The Reasons of all which Phænomena seem to be,
That petrify’d Wood having lain in some place where it was well soak’d with petrifying water (that is, such a water as is well impregnated with stony and earthy particles) did by degrees separate, either by straining and filtration, or perhaps, by precipitation, cohesion or coagulation, abundance of stony particles from the permeating water, which stony particles, being by means of the fluid vehicle convey’d, not onely into the Microscopical pores, and so perfectly stopping them up, but also into the pores or interstitia, which may, perhaps, be even in the texture or Schematisme of that part of the Wood, which, through the Microscope, appears most solid, do thereby so augment the weight of the Wood, as to make it above three times heavier then water, and perhaps, six times as heavie as it was when Wood.
Next, they thereby so lock up and fetter the parts of the Wood, that the fire cannot easily make them flie away, but the action of the fire upon them is onely able to Char those parts, as it were, like a piece of Wood, if it be clos’d very fast up in Clay, and kept a good while red-hot in the fire, will by the heat of the fire be charr’d and not consum’d, which may, perhaps, also be somewhat of the cause, why the petrify’d substance appear’d of a dark brown colour after it had been burnt.
By this intrusion of the petrifying particles, this substance also becomes hard and friable; for the smaller pores of the Wood being perfectly wedg’d, and stuft up with those stony particles, the small parts of the Wood have no places or pores into which they may slide upon bending, and consequently little or no flexion or yielding at all can be caus’d in such a substance.
The remaining particles likewise of the Wood among the stony particles, may keep them from cracking and flying when put into the fire, as they are very apt to do in a Flint.
Nor is Wood the onely substance that may by this kind of transmutation be chang’d into stone; for I my self have seen and examin’d very many kinds of substances, and among very credible Authours, we may meet with Histories of such Metamorphoses wrought almost on all kind of substances, both Vegetable and Animal, which Histories, it is not my business at present, either to relate, or epitomise, but only to set down some Observation I lately made on several kind of petrify’d Shels, found about Keinsham, which lies within four or five miles of Bristol, which are commonly call’d Serpentine-stones.
Examining several of these very curiously figur’d bodies (which are commonly thought to be Stones form’d by some extraordinary Plastick virtue latent in the Earth it self) I took notice of these particulars:
First, that these figured bodies, or stones, were of very differing substances, as to hardness: some of Clay, some Marle, some soft Stone, almost of the hardness of those soft stones which Masons call Fire-stone, others as hard as Portland stone, others as hard as Marble, and some as hard as a Flint or Crystal.
Next, they were of very differing substances as to transparency and colour; some white, some almost black, some brown, some Metalline, or like Marchasites; some transparent like white Marble, others like flaw’d Crystal, some gray, some of divers colours; some radiated like those long petrify’d drops, which are commonly found at the Peak, and in other subterraneous caverns, which have a kind of pith in the middle.
Thirdly, that they were very different as to the manner of their outward figuration; for some of them seem’d to have been the substance that had fill’d the Shell of some kind of Shel-fish; others, to have been the substance that had contain’d or enwrapp’d one of those Shels, on both which, the perfect impression either of the inside or outside of such Shells seem’d to be left, but for the most part, those impressions seem’d to be made by an imperfect or broken Shell, the great end or mouth of the Shell being always wanting, and oftentimes the little end, and sometimes half, and in some there were impressions, just as if there had been holes broken in the figurating, imprinting or moulding Shell; some of them seem’d to be made by such a Shell very much brused or flaw’d, insomuch that one would verily have thought that very figur’d stone had been broken or brused whilst a gelly, as ’twere, and so hardned, but within in the grain of the stone, there appear’d not the least sign of any such bruse or breaking, but onely on the very uttermost superficies.