICAL SETTING AND CULTURAL SEQUENCE 2.1. Chalcolithic sites Over 200 Chalcolithic sites have been reported from Maharashtra, a majority of which belonged to the Early Jorwe 'U^ll: period followed by the Walwa and very few of the Late Jorwe | ' '^ a period. Of the total fourteen excavated Chalcolithic sites, in western Maharashtra only Inamgaon, Kaothe, Walki, ^, Tuljapur Garhi and Adam (Fig 2.1) have produced reports of ' detailed faunal studies. Nevasa, Apegaon, Daimabad and Nasik have given only brief reports of the animals, the rest of the excavation reports do not mention anything about the faunal remains except for some small description of stray animal motifs depicted on the pottery. Published data from the above sites are also used for comparative purposes. INAMGAON The Chalcolithic site at Inamgaon (N lat. 18"36'; E long. 74*32') in Pune district is situated on the right bank of the river Ghod, a tributary of the Bhima. The total inhabited 7 i i area roughly measures 550 X 430 m. The maximum length of the \ mound northsouth is 215 m and the breadth eastwest is 175 m. The total cultural deposit is 4.IB m thick. Three cultural periods were noticed and they are as follows: Malwa Phase 1600 B.C.-1400 B.C. Early Jorwe Phase 1400 B.C.- 1000 B.C. and Late Jorwe Phase 1000 B.C.- 700 B.C. This is one of the most extensive Chalcolithic sites in Maharashtra. This site was excavated by Late Prof. H.D. 13 Sankalia, Prof. M.K. Dhavalikar and Dr. Z.D. Ansari from the department of Archaeology, Deccan College, Pune for about twelve field Beasons between 1968-1984 (Dhavalikar, et.aJ. 19BBa). The Chalcolithic settlement at Inamgaon is situated on an alluvial fill terrace about 14 m above the bed level of the river Ghod. Geologically this area is covered by Cretaceous-Eocene Deccan Trap basalts. Except the older alluvium of the late Pleistocene age and the sub-recent alluvium of the Holocene age there are no later formations. This area falls in typical semi-and zone with the mean annual rainfall 500 mm. The rainfall is received from the Southwest monsoons during the four months from mid June to mid October. The soils around this region are black in PI i colour. Black colour of the soil is due to the presence of clay-humus colloidal complex formed by blo-inorganic processes. The vegetation is of scrub type. The xerophytic vegetation includes typical species like Bor {2 i zyphus jujuhi) ^ wild Babhul {Acacia arabica)^ Khair iAcacia catechu) ^ Chinch (Tamarindus mdica) , etc. The food economy of the early farming communities at Inamgaon was based on subsistence agriculture, stock- raising, hunting and fishing. The plant remains from the site reveal that the inhabitants had knowledge of double cropping (Kajale 1988). Large rectangular structures are identified as granaries in the Malwa and the Early Jorwe phases. In the Malwa and the Early Jorwe, the structures are rectangular in shape and are circular in the Late Jorwe 7 ^. 14 phase <Dh«valikar 1988). A major part of the faunal remains have been studied by Thomas (1988). The faunal assemblage comprises mammals, reptiles, birds, fishes and molluscs. Over 35 animal species are identified at Inamgaon. The domestic animals identified are cattle, buffalo, sheep, goat, dog, pig, horse and ass and the wild animal species are sambar, chital, blackbuck, foui— horned antelope, hare and mongoose, etc. WALK I The ancient site Walki (N lat.lB* 35'; E long.74» 18) is located about 32 km west of Inamgaon, in the Pune district. It is situated on the right bank of the river Bhima near the confluence of river the Mula. This was excavated by Prof. M.K. Dhavalikar for two field seasons between 1985 and 1987. The site was probably occupied around 1200 B.C. (Dhavalikar et. al. 1990b). The site is located in the semi-arid zone of north Deccan where the annual rainfall is around 500 mm and most of it occurs during the monsoon months from June to October. The remaining eight months are characterised by extremely dry weather. In the earlier part of this century, there was thick scrub forest, and small games were plentifully available and also small herds of deer and wild boar. But the increasing population has been destroying the forest cover with the result that the landscape today is totally bare and almost all wild