Recent, relic and buried soils in the forefield of Werenskiold Glacier, SW Spitsbergen
Abstract: Soils, having a well−developed sequence of A and Bw horizons, are widespread on the uplifted marine terrace 8–12 m a.s.l. in the proximity of Nottinghambukta Bay. The present−day origin of these soils is however questionable, while similarly developed soils, but buried under the cover of t...
| Main Authors: | , |
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.603.1396 http://www.polar.pan.pl/ppr30/PPR30-161.pdf |