BUFFALO, N.Y. -- For centuries, trowels and handpicks have been traditional tools of the trade for archeologists, but a University at Buffalo geophysicist who has been working at an archeological site in Jordan is proposing that some decidedly 21st-century technologies, like tablet PCs equipped with fancy navigational software, ought to be standard gear as well.

"Non-invasive geophysical techniques, which allow researchers to image what's under the ground without digging, and real-time differential Global Positioning Satellite (GPS) technology, which provides resolution and accuracy to within a meter, can provide archeological teams with significant benefits," said Gregory S. Baker, Ph.D., associate professor of geology in UB's College of Arts and Sciences.

By helping archeological teams target with greater accuracy where an excavation will provide the greatest archeological "payoff," the integration of both of these techniques on a commonly available -- and portable -- platform like the tablet PC, could save them time and money, he added.

This past summer, Baker successfully used these techniques at the excavation, led by John Oleson, Ph.D., of the University of Victoria, of an ancient Roman fort in southern Jordan.

Baker said it's an example of how geophysical techniques used to image subsurface features non-invasively can prove critical in helping archeologists determine where to start excavating to find suspected features.

He has submitted a proposal on this methodology, which he calls "synergistic archeogeophysics," to the National Science Foundation.

Typically, Baker explained, after the geophysical data are collected and processed, archeologists view them on a computer screen, then try to locate the suspected subsurface features in the field.

"The trouble lies in translating the geophysical images we collect into something that is truly useful to archeologists," said Baker.

"Right now, it's pretty archaic," he said. "An archeologist will try to locate a feature in the field using a tape measure and a printout of the geophysical data."

This past summer, Baker applied real-time differential GPS to the Jordanian project.

Archeologists at the Jordanian site are looking for evidence that the Roman fort may have included a large kiln site, indicating that as the Romans moved into a new area and conquered territory, they established a local means for producing pottery.

"There's tremendous interest in whether or not there was a large-scale kiln area at this site," said Baker, noting that the fort is one of the few examples in Jordan of an ancient Roman military installation.

"We were looking for a magnetic signal under the surface because once you heat earth past the Curie temperature, as would be the case during the firing process, it acquires a permanent magnetic signal that persists even today," he said.

Using magnetometers, Baker, along with Heather Ambrose, a master's-degree candidate in the UB Department of Geology, and Scott Gagliardi, an undergraduate geology major, surveyed the area in an effort to identify subsurface areas with magnetic signatures.

They found some localized "hot spots," which Baker said "have a pretty high likelihood of indicating there's a kiln there.

"Since we collected the magnetics data with real-time differential GPS, we were able then to come back to the archeologists, show them the images and give them the exact latitude and longitude coordinates," said Baker.

"When they returned to the field, they were able to locate these coordinates to within one meter, even though this was the middle of the desert and there were no landmarks to assist them," he said.

If the archeologists had not used the real-time differential GPS, Baker said the best they could have hoped for would have been to pinpoint coordinates to within 20-30 meters, which would have made finding the "hot spots" practically impossible.

The archeologists now are excavating up to three meters below the earth's surface, which is where Baker's data indicates they should find the kiln.

Baker's research at the site is funded by the National Science Foundation.

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