The Königstein is a 189 m high hill in the northern Harz Foreland in the German state of Saxony-Anhalt.[1] It is also known as the Kamelfelsen ("Camel Rocks") due to its unusually shaped sandstone rock formation.
Königstein | |
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![]() The Königstein from the south | |
Highest point | |
Elevation | 189 m (620 ft) |
Coordinates | 51°48′46″N 11°03′01″E |
Geography | |
Westerhausen, Saxony-Anhalt | |
Parent range | Harz Mountains |
The Königstein lies in the northern Harz Foreland, northwest of Westerhausen (near Quedlinburg) on the road towards Börnecke. Its neighbouring hill to the northwest is the 178 m high Jätchenberg. The federal road B 6n runs by to the north. The Königstein is a ridge running from northwest to southeast. Its northeastern flank is relatively steep, but its southwestern slopes fall away much more gently. It is mostly covered in deciduous forest.[1] The vineyard on the southern slopes of the Königstein belongs to the Saale-Unstrut wine-growing area.[2][3] The crest of the ridge is dominated by the striking Kamelfelsen rocks, whose name derives from their shape: seen from the south or north they are supposed to resemble two camels lying down.[4]
The Kamelfelsen consist of hardened sandstone, which also has very soft and crumbly sections. This rock formation, like the well-known Teufelsmauer, was created as a result of the formation of the fault-block mountains of the Harz and the earth movements in the northern Harz Foreland resulting from it. Like the nearby Teufelsmauer, the Königstein is a "rib" of harder rock (Schichtrippe) from the Lower Cretaceous. The Königstein was first placed under protection as a geological feature in 1932 and has been registered as a natural monument since 1997.[4][5] There are several climbing routes on the Kamelfelsen up to climbing grade VIIIb (Saxon grading).[6]
The Königstein was probably used during the Stone Age as a cult site, and Germanic summer solstice celebrations may have taken place here,.[7] The "sun discs" (Sonnenräder) on the rocks - circular shapes cut into the rock, about 1 metre or more in diameter which are distributed around the lower part of the rocks on their northern side - are artifacts resulting from the production of millstones.[7][8] There are also several archaeological sites in the immediate vicinity. The last important find was made during the construction of the German federal road B 6n which runs close by the site.[9]