Autor: Kolodynska-Gawrysiak, R. - Katalog OPAC zbiorów

Skocz do pozycji: 1.

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

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Skocz do pozycji: 2.

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

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Skocz do pozycji: 3.

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

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