Neandertal (valley) in the context of "Neanderthal Museum"

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⭐ Core Definition: Neandertal (valley)

The Neandertal (/niˈændərˌtɑːl/, also US: /-ˌtɔːl/, 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. The valley lies within the limits of the towns of Erkrath and Mettmann. In August 1856, the area became famous for the discovery of Neanderthal 1, one of the first specimens of Homo neanderthalensis to be found.

The Neandertal was originally a limestone canyon widely known for its rugged scenery, waterfalls and caves. However, industrial quarrying during the 19th and 20th centuries removed most of the limestone and dramatically changed the shape of the valley. It was during such a quarrying operation that the bones of the original Neanderthal man were found in a cave known as Kleine Feldhofer Grotte. Neither the cave nor the cliff in which the bones were located still exist.

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👉 Neandertal (valley) in the context of Neanderthal Museum

The Neanderthal Museum is a museum in Mettmann, Germany. It was established in 1996. Located at the site of the first Neanderthal man discovery in the Neandertal, it features an exhibit centered on human evolution. The museum was constructed in 1996 to a design by the architects Zamp Kelp, Julius Krauss and Arno Brandlhuber and draws about 170,000 visitors per year. It includes an archaeological park on the original discovery site, a Stone Age workshop, as well as an art trail named "human traces". All signs, as well as the audio guide offered, are available in German and English.

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Neandertal (valley) in the context of Neanderthals in Gibraltar

The Neanderthals in Gibraltar were among the first to be discovered by modern scientists and have been among the most well studied of their species according to a number of extinction studies which emphasize regional differences, usually claiming the Iberian Peninsula partially acted as a “refuge” for the shrinking Neanderthal populations and the Gibraltar population of Neanderthals as having been one of many dwindling populations of archaic human populations, existing just until around 42,000 years ago. Many other Neanderthal populations went extinct around the same time.

The skull of a Neanderthal woman, discovered in a quarry in 1848, was only the second Neanderthal skull ever found and the first adult Neanderthal skull to be discovered, eight years before the discovery of the skull for which the species was named in Neandertal, Germany; had it been recognised as a separate species, it might have been called Calpican (or Gibraltarian) rather than Neanderthal Man. The skull of a Neanderthal child was discovered nearby in 1926. The Neanderthals are known to have occupied ten sites on the Gibraltar peninsula at the southern tip of Iberia, which may have had one of the densest areas of Neanderthal settlement of anywhere in Europe, although not necessarily the last place of possible habitation.

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Neandertal (valley) in the context of Kleine Feldhofer Grotte

Kleine Feldhofer Grotte was a karstic limestone cave and a paleoanthropologic site in the Neander Valley in western Germany. In August 1856, the Neanderthal type specimen was unearthed from the cave. Miners uncovered a skull cap and a number of skeletal bones to be labeled Neanderthal. The bones belong to at least three distinct individuals.

The cave was situated in a limestone gorge with the interior dimensions of 3 m (9.8 ft) in width by 5 m (16 ft) in length by 3 m (9.8 ft) in height, and a 1 m (3.3 ft) opening 20 m (66 ft) above the valley floor in the south wall which was 50 m (160 ft) high. The cave got its name from the nearby large farm of the Feldhof.

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