Title variants
Palaeogeographical Background of Development of the Valley in the Załęcze Warta River Bend (Wieluń Upland)
Languages of publication
Abstracts
The author describes the relief and geological structure of the Warta valley in its river gap across the Wieluń Upland, being 43 km long. There is underlined an interesting geological history of this area reflected in the fluvia land karst relief and in
a complicated system of under ground and surface water circulation
(for summary see page 176-178).
a complicated system of under ground and surface water circulation
(for summary see page 176-178).
Keywords
Publisher
Year
Volume
Physical description
Dates
published
1986
Contributors
author
other
References
Document Type
Publication order reference
Identifiers
URI
http://hdl.handle.net/11089/15925
YADDA identifier
bwmeta1.element.hdl_11089_15925