CHAPTER V.
MINERALLS AND FOSSILLS.
[IN its etymological sense the term fossil signifies that which may be dug out of the earth. It is strictly applicable therefore, not only to mineral bodies, and the petrified forms of plants and animals found in the substance of the earth, but even to antiquities and works of art, discovered in a similar situation. The chapter of Aubrey’s work now under consideration mentions only mineralogical subjects; whence it would appear that he employed the term “mineralls” instead of “metals”, including such mineral substances as were not metals under the general term “fossills”.
At present the term fossil is restricted to antediluvian organic remains; which are considered by Aubrey, in Chapter VII. under the name of “Formed Stones”.—J. B.]
THIS county cannot boast much of mineralls: it is more celebrated for superficiall treasure.
At Dracot Cerne and at Easton Piers doe appeare at the surface of the earth frequently a kind of bastard iron oare, which seems to be a vancourier of iron oare, but it is in small quantity and course.
At Send, vulgarly called Seen, the hill whereon it stands is iron-oare, and the richest that ever I saw. (See Chap. II.)
About Hedington fields, Whetham, Bromham, Bowdon Parke, &c. are still ploughed-up cindres; sc. the scoria of melted iron, which must have been smelted by the Romans (for the Saxons were no artists), who used only foot-blasts, and so left the best part of the metall behind. These cinders would be of great use for the fluxing of the iron-oare at Send.
At Redhill, in the parish of….. (I thinke Calne) they digge plenty of ruddle; which is a bolus, and with which they drench their sheep and cattle for ……… and poor people use it with good successe for …… This is a red sandy hill, tinged by {iron}, and is a soile that bears very good carrets.
Mr. John Power of Kington St. Michael (an emperick) told me heretofore that in Pewsham Forest is vitriol; which information he had from his uncle Mr. …. Perm, who was an ingeniose and learned man in those daies, and a chymist, which was then rare.
At Dracot Cerne is good quantity of vitriol-oare, which with galles turnes as black as inke.
About the beginning of the raigne of King James the First, Sir Walter Long [of Dracot] digged for silver, a deep pitt, through blew clay, and gott five pounds worth, for sixty pounds charges or more. It was on the west end of the stable: but I doubt there was a cheat put upon him. Here are great indications of iron, and it may be of coale; but what hopes he should have to discover silver does passe my understanding. There was a great friendship between Sir Walter Raleigh and Sir Walter Long, and they were allied: and the pitt was sunk in Sir W. Raleigh’s time, so that he must certainly have been consulted with. I have here annexed Sir James Long’s letter.
“Mr. Aubrey, I cannot obey your commands concerning my grandfather’s sinking of pitts for metalls here at Draycott, there being no person alive hereabouts who was born at that time. What I have heard was so long since, and I then so young, that there is little heed to be taken of what I can say; but in generall I can say that I doe believe here are many metalls and mineralls in these parts; particularly silver-oare of the blew sort, of which there are many stones in the bottome of the river Avon, which are extremely heavy, and have the hardnesse of a file, by reason of the many minerall and metalline veines. I have consulted many bookes treating of minerall matters, and find them suite exactly with the Hungarian blew silver oare. Some sixteen or eighteen yeares ago in digging a well neer my house, many stones very weighty where digged out of the rocks, which also slaked with long lyeing in the weather. I shewed some to Monsieur Cock, since Baron of Crownstronie in Sweden, who had travelled ten yeares to all the mines in North Europe, and was recommended to me by a London merchant, in his journey to Mindip, and staied with me here about three weekes. He told me the grains in that oare seemed to be gold rather than copper; they resembled small pinnes heads. Wee pounded some of it, and tried to melt the dust unwashed in a crucible; but the sulphur carried the metall away, if there was any, as he said. He has been in England since, by the name of Baron Crownstrome, to treat from his master the King of Sweden, over whose mines he is superintendant, as his father was before him. The vitriol-oare we find here is like suckwood, which being layd in a dry place slakes itself into graine of blew vitriol, calcines red, and with a small quantitie of galles makes our water very black inke. It is acid tasted as other vitriol, and apt to raise a flux in the mouth. Sir, yours, &c.
August 12, 1689. J. L”.
“In the parish of Great Badminton, in a field called Twelve Acres, the husbandmen doe often times plough up and find iron bulletts, as big as pistoll bulletts; sometimes almost as big as muskett bulletts”. Dr. Childrey’s Britannia Baconica, p. 80. [“Britannia Baconica, or the Natural Rarities of England, Scotland, and Wales, historically related, according to the precepts of Lord Bacon”. By Joshua Childrey, D.D. 1661. 8°.]
