# Dobecki 1992: Seismic investigations in the vicinity of the Great Sphinx of Giza, Egypt

> Thomas L. Dobecki, Robert M. Schoch, 1992. 8 records on Mysteries Department cite it. The one peer-reviewed publication of the redating camp's field data.

Source: https://mysteriesdept.com/sources/SRC0CTWRWCE2JAW/seismic-investigations-in-the-vicinity-of-the-great-sphinx  
Publisher: Mysteries Department  
Licence: CC BY 4.0 (credit Mysteries Department and link the page)  

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[Sources](https://mysteriesdept.com/sources)[Great Sphinx of Giza](https://mysteriesdept.com/mysteries/great-sphinx)Dobecki 1992

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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.

**Great Sphinx of Giza** Articledoi: **[10.1002/gea.3340070603](https://doi.org/10.1002/gea.3340070603)** Checked against the original0

## 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 low-velocity layer is subsurface weathering whose depth is proportional to exposure time, and the thinner…](https://mysteriesdept.com/mysteries/great-sphinx/answers/ANS0CTWSREW6Q63/the-low-velocity-layer-is-subsurface-weathering-whose-depth)

Answer

ANS

[Seismic refraction profiles around the Sphinx (Dobecki and Schoch, April 1991)](https://mysteriesdept.com/datasets/DAT0CTWSZ1T0EZE/seismic-refraction-profiles-around-the-sphinx-dobecki-and)

Dataset

DAT

[Schoch and Dobecki report a low-velocity weathered layer beneath the ditch floor, 1.8 to 2.5 m on the front…](https://mysteriesdept.com/mysteries/great-sphinx/evidence/EVD0CTWSHVY4PV6/schoch-and-dobecki-report-a-low-velocity-weathered-layer)

Evidence

EVD

[The 1991 refraction lines found a 1.8 to 2.5 m weathered layer on the front and sides and 1.2 m at the rear.](https://mysteriesdept.com/mysteries/great-sphinx/evidence/EVD0CTWSRPP41GH/the-1991-refraction-lines-found-a-1-8-to-2-5-m-weathered)

Evidence

EVD

[Schoch and West present the rain-erosion redating; Dobecki and Schoch publish the seismic survey in 1992](https://mysteriesdept.com/mysteries/great-sphinx/events/EVT0CTWSAHJ2AT6/schoch-and-west-present-the-rain-erosion-redating-dobecki)

EVT

[The Great Sphinx of Giza](https://mysteriesdept.com/mysteries/great-sphinx)

The mystery article

MYS

[Does the weathered layer under the ditch floor measure how long each part has been exposed?](https://mysteriesdept.com/mysteries/great-sphinx/questions/QST0CTWSD7G59TK/does-the-weathered-layer-under-the-ditch-floor-measure-how)

Question

QST

[What explains the weathering of the body and the enclosure walls?](https://mysteriesdept.com/mysteries/great-sphinx/questions/QST0CTWSCZP7K5T/what-explains-the-weathering-of-the-body-and-the-enclosure)

Question

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
```

[Find it at doi.org](https://doi.org/10.1002/gea.3340070603)

Key

**SRC** 0CTWRWCE2JAW

Kind

Journal article

Rights

The publisher's

Checked

Against the published article

Added by

[apollo](https://mysteriesdept.com/u/apollo)

The record

Bibliographic records are CC0. Take this one as CSL-JSON, BibTeX or RIS.

[CSL-JSON](https://mysteriesdept.com/sources/SRC0CTWRWCE2JAW/seismic-investigations-in-the-vicinity-of-the-great-sphinx/csl.json)
