Dr. Jami Lockhart and Tim Mulvihill collecting data using the gradiometers.
Dr. Jami Lockhart and Tim Mulvihill collecting data using the gradiometers.

Tim Mulvihill, UAFS Research Station

During early January of 2017, archeologists (Tim Mulvihill, Dr. Jami Lockhart and Dr. George Sabo) from the Arkansas Archeological Survey conducted a geophysical survey (remote sensing) of a Late Woodland site in the Arkansas River Valley. The site was originally researched during the 1960’s, but no work had been done there since. A new contour map of the site was completed and forty-seven 20m x 20m units were then established to collect the data. At this point, only magnetometry data was collected using two Bartington 601-2 gradiometers. Magnetometry is a passive technology that measures very small variations in the earth’s natural magnetic properties.  Soils that have been disturbed reflect a change in this natural magnetic alignment.  Likewise, materials that have fired have a measurably different magnetic signature than their surroundings. This technology works well to identify prehistoric features.  In addition, the survey grids were georeferenced by Michael Evans using a Trimble Geo7X GNSS. Initial results were promising. Multiple anomalies identify the site area and some may even represent structures. A low mound on the property is also quite apparent in the geophysical data. We hope to conduct further geophysical work at the site in the future using other technologies.
Dr. Jami Lockhart running the gradiometer.
Dr. Jami Lockhart running the gradiometer.
Gradiometry data from the site. Darker areas indicate increased magnetism.
Gradiometry data from the site. Darker areas indicate increased magnetism.
Michael Evans using the Trimble Geo7X to georeference the grid.
Michael Evans using the Trimble Geo7X to georeference the grid.
Getting ready to conduct geophysical survey.
Getting ready to conduct geophysical survey.