{"title":"Geomorphological survey at Padang Candi, Kuantan Singingi Regency, Central Sumatra, Indonesia","authors":"J. Arif","doi":"10.24164/pw.v8i1.290","DOIUrl":null,"url":null,"abstract":"Padang Candi site in the Kuantan Singingi Regency of Riau Province, located about 19.3 km southwest of Taluk city, and about 3 km northeast of Lubuk Jambi. In the year 2000s, some archaeological stuff have been found at Padang Candi, among others, various sized of bricks as a raw material for building construction, and some gold plate with scrip. It is presumed those stuffs had a connection with the Sriwijaya Kingdom between AD 800. The goal of the paper is to gain a spectrum of understanding about the assemblages of bricks as a raw material for building construction was found, on three sites that are at Sector-I (sec-I), and the others in small quantities were found at Sector-II (sec-II) and Sector-III (sec-III) on the basis of geomorphological study. This study involves the geomorphological investigation of the area at the scale of 1:2000. In terms of geomorphology, the landscape at Padang Candi consists of two units, namely, the Floodplain Unit formed by Quaternary river alluvium (Qal), and the Low Hilly Unit composed by Tuff Unit as a part of the Miocene Telisa Formation (Tmtu). Sector-I (sec-I) situated on the relatively higher isolated hilly than sec-II and sec-III. The area westward of sec-II might be remains of ancient settlement, and there is trench-like morphology found eastward of sec-I. In the matter of sec-1 which is situated on isolated hilly, evoke a curiosity about the status of building construction at sec-I. The presence of the trench-like morphology also gives arises of curiosity about its function. Those matter should be a consideration by archaeologist when do next excavation and study, including the area which is supposed as an ancient settlement.","PeriodicalId":31467,"journal":{"name":"Pubawidya Jurnal Penelitian dan Pengembangan Arkeologi","volume":"25 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2019-10-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Pubawidya Jurnal Penelitian dan Pengembangan Arkeologi","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.24164/pw.v8i1.290","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
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摘要

巴东坎迪遗址位于廖内省关丹Singingi县,位于塔鲁克市西南约19.3公里,鲁比克占比东北约3公里。2000年,在巴东坎地发现了一些考古物品,其中包括作为建筑原料的各种大小的砖块,以及一些带有纸片的金板。据推测,这些东西与公元800年的斯里维加亚王国有关。本文的目标是获得对作为建筑原材料的砖块组合的理解范围,这些砖块是在第i区(seci)的三个地点发现的,其他少量的砖块是在第ii区(seci)和第三区(seci - iii)根据地形学研究发现的。本研究对该地区进行了1:2000比例尺的地貌调查。在地貌方面,巴东坎地的景观由两个单元组成,即第四纪河流冲积形成的漫滩单元(Qal)和中新世特利萨组(Tmtu)组成的凝灰岩单元(Tuff Unit)。i区(seci)比seci区和seci区位于相对较高的孤立丘陵上。ⅱⅱ以西可能为古聚落遗迹,ⅱⅱ以东为沟槽状地貌。sec-1位于孤立的丘陵上,引起人们对sec-1建筑施工状况的好奇。沟槽状形态的存在也引起了人们对其功能的好奇。这些问题应该是考古学家在进行下一次挖掘和研究时考虑到的,包括被认为是古代定居点的地区。
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Geomorphological survey at Padang Candi, Kuantan Singingi Regency, Central Sumatra, Indonesia
Padang Candi site in the Kuantan Singingi Regency of Riau Province, located about 19.3 km southwest of Taluk city, and about 3 km northeast of Lubuk Jambi. In the year 2000s, some archaeological stuff have been found at Padang Candi, among others, various sized of bricks as a raw material for building construction, and some gold plate with scrip. It is presumed those stuffs had a connection with the Sriwijaya Kingdom between AD 800. The goal of the paper is to gain a spectrum of understanding about the assemblages of bricks as a raw material for building construction was found, on three sites that are at Sector-I (sec-I), and the others in small quantities were found at Sector-II (sec-II) and Sector-III (sec-III) on the basis of geomorphological study. This study involves the geomorphological investigation of the area at the scale of 1:2000. In terms of geomorphology, the landscape at Padang Candi consists of two units, namely, the Floodplain Unit formed by Quaternary river alluvium (Qal), and the Low Hilly Unit composed by Tuff Unit as a part of the Miocene Telisa Formation (Tmtu). Sector-I (sec-I) situated on the relatively higher isolated hilly than sec-II and sec-III. The area westward of sec-II might be remains of ancient settlement, and there is trench-like morphology found eastward of sec-I. In the matter of sec-1 which is situated on isolated hilly, evoke a curiosity about the status of building construction at sec-I. The presence of the trench-like morphology also gives arises of curiosity about its function. Those matter should be a consideration by archaeologist when do next excavation and study, including the area which is supposed as an ancient settlement.
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