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Seismic investigations in the vicinity of the Great Sphinx of Giza, Egypt
Thomas L. Dobecki, Robert M. Schoch, 1992. Geoarchaeology 7(6): 527-544.
Seismic refraction profiles around the Sphinx reporting a weathered low-velocity layer beneath the ditch floor, deeper on the sides and front than at the rear, read by Schoch as evidence of long exposure.
What it's used for here
The one peer-reviewed publication of the redating camp's field data.
Cited by on this site 8 records
The Great Sphinx of Giza
MYSThe mystery article
QST
Cite it
Dobecki, T. L., & Schoch, R. M. (1992). Seismic investigations in the vicinity of the Great Sphinx of Giza, Egypt. Geoarchaeology 7(6): 527-544. https://doi.org/10.1002/gea.3340070603
@article{dobecki1992seismic,
author = {Dobecki, Thomas L. and Schoch, Robert M.},
title = {Seismic investigations in the vicinity of the Great Sphinx of Giza, Egypt},
journal = {Geoarchaeology 7(6): 527-544},
year = {1992},
doi = {10.1002/gea.3340070603},
url = {https://doi.org/10.1002/gea.3340070603}
}TY - JOUR TI - Seismic investigations in the vicinity of the Great Sphinx of Giza, Egypt AU - Dobecki, Thomas L. AU - Schoch, Robert M. PY - 1992 JO - Geoarchaeology 7(6): 527-544 DO - 10.1002/gea.3340070603 UR - https://doi.org/10.1002/gea.3340070603 ER -
Dobecki, Thomas L. and Robert M. Schoch. “Seismic investigations in the vicinity of the Great Sphinx of Giza, Egypt.” Geoarchaeology 7(6): 527-544 (1992). https://doi.org/10.1002/gea.3340070603.