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Bears' Cave (Romanian: Peștera Urșilor, Hungarian: Medve-barlang) is located in the western Apuseni Mountains, on the outskirts of Chișcău village, Bihor County, northwestern Romania. It was discovered in 1975 by Speodava, an amateur spelaeologist group.
The cave bear had a very broad, domed skull with a steep forehead; its stout body had long thighs, massive shins and in-turning feet, making it similar in skeletal structure to the brown bear. [15] Cave bears were comparable in size to, or larger than, the largest modern-day bears, measuring up to 2 m (6.6 ft) in length. [16]
The Fauthsloch. The cave system was developed over a period of about five million years. [7] Fossils show that 20,000 years ago, bears, rhinoceroses and German cave lions roamed the area, [1] and full reconstructions of the bear's skeletons can be viewed on the site today. 8,000 years ago, it was inhabited by humans. [8]
Articles relating to the cave bear (Ursus spelaeus) and its remains. It is a prehistoric species of bear that lived in Europe and Asia during the Pleistocene and became extinct about 24,000 years ago during the Last Glacial Maximum. Both the word cave and the scientific name spelaeus are used because fossils of this species were mostly found in ...
Kletno Bear Cave (Polish: Jaskinia Niedźwiedzia w Kletnie) is the longest cave located in the Śnieżnik Mountains, which are part of the greater Sudeten mountain range. It was discovered in 1966, near the village of Kletno in Poland. It is famous for its many excavations of the cave bear (Ursus spelaeus). [1]
The Chauvet-Pont-d'Arc Cave (French: Grotte Chauvet-Pont d'Arc, French pronunciation: [ɡʁɔt ʃovɛ pɔ̃ daʁk]) in the Ardèche department of southeastern France is a cave that contains some of the best-preserved figurative cave paintings in the world, [1] as well as other evidence of Upper Paleolithic life. [2]
The remains of bears can also be seen inside the caves and allusions have been made to it being the last bear den in Ireland. The cave is typical of the Clare caves, consisting in the main of stream passage and ending in a sump. The general direction is east to west but turns due south some 600 metres (2,000 ft) into the cave.
Cave bear teeth show greater wear than most modern bear species, suggesting a diet of tough materials. However, tubers and other gritty food, which cause distinctive tooth wear in modern brown bears, do not appear to have constituted a major part of cave bears' diets on the basis of dental microwear analysis. [6]