The Bouguer anomalies in the gravity data are analysed.
2.
The Tajo and Duero basins are elevated and yet show a negative Bouguer anomaly.
3.
At scales between entire mountain ranges and ore bodies, Bouguer anomalies may indicate rock types.
4.
Along the Mediterranean Coast there is a positive Bouguer anomaly due to lithosphere thinned to less than 75 km.
5.
The Bouguer anomaly is a correction of the gravitational data which takes into account the heights of different terrains.
6.
In the Ossa Moena zone and South Portuguese Zone there is a positive Bouguer anomaly, due to higher crustal density.
7.
The Bouguer anomalies usually are negative in the mountains because they involve reducing out the attraction of the mountain mass, by about 100 milligals per kilometre of mountain height.
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