DE MOERASKALK VAN WILDERVANK (GR.)
Samenvatting
An elongated depression west of Wildervank, filled with gyttja, hypnaceous peat, sand, loam and fen peat, was found to contain lime deposits in the basic gyttja. A water flow from a system under pressure welled up in the depression, where low temperatures of the Younger Dryas caused lime from this water to precipitate. The fact that this lime was not dissolved lateron points to a high watertable in the area.
