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    Wyświetlanie 1-5 z 5
    Tytuł:
    Sediment transport along the gullies in flysch badlands : an example from SW Slovenia
    Autorzy:
    Zorn, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/295196.pdf
    Data publikacji:
    2011
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    badlands
    gullies
    erosion processes
    flysch
    Istria
    Slovenia
    Opis:
    Sediment transport along erosion gullies in flysch badlands under Sub-Mediterranean climate is presented. Presented are weekly measurements, compiled measurements by months, as well as correlations of sediment transport with selected weather data. Sediment transport was measured up to 19 kg m-2 and was largely dependent on special weather conditions.
    Źródło:
    Landform Analysis; 2011, 17; 229-235
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The geomorphological effectiveness of extreme meteorological phenomena on flysch slopes
    Autorzy:
    Gorczyca, E.
    Powiązania:
    https://bibliotekanauki.pl/articles/294721.pdf
    Data publikacji:
    2008
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    extreme events
    heavy rainfall
    landslies
    flysch slopes
    Beskid Wyspowy
    Bieszczady Niskie
    Opis:
    Extreme events tend to cause large-scale slope system changes. During the last ten years, a series of extreme meteorological events caused considerable transformation of the slopes and valleys in various parts of the Carpathian Mountains. This paper presents the geomorphological effects of extreme rainfall and thaw events on the slopes of two catchments: the lososina catchment (Beskid Wyspowy) and the Hoczewka catchment with an area around the Solinskie Lake (Bieszczady Niskie). The bulk of the discussion concerns a study carried out in the Lososina catchment after three separate extreme events that were followed by a considerable transformation of the slopes due to landsliding. The studies carried out in the Biesr.cr.ady Range, where a single extreme event produced only spatially limited effects, were mainly used for comparison. '[he disparity between the responses of the two slope systems was a result of differences between the systems themselves, including their geology, geomorphology and landslide record, and of the difference in the scale of the extreme events.
    Źródło:
    Landform Analysis; 2008, 6; 15-27
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The structural control of the Mroczna Cave development on the slopes of Mt Kornuty (the Flysch Carpathians, Beskid Niski Mts)
    Autorzy:
    Zatorski, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/295108.pdf
    Data publikacji:
    2014
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    mass movements
    flysch Carpathians
    crevice-type cave
    structural control
    anisotropic rock massif
    Opis:
    The Mroczna Cave is one of the longest caves in the Beskid Niski Mts., located on the south-western slopes of Mt Kornuty, along the main scarp of the landslide. According to the geomechanical criterion, it is dilation cave, where extension has played a major role. Morphotectonic analysis indicates that the main gravitational movement was of a toppling nature but there were also rotation around the vertical axis as well as a backward rotation. The relatively large cave depth (15.5 m) and its shape (cross-section of its passages) indicate that it was formed along a new gravitational cutting surface of the rock massif, associated with joint sets.
    Źródło:
    Landform Analysis; 2014, 27; 55-65
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The identification of neotectonics based on changes of valley floor width
    Autorzy:
    Bil, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/294316.pdf
    Data publikacji:
    2002
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    Outer Western Carpathians
    flysch
    neotectonics
    morphometry
    topographic maps analysis
    valley floor width
    Opis:
    This paper concerns the identification of neotectonics structures on the basis of topographic maps analysis. The investigation parameter is valley floor width (VFW), this being applied to the drainage basin of the BeCva river, Czech Republic. It is firstly necessary to determine the theoretic profile of the VFW downstream increment. For its construction the magnitudo was used (Shreve, 1966). Then, the differences between the real VFW and the theoretical VFW were calculated. The differences were classified according to the associated bedrock lithology. The sections where differences were widely divergent from the average are assumed to be have been affected by neotectonics.
    Źródło:
    Landform Analysis; 2002, 3; 77-85
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Dendrochronological study of the Sawicki landslide activity in the Beskid Niski Mts (Polish Flysch Carpathians)
    Autorzy:
    Kiszka, K.
    Powiązania:
    https://bibliotekanauki.pl/articles/294653.pdf
    Data publikacji:
    2016
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    dendrogeomorphology
    mass movement
    landslide activity
    Sawicki landslide
    eccentricity of tree rings
    Beskid Niski Mountains
    Opis:
    The article presents the results of the dendrogeomorphological study of the activity of the Sawicki landslide, located in the Beskid Niski Mts (Polish Flysch Carpathians). The study was conducted within two study sites in the lower part of the landslide. The landslide movements were dated using the dendrogeomorphological method, basing on the eccentricity indicators calculated for the two coniferous species, i.e. Scots pine (Pinus sylvestris) and silver fir (Abies alba). It was found landslide activity in years: 1899, 1901, 1905, 1910, 1913–1914, 1920–1921, 1929–1931, 1935, 1937, 1945, 1977, 1979, 1981, 1984–1985, 1990, 1992–1993, 1997, 2003–2004, 2006, 2010–2012. The greatest activity was characterized for the northern part of the study site B and the south-western slopes of the Szklarki stream valley (study site A). Studies have shown only a partial dependence between precipitation and landslide episodes. The data were confronted with the results of dendrogeomorphological studies, conducted in the northern and central parts of the landslide. The results demonstrate the significant complexity of mass movements within large-area landslide.
    Źródło:
    Landform Analysis; 2016, 32; 9-26
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-5 z 5

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