Rhenish Massif

Coordinates: 51°00′N 7°50′E / 51.000°N 7.833°E / 51.000; 7.833
Source: Wikipedia, the free encyclopedia.
Rhenish Massif
Highest point
PeakGroßer Feldberg
Elevation2,881 ft (878 m)
Geography
CountriesGermany, Belgium, Luxembourg and France
StatesNorth Rhine-Westphalia, Rhineland-Palatinate and Hesse
Parent rangeCentral Uplands
Geology
OrogenyVariscan (Hercynian)
Age of rockDevonian and Carboniferous
Type of rockmetamorphic rock
Satellite image with outlines (grey-drawn outline) of the Rhenish Slate Mountains (green trees). Above left the mouth of the Rhine into the North Sea.

The Rhenish Massif,[1] Rhine Massif[2] or Rhenish Uplands[3] (German: Rheinisches Schiefergebirge, pronounced [ˈʁaɪnɪʃəs ˈʃiːfɐɡəˌbɪʁɡə] : 'Rhenish Slate Uplands') is a geologic massif in western Germany, eastern Belgium, Luxembourg and northeastern France. It is drained centrally, south to north by the river Rhine and a few of its tributaries.

West of the indent of the

Taunus Mountains
form the rest, the south-east.

The massif hosts the

Luxembourgish
: Musel).

Geology

Geological sketch of the Rhenish Massif

Geologically the Rhenish Massif consists of

Rhenohercynian zone of this orogeny, that also encompasses the Harz further east and Devonian rocks of Cornwall (southwestern England
).

Most rocks in the Rhenish Massif were originally sediments, mostly deposited during the

Rhenohercynian basin. In some places in the Ardennes, even older rocks of Cambrian to Silurian age crop out as massifs overlain by Devonian slates. These older rocks form smaller massifs of their own (Stavelot, Rocroi, Givonne and Serpont). In the eastern Rhenish Massif some very limited outcrops in the Sauerland show rocks of Ordovician and lower Siliurian age. Further Ordovician rock exposures are part of the southern Taunus
.

The second rock type are Tertiary and Quaternary igneous rocks, which most prominently occur in the Vulkaneifel, the Westerwald and the Vogelsberg. The volcanic rocks have been linked to a mantle plume that, due to its low density and buoyancy, uplifted the entire region during the last few hundred thousand years, as measured from the present elevation of old river terraces.[4]

Mountain and hill ranges

The mountain and hill ranges within the Rhenish Massif - some with maximum height in metres above sea level (NN)) are given below:

West of the Rhine from north(west) to south(east)

East of the Rhine from north(west) to south(east)

References

  1. ^ Vogel, Miller and Greiling (1987).
  2. ^ Dickinson, Robert E (1964). Germany: A regional and economic geography (2nd ed.). London: Methuen, pp. 428-459. ASIN B000IOFSEQ.
  3. ^ Elkins, T H (1972). Germany (3rd ed.). London: Chatto & Windus, 1972, pp. 226-236. ASIN B0011Z9KJA.
  4. ^ Garcia-Castellanos, D., S.A.P.L. Cloetingh & R.T. van Balen, 2000. Modeling the middle Pleistocene uplift in the Ardennes-Rhenish Massif: Thermo-mechanical weakening under the Eifel? Global Planet. Change 27, 39-52, doi:10.1016/S0921-8181(01)00058-3

Literature

51°00′N 7°50′E / 51.000°N 7.833°E / 51.000; 7.833