Geomatics adds a spatial memory.
An observation can stay near its image, its elevation, its measurement, its doubt.
Not the point
Data is not the conclusion.
It becomes useful only in friction:
- between a layer and an outcrop;
- between a model and a slope;
- between a measurement and a story that still needs proof.
Tension
Geology keeps the work grounded. Geomatics keeps it possible to return.