THE RAMBLES OF A NATURALIST. VOL. II. LONDON : Printed by SPOTTISWOODE & Co. New-street Square. THE RAMBLES OF A NATURALIST ON THE COASTS OF FRANCE, SPAIN, AND SICILY. BY A. DE QUATREFAGES, MEMBER OF THE INSTITUTE, PROFESSOR OF ETHNOLOGY AT THE MUSEUM OF NATURAL HISTORY AT THE JARDIN DBS PLANTES, ETC. ETC. TRANSLATED (with the Author's sanction and co-operation) BY E. C. OTTE, HONORARY MEMBER OF THE LITERARY AND PHILOSOPHICAL SOCIETY OF ST. ANDREWS. IN TWO VOLUMES. VOL. II. LONDON: LONGMAN, BROWN, GREEN, LONGMANS, & ROBERTS. 1857. CONTENTS OF THE SECOND VOLUME. CHAPTER V. THE COASTS OF SICILY. MILAZZO, STROMBOLI, GIARDINI. Zoological poverty of the western coasts of Sicily. — Journey by land from Trapani to Cephalu. — Milazzo. — Sedimentary rocks of contemporaneous formation. — Milne Edwards's submarine excursions. — Stromboli. — Excursion to the volcano. — Phospho- rescence of the sea. — Messina. — Giardini. — Difference between the natural method and classifications. — Embryological studies of Milne Edwards ; progressive characterisation of animal species. — Blanchard's investigations on the nervous system. — Organic complication of some of the lower animals. — Degradation of superior types ; the Amphioxus. — Simultaneous appearance of different animal types in ancient geological epochs - Page 1 CHAP. VI. THE COASTS OF SICILY. ETNA. Aspect and nature of the coast from Giardini to Catania. — Cata- nia ; its harbour ; its soil. — Etna. — Excursion to the volcano. — Nicolosi; the Casa Gemellaro; a night passed at the foot of the cone; the great crater; the crater of 1843. — Eruption of 1669 ; VI CONTENTS OF its traces as far as the town of Catania. — Elie de Beaumont's theory of Etna. — Observations made in the crater of Vesuvius. — Examples of the slight degree of solidity of the earth's crust. — Approximate calculation of volcanic forces Page 7 1 CHAP. VII. THE BAY OF BISCAY. BIARRITZ. — GUETTARY. — SAINT -JEAN-DE-LUZ. Departure for the Bay of Biscay. — Bayonne. — The bar of the Adour. — Biarritz. — La chambre d' 'amour. — Geological problems relating to the age of neighbouring rocks. — Guettary. — Saint- Jean-de-Luz. — Encroachment of the sea. — Wearing away of the coast; the ground swell. — Hermellas. — Extreme variability in the type of the Annelids. — The Polyophthalmians j organic com- plication. — Realisation of some of the fables of mythology. — Independence of the nervous centres in certain of the lower animals ; transposition of the ordinary seat of certain sensations 135 CHAP. VIII. THE BAY OF BISCAY. SAINT SEBASTIAN. The road leading from Saint-Jean-de-Luz to Saint Sebastian ; the Bidassoa ; the Isle of Pheasants. — Saint Sebastian. — The Basques : their claims as a race ; their probable origin ; their fueros ; their ethnological characters. — The Teredo ; its mode of reproduction ; means of preserving wood from its attacks. — Embryological studies ; nature of germs ; theories of evolution, of accolement and of epigeuesis ; distinct life of germs. — Development of the Her- mella and the Teredo. — Metamorphoses. — General idea of life 185 CHAP. IX. THE COASTS OF SAINTONGE. LA ROCHELLE. Journey from Paris to La Rochelle. — Historical notice of that town ; its origin ; its constitution ; its sieges. — Decay of La Rochelle. — Poverty of the coast ; reciprocal dependence of the kingdoms of THE SECOND VOLUME. Vll nature. — The Branchellion ; its external characters ; its lym- phatic respiration. — The natural method ; insufficiency of the principle of dominant characters in the study of the lower animals Page 251 CHAP. X. THE COASTS OF SAINTONGE. CHATELAILLON ; ESNANDES. The evident marks of great changes in the coast of Saintonge ; encroachment of the sea; destruction of Montmeillan, and of Chatelaillon ; accumulations due to marine action ; salt marshes. — The former gulf of Poitou; elevation of Saint-Michel-en- 1'Henn ; Esnandes. — Walton the Irishman ; his introduction of a new breed of sheep ; his nets ; the aeon and bouchot; Mussel-beds. — Excursions to Esnandes ; shrimp-fishing. — The Termites; ancient fables regarding them ; habits of the Termes bellicosus ; the buildings erected by these insects ; fecundity of the queen ; the ravages occasioned by them. — French Termites; their recent appearance in Europe ; the Rochelle Termites ; the destruction they have effected in the Prefecture of that city. — Observations made on Termites in confinement; means of destroying these insects. — The recent observations of M. Lespes. — The moral and spiritual influences of zoological studies - 294 APPENDIX - .... 355 RAMBLES OF A NATURALIST, CHAPTER V. THE COASTS OF SICILY. MILAZZO, STROMBOLI, JARDINI. 7" Zoological poverty of the western coasts of Sicily. — Journey by land from Trapani to Cephalu. — Milazzo. — Sedimentary rocks of contemporaneous formation. — Milne Edwards's submarine excursions. — Stromboli. — Excursion to the volcano. — Phospho- rescence of the sea. — Messina. — Jardini. — Difference between the natural method and classifications. — Embryological studies of Milne Edwards ; progressive characterisation of animal species. — Blanchard's investigations on the nervous system. — Organic complication of some of the lower animals. — Degradation of superior types; the Amphioxus. — Simultaneous appearance of different animal types in ancient geological epochs. IT had been our intention, when we first arrived in Sicily, to make the entire circuit of the island, but the information which we obtained in the course of our wanderings, gradually modified our original plans. Our men had now begun to comprehend the object of our voyage, and had learned, day by day, better to appreciate the conditions necessary to the success of our researches. Artese and Cannel, VOL. II. B 2 RAMBLES OF A NATUKALIST. who, from their perfect knowledge of the coasts, might have served as pilots, expressed strong doubts as to the utility of an exploration of the west coast, where, as they told us, we should find nothing but pestilential marshes, or shingle and sand. On con- sulting our maps, and considering the geological conformation of the district, we found that their statements were well grounded. Indeed, Sicily everywhere bears traces of those violent forces, which, by their action on the solid crust of our globe, have elevated this island above the waves. Amid the thousand irregularities which mark the contour of the land, and are the inevitable result of this mode of formation, we could perceive how differently these forces had acted at different points. To the west, east, and south-east, the low chains of mountains gradually slope towards the sea, and either terminate in undulating hills or merge into extended plains and low tracts of shore covered with salt marshes. A few isolated peaks, which, in some cases, are of an entirely volcanic origin, like Monte- Bosso, rise above the others, although few attain a height of more than 2000 feet ; Monte-Caramata is, indeed, an exception to this rule, for its calcareous rocks, which command the town of Orte, rise to an elevation of 4000 feet. In the centre of the island the mountains are higher, and several of them have an altitude of more than 3000 feet ; still, the true mountainous region of Sicily lies in the north and north-east of the island. Here the subterranean forces, acting with their whole intensity, have pro- truded huge masses of gneiss and granite through THE COASTS OF SICILY. 3 the strata of limestone, of sandstone and argillace- ous schist formations. The Pelorian and Madonian chains * exhibit numerous summits, which rise up- wards of 4000 feet above the level of the sea; some even exceed 5000 feet; and one of them, the Pizzo di Palermo, attains an altitude of nearly 6000 feet. These high mountain-chains, which extend like a wall from Palermo to Messina, are broken here and there by the intervention of a cape or a small penin- sula, whose deeply indented shores seemed to promise us an abundant harvest. After much deliberation, it was decided that these should form the scene of our next explorations on leaving Favignana. In order to lose no time by this retrograde move- ment, we resolved once more to leave our boat ; and having given Perone orders to await our arrival at Cephalu, we set forth, accompanied only by the faithful Carmel, and, guided by the muleteers on whose mules we were to make the journey, tra- versed a part of Sicily which is very rarely visited by strangers. Here, as at Trapani, we everywhere observed mournful traces of deficient civilisation, associated with the remains of the splendour of a bygone age. The church of Castelvetrano, in which lie the re- * The Pelores mountains, formerly known as the Neptunian chain, border the whole north coast of Sicily from east to west, and seldom devjate far from the coast line. The Madonian chain, which was designated by the ancients under the name of the Nembrodes, is situated to the south of the preceding range, extend- ing in the same direction. Numerous less elevated branches join these two larger chains, intersecting the district of Sicily in every direction. B 2 4 RAMBLES OF A NATURALIST. mains of the conqueror of Lepanto*, is crumbling to ruins, with all its treasures, unheeded ; while, at a distance of six miles, lie the colossal ruins of Selinontef, the ancient rival of Carthage and of Syracuse. At Salerni and at Calatafimi, the old Saracenic and Norman castles have opened their dis- mantled keeps to a ragged population, in whom our presence seemed to excite the most indescribable astonishment. At Alcamo, a town containing 20,000 inhabitants, and having broad well-paved streets, which is situated on the only high road of Sicily, and is one of the principal places of resort of the Palermo grandees when they do chance to travel, we were obliged, as everywhere else, to lend the landlord of the hotel money to buy our dinner. Through the whole of our journeyings, along unbeaten tracts as well as in the high road, every traveller we met had a loaded carbine slung across his saddle * Amongst the other curiosities contained in this church I may instance, in addition to the tomb of Don John of Austria, the four Sibyls, which are placed side by side with the four Evangelists in the Choir. f The town of Selinonte, which was almost always at enmity with Segeste, and often in alliance with Syracuse, continued for a long time to prosper in its wars. It succumbed for the first time to Hannibal ; but the inhabitants, having been brought back to the charge by Hermocrates, re-took the town. Although Selinonte was almost always a tributary of the Carthaginians, it promptly revived, until, being successively besieged by the Syracusans and the Carthaginians, it called the Romans to its aid, and soon fell to rise no more. No ancient city in Sicily affords so high an idea of the religious feeling and of the wealth of its inhabitants, as Selinonte Accumulated in a vast solitude, bounded by distant mountains and the neighbouring sea, these colossal ruins and memorable sanctuaries strike the imagination with astonishment. THE COASTS OF SICILY. 5 — a precaution which either betrayed an adherence to the manners of a bygone age, or the necessity of being prepared for the chance of existing danger. To crown all, the cultivation of the potato* had not * Botanists call this plant the Solanum tuberosum. We would observe here that the tubers, or tubercles, which we eat, are not the roots of the plant, as is generally supposed, but true subterranean stems or branches, which are enlarged at different parts, and which owe their nutritive properties to the great quantity of amylaceous matter or starch which they contain. We will extract from M. Duchartre's work, the following historical details in reference to the origin and the progress of the cultivation of the potato in Europe : — " The potatoe was known from time immemorial in Peru, where the inhabitants designated it by the name of papas, but the true place of its origin has not yet been precisely determined. It was introduced into Europe about three centuries ago, for it would appear that Captain John Hawkins first brought it to Ireland in 1565, having procured a few roots at Santa Fe de Bogota. These plants were, however, entirely neglected ; but the celebrated navigator, Francis Drake, who had been the companion of Hawkins, fully comprehending the importance which this acquisition might prove to Europe, carried some of these plants to Virginia, from whence he afterwards conveyed them to London in 1586, and this circumstance has led to the belief that the potatoe was a native of Virginia. Drake gave his specimens to his own gardener, and amongst others to the botanist Clusius, who was the first to recognise the botanical character of the plant. The new plant was, however, entirely forgotten, until Sir Walter Raleigh, finding it again in Virginia, brought a large number back with him to England in the beginning of the seventeenth century, and this time the introduction of the plant proved definitely successful. " Still the cultivation of the potatoe made very slow progress, and a convincing proof of its scarcity is shown by the fact, that in 1616 a dish of these vegetables appeared at the table of the King of France as a rarity of high price. It did not penetrate into Germany till 1G50, and until the close of the eighteenth century was only cultivated in limited districts. It was through the efforts of Par- mentier that it became generally diffused in France ; and probably B 3 6 RAMBLES OF A NATURALIST. yet penetrated to this region — a fact which, perhaps, more than any other, illustrates the stationary con- dition of this part of Sicily; indeed, during the whole time in which we were stationed west of Palermo, we were never able to procure these vege- tables, which everywhere else constitute an almost unfailing resource to the poor. The road which we had taken led us back to Pa- lermo. We once more passed through this town, after having admired, for the last time, the strange and magnificent church of Morreale ; we took a hasty survey of the castle of La Bagaria, which stands in the midst of its princely villas like a king surrounded by his court; we next reached the ancient Himera which, under the modern name of Termini, yearly attracts a vast crowd of persons who come to seek health at the warm springs for which this place is celebrated. This part of our journey af- forded us the greatest possible enjoyment, for the weather, which had previously been cold and rainy, had become fine and settled within the preceding few days, whilst the land displayed in every part a most exuberant vegetation. Our road followed the irregularities of the coast, skirting from time to time at the foot of mountains, and was sometimes bordered with rose-laurels in full blossom*, and his attempts would have proved ineffectual, had not the famine which followed the first wars of the revolution compelled men to submit their prejudices to the pressure of necessity, and in a few years' time the potatoe spread to the smallest villages of France." * The shrub which is designated by this name, belongs, in reality, neither to the genus or family of the Laurels, but to the genus Nerion, and to the family of the Apocynacece. The species to THE COASTS OF SICILY. 