Finally, the result of groundwater potential map derived from belief map was validated using testing data.
The burn probability map was validated using historical records of burned patches.
The groundwater recharging map was validated with the measured electrical conductivity (EC) values in the groundwater of the study area.
Finally, groundwater potential zone map is validated using average groundwater level data from 32 wells scattered over the study area.
Thus prepared map was validated with the landslides dataset and an acceptable model was developed, which could better represent the landslide susceptibility condition in the study area.
A "robustness map" is created using simulations results of a 6-degree-of-freedom (6-DOF) system, and such a map is validated by two more complicated models.
The predicted map was validated by independent experimental studies on hypoeutectic Al Si alloys and it is in perfect agreement with microstructure observation and undercooling measurements.
Accordingly, the final landslide susceptibility map was validated using known landslide locations (Yilmaz, 2010).
The C × E generated genetic map was validated aligning the sequence based markers along the draft scaffold/pseudo-molecules available from the PGSC website [ 25].
The quality of this physical map was validated, but it could still benefit from better computational tools for identifying Q-clones.
