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