7 sometimes by tall, shrub-like Solanaceae*, in the midst of which rose the smooth stems of the gigantic Agavef, which were often upwards of twenty feet in height. Long-tendrilled vines encircled, with their indented leaves, the trunks of the flowering Cactus, and blended their light and graceful garlands with the strangely twisted branches of these un- which we here refer is the one generally cultivated in our gardens. It grows wild along the brooks and streams of almost all the districts skirting the Mediterranean, and hence its abundant occurrence on the shores of the Eurotas was not an exceptional case. Botanists designate the shrub under the name of Nerium oleander. * The family of the Solanacece is very remarkable on account of its including plants, some of which are thoroughly impregnated with the most deadly poisons, whilst others, on the contrary, yield substances which are alike nutrient and agreeable to the taste. Among the former, we may instance Belladonna (Atropa belladonna), the Mandragora (Atropa. mandragora), Henbane (Hyoscyamus niger), Stramonium (Datura stramonium), Common Night-shade (Solanum nigrum), Tobacco (Nicotiana tabacum). All these plants owe their poisonous properties to special principles, which che- mists have succeeded in isolating, and which they have ^called, in accordance with their various sources of origin, Atropine, Hyoscy- amine, Daturine, Solanine, Nicotine, &c. Among the edible plants of this family we may mention the Pimento (Capsicum annuum), the Tomato (Li/coper sicum esculentum), the Egg-apple (Solanum melonyena), and more especially the Potato (Solanum tuberosum), whose history we have already briefly sketched in a preceding note. f This species, which is incorrectly designated under the name of Aloe, belongs to another genus, and is the Agave americana, a native of South America. This Agave was imported into Europe in 1561, and is thoroughly naturalised in most of the countries bordering on the Mediterranean. In Sicily it grows wild among the rocks, and it is planted round fields to form hedges, which are rendered absolutely impenetrable by its enormous leaves, bristling with thorns. B 4 8 RAMBLES OF A NATURALIST. wieldy plants. Woods of Olive trees, and groves of Orange, Citron, and Carob trees, gave variety to the landscape. Sometimes we caught a glimpse to our right of some small valley, lying within the recesses of the mountains whose sides were clothed with verdure enlivened here and there by patches of thickly clustering rose bushes, which were covered with a thousand small red or white blossoms, whilst to our left the sea stretched its bright blue horizon as far as the eye could reach, bounded by its pictu- resque and deeply indented shores, and by the lofty promontories, whose summits were often crowned with the rich tufts and expanded leaves of the tall date tree. On approaching Cephalu, the experienced eye of Carmel had recognised the Santa Rosalia with her sails spread, hastening towards our place of rendez- vous. Our bark and our mules arrived at the same time, and in a few moments we were steering to- wards the peninsula of Milazzo. For the first hour the shore along which we were sailing was as rich and beautiful as the one we had just left ; but after a time the mountains increased in height as they approached the shore, and seemed, with their sharp and clear outlines, as if they had just emerged from the sea ; but still they were green and richly varied. The scene was very different from that desolate region, and those arid and rugged rocks which had oppressed our sight westward of Palermo ; here, everything betrayed the presence of man, and of a more active state of civilisation. Numerous vil- lages appeared in the distance, their white houses THE COASTS OF SICILY. 9 and turreted steeples rising from the midst of fields and rich clumps of trees, whilst almost every bay along the shore had its own group of habitations clustered around some protecting tower or fortress, whose services were fortunately no longer needed,, since the conquest of Algiers. When we turned away from this picturesque landscape, which lay to the right of our boat, we saw before us the island of Lipari, which seemed gradually to rise from the bosom of the waves, its sister islets, Alicuri, Fili- curi, and Saline forming at our left a vast semi- circle, while behind us the sun, like a reddened ball, sunk beyond the arched promontory of Cephalu, bathing land, sky, and sea in a glowing tint of the richest ochre. At the break of day, we were opposite to Mi- lazzo*, and a few hours afterwards we had taken possession of most comfortable quarters, admirably situated for our researches. Through the kind intervention of the French Charge d' Affaires, M. le Baron Lucifero had generously given us the use of his country-house, which was situated at the extreme point of the peninsula, and only at a few minutes' distance from either coast. Our tables were soon arranged and supplied with all the apparatus necessary for our work, and without further delay we began to explore our new domain. Similar in this respect to the islands of Favignana, * Milazzo is the ancient Milas, -where the consul Duilius gained the first naval victory over the Carthaginians, 260 years before the Christian era. To perpetuate the memory of this triumph, the Romans erected a rostral column, which is still in existence. 10 RAMBLES OF A NATURALIST. Milazzo is never -visited by the few strangers whom the love of travelling leads to Sicily. This little town, which entirely occupies the narrow isthmus on which it is built, is surrounded on the one side by the peninsula which bears its name, and on the other by a small plain which is partially enclosed by the semi- circular chain of the Pelorias mountains, behind which may be seen the distant summit of Mount Etna. Narrow paths, which are only practicable for the mules of the country, communicate with the high roads of Messina and Palermo. The inhabitants of Milazzo, who are thus isolated from the rest of the island, appeared to us to exhibit much more energy and activity than the rest of their countrymen. We had nowhere met with so good a mode of cultivation, for not an inch of ground is lost either on the plain or the peninsula. Vines and Olives almost everywhere supply the place of the Cactus or the Agave, and descending to the very water's edge, they afford shade to the simply but elegantly built country-houses, whose terraces overhang the sea. A small harbour, which is well sheltered against the west and north winds, is fa- vourable to the export of the different products of the soil, and this trade is sufficient to keep the population in a condition of ease and comfort. The streets near the harbour are broad and tolerably well built, but they change into winding lanes, as they as- cend the steep hill, which, rising perpendicularly on the west side, is surmounted by a fortress which is manned by a tolerably large garrison. Milazzo was for several years the residence of Louis Philippe, TIJE COASTS OF SICILY. 11 then Duke of Orleans, who, having been banished from France on account of his name, and not per- mitted to remain at the court of Naples on account of his liberal opinions, came to seek an asylum in this remote corner of the world. It may be, that in the midst of the splendours and the troubles that chequered his life while he was king of the French, he often recalled the humble white cottage which was pointed out to us by our guides as his former residence ; and it may be, too, that even without foreseeing the sorrows of exile, he may often have regretted the calm and peaceful days he spent at Milazzo. The peninsula of Milazzo consists of an irregu- larly-shaped and somewhat elliptically formed tongue of land, whose greatest width scarcely measures a mile and a half, but which extends nearly six miles into the sea at right angles from the shore. Its geo- logical constitution is very remarkable ; for the coast, from which it seems to take its origin, consists of sandstone for a considerable distance in all directions, but, as soon as we pass beyond the isthmus, we find that the rocks are composed of gneiss and mica schists, both of which are of more ancient origin. These rocks extend over the greater portion of the territory, and form in the centre of the peninsula a small mountain, known as the Monte Venereo. Beyond this we find strata of the same nature for a short distance, but these rocks soon disappear under beds of round pebbles, and sand transformed into sand- stone rock. Beyond this again, on the borders of a steep cliff, there is a thin stratum filled with 12 RAMBLES OF A NATURALIST. fossils, belonging to the Palermo limestone, while the extremity of the cape consists of compact calcareous rock, which penetrates to some depth. This locality, therefore, presents in their order of natural superpo- sition, specimens, as it were, of almost all the principal strata, which, either isolated or combined into large masses, compose more than two-thirds of Sicily. These calcareous strata, of which we have spoken, have been worn away by the action of the waves, and hollowed into recesses and basins, in which grow thick tufts of Algae and Fuci, which afford asylums to numerous marine populations. These excavations constituted so many preserves, which promised us the most ample success. We had also reckoned upon finding numerous representatives of different littoral species under the detached blocks of stone, which are here scarcely covered by more than a few inches of water, but we soon saw that an unforeseen circum- stance would frustrate our hopes. Under the influ- ence of conditions which are somewhat difficult to understand, but amongst which a more or less power- ful evaporation undoubtedly plays an active part, the water of these seas in some cases dissolves, and in other cases deposits a certain quantity of the lime which it has removed from the submerged rocks. In the latter case, the calcareous matter is deposited like a sort of varnish on the surface of the stones and boulders, which it agglutinates to one another, and thus blocks up the passages, by which Annelids and Worms of every kind might otherwise penetrate into the interstices of the stone. This incrusting matter presented a very great resistance, and the THE COASTS OF SICILY. 13 united efforts of our men, although they were provided with powerful levers, were often insuffi- cient to displace a stone, which, had it been free, any one of our party could easily have moved with his unaided hands. While this gradual deposition goes on, the sedi- mentary rock retains and encloses in the mass small isolated pebbles, and sometimes even the remains of human industry. This remarkable fact, combined with others of the same nature, at once explains and refutes the opinions of some geologists, who have at- tempted to refer the appearance of man on the surface of the globe to a very remote period. The sedimentary rock of Milazzo is of a very compact structure, and as it fully equals in hardness the primary limestone which it covers, it would be easy at first sight to confound the two. The discovery in rocks of recent formation of fragments of brick and earthenware might, therefore, lead to the inference that these remains were contemporaneous with the rock itself, if one did not bear in mind that a similar phenomenon is daily taking place before our eyes. The incrustation of the rocks of Milazzo is a fact analogous to those which have been observed on the shores of some of the islands of the Archipelago, and which are exhibited on a larger scale along the rocky heights of Guadaloupe. Here the sea has incrusted and united immense masses of sand and fragments of shells, converting them into a sort of breccia. In these breccias, human bones have been discovered, intermixed with a few traces of a rude stage of civi- lisation; but there were also found in the same deposits 14 KAMBLES OF A NATURALIST. different remains of European vessels that had been shipwrecked within the last few years. It is, there- fore, evident that the formation of these marine rocks of Guadaloupe is proceeding with great rapi- dity, for their whole mass, although of considerable extent, belongs exclusively to the present geological epoch. The bones and debris of every kind which are found there cannot, therefore, be regarded as fossils, since this expression is limited to those or- ganic remains which are contemporaneous with pre- ceding geological epochs ; and hence it may be said that in our day, no less than in the time of Cuvier, a true fossil man is a discovery that still remains to be made. Notwithstanding the unexpected difficulty which the agglutination of the stones threw in the way of our researches, our sojourn in the peninsula of Milazzo was productive of much enjoyment to all of us. The daily increasing heat seemed to give rise to a marvellous development of life, both on the land and on the sea. Thousands of insects, many of which had never found a place in our zoological catalogues, were swarming over the fields and woods, and M. Blanchard found no difficulty in filling several cases with numerous and curious specimens. Some living reptiles, too, were caught and added to our col- lections, and they still constitute a portion of the spe- cial menagerie which was established at the museum by MM. Dumeril and Bibron. We collected, amongst others, two large black snakes, which were perfectly harmless, notwithstanding their formidable appear- ance ; and some fine specimens of the Guecko, an ani- THE COASTS OF SICILY. 15 mal which is somewhat similar to a lizard, but whose flat body, short tail, and greyish skin covered with tubercles, give it a very repulsive appearance. Like the majority of its congeners, this Gecko, which is vulgarly known as the Terrentola, is the terror of the inhabitants of the country, who regard it as very venomous, and watch with horror the rapidity with which it runs along the smoothest walls, on which its claws and the scales that cover its toes enable it easily to find points of support. Nothing, however, that we heard in regard to this animal can compare with the terrific reports that are made of it by some travellers in the East, and at the Cape of Good Hope. There the Geckos are regarded as accursed beings, disseminating death around them, sometimes causing their victims, by a mere touch, to perish in a few hours, and sometimes giving rise to an incurable leprosy by a slight bite. It is not easy to determine how much truth there is in these evident exaggerations ; but when we re- member the absurd stories that are commonly circu- lated and believed in our country districts concerning the Salamander and the timid Newt, one is led to think that the Gecko may be a perfectly innocent animal, and that its nocturnal habits may have been the principal means of rendering it an object of terror. Whilst M. Blanchard was carrying on an active war against these inhabitants of the land and air, M. Milne Edwards and myself were directing all our efforts to the sea ; and to our various means of inves- tigation we were now going to add another, which 16 K AMBLES OF A NATURALIST. was more powerful than any which we had hitherto employed. Instead of merely exploring the acces- sible parts of the shore, or dredging at hap-hazard, we were now about to descend to the bottom of the sea ; and, in the enjoyment of perfect liberty of action, we were actually going to pursue the marine animals into their most hidden retreats within the recesses of those rocks, which were so deeply buried beneath the waves as to appear to defy all our efforts. The execution of this project, the idea of which originated with Milne Edwards, demanded some precautions. First, it was necessary to be well as- sured of the working condition of our apparatus, and so to combine and arrange its different parts, as to foresee all possible accidents, and to secure the means of remedying them, should they occur. In the course of a few days, everything was arranged, and after some preliminary trials, M. Milne Edwards made his first submarine excursion within the harbour of Mi- lazzo. For more than half an hour, he remained at the bottom of the sea, which he traversed in all directions, turning over the stones, examining frond by frond the tufts of Algas, and collecting together and observing on the spot the different zoophytes which live at a depth of from ten to thirteen feet below the surface of the water. After this first attempt, M. Edwards descended to much greater depths ; and in the Bay of Taormine and elsewhere, we saw him, at a depth of upwards of twenty-five feet below the surface of the water, working for more than three-quarters of an hour to detach with a pickaxe some of those large Panopeas of the Me- THE COASTS OF SICILY. 17 diterranean, which had been known only by their large bivalve shells. The apparatus employed by M. Milne Edwards in these submarine explorations was that which had been invented by Colonel Paulin, a former Com- mandant of the Fire Brigade of Paris, to be used in case of fires in cellars. A metallic helmet, pro- vided with a glass visor, encircled the head of the diver, and was fastened round the neck by means of a leather frame supported by a padded collar. This helmet, which was in truth a miniature diving- bell, communicated by a flexible tube with the air- pump, which was worked by two of our men, whilst two others stood ready to replace their companions. The rest of the crew, under the orders of Perone, held the end of a rope which, passing through a pulley that was attached to the yard, was fixed to a sort of harness by which we were enabled quickly to draw up and embark the diver, who had been drawn to the bottom of the water by means of heavy lead soles, which were kept in their places by strong straps. M. Blanchard took charge of the air-tube, and watched that it did not become twisted by the different movements made by M. Edwards or by the swaying to and fro of our boat, while I retained in my hand the rope by which the diver was to make his signals, and God only knows with what anxiety I watched its faintest motion. This will be readily understood on considering that the slight- est mistake might have proved fatal to M. Milne Edwards. Notwithstanding all our care, the means of safety at our disposal were very imperfect; for it VOL. II. C 18 RAMBLES OF A NATURALIST. required fully two minutes to draw the diver from the water and loose his helmet. On one occasion the yard cracked, and threatened to break at the very moment when I had given orders to haul in the rope under the impression that I had received a signal of distress; our men instantly sprang towards the water, and they would soon have brought M. Edwards to the surface, but more than five minutes elapsed between the moment when I thought I felt the cord move, and that in which M. Edwards was able to breathe the air freely ; and this length of time would have been more than suf- ficient to determine a fatal condition of asphyxia. Happily, however, I had been deceived by an in- voluntary motion imparted to the telegraphic line ; but one may easily perceive that researches of this nature were not devoid of danger, and it certainly requires an amount of zeal very uncommon among naturalists of our day to risk so perilous an under- taking. M. Edwards, however, reaped an ample harvest as the reward of his labours ; for each time that he returned from the bottom of the sea, his box was richly laden with Molluscs and Zoophytes. The most precious, however, of all the treasures which he collected from these submarine depths, was an immense quantity of the ova of Molluscs and An- nelids. After being deposited in small basins, to which the waves entered merely by penetrating through the walls of dry stones which had been raised around them, these eggs continued to be de- veloped, and thus enabled M. Edwards to study THE COASTS OF SICILY. 