animals became totally extinct with the depletion of 15 the forest cover. The important feature of this Jorwe culture site le xte circular huts with flimsy floors and had no solid walls which indicate their temporary nature. The settlement was occupied only during the winter season. The bone tool made of the shoulder bone of cattle, had two perforations and was triangle in shape and the 35 cm long antler fragment which was hollow, are very significant and unique findings. yid"^ (e* Probably these two tools were associated with agricultural C operat ions. More than 50,000 fragments of bones have been collected from this excavation. The 26 species identified include mammals, birds, reptiles and fishes. Cattle was the most predominant animal in the food economy and the second most important animal was blackbuck which was excessively hunted by the inhabitants of Walki (Joglekar 1992; Joglekar and Thomas 1995). KAOTHE The Chalcolithic site, Kaothe (N lat. 21* 00'; E long. 74*18') is situated on the left bank of the river Kan, a tributary of the river Panjhara which is a major tributary of the river Tapi. This site was excavated under the leadership of Prof. M.K. Dhavalikar. Kaothe is located at a distance of half a kilometer west of the present village at an elevation of 451 m. The river Kan has developed a shallow meander and the Chalcolithic settlement is confined to the inner periphery of the meander on a 7 to 8 m high alluvial flat surface. The settlement is roughly oblong in shape and spread 16 over an extensive area of about 30 hector. Kaothe is a eingle culture site, cultural debris la very thin therefore, trenches were dug in three localities viz. KTE I located in the eastern side of the site, KTE II was in the central part, whereas KTE III was located to the northwest of KTE II. The single radiocarbon date available for the Kaothe is 1920 + 90 B.C. (uncalibrated). This provides a time bracket of 2000 - 1800 B.C. for Kaothe cultural phase. (Dhavalikar, et.al. 1990a). The region around the ancient site is covered by Cretaceous - Eocene Deccan trap basalts and the common rock type is mainly compact and vesicular varieties of basalt. This region can broadly be classified as hot semi-arid monsoonic. It receives an average rainfall of about 1200 mm. This area is less affected by droughts and scarcity conditions as compared to similar semi arid region of Deccan upland drained by the rivers Godavari, Bhima and Krishna. Soils are pedocal type black soils or vertisols and are medium textured with clay content varying from 35 to 50*/.. The black colour of the soil is mainly due to the presence of clay-humus colloidal complex formed by blo-inorganic process. The natural vegetation around Kaothe consists of thorn and scrub type forest represented by xerophytic plant species, include Bor (Zyzyphus jujuba), Babhul (Acacia arabjca wild), Chinch (Tamrindus indica) y etc., and the wild animals of this region are fox, jackal, wolf and hare. 17 Thomae and Joglekar (1990) have studied the faunal remains and identified 38 species of animals which include mammals, reptiles, birds, fishes, crustaceans and molluscs. Domestic animals reported from here include cattle, buffalo, sheep, goat, piQ and dog, while wild animals are nilgai, blackbuck, four-horned antelope, chital, sambar, hog deer, barking deer, wild pig, fox, civet, bear, langur, porcupine, mongoose and rat. AQ crpmpared to eoma of the other archaeological sites, the density of faunal assemblage at Kaothe is more considering the thickness of the deposit as well as the area excavated. Probably it reveals the fact that the inhabitants of Kaothe were more depended on animal food rather than agricultural products in their subsistence (Thomas and Joglekar 1990). Pit dwelling is an important feature of this culture. The evidence from Palaeobotany, Zooarchaeology and Ethnographic parallels indicates a seasonal occupation at the site. These Savalda people may have occupied the site only during monsoon. Their economy was based more on stock- raising, subsistence agriculture and hunting-fishing. NASIK Nasik (N lat. 20" 00'; E long.73' 51") is an ancient town situated on both bank of the river Godavari. This site was excavated by H.D. Sankalia and 5.B.
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