A pliocene cliff-line around the Giza Pyramids Plateau, Egypt

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Dateien:
Aufrufstatistik

URI: http://nbn-resolving.de/urn:nbn:de:bsz:21-opus-38567
http://hdl.handle.net/10900/49278
Dokumentart: (wissenschaftlicher) Artikel
Date: 1982
Language: English
Faculty: 7 Mathematisch-Naturwissenschaftliche Fakultät
Department: Geographie, Geoökologie, Geowissenschaft
DDC Classifikation: 550 - Earth sciences
Keywords: Pyramide
Other Keywords:
Giza , Pyramids , Plateau
License: Publishing license excluding print on demand
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Abstract:

Aigner, T., 1983. A Pliocene cliff-line around the Giza Pyramids Plateau, Egypt. Palaeogeogr., Palaeoclimatol., Palaeoecol., 4 2 : 313—322. Escarpments bordering the Giza Pyramids Plateau represent the cliff-line of a Pliocene transgression up the pre-Nile ("Eonile") Valley. Geomorphologically, a limestone cliff can be distinguished from a slip-block shore associated with a distinct fining-up sequence. Differences in bedrock lithology and in structure (Joint pattern, faults) are morphogenetic Controls. The pre-Pliocene morphology with escarpments that allowed the development of later cliff-lines is related to deep incision of the Eonile drainage system caused by the desiccation of the Mediterranean Sea during the Messinian.

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