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Although it was originally upright, it is now fallen and has now sunk so deep that only its upper face shows.

It is believed that it is one of a pair of 'portal' stones that would have marked the entrance to the circle from the earliest phase of building.

a researcher who uses carbon dating on ancient times-18a researcher who uses carbon dating on ancient times-60

Developing accurate C budgets for seagrass meadows is indeed complex; we discuss these complexities, and, in addition, we review techniques and methodologies that will aid development of C budgets.

We also consider a simple process-based data assimilation model for predicting how seagrasses will respond to future change, accompanied by a practical list of research priorities.

This newly discovered part of the Stonehenge landscape has been dubbed 'Bluestonehenge', due to the fact that it was formed of 24/25 'Bluestone' menhirs, currently thought to have been later moved to Stonehenge during the second phase of construction.

The discovery another such monument on the supports the idea of an intimate connection between the megliths, the landscape, the visible heavens and the after-life. The 'Heel-stone' is a large upright, un-worked sarsen (hard sandstone) which lies immediately adjacent to the A344 road.

The Stonehenge end of the avenue is aligned to the summer solstice sunrise, with the other end terminating at another henge/circle by the River Avon.

similar ceremonial route/avenue (The 'West-Kennet' Avenue), ran from the River Avon past 'The Sanctuary' and on to Avebury.

In this earliest layer there usually was also found a single bluestone fragment of the variety called "rhyolite"...

The rest of the filling of these holes was a rather uniform mass of fine dirt...

The monument we see today is the result of several different construction phases with the same area having been used long before Stonehenge itself existed as testified by the adjacent Cursus and large post-holes, both dated from well before any of the acknowledged construction phases.

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