19 at his leisure every phase of their curious evolution. I for my part found in the grottoes of the Cape a large number of Annelids, Nemertes, Planarias, and Phlebenterous Molluscs, and I also discovered a new species of Gasteropodous Mollusc allied to those Tritonias, whose organisation was first made known to us by Cuvier. The Sicilian species, although of smaller size, is much more remarkable than the one which inhabits the coasts of France. Figure to yourself a little slug of a somewhat elon- gated shape, bearing on its sides a row of branchiae, looking like so many exquisitely delicate living tufts. In the place of the smooth and opaque ten- tacles of our snails, imagine two large crystal horns, from each of which escapes a tuft of rosy branches, intermingled with violet-coloured blossoms ; and lastly stretch over the front part of its head a spangled veil of the finest gauze, and you will have some idea, although a very imperfect one, of this lovely little creature, which is one of the most mar- vellously beautiful living gems that I have ever seen. Although the localities adapted for our researches on the isthmus of Milazzo were rich in animal species, they were of limited extent, and three weeks sufficed to exhaust them : this circumstance, together with the advanced season of the year, combined to make us think of hastening our departure. From the terraces of the Villa Lucifero, we could perceive a black cone rising abruptly from the sea, which was almost always encircled by a light cloud of smoke. This was the island of Stromboli, whose c 2 20 RAMBLES OF A NATURALIST. volcano being in a state of incessant activity, serves as a natural beacon light to vessels passing from Naples to Messina. After having visited the gra- nitic, schistose, and calcareous rocks, and after having studied the populations belonging to each of them, we wished now to compare them with the coasts and fauna belonging to volcanic districts. We therefore set sail for Stromboli, and the evening of our departure was followed by one of those glorious nights which seem to appertain especially to the favoured climes of the South. The sun had disappeared in the west in a bed of gold and purple, the stars had risen in the east and spread over the entire vault of heaven, while the thousand rays of their phosphorescent and quivering light threw so bright a gleam over land and sea that we were now able to distinguish, as through a thin and filmy veil, the distant chain of the Pelorian mountains, and the summit of Mount Etna. The wind was blowing gently from the south, at one time swelling our lateen sail, and at another letting it flap loosely against the mast, so that our sailors were obliged to have recourse to their oars. One of our men would then begin a monotonous song, while the oars, rising and falling in cadence with the voice of the singer, seemed to harmonise with the rhythm of his wild and sonorous chant. Each stroke of the oar was followed by a tremulous phosphorescence which, vanishing almost as soon as it was perceived, revealed to us the presence of those minute animal- cules which produce light as the torpedo engenders electricity. When the breeze again sprang up, the THE COASTS OF SICILY. 21 chant ceased^ and the oars were drawn in and laid along the side of the boat, while our men, stretched upon their benches, resumed their interrupted slum- bers, and the light splash of the water round our prow was the only sound that broke upon the si- lence of the sea, which is at all times deeper than that on land. We continued for a long time to admire this scene, whose grandeur was due to its calm simplicity, and then stretching ourselves upon our mattresses, which were screened by a slight awning, we too fell asleep, soothed to rest by the scarcely perceptible oscillations of our boat. By break of day we were all again on the alert. The Cape of Milazzo was very far behind us, and yet Stromboli seemed to be scarcely any nearer. In these warm regions the extreme transparency of the air for a long time deceives the northern traveller as to the actual length of distances. We had thought when we left Milazzo that we were not more than twelve or fifteen miles from Stromboli, instead of which these two points are in reality separated by about forty miles. We had scarcely made half the distance since the preceding evening, but at this moment the wind freshened, and the dark moun- tain seemed to grow before our eyes as we ra- pidly approached it, and we were soon able to distin- guish its rugged sides, its lava and trachyte beds, its strangely twisted rocks with its beach of fine sand, which was black like the rest of the island, excepting where the waves as they broke seemed to leave a line of milky foam in their wake. Stromboli, properly speaking, is only a volcanic c 3 22 RAMBLES OF A NATURALIST. cone, measuring about nine miles in circumference, and rising to a height of about 2000 feet above the level of the sea. To the south the declivity, which is composed of old scorias, becomes a little less steep, and forms a narrow and inclined plane, over which are scattered about thirty houses, the materials of which have all been supplied by the lava. A few other habitations are clustered together in the north of the island in a somewhat similar locality, and here a little white- washed church forms a striking object by its contrast to the dark rocks around it. In the midst of the lava and scoriaB which have been decomposed by the slow and gradual action of suc- ceeding ages, a few garden vegetables and some vines are cultivated, but the produce of these plants would be insufficient for the maintenance of the population, if they did not find lucrative employment in the coral fishery. The mode of collecting the coral, which we had an opportunity of observing, remains at the present day the same as it was a century and a half ago, when it was fully described by Marsigli.* Each boat includes at least three men, who are provided with a cross, to whose equal arms are attached strong hempen nets. A large stone, which is placed in the centre of the apparatus, draws it rapidly to the bottom of the water, and not unfrequently to a depth of two or three hundred feet. While one of the Marsigli, who was born at Bologna of a noble family, died in 1730. He was distinguished as a soldier and as a man of science. His principal work on natural history is entitled " A Physical Essay on the History of the Sea." THE COASTS OF SICILY. 23 fishermen is alternately raising and lowering the machine, the remaining two or three men are engaged in gently rowing the boat, so as to sweep over a certain space ; after a time the whole is drawn in, and the fragments of coral which have been torn up and retained by the meshes of the net, are carefully removed. A rapid survey sufficed to show us that our zoo- logical researches would not be extended by a pro- longed sojourn at Stromboli ; animal life seeming to shun these calcined rocks, which are as sterile under water as they are in the open air ; but before quitting this district, we were anxious to visit the volcano. The receiver of customs, who had provided us with safe guides, agreed to accompany us, and each of us being provided with a stout stick or pole, we soon began the ascent. A very steep path in the midst of the moving sand led us, after three quarters of an hour's walking, beyond the zone of the vineyards. Here our difficulties increased; for the ground, which was more and more inclined, became less firm as we advanced, and was, moreover, covered with large thistles, whose sharp prickles penetrated at every step through our thin clothing. We very soon, however, passed beyond the limit of these prickly plants ; for now every trace of vegetation disappeared, and we saw nothing around us but the old beds of lava, which in one place had been accumulated to- gether like enormous scoriae, whilst in another they were entirely concealed beneath the black and hot ashes which we could feel sliding from under our feet at every step we endeavoured to take in advance. c 4 24 KAMBLES OF A NATURALIST. This part of our expedition was very arduous, and we were more than an hour in reaching the eastern summit of the island. Here we found a narrow ledge like the angle of a roof, the two sides of which sloped each in its own direction ; the left- hand declivity led to the part of the mountain which we had just quitted, whilst the right-hand slope, whose inclination was precisely that which would be assumed by moving substances obeying the laws of gravity, presented a perfectly smooth surface, which was terminated by a rock, lying about 1500 feet below us, and overhanging a vertical precipice. We crossed rapidly over this edge, and reached the summit of the old cone, which is more than 600 feet above the present crater, which opens on its crumbled sides. As if to celebrate our arrival, the volcano saluted us by an eruption. We saw the abyss kindling at our feet, whilst a magnificent jet of fire rose towards us with a noise resembling the repeated discharge of artillery. Standing immediately above the crater, and unable to advance far over this moving soil, we were impeded in our observations by the mountain itself; whilst we were moreover almost constantly sur- rounded by clouds impregnated with stifling gases. To avoid these inconveniences, we descended to a lateral ridge, where we were able at our leisure to contemplate the desolate scene displayed before our eyes. Three concentric ridges, of which the two outer ones are partially destroyed, encompass the volcanic crater. Behind us steep declivities stretched down to the cultivated regions, which we had found THE COASTS OF SICILY. 25 it so arduous to traverse, but which appeared, when seen from our elevated position, to be a mere plain. To the left our eyes rested on the highest peak of the island, which was once a portion of the most ancient and the outermost of the three concentric ridges, and which was separated from us by a deep ravine. To the right was the small elevation from which we had just descended ; whilst in front of us the ridge on which we were standing curved in a semicircle towards a mass of lava suspended over a precipice, and at the same time enclosed a steeply inclined mass of cinders and scoria3 abruptly cut by the edges of the abyss, into which the existing crater opens. This crater encloses within its walls six distinct mouths. Two of these secondary craters eject that smoke, impregnated with hydrochloric and sulphur- ous acid gases, which is at all times being emitted from the summit of the mountain. The third mouth, which is situated to the right, also throws out a thick and whitish smoke, in the midst of which red fiery stones flash like sparks as they incessantly rise and fall in the midst of a strange noise, resembling the heavy surf driven on a storm-beaten coast, and making one involuntarily think of the mythical caves of the demons. To the left lie the three mouths which exhibit only intermittent eruptions ; two of these evidently belong to the same focus, for they always kindle and become extinguished simultaneously. The third, whose eruptions are much less frequent than the others, is nearest to the spectator. The most formidable detonations proceed from this crater, 26 KAMBLES OF A NATUKALIST. which, moreover, throws up the highest jets of burning cinders and rocks. As we had arrived in broad daylight, we had been enabled thoroughly to examine all these rocks of lava, and at our leisure to contemplate the steep ridges, the declivities of ashes, and all that singular scene whose uniform blackness was only broken in a few places by masses of sombre red scoria? ; but the sun had now set, and the short twilight of these southern latitudes was rapidly giving place to night. In proportion as the light became extin- guished in the sky, it seemed to revive within the depths of the abyss. The smoke assumed a redder tint, becoming . gradually more and more fiery, the showers of sparks increased, while the concentrated light within the crater itself enabled us better to follow each varying phase of the eruption. The explosions of the two smaller mouths recurred every seven or eight minutes, whilst ten or twelve minutes intervened between the eruptions of the large crater. The phenomenon was always effected in the same manner; thus, for instance, at the moment when the volcano began to exhibit signs of activity, the smoke which issued from the openings to the right, rapidly assumed a bright and vivid red colour, while more and more quickly recurring detonations pre- ceded every jet of burning matter. These jets were thrown up in diverging directions, and almost with- out any smoke, from one of the two sister-craters, whilst from the other they darted upwards, as if im- pelled by the current of violet- coloured vapour that escaped from the mountain with a loud whistling THE COASTS OF SICILY. 27 sound. The principal crater ejected a broad and expanded jet of incandescent rocks and lava, which nearly reached the platform on which we were standing, and fell with a loud noise, one portion being carried into the sea, and the remainder thrown back into the abyss from whence it had been ejected, whilst the wind blew over us clouds of the black and fine sand and ashes. The night had long since closed around us, and our guides were urgent that we should make the descent ; we were therefore compelled to yield to their request, and prepare for our return; but before we made our final retreat, we waited to see another eruption, and this fortunately proved to be most magnificent. The three mouths were playing si- multaneously, and reflecting the reddish brightness of the lava, whilst the triple enclosure of the crater revealed itself once more to our eyes. After we had sufficiently admired this grand spectacle, we took one of the paths to the right, which being entirely formed of fine sand, facilitated our return quite as much as it aggravated the difficulties of our ascent. Our guide had assured us that on this side of the mountain there was not a single stone to be met with, and on the strength of this assertion, M. Edwards and myself set off at full speed, and soon left our more circumspect companions far behind us. There was something very singular in this descent. The blackness of the soil absorbed the faint rays of the stars, while the night was so dark that I could scarcely see the white jacket of our guide at three paces in front of me. Impelled by my own impetus, 28 RAMBLES OF A NATURALIST. and by the declivity of the mountain, I advanced without fatigue, but with no direct aim and as if I were moving in a dream, in the midst of thick dark- ness, over ground which slid away from my feet. In ten minutes' time, we had passed beyond the limits to which the ashes and cinders extended, and here it became necessary to proceed with the greatest caution, as we had literally to feel our way for the rest of the descent. Our hands were touching the O edges of steep declivities which we could not see, and the extremities of rocks which we were obliged to descend step by step. At length, however, we reached the shore without accident, where in about half an hour we were joined by the rest of our party. Without loss of time, we at once returned to our boat in order that we might observe the volcano from the sea ; the view, however, was not nearly so striking as on the mountain itself, the crater being too distant from the spectator. We may indeed dis- tinguish the jet of burning matters which are thrown up from the volcano, but the scene has none of that magnificent grandeur which it possesses when it is viewed from the mountain top, where the incandescent smoke rises in eddying clouds round the old and half- crumbled cones which are illuminated by the tempo- rary flashes of the eruptions. This slight disappointment, however, did not make us regret our nocturnal expedition ; for the sea, as if by way of atonement, exhibited to us in all its splendour the glorious phenomena of its phospho- rescence. For more than an hour, the waters around us seemed to be kindled into a blaze of light, as if THE COASTS OF SICILY. 