د ا رسة تاريخية ولغوية لحادثة الطوفان في بلاد ال ا رفدين. (Arabic)

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  • Additional Information
    • Alternate Title:
      Historical and linguistic study of the event of flood in Mesopotamia. (English)
    • Subject Terms:
      MESOPOTAMIA; PERSIAN Gulf; MIDDLE East
    • Abstract:
      Some civilizations of the ancient Near East have dealt with the flood incident, including the different civilizations of Mesopotamia, especially the Sumerian and Babylonian ones. For the purpose of studying this accident and its geographical extensions within the lands of Mesopotamia, starting from the Persian Gulf and ending in the northernmost part of Mesopotamia, a focus was made on the ancient cities that are compatible with the flood event, as well as studying the geological extensions within the scale of the geological time with finding linguistic interpretations of some of the cuneiform texts and books. As a result, the study concluded that the flood incident started from the Arabian Gulf and extended south of Baghdad. [ABSTRACT FROM AUTHOR]
    • Abstract:
      لقد تناولت بعض الحضا ا رت الشرق الأدنى القديم حادثة الطوفان بما فييا حضا ا رت بلبد ال ا رفدين المختمفة وبالأخص السومرية والبابمية منيا . ولغرض د ا رسة ىذه الحادثة وامتداداتيا الجغ ا رفية ضمن أ ا رضي بلبد ال ا رفدين إبتداء اً من الخميج العربي و انتياءا بأقصى شمالي بلبد ال ا رفدين ، تم التركيز عمى المدن ألقديمة المتوافقة مع حادثة الطوفان وكذلك د ا رسة الامتدادات الجيولوجية ضمن مقياس الزمن الجيولوجي مع ايجاد تفسي ا رت لغوية لبعض ما ورد في النصوص المسمارية والكتب السماوية . ونتيجة لذلك ، فقد توصمت الد ا رسة بأن حادثة الطوفان ابتدأت من ألخميج ألعربي وامتدت إلى جنوبي بغداد . [ABSTRACT FROM AUTHOR]
    • Abstract:
      Copyright of Journal of College of Education / Wasit is the property of Republic of Iraq Ministry of Higher Education & Scientific Research (MOHESR) and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)