Differentiation of fen bedrock in the Ełk Lakeland (NE Poland) in relation to late Pleistocene terrain morphogenesis
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 which cover the area of 7.3 % of the Ełk Lakeland me...
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Format: | Article |
Language: | English |
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Sciendo
2015-12-01
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Series: | Soil Science Annual |
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Online Access: | http://www.degruyter.com/view/j/ssa.2015.66.issue-4/ssa-2015-0033/ssa-2015-0033.xml?format=INT |