2\) they had borrowed some of the hidden fires of Strom- boli. The waves as they broke along the reeky shore encircled it with a glowing band of light, whilst every projecting cliff was circled with a wreath of fire. Our boat seemed as if it were opening for itself a passage through some glowing and fused liquid, whilst in its wake it left a long track of light, each stroke of the oar brightening the bosom of the waves with a broad silver gleam. The water that was taken up in a bucket presented the appearance of molten lead, as we slowly poured it back into the sea. Everywhere over this brilliant surface of calm light, myriads of dazzling green sparks and globes of fire were flashing, quivering and dying amid the undula- tions of the waves, and these sparks and globes of fire were so many living beings — animals belong- ing to the Crustaceans, Annelids and Medusae. At certain times of the year, and probably at the period in which the accomplishment of the reproductive functions requires a superabundant manifestation of vital activity, these microscopical beings acquire the property of emitting light at each muscular con- traction; and hence every movement in these animalcules is made apparent by a luminous flash. The numerous observations which I made on the coasts of Brittany and Normandy, led me long ago to this conclusion, which has been further confirmed by new researches. Professor Ehrenberg, on the other hand, is of opinion that some Annelids possess, like Glow-worms *, a special organ whose function is * The name of Glow-worm has been given to different species, 30 RAMBLES OF A NATURALIST. to produce light. Fishermen are well aware of the fact that a substance exudes from the bodies of some Molluscs which shines in the dark like decayed wood or putrid fish, and in these animals the phenomenon no doubt depends on a slow combustion. Neverthe- less, an observation made by MM. Audouin and Milne Edwards seems to throw some doubt on this explanation ; for these naturalists saw the phospho- rescent liquid of the Pholades flow in a stream along the bottom of a vessel filled with spirit, and com- bine into one mass, where it formed a luminous stratum without losing any of its intensity. It is evident, therefore, that phenomena of a very differ- ent nature have been confounded under the common and even to different genera of the Coleoptera. Those which are met -with in France, more particularly in the neighbourhood of Paris, belong to two species of the genus Lampyris ; the commoner of the two is the Lampyris spkndidula, the other is the L. hemiptera. In these two species the female alone possesses the faculty of producing light. Unprovided with wings, and unable to leave the tufts of grass or the thick bushes which conceal her, she would fail to be discovered by the male insect, if nature had not provided her with a species of torch, which she can light or extinguish almost at will. The luminous organ occupies the three last segments of the abdomen, and is formed by a tissue of a somewhat fatty appearance, in which we discover a large number of trachea?. This abundance of vessels, destined to convey the air into the phosphorescent portion of the body, leads to the supposition that the production of light may here be due to a sort of slow combustion, analogous, for example, to that of phosphorus. The experiments of Macaire, and more recently still those of M. Matteucci, have placed the reality of this explanation beyond doubt. The light of the Lampyris is ex- tinguished in all gases unable to support combustion, while it is rekindled in oxygen, and carbonic acid is evolved. Hence, in this respect, these insects present the same chemical relations as burning charcoal. THE COASTS OF SICILY. 31 denomination of phosphorescence, and that this curious question is by no means settled. After having passed the rest of the night at anchor opposite to Stromboli, we set sail the next morning for Messina. This passage of nearly sixty miles was not entirely lost as far as our researches were con- cerned ; for Milne Edwards and myself had become such good sailors, that as long as the weather con- tinued calm, we were under no apprehensions of sea- sickness. Therefore, while M. Blanchard was ar- ranging his cases, and fixing and labelling the insects which he had found at Milazzo and on Stromboli, we were busy in dropping our bags and nets to arrest in its passage every living creature that chanced to come within reach of our snares. In this manner we procured various remarkable larvae belonging to Annelids and Crustaceans, together with several curious specimens of the Medusidae ; amongst others, the Velella *, a lovely little zoophyte, which possesses more than one claim to our notice. Its dark blue umbrella, which is provided on its lower surface with numerous suckers, is strengthened above by cartilagi- nous plates, enclosing a certain quantity of air, whilst a layer of the same nature, which is placed vertically upon the others, crosses the back of the animal in an oblique direction. Supported on the surface of the water by means of the air with which they are * The Velellas, which were placed by Cuvier among the ordinary Acalephse, have in recent times been classed with the hydrostatic Acalephac or Siphonophora, of which we have already spoken in the first volume. (See the Memoir of Yogt, entitled Siphunophorcs dc la Mer de Nice.) 32 RAMBLES OF A NATURALIST. ballasted, and urged onwards by the wind which strikes their vertical plates like so many sails, the Velellas often float in large numbers on the waves. We did not, it is true, meet with any of these living flotillas, but we saw several isolated individuals. We also collected some specimens of the lanthina, a charming little Gasteropodous Mollusc, whose body, enclosed in a pale violet-coloured shell, is suspended to a spongy mass looking like consolidated soap froth, which prevents the animal from sinking to the bottom. These various captures enabled us patiently to support the wearisomeness of our voyage, which at one time was interrupted by calms, and at another by contrary winds. At length, after a second night on the sea, which we passed within a mile and a half of the lighthouse of Messina *, we entered the narrow channel, which separates Sicily from Italy, and in another hour we were standing on the quay at the moment when the sun, rising behind the Calabrian * Messina is one of the most ancient cities of Sicily. It is believed to have been founded about ten centuries before our era, when it bore the name of Zancle, and subsequently that of Messana. The position of Messina, its vicinity to the continent, and the beauty of its situation and excellence of its harbour, have made it play a considerable part in the history of Sicily. It has always been regarded as the key of the island, and from this very importance it has suffered greatly. Again and again taken and retaken, re- peatedly destroyed, and as often rebuilt, it has resisted alike the attacks of man and the convulsions of nature. The earthquake of 1783, amongst others, destroyed it almost entirely, and hence it contains none of those ancient edifices which one might expect to meet with in a city whose origin dates back nearly three thousand years. THE COASTS OF SICILY. 33 heights, was gilding the summits of the Pelores, whose chain of mountains stretches as far as the straits, and commands the town. To naturalists, who, like ourselves, had not had any society for nearly four months beyond that of their boat's crew, Messina possessed a special attraction. We even met with persons here to whom we could speak on scien- tific matters, and at the hotel of La Vittoria, we en- countered the celebrated German traveller Riippel, who, after two years' travelling in Abyssinia and on the borders of the Red Sea, had come to Sicily to study the fishes of the Mediterranean. While we remained at Messina, our labours were daily shared by several distinguished men, whose acquaintance we were fortunate enough to make during our stay ; amongst these, we may mention M. Tardi, a young mathematician already known by several interesting publications ; Dr. Cocco, a naturalist who struggles courageously against the indifference of an ignorant public and the bad will of a suspicious government ; and Dr. Cupari, whose rare talents have led him to be called to the University of Pisa; and, thanks to this pleasant intercourse, our labours seemed at once more easy and more productive of valuable results. However, it was time soon to return to our wander- ing life, for ten days had sufficed to explore the harbour of Messina and the sand thrown up by the whirlpool of Charybdis. The Santa Rosalia was therefore again put to sea, and skirting along the rugged coast, which borders this portion of Sicily, we entered the little harbour of Jardini at the foot VOL. II. D 34 RAMBLES OF A NATURALIST. of the mountains on which stands Taormine *, with its magnificent amphitheatre facing Mount Etna, whose black lava beds reached nearly to the point which we occupied. Here we resumed our labours with increased ardour, and feeling that the close of the season was now approaching, we directed our efforts rather to the completion of the studies which we had already begun than to the attempt of making new discoveries, and in this respect the Bay of Taormine was admirably adapted to our purpose. Indeed, notwithstanding the oppressive heat, which daily raised the thermometer to the height of 112° F., * On reaching Taormine «from the south coast, the road follows the sinuosities of the sea-shore, skirting along the side of a tolerably well cultivated coast, till it reaches the point of Castel-Sciso, which forms the commencement of a bay, which is bounded by Mount Taurus. It was at the base of this little gulf, that the ancient city rose on different plateaux of the mountain. Owing to its difficulty of access, it was almost always the last place taken by the conquerors of Sicily. The Saracens did not definitely become masters of it until the year 961, and their possession of it retarded for a long time their final expulsion from the country by the Normans. The ancient Tauromenium, which was formerly one of the most splendid cities of ancient Sicily, is now a very unimportant place, but its situation is magnificent, and its ancient ruins, which date from various epochs, offer a variety of aspects, presenting a degree of incomparable beauty. Among its many splendid remains, there is none that can be compared to the amphitheatre. Elevated upon one of the heights, which command the plateau of Mount Taurus* and partly cut out of the rock, this edifice, by its situation, is one of the most picturesque that it is possible to imagine. Its form and its principal arrangement testify to its Greek origin, while Roman splendour is ostentatiously apparent in the traces of thorough re-construction which this theatre seems to have under- gone under Augustus. It was adapted to hold from eleven to twelve thousand spectators. THE COASTS OF SICILY. 35 we completed some of the labours which we had begun at Torre dell' Isola and the other stations which we had subsequently made the scene of our researches. In the course of our various expeditions, Milne Edwards had completed his researches on the Acalephae, and had terminated those observations on the circulation to which we have already referred, and which were subsequently destined to acquire a character of more general application from the eluci- dation afforded by the various collections of M. Va- lenciennes*, who enriched M. Edwards's Memoir with * M. Valenciennes, who is a member of the Institute and a professor at the Jardin des Plantes, occupies in science a position which is very rarely attained, for he is accepted as the chief of a very important section of Zoology, even by those who are opposed to him on special points, and in the estimation of his colleagues he undoubtedly ranks as the first ichthyologist of the age. First as the pupil, and afterwards as the assistant and collaborateur of Cuvier, he commenced with him the work, entitled Histoire Naturelle des Poissons, the first two volumes of which were published in 1828. Six other volumes appeared before the death of Cuvier. In these first eight volumes, the parts contributed by M. Valenciennes are clearly defined by the signatures, which each of these two authors subscribed to his own work. The portions of the work which have appeared subsequently to that period are entirely due to M. Valen- ciennes. It is to be hoped that the difficulties which have so long retarded the completion of this great work, may soon be overcome. Having been admitted from early youth to the intimate acquain- tance of Cuvier and of Humboldt, and being consequently brought into immediate contact with the great founders of modern science, M. Valenciennes was not likely to limit his studies to the external forms of animals. Both in his great work, as well as in all his Memoirs, we find that the anatomical history, is always conjoined to the external description of the animal. Several researches on the incubation of serpents, on the respiration of fishes, and on the minute structure of the tissues, &c., have moreover amply shown D 2 36 KAMBLES OF A NATURALIST. many valuable remarks. Many curious facts, although possessed of less intrinsic value, were now added to these important results. But since the discovery of the method of descending to the bottom of the sea had enabled us to collect an abundant supply of the eggs of a great number of the Molluscs and Annelids, Milne Edwards had devoted his attention almost exclusively to the study of embryology. Facts that relate to the development of living beings have at all times possessed extreme interest ; and in our own day they have acquired an additional importance. There can scarcely be a more attractive spectacle presented to the true philosopher of nature that this naturalist has comprehended and shares the physiological tendencies of our age. Few men have rendered more signal services to the Museum of the Jardin des Plantes than M. Valenciennes. Independently of his labours while assistant to Cuvier, he has arranged two collections in the Museum, which were not represented before his time — viz., that of Intestinal Worms and that of existing Molluscs — and he has completely restored the collection of the Sponges, Echinoderms and Polyparies, while he has thoroughly remodelled the collection of Shells. Unfortunately the result of these very long and arduous labours, in which he has been ably seconded by his assistant M. Rousseau, can only be appreciated by those who have seen the full extent of his work ; for, in consequence of want of space, the greater part of these objects cannot be exhibited to the general public. We ought to observe, however, that no one could be more liberal than M. Valenciennes in throwing open these collections for the inspection of those who are anxious to consult them for the purposes of science. Thus, for instance, M. Valenciennes unre- servedly placed them, together with his own valuable notes, at the free disposal of MM. Milne Edwards and Jules Haime for their Histoire des Polypiers, of MM. Blanchard and Dujardin for their researches on the Intestinal Worms, and of M. Agassiz for his researches on Echinodermata. THE COASTS OF SICILY. 