Geophysical surveys begins.

This photograph shows Willis Monroe and our driver, Mehmet Tekin, helping with a geophysical surveying on the citadel mound two days ago. We are, in effect, trying to find the western edge of the Bronze Palace before we start the excavations. Our efforts in previous seasons have been entirely concentrated on the eastern part of the building, so we need to expand our explorations.

Resistivity survey on the citadel mound. Mehmet is pouring water into the holes made for the probes in order to overcome contact resistance. This is a serious problem for us because the ground is so dry. It will not rain again until September.

As I mentioned earlier, the Bronze Palace was built, in part, on a thick platform of mudbricks which served as a strong foundation for the building. One clue we have about the location of the western edge of the palace is a steep slope about a meter high and approximately 80m (=240 feet) west of our current excavation area. Since the mudbrick platform should erode more slowly than other materials, it makes sense that this steep erosional escarpment might just be the edge of the platform for the palace.

To test this hypothesis, we are trying to map the ancient subsurface features, like the walls of the palace, using electrical resistivity. This is a geophysical survey technique in which we pass an electrical current underground between two probes. A second set of probes measures the grounds’s resistance to the flow of electricity. Buried walls affect how easily an electrical current flows underground between two points and, if we collect readings systematically along our site grid, we can map them and “see” features below ground without excavating.

The frame that Willis and Mehmet are inserting into the ground holds two of the probes and a long yellow wire connects to two distant probes, some 50m away. These probes create the electrical field and measure the subsurface effects. The box on top of the frame collects the measurements; we have sophisticated mapping software on our field laptop that allows us to convert the resistance readings into a map of subsurface features.

As you can see in the photograph, there is nothing visible on the ground to guide our excavations, so we rely on subsurface geophysics to help us choose the best places to dig.

For any UAkron students who might be reading this post, I will be teaching my Archaeogeophysical Survey course again in the Spring of 2012. It’s a fun class and you never know where it might lead you.

About matney

Dr. Matney is Professor of Archaeology in the Department of Anthropology and Classical Studies at the University of Akron. He is the Director of the Ziyaret Tepe Archaeological Expedition.
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