Article ID Journal Published Year Pages File Type
9491238 Journal of Hydrology 2005 12 Pages PDF
Abstract
GPR and EM31 surveys across Sphagnum pools (defined here as Sphagnum filled wet depressions) suggest a continuous sequence of underlying lake sediment and glacio-marine deposits devoid of elevated mineral surfaces. We suggest that Sphagnum pools developed after peatland formation (secondary features) due to changes in water table, peat accumulation and/or climatic controls.
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Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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Stratigraphic controls on pool formation in a domed bog inferred from ground penetrating radar (GPR)
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