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Wyszukujesz frazę "Kolodynska-Gawrysiak, R." wg kryterium: Autor

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    Wyświetlanie 1-11 z 11
    Tytuł:
    Rola uwarunkowań lokalnych w ewolucji suchych dolin Wyżyny Lubelskiej podczas późnego vistulianu i holocenu
    Autorzy:
    Kołodyńska-Gawrysiak, R.
    Powiązania:
    https://bibliotekanauki.pl/articles/295184.pdf
    Data publikacji:
    2008
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    suche doliny
    Wyżyna Lubelska
    vistulian
    holocen
    Źródło:
    Landform Analysis; 2008, 9; 37-40
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Uwarunkowania i przebieg holoceńskiej denudacji w rejonie wielokulturowej osady w panieńszczyźnie koło Lublina
    Conditioning and development of the Holocene denudation in region of multiculture archaeological site in Panienszczyzna near Lublin
    Autorzy:
    Kolodynska-Gawrysiak, R.
    Bienia, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/2084648.pdf
    Data publikacji:
    2010
    Wydawca:
    Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
    Tematy:
    okolice Lublina
    osady
    gleby lessowe
    holocen
    wplyw czlowieka
    Opis:
    The research on conditions and development of the Holocene denudation was performed in a region of the multicultural site in Panieńszczyzna near Lublin. The natural environment of the site, diversified relief developed in loess cover favored denudation processes throughout the Holocene. However, denudation was significantly activated not earlier that the second half of the Holocene due to human impact, namely deforestation and land cultivation. There were two phases of high denudation rate: Neolith (mainly the KPL period) and since 19th century AD.
    Źródło:
    Prace i Studia Geograficzne; 2010, 45; 89-104
    0208-4589
    Pojawia się w:
    Prace i Studia Geograficzne
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Ocena wykorzystania potencjału turystycznego i rekreacyjnego wąwozów lessowych w gminie Kazimierz Dolny
    Assessment of utilization of touristic and recreational potential of loess gullies in Kazimierz Dolny county
    Autorzy:
    Kolodynska-Gawrysiak, R.
    Gawrysiak, L.
    Zlobicki, W.
    Jezierski, W.
    Powiązania:
    https://bibliotekanauki.pl/articles/86015.pdf
    Data publikacji:
    2012
    Wydawca:
    Polska Asocjacja Ekologii Krajobrazu
    Tematy:
    gmina Kazimierz Dolny
    walory turystyczne
    walory rekreacyjne
    wawozy lessowe
    wykorzystanie
    udostepnienie turystyczne
    zagospodarowanie turystyczne
    Źródło:
    Problemy Ekologii Krajobrazu; 2012, 34
    1899-3850
    Pojawia się w:
    Problemy Ekologii Krajobrazu
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Walory geoturystyczne rzeźby lessowej zachodniej części Wyżyny Lubelskiej
    Geotourism assets of loess relief in western part of the Lublin Upland
    Autorzy:
    Zgłobicki, W.
    Kołodyńska-Gawrysiak, R.
    Gawrysiak, L.
    Pawłowski, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074887.pdf
    Data publikacji:
    2012
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    geoturystyka
    studzienki ściekowe
    rzeźba lessowa
    Wyżyna Lubelska
    geoturism
    gullies
    loess relief
    Lublin Upland
    Opis:
    The characteristic group of loess relief in the western part of the Lublin Upland makes up a unique and varied landscape that is particularly attractive for tourists. Gullies, whose density exceeds 11 km/km2 in the Kazimierz Dolny area, are the best known element of the loess landscape. Along the gullies, tourist and interpretive trails have been established, but there is a lack of well-prepared geotourism trails. The southern part of the study area, the Urzędów Hills, is particularly underdeveloped in terms of tourism. This study presents the key characteristics of loess relief in the western part of the Lublin Upland, the current development of tourist infrastructure, and prospects for geotourism based on the unique landforms in the area. A few geotourism trails focusing on the unique loess relief features have been proposed, and attention has been drawn to threats to these landscape assets posed by certain forms of adventure tourism and problems related to private land ownership.
    Źródło:
    Przegląd Geologiczny; 2012, 60, 1; 26-31
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Cechy osadów i rozwój sedymentacji w zagłębieniach bezodpływowych obszarów lessowych na przykładzie stanowiska Snopków (Płaskowyż Nałęczowski, wschodnia Polska)
    The features of sediments and sedimentation development in the closed depression on loess area - a case study: Snopkow site (Naleczow Plateau, E Poland)
    Autorzy:
    Kolodynska-Gawrysiak, R.
    Mroczek, P.
    Chabudzinski, L.
