Stonehenge | Page 5

Frank Stevens
Pagan; and the condemnation was as concise and universal as the phrase "Jews, Turks, Infidels, and Heretics" of the Christian Prayer Book to-day. In the early days of the Moyen Age, the Saracen stood for all that was antagonistic to Christianity. Consequently the stones of Stonehenge were Saracen or heathen stones, which the Wiltshire tongue has shortened in due time to Sarsen.
This confusion of ideas may seem amusing, but it is not more absurd than the existing popular idea that Stonehenge is of Druidical origin. The stone circle of Salisbury Plain was many hundred years old when those half mythical Celtic priests first set foot in England, and the Druids of yesterday have about as much connection with Stonehenge as the Salvation Army of to-day.
The Sarsen well repays a close examination. A glance at one of these stones as it lies on the Downland, shows that it has suffered greatly from the weather. It is the core, or kernel, of a much larger block of friable sandstone, worn away on all sides by wind and weather. Moreover, these isolated blocks appear on the Downs in a country devoid of any rock save chalk.
How came they in their present position? In one sense they never came at all; for they existed on the surface of the chalk from the time it rose from the bottom of the sea to its present position. They are, in fact, the remains of a great sheet of fine sand and gravel cemented together by silex, which formerly overlay the chalk downs, the other parts of which have been dissolved and worn by wind and rain until only the harder cores or kernels survive to tell the tale. And the proof of this is not far to seek. The chalk of the London Basin is still capped by layers of such sandstone, as may be seen at Purfleet in Essex. The titanic sheep, or Grey Wethers, therefore, are merely a small residue of that widespread sandy deposit which once covered the whole of the south of England with its inhospitable sheet, and of which larger patches remain to-day in Surrey, Hampshire, and the Isle of Wight. But though the hand of Time and the buffets of the weather have been heavy on the Sarsens, the hand of man has likewise borne its share. In a district like the Plain, devoid of building material other than flint, these stones have attracted the unwelcome attention of the farmers. Walls, gateposts, and paving-stones have accounted for many, while in the interest of the road-mender many a noble Grey Wether has been led to slaughter to provide macadam for the roads. Hence it is not surprising that the number of Sarsen stones to be found on the Plain where Nature placed them is becoming less and less. Indeed, the time may yet come when they will be as extinct as the Great Bustard who once strutted among them, and their memory will survive only in their accidental use in a prehistoric monument like Stonehenge.
THE FOREIGN STONES
While the Sarsens usually awake the greatest interest by reason of their bulk, and the problem of how a primitive people was able to deal with them, a far greater problem is presented by the small uprights, or Foreign Stones, the like of which cannot be matched within a hundred miles of Salisbury Plain, while some can only be found upon the continent of Europe. Fragments carefully removed and submitted to mineralogists have made this fact abundantly clear, and consequently it is possible to arrive at the very definite conclusion that Stonehenge is certainly not a "Wiltshire" monument, and probably that it is not even "British" at all.
Where have the stones come from? One school of writers ventures to suggest Kildare in Ireland. Others suggest Wales, Cornwall, Dartmoor, Shropshire, or Cumberland, where similar rocks are to be found, though perhaps not absolutely identical in character. Yet another theory advanced is that the Foreign Stones were transported to the plain as boulders of the "glacial drift." It has even been stated that the gravels of the district contain small pebbles composed of rock similar to these mysterious Foreign Stones. The statement has indeed been made, but as yet no Wiltshire geologist has produced one of these pebbles of which so much is written, and so little seen.
These Glacial Drift theorists, further account for the absence of these foreign stones elsewhere than at Stonehenge, by yet another theory, that they, like most of the Sarsens, have all been used up for millstones, gateposts, and road metal.
There are many millstones and gateposts in Wiltshire, but where is there one which corresponds in any way to the upright Foreign Stones at Stonehenge? The production of pebbles from the gravels of Wilts, or of a specimen gatepost or millstone would
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