Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden, to Washington Headquarters Services, Directorate for information Operations and Reports, 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302, and Geonics EM61 cart, MTADS EM61 and EM-63 cart data from Camp Sibert were investigated to determine if the number of "can't analyze" anomalies could be reduced and more objective stop-digging criteria selected. Many of the "can't analyze" anomalies in the MTADS EM61 were caused by cart-bounce along North-South transects and could be avoided by using only East-West transect data. However, poor data coverage increased the chances of generating false negative declarations. If North-South transects are retained, sensor motion relative to the ground can cause difficulties in obtaining good model fits to the data. A modeling framework developed elsewhere was used to determine if an anomaly was caused by sensor motion or a compact metallic target. The method has promise but had limited applicability due to the lack of accurate ground-clearance and topographic data. To determine an objective operating point, the training data must be representative of the test-data. In particular, outliers need to be avoided and here this was achieved by using multiple feature vectors, obtained by analysis of a depth versus misfit curve, in the classification. Using this technique a false-negative in the EM-63 data could be avoided. We investigated the cause of the can't analyze anomalies of geological origin whose amplitude exceeded 25 mV along the E-W transects. We hypothesized that many of these anomalies were due to sensor movement relative to ground. The background response was modeled by estimating a ground clearance from the elevation data and assuming that the background magnetic susceptibility was uniform in each cell. The accuracy of our modeling was limited due to filtering artifacts in the observed data, the accuracy of the ground clearance estimate, and small scale topography (i.e. depressions and bumps on the surface that would affect the measured data).In many cases we found that small scale anomalies could be predicted using our modeling techniques and that sensor movement was indeed the likely cause. We also found that there were a number of metallic anomalies whose response could not be properly modeled due to variations in the signal from the background due to sensor movement. There were also several anomalies that were caused by longer wavelength spatial variations in magnetic soil properties that were not suppressed by the detrend filters that were used to pre-process the sensor data. We conclude that sensor movement relative to th...