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'Değirmentepe' or 'Değirmentepe Hüyük' is an archaeological site which is located at 50 km north of the river Euphrates and at 24 km in the northeast of Malatya province in eastern Anatolia. It is now submerged in the reservoir area of ​​the Karakaya and Atatürk dams. Rescue excavations were undertaken in 1978 under the supervision of Ufuk Esin of Istanbul University and interrupted in 1989 by flooding of the dams. Four archaeological layers whose dates are determined by techniques such as C14 and traces of fusion have been discovered in this mound:

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  • Değirmentepe (en)
  • Değirmentepe (es)
  • Değirmentepe (fr)
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  • 'Değirmentepe' or 'Değirmentepe Hüyük' is an archaeological site which is located at 50 km north of the river Euphrates and at 24 km in the northeast of Malatya province in eastern Anatolia. It is now submerged in the reservoir area of ​​the Karakaya and Atatürk dams. Rescue excavations were undertaken in 1978 under the supervision of Ufuk Esin of Istanbul University and interrupted in 1989 by flooding of the dams. Four archaeological layers whose dates are determined by techniques such as C14 and traces of fusion have been discovered in this mound: (en)
  • Değirmentepe ou Değirmentepe Hüyük est un site archéologique qui se situe à 50 km au nord du fleuve Euphrate à 24 km au nord-est de la province de Malatya en Anatolie orientale. Il est immergé dans la zone de réservoir des barrages de Karakaya et Atatürk. Des fouilles de sauvetage ont été entreprises en 1978 sous la supervision d'Ufuk Esin de l'Université d'Istanbul et interrompue en 1989 par les inondations des barrages. Quatre couches archéologiques dont les datations sont déterminées par des techniques telles que le C14 et les traces de fusion ont été découvertes dans ce monticule : (fr)
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  • 'Değirmentepe' or 'Değirmentepe Hüyük' is an archaeological site which is located at 50 km north of the river Euphrates and at 24 km in the northeast of Malatya province in eastern Anatolia. It is now submerged in the reservoir area of ​​the Karakaya and Atatürk dams. Rescue excavations were undertaken in 1978 under the supervision of Ufuk Esin of Istanbul University and interrupted in 1989 by flooding of the dams. Four archaeological layers whose dates are determined by techniques such as C14 and traces of fusion have been discovered in this mound: 1. * Middle Ages (late Roman-Byzantine period) 2. * Iron Age (1000 BC) 3. * Bronze Age ancient I (Karaz or Khirbet Kerak culture, end of 4th millennium-beginning of 3rd millennium BCE) 4. * Chalcolithic Age (Ubaid period, second half of Vth millennium BCE.) The Chalcolithic Değirmepe level of Obaid-4 of the second half of the Vth millennium BCE, of which the sites of Tülintepe, Seyh Hüyük and Kurban Hüyük are contemporary, contain skeletons of adolescents with skull deformed. The remains of this cultural phase belonging to the Chalcolithic are relatively well preserved. However, serious damage caused by occasional flooding of the Euphrates, especially on architectural structures and the cemetery is to be deplored. Cranial deformities are not observed on human remains discovered and identified in Iron Age periods and medieval levels from Değrentepe. The Chalcolithic period of this ancient village is characterized by rectangular mud brick houses that communicate with each other. We see the appearance of domestic animals such as dogs, sheeps, goats, pigs and Bovinae than at the beginning of the Chalcolithic. barley, wheat, oats, and peas were the most commonly cultivated plants. Many potterys characteristic of the Obaid culture have been found at the site. Archaeologists have discovered 450 sealings there which testify to the presence of notables capable of managing the productions · . (en)
  • Değirmentepe ou Değirmentepe Hüyük est un site archéologique qui se situe à 50 km au nord du fleuve Euphrate à 24 km au nord-est de la province de Malatya en Anatolie orientale. Il est immergé dans la zone de réservoir des barrages de Karakaya et Atatürk. Des fouilles de sauvetage ont été entreprises en 1978 sous la supervision d'Ufuk Esin de l'Université d'Istanbul et interrompue en 1989 par les inondations des barrages. Quatre couches archéologiques dont les datations sont déterminées par des techniques telles que le C14 et les traces de fusion ont été découvertes dans ce monticule : 1. * Moyen Âge (période romaine-byzantine tardive); 2. * Âge du fer (1000 avant JC); 3. * Âge du bronze ancien I (culture Karaz ou Khirbet Kerak, fin du 4ème millénaire-début du IIIe millénaire av. J.-C.); 4. * Âge chalcolithique (culture d'Obeïd, seconde moitié du Ve millénaire av. J.-C.). Le niveau chalcolithique Değirmentepe d'Obeïd-4 de la seconde moitié du Ve millénaire av. J.-C., dont les sites de Tülintepe, Seyh Hüyük et Kurban Hüyük sont contemporains, contiennent des squelettes d'adolescents au crâne déformé. Les vestiges de cette phase culturelle appartenant au Chalcolithique sont relativement bien conservés. Il faut cependant y déplorer de graves dommages causés par des inondations occasionnelles de l'Euphrate, notamment sur les structures architecturales et les cimetières. Les déformations crâniennes ne sont pas observées sur les restes humains découverts et identifiés aux périodes de l'âge du fer et aux niveaux médiévaux de Değirmentepe. L'époque chalcolithique de cet ancien village est caractérisée par des maisons rectangulaires en briques de boue qui communiquent les unes avec les autres. On y constate l’apparition d'animaux domestiques comme les chiens, les moutons, les chèvres, les porcs et les bovins qu'au début du Chalcolithique. L'orge, le blé, l'avoine et les pois étaient les plantes les plus fréquemment cultivées. Beaucoup de poteries caractéristiques de la culture Obeid, ont été trouvées sur le site. Les archéologues y ont découvert 450 scellements qui témoignent de la présence de notables capables de gérer les productions. (fr)
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