It's as well when we try to guess how ancient societies built things, to remind ourselves that even erecting something as modern as the Iron Bridge over the Severn in Shropshire baffled industrial archaeologists for years because there are no written accounts of the technique. The only paperwork surviving is the accounts.
It was a chance sighting of a contemporary painting by a Swedish artist of the bridge at a very early stage, that gave the game away; proven by experiments with replica castings and accumulated knowledge of what was available at the time. And that was in the 18C, not some millennia pre-Roman.
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Pgk Pgk –
The warm period is the one we inhabit now, starting around 11 000 years ago, but these are slow processes (in human terms) and the stones could have been dropped some thousands of years previously. If the hypothesis is right that they are erratics, and that is more credible than the idea of purely human action, it was an ice-sheet flow that transported them. Not glaciers. A glacier is very local and Southern England was not glaciated.
The henge's builders would have known the local Chalk was of little use but they could have used the relatively soft oolitic limestone from not too far away, the Greensand (a sandstone) if that outcrops from beneath the Chalk anywhere nearby, or perhaps the tough Carboniferous limestone from the Mendip Hills. Even maybe the Dolomitic Conglomerate (strictly, a breccia) that mantles Mendip, which looks good but it is horrible stuff to work so an unlikely choice. There is also a lot of sandstone around Bristol they could have used, but that is getting a long way for tree-trunk haulage.
I find it very unlikely they would have rollered huge boulders some 200 miles by modern road distance, including rafting them across the very dangerous Severn Estuary, up hill and down dale, from West Wales; when other rocks were available much closer to the site. The received wisdom that they did is simple, unquestioned correlation; but the ice-sheet hypothesis needed research and knowledge long post-dating the historians' idea.
Many old buildings in Exeter use very similar breccia for their bulk infill, and an easily-worked volcanic lava for the detail masonry; the structures date from as recently as late-Mediaeval; and both rocks are local.