Blown sand movements at Kiskunhalas on the Danube-Tisza interfluve, Hungary
The largest blown-sand area of Hungary is located on the DanubeTisza Interfluve. Here the most significant aeolian activity took place during the Pleistocene, however the aeolian transformation of the landscape occurred also in the Holocene and even in historical times. The aims of the study were (1...
Elmentve itt :
| Szerzők: | |
|---|---|
| Dokumentumtípus: | Cikk |
| Megjelent: |
2009
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| Sorozat: | Journal of environmental geography
2 No. 3-4 |
| Kulcsszavak: | Éghajlati változás - Magyarország - regionális |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/5910 |