Die spätwürmeiszeitlichen Stadien auf der schweizerischen Alpennordseite

René Hantke
Investigations on late Würmian readvance stages of the glaciers on the northern slope of the Swiss Alps have shown that correlations can be made between the different glacier systems. The well developed end nioraines of the Zurich stage, 15 to 20 km behind the outermost Würmian moraines, are damming lake basins that had already formed during older ice advances. The next readvance, the Hürden stage, has also been recognized in all glacier systems. End moraines...