Soft‐bedded subglacial meltwater channel from the Welzow‐Süd opencast lignite mine, Lower Lusatia, eastern Germany
An excellent section in the Welzow‐Süd open‐cast lignite mine in Lower Lusatia, eastern Germany, provided a rare opportunity to study a small (5 m deep), buried subglacial meltwater channel of Saalian age. The channel is steep‐sided and distinctly U‐shaped. It is separated from undeformed outwash de...
| Published in: | Boreas |
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| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
1999
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1111/j.1502-3885.1999.tb00226.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1999.tb00226.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1999.tb00226.x |
| Summary: | An excellent section in the Welzow‐Süd open‐cast lignite mine in Lower Lusatia, eastern Germany, provided a rare opportunity to study a small (5 m deep), buried subglacial meltwater channel of Saalian age. The channel is steep‐sided and distinctly U‐shaped. It is separated from undeformed outwash deposits in which it is incised by a sharp erosional contact and it is filled with meltwater sand and till. The till was possibly squeezed into the channel from the adjacent ice/bed interface. Directly beneath the channel, there is a partly truncated diapir of clayey silt, evidencing sediment intrusion into the channel from below. During channel formation, the pressure gradient was oriented from the surrounding sediments into the channel, so that the channel served as a drainage conduit for groundwater from the adjacent subglacial aquifer. The substratum consists largely of sandy aquifers with a total thickness of about 100 m, separated by two aquitards. Channel formation was initiated when hydraulic transmissivity of the bed did not suffice to evacuate all the subglacial meltwater as groundwater flow. As the Welzow‐Süd channel belongs to a dense network of subglacial channels in eastern Germany, temporary ice‐sheet instability in this region prior to channel formation seems possible. |
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