
Fig. 19: Geometry of the Moon's extreme paths at Stonehenge at mid-summer c2100BC
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Fig. 71: Temperature variations in England over last 20,000 years: HH Lamb
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Fig. 22: Pollen zones and forest cover
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Superimposed on this at greatly extended intervals were periods of heavy rainfall. An expert (Godwin 1956 p203) writes 'Oaks which grew in the English fenland during the warmest postglacial times, and have been found lying preserved in the peat, perhaps from Sub-Boreal times, are reported to be often of remarkably large size, e.g. with trunks reaching a height of 27.5m (90ft) before the first branch'. The countryside of the Stone henge, when construction commenced, was probably fairly lush forest punctuated by scrub and ragged, cleared areas of various sizes, these supporting early forms of crops and livestock, Fig 22.
Inevitably, all places having the same contemporaneous latitude as Stonehenge experienced a change of climate (as every part of the world must have done to some extent) and these included Svalbard northeast of Greenland, Iceland, the south of France, the heel of Italy, Greece, central Turkey, Azerbaijan, Ormsk and the Gyda peninsular on the Arctic Ocean. However, because of their different geographies their experience of this scenario would have varied.