A GEOPHYSICAL INVESTIGATION OF THE FORT LA PRESENTATION ARCHAEOLOGICAL SITE, OGDENSBURG, NY
Seismic, electrical resistivity and magnetic traverses were conducted to locate the remnants of the fort. These remnants include the wall, foundation and cornerstones. The seismic refraction survey indicated about 30' (10 meters) of glacial till overlying the Ogdensburg dolostone bedrock. Vertical electrical sounding (VES) at the site indicates 6' of high resistivity sand overlying a low resistivity material, probably clay.
The magnetic profiles indicated several magnetic anomalies with magnitudes of 2000 nanotesla and steep magnetic gradient. Normally magnetic anomalies of this magnitude are due to Precambrian basement rock however, the steep gradients indicate a depth of about 2 meters placing their source in the overlying glacial till.
Four resistivity profiles were conducted across the site. Resistivity measurements were made at 2 meter intervals and an electrode spacing of 4 meters. The resistivity profiles indicate several resistivity anomalies as high as 200 ohm-meters in the upper 2 meters. In summary, even though the source of the magnetic and resistivity anomalies is unknown, it's possible they are related to some of the remnants at the site.