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Kupgal petroglyphs : ウィキペディア英語版 | Kupgal petroglyphs
The Kupgal petroglyphs are works of rock art found at Kupgal in Bellary district of Karnataka, India. Thousands of petroglyphs have been found at Kupgal, which date to the neolithic or even the old stone age. The site, which includes examples of rock gongs, was discovered first in 1892, but subsequently became lost to researchers until it was rediscovered in the early 21st century. This site features peculiar rock formations with unusual depressions which make musical sounds when struck with boulders. ==The site== The site is situated in the Bellary district of mid-eastern Karnataka, approximately 5 km north-east of the town of Bellary. Archaeological sites in this area appear in the literature under different names, but the names of Sanganakallu and Kupgal, two local villages, occur commonly. Here, neolithic remains are found concentrated on the tops and slopes of an outcrop of granitic hills while remains of the megalithic (Iron Age) and Early Historic, and subsequent periods are found predominantly in surrounding peneplain. Of the many sites here, the largest is located on the biggest and northernmost of the granitic hills. It was called Peacock Hill by the British during the colonial period and was sometimes referred to as such in early literature. Locals, generally call the hill ''Hiregudda'', which simply means ‘Big Hill’ in the local Kannada language. Most archaeological literature, however, refers to the hill as Kupgal hill, after a neighbouring village (though the nearest village is Sirivaram). Recent archaeological research has dated the main period of Neolithic occupation on this hill top between 4000 and 3300 years ago 〔Fuller,D.Q,Boivin,N. & Korisettar,R. (2007). Dating the Neolithic of South India: new radiometric evidence for key economic, social and ritual transformations. Antiquity81(313), 755-778.〕 Kupgal hill is a fairly large granitic hill with several peaks, with a large dolerite trap dyke running along its axis. Petroglyphs belonging to different periods, from the neolithic to the modern day, can be found bruised or engraved on the black rocks all along the dyke. A heavy concentration of rock art is seen where the dyke emerges across the upper northern peak of the hill.
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