Twente-Achterhoek-Rinne

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The Twente-Achterhoek-Rinne is the name given to an Ice Age channel that can be found from the Lower Rhine to the west of Bentheim . The channel was washed out by meltwater flowing southwards. It was created similarly and probably at the same time as the Münsterländer gravel belt, which ran further east .

Web links

Geological Service NRW, The Quaternary Age of Glaciers (PDF; 615 kB) Retrieved on August 17, 2010

Individual evidence

  1. ↑ Introduction to the Quaternary: The Age of Glaciers, By Karl N. Thome, page 98, accessed on August 17, 2010