37 than that of seeing life progressively manifested before his eyes in a body which had hitherto been apparently inert, and of watching a seed or an egg becoming transformed into a plant or an animal. The development of a germ realises in its phenomena of evolution the strangest metamorphoses that the imagination of poets had ever conceived, and by its phenomena of epigenesis we are enabled to take part as it were in creations of a still more incomprehen- sible character. All these mysteries, which are accom- plished beneath the eye of the observer, were long regarded as marvellous but isolated facts, which were not investigated beyond the point necessary for their confirmation. At the present day, however, we turn to these facts for a solution of the highest problems of natural philosophy. And here the first question which presents itself is : Where are the termination and commencement of the vegetable and the animal kingdoms ? What are the common attributes of the representatives of these two fundamental types of animated creation ? What are the links that associate the offspring with its progenitors, constituting that ideal being which we term a species ? Deeply in- teresting are questions such as these, which it is perhaps reserved for embryology to answer, now that' naturalists have ceased to limit their studies to a few representatives of the highest types, and have ex- tended their researches to the last links of the great series in the scale of being. Among the most difficult problems that naturalists have proposed to themselves for solution, there is one, perhaps, which they will never definitely solve, D 3 38 RAMBLES OF A NATURALIST. although they are incessantly approximating to the goal of their inquiries, somewhat in the same manner as in geometry, where certain curves only come in contact at an infinite distance with the straight line which forms their limit. The problem we refer to is that of the natural method, which we must be careful not to confound with classification. By this natural method we are enabled to appre- ciate the different relations which connect with one another the elements of a group and the groups themselves ; by classification we endeavour to re- present these relations; but this latter method is necessarily inefficient. Being obliged in our books and delineations to describe and illustrate one by one the objects of our researches, we are enabled to represent each of them in immediate connexion with the object which precedes it and with that which follows it. From hence arise innumerable errors on the part of those, and they are unhappily too nume- rous, who, confounding these two very distinct things, mistake the means for the end and the classification for the method. Let us here refer to the words of a master, who after thirty years' labours and medita- tions appears to have foreseen and protested against the theories, which various false disciples have endea- voured to disseminate in his name. In that Histoire des Poissons, which the illustrious successor of Linnaeus began, and which M. Valenciennes is at this moment completing, Cuvier thus expressed himself : f< The further we advance in the study of nature, the more thoroughly shall we recognise the necessity of considering each being and each group THE COASTS OP SICILY. 39 of beings independently, and in accordance with the character which they represent by their properties and organisation. We shall also see how necessary it is not to abstract any one of these relations, or any one of the links, which unite it either to the most nearly allied beings, or to others. If we once assume this point of view, the difficulties of the question will vanish, and everything will present itself simply and readily to the observation of the naturalist. Our systematic methods of classification only take into account the most proximate relations ; they simply place a being between two other beings, and hence they are constantly at fault. The true natural method regards every organised being as if it were placed in the midst of all the others, it indi- cates all the radiations by which it is more or less closely connected with the meshes of that immense network which constitutes organised nature, and it is only by this method that we can attain to elevated, true, and grand ideas of nature worthy of herself and of the Creator. Indeed, ten or twenty links would often be insufficient to express these innumer- able relations." * What then is that Ariadne's clue, which, guiding the naturalist through the labyrinth, will enable him to see and comprehend, in the case of each of the beings which he is studying, these ten or twenty links of which Cuvier speaks ? This great man * Cuvier has often been reproached for having made classi- fication the aim and object of zoology, but the passage which I have literally transcribed will sljow how unfounded is such an accusation. See the introduction to VHistoire Naturelle des Poissons, tome ler. D 4 40 KAMBLES OP A NATURALIST. thought that they were to be sought exclusively in the organisation of adult animals, and more especially in the nervous system, and in this respect he departed from the principle that had been established by the genius of Jussieu, who sought in the embryo itself the primordial divisions of the vegetable kingdom. Zoology is only now beginning to enter upon that course of inquiry which- has been so long and steadily pursued by botany, and it at length turns to embryology, which has already furnished it with more than one satisfactory reply both in respect to the present and the future. Milne Edwards was one of the first to enter upon this new line of investigation *, and, as early as 1833, on presenting to the Academy a memoir re- lating to the changes of form experienced by different crustaceans, he showed that these metamor- phoses always tend to impress upon the animal a more and more special character, and that they suc- ceed one another in a determinate order, the most important being those which are the earliest mani- fested. Thus, for instance, in the Isopods, a family to which belongs the "Woodlouse (Oniscus), with which every one is well acquainted, the young animal first presents the peculiar characters of the family, next it acquires those which determine the genus, and lastly those which enable us to distinguish the species. About the same time the celebrated German * We here only speak of the application of Embryology to the improvement of the zoological method. We will postpone to a future occasion a consideration of its anatomical and physiological applications. THE COASTS OF SICILY. 41 physiologist Baer * developed analogous principles, and since that date these researches have been con- siderably multiplied ; and if we would here cite all the authors who have furnished proofs in support of this general fact, we should be compelled to give the names of almost all modern embryologists. The most various researches, undertaken and con- cluded by men whose doctrines often differ in respect to many points, have nevertheless led to this one general and identical result, that every germ in the course of development is characterised from the first as a vegetable or animal. In animals the pri- mordial type is distinguished from the very earliest time; next appear the characters essential to the secondary types ; while, at a later stage, those of an inferior zoological importance make their appearance, and so on, until each part of the organism has acquired the proportions, forms and colours, which characterise the species. We thus see that the different phases of develop- * Baer, the author of a great number of works on zoology and physiology, has connected his name with one of the most curious discoveries of the present day. He was the first who saw and studied the ovum of the Mammalia, hut in these observations, which were made in 1827, he compared it to the germinative vesicle, which Purkinje had discovered in the bird's egg. This conclusion led him to draw a fundamental distinction between the elements of reproduction in these two classes. It was not till 1834 that M. Coste demonstrated in the ovule of Baer the existence of a distinct germinative vesicle, and thus completed the discovery of the German physiologist, or rather he assigned to it its true value, by proving that the Mammalia, and Man himself, are propagated by true ova or eggs, which may be compared, in all respects, to those of birds. 42 RAMBLES OF A NATURALIST. ment correspond to more and more closely restricted zoological groups. The embryo acquires first the characters of the sub-division to which it belongs, then successively those of the class, family, tribe, genus, sub-genus, and species. Consequently two embryos which could not at first be distinguished in any way from one another, cease to resemble each other as they continue to grow, if they belong to remote groups, but they continue to be like one another for a longer time, if there exist greater affinities between the two species to which they appertain. Both follow one common road, if we may so express ourselves, until having reached a certain point they take divergent paths, and each assumes its own peculiar and distinctive characters. If these facts be true, and if the consequences that we have deduced from them be correct, animals belonging to one fundamental group and to one and the same great sub-division of the animal kingdom will continue to be like one another during a certain period of their embryonic life ; subsequently they will differ from one another, but they will at no period assume the characters essential to one of the other sub-divisions. The Articulata, for instance, can never assimilate to the Mollusca, nor the Verte- brata to the Radiata. The immense majority of facts which have been collected in reference to this subject, fully justify this conclusion. Nevertheless Loven *, a naturalist of distinguished merit, de- * A Swedish naturalist who has published, among other works, some very important researches on the development of the Cam- panularias and Syncorynes, and who shares with Milne Edwards THE COASTS OF SICILY. 43 scribed a larva which, according to his statement, had undergone the most singular metamorphoses, and which he believed to belong to a family of the Annelids, viz., the Nereids. These animals belong to the Articulata, but the larva was said to possess at one time the characters peculiar to Polypes, which constitute a section of the sub-division of the Radiata. In this case, facts and theory were com- pletely at variance, and many persons in Milne Edwards's place would have treated with contempt an objection borrowed from a small worm who plays but an insignificant part in the animal scale ; but from his familiarity with the study of the inferior animals this naturalist was led to adopt a different course, and from the very first day of our arrival in Sicily, the embryology of the Annelids constituted the spe- cial subject of his studies. From the very com- mencement of his researches, his own views were confirmed in all respects by the clearest and most definite facts, while the apparent exception that had been recorded by Loven disappeared when it was tested by an investigation fully as profound as that of the learned Swede. Milne Edwards ascertained, however, at the same time that Annelids are sub- jected, before they assume their definite form, to metamorphoses, which may, up to a certain point, be compared with those of insects. We will take, by way of illustration, one of those sedentary species, which from their size and their the honour of having discovered the gastro- vascular system of that group of Gasteropodous Molluscs, which I have proposed to desig- nate under the name of the PMebenterata. (See Vol. I. p. 348.) 44 RAMBLES OF A NATURALIST. accurately defined characters are admirably adapted for observation. We will follow through all the phases of its existence that large Terebella ( Tere- bella nelmlosa), whose body, which is of a brown colour spotted with red and white, sometimes mea- sures from six to seven inches in length. On its sides are arranged small flattened protuberances, each of which carries a bundle of simple cirrhi, slightly curved, whilst below there is a row of hooked cir- rhi, whose shape somewhat resembles the cock of a gun. On its back, near the head, are six pairs of ramified branchiae, which being incessantly agitated by the blood, alternately present an amber tint or a deep coral red, according as the liquid leaves their branches or flows through their ultimate divisions. From the head escapes a tuft of a hundred to a hundred and fifty white extensile and contractile filaments, which are ever in motion. These are so many living cables, which the animal is able to ex- tend in every direction to the distance of more than a foot, and which serve it in the place of arms. When fixed by their extremities, they enable the Terebella to raise itself along the most highly polished surfaces, as for instance, along the sides of a glass vessel ; at other times, seizing from a distance grains of sand or fragments of shell, they bring them close to the Annelid, and arrange them round the body in the necessary order to enable the animal to take up these substances, and, by cementing them together with a viscid humour, to form a tube or gallery, often of very considerable length, within which it lives in security. THE COASTS OF SICILY. 45 At the period of reproduction, the entire body of the female Terebella becomes filled with eggs, which by a mechanism which is not yet fully explained are all thrown off simultaneously, and which being retained by a sort of transparent jelly, form at the entrance of the tube a very nearly spherical mass of considerable size. Analogous phenomena occur in the male Terebella, but the fecundating liquid which is expelled by the latter diffuses itself freely in the water, and flowing in all directions conveys life to the germs, which are vivified by contact with it. Here, as in fishes, nature seems to trust to chance to secure the perpetuation of the species, yet nevertheless everything is so arranged, that this great end cannot fail to be fully accomplished. Among the numerous masses of eggs that we had collected in our glasses not a single one proved to be sterile, the strongest evidence that all must have been brought In contact with the vivifying liquid. As soon as fecundation is accomplished, the egg of the Annelid becomes the seat of mysterious move- ments, analogous to those which MM. Prevost and Dumas * were the first to discover in the egg of the * M. Dumas, a member of the Institute, and professor in the Faculty of Sciences and in the School of Medicine at Paris, owes the high position which he occupies entirely to his own exertions. He was scarcely apprenticed as an articled pupil to a pharmacien of Geneva, when he became known for the perfection of his pre- parations of iodine, and being soon afterwards associated with Prevost, he undertook, in conjunction with that learned physician, a series of researches on generation in general, on the embryology of the Batrachians, &c. Being attracted to Paris by that secret instinct which always draws to the largest theatre those who are 46 RAMBLES OF A NATURALIST. frog. The elements of the yolk or Vitellus group themselves in different manners, and finally present four distinct masses thrust into the centre of the egg by a whitish and granular substance. The process of development goes on rapidly, and we soon have before us a sort of spherical sac, whose interior is entirely occupied by the remainder of the Vitellus. No organ is as yet visible; we merely observe two small coloured spots, which indicate the place of the eyes. In this state of extreme im- perfection, the young Terebella bursts through the membrane of the egg; at this period the body is rounded, and bristling in all parts with vibratile cilia. In this condition it resembles certain of the Infusoria, or perhaps still more those reproductive best able to play their part in it, M. Dumas was appointed chemical demonstrator at the Ecole Polytechnique, and the final direction of his studies was thus determined. We need scarcely here refer to the eminent part which he has played as a chemist, both independently, by his own researches, and through the numerous pupils who have accepted him as their leader, nor will it be necessary here to show how the ideas which he advocated have progressively replaced the electro-chemical theory of the illustrious Berzelius. But we ought to observe, that in the midst of his various successes and engage- ments, M. Dumas has never entirely forgotten the science which constituted the object of his early studies. For the last twelve or fifteen years his labours have been directed towards physiology, and especially to the application of chemistry to that science. By the influence which he has exerted in this direction, he must be considered as the actual leader of physiological chemistry, appearing in this respect, as the successor of Van Helmont, Sylvius, and Fourcroy. The present is not the place in which to discuss these doctrines, but I shall undoubtedly some day have occasion to revert to the subject, when I shall consider the labours and views of M. Dumas in relation to organised beings. THE COASTS OF SICILY. 