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In online forums (such as the Geophysics for Archaeology LinkedIn group and the now-defunct Geoarchaeology Listserv ), a heated debate erupted in 2015: Did the 2013 patch introduce as many problems as it solved?
In the world of archaeological geophysics, few tools have commanded as much respect and niche utility as the ground conductivity meter. For specialists working on large-scale landscape surveys, the term "patch geonics 2013" has become a whispered legend—a reference to a specific software routine, a calibration method, or perhaps a forgotten firmware update that changed how we interpret shallow subsurface features.
The update added support for RASAT , a Turkish Earth Observation Satellite, allowing for automated image correction of 7.5m panchromatic and 15m multispectral imagery.
Geonics revised the theoretical response curves for the EM38’s two coil orientations (vertical dipole for deeper penetration, horizontal dipole for shallow mapping). The patch provided new coefficients specifically for "patch" surveys—small, high-resolution grids (e.g., 20m x 20m) where edge effects previously caused mathematical anomalies.
In online forums (such as the Geophysics for Archaeology LinkedIn group and the now-defunct Geoarchaeology Listserv ), a heated debate erupted in 2015: Did the 2013 patch introduce as many problems as it solved?
In the world of archaeological geophysics, few tools have commanded as much respect and niche utility as the ground conductivity meter. For specialists working on large-scale landscape surveys, the term "patch geonics 2013" has become a whispered legend—a reference to a specific software routine, a calibration method, or perhaps a forgotten firmware update that changed how we interpret shallow subsurface features. patch geonics 2013
The update added support for RASAT , a Turkish Earth Observation Satellite, allowing for automated image correction of 7.5m panchromatic and 15m multispectral imagery. In online forums (such as the Geophysics for
Geonics revised the theoretical response curves for the EM38’s two coil orientations (vertical dipole for deeper penetration, horizontal dipole for shallow mapping). The patch provided new coefficients specifically for "patch" surveys—small, high-resolution grids (e.g., 20m x 20m) where edge effects previously caused mathematical anomalies. The update added support for RASAT , a
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