    Powiązania:
    https://bibliotekanauki.pl/articles/2084279.pdf
    Data publikacji:
    2013
    Wydawca:
    Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
    Tematy:
    osady
    sedymentacja osadow
    obszary lessowe
    zaglebienia bezodplywowe
    Plaskowyz Naleczowski
    Polska Wschodnia
    Opis:
    Closed depressions are characteristic elements of the loess plateau landscape. They formed by suffosive processes occurring within initial depressions in the loess cover. Detailed study were conducted in the eastern part of the Nałęczów Plateau (Lublin Upland) in one of the closed depressions located near a multicultural archaeological site. In the closed depression the Holocene soil-sediment sequence of a total thickness 1,3 m were documented. The soil-sediment sequence filling the closed depression and its bottom-forming loesses were detailed physico-chemical and micromorphological analyses as well as C-14 dating performed. This allowed to determine of postglacial litho- and pedogenesis development in the closed depression. Four major phases of Holocene sedimentation were recognized, witch were correlated with human settlement activity from Neolithic to modern times.
    Źródło:
    Prace i Studia Geograficzne; 2013, 51; 29-43
    0208-4589
    Pojawia się w:
    Prace i Studia Geograficzne
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Dziedzictwo geomorfologiczne Polski jako atrakcja turystyczna
    Geomorphologic heritage of Poland as a tourist attraction
    Autorzy:
    Warowna, J.
    Zglobicki, W.
    Kolodynska-Gawrysiak, R.
    Migon, P.
    Kiebala, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/880345.pdf
    Data publikacji:
    2013
    Wydawca:
    Szkoła Główna Gospodarstwa Wiejskiego w Warszawie. Leśny Zakład Doświadczalny. Centrum Edukacji Przyrodniczo-Leśnej w Rogowie
    Tematy:
    Polska
    geomorfologia
    rzezba terenu
    atrakcyjnosc turystyczna
    stanowiska geomorfologiczne
    geoturystyka
    Źródło:
    Studia i Materiały Centrum Edukacji Przyrodniczo-Leśnej; 2013, 15, 4[37]
    1509-1414
    Pojawia się w:
    Studia i Materiały Centrum Edukacji Przyrodniczo-Leśnej
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Geomorphosites of Poland : the role played by the Central Register of Geosites
    Autorzy:
    Warowna, J.
    Migoń, P.
    Kołodyńska-Gawrysiak, R.
    Kiebała, G.
    Zgłobicki, W.
    Powiązania:
    https://bibliotekanauki.pl/articles/294645.pdf
    Data publikacji:
    2013
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    Geomorphosites
    geoheritage
    geodiversity
    Polska
    Opis:
    Poland is a country of considerable geomorphological diversity and includes a range of physical landscapes, from high mountains through uplands, plains, glaciated lowlands, large river valleys, to coasts. Within them, numerous localities may be considered as geomorphosites, illustrating key stages in the geomorphic evolution of the territory, classic landforms and the recent operation of geomorphic processes. The only database that aims to cover all geosites in Poland, including sites of geomorphological interest, is the Polish Central Register of Geosites (PCRG), managed by the state geological survey – the Polish Geological Institute (PIG). Among more than 2200 geosites recorded about 30% can be considered as geomorphosites. Their spatial coverage is very uneven. Most are located in the upland belt of southern Poland (40%) and in northern part of the country, within the extent of the late Pleistocene ice sheet (29%), while the Carpathians are under-represented. Thematically, geosites illustrating various examples of denudational relief dominate (45%). Significantly less common are glacifluvial (13%), glacial (11%) and fluvial (10%) landforms. Tors and residual hills are most common among geomorphosites (205 sites), followed by moraines (52), dunes (49), gullies and their systems (45) and river valleys (34). Thus, PCRG does not yet adequately reflect the diversity of the geomorphological heritage of Poland.
    Źródło:
    Landform Analysis; 2013, 22; 117-124
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Geological conditions of the distribution of closed depressions in the Nałęczów Plateau (Lublin Upland, E Poland): are they an origin determinant?
    Autorzy:
    Kołodyńska-Gawrysiak, R.
    Harasimiuk, M.
    Chabudziński, Ł.
    Jezierski, W.
    Telecka, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/295150.pdf
    Data publikacji:
    2015
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    closed depressions
    loess
    glacial tills
    Opis:
    Closed depressions (CDs) are landforms typical for loess areas. 1761 CDs have been inventoried within the Nałęczów Plateau. Large concentrations of CDs: 30–40 forms per km2 occur in areas where thick (more than 10 m) complex of glacigenic sediments (mainly glacial tills) or clay (limniglacial) deposits underlying loess cover. Areas with a low concentration of CDs (fewer than 10 forms per km2) correspond to areas where the loess cover lies on a bedrock (opokas) or on thin sandy-gravelly deposits. The distributions of CDs depends on the conditions of Pleistocene permafrost development and melting, linked with lithological properties of the sediments under loess cover.
    Źródło:
    Landform Analysis; 2015, 29; 9-18
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The importance of geological conditions for the formation of past thermokarst closed depressions in the loess areas of eastern Poland
    Autorzy:
    Kołodyńska-Gawrysiak, R.
    Harasimiuk, M.
    Chabudziński, Ł.
    Jezierski, W.
