The Devil's Table (german: Teufelstisch) in
Hinterweidenthal
Hinterweidenthal is a municipality in Südwestpfalz district, in Rhineland-Palatinate, western Germany
Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in E ...
is a 14 metre high
mushroom rock
A mushroom rock, also called rock pedestal, or a pedestal rock, is a naturally occurring rock whose shape, as its name implies, resembles a mushroom. The rocks are deformed in a number of different ways: by erosion and weathering, glacial action ...
in the German part of the
Wasgau
The Wasgau (german: Wasgau, french: Vasgovie) is a Franco-German hill range in the German state of Rhineland-Palatinate and the French departments of Bas-Rhin and Moselle. It is formed from the southern part of the Palatine Forest and the north ...
region, the southern
Palatine Forest in the state of
Rhineland-Palatinate
Rhineland-Palatinate ( , ; german: link=no, Rheinland-Pfalz ; lb, Rheinland-Pfalz ; pfl, Rhoilond-Palz) is a western state of Germany. It covers and has about 4.05 million residents. It is the ninth largest and sixth most populous of the ...
). Thanks to its location in the territory of the village of Kaltenbach - formerly part of
Wilgartswiesen
Wilgartswiesen is a municipality in Südwestpfalz district, in Rhineland-Palatinate, western Germany.
Geography
The municipality lies in the southern part of the Palatine Forest, the German part of the Wasgau, in the middle of the Palatine Fo ...
– it is often called the Kaltenbach Devil's Table (''Kaltenbacher Teufelstisch''), especially in old literary sources. It is larger and better known than the
Devil's Table of Salzwoog, which is only 5 kilometres away to the southwest.
The Hinterweidenthal Devil's Table is one of the
landscape symbols of the
Palatinate and is also the subject of a local legend. In 1947 the rock was portrayed on a Rhineland-Palatinate postage stamp.
Geography
The Devil's Table stands a few hundred metres south of the
B 10 road and west of Hinterweidenthal-Kaltenbach on a 312-metre-high
ridge, which runs for over two kilometres from
Etschberg
Etschberg is an ''Ortsgemeinde'' – a Municipalities of Germany, municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality – in the Kusel (district), Kusel Districts of Germany, district in Rhineland-Palatinate, German ...
in the southwest to the 324-metre-high in the northeast. The rock towers prominently over the surrounding woods. At night it is lit from the northern side, so that it can be seen from the B 10.
At the foot of the hill on which the Devil's Table stands, is a car park, an inn and the Devil's Table Adventure Park (''Erlebnispark Teufelstisch'').
Geology
Stratigraphy
The German term
Buntsandstein
The Buntsandstein (German for ''coloured'' or ''colourful sandstone'') or Bunter sandstone is a lithostratigraphy, lithostratigraphic and allostratigraphy, allostratigraphic unit (a sequence of rock strata) in the Subsurface (geology), subsurface ...
is used to describe a lithostratigraphic rock unit that consists largely of interbedded sand-, silt- and claystones. These lithologies were sedimented in a large basin covering an area equivalent to that lying between
England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe b ...
and
Poland
Poland, officially the Republic of Poland, is a country in Central Europe. It is divided into 16 administrative provinces called voivodeships, covering an area of . Poland has a population of over 38 million and is the fifth-most populous ...
in a west-east direction and
Scandinavia
Scandinavia; Sámi languages: /. ( ) is a subregion#Europe, subregion in Northern Europe, with strong historical, cultural, and linguistic ties between its constituent peoples. In English usage, ''Scandinavia'' most commonly refers to Denmark, ...
and
Switzerland
). Swiss law does not designate a ''capital'' as such, but the federal parliament and government are installed in Bern, while other federal institutions, such as the federal courts, are in other cities (Bellinzona, Lausanne, Luzern, Neuchâtel ...
in the north-south direction. The Dahner Felsenland (Dahn Rockland) is dominated by sandstones that were deposited during the Early Buntsandstein, about 252.2 until 249 Ma before present. This succession - that also forms the Devil’s Table – is locally known as the Rehberg Formation, which is stratigraphically equivalent to the
Bernburg Formation
The Bernburg Formation is a geologic formation in Germany. It preserves fossils dating back to the Permian period.
