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The Externsteine 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.
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 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 from the early 9th century, 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.
Detmold, NRW, Ostwestfalen-Lippe
These rocks are impressive but difficult to capture. The sky on this warm summer evening became overcast for a while
Yantra in Yoga Vidya Ashram Germany. Yantras are powerful paintings used for meditation.
Yantras im Haus Yoga Vidya Bad Meinberg. Yantras sind machtvolle Gemälde für die Meditation.
The Externsteine are a distinctive rock formation located in the Teutoburger Wald region of northwestern Germany, not far from the city of Detmold at Horn-Bad Meinberg. The formation consists of several tall, narrow columns of rock which rise abruptly from the surrounding wooded hills. The name probably means "stones of the Egge".
"Externsteine is a natural outcropping of five sandstone pillars, the tallest of which is 37.5 m (123 ft) high and form a wall of several hundred metres in length, in a region that is otherwise largely devoid of rocks. The pillars have been modified and decorated by humans over the centuries. The geological formation consists of a hard, erosion-resistant sandstone, laid down during the early Cretaceous era about 120 million years ago, near the edge of a large shallow sea that covered large parts of Northern Europe at the time."