Archaeologia/Volume 13/Account of Flint Weapons discovered at Hoxne in Suffolk
Read June 22, 1797.
I TAKE the liberty to request you to lay before the Society some flints found in the parish of Hoxne, in the county of Suffolk, which, if not particularly objects of curiosity in themselves, must, I think, be considered in that light, from the situation in which they were found. See Pl. XIV, XV.
They are, I think, evidently weapons of war, fabricated and used by a people who had not the use of metals. They lay in great numbers at the depth of about twelve feet, in a stratified soil, which was dug into for the purpose of raising clay for bricks.
The strata are as follows:
2. Argill 712 feet.
3. Sand mixed with shells and other marine substances 1 foot.
4. A gravelly soil, in which the flints are found, generally at the rate of five or six in a square yard, 2 feet.Flint Weapon found at Hoxne in Suffolk.
Flint Weapon found at Hoxne in Suffolk.
The situation in which these weapons were found may tempt us to refer them to a very remote period indeed; even beyond that of the present world; but, whatever our conjectures on that head may be, it will be difficult to account for the stratum in which they lie being covered with another stratum, which, on that supposition, may be conjectured to have been once the bottom, or at least the shore, of the sea. The manner in which they lie would lead to the persuasion that it was a place of their manufacture and not of their accidental deposit; and the numbers of them were so great that the man who carried on the brick-work told me that, before he was aware of their being objects of curiosity, he had emptied baskets full of them into the ruts of the adjoining road. It may be conjectured that the different strata were formed by inundations happening at distant periods, and bringing down in succession the different materials of which they consist: to which I can only say, that the ground in question does not lie at the foot of any higher ground, but does itself overhang a tract of boggy earth, which extends under the fourth stratum; so that it should rather seem that torrents had washed away the incumbent strata and left the bog-earth bare, than that the bog earth was covered by them, especially as the strata appear to be disposed horizontally, and present their edges to the abrupt termination of the high ground.
If you think the above worthy the notice of the Society, you will please to lay it before them.
I am, Sir,
with great respect,
Your faithful humble Servant,
JOHN FRERE.