Imaging Islamic architecture in the multileveled archaeological settlement of Tell Dibgou, Northeast Nile Delta, Egypt

Author:

Ibrahim Amin1,Senosy Mahmoud M2,El-Khadragy Ali3,Saada Saada Ahmed4,Abdelrahman Kamal5,Alarifi Saad S5ORCID,Mickus Kevin6

Affiliation:

1. Zagazig University, Environmental Geophysics Lab (ZEGL), Geology Department, Faculty of Science , 44519 Zagazig , Egypt

2. Geology Department, Faculty of Science, Assiut University , 71515 Assiut , Egypt

3. Geology Department, Faculty of Science, Zagazig University , 44519 Zagazig, Egypt

4. Geology Department, Faculty of Science, Suez University , 43518 Suez, Egypt

5. Department of Geology and Geophysics, College of Science, King Saud University , 11451 Riyadh , Saudi Arabia

6. Department of Geology, Missouri State University , Springfield, MO, 65897 , USA

Abstract

Abstract Tell Dibgou, northeastern Nile Delta (Egypt), is a typical type of complex archaeological site that contains ruins from different chronological periods (Pharaonic, Byzantine, Greece-Roman and Islamic), as evidenced by the findings of pottery kilns, pottery shards, fired brick and colored glass. This study aims to image the topmost archaeological layer of Islamic architecture using electrical resistivity tomography and land-based magnetic surveys. Two nearby areas in the northern part of Tell Dibgou were investigated; the first was surveyed using resistivity tomography and magnetics, and the second used total-field and vertical magnetic gradients. Several electrode arrays (dipole–dipole, Wenner Beta, Wenner Schlumberger and pole–dipole) were tested to select the one that provides better resolution. Two inversion schemes were applied where the smoothness-constrained inversion smeared and blurred the archaeological boundaries, and the robust inversion produced models with well-defined and sharp edges. The vertical extent of the topmost archaeological layer of Islamic settlers was imaged using the electrical resistivity tomography; however, the presence of slag debris, collapsed bricks, and pottery shards at shallow depths complicated the discrimination of the closest walls. The interpretation of magnetic data (total and vertical gradients) in terms of depth and geometry was executed using semi-automated techniques such as three-dimensional, Euler deconvolution and tilt angle derivative. The geometry of archaeological targets is interpreted to be closed rooms, water tanks and corridors constructed from fired brick walls filled with clay sediments. The depths yielded from both techniques are comparable and range from >1 m to up to 2 m.

Publisher

Oxford University Press (OUP)

Subject

Management, Monitoring, Policy and Law,Industrial and Manufacturing Engineering,Geology,Geophysics

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