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Potential of satellite based sensors for studying distribution of archaeological sites along palaeo channels: Harappan sites a case study

机译:基于卫星的传感器在研究古河道沿线考古遗址分布方面的潜力:哈拉潘遗址的案例研究

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A large number of remote sensing based studies have shown evidence of a prominent river system, which has become buried under sand cover of Thar Desert sometime during late Holocene. This major river has been identified as Sarasvati, a legendary river mentioned in ancient Indian texts. This region is rich with archaeological sites of Harappan civilization (2500-500 BC). The present study has utilised digital image processing and enhancements techniques on multisensor satellite data followed by field investigations to reconfirm known traces and detect hitherto unknown traces of palaeochannels of Sarasvati river through parts of Indus alluvial plain in Thar desert. Potentials of IRS-P4 OCM (Primarily an Ocean Color Sensor, with eight narrow spectral channels, high radiometric resolution of 12 bits and large swath of 1420 m) could be exploited for the first time to detect hitherto unknown traces of palaeochannels of Sarasvati river through sand dune topography of Thar desert in parts of Western Rajasthan in India and adjoining parts of Pakistan by applying Principal Component Analysis technique. Pattern of palaochannels indicate westward migration of the Sarasvati river in parts of Indus alluvial plain. Database of more than 1000 archaeological sites compiled from various published sources, prepared in GIS environment could be utilised to understand their relationship with identified courses of the Sarasvati palaeochannels. Through this study it was found that there is a large spread of Mature Harappan (2200 -1700 BC) sites along the palaeochannel of the Sarasvati and its tributaries in north-west India, but late Harappan (1700-1500 BC) sites are limited to further west in adjoining regions of Pakistan indicating that the shift of cluster of settlements have followed the pattern of river migration towards west. Digital terrain modelling by superimposing archaeological sites on SRTM DEM along with draped satellite data (Resourcesat-1 AWiFS and IRS-1D LISS-III) has helped in identifying geomorphological guides for archaeological investigations such as presence of relict natural levees seen as raised mounds and coincidence of known archaeological sites over them. It is suggested that other relict natural levees or raised mounds adjoining the identified palaochannel courses may be taken up for further archaeological exploration.
机译:大量基于遥感的研究表明,有明显的河流系统的证据,该河流系统在全新世晚期的某个时候被埋在塔尔沙漠的沙层下。这条主要河流被确定为萨拉斯瓦蒂河,这是印度古代文字中提到的传奇河流。该地区拥有哈拉潘文明的考古遗址(公元前2500-500年)。本研究利用多传感器卫星数据的数字图像处理和增强技术,随后进行野外调查,以重新确认塔拉斯沙漠中印度河冲积平原部分地带的萨拉斯瓦蒂河古河道的痕迹,并迄今尚未发现的痕迹。可以首次利用IRS-P4 OCM(主要是海洋颜色传感器,具有八个狭窄的光谱通道,12位的高辐射分辨率和1420 m的大条带)的潜力,以检测迄今为止穿越萨拉斯瓦蒂河的古河道的未知痕迹应用主成分分析技术,对印度西部拉贾斯坦邦和巴基斯坦邻近地区的塔尔沙漠沙丘地形进行了研究。 palaochannels的模式表明萨拉斯瓦蒂河在印度河冲积平原的部分地区向西迁移。在GIS环境中准备的,从各种公开来源汇编的1000多个考古遗址的数据库可用于了解它们与已确定的萨拉斯瓦蒂古河道的关系。通过这项研究发现,在印度西北部的萨拉斯瓦蒂及其支流古河道上,有大量的成熟哈拉蓬(2200 -1700 BC)遗址,但哈拉蓬晚期(1700-1500 BC)遗址限于在巴基斯坦毗邻地区的更西边,表明定居点集群的转移遵循了河流向西迁移的模式。通过将SRTM DEM上的考古遗址与悬垂的卫星数据(Resourcesat-1 AWiFS和IRS-1D LISS-III)叠加在一起进行数字地形建模,有助于确定考古研究的地貌指南,例如存在被视为土丘和巧合的遗迹天然堤坝上面已知的考古遗址。建议与已确定的palaochannel路线相邻的其他遗迹天然堤防或凸起的土墩可用于进一步的考古探索。

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