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One introduced a characteristics of Lubsza river-basin in aspect of geographical, administrative location and state of existing water-sewage-treatment. On this base one accomplished analyses and one defined activity directions, which would improve present sanitary and ecological state of river-basins in accordance to requirements of the new Water Law.
On the example of two main objects - Morasko Hill near Poznań and morainic pleateau of Konin area, the multiplisity and superposition of glacitectonic structures are presented (figs. 1 and 2). According to author's idea of Quaternary stratigraphy, with four long cold periods complicated klimatologically ("Glacials" with seperate glacial cover development) and three temperature/humidity worm...
Nowadays in SW Poland a conection between Odra riverbed and halotectonic structures system may be observed. It indicates, that its reactivation had a fundamental participation in forming of present river drainage system. Area of vertical block-fault movement in Odra zone is derivative of compression in Permian-Mesozoic cover in NS direction. Result of this movement are noticed earthquakes in 15. century...
One presented in work attempt of connection OCR value with grounds about different genesis and of different history of glacier charges, stepping out in this same geologic profile. They are grounds connected with Middle-Poland glaciation (G III + 1) about age in range 195-128 thousand of years BP. Glacial grounds step out in ceiling and one was not subjected to charge from glacier. Instead lower situated...
The article presents two churches of Romanesque architecture and the material they are built of. These monuments are located in the southern part of Great Poland. The special emphasis was placed on a common. Tertiary sandstone and the source of its transport to the studied churches.
Łuk Mużakowa jest zerodowaną moreną czołową, zdeformowaną w czasie zlodowacenia środkowopolskiego (Elstery) znajdującą się na styku Polski, Brandenburgii i Saksonii. Występują tutaj także pokłady węgla brunatnego z oligocenu i miocenu. W artykule opisano kilka miejsc występowania struktur glacitektonicznych i ich struktury geomorfologiczne na powierzchni ziemi. Najważniejszym, opisanym miejscem są...
There is no doubt that from the beginning of the Neolithic Age through the Bronze Age (approximately 1700 B. C.) and the Iron Age (from about 700 B. C.) till today higher and higher as well as more frequent flood waves have been observed in the river valleys of the East Mid-European Lowland. This phenomenon cannot be justified by climatic and weather changes observed in this period. They were neither...
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