47 bodies in the lower plants, which M. Thuret has made known to us, and which for some hours present the characters of animality. It is not possible, however, long to remain in doubt, for the embryo unfolds itself, becomes elongated, and throws out at its anterior part a minute smooth tubercle, bearing on its surface and on each side of it a round eye-point. From this moment its nature is definitely fixed. The observer cannot yet, it is true, recognise the class, family and genus to which the nascent being which he is observing belongs; but he may boldly affirm that when it has reached its perfect state, this being will be an articulate animal, for it already possesses all the fundamental characters of this great sub-division. Its body is composed of two symmetrical lateral halves, its dorsal and ventral surfaces may be clearly distinguished, its digestive canal stretches from the front to the pos- terior part of its body. Everything still seems to be homogeneous in this microscopical embryo ; we dis- cover no muscle, and yet it contracts in every direc- tion, rolls itself into a ball, or flattens itself into a disc, and in these extreme movements it exhibits temporarily those forms which deceived the skilful Swedish naturalist. At this epoch it is still impossible to recognise a priori if the embryo will become an Annelid, or if, stopping at the last series of the sub-division, it may belong to the groups of smooth worms, as, for instance, to the Nemertes. Our uncertainty is here of short du- ration, for rings appear upon the body and are rapidly multiplied, being always formed successively from 48 RAMBLES OF A NATURALIST. before backwards, each succeeding the last formed one. We see, therefore, that the embryo will be an articulate animal with its body divided into segments. In this state it reminds us by its external form of the leech, but cirrhi soon appear upon the sides. We now ask whether the young animal is allied to the earthworm or the Nais*, which exhibit distinct rings * Every one is familiar with the earthworm, which is known in zoology as the Lumbricus. The Nais resembles it in many par- ticulars, but instead of living exclusively in the humid earth, it lives in the water, at one time making for itself a passage or tunnel within the mud, and at another time attaching itself to the branches of aquatic plants. "We will here mention a curious result connected with those great questions of general harmony which fall so essen- tially within the province of modern science. The Lumbricus and the Nais had at all times been classed in the same group with Marine Annelids. But these first two genera have both sexes reunited in one individual, whilst my own observations, confirmed by a great number of zoologists, have demonstrated that in the Annelids the sexes are separate ; hence it is necessary to place these animals in a different group. On the other hand, the resem- blances which had caused them to be united with the Annelids are un- deniable, and I have therefore been led to regard these resemblances as being indications not of direct, but of collateral affinities, or analogies. On examining the entire group of Worms from this point of view, we find that they may be separated into two series which I have designated as that of Les Vers Monoiques, and that of Les Vers Dioiques, of which I have given a table in the first note in the Appendix of Volume I. Here a very remarkable general fact presents itself to our notice. All the Lumbricidse comprising Nais, inhabit fresh water, whilst all the Annelids, whether they belong to the wandering or the tubicolous groups, live in salt water. The former inhabit lakes, rivers, and brooks, whilst the latter are only found in the sea. The older authors have indeed spoken of Marine Naides and Marine Lumbricidae, but in examining the species which are thus designated I have always found that they were either true Annelids or special genera allied to that class, like the Echiuri and the Polyophthalmia. THE COASTS OF SICILY. 49 and are provided with cirrhi, but have no feet. This cannot be the case, for here are protuberances which appear upon the sides of each segment, and hence the embryo belongs to the group of Annelids, pro- perly so called. It remains to be decided whether it will traverse its native sands under the form of a wandering Annelid, or whether it will be confined in a narrow tube, and lead the retired life of a tubicolous worm. This last doubt soon vanishes, for a small tubercle now appears in front of the head, which lengthens and begins to play the part assigned to the extensible filaments of which we have spoken. Other similar appendages soon appear by the side of the former, and from that moment the animal, being provided with the organs necessary to secure its relations with the external world, surrounds itself with a tube and begins to lead the life of a recluse. We see, therefore, that at each phase of its deve- lopment, the special nature of the Terebella becomes more distinctly characterised. We have recognised successively how the embryo belonged to the great division of the Articulata, then to that sub-division of it in which the body is divided into segments, then that it is a true Annelid, and finally that it is a tubi- colous worm. Investigate it a little longer, and we shall be able to recognise its genus and its species. This is very much the same, as if being interested in Thus the type of the Lumbricus and the type of the Annelid mutually replace one another according to the nature of the waters in which they live. These animals constitute corresponding terms to one another in nature as well as in our classifications ; they are the Geographical Analogues of each other. VOL. II. E 50 RAMBLES OF A NATURALIST. obtaining detailed information concerning some indi- vidual, we were first to learn that he was born in the old continent, next that he was a European, and then successively that he was a Frenchman and a Parisian, and that he lived in such a street, at such a number, and, lastly, that he bore such or such a name. From these and many other similar facts, we surely have the right to conclude that the dif- ferent degrees of zoological relationship or affinity stand in direct connection with the duration of the primordial resemblances, exhibited by the embryos. Or to express the same idea differently, may we not admit that the apparent identity between two germs in the course of development will persist for a longer or shorter period according as these germs belong to animals, more or less resembling one another in their nature ? We have purposely employed the words apparent identity, for it is often difficult to ascertain whether the identity is real or only apparent. Two Tere- bellas of different species cannot be distinguished from one another until their development is com- plete. Does this imply that the germs were really identical up to this one definite epoch ? We do not think so : and we concur with M. Chevreul in be- lieving that the manifestation of differences under the influence of similar circumstances, in beings which hitherto might have been confounded, implies the existence of corresponding differences in an anterior state of organisation.* These differences * Considerations sur la Philosophic de V Anatomic. (Journal des Savants, 1840.) THE COASTS OF SICILY. 51 do not the less exist, because they are inappreciable to our senses, and it is from the want of duly recog- nising this distinction, that men of high reputation have suffered themselves, more especially in Ger- many, to be led away by hazardous speculations, giving rise to abstract theories, which, although decorated with the name of the philosophy of nature, have for many years retarded the true progress of the natural sciences. Whilst these different labours occupied M. Milne Edwards, his companions did not remain idle. M. Blanchard had ably fulfilled the task that had been entrusted to him by the directors of the Jardin des Plantes. More than 2000 species of insects, represented by at least 8000 individuals, were collected in his cases. About 500 of these species were wanting in the galleries of the museum, and fully 300 were altogether new to science ; our companion therefore had given active proofs of his industry. But while he acquitted himself of the duties imposed upon him in his capacity of assistant naturalist and collector of specimens, M. Blanchard had by no means neglected labours of a higher order, and he might well look with pride and satis- faction at his collection of drawings and notes. Amongst other things, he had drawn up a highly interesting memoir on the nervous system of the Gasteropodous Molluscs; for, notwithstanding the magnificent labours of Cuvier, much still remained to be done in reference to these animals. Tfieir nervous system especially was but little known. Cuvier had only distinguished a very small number £2 52 RAMBLES OF A NATURALIST. of ganglia or central masses, from whence are given off the branches which convey both sensibility and motion to every part of the body. M. Blanchard, however, discovered in this apparatus a most un- expected degree of complication, and he showed that in certain species these ganglia are very numerous, and that instead of the five or six hitherto observed, there existed nearly thirty of these masses. This first memoir by M. Blanchard on the nervous system of the Invertebrata was the means of leading this naturalist to other highly important results. Endowed with a singular steadiness of hand, and an extreme clearness of sight which enabled him to distinguish, without the aid of instruments, the most delicate nervous filaments, he entered upon researches of a similar nature on the nervous system of insects — a class of investigations which present such extreme difficulty, that few naturalists have grappled with them. And fortunately his labours were recompensed by the discovery of a complete nervous system, especially distributed to the organs of circulation and respira- tion. This is a very remarkable example of the di- vision of physiological labour, and at the same time a new proof that the more closely we examine these too much neglected beings, the more fully we shall recognise that they possess, in the eyes of the Creator, as high a degree of importance as animals of the largest size. The observations of Lyonnet on the goat-moth, and those of Strauss-Durckheim on the cockchafer *, have shown that the organism is fully * M. Strauss-Durckheim, a French zoologist, was one of the first who fully comprehended the importance of Monographs. He THE COASTS OP SICILY. 53 as complicated, if not more so, in insects, as in the largest animals, such as the elephant ; and M. Blan- chard, by adding many important facts to those which had been discovered by his predecessors, has further confirmed this general result. Encouraged by his first success, M. Blanchard extended his investigations on the nervous system to those singular beings, whose existence and mode of O G ^ propagation continued to within a few months of the present time (1854) to constitute one of the most curious problems of zoology.* We here refer to the Helminthess or intestinal worms — animals which are sometimes developed in the very midst of the living tissues, in the muscular substance, in the brain, and in the ball of the eye, and therefore in parts which to all appearance are the best protected from any external influences. Lamarck and Cuvier almost absolutely denied them the possession of a nervous system. Many naturalists shared in this opinion, and if any isolated observation appeared to justify accordingly resolved to give a history of the leading groups, by taking as a terra of comparison one of the principal species, -whose anatomy had been pursued to its utmost limits. It was thus that he chose the Cockchafer as the type of articulate animals, and Cuvier con- sidered this work as the only one which could be compared with that of Lyonnet. In making his delicate preparations, M. Strauss- Durckheim had recourse to several ingenious inventions, and amongst others we owe to him the discovery of a very simple method of making extremely fine injection tubes. His labours have unhappily been suspended by premature infirmity, for, like Geoffroy and Savigny he has almost entirely lost his sight. * I have elsewhere stated (see Vol. I. p. 345), that the researches of Van Beneden and Kuchenmeister have almost entirely solved the problem of the reproduction of the intestinal worms. E 3 54 RAMBLES OF A NATURALIST. the philosophical doubts of the majority of inquirers, nothing authorised the admission in any general manner, that these animals were characterised by a well-defined nervous apparatus ; nevertheless M. Blanchard has shown that such is the case, and he has confirmed or rectified by numerous examples the facts which had been obtained in reference to the Distomata and the Nematoides* by Bojanusf, MehlisJ, Laurer §, Cloquet ||, &c. He has shown that the Taenias IF present a most singular arrangement, which * The Distomata are a group of intestinal worms comprising the Liver-fluke, which is so common in sheep, together with all the worms which are allied to that form. The group of the Nemato'ides is composed of the Ascarides, and all the genera which are allied to that type. f Bojanus, who is. one of the most distinguished anatomists of Germany, commenced in 1817 a series of anatomical observations on intestinal worms, which had before that time been studied only in reference to their external characters. He was the first to discover the Sporocysts, and to recognise the nature of the Cercarese. We moreover owe to him several important works, amongst others a magnificent anatomical memoir on the European Tortoise. J Mehlis was one of the first who noticed the nervous system of the Trematoda, in an anatomical description of the Distoma hepaticum and D. lanceolatum. § We owe to Laurer, amongst other works, some highly interest- ing researches on the anatomy of the Amphistoma. || M. Cloquet has published, on the anatomy of the Ascaris lumbricoides, a memoir which has long been the best on the subject. ^[ The Tsenia, which is vulgarly regarded as a solitary worm, does not by any means merit this appellation, for even in man several of these animals are often simultaneously present, and certain species occur in large numbers, more especially in fishes, many individuals being present in the same intestinal tube. We would here remark that in accordance with Van Beneden's view each Tsenia is not an individual, but an aggregation of many indi- viduals, which being at first united, become successively isolated, THE COASTS OF SICILY. 55 constitutes another exceptional character in these al- ready remarkable worms. All these facts, illustrated and confirmed by extremely delicate preparations, were submitted to the most competent judges, and the consequences deduced from them are highly im- portant. They have led us to recognise the fact that very different animals have hitherto been confounded under one common denomination, and they have enabled us to appreciate the relations which connect these different types with already established groups, and finally they have removed an extremely nume- rous class from the animals which we regard as al- together devoid of a nervous system. This is a very important result. The nervous system, says the illustrious author of the Regne Animal, represents, so to speak, the whole animal. We are far from accepting this doctrine uncondition- ally, but at the same time we cannot deny extreme importance to that system, which appears in the highest living beings to distribute life to every part of the organism.* The absence of this system is in and lead an independent life as soon as their organisation is com- pleted. We ought to add that these ideas, startling as they may appear, very probably express the truth. * It is well known that in order to remove from a limb every trace of sensibility and motion, it is sufficient to cut, or simply to compress, the nerve which supplies it. The limb itself, however, does not die, inasmuch as the circulation and the nutrition are carried on very nearly in the same way as before the operation, and we might, therefore, be led to believe that the words of the text convey a very great exaggeration, but it is well known that there exist in the superior animals, and even amongst a certain number E 4 56 KAMBLES OF A NATURALIST. itself sufficient to set aside in a distinct category, as it were, all those animals in which such a deficiency- is definitely established, but the number of these animals is very limited. In proportion as we care- fully study the most apparently degraded animals, we discover more and more traces of the existence of this system in the greater number of them. Cuvier had admitted its presence in the animals which were classed by him in his first three divisions of the animal kingdom, but he denied its existence, or re- garded it as present in mere traces, in all the Ra- diata. It is now some years since MM. Tiedemann *, of the Invertebrata, two distinct nervous systems. One of these systems has for its centre the brain and the spinal cord, and the nerves which issue from it are called nerves of animal life, which exclusively preside over the functions of sensibility and voluntary motion. The other nervous system, which is called the system of the great sympathetic, has for its centres ganglia, varying in number and size, which in all the Vertebrata are situated in the abdomen. The nerves which emanate from hence are called the nerves of vegetative life, and they preside over the involuntary movements which occur throughout the whole body, and do not communicate any sensibility to the organs. These nerves, which are very numerous, and much ramified, everywhere accompany the vessels, and it is probable that it is under their influence that the phenomena of nutrition are accomplished. * Professor Tiedemann, who is a foreign associate of the Institute, is one of the most illustrious representatives of science in Germany. He for a long time occupied a Professor's chair at Heidelberg, where his reputation attracted a crowd of students from all countries, and he now lives in retirement at Frankfort. We owe to him a large number of anatomical and physiological works, among which we shall more especially mention his different Monographs on the Brain of Man, the Apes, and certain other Mammals, his treatises on Zoology and Physiology, his Anatomy of the Echinodermata, which received the prize awarded by the Institute, &c. THE COASTS OF SICILY. 