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II.—On the Glaciation of the Navis Valley in North Tirol
Published online by Cambridge University Press: 01 May 2009
Extract
In a previous paper it was shown that one prominent topographical feature of the Tarntal district, the great cirque called the ‘Grübl’,. could be explained as the effect of erosion by a short icetongue which formed when the snow-line persisted for a time at about 2400 metres above sea-level. The basin-shaped hollow of the Upper Tarntal was held to be due to another stand of the snow-limit at 2650 metres. It remains to be seen whether these conclusions are supported by evidence of a similar nature collected over a wider area.
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References
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page 248 note 2 Only the simplest form is here described. For details and figures see Max Eckert, “Das Gottesacker, ein Karrenfeld im Allgäu ”: Wiss. Ergänzungsheft zur Zeitschritt der D. und Ö. Alpenverein.
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