Abstract
BOHEMIA is an excellent region for radio-geological investigation. In the first place, we have the ore region of Jáchymov (Joachimsthal), where pitch-blende is found. However, in the Krkonoˇe (Riesen Gebirge) and in the Jizera Mts., where there are no deposits of pitch-blende, strong radioactive springs (containing up to 200 Mache units) occur very frequently along faults, contacts, etc. This district has been investigated by us radio-geologically in the same manner as that in which Genser investigated the German portion of the Krušné Hory (Erz Gebirge)1.
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References
Geol. Rundschau, 182; 1932.
Bounck-Santholzer, Garlands Beiträdge z. Geophys., 33, 60; 1931.
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SANTHOLZER, W., ULRICH, F. Radio-Geological Survey of Czechoslovakia. Nature 133, 461 (1934). https://doi.org/10.1038/133461a0
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DOI: https://doi.org/10.1038/133461a0
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