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The Natural History of Wiltshire

Chapter 13: CHAPTER VI. STONES.
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About This Book

A collection of antiquarian observations and field notes about Wiltshire that blends natural history, topography, and local antiquities. It surveys landscapes, geological features, flora and fauna, and ancient monuments, often describing barrows, churches, and curiosities in fragmentary entries. It preserves customs, folklore, and oral traditions alongside practical descriptions and speculative explanations. The work reads as a compendium of curious facts and suggestions, combining empirical interest with anecdote and personal reflection to illustrate both the county’s features and the author’s method of inquiry.

CHAPTER VI.
STONES.

I WILL begin with freestone (lapis arenarius), as the best kind of stone that this country doth afford.

The quarre at Haselbury [near Box] was most eminent for freestone in the western parts, before the discovery of the Portland quarrie, which was but about anno 1600. The church of Portland, which stands by the sea side upon the quarrie, (which lies not very deep, sc. ten foot), is of Cane stone, from Normandie. Malmesbury Abbey and the other Wiltshire religious houses are of Haselbury stone. The old tradition is that St. Adelm, Abbot of Malmesbury, riding over the ground at Haselbury, did throw down his glove, and bad them dig there, and they should find great treasure, meaning the quarre.


AT Chilmarke is a very great quarrie of freestone, whereof the religious houses of the south part of Wiltshire and Dorset were built.

[The walls, buttresses, and other substantial parts of Salisbury Cathedral are constructed of the Chilmarke stone.—J. B.]

At Teffont Ewyas is a quarrie of very good white freestone, not long since discovered.

At Compton Basset is a quarrie of soft white stone betwixt chalke and freestone: it endures fire admirably well, and would be good for reverbatory furnaces: it is much used for ovens and hearth-stones: it is as white as chalke. At my Lord Stowell’s house at Aubury is a chimney piece carved of it in figures; but it doth not endure the weather, and therefore it ought not to be exposed to sun and raine.

At Yatton Keynel, in Longdean, is a freestone quarrie, but it doth not endure the weather well.

In Alderton-field is a freestone quarrie, discovered a little before the civill-warres broke forth.

In Bower Chalke field, in the land that belongs to the farme of Broad Chalke, is a quarrie of freestone of a dirty greenish colour, very soft, but endures the weather well. The church and houses there are built with it, and the barne of the farme, w{hi}ch is of great antiquity.


The common stone in Malmesbury hundred and thereabout is oftentimes blewish in the inside, and full of very small cockles, as at Easton Piers. These stones are dampish and sweate, and doe emitt a cold and unwholsome dampe, sc. the vitriolate petrified salt in it exerts itselfe.


I know no where in this county that lime is made, unlesse it be made of Chalke stones: whereas between Bath and Bristoll all the stone is lime-stone. If lime were at xs. or xxs. per lib. it would be valued above all other drugges.


At Swindon is a quarrie of stones, excellent for paveing halls, staire-cases, &c; it being pretty white and smooth, and of such a texture as not to be moist or wett in damp weather. It is used at London in Montagu-house, and in Barkeley-house &c. (and at Cornberry, Oxon. JOHN EVELYN). This stone is not inferior to Purbac grubbes, but whiter. It takes a little polish, and is a dry stone. It was discovered but about 1640, yet it lies not above four or five foot deep. It is near the towne, and not above [ten] miles from the river of Thames at Lechlade. [The Wilts and Berks Canal and the Great Western Railway now pass close to the town of Swindon, and afford great faculties for the conveyance of this stone, which is now in consequence very extensively used.—J. B.]


If Chalk may be numbred among stones, we have great plenty of it. I doe believe that all chalke was once marle; that is, that chalke has undergone subterraneous bakeings, and is become hard: e. g, as wee make tobacco-pipes.


Pebbles.—The millers in our country use to putt a black pebble under the pinne of ye axis of the mill-wheele, to keep the brasse underneath from wearing; and they doe find by experience, that nothing doth weare so long as that. The bakers take a certain pebble, which they putt in the vaulture of their oven, which they call the warning-stone: for when that is white the oven is hot.

