Die glazialen Übertiefungen im Saalachgletscher-Gebiet zwischen Inzell und Königssee

Kurt Bader
By combining the two geophysical methods, refraction seismic (with small explosions) and geoelectrical sounding, shape and fill of glacial eroded valleys can be researched. Especially with the help of the seismic velocities the quaternary fill can be divided in glacial consolidated and not consolidated sediments, and thereby the scale of the Würm glacial depth erosion be compared with that of the preceeding ice ages. Again it is stated, that the Würm glaciers mostly eroded only...