    Powiązania:
    https://bibliotekanauki.pl/articles/2060444.pdf
    Data publikacji:
    2018
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    closed depressions
    loess
    past permafrost
    thermokarst
    geological conditions
    Opis:
    Closed depressions (CDs) are common forms occurring in the European loess belt. So far, investigations of CDs in Europe have suggested various natural or/and anthropogenic processes leading to their formation. The origins of CDs occurring in the loess areas of Poland have been the subject of few investigations, and their results have not clarified the problem. Most frequently, the age of CDs is linked with the post-glacial period, or the final stages of the formation of the loess cover. The investigations of CDs carried out in eastern Poland (Nałęczów Plateau) have so far revealed some patterns with regard to the morphometric characteristics and distribution of CDs on the regional scale. They also suggest the impact of thermokarst processes on the formation of the CDs. Five main lithogenetic types of sediment underlying the loess cover have been documented: glacial tills, clay and clayey loams, patches of glacial tills and sandy deposits, sands with gravels, and the bedrock. The relief under the loess cover has also been documented. The types of sediment as well as the relief under the loess cover have an impact on local differences of water content in the loess sediments. It was found that the variatiability of the geological conditions in the Nałęczów Plateau in the Pleistocene had an impact on the local variation of the ice content in the upper part of the former permafrost. This led to local predispositions for the development of thermokarst CDs during the Last Glacial. Areas with a high density of CDs have less permeable sediments (glacial tills, clay and clayey loams) and small relative heights under the loess cover. In the Pleistocene, these areas had higher ice content in the upper part of the permafrost. A model of thermokarst CDs development in the loess areas in eastern Poland is proposed. The model shows that the distribution and size of thermokarst CDs depends on the thickness of the loess cover as well as the types and relief of sediments underlying the loess. The development of thermokarst in the region studied may have consisted of multiple stages resulting in superimposed CDs. Between two and four stages of thermokarst CDs development can be distinguished on the Nałęczów Plateau. The two main stages occurred in MIS 4/3 (~58 ka or 55-50 ka Oerel and Glinde interstadials) and MIS 2/1 (~12 ka). These landforms may have developed also during the Denekamp Interstadial (32-28 ka) and ~15 ka. The present investigations indicate significant morphogenetic effects of permafrost melting on the contemporary relief of the loess areas.
    Źródło:
    Geological Quarterly; 2018, 62, 3; 685--704
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Grain-size and microstructure of the loess from closed depressions in the Naleczow Plateau (East Poland)
    Autorzy:
    Kolodynska-Gawrysiak, R.
    Trzcinski, J.
    Zaremba, M.
    Mroczek, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/971455.pdf
    Data publikacji:
    2019
    Wydawca:
    Uniwersytet Marii Curie-Skłodowskiej. Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej
    Opis:
    The investigation was conducted in the eastern part of the Nałęczów Plateau, a region of the Lublin Upland, in eastern Poland. The loess cover of this region was formed mainly during the last glaciation, and loess accumulation lasted until 15,000–12,000 BP. The undulating loess plateau with numerous oval-shaped closed depressions (CDs) is the main landform in the study area. Particle size distribution and SEM analyses were conducted for loess profiles under the bottoms and on the slopes of 4 CDs. Grain-size distribution characteristics as well as qualitative and quantitative micromorphological characteristics of the the loess forming the bottoms and slopes of the depressions were compared and discussed. It was documented that the differences between the loess forming the bottoms and slopes of the depressions are insignificant in the case of clay fraction content, but are considerable in the case of microstructure characteristics. The differences documented result from the impact of syn- and post-depositional diagenetic processes related mainly to suffosion and hydroconsolidation occurring under the influence of water. A quantitative assessment of the morphological effects of these processes was carried out in the context of the origin of closed depressions. The morphological effect of Holocene diagenetic processes was manifested in the deepening of the initial closed depressions formed previously under the influence of primary morphogenetic processes.
    Źródło:
    Polish Journal of Soil Science; 2019, 52, 2; 295-305
    0079-2985
    Pojawia się w:
    Polish Journal of Soil Science
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The impact of palaeorelief on the origin of some closed depressions in loess areas in the Lublin Upland
    Autorzy:
    Kolodynska-Gawrysiak, R.
    Powiązania:
    https://bibliotekanauki.pl/articles/905173.pdf
    Data publikacji:
    2019
    Wydawca:
    Uniwersytet Marii Curie-Skłodowskiej. Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej
    Opis:
    Closed depressions (CDs) are common small forms occurring in the European loess belt. The age, origin and evolution of these forms is highly debated. Some CDs are reproduced in the loess cover. Their formation was directly influenced by the relief of sediments underlying the loess cover and varying in terms of age and origin. Two depressions of this type were documented within the thin (8 m) loess covers in the Nałęczów Plateau and the Dubienka Depression, using the electrical resistivity method. The age of the reproduced forms varies. The CD in Sadurki formed during the Vistulian. The CD in the Horodło site was forming from the Odranian to the Vistulian glaciation.
    Źródło:
    Polish Journal of Soil Science; 2019, 52, 1
    0079-2985
    Pojawia się w:
    Polish Journal of Soil Science
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-11 z 11

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