Fig. 11From: Holocene environmental changes and human impact in the northern Swiss Jura as reflected by data from the Delémont valleyCompiled cross-section through Site 6 (Courrendlin-Vers La Vieille Eglise), constructed from the field and laboratory data collected from the site area located at the border of terrace T2 formed during the Würmian Upper Pleniglacial (legend in Fig. 6). Between the Bronze Age onwards and the early Middle Ages sediment accumulated in an abandoned meander of the Birse (height exaggerated by a factor of 10). The local stratigraphy and sedimentology (ringed numbers) is described in detail in Online Resource 6Back to article page