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Old and Young Drift are geographic names given to the morainic landscapes that were formed in Central Europe; the Old Drift during the older ice ages and the Young Drift during the latest glaciations – the Weichselian in North Germany and the Würm in the Alps. Their landforms are quite different. Areas of Old Drift have been heavily flattened and…
Regions, Old Drift & Young Drift
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old drift young glacial landforms areas landscapes formed less ice central europe whilst moraines morainic heavily result processes ablation accumulation
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| denudation | instance of | Areas of Old Drift have been heavily flattened and transformed as a result of geomorphic processes | 0.80 | text |
| erosion | instance of | Areas of Old Drift have been heavily flattened and transformed as a result of geomorphic processes | 0.80 | text |
| whilst areas of Young Drift have largely retained their original shape | instance of | Areas of Old Drift have been heavily flattened and transformed as a result of geomorphic processes | 0.80 | text |
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