What can we learn from geoarchaeology?

Geoarchaeological Techniques

Researchers currently use a variety of geoarchaeological techniques to to explore hidden sites and examine buried artifacts without conducting a major excavation. For example, a simple soil auger, which uses sharp blades attached to a hollow cylinder to drill into the earth, can reveal a great deal about sediments lying beneath the surface. Most augers bore small holes and reach depths of 26 feet (8 meters). Scientists analyze the soil samples removed by augers to detect archaeological deposits and determine how far they extend laterally. Once their probing finds evidence of promising deposits, researchers can begin a more significant excavation.

Remote-sensing technologies offer geoarchaeologists more sophisticated options to find hidden sites. For example, ground-penetrating radar uses low-frequency waves to produce an image of deeply buried artifacts and features. These waves penetrate to depths of 33 feet (10 meters), and as they encounter various deposits or remains, they produce an echo that helps to define boundaries and object shapes. The deeper the material, the longer it takes the echo to travel back to the surface. This indicates the depth of the material.

When digging finally begins, geoarchaeologists often spend much of their time "reading" the soil for clues. One major goal of this process is creating landscape histories of a specific geographic region. A landscape history answers key questions about an ancient environment. Did sea levels rise? Did rivers overflow their banks? Did a volcano erupt nearby? The answers are held in how soils are deposited. For example, the presence of dark soil layers indicates buried topsoils. Because topsoils take a while to form, they usually indicate a stable landscape -- and a place where an ancient settlement may have been located. By the same token, areas of sediment erosion and storage provide telltale signs of how a river changed its course over time.

Piecing together a landscape history enables scientists to predict where buried cultural deposits are likely to occur. In the Great Plains, archaeologists used these techniques to make a startling discovery about early Americans. Until recently, most anthropologists believed that ancient humans crossed the Bering land bridge about 11,500 years ago and began migrating across North America. But landscape histories in Iowa and Kansas have led to excavations revealing much older sites and indicating that humans settled the continent earlier than expected.

Ultimately, this is what geoarchaeology provides -- a richer and more detailed story to accompany an excavation. Scientists call this story archaeological context, and they rely on it to interpret artifacts, understand their meaning and tell the nearly 200,000-year history of humans.

Related HowStuffWorks Articles


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  • Artz, Joe Alan. "Geoarchaeology in Iowa." The University of Iowa Office of the State Archaeologist. (Aug. 29, 2010)http://www.uiowa.edu/~osa/geo/geo.htm
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