Radiocarbon dating stonehenge
Stonehenge has been a legally protected Scheduled Ancient Monument since 1882 when legislation to protect historic monuments was first successfully introduced in Britain.The site and its surroundings were added to UNESCO’s list of World Heritage Sites in 1986.[Research finds Neanderthals were more thoughtful than we once imagined] The structures were first discovered in the early 1990s by a teenage boy with a sense of curiosity.According to the Atlantic magazine, 15-year-old Bruno Kowalsczewski spent three years hauling away rocks and rubble from the hillside until he uncovered a passageway so narrow that only the thinnest members of the local spelunking club could squeeze through.The remains also date to around this period – between 30 BC, the study suggests.Stonehenge is a prehistoric monument in Wiltshire, England, 2 miles (3 km) west of Amesbury and 8 miles (13 km) north of Salisbury.They were stored in a local museum, while the remaining 49 were reburied because they were thought to be of no scientific value.The oldest remains were found in one of the 56 pits circling Stonehenge, called the Aubrey Holes, which date to the earliest phases of Stonehenge, around 3000 BC.
The carbon-dated remains are three of 52 cremation burials originally excavated during the 1920s.Gingerly, they made their way through the rough-hewn tunnel, past puddles and piles of animal bones and spindly mineral formations, until they arrived at a wide chamber 300 meters deep and found the extraordinary constructions inside.Alternative theories about Stonehenge Theories have ranged from moon temple, to observatory, and even a UFO landing site.Stonehenge stood as giant tombstones to the dead for centuries—perhaps marking the cemetery of a ruling prehistoric dynasty—new radiocarbon dating suggests.The site appears to have been intended as a cemetery from the very start, around 5,000 years ago—centuries before the giant sandstone blocks were erected—the new study says.
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Mineral-laden water dripped from the ceiling, accumulating on spiny stalagmites below.