57 Costa *, and Krohn f have demonstrated its existence in the Echinoderms to which belong the star-fishes, while MM. Ehrenberg, Grant, Milne Edwards and Agassiz have described it in the Acalephas, while we ourselves have discovered it in the Nemertes and the Planarias, animals which are very nearly allied to certain intestinal worms, although they live in water. Fully half of the Radiata and all the Worms, there- fore, possess nerves as distinct as the higher animals. A most interesting question is connected with that of the existence or absence of the nervous system. What relations exist between the external world and these lowest representatives of the animal creation ? Do Annelids, Star- fishes, and Medusa? possess the senses of sight and hearing ? Lamarck, influenced by theoretical ideas, denied them all sensation, and designated the majority of the inferior animals by the denomination of animaux apathiques, and, without being equally explicit, Cuvier seems to * Dr. Costa, a physician and naturalist at Naples, has published a great number of very interesting memoirs, which bear principally upon the marine animals of his native country. He was one of the first who studied with care the anatomy of the Amphioxus, a very remarkable fish, to which I have referred in a subsequent part of the present chapter. f The naturalist Krohn has also specially devoted his attention to the marine animals. Amongst other works, we are indebted to him for a very interesting memoir on the mode of reproduction of the Salpae, in which he has confirmed, and at the same time more fully developed, the facts announced by Chamisso, which had long been treated as fabulous. He has shown that the mode of genera- tion of these Molluscs, compels us to include them among those animals in which Steenstrup's theory of alternate generations is exhibited. See VoL I. p. 219. 58 EAMBLES OF A NATURALIST. have inclined to the same view, which is maintained even at the present day by some eminent naturalists. Experience and observation appear to us to be opposed to these theories ; for not only do a large number of the inferior animals possess sensorial organs by which they must consequently perceive sensations, but these organs are even in some cases much more multiplied than in Mammals or Birds. Thus for instance several of them realise the fable of Argus, or the strange conception of Fourier in relation to the fifth member which is to complete the human being, when the globe will be covered with phalansteries. Certain Star-fishes have a well characterised eye at the extremity of each of their rays, while the Nemertes and the Planarias are often provided on the lower and upper surface of their heads with fifty or sixty, and sometimes even a larger number of -distinct eyes. Ehrenberg has made known to us a small Annelid, which is furnished with two eyes in its head, and two others at the ex- tremity of its tail ; and I found both in our seas of Brittany and during my stay in Sicily, three totally distinct species, presenting the same peculiarity. Yet the tufts of Corallina at Favignana and Milazzo nourished thousands of little worms, which are even more remarkable in this respect. These worms, which I have named Poly ophthalmia, and to which I shall have occasion presently to revert, are provided in front with three double or triple eyes, while a series of the same organs are placed along the entire length of the body, passing from the head to the tail.* * See Chapter VIII. on Guettary. THE COASTS OF SICILY. 59 We see, therefore, how much we have advanced since the period when Reaumur called the Medusae masses of living jelly, and when Cuvier believed with other naturalists in the existence of Parenchyma- tous Worms. In proportion as zoologists have more thoroughly investigated the mysteries of the inferior world, organisation seems to have grown more com- plicated, and to have assumed the most unexpected forms. Let us beware, however, of falling into an opposite extreme. After having admitted without sufficient proof; and by a sort of a priori reasoning, the organic simplicity of the lower animals, we must not conclude from a few already known facts, that they all present an equal degree of complication. At the lowest point of the zoological scale, there exist beings in which all the vital acts are accomplished, simultaneously and in the same manner, over all por- tions of the body, and whose organs appear to be fused together into one homogeneous structure. I will here give a few examples by way of illustration. In the living sponge, a sort of semi-fluid varnish covers with a thin stratum that horny and more or less solid skeleton, which is so familiar to all of us. This varnish is the actual animal, the structure which we commonly term sponge, being, in fact, its skeleton. The Amoeba, which is still more simple, appears to be nothing more than a drop of this living varnish endowed with locomotion, but not having even a determinate form. The eye when aided by the micro- scope may see these animals flow together into a mass, as drops of oil would flow over the slide, while they present the most diversified and irregular forms. 60 RAMBLES OF A NATURALIST. Finally, M. Dujardin has shown us that the Khizo- pods are animals covered with a shell, but whose body is without any definite organisation. A Gromia and a Milliola, before they climb up the polished side of a glass vessel, form for themselves on the instant, and at the cost of the substance which composes them, a sort of foot, which stretches out, and becom- ing elongated, affords them a point of support ; as soon as they no longer need this assistance, this temporary organ returns into the common mass, and becomes confounded with it just in the same manner as a thread of viscid matter returns to the substance from which it had been drawn out. Between these extreme points of the animal scale and the creatures of which we have just now spoken, there no doubt exist many intermediate forms ; for, as Linnaeus has said, nature does not make any sudden bounds, and always proceeds by insensible gradations. Here, perhaps, more than elsewhere, experience and observ- ation ought to precede all theoretical conceptions. It is, moreover, by following these two infallible guides that modern zoology has arrived at a result which seems to be the counterpart of those we have indicated. At the same time that it discovered in these last animal series (the worms) a most unexpected organic complication, it also recognised the fact, that the superior groups themselves comprise degraded species, which appear to have lost almost all the essential characters of their fundamental type ; and there are certain points of view from which we are justified in asserting that there exist inferior mammals, birds and reptiles. This proposition is most abso- THE COASTS OF SICILY. 61 lutely true for the class of the Fishes ; for the group of the Myxinoides, Lampreys, and more especially the Amphioxus, can leave no doubt on this subject. The Ainphioxus is a small fish which lives in the sands of the sea, where it conceals itself and moves about with incredible rapidity. Its body, which is perfectly transparent, terminates in a point at both extremities, a circumstance from which it has derived its name. The Amphioxus has been found on the coasts of Cornwall, in the Baltic, at Naples, and at Messina, where I caught a- great number at the distance of a few yards from the whirlpool of Cha- rybdis. It has been investigated successively by Goodsir* in Great Britain, by Costa in Italy, by Retzius, Rathke f> and more especially by Miiller, * John Goodsir, one of the most distinguished physiologists of Great Britain, is Professor of Anatomy in the University of Edin- burgh, and has published several important memoirs. He was one of the first who announced, in relation to the mechanism of secretions, a doctrine which seems to be more and more thoroughly confirmed by facts. According to this distinguished physiologist, the secreted fluids do not exude directly from the membranes which yield them, but they first accumulate in the epithelial cells, which always cover the secreting surfaces. These cells are, therefore, the fundamental element of every secreting system. The facts discovered by Goodsir in reference to the digestion of fatty matters, and the conclusions which he has deduced from them, afford the most probable explanation that has been offered in reference to this very obscure point, notwithstanding the many attempts that have been made to elucidate it. f Rathke is one of the most distinguished anatomists and natu- ralists of Germany, and his researches have been extended to almost every department of the animal kingdom. He has specially occupied himself with embryology, and amongst other works we. owe to him some highly interesting researches on the formation of 62 RAMBLES OF A NATUKALIST. in Germany. I have myself made this fish the subject of a most careful investigation, and at the present day we may consider its organisation as per- fectly known. Yet while we have no difficulty in asserting most definitely that it belongs neither to the Mollusca, the Articulata, nor the Kadiata, it scarcely merits the name of a Vertebrate. It has hitherto been admitted that the essential characters of this sub-division of the animal kingdom are the presence of a vertebral column, a brain, a heart and red blood, yet the Amphioxus possesses neither heart nor brain, properly so called, nor any distinct vertebral column, and its blood is entirely colourless. The impulse necessary to make the nutrient fluid pass through the circulatory circle is communicated to it by large vascular trunks. The blood resembles that of the Molluscs. The vertebral column is repre- sented by a cartilaginous stem, entirely composed of cells, and extending from the head to the tail. The brain, which is not protected by the slightest appear- ance of a cranium, is only distinguished from the spinal cord by the direction of the nerves which issue from it. The eye is entirely enclosed in the interior of the tissues, but owing to their perfect transparency, it is probable that the functions of the organ of sight are not the less perfectly accom- plished. This diaphanous character of the Amphi- oxus enables us, moreover, to ascertain that it pos- sesses a mouth, which belongs rather to the Mollusc the venous system, and on the manner in which the circulation of the adult gradually succeeds that of the foetus. His Embryology of the Cray Fish—AstacusJluviatilis — is also a very remarkable work. THE COASTS OP SICILY. 63 than the Fish, together with a circulating apparatus and a mode of digestion which remind us of similar organs in the Annelids, &c. The attentive study of the Amphioxus has led to consequences of the highest importance both to zoology and physiology. Confirming in this respect the embryological results to which we have already referred, it shows us in this degradation of an animal, a permanent condition which recalls in certain respects the transitory condition of the most perfect animals belonging to the same type. Thus during the first periods of its development, the embryo of an ordinary fish, as for instance a Salmon, possesses peculiarities of organisation which remind us of those which we observe in the Amphioxus, but whilst these peculiarities are persistent throughout the whole life of the latter animal, they are soon effaced in the young salmon to give place to other definite characters. The embryology of the Annelids ex-' hibits precisely similar facts ; thus, for instance, in the early period of its existence, the larva of the Terebella closely resembles a Nemertes, and thus the results which have been furnished by the anatomy and embryology of Fishes and Annelids are perfectly in accordance with one another, notwithstanding the great distance which separates these two groups.* By the very fact of its degradation, the Amphi- oxus departs from the Vertebrata to approximate * Let us once more remind our readers that we speak here of partial resemblances and not of identity. A young Terebella is at no time an adult Nemertes, nor can a Salmon ever have been an Amphioxus. 64 RAMBLES OF A NATURALIST. more nearly to the lower divisions. Nevertheless the new affinities which are thus manifested do not connect it with those animals which occupy the highest places in these divisions. The Amphioxus by its organic structure never reminds us of the Cephalopods, or the Insects, or the Crustaceans, but it rather approximates to the Acephalous Molluscs, as, for instance, the Oyster, and to the Annelids ; or, in other words, to the lowest repre- sentatives of the Molluscous or Articulate type. Here, also, we find a manifest accordance between the results furnished by anatomy, and those which have been obtained from embryology. All germs resemble one another in the first period of their development, and they successively differ from each other in proportion to the advanced condition of their development, and consequently the beings which are evolved from these germs deviate from one another, in proportion to the degree in which they may be considered as representatives of their type. Consequently, also, the series resulting from these successive phases of development will be widely separated at their summits, but will approxi- mate at their bases ; and hence the relations borne by one series to another will be exhibited by the inferior but not by the superior animals. In order to elucidate the more abstract features of the preceding ideas we shall have recourse to a homely comparison, which will easily be understood. Thus, for instance, we may represent the course pur- sued by the germs in the process of their development, as a high road covered with travellers. From this highway, which at first gives off no branches, THE COASTS OF SICILY. 65 numerous roads after a time turn off to the right and left, diverging more and more from the central route. It is evident that those travellers who have entered upon these branch roads will deviate more and more from one another, in proportion as they advance. Here, then, in those who have reached the greatest distance from the general starting-point, we have a representation, in some measure, of the superior animals; whilst those who have only advanced a short distance from the main road, represent the inferior animals. The Salmon, to which we lately referred, the Cephalopods, the Insects, and Crusta- ceans correspond to the active travellers, and these manifest scarcely any points of resemblance to one another ; while the Amphioxus and the Annelids cor- respond to the sluggish pedestrians, and amongst these we discover many points in common. In the same manner the two sub-kingdoms of the Vertebrata and the Invertebrata, which appear very dissimilar to one another when they are studied in their higher representatives, are very nearly brought into contact through these lower species, which may be regarded as degraded representatives. We see how thoroughly in the Amphioxus every- thing appears to have been created as if for the pur- pose of affording the most complete refutation of those doctrines which have been advanced by naturalists, who, either through adherence to an antiquated science, or perhaps from the fear of in- curring labour and fatigue, look with contempt upon the study of the lower animals, and rejecting the consequences which may be deduced from it, appeal VOL. II. F 66 RAMBLES OF A NATURALIST. solely and incessantly to the Vertebrata. In the presence of the facts which this fish has taught us they may, perhaps, be more ready in future to admit the value of observations made in reference to animals so low in the scale of being as worms and zoophytes. Unless we actually deny the evidence of facts, we are compelled at the present day to admit that the representatives of the same type often differ very widely from one anr ,\er, and that their organisation may present very different degrees of perfection and degradation. We must, moreover, here remember what are the facts which anatomy, in ac- cordance with embryology, has taught us in reference to the existence of distinct fundamental types, which are modified in a thousand different ways to engender secondary and tertiary types * ; for by a consideration of these facts we shall find that those systematic conceptions will speedily vanish which have been the means of giving at once so abnormal and false an idea of animated nature. Living beings will then no longer appear to us to be circumscribed within narrow series, which to whatever extent we may suppose them to be multiplied, will still invariably possess the inconvenience of reminding us of a Jr o straight line. The surface of our globe, like the immensity of the heavens, exhibits to us the creative power under a very different aspect ; for we see it giving development to plants and animals in the same manner as it has produced the stars, distributing them into natural groups as it has reunited the * See Chapter II. in Volume I. on the Archipelago of Brehat. THE COASTS OF SICILY. 