A new geological study examines how Stonehenge’s Altar Stone—a roughly six-ton micaceous sandstone monolith at the centre of the monument—reached Salisbury Plain. Multiple reports say the stone’s source is likely in northeast Scotland, and that researchers used geological analysis and computer modelling to consider a long-distance transport route of roughly 435 miles (700 kilometres). The central hypothesis is that ice and glacial processes could have moved the rock southwards, potentially across Britain during periods when ice sheets covered parts of the landscape. One outlet notes that the glacier explanation is “widely debated,” while another reports that although glacial transport is plausible in principle, it appears less likely than alternative scenarios. Some coverage also references the possibility that later humans may have relocated the stone after it had been carried or affected by glacial conditions. Overall, the reports agree that the stone’s travel path is uncertain, and that the new findings add evidence and modelling constraints to longstanding questions about how the megalith arrived at Stonehenge.