IV.

What kind or kinds of epidemic sickness earthquakes may produce as an effect immediate and at the place, will appear from other instances. One of the most remarkable of earthquakes was that which destroyed Port Royal and nearly all the planters’ houses and sugar-works throughout the island of Jamaica on the 7th of June, 1692. Jamaica had been an English colony for little more than thirty years, during which time it had passed from its state of lethargy under the Spaniards into an emporium of commerce with a rapidly growing population of slaves and whites. The business capital was at Port Royal, wholly built since the British occupation. The site of it was a sandy key or shoal which was said to have risen perceptibly within the memory of original settlers; a writer in September, 1667, said of it: “wherever you dig five or six feet, water will appear which ebbs and flows as the tide. It is not salt, but brackish[769].” A quay had been built along this spit of land, at which vessels of 700 tons could lie afloat. It was here that the havoc of the earthquake was most complete.

Sloane, who had visited Jamaica a few years before, said that the inhabitants expect an earthquake every year, and that some of them were of opinion that they follow their great rains[770]. The year 1692 began in Jamaica with very dry and hot weather which continued until May: then came gales and heavy rains until the end of the month, and from that time until the day of the earthquake, the 7th of June, the weather was excessively hot, calm and dry. The shakes began at 11.40 a.m., and at the third shake, the ground of nearly all Port Royal fell in suddenly, so that in the course of a minute or two most of the houses were under water and the whole wharf was covered by the sea to the depth of several fathoms. The loss of life was, of course, greatest where population was densest; but in the interior of the island the effects on the soil were greater than at the shore: in the north a thousand acres of land sank and thirteen people with it; mountains on either side of a narrow gorge came together and blocked the way; wide chasms appeared in the ground, and on one mountain side there were some dozen openings from which brackish water spouted forth. The first effect in the streets of Port Royal was that men and women seemed all at once to be floundering up to the neck in the wet shifting sand, and were speedily drowned or floated away by the inrushing water. The shakes ceased for days at a time, and then began again, five or six perhaps in twenty-four hours; so that those who had escaped to ships in the bay remained on board for two months, being afraid to come ashore. The weather was hotter after the earthquake than before, and mosquitoes swarmed in unheard of numbers.

During the upheavals or subsidences in Port Royal, and the rushing of water into or from the gapings in the ground, “ill stenches and offensive smells” arose, so that “by means of the openings and the vapours at that time belcht forth from the earth into the air, the sky, which before was clear and blue, was in a minute’s time become dull and reddish looking (as I have heard it compared often) like a red-hot oven.” A very great mortality followed among those who had escaped the earthquake. Some of them settled at Leguanea, others at the place on the bay which became the Kingston of later history, enduring many hardships in their hastily built shelters, from the heavy rains that followed the earthquake, and from want of clothes, food and comforts.

One writes: “Our people settled a town at Leguanea side; and there is about five hundred graves already [20th September, 1692], and people every day is dying still. I went about once to see it, and I had like to have tipt off.” Another says: “Almost half the people that escaped upon Port Royal are since dead of a malignant fever”: and another, referring to the hasty settlement on the bay at Kingston, says “they died miserably in heaps.” But the most interesting information is his next sentence: “Indeed there was a general sickness (supposed to proceed from the hurtful vapours belched from the many openings of the earth) all over the island, so general that few escaped being sick: and ’tis thought it swept away in all parts of the island three thousand souls, the greatest part from Kingstown, only yet an unhealthy place[771].”

