Jezioro Lake is the only natural lake in southern Poland outside mountainous areas to have existed continuously since the Pleistocene. The record of environmental change in the Late Vistulian (Weichselian) and Holocene is preserved in the deposits and landforms around the lake. This paper presents the results of paleogeographical and paleoecological research that emabled us to reconstruct the history of the Jezioro Lake. At the end of the Vistulian period, the outlet of the lake was blocked by a parabolic dune moving in from the west. Limnic sedimentation was evident in the sediment core at all levels from the Holocene, with remains of Cladocera, Chironomidae larvae, and aquatic plants. The lake did not disappear at that time, although its area decreased by a factor of 12 by the end of the period. Paleobotanical research permitted the reconstruction of sequences of plant communities and changes in nutrient status and water level. An initial oligotrophic lake, as indicated by the presence of Isoe¨tes lacustris L., changed to a eutrophic lake, as indicated by the presence of Potamogeton natans L. and Nuphar sp., then the lake progressed to the present-day dystrophic lake that is surrounded by a swamp. The profile of organic deposits contains a record of environmental change at least since the Younger Dryas in southern Poland.

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Abstract

Poland’s Koźle Basin contains numerous craters created from the explosions of World War II aerial bombs as well as craters left by unexploded ordnance. The state of the local environment has been severely affected. This situation presents an obstacle to spatial management of the land to this day. This research programme studied the distribution of postmilitary anthropogenic geohazards in the area. It was intended to help to indicate the appropriate courses of action, including in the field of spatial planning, in the areas affected by former bombing. Desk studies focused on photo-interpretive analysis of archival aerial photographs and took advantage of the potential of high-resolution shaded relief rasters created from digital terrain models derived from LiDAR scanning. Field studies used classic geomorphological methods. Studies conducted so far in the bombed areas indicate the necessity of carrying out systematic, anticipatory, accurate surveys of the land and soil surface with the use of geophysical methods. Currently, the traces identified in the field suggest that the amount of unexploded ordnance remaining in the ground is very large.

One of the largest territories affected by the aerial bombardment carried out in Europe in 1944 is located near Kędzierzyn-Koźle. Surrounded by former synthetic fuel production plants, it contains craters from the explosions of detonation and general-purpose bombs, as well as smaller craters indicating the existence of unexploded bombs. The research presented in this article was conducted in forested areas and swampy wastelands, where these forms have been preserved until today. The article includes the analysis of their distribution and morphology, as well as characteristic cases occurring in multiple geoenvironmental situations. It also provides a model for research work leading to the determination of the most likely locations of unexploded bombs.

The central part of the Woźniki-Wieluń Upland is characterised by mature old glacial landforms associated with the Middle-Polish Glaciations. In some areas, however, more pronounced post-glacial landforms can be observed that were remodelled by later morphogenetic processes to a lesser extent. To the south-east of Krzepice, in the vicinity of Dolisko, there is an extensive depression in which twelve parallel ridges can be found. In terms of their morphology and location as well as due to their relationship to the surrounding landforms, the ridges examined resemble forms that would be referred to as drumlins, glaciotectonic forms or glacial curvilineations in late glacial areas. The material presented is the result of the initial research stage. The studies conducted in this stage involved primarily geomorphological mapping supplemented by an analysis of landforms on a shaded relief model and on an orthophotomap. At the current stage of studies on the glacigenic landforms in the vicinity of Dolisko, three scenarios concerning their origins have been put forward that need to be verified. The first scenario involves glaciotectonic origins, the second assumes that they were formed in the same manner as classic drumlins, fluted moraines or longitudinal squeeze ridges, and the third scenario assumes that they have the same origins as glacial curvilineations. The group of glacigenic ridges discussed is a glacial landform unique in southern Poland.

Zarys treści. W pracy przedstawiono typowe przypadki konstruktorskiej działalności bobrów w dolinach Małej Panwi i Liswarty oraz ich dopływów. Przeprowadzone badania wskazują, że bobry chętniej zasiedlają małe rzeki 3-4 rzędu niż rzeki główne. Najliczniejsze ślady działalno-ści bobrów zaobserwowano na zalesionych odcinkach dolin Leńcy i Olszynki, gdzie gryzonie przekształciły 28-35% długości koryt rzecznych. Interesującym, niemal symbolicznym przypadkiem jest "naprawa" przez bobry grobli ziemnych starych stawów antropogenicznych i utworzenie w ich miejscu stawów bobrowych.Słowa kluczowe: bobry, tamy bobrowe, dawne obiekty hydrotechniczne, Mała Panew, Liswarta. WprowadzenieW dolinach rzecznych w Polsce, podobnie jak w wielu miejscach w Europie Środkowej, widoczne są pozostałości dawnych systemów hydrotechnicznych wykorzystywanych przez młyny zbożowe, kuźnice i tartaki (m

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