Ein randglaziales Sediment aus der Rißkaltzeit bei Wehr (Südschwarzwald)

Hartmut Leser
A geomorphological mapping of the sheet Wehr of the GMK 25 (= Geomorphological Map 1:25 000) was carried out. On that occasion sediments of the Riß-Glacial were discovered in the valleys of the river Wehra and the brook Hasel. The author discusses by example of a profile of the Meierhofstraße at Wehr the glacial and geomorphogenetic character of a sandy silt- and loam-deposit. The soil type of the profile is a pseudogley. The sedimentological type...