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EN
This article presents a proposal for recognizing the weather and part of a day in digital photos encoded in the bitmap format, based on auctorial edge detection algorithm of horizon to demarcate the sky and k-nearest neighbours algorithm, to classify the daytime in the picture as “day” or “night” and to classify the weather as “sunny” or “cloudy”. To verify the effectiveness of the classification the Internal Bagging-5 model was applied. The data for surveys in the form of pictures was prepared on self-provision. To test the method in a different location, data from the Internet was used.
3
Content available Mapy geologiczno-turystyczne parków narodowych
EN
In 2010, the geological-tourist maps were compiled for the Białowieża National Park (Krzywicki&Pielach, 2010), Babia Góra National Park (Wójcik et al., 2010), Polesie National Park (Kucharska & Danel, 2010), Roztocze National Park (Krąpiec et al., 2010), Wigry National Park (Rychel et al., 2010 ). The maps were commissioned by the Ministry of Environment and their preparation financed by the National Fund for Environmental Protection and Water Management. The sets prepared for each of the above listed national parks include: a colour map with the geological and tourist legends accompanied by a comprehensive description, photos, graphs and other visuals. The maps are important tool for popularization and promotion of geotourism as they meet availability criteria. Moreover, the presentation is not only clear but also satisfactory even for a demanding tourist.
EN
This paper outlines a new approach to reconstructing Vistulian ice sheet limits in NE Poland and adjacent areas of Lithuania and Belarus. It is based on geological investigations of landforms and deposits either of a hypothetical boundary to the Vistulian ice sheet limits. The main conclusions are: 1 - the area was covered twice by the Vistulian ice sheet; the first time during the Świecie Stadial (67-50 ka BP) and the second time during the Main Stadial (24-12 ka BP); 2 - the limit of the older stadial was farther to the south a that of the younger one; 3 - due to covering of the Eemian sediments by the ice sheet of the Świecie Stadial the limit of the Vistulian Glaciation has moved about 15-20 km southwards.
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