Sion lies midway along the upper Rhône Valley, an east‑west trench gouged by repeated Pleistocene glaciers and now flanked by the Pennine and Bernese Alps. The settlement area sits on the alluvial fan of the Sionne torrent, a cone of well‑sorted sands and gravels that projects onto the wider Rhône flood‑plain.
Millbarrow once stood on a low chalk spur 2 km north‑west of Avebury, just above the spring‑line where the Kennet valley opens onto the Marlborough Downs (NGR SU 0943 7221). From its east–west‑aligned crest the ground falls gently south to Windmill Hill and east into the Kennet valley, giving the mound clear sight of the Avebury monument complex, and easy access to water and pasture.
Sitting on the south‑east shoulder of Windmill Hill (grid ref. SU 086 070), 140 ft (43 m) above the Kennet valley, the Horslip long barrow commands the same chalk ridge that carries the famous Early‑Neolithic causewayed enclosure 400 m upslope.
Quite recently, initial excavation evidence from Bubenec, close to Prague was first announced to the public, pending full publication. As part of that media activity, the head archaeologist for the dig, Petra Maříková Vlčková explained that the excavation; below the future Canadian Embassy, in Prague’s Bubeneč district, cut through almost two metres of undisturbed deposits – a rarity in Central Europe.
The village of Dunning in Perthshire, Scotland, has been revealed through excavation as having traces of human activity dating back 10,000 years. This included evidence of what could be the earliest farming activity recorded in Scotland so far, and also remains of hunter-gathering activity dating back to the Mesolithic period.
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