See also
* List of fossiliferous stratigraphic units in Germany
See also
* Lists of fossiliferous stratigraphic units in Eur ...
of the Central
Germanic Basin The Germanic Basin (german: Germanisches Becken) is a large region of sedimentation in Western and Central Europe that, during the Permian and Triassic periods, extended from England in the west to the eastern border of Poland in the east.
To the ...
.
Lithologic description
The circa 150 m thick Rehberg Formation is characterised by alternating hard sandstones – so called “rock zones” and less resistant sandstones referred to as “thin layers“.
The rock zones consist of partially silicified, medium- and coarse-grained sandstones, which are in part gravelly. These are commonly massive cross-bedded units with a red to violet colouration, which were deposited mostly in a fluvial environment. The fine-grained “thin layers“ on the other hand show no silicification and indicate a deposition in stagnant water. These layers were deposited mostly as
aeolian sediment.
The lack of
boulder
In geology, a boulder (or rarely bowlder) is a rock fragment with size greater than in diameter. Smaller pieces are called cobbles and pebbles. While a boulder may be small enough to move or roll manually, others are extremely massive.
In c ...
s and
clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4).
Clays develop plasticity when wet, due to a molecular film of water surrounding the clay par ...
in these fine-grained and light brick-red to orange coloured thin layers indicates the absence of water for the most part of the sedimentation process. They represent wind-driven sedimentary deposits in closed drainage basins under arid and hot desert climate conditions.
The
provenance
Provenance (from the French ''provenir'', 'to come from/forth') is the chronology of the ownership, custody or location of a historical object. The term was originally mostly used in relation to works of art but is now used in similar senses i ...
area of the sediment was the Gallic land, which bordered the
Buntsandstein
The Buntsandstein (German for ''coloured'' or ''colourful sandstone'') or Bunter sandstone is a lithostratigraphy, lithostratigraphic and allostratigraphy, allostratigraphic unit (a sequence of rock strata) in the Subsurface (geology), subsurface ...
basin to the west. This uplifted source area stretched from today’s
Belgium
Belgium, ; french: Belgique ; german: Belgien officially the Kingdom of Belgium, is a country in Northwestern Europe. The country is bordered by the Netherlands to the north, Germany to the east, Luxembourg to the southeast, France to th ...
to the
Massif Central
The (; oc, Massís Central, ; literally ''"Central Massif"'') is a highland region in south-central France, consisting of mountains and plateaus. It covers about 15% of mainland France.
Subject to volcanism that has subsided in the last 10,00 ...
in
France
France (), officially the French Republic ( ), is a country primarily located in Western Europe. It also comprises of Overseas France, overseas regions and territories in the Americas and the Atlantic Ocean, Atlantic, Pacific Ocean, Pac ...
.
Formation of the Devil’s Table
The Rehberg Formation commonly forms table rock formations such as the Devil’s Table. The siliceous harder rock zones lie on top of the softer thin layers, that are more susceptible to weathering and erosion. The tabletop-like blocks protect the remaining pillars of less resistant material from further erosion. The shape of the Devil’s Table and its thin pillars is defined by preexisting fractures at the upper and lower end of the tabletop.
The natural monument of the „Devil’s Table“ represents an important landmark of the
Palatinate Forest and was classified as a „National Geotope“ in 2006. In the surrounding are, there are numerous impressive rock formations in the Dahn Rockland, which are also worth a visit!
References
External links
Pfalzbilder: ''Kaltenbacher Teufelstisch''(photos)
{{Coord, 49, 11, 41.65, N, 7, 44, 37.54, E, type:mountain_elevation:275_region:DE-RP, display=title
Rock formations of Rhineland-Palatinate
Climbing areas of Germany
Landforms of Rhineland-Palatinate
Palatinate (region)
Natural monuments in Rhineland-Palatinate