The enigmatic altar stone of Stonehenge, a six-ton sandstone block, may have begun its long journey from the northeast of Scotland dragged by glaciers during the last ice age. A team of researchers from Sheffield Hallam University and Curtin University analyzed the ancient movement of ice and proposed that the material reached Dogger Bank, in the present North Sea, before prehistoric groups transported it hundreds of kilometers more to the Salisbury Plain.
Until now, it was known that this central megalith comes from the Scottish Orkney basin, about 700 kilometers from the monument. The distance raised a key question: how did such a massive rock move? By combining dating of mineral grains with computer models of the ice sheets, the scientists assessed both the origin and the feasibility of partial glacial transport.
Dr. Remy Veness, co-author of the work, explained that the finding offers a plausible explanation for part of the journey. “The exciting thing about these results is that they could imply that the people of Doggerland attributed cultural significance to the altar stone long before it was incorporated into Stonehenge,” he noted. Hypothetically, the block would have been valued enough to move it at least twice: first to rescue it from the advancing sea at the end of the ice age and then to its final destination.
Doggerland was a Neolithic landscape off the east coast of England that now lies underwater. Without natural rocky outcrops, any large stone found there must have come from elsewhere, possibly deposited by ice. From that intermediate area, human transport could have followed routes like the Berkshire Ridgeway, considered the oldest road in Europe and active during the time of Stonehenge's construction.










