Zobrazeno 1 - 8
of 8
pro vyhledávání: '"disappearance of lakes"'
Autor:
Lemkowska Bożena
Publikováno v:
Soil Science Annual, Vol 67, Iss 2, Pp 57-63 (2016)
The Mrągowo Lake District (NE Poland) with the area of 182 800 hectares was formed in 1/3 during the Poznań phase (POZ) of the Vistulian glaciation, and in 2/3 in the Pomeranian phase (POM) of that glaciation. A number of fens in the Mrągowo Lake
Externí odkaz:
https://doaj.org/article/87a9e77dfffc4a7ca706f2cfd84c2d32
Autor:
Lemkowska Bożena
Publikováno v:
Soil Science Annual, Vol 66, Iss 4, Pp 161-167 (2015)
The Ełk Lakeland (NE Poland) with the area of 263 100 ha was formed during Vistulian glaciation. More than 66% of this region was shaped during the Leszno phase, 15% during the Poznań phase, and 19% during the Pomeranian phase. There are 1854 fens
Externí odkaz:
https://doaj.org/article/73958e2aeba240e5a34be4e1e3046ebb
Autor:
Adam Piasecki, Rajmund Skowron
Publikováno v:
Limnological Review, Vol 14, Iss 1, Pp 33-43 (2014)
The paper presents the changes that have occurred in the morphometry of Lakes Gopło and Ostrowskie, which are located in central Poland. The analysis covered the period characterised by increased human interference into the water cycle, which has be
Externí odkaz:
https://doaj.org/article/c49ca799eca746529794a633e7743a60
Autor:
Bożena Lemkowska
Publikováno v:
Soil Science Annual, Vol 67, Iss 2, Pp 57-63 (2016)
The Mrągowo Lake District (NE Poland) with the area of 182 800 hectares was formed in 1/3 during the Poznań phase (POZ) of the Vistulian glaciation, and in 2/3 in the Pomeranian phase (POM) of that glaciation. A number of fens in the Mrągowo Lake
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::74ea45531de47ca88b17076891d670d7
http://www.degruyter.com/view/j/ssa.2016.67.issue-2/ssa-2016-0008/ssa-2016-0008.xml?format=INT
http://www.degruyter.com/view/j/ssa.2016.67.issue-2/ssa-2016-0008/ssa-2016-0008.xml?format=INT
Autor:
Bożena Lemkowska
Publikováno v:
Soil Science Annual, Vol 66, Iss 4, Pp 161-167 (2015)
The Ełk Lakeland (NE Poland) with the area of 263 100 ha was formed during Vistulian glaciation. More than 66% of this region was shaped during the Leszno phase, 15% during the Poznań phase, and 19% during the Pomeranian phase. There are 1854 fens
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aec4f0bfa97c343f04f25b9730b4c50f
http://www.degruyter.com/view/j/ssa.2015.66.issue-4/ssa-2015-0033/ssa-2015-0033.xml?format=INT
http://www.degruyter.com/view/j/ssa.2015.66.issue-4/ssa-2015-0033/ssa-2015-0033.xml?format=INT
Autor:
Piasecki Adam, Skowron Rajmund
Publikováno v:
Limnological Review, Vol 14, Iss 1, Pp 33-43 (2014)
Limnological Review; Volume 14; Issue 1; Pages: 33-43
Limnological Review; Volume 14; Issue 1; Pages: 33-43
The paper presents the changes that have occurred in the morphometry of Lakes Gopło and Ostrowskie, which are located in central Poland. The analysis covered the period characterised by increased human interference into the water cycle, which has be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::89f4490364adfee0d709da042ce4a878
https://doaj.org/article/c49ca799eca746529794a633e7743a60
https://doaj.org/article/c49ca799eca746529794a633e7743a60
Autor:
Andrzej Fabich, Monika Kwidzińska
Publikováno v:
Limnological Review; Volume 12; Issue 4; Pages: 169-177
The paper presents the changes in the water surface area of Lakes Udzierz and Mątasek located in the headwaters of the catchment of the River Mątawa (tributary of the River Vistula). The assessment of the rate of changes was based on Polish and Ger
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::348d9d3d1577044c14c2dda56cf543cc
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