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Administrative boundary Switzerland - INSPIRE
Administrative boundary is a sub layer of Administrative units and is based on the data set swissBOUNDARIES3D by swisstopo. It contains all administrative units and national bou...
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Administrative units Switzerland - INSPIRE
Administrative units is based on the data set swissBOUNDARIES3D by swisstopo. It contains all administrative units and national boundaries of Switzerland and the Principality of...
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Official index of cities and towns including postal codes and perimeter
In Article 24 of the regulations governing geographic names (GeoNV), the Federal Office of Topography (swisstopo) is commissioned to establish, administer and publish the new of...
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Transition of reference frames LV03 - LV95: Coordinate changes LV03->LV95
The coordinate changes between the old frame of reference LV03 and the new one LV95, respectively the deformations from MN03, are represented in relation to Zimmerwald (BE): the...
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Lithological-petrographic map of Switzerland – Genesis 1:500000
The 1:500'000 geotechnical map (GK500) of the Georesources Switzerland Group shows the subsurface strata classified according to lithological-petrographic criteria. The legend i...
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Lithological-petrographic map of Switzerland – Classification of rocks 1:500000
The 1:500,000 geotechnical map (GK500) of the Georesources Switzerland Group shows the subsurface strata classified according to lithological-petrographic criteria. The legend i...
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Switzerland During the Last Glacial Maximum (LGM) 1:500000 (vector map)
The map (GK500-LGM) shows the maximum extent of glaciation in Switzerland at the height of the last Ice Age around 24,000 years ago. It presents the latest results of current re...
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Natural stones on buildings
This dataset shows the use of stone in the construction of over 4,000 buildings in Switzerland. The data was collected by Francis de Quervain between 1954 and 1983. Over the pas...
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Inclination Map of Switzerland 1:500000
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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Geoid model CHGeo2004 in ETRS89
Swiss geoid model in the version of 2004 (CHGeo2004) in the reference system ETRS89. It forms the zero reference surface (approximated mean sea level) for height determination a...
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Geoid model CHGeo2004 in CH1903
Swiss geoid model in the version of 2004 (CHGeo2004) in the reference system CH1903. It forms the zero reference surface (approximated mean sea level) for height determination a...
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Simplified map of the near-surface mineral resources of Switzerland 1:500'000
The map of near-surface mineral resources of Switzerland 1:500'000 (GK500) of the Georesources Switzerland Group shows the subsurface strata classified according to lithological...
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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...
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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...
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Geothermal Map of Switzerland 1:500000
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. The heat itself is released in the Earth...
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Aeromagnetic Map of Switzerland 1:500000
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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Declination Map of Switzerland 1:500000
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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Aeromagnetic Map of the Swiss Plateau and the Jura Mountains
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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Transition of reference frames LV03 - LV95: Triangular network (CHENyx06 and ...
The triangular network of the national survey (FINELTRA-LV) was completed in the 90's and has permitted to transform geodata from LV03 to LV95 and vice versa with an accuracy of...
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Switzerland During the Last Glacial Maximum (LGM) 1:500000
The map (GK500-LGM) shows the maximum extent of glaciation in Switzerland at the height of the last Ice Age around 24,000 years ago. It presents the latest results of current re...
- SERVICE
- WMS
- WMTS