An investigation was carried out on peatlands in the Łódź region. Geological and geomorphological studies focused on 31 sites. The peatland basins are located in moraine plateau and valleys. The diversity of basins in these areas was affected by geomorphological processes: glacial, fluvioglacial, slope, aeolian, thermokarst and fluvial. Peatlands in the region formed in different groups of basins: basins in the moraine area, basins of aeolian origin, basins in valleys (with a distinction between active and inactive valleys). Paleoecological analyses of biogenic deposits show that the peatlands developed from the Late Weichselian to the Subatlantic Period. The schemes of creation and development of the peatlands presented in this study prove...
The Grel raised peat bog is located in the Ludźmierz village vicinity in the Orawa-Nowy Targ Basin. ...
The Żabieniec kettle hole is the first peatland in central Poland analyzed quantitatively with four ...
The Mrągowo Lake District (NE Poland) with the area of 182 800 hectares was formed in 1/3 during the...
The diversity of origins of peatland basins in Central Poland allowed the peatlands to be distinguis...
Studies of infills of present-day peatland basins of the Łódź Region revealed the presence of lacust...
Four peatlands areas were investigated in this thesis, i.e. Lommaflet and Gatmyren are typical mire...
Macroscopic and laboratory tests of over 4-metre-thick organic deposits of Krzywopłoty profile (gytt...
The paper aims to assess the land use changes and the dynamics of the landscape pattern of the Gróje...
Late Glacial organic succession is recorded at the Żabieniec and Koźmin Las sites, in the Łódź regio...
Wśród form geomorfologicznych Kotliny Szczercowskiej znaczną powierzchnię stanowią równiny torfowe. ...
Artykuł poświęcony jest problematyce genezy równin torfowiskowych w strefie „staroglacjalnej” połudn...
Macroscopic and laboratory tests of over 4-metre-thick organic deposits of Krzywopłoty profile (gyt...
The environmental variability during the Mazovian/Holsteinian interglacial is better understood than...
Niewielkie torfowiska występujące w dolinach południowej Polski są słabo poznane, a ich rola w kszta...
In the northern part of the Polish Outer Carpathians, the Beskid Makowski Mts., four landslides form...
The Grel raised peat bog is located in the Ludźmierz village vicinity in the Orawa-Nowy Targ Basin. ...
The Żabieniec kettle hole is the first peatland in central Poland analyzed quantitatively with four ...
The Mrągowo Lake District (NE Poland) with the area of 182 800 hectares was formed in 1/3 during the...
The diversity of origins of peatland basins in Central Poland allowed the peatlands to be distinguis...
Studies of infills of present-day peatland basins of the Łódź Region revealed the presence of lacust...
Four peatlands areas were investigated in this thesis, i.e. Lommaflet and Gatmyren are typical mire...
Macroscopic and laboratory tests of over 4-metre-thick organic deposits of Krzywopłoty profile (gytt...
The paper aims to assess the land use changes and the dynamics of the landscape pattern of the Gróje...
Late Glacial organic succession is recorded at the Żabieniec and Koźmin Las sites, in the Łódź regio...
Wśród form geomorfologicznych Kotliny Szczercowskiej znaczną powierzchnię stanowią równiny torfowe. ...
Artykuł poświęcony jest problematyce genezy równin torfowiskowych w strefie „staroglacjalnej” połudn...
Macroscopic and laboratory tests of over 4-metre-thick organic deposits of Krzywopłoty profile (gyt...
The environmental variability during the Mazovian/Holsteinian interglacial is better understood than...
Niewielkie torfowiska występujące w dolinach południowej Polski są słabo poznane, a ich rola w kszta...
In the northern part of the Polish Outer Carpathians, the Beskid Makowski Mts., four landslides form...
The Grel raised peat bog is located in the Ludźmierz village vicinity in the Orawa-Nowy Targ Basin. ...
The Żabieniec kettle hole is the first peatland in central Poland analyzed quantitatively with four ...
The Mrągowo Lake District (NE Poland) with the area of 182 800 hectares was formed in 1/3 during the...