That great mortality from a malignant fever after the earthquake of 7th June, 1692, is usually counted an epidemic of the yellow fever which became established at Kingston and Port Royal from that time for at least a century and a half. I have not found any contemporary medical account of it, but all the later writers on yellow fever at Kingston and Port Royal have accepted the tradition that it was yellow fever. But there was one peculiarity, which marks it off from all subsequent epidemics of yellow fever--the sickness was all over the island, so general that few escaped being sick, and was supposed to proceed from the hurtful vapours belched from the many openings of the ground in and near Port Royal. In all subsequent experience yellow fever has been almost confined to the shore or to the ships in the bay[772]. Certainly it has never been all over the island as in 1692, “so general that few escaped being sick”: that is rather in the manner of influenza, although there is nothing to show that the sickness of the interior was so different from that of the shore as to be counted an influenza, or that the mortality of the sick was other than that of a “malignant fever.”

The earthquake at Port Royal in 1692 produced “ill stenches and offensive smells.” The tidal waves, or the subterranean vibrations which caused them, in tearing up the mud at the bottom of the channel at Bridgetown, Barbados, in 1755, had in like manner sent forth a great stench which poisoned the fish. Such offensive vapours were supposed in former times to come, as in a figure, from “the bowels of the earth”; and undoubtedly the sulphurous fumes which have overhung the region of Sicilian earthquakes must have had a source as deep as the strange minerals or “fossils” of Boyle’s hypothesis. But, while the commotion of an earthquake is deep, it is also superficial; whatever miasmata issue from the ground in the ordinary alternations of wet and drought, would be discharged into the atmosphere in unusual quantity and with unusual force in such disturbances of soil as sunk Port Royal in 1692 or were felt at Barbados across the whole width of the Atlantic in 1755. Nor is that effect upon miasmata instantaneous or quickly past; in Jamaica the rumblings and shakes lasted for nearly two months, during which time the pressure upon the gases in the subsoil must have been such as to make them pass into the atmosphere in stronger ascending currents than the mere alternations of moisture and drought would have done. And just as the ordinary seasonal changes in the level of the ground-water are of little or no account for miasmatic-infective disease unless the soil in which they occur be full of organic impurities from human occupancy, so one may reason that the great cataclysmic changes of the earth’s crust are, in this hypothesis of influenza, of most account as touching the stratum of soil wherein lie organic impurities, and as touching those areas of the surface,--the sites of cities, the populous plains, the shores of bays, the bottoms of harbours or any other definite spots--in which the products of organic decomposition are present in largest amount and, perhaps, of somewhat special kind. Such impurities of the soil are indeed a _vera causa_ of infective disease, known to be capable of the effect which has to be accounted for; and, as discharged into the air in great volume and with great force by some upheaval, they would make a local beginning of that “aer inimicus” which the Roman poet figures as creeping like a mist from one region of the heavens to another so that it corrupts each successive tract of air with its own baleful qualities, “reddatque sui simile atque alienum.”

But, as soon as we begin to apply this formula to particular historic cases, difficulties and ambiguities arise[773]. To come back to the instance of Jamaica in 1692, did the general sickness of the island, manifestly miasmatic as it was, and due to disturbances of soil, become an influenza for other regions of the globe? About fifteen months after there was, indeed, a universal catarrh in Britain and Ireland, of no great fatality, which is said by Molyneux, of Dublin, to have prevailed also in the northern parts of France, Flanders, and Holland, but is not reported in the usual way from Europe generally nor from America. Let us suppose a miasmatic cloud formed over the island of Jamaica in June, July, August and September, a cloud of infective particles which might produce influenza at a distance from its place of origin, whatever disease the miasmata after the earthquake may have produced in Jamaica itself. Let this invisible cloud, or emanation, get into the warm atmosphere over the great oceanic current that sets out from the Gulf of Mexico. The vehicle lies ready to hand,--to receive the miasmata not far from their place of origin, to carry them far into the Atlantic, and to bring them, perhaps, to the shores of Britain. This may seem a sufficiently plausible source of the influenza of October and November, 1693, which appears to have been felt only in the British Isles and on the opposite shores of the North Sea. But Webster’s own choice is the volcanic eruption in Iceland in the same year as the influenza; and if we prefer, in this hypothesis, an earthquake to an active volcano, there is a rival source for the British influenza of 1693, nearer both in place and time than that of Jamaica in 1692, and not less important in respect of miasmatic disease in its own locality. This was the disastrous series of earthquakes in Calabria and Sicily, culminating on the 9th of January, 1693. The following extracts from the account sent to the Royal Society will show how great was the commotion of soil, of underground water, and of atmosphere, and how close the connexion of these with the sickness ensuing[774]:

