Rosswald-Schuppe

Representation and status

Color CMYK
N/A
Color RGB
R: 241 G: 239 B: 237
Rank
tectonic slice
Validity
Unit is in Use
Status
local name (informal)

Nomenclature

Deutsch
Rosswald-Schuppe
Français
Écaille de Rosswald
Italiano
Scaglia di Rosswald
English
Rosswald Slice
Origin of the Name

Rosswald (VS)

Historical Variants

Rosswald Slice (TK500, Gouffon et al. 2024)

Hierarchy and sequence

Palaenography and tectonic

Paleogeography
Valaisan Basin
Tectonic unit (resp. main category)
Kind of protolith
  • tectonic
Metamorphism
non metamorphic

References

Definition
Gouffon Yves (Editor) (2024) : Tectonic Map of Switzerland 1:500000, Explanatory notes. Federal Office of Topography swisstopo, Wabern

p.62: The Rosswald Slice is present only east of the Rhône-Simplon Fault. In the Brig area (upper Valais), the Roignais-Versoyen Slice forms the reverse limb of a large anticline, whereas the Rosswald Slice forms the normal, thrusting limb. Both are present for the first 20 km east of the Rhône-Simplon Fault; only the Rosswald Slice continues further east. This slice contains only the upper formation of the “Valaisan Flysch”. It borders the Lepontic units to the north between the Visp – Brig area and the Valle Leventina. Its eastern termination is not clear. Probst (1980) splits it in several units and connects one of them with the Grava Nappe, through the large synform east of Airolo where it would have been partly eroded.

  • Formation de St-Christophe

    Name Origin

    St-Christophe (VS), chapelle à l'ouest de Verbier

    Rank
    lithostratigraphic Formation
    Status
    informal term
    Nomenclatorial Remarks
    <p>Constitue une "trilogie" typique avec les Formations des Marmontains et de l'Aroley sous-jacentes.</p>
    In short

    Formation de la la partie supérieure de la «trilogie valaisanne», constituée d'une séquence turbiditique monotone: alternance fine de calcaires gréseux micacés, rarement conglomératiques, et de calcschistes argilo-gréseux (flysch calcaire de type «Bündnerschiefer»).

    Age
    Late Cretaceous
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