Syncline of Thalheim
The syncline of Thalheim is a geological trough structure ( syncline ) in the main roe stone of the Swiss Jura , which is cut by the Aare in the transition from the folded Jura to the tabular Jura . It is the middle of three fold and thrust structures in the area of the Aare breakthrough. At the Gislifluh in the south of the Thalheim syncline, the syncline is cut off by a thrust . The rock slab of the Gislifluh, also made of main roe stone, dips below the Mittelland Molasse with a 20 ° gradient .
The Thalheim syncline is a station on the Schinznach-Bad Geoweg , a geological educational trail in Aargau .