[CAS. 172] resembling columns or pillars. So too Pindar might very justly have said, “The Gaditanian Gates,” if he had in mind the pillars at the mouth; for these mouths are very similar to gates. On the other hand, Gades is not in a position to indicate an extremity, but is situated about the middle of a long coast forming a kind of gulf. The supposition that the pillars of the temple of Hercules in Gades are intended, appears to me still less probable. It seems most likely that the name was originally conferred not by merchants, but generals, its celebrity afterwards became universal, as was the case with the Indian pillars. Besides, the inscription recorded refutes this idea, since it contains no religious dedication, but a mere list of expenses; whereas the pillars of Hercules should have been a record of the hero’s wonderful deeds, not of Phœnician expenditure.
7. Polybius relates that there is a spring within the temple of Hercules at Gades, having a descent of a few steps to fresh water, which is affected in a manner the reverse of the sea-tides, subsiding at the flow of the tide, and springing at the ebb. He assigns as the cause of this phenomenon, that air rises from the interior to the surface of the earth; when this surface is covered by the waves, at the rising of the sea, the air is deprived of its ordinary vents, and returns to the interior, stopping up the passages of the spring, and causing a want of water, but when the surface is again laid bare, the air having a direct exit liberates the channels which feed the spring, so that it gushes freely. Artemidorus rejects this explanation, and substitutes one of his own, recording at the same time the opinion of the historian Silanus; but neither one or other of their views seems to me worth relating, since both he and Silanus were ignorant in regard to these matters. Posidonius asserts that the entire account is false, and adds that there are two wells in the temple of Hercules, and a third in the city. That the smaller of the two in the temple of Hercules, if drawn from frequently, will become for a time exhausted, but that on ceasing to draw from it, it fills again: while in regard to the larger, it may be drawn from during the whole day; that it is true it becomes lower, like all other wells, but that it fills again during the night when drawing ceases. [He adds] that the ebb tide frequently happening to occur during the period of its re-filling, gave rise to the groundless belief of the inhabitants as to its being affected in an opposite manner [to the tides of the ocean]. However it is not only related by him that it is a commonly believed fact, but we have received it from tradition as much referred to amongst paradoxes.1292 We have likewise heard that there are wells both within the city and also in the gardens without, but that on account of the inferiority of this water, tanks are generally constructed throughout the city for the supply of water: whether likewise any of these reservoirs give any signs of being affected in an opposite manner to the tides, we know not. If such be the case, the causes thereof should be received as amongst phenomena hard to be explained. It is likely that Polybius may have assigned the proper reason; but it is also likely that certain of the channels of the springs being damped outside become relaxed, and so let the water run out into the surrounding land, instead of forcing it along its ancient passage to the spring; and there will of course be moisture when the tide overflows.1293 But if, as Athenodorus asserts, the ebb and flow resemble the inspiration and expiration of the breath, it is possible that some of the currents of water which naturally have an efflux on to the surface of the earth, through various channels, the mouths of which we denominate springs and fountains, are by other channels drawn towards the depths of the sea, and raise it, so as to produce a flood-tide; when the expiration is sufficient, they leave off the course in which they are then flowing, and again revert to their former direction, when that again takes a change.1294
8. I cannot tell how it is that Posidonius, who describes the Phœnicians as sagacious in other things, should here attribute [Pg 260]
[CAS. 173] to them folly rather than shrewdness. The sun completes his revolution in the space of a day and night, being a portion of the time beneath the earth, and a portion of the time shining upon it. Now he asserts that the motion of the sea corresponds with the revolution of the heavenly bodies, and experiences a diurnal, monthly, and annual change, in strict accordance with the changes of the moon. For [he continues] when the moon is elevated one sign of the zodiac1295 above the horizon, the sea begins sensibly to swell and cover the shores, until she has attained her meridian; but when that satellite begins to decline, the sea again retires by degrees, until the moon wants merely one sign of the zodiac from setting; it then remains stationary until the moon has set, and also descended one sign of the zodiac below the horizon, when it again rises until she has attained her meridian below the earth; it then retires again until the moon is within one sign of the zodiac of her rising above the horizon, when it remains stationary until the moon has risen one sign of the zodiac above the earth, and then begins to rise as before. Such he describes to be the diurnal revolution. In respect to the monthly revolution, [he says] that the spring-tides occur at the time of the new moon, when they decrease until the first quarter; they then increase until full moon, when they again decrease until the last quarter, after which they increase till the new moon; [he adds] that these increases ought to be understood both of their duration and speed. In regard to the annual revolution, he says that he learned from the statements of the Gaditanians, that both the ebb and flow tides were at their extremes at the summer solstice: and that hence he conjectured that they decreased until the [autumnal] equinox; then increased till the winter solstice; then decreased again until the vernal equinox; and [finally] increased until the summer solstice. But since these revolutions occur twice in the four-and-twenty hours, the sea rising twice and receding twice, and that regularly every day and night, how is it that the filling and failing of the well do not frequently occur during the ebb and flow of the tide? or if it be allowed that this does often occur, why does it not do so in the same proportion? and if it does so in the same proportion, how comes it that the Gaditanians are not competent to observe what is of daily occurrence, while they are nevertheless competent to the observing of revolutions which occur but once in the year. That Posidonius himself credited these reports is evident from his own conjecture respecting the decrease and increase [of the sea] from solstice to solstice. However, it is not likely, being an observant people, that they should be ignorant of what actually occurred, whilst giving credit to imaginary phenomena.
9. Posidonius tells us that Seleucus, a native of the country next the Erythræan Sea,1296 states that the regularity and irregularity of the ebb and flow of the sea follow the different positions of the moon in the zodiac; that when she is in the equinoctial signs the tides are regular, but that when she is in the signs next the tropics, the tides are irregular both in their height and force; and that for the remaining signs the irregularity is greater or less, according as they are more or less removed from the signs before mentioned. Posidonius adds, that during the summer solstice and whilst the moon was full, he himself passed many days in the temple of Hercules at Gades, but could not observe any thing of these annual irregularities. However, about the new moon of the same month he observed at Ilipa1297 a great change in the reflux of the water of the Guadalquiver, as compared with previous flood-tides, in which the water did not rise half as high as the banks, and that then the water poured in so copiously, that the soldiers there dipped their supply without difficulty, although Ilipa is about 700 stadia from the sea. He says, that the plains next the sea were covered by the tides to a distance of 301298 stadia, and to such a depth as to form islands, while the basement of the temple in the enclosure dedicated to Hercules, and the top of the mole in front of the harbour of Gades, were not covered higher than 10 cubits, as observed by actual soundings; but if any one should add the double of that for the occasional risings of the tide which occur, [neither] thus would he be able to estimate the violence with which the full force of the high tide rushes over the plains. Posidonius informs us that this violence [of the tide] is common to all the coasts of Spain on the Atlantic,1299 but what he [Pg 262] [CAS. 175] relates concerning the Ebro is unusual and peculiar to itself, for he says that it sometimes overflows after continued north winds, although there may have been neither rains nor snows. The cause of this [he supposes] to be the lake through which the Ebro flows, its waters being driven by the winds into the current of the river.1300
10. The same writer mentions a tree at Gades, which had boughs reaching to the ground; its sword-shaped leaves often measuring a cubit long, and four fingers broad. Also that about Carthagena there was a tree whose thorns produced a