Last updated
December 31, 1979
Terms of use

Description

Geomagnetic maps are the result of measurements of total intensity, declination and inclination. The declination describes the angle formed between magnetic and geographic north. Because the Earth's magnetic field changes over time, the data in this map always relate to a specific time period. The values can be adapted using correction formulae, which have experimentally determined coefficients. Paper map: G. Fischer & P.-A. Schnegg, 1979 (explanatory text on the back of the map). Vector map: 2001.

Resources

Additional information

Identifier
8f38b25f-f984-450a-ae48-02290e82136c@bundesamt-fur-landestopografie-swisstopo
Issued date
December 31, 1979
Modified date
-
Publisher
Bundesamt für Landestopografie swisstopo
Contact points
milan.beres@swisstopo.ch
Languages
  • English
  • German
  • French
  • Italian
Further information
Landing page
http://www.sgpk.ethz.ch/
Documentation
Temporal coverage
-
Spatial coverage
Landeskarte 1:500'000
Update interval
Continuous
Metadata Access
API (JSON) Download XML

Got questions?

Ask the publisher directly

milan.beres@swisstopo.ch