http://hdl.handle.net/11089/3087 Mon, 06 Apr 2026 17:38:44 GMT 2026-04-06T17:38:44Z https://dspace.uni.lodz.pl:443/xmlui/bitstream/id/03cbd659-d3e0-4aa4-a2b6-bbefd7d85e2b/ http://hdl.handle.net/11089/3087 http://hdl.handle.net/11089/3362 Ogólne cechy potencjału leczniczego klimatu i bioklimatu Uniejowa Błażejczyk, Krzysztof; Szmyd, Jakub; Adamczyk, Anna Beata The paper presents general features of the climate and bioclimate of Uniejów assessed from the point of view of the possibility to apply them to climate therapy. The authors have used multiannual data from meteorological stations located in the vicinity of Uniejów. It was found that the climate and bioclimate of the city are suitable for climate therapy. The most useful is the period from the beginning of May to the middle of October when the majority of patients can practice one of several forms of climate therapy (aerotherapy, heliotherapy, terrain therapy). Sun, 01 Jan 2012 00:00:00 GMT http://hdl.handle.net/11089/3362 2012-01-01T00:00:00Z http://hdl.handle.net/11089/3361 Historia rozwoju doliny Warty w basenie uniejowskim Petera-Zganiacz, Joanna; Forysiak, Jacek The conditions existing in the Uniejów Basin were favourable to formation of outflow after successive glaciations due to subsidence in Adamow graben. The last glacial episode in this area was the Warta stage. During the recession of continental glacier the waters flew away towards the south, but when the glacier receded to the north, a valley began to form with an outflow in the northern direction. During the time of the Eemian Interglacial the valley bottom was fairly wide and it was on the ordinate of 80.0 m. above see level. In the Vistulian the aggradation tendencies dominated. A high Plenivistulian terrace formed in the Warta valley (but only in the southern part of the Uniejów Basin) and a low Late Plenivistulian terrace. On the surface of the vast low terraca there are remains of multichannel river system which formed in Younger Dryas and were reactivated in the Holocene. The Warta river-bed was gradually lowering from the begining of Holocene until the Atlantic period, when this tendency was reversed as a result of intensified human- generated supply of mineral material into the river-bed. Over the last two centuries the Warta transformed into a one-channel river in consequence of strong human impact. Sun, 01 Jan 2012 00:00:00 GMT http://hdl.handle.net/11089/3361 2012-01-01T00:00:00Z http://hdl.handle.net/11089/3360 Miasto i gmina Uniejów w pracach doktorskich, magisterskich i licencjackich opracowanych na Wydziale Nauk Geograficznych Uniwersytetu Łódzkiego Wiluś, Robert Sun, 01 Jan 2012 00:00:00 GMT http://hdl.handle.net/11089/3360 2012-01-01T00:00:00Z http://hdl.handle.net/11089/3359 „Świeża woda zdrowia doda”. Opowieść o wodzie. Studium etnograficzne Plucińska, Aldona Jadwiga When we consider water in the cultural context, it allows us to understand and appreciate its role and importance in the life of people in the present-day civilisation. It is the main element of many family and annual rituals. It pervades the material, social and spiritual aspects of culture with the same intensity in the 21st century as in the past. Water allows man to move from one space to another and to transgress boundaries without negative consequences for himself and for the environment in which exists. In the past our ancestors used water to propitiate Nature, making also use of their bodies for that purpose, thus creating cultural codes which form cultural sequences connecting the past with the present. The inscription on kitchen towels „Fresh water will make you healthy”, no longer known to the youngest generations in the visual form, still remains actual. Each of us likes fresh water for drinking; we also seek water for its therapeutic properties, and prefer recreation in places with water reservoirs, both natural and artificial. In this way we get closer to the Beginning. Sun, 01 Jan 2012 00:00:00 GMT http://hdl.handle.net/11089/3359 2012-01-01T00:00:00Z