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Gravimetric Map of Switzerland (Bouguer Anomalies) 1:500000
Gravitational acceleration or gravity depends on the location of the measuring point and the mass distribution in the subsurface structure. A Bouguer anomaly is the difference b...
- SERVICE
- WMS
- API
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Gravimetric Map of Switzerland (Isostatic Anomalies) 1:500000
Isostatic anomalies can be deduced using the Pratt or Airy hypothesis. These anomalies correspond to the static flotation of the Earth’s crust in the upper mantle. The deviation...
- SERVICE
- WMS
- API
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GeoMaps 500 Vector
Six «GeoMaps» at 1:500000 scale give a broad overview of the composition and major features of the underlying structure of Switzerland. The geological map provides an overview o...
- HTML
- WMS
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GeoMaps 500 Raster
Six «GeoMaps» at 1:500000 scale give a broad overview of the composition and major features of the underlying structure of Switzerland. The geological map provides an overview o...
- HTML
- WMS
-
GeoMaps 500 Raster
Six «GeoMaps» at 1:500000 scale give a broad overview of the composition and major features of the underlying structure of Switzerland. The geological map provides an overview o...
- HTML
- WMS
-
Gravimetric Map of Switzerland (Isostatic Anomalies) 1:500000
Isostatic anomalies can be deduced using the Pratt or Airy hypothesis. These anomalies correspond to the static flotation of the Earth’s crust in the upper mantle. The deviation...
- SERVICE
- WMS
- API
-
Gravimetric Map of Switzerland (Bouguer Anomalies) 1:500000
Gravitational acceleration or gravity depends on the location of the measuring point and the mass distribution in the subsurface structure. A Bouguer anomaly is the difference b...
- SERVICE
- WMS
- API
-
GeoMaps 500 Vector
Six «GeoMaps» at 1:500000 scale give a broad overview of the composition and major features of the underlying structure of Switzerland. The geological map provides an overview o...
- HTML
- WMS