ABSTRACT 



Magnetic elements observed with a Vector Airborne iVlagne- 

 tometer, under Loran-C control, are used to calculate the 

 directional components for the anomaly associated with 

 Piantagenet Bank. Also determined are the total intensity, 

 inclination, and declination of the anomalous magnetic field. 

 A theoretical source body is presented as a possible solution 

 to the Piantagenet Bank anomaly. 



