Externsteine — Externsteine in Teutoburg Forrest near Horn-Bad Meinberg

Monumental monolith (other)Fringe site

Externsteine

Germany

Dated12,500 years ago – 9600 BCE

Photo Daniel Schwen · CC BY-SA 2.5Source file on Wikimedia Commons

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Overview

About this site

What the sources say

The Externsteine ([ˈɛkstɐnʃtaɪnə]) is a distinctive sandstone rock formation located in the Teutoburg Forest, near the town of Horn-Bad Meinberg in the Lippe district of the German state of North Rhine-Westphalia.

The formation is a tor consisting of several tall, narrow columns of rock which rise abruptly from the surrounding wooded hills. The Hermannsweg, a long-distance hiking trail, passes through the formation.

In a popular tradition going back to an idea proposed to Hermann Hamelmann in 1564, the Externsteine are identified as a sacred site of the pagan Saxons, and the location of the Irminsul idol reportedly destroyed by Charlemagne; there is however no archaeological evidence that would confirm the site's use during the relevant period.

The stones were used as the site of a hermitage in the Middle Ages, and by at least the high medieval period were the site of a Christian chapel. The Externsteine relief is a medieval depiction of the Descent from the Cross. It remains controversial whether the site was already used for Christian worship in the 8th to early 10th centuries.

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Where it sits in time

The site's dated range, placed against world reference points.

The scale is logarithmic: each step to the left is about ten times older than the last.

10700–9600 BCEHow this date was established: Radiocarbon datingMeasured

What this badge meansA physical measurement of this site: a radiocarbon date, a tree-ring count, a luminescence date, or a record that can itself be dated.
Source for this date

The full article

Externsteine: the whole story

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In brief

Sources for this section

The Externsteine is a distinctive sandstone rock formation in the Teutoburg Forest, near the town of Horn-Bad Meinberg in the Lippe district of North Rhine-Westphalia, Germany. It is a tor of several tall, narrow columns of rock rising abruptly from the surrounding wooded hills. The formation stretches for several hundred metres and ends in a series of 13 highly visible, mostly free-standing pillars, numbered I-XIII from northwest to southeast. Rock II, the Turmfels, rises 37.5 m (123 ft) above its surroundings.

The rock is a hard sandstone laid down during the early Cretaceous era about 100 million years ago, and about 70 million years ago its layers were folded to an almost vertical position. The pillars have been modified and decorated by humans over the centuries. The Grottenfels (I) contains a human-made grotto of three chambers, and an inscription dated to 1115 indicates that an altar was consecrated there. The Externsteine relief is a medieval depiction of the Descent from the Cross, and a rectangular chamber, the Höhenkammer, was cut into the peak of rock II.

Archaeological excavations have yielded Upper Paleolithic stone tools dating from about 10,700 BC to 9,600 BC, and microliths of the Ahrensburg culture were found beneath an overhang on rock VIII, so nomadic groups used the stones as temporary shelter. No archaeological evidence substantiates use of the site between the end of the Upper Paleolithic and the Carolingian period (9th century). Excavations in the 1930s produced evidence of use from the late 10th to the 15th centuries, and the stones served as a hermitage and, by the high medieval period, a Christian chapel.

A popular tradition going back to an idea proposed to Hermann Hamelmann in 1564 identifies the Externsteine as a sacred site of the pagan Saxons and the location of the Irminsul idol reportedly destroyed by Charlemagne, but no archaeological evidence confirms use of the site in that period. The site has also been linked to archaeoastronomical speculation: a circular hole above the altar stone in the Höhenkammer has been said to face the sunrise at the summer solstice.

The origin of the name is debated. The oldest recorded forms, Agistersten and Eggesterenstein, date from 1093. Some link it to the magpie, but more recent linguistic research suggests the Germanic ag, meaning sharp or pointy, so that the physical geology of the stones likely gave rise to their name.

Name

Sources for this section

The etymology of the name Extern- is unclear, in older texts it is written as ”Estern” or Eastern (-steine meaning "stones" or "rocks"). The Latinized spelling with x is first recorded in the 16th century, but became common only in the late 19th century.

The oldest recorded forms of the name read Agistersten and Eggesterenstein, both dated 1093.

Other forms of the name include Egesterenstein (12th century), Egestersteyn (1366), Egersteyne (1369), Egestersten (1385), Egesternsteyn (15th century), Eygesternsteyn (1514), Externsteine (1533), Egesterennstein (1583), Agisterstein (1592).

Hamelmann (1564) gives the Latinized name rupes picarum ("rock of the magpies"), associating the name with Westphalian word Eckster "magpie" (Standard German Elster).

Eckster "magpie" is argued to be the actual etymology of the name by Schröder (1964), who also

connects other Westphalian toponyms Externbrock, Externmühle, Exter, Extern, Exten an der Exter.

Other scholars identify the association with magpies as folk etymology; Plassmann (1961) connects the name with a giant Ecke or Ekka of the Eckenlied, a medieval poem of the Theoderic cycle.

Bahlow (1962, 1965) connects the name to the hydronym Exter.

More recent linguistic research assigns a much higher probability to a different explanation. The Germanic ag means "sharp, edged or pointy". In Middle Low German Egge was used for long rocky ridges. It is found today in Eggegebirge, for example, which lies south of the Teutoburg Forest. That latter area was also known as Osning (Osnegge). Thus, rather than reflecting mythological associations, the physical geology of the stones likely gave rise to their name.