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Geological Formations

Neandertal (valley)

Erosional and Karst Formations

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The Neandertal is a small valley of the river Düssel in North Rhine-Westphalia, Germany, about 12 kilometers east of Düsseldorf, straddling the towns of Erkrath and Mettmann. It formed as a limestone gorge cut by the river, originally known for dramatic cliffs, waterfalls and caves, though large-scale limestone quarrying in the 1800s and 1900s removed much of the original canyon walls. In August 1856, quarry workers found skeletal remains in a cave called the Kleine Feldhofer Grotte, a find later named Neanderthal 1 and recognized as one of the first identified specimens of Homo neanderthalensis; further excavations in 1997 and 2000 recovered remains of at least three more individuals dating to about 40,000 years ago. The valley takes its modern name from Joachim Neander, a 17th-century pastor and hymn writer who drew inspiration from the gorge, and the Neanderthal Museum now stands on the site.

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Neandertal (valley) (Wikipedia)
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The Neandertal (, also US: , German: [neˈʔandɐtʰaːl] ; sometimes called "the Neander Valley" in English) is a small valley of the river Düssel in the German state of North Rhine-Westphalia, located about 12 km (7.5 mi) east of Düsseldorf, the capital city of North Rhine-Westphalia.
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