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Fig. 13 | Swiss Journal of Geosciences

Fig. 13

From: Holocene environmental changes and human impact in the northern Swiss Jura as reflected by data from the Delémont valley

Fig. 13

Compiled cross-section through Site 8 (Courrendlin-Les Pécas), constructed from the field and laboratory data collected from the site area. A palaeochannel cut into the Oligocene molasse was episodically active between about 550–1,300 cal AD. Its fill is constituted of clayey silts alternating with organic deposits (legend in Fig. 6). Some pieces of driftwood were dated by dendrochronology and others by 14C (full reference, see Online Resource 8)

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