Ground anomaly detection in VeldScan means finding places where independent sensors agree something is unusual — vegetation, radar, thermal, relief, and mineral spectral cues — then ranking those spots for your field check.
Rain can green a patch of grass. Fertilizer can stress another. One layer alone is noisy. When several independent signals align on the same geometry, the candidate becomes more interesting — still not a confirmation.
Outputs you get
Shape, size, and heading estimates
Agreement percentage across layers
Working hypotheses (wall, track, channel, void suspicion, human disturbance)
Walk plan / grid for detector work
Export to PDF, KML, or GPX for offline use
Typical scan size
About 10×10 m to 120×120 m. Larger parcels dilute thermal and radar pixels into averages; VeldScan is built for focused field parcels, not country-scale mapping.