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Archeology for Interpreters > 4. What Do Archeologists Do?

How do archeologists know where to look for sites?

Archeologists may use non-invasive techniques to initially characterize a site or part of a site.

Geophysical prospecting

[photo] Emerald Mound, the second largest ceremonial mound 
                in the United States. (NPS)

Aerial photograph of Emerald Mound. (NPS)

Geophysical prospecting is the use of high-resolution geophysical methods to discover archeological sites. These methods may also be called “remote sensing” or “archeogeophysics”. Advantages to geophysical methods are that they are nondestructive and provide rapid reconnaissance. Their major limitation is that they use non-contact techniques. The best they can do is detect anomalies, which archeologists must then investigate directly to interpret. These methods are also instrument-intensive and initially expensive (see Bevan 1998.)

Remote sensing identifies archeological features buried below ground that still leave their mark on the landscape. Shallow ground occurs over buried features such as buildings, walls, and streets; deeper ground is found within pits and ditches. These variations in depth affect the growth of plants and soil color-producing patterns that are usually only visible from above (McIntosh 1999:44). Common remote scanning methods include:

Aerial photography is the simplest of all the remote sensing techniques. It only requires a camera and a way to get it airborne, above the potential archeological site. Variations within the site that would have been totally unnoticed from the ground become obvious from a higher vantagepoint. Hot air balloons, airplanes, helicopters, and tethered blimps are all ways of getting these kinds of pictures.

Electrical resistivity is the most flexible and most generally useful technique for a wide variety of sites and is the best method to control or adjust the depth of investigation. Electrical resistivity methods are noninvasive. A resistivity meter measures the difficulty of pushing electricity through the soil—more resistance requires more voltage. The soil's actual ability to conduct the current comes from the amount of moisture it holds. Compacted areas, such as floors and trails, restrict the amount of moisture that the soil can hold, and will show up as being highly resistive during this test. Places where the soil has been disturbed, such as filled holes, trenches, and ditches, will collect more moisture than surrounding soil and will show up on the test as having low resistivity.

Flags 
                mark where archeologists using metal detectors located buried 
                artifacts at Little Bighorn Battlefield National Monument. (Midwest 
                Archeological Center, NPS)

Flags mark where metal detectors located buried artifacts at Little Bighorn Battlefield National Monument. (Midwest Archeological Center, NPS)

Electromagnetic (EM) surveys detect metals (ferrous and nonferrous) and changes in soil conductivity that may be related to moisture or chemical content. Current is induced into the ground and electrical conductivity is measured. Conductivity is the opposite of resistivity. The advantage over resistivity is that resistivity meters must make contact with the ground, while EM meters do not need to. Conductivity is most easily read in saturated soils.

Metal detectors operate using conductivity. Although often used in illegal and unethical artifact prospecting, metal detectors do have legitimate archeological uses. Metal detectors are electromagnetic devices that work at low frequencies. They are effective to the depth that is approximately the width of the search coil. Depth also depends on the size and orientation of the buried object and the amount of corrosion.

Ground Penetrating Radar (GPR) is commonly used in archeology to make accurate site maps and get an overall picture of the subsurface. GPR uses low-power radio waves to detect changes in density in the subsurface layers and locate buried objects. It is best to combine GPR with other methods such as EM, resistivity, and magnetometry to ensure wide coverage. GPR, like most remote sensing, is not very effective in urban settings because of interference from buildings, power lines, cars, and other objects.

An 
                archeologist uses a magnetometer at the Presidio of San Francisco, 
                Golden Gate National Recreation Area (NPS)

An archeologist uses a magnetometer at the Presidio of San Francisco, Golden Gate National Recreation Area (NPS)

Magnetic prospecting is useful and fairly inexpensive. Objects buried underground or in different ground layer densities will create small disturbances in the earth's natural magnetic field where they focus the magnetic flow into a stronger field. If an object is more permeable than the soil (which has magnetic properties), then the magnetic field will be stronger through that object. A magnetometer, also referred to as a gradiometer or proton magnetometer, measures how these variations in the Earth's magnetic field affect the protons of the subsurface objects.

Fun fact

NASA flew its remote sensing device Thermal Infrared Multispectral Scanner (TIMS) over Chaco Canyon, New Mexico. By measuring temperature differences on the ground, TIMS detected prehistoric roads from AD 900 or 1000.

Case study

An Analysis of Magnetic Gradiometer Surveys at the Fort Clastop National Memorial
Read about a magnetic survey of the site of Fort Clatsop, Oregon erected by Lewis and Clark in 1805.

NPS Archeologists Assist in Locating Graves at Vicksburg National Cemetery
Archeologists at Vicksburg used noninvasive survey to locate unmarked and unrecorded burials. In combination with historical records, some individuals were identified.

TSM/MJB