Geisslingen-Schotter
Back to QuaternaryRepresentation and status
- Color CMYK
- (12%,0%,16%,16%)
- Color RGB
- R: 190 G: 215 B: 180
- Rank
- lithostratigraphic Formation
- Validity
- Unit is in Use
- Status
- local name (informal)
Nomenclature
- Deutsch
- Geisslingen-Schotter
- Français
- Gravier de Geisslingen
- Italiano
- Ghiaia di Geisslingen
- English
- Geisslingen Gravel
- Origin of the Name
-
Geisslingen (Deutschland), Klettgau
- Historical Variants
-
«Risszeitliche Schotter», Geisslingen-Schotter (Graf 2009, Bl. Eglisau)
Hierarchy and sequence
- Units at roof
Age
- Age at top
-
- Middle Pleistocene
- Age at base
-
- Middle Pleistocene
- Dating Method
-
U/Th-Datierungen von Kalzitzernenten (> 300 ka) (Graf 2009).
Geography
- Geographical extent
- Im Klettgau kann der Geisslingen-Schotter ostwärts bis ins Schaffhauser Mühlental verfolgt werden, nordwestlich von Schaffhausen hängt er möglicherweise mit dem Schotter der Ryhirt-Formation zusammen (Graf 2009).
- Type area
- Klettgau
- Type profile
-
-
Hardau (SH), W Schaffhausen
Coordinates- (2687000 / 1283100)
-
Hardau (SH), W Schaffhausen
Palaenography and tectonic
-
- Hochterrasse
- Kind of protolith
-
- sedimentary
- Conditions of formation
-
Glazifluviatile Ablagerung.
References
- Definition
-
(2011) :
Quaternary glaciation history of northern Switzerland. E&G Quaternary Science Journal 60/2-3, 282-305
This trough was later filled by glaciofluvial gravel (‘Geisslingen-Schotter’), with deposition in the eastern part originating from the Lake Constance-Rhine glacier, and in the southern channel from the Walensee branch of the Rhine glacier. The maximum ice extent during this phase (Hagenholz advance) was about 25 km SE of Klettgau, close to the present airport of Zurich (Graf 2009a).
- Important Publications
-
(2015) : Luminescence dating of Middle Pleistocene proglacial deposits from northern Switzerland: methodological aspects and stratigraphical conclusions. Boreas