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Gravimetric Map of Switzerland (Isostatic Anomalies) 1:500000
Regions and cities, Environment
There is no description for this dataset
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Inclination Map of Switzerland 1:500000
Regions and cities, Environment
Geomagnetic maps are the result of measurements of total intensity, declination and inclination. The inclination is the angle formed by the orientation of the magnetic field rel...
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Geothermal Map of Switzerland 1:500000
Regions and cities, Environment
The geothermal map shows the thermal energy that is produced in the subsurface and traverses the Earth's surface within an area of 1 m2 (mW/m2). The heat flow data is calculated...
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Aeromagnetic Map of the Swiss Plateau and the Jura Mountains
Regions and cities, Environment
The overall magnetisation of a rock consists of induced magnetisation caused by the Earth's magnetic field and of remanent magnetisation acquired by the rock during its formatio...
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Gravimetric Map of Switzerland (Bouguer Anomalies) 1:500000
Regions and cities, Environment
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...
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Declination Map of Switzerland 1:500000
Regions and cities, Environment
Geomagnetic maps are the result of measurements of total intensity, declination and inclination. The declination describes the angle formed between magnetic and geographic north...
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Total Intensity Map of Switzerland 1:500000
Regions and cities, Environment
Geomagnetic maps are the result of measurements of total intensity, declination and inclination. The geomagnetic field is defined by a vector, which isrepresented in terms of it...
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Aeromagnetic Map of Switzerland 1:500000
Regions and cities, Environment
The overall magnetisation of a rock consists of induced magnetisation caused by the Earth's magnetic field and of remanent magnetisation acquired by the rock during its formatio...
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Gravimetric Map of Switzerland (Isostatic Anomalies) 1:500000
Regions and cities, Environment
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...