Otzberg

Otzberg
Coat of arms
Otzberg
Location of Otzberg within Darmstadt-Dieburg district
Coordinates: 49°50′N 08°55′E / 49.833°N 8.917°E / 49.833; 8.917Coordinates: 49°50′N 08°55′E / 49.833°N 8.917°E / 49.833; 8.917
Country	Germany
State	Hesse
Admin. region	Darmstadt
District	Darmstadt-Dieburg
Government
• Mayor	Matthias Weber
Area
• Total	41.95 km2 (16.20 sq mi)
Elevation	170-367 m (−1,034 ft)
Population (2015-12-31)
• Total	6,360
• Density	150/km2 (390/sq mi)
Time zone	CET/CEST (UTC+1/+2)
Postal codes	64853
Dialling codes	06162, 06163
Vehicle registration	DA
Website	www.otzberg.de

Otzberg is a municipality in the district of Darmstadt-Dieburg, located in the Odenwald forest region of Germany. It was founded in 1972 by the merger of six former independent municipalities.

Otzberg consists of seven villages: Habitzheim, Hering, Lengfeld with Zipfen, Nieder-Klingen, Ober-Klingen and Ober-Nauses, and Schloss-Nauses.

One place of interest in Otzberg is its eponymous castle, a medieval fortress that was first mentioned in 1231. It is widely known for its white tower. The castle itself has been slowly reconstructed to resemble its medieval appearance.

The town is located in the northern Odenwald in southern Hesse. The Otzberg, an extinct volcano, rises above the village, reaching a height of 367 m above sea level. In clear conditions one can see from here to Frankfurt am Main and the Taunus.

The Otzberg is an extinct volcano made of Böllstein gneiss, formed on an old fault zone (the Otzberg column), which continues to the south and separates the eastern Böllsteiner, which is about 50 million years younger than western Bergsträßer Odw.

The Böllstein gneiss and basalt Otzberg caused by large movements of the earth's crust in two different geological eras:

In the Palaeozoic (Paleozoic) walked the continental drift a southern continent to continent on a north. This collided intervening dwarf-continent and in the Devonian and Carboniferous period (about 380-320 million years ago), the Variscan Mountains to the Odw counts delayed. was already in the history of Böllsteiner gneiss. He emerged from granitic rocks, which have penetrated about 410 million years ago as molten rock from below into older sedimentary rocks. These were common - sunk into deeper areas of the earth's crust and converted there, at a high temperature pressure to schists and gneisses - a result of the co-thrusts. At the Otzberg column is welded these rocks - in the course of plate collision - with those of the Bergstrasse Odws.

Many millions of years later, the mountain was already removed down to his torso and powerful Buntsandstein, Muschelkalk, Keuper and law - deposits had altered the landscape, it came in Central Europe back to strong movements in the crust: In connection with a rift zone from the Mediterranean to the North Sea broke - in the Tertiary about 45 million years - the Upper Rhine Graben - and hence the Erbacher-Michelstädter ditch. To the subsidence in the Rhine-Main area also includes the Tire Bay. As a result, many cross dissected and transverse fractures in the area now Odenwald mountain blocks and ditches, so that magma could penetrate to the surface. Were formed in the central and northern Odw approximately 35-20 million years ago volcanoes such as the Otzberg. Some columns were filled with ore-bearing quartz and Schwerspatlösungen.