Mader Stein

Mader Stein
Mader Stein
	Maderstein
	Mader Stein Schwalm-Eder-Kreis, Hesse, Germany
Highest point
Elevation	265 m (869 ft)  Normalhöhennull
Prominence	55 m (180 ft)  Lamsberg
Isolation	0.7 km (0.43 mi)  Lamsberg
Coordinates	51°10′04″N 9°22′53″E
Geography
Location	Schwalm-Eder-Kreis, Hesse, Germany
Parent range	West Hesse Depression
Geology
Age of rock	Miocene
Mountain type	neck of an extinct volcano
Type of rock	basalt

Mader Stein, or Maderstein, is a 265 m (869 ft) (NHN) high hill in North Hesse, Schwalm-Eder-Kreis, north-east of the village of Maden, which belongs to the town of Gudensberg.

Geology

The hill is the remains of an extinct volcano that belongs to the West Hesse Depression.[1] The volcano was active in the Miocene, i.e. during the period about 23 to 5 million years ago (Ma). The only part of the volcano that is left is the neck; the rest has been eroded. The alkali basalt has a silica (SiO₂) volume percentage of 45–55%.[2] The main minerals in the rock are plagioclase, augite and olivine.

The hill cannot be called a kuppe because the top is covered with rock formations. Instead Mader Stein can considered a rocky hillock. The columns of basalt of the hill are sub-horizontal, as at Scharfenstein.

Biotope

The hill, is part of a 311 ha Habitats Directive (German: Flora, Fauna, Habitat; FFH) conservation area that covers the Gudensberg region and the Falkenstein forest (FFH-Nr. 4721-304)[3]. Basalt is relatively poor in nutrients and minerals for plants, and the summit of the hill is very hot and dry in summer, which gives rise to unique flora successions. In particular, Dictamnus, a flowering plant in the family Rutaceae, is found on Mader Stein and Nenkel, although it is very rare in the rest of Germany.[4] To maintain this situation the town of Gudensberg regularly sends people to cut down bushes (in particular blackthorn) that encroach on the summit of the hill.[5]

Steel engraving of Mader Stein (right) and the Odernberg in Gudensberg (left) from the collection of Ernst Wahle, kept at the library of the University of Heidelberg.

Traditions

In previous times the hill was climbed on Ascension Day to dance or collect wild herbs. During Advent a Christmas tree is illuminated on the top of the hill.

Northern panorama from the top of Mader Stein. On the left of the tree is the town of Gudensberg around the Obernberg. Right of the tree are, from left to right, the Lamsberg with a wind turbine and Lotterberg

Legend

The first Christian church in Fritzlar was built by Saint Boniface in the year 732 from the wood of the Donar's Oak that he felled in Gaesmere, part of the town of Fritzlar, in the year 723/24.[6] It is said that the Devil, who lived on Mader Stein (or the nearby Lamsberg), wanted to destroy the church with a stone. There are two different versions of the next part:

Either the stone caught in his sleeve, or
the stone was deflected by the upheld shield of the archangel Michael.

Either way, the stone fell in a field on the outskirts of Maden. This is a real stone; a menhir called Wotanstein. The marks and scratches on the stone are said to have been caused by the devil's claws.

gollark: Just offload it to an out of game server.

gollark: <@!151391317740486657> Yes, and no.

gollark: If people kill me it plays loud ender dragon noises, and interestingly enough continues to play them even when I'm not actually alive.

gollark: The speaker is mostly just for my death contingency.

gollark: Otherwise it would be nice to have something to stop me flying stupidly fast at walls.

References

Wedepohl, K. H. (1985). "Origin of the Tertiary basaltic volcanism in the Northern Hessian Depression". Contributions to Mineralogy and Petrology. 89: 122–143. Bibcode:1985CoMP...89..122W. doi:10.1007/BF00379448. ISSN 0010-7999.
Wilson, Marjorie; Downs, Hilary (1991). "Tertiary–Quaternary extension-related alkaline magmatism in Western and Central Europe". Journal of Petrology. 32 (4): 811–849. Bibcode:1991JPet...32..811W. doi:10.1093/petrology/32.4.811. ISSN 0022-3530.
Map services of the Federal Agency for Nature Conservation
Baumann, Kurt; Bönsel, Dirk; Gregor, Thomas & Starke-Ottich, Indra (2011). "Die Hinkelsteinschneise – der letzte Rest des Frankfurter Weidewaldes" (PDF). Senckenberg – Natur, Forschung, Museum. Vol. 141 no. 7/8. Senckenberg-Museum. pp. 240–245.
Ulrike Lange-Michael (January 6, 2014). "Basalthügel-Landschaft des Chattengaus soll erhalten werden" (in German). Hessische/Niedersächsische Allgemeine.
Reinhold Rau (Berb.) (1968). Briefe des Bonifatius. Willibalds Leben des Bonifatius (in German). Darmstadt. p. 494. ... in loco qui dicitur Gaesmere".

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[1] Wedepohl, K. H. (1985). "Origin of the Tertiary basaltic volcanism in the Northern Hessian Depression". Contributions to Mineralogy and Petrology. 89: 122–143. Bibcode:1985CoMP...89..122W. doi:10.1007/BF00379448. ISSN 0010-7999.

[2] Wilson, Marjorie; Downs, Hilary (1991). "Tertiary–Quaternary extension-related alkaline magmatism in Western and Central Europe". Journal of Petrology. 32 (4): 811–849. Bibcode:1991JPet...32..811W. doi:10.1093/petrology/32.4.811. ISSN 0022-3530.

[DE_BFN-Karten-3] Map services of the Federal Agency for Nature Conservation

[4] Baumann, Kurt; Bönsel, Dirk; Gregor, Thomas & Starke-Ottich, Indra (2011). "Die Hinkelsteinschneise – der letzte Rest des Frankfurter Weidewaldes" (PDF). Senckenberg – Natur, Forschung, Museum. Vol. 141 no. 7/8. Senckenberg-Museum. pp. 240–245.

[5] Ulrike Lange-Michael (January 6, 2014). "Basalthügel-Landschaft des Chattengaus soll erhalten werden" (in German). Hessische/Niedersächsische Allgemeine.

[6] Reinhold Rau (Berb.) (1968). Briefe des Bonifatius. Willibalds Leben des Bonifatius (in German). Darmstadt. p. 494. ... in loco qui dicitur Gaesmere".