“In the plain of Catania, an open place, it is reported that from one of the clefts in the ground, narrow but very long and about four miles off the sea, the water was thrown forth altogether as salt as that of the sea, [as in Jamaica the year before]. In Syracuse and other places near the sea, the waters in many wells, which at first were salt, are become fresh again.... The fountain Arethusa for the space of some months was so brackish that the Syracusans could make no use of it, and now that it is grown sweeter the spring is increased to near double. In the city of Termini all the running waters are dried up.... It was contrary with the hot-baths, which were augmented by a third part.

Darkness and obscurity of the air has always been over us, but still inferior to that on the 10th and 11th of January; and often these clouds have been thin and light, and of a great extent, such as the authors call _rarae nubeculae_. The sun often and the moon always obscured at the rising and setting, and the horizon all day long dusky....

The effects it has had on humane bodies (although I do not believe they have all immediately been caused by the earthquake) have (yet) been various: such as foolishness (but not to any great degree), madness, dulness, sottishness, and stolidity everywhere: hypochondriack, melancholick and cholerick distempers. Every-day fevers have been common, with many continual and tertian: malignant, mortal and dangerous ones in a great number, with deliria and lethargies. Where there has been any infection caused by the natural malignity of the air, infinite mortality has followed. The smallpox has made great destruction among children.”

Thus we find in Sicily a great disturbance of soil followed, as in Jamaica, by a great increase of local sickness, and by an atmosphere visibly charged with products of the earthquake for months after. This is a nearer source than the Jamaican for the British influenza of Oct.-Nov. 1693,--nearer in time, if that be any advantage for the theory, nearer also in place. There are, however, no intermediate stages to connect the influenza on the northern edge of the European continent with the disturbance of soil and the miasmata arising therefrom in Sicily and Calabria. If there had been any such dry fog as spread all over Europe from the Calabrian earthquake of January, 1783, it would have been a help at least to the imagination in bridging over a gulf of space and time.

As to the interval of time, it should at all events be kept in mind that the same difficulty has to be reckoned with in any hypothesis of influenza and in every great historic instance. In the instance still before us, the infection began in England, according to Molyneux, in October, 1693, and was in Dublin a month later. But we must assume it to have been in the air for some time before it became effective upon mankind. Influenza has been observed, with curious uniformity, to attack the horses, say of London, of Plymouth, of Edinburgh, or of Dublin (as on the occasion before this, 1688) two months or more in advance of the inhabitants of the respective places; and if it had waited, so to speak, for two months before it showed its effects upon men, it may have waited equally long, or longer, before it showed its effects upon horses. That would give at least four months; and then we know, from such an influenza as that of 1743, that there may be weeks, perhaps months, between its prevalence in Naples, Rome or Milan, and its prevalence in London or Edinburgh, and, from the influenza of 1693 itself, that it was a month later in Dublin than in London. An earthquake in Sicily on the 9th of January, 1693, with effects there for months after upon the water, the air, and the prevalent diseases, is not excluded by lapse of time from being a _vera causa_ of an influenza in England in October of the same year, and in Ireland in November. The sort of proof which most men desire, a proof such as we rarely get, and one that is suspiciously neat when we do get it, would be to find an influenza in Sicily and Calabria following the earthquake, and to trace the same step by step over Europe. But the miasmatic sickness in the countries of the earthquakes was not influenza, so far as is known; and there was no epidemic catarrh, so far as is known, in any other part of Europe but the British Isles and the neighbouring shores of the North Sea.