These bulletts are Dr. Th. Willises aperitive pills; sc. he putts a barre of iron into the smith’s forge, and gives it a sparkling heat; then thrusts it against a roll of brimstone, and the barre will melt down into these bulletts; of which he made his aperitive pills. In this region is a great deale of iron, and the Bath waters give sufficient evidence that there is store of sulphur; so that heretofore when the earthquakes were hereabouts, store of such bulletts must necessarily be made and vomited up. [Dr. Willis was one of the most eminent physicians of his age, and author of numerous Latin works on medical subjects. The above extract is a curious illustration of the state of professional knowledge at the time.—J. B.]
Copperas.—Thunder-stones, as the vulgar call them, are a pyrites; their fibres doe all tend to the centre. They are found at Broad Chalke frequently, and particularly in the earth pitts belonging to the parsonage shares, below Bury Hill, next Knighton hedge; but wee are too fare from a navigable river to make profit by them; but at the Isle of Wight they are gathered from the chalkie rocks, and carried by boates to Deptford, to make copperas; where they doe first expose them to the aire and raine, which makes them slake, and fall to pieces from the centre, and shoot out a pale blewish salt; and then they boile the salt with pieces of old rusty iron.
In the chalkie rocks at Lavington is umber, which painters have used, and Dr. Chr. Meret hath inserted it in his Pinax. [“Pinax Rerum Naturalium Britannicarum, continens Vegetabilia, Animalia, et Fossilia in hac Insula reperta”. By Christopher Merret, M.D., 1666, 12mo.]
In the parish of Steeple Ashton, at West Ashton, in the grounds of Mr. Tho. Beech, is found plenty of a very ponderous marchasite, of which Prince Rupert made tryall, but without effect. It flieth away in sulphur, and the fumes are extreme unwholsom: it is full of (as it were) brasse, and strikes fire very well. It is mundick, or mock-oare. The Earle of Pembroke hath a way to analyse it: not by fire, but by corroding waters.
Anno Domini, 1685, in Chilmark, was found by digging of a well a blewish oare, with brasse-like veines in it; it runnes two foot thick. I had this oare tryed, and it flew away in sulphur, like that of Steeple Ashton.
On Flamstone downe (in the parish of Bishopston) neer the Race-way a quarrie of sparre exerts itselfe to the surface of the turfe. It is the finest sparre that ever I beheld. I have made as good glasse of this sparre as the Venice glasse. It is of a bright colour with a very little tincture of yellow; transparent; and runnes in stirias, like nitre; it is extraordinary hard till it is broken, and then it breakes into very minute pieces.
We have no mines of lead; nor can I well suspect where we should find any: but not far off in Glocestershire, at Sodbury, there is. Capt. Ralph Greatorex, the mathematical instrument maker, sayes that it is good lead, and that it was a Roman lead-worke.
Tis some satisfaction to know where a minerall is not. Iron or coale is not to be look’t for in a chalky country. As yet we have not discovered any coale in this county; but are supplied with it from Glocestershire adjoyning, where the forest of Kingswood (near Bristowe) aboundeth most with coale of any place in the west of England: all that tract under ground full of this fossill. It is very observable that here are the most holly trees of any place in the west. It seemes to me that the holly tree delights in the effluvium of this fossil, which may serve as a guide to find it. I was curious to be satisfied whether holly trees were also common about the collieries at Newcastle, and Dr..... , Deane of Durham, affirmes they are. These indications induce me to thinke it probable that coale may be found in Dracot Parke. The Earledomes, near Downton, (woods so called belonging to the Earledome of Pembroke,) for the same reason, not unlike ground for coale.
They have tryed for coale at Alderbery Common, but was baffled in it. (I have heard it credibly reported that coale has been found in Urchfont parish, about fifty or sixty yeares since; but upon account of the scarcity of workmen, depth of the coale, and the then plenty of firing out of ye great wood called Crookwood, it did not quit the cost, and so the mines were stop’d up. There hath been great talk several times of searching after coale here again. Crookwood, once full of sturdy oakes, is now destroyed, and all sort of fuel very dear in all the circumjacent country. It lies very commodious, being situate about the middle of the whole county; three miles from the populous town of the Devises, two miles from Lavington, &c.-BISHOP TANNER.)
[Several abortive attempts have been made at different periods to find coal on Malmesbury Common.—J. B.]