In the river Avon at Lacock are large round pebbles. I have not seen the like elsewhere. Quaere, if any transparent ones? From Merton, southward to the sea, is pebbly.

There was a time when all pebbles were liquid. Wee find them all ovalish. How should this come to passe? As for salts, some shoot cubicall, some hexagonall. Why might there not be a time, when these pebbles were making in embryone (in fieri), for such a shooting as falls into an ovalish figure?

Pebbles doe breake according to the length of the greatest diameter: but those wee doe find broken in the earth are broken according to their shortest diameter. I have broken above an hundred of them, to try to have one broken at the shortest diameter, to save the charge and paines of grinding them for molers to grind colours for limming; and they all brake the long way as aforsayd.


Black flints are found in great plenty in the chalkie country. They are a kind of pyrites, and are as regular; ’tis certain they have been “in fluore”.

Excellent fire-flints are digged up at Dun’s Pit in Groveley, and fitted for gunnes by Mr. Th. Sadler of Steeple Langford.


Anno 1655, I desired Dr. W. Harvey to tell me how flints were generated. He sayd to me that the black of the flint is but a natural vitrification of the chalke: and added that the medicine of the flint is excellent for the stone, and I thinke he said for the greene sicknesse; and that in some flints are found stones in next degree to a diamond. The doctor had his armes and his wife’s cutt in such a one, which was bigger than the naile of my middle finger; found at Folkston in Kent, where he told me he was borne.

In the stone-brash country in North Wilts flints are very rare, and those that are found are but little. I once found one, when I was a little boy learning to read, in the west field by Easton Piers, as big as one’s fist, and of a kind of liver colour. Such coloured flints are very common in and about Long Lane near Stuston, [Sherston?—J. B.] and no where else that I ever heard of.

It is reported that at Tydworth a diamond was found in a flint, which the Countess of Marleborough had set in a ring. I have seen small fluores in flints (sparkles in the hollow of flints) like diamonds; but when they are applied to the diamond mill they are so soft that they come to nothing. But, had he that first found out the way of cutting transparent pebbles (which was not long before the late civill warres) kept it a secret, he might have got thousands of pounds by it; for there is no way to distinguish it from a diamond but by the mill.


I shall conclude with the stones called the Grey Wethers; which lye scattered all over the downes about Marleborough, and incumber the ground for at least seven miles diameter; and in many places they are, as it were, sown so thick, that travellers in the twylight at a distance take them to be flocks of sheep (wethers) from whence they have their name. So that this tract of ground looks as if it had been the scene where the giants had fought with huge stones against the Gods, as is described by Hesiod in his {Gk: theogonia}.

They are also (far from the rode) commonly called Sarsdens, or Sarsdon stones. About two or three miles from Andover is a village called Sersden, i. e. Csars dene, perhaps don: Cæsar’s dene, Cæsar’s plains; now Salisbury plaine. (So Salisbury, Cæsaris Burgus.) But I have mett with this kind of stones sometimes as far as from Christian Malford in Wilts to Abington; and on the downes about Royston, &c. as far as Huntington, are here and there those Sarsden-stones. They peep above the ground a yard and more high, bigger and lesser. Those that lie in the weather are so hard that no toole can touch them. They take a good polish. As for their colour, some are a kind of dirty red, towards porphyry; some perfect white; some dusky white; some blew, like deep blew marle; some of a kind of olive greenish colour; but generally they are whitish. Many of them are mighty great ones, and particularly those in Overton Wood. Of these kind of stones are framed the two stupendous antiquities of Aubury and Stone-heng. I have heard the minister of Aubury say those huge stones may be broken in what part of them you please without any great trouble. The manner is thus: they make a fire on that line of the stone where they would have it to crack; and, after the stone is well heated, draw over a line with cold water, and immediately give a smart knock with a smyth’s sledge, and it will breake like the collets at the glasse-house. [This system of destruction is still adopted on the downs in the neighbourhood of Avebury. Many of the upright stones of the great Celtic Temple in that parish have been thus destroyed in my time.—J. B.]

Sir Christopher Wren sayes they doe pitch (incline) all one way, like arrowes shot. Quaere de hoc, and if so to what part of the heavens they point? Sir Christopher thinks they were cast up by a vulcano.