67 different constellations, and finally binding together their thousand families by simple and multiplied links, in the same manner as it has rendered the worlds which people space dependent one upon the other. The doctrines that we here advocate, received, some years since, a brilliant confirmation, which utterly excludes all doubt. Palaeontology, that science which dates from Cuvier as its founder, but whose progress has been at once sure and rapid, has arrived by an independent course of investigation at absolutely similar results, deduced from the study of the order of succession of animals from the most ancient geological periods to our own day. In truth, life has not glided along the surface of the globe by gradual and, as it were, concealed steps, by the intervention of beings, which at first were of the simplest structure, and gradually became more per- fected, until they, in their turn, gave birth to still more perfect animals. The animal kingdom does not present one sole and progressive mode of deve- lopment, as has been conjectured by the naturalists whose views we oppose. On the contrary, from the very beginning, we find that there must have been simultaneously present the four fundamental groups which, even at the present day, include the entire mass of created animals ; for we find that the Vertebrata, Articulata, Mollusca, and Radiata, are buried side by side in the ancient fossil beds of the earlier world. Even more than this, the three inferior sub-divi- sions possessed at that remote period representatives of almost all existing classes ; and if it is otherwise F 2 68 RAMBLES OF A NATURALIST. in respect to the Vertebrata — if Keptiles, Birds, and Mammals are wanting in these primitive faunas — a simple explanation of their absence would be fur- nished on the supposition of the external conditions being incompatible with their mode of life. Moreover, in proportion as we rise to the more modern geological strata, we find these types modi- fied ; in some cases making a gradual advance towards perfection, up to the appearance of Man upon the globe, much in the same manner as we observed the progressive advancement of the young Terebella as it passed through each successive phase of its ex- istence ; while at another time the most perfect species seem lost, remaining to us only in their in- ferior forms, and thus giving rise to recurrent series, as we still see at the present day in certain animals, as, for instance, in the Lernea, which seems to re- trograde by the very progress of its development.* * The Lerneas are Crustaceans, which are extremely curious, on account of the metamorphoses which they undergo, the result of which, more especially in the females, is to induce a progressive degradation. These animals in their early age bear a considerable de- gree of resemblance to the Cyclops, a small Crustacean which occurs in great abundance in our fresh waters. They are at this period provided with a well-characterised frontal eye, whilst their natatory legs enable them to swim freely ; but after having undergone several moults, they finally affix themselves upon another animal, at whose expense they subsist for the rest of their lives. The females attach themselves by some means to the body of this animal, whilst the males have their bodies attached to those of the females. The eyes and the limbs become gradually atrophied and disappear, while the different portions of the mouth become converted into a simple sucker. The changes experienced by the males are less marked, but the females become so completely degraded, that their nature was THE COASTS OF SICILY. 69 Is there not something almost marvellous in this accordance ? M. Agassiz * in his great work on the Fossil Fishes and Echinoderms, has especially in- fer a long time misunderstood, and Cuvier placed them amongst the intestinal worms. * M. Agassiz, a corresponding member of the Institute, is a native of Switzerland. This naturalist has followed, with the greatest ardour, the paths of inquiry first opened by Cuvier, and it may be said that he has done for Fossil Fishes what the founder of Palaeontology had done for the Mammalia, and hence his work on this subject will always be regarded as a standard authority in this department of science. M. Agassiz has, moreover, not limited himself to extinct species, but he has undertaken a great work on the Fishes of Europe, in which their anatomy and embryology occupy a considerable place. His palseontological studies have extended to the Echinodermata, and he has published, in relation to this subject, the extremely important memoir to which I have alluded in the text, Resume d'un Travail d' ensemble sur F Organisa- tion, la Classification, et le Developpement propressif des Echino- dcrmes dans la Serie des Terrains. Led by the direction of his zoological studies to devote his attention to geology, M. Agassiz has advanced certain views in relation to the former extension of the glaciers, and the actions which they have exerted on the earth's crust; and these views, which were at first much opposed, now find many supporters. In order to confirm these statements by prolonged observations, M. Agassiz spent several successive summers on the most elevated parts of the Swiss Alps. With a view of completing these great works, M. Agassiz collected around him a band of eminent collaborateurs ; amongst whom we may instance Professor Vogt, who contributed th^ einbryological details in relation to the salmon in the volume ou the Salmonidse ; Valentin, to whom we owe a very detailed ana- tomical monograph on the genus Echinus ; and M. Desor, who has published a volume on the History of the Glaciers. M. Agassiz, who has been residing for several years in the United States, appears recently to have given a somewhat different direction to his studies ; for he now devotes himself more especially to the study of the inferior animals, and in his anatomical researches on the Medusae, he has discovered some very curious and highly important facts. F 3 70 EAMBLES OF A NATURALIST. sisted upon these important considerations; nor has he scrupled to express in the following terms the consequences to which he was led by the result of his remarkable investigations. " The most natural zoological arrangement is the most general expres- sion of geological order, and vice versa, the order of succession of beings is the most certain indication of true natural affinities." In glancing in the preceding pages at some of the leading problems which zoolo- gists of the present day are endeavouring to solve* we have expounded the doctrines of that physio- logical school to which we are proud to belong. In order to arrive at the solution of these problems, we have successively interrogated the anatomy of adult animals, embryological phenomena, and geological facts, and everywhere the reply has been one and the same. We may, therefore, confidently assert that the past and the present of our globe agree in sanctioning the fundamental ideas which lead us to the ultimate aim of all our inquiries — truth. 71 CHAP. VI. TIIE COASTS OF SICILY. ETNA. Aspect and nature of the coasts from Giardini to Catania. — Catania ; its harbour ; its soil. — Etna. — Excursion to the volcano. — Nicolosi, the Casa Gemellaro ; a night passed at the foot of the cone ; the great crater ; the crater of 1843. — Eruption of 1669 ; its traces as far as the town of Catania. — Elie de Beaumont's theory of Etna. — Observations made in the crater of Vesuvius. — Examples of the slight degree of solidity of the earth's crust. — Approximate calculation of volcanic forces. SINCE our departure from Milazzo we had scarcely lost sight of the summit of Mount Etna, which was still smoking from the eruption of 1843. At Giar- dini we had obtained a view of the whole eastern side of the volcano, and here we saw the first bed of lava, the same which, 396 years before the Christian era*, was poured forth for a distance of nearly twenty miles from the crater, where it formed Point Schiso. We had often during the night watched the smoke which, escaping from the cone, reflected the reddish tint of the subterranean fires over all the neighbour- ing district ; and often, too, a hollow rumbling sound, * Historical and Topographical Map of the Eruptions of Etna from the Era of the Sicani to the Present Time (1824), by Joseph Gemellaro. This map is accompanied with a description in English and Italian. F 4 72 RAMBLES OF A NATURALIST. but one that indicated inconceivable power, had fallen upon our ears either as a threat or a distant warning. As we skirted along the coast, which stretches for thirty miles between Taormine and Catania, we had everywhere recognised the action of volcanic forces ; indeed, the whole of this coast, the rocks, mud, and sands, all owe their origin to the volcano. At every point the tufa of Etna is poured down into the sea, and is in all cases the result of eruptions which belong to the present geological period. A few beds of recent lava-streams also extend to the shore, and contrast by their black colour with the greyish tinge of the rest of the rock. Occasionally, too, these beds are superposed one upon another, as at Aci Eeale, where the Scalazza is formed of seven distinct strata. Sometimes, also, eruptive rocks, whose origin goes back to the most remote geo- logical ages, attracted our attention. The basaltic rocks of Cape Mulini, those of Castello d'Aci, of Fariglioni, and the Cyclopean islands, attest that in all ages this part of Sicily has been the theatre of the most formidable phenomena. Catania is, indeed, worthy of being the capital of a district that has been so fatally endowed ; for, although it is separated from the great crater which is the centre of action of the subterranean fires, by a distance of nearly twenty five miles as the crow flies, this town appears to be a direct product of the volcano. En- closed within four lava beds of different ages, the materials for its houses and the pavement for its streets have been alike derived from this source ; while it is only through the lava that the inhabitants THE COASTS OF SICILY. 73 can reach the springs that supply them with water. The liquid fire has filled up its harbours, consumed its gardens, broken down its walls, and buried entire districts. Earthquakes, moreover, have destroyed what the lava had spared, and yet Catania has ever risen from the midst of her ruins, and after each new destruction has laid down wider streets, erected loftier palaces, and founded more splendid convents and churches. Yet she has not been able wholly to efface the traces of these catastrophes ; and standing upon this soil, which has been so often upheaved, we everywhere found ample materials on which to begin those geological observations which, for a few days, were to supersede our ordinary zoological studies. The little inlet of the sea which at the present day forms the harbour of Catania, bears no resem- blance to that magnificent port which was cele- brated by the poets of antiquity, who inform us that it reached more than three miles inland, penetrating to the very hills of Licatia, and everywhere secur- ing to ships a safe anchorage, protected by an island.* The harbour in which Ulysses found * " Portus ab accessu ventorum immotus et ingens Ipse, sed horrificis juxta tonat JEtna ruinis." VIRGIL. We still daily meet with proofs of the existence of this ancient strand. In the eastern portions of Catania the wells traverse a thick stratum of lava until they reach a bed of clay or sand, which is occasionally intermixed with boulders and rounded pebbles ; and here may be found a large number of shells, belonging to the same Molluscs which in the present day live within the harbour and along the neighbouring coasts. Fragments of wood have also been found in the same locality. 74 RAMBLES OF A NATURALIST. shelter has ceased to exist for many centuries. A hundred and twenty-four years before our era, a current of lava, bursting forth about six miles from the town, inundated the whole country lying to the east of Catania, blocked up the harbour, and passing over the banks changed the strand, which was once so easy and safe of access, into an unap- proachable rocky height. Fifteen hundred years afterwards — namely, in 1381 — another stream fol- lowed nearly the same direction, destroying the rich plantations of olive trees which had shot up on the old lava, and terminating its havoc by almost blocking up the little harbour of Ognina at about three miles' distance from Catania; while two other streams, very nearly parallel to the preceding one, enclosed the town to the west and north. One of these streams is referred back to the year 527 before our era; but this stream is of inconsiderable extent, and terminates within the harbour. The other stream dates no further back than the year 1669, an epoch which is well known to every Sicilian, and which recalls one of the most formidable erup- tions of which we have any record. After having broken down a large extent of wall, it penetrated into the town, throwing into the very midst of the most populous districts vast masses of lava, which are worked in the present day as quarries. Catania is situated at the southern extremity of the mountain side in whose centre lies the cone of the crater, and which almost entirely occupies a vast and nearly circular plain, bordered to the east by the sea, and to the south by the plain of Catania, THE COASTS OF SICILY. 75 and to the west and north by high mountains of sandstone and calcareous rocks. A spur of this latter chain advances towards Etna, where it is soon lost beneath the volcanic tufa. From this point two small streams proceed — the Onobola and the Simete — which encircle the base of the mountain, marking almost exactly its limits, and transforming this burning focus into a veritable isthmus. Isolated in the midst of its well-defined domain, Mount Etna rises in a pyramidal form to a height of nearly 11,000 feet*, and measures at its base from thirty to forty miles in diameter. This vast extent of surface, and the facility with which the eye can embrace every part of the mountain range, give to Etna a very different aspect from that which one might have expected. There is nothing menacing or abrupt in its appearance; and as the eye follows its broad and finely developed outline, which seems to rise in gentle slopes to the culminat- * The absolute height of Etna varies with that of the cone which terminates it, and as the latter is modified by every eruption, new measurements are frequently required. Two distinguished English- men have obtained, by very different methods, results differing only by one unit, for the elevation of the highest summit before 1835. Admiral Smyth obtained his result by trigonometrical operations, according to which, the height of the mountain was 10,874 feet Sir John Herschel by the use of barometrical observations obtained 10,872£ feet. We see therefore that the mean of these two results would be about 10,873 feet; but the summit which yielded these results no longer exists, and it would appear that the actual height scarcely equals that of another point of the crater, which was found by the same observers to be forty-three feet lower than the former. The height of Etna at the time of our ascent must therefore have been about 10,830 feet 76 RAMBLES OP A NATUEALIST. ing point, one is led to ask if this can in truth be the outline of that Etna which Pindar called the column of the heavens. We are apt, on looking at the mountain, to regard the narratives of preceding travellers as fabulous ; we flatter ourselves that we can attain without fatigue the summit, which appears to be so slightly elevated above the horizon; and nothing short of actual experience can rectify this error.* The declivities of which we have spoken are moreover variable, and the contour resulting from them consequently presents interruptions which may be easily perceived even by the naked eye. M. Elie de Beaumont f was the first to direct the attention of geologists to this important fact in connection with the formation of Mount Etna. The outline of the volcano forms an irregular circle of consi- derably more than 100 miles in extent, a more or less prominent range of heights separating it at * The actual angle of inclination almost always differs consider- ably from the estimate that is formed of it, even by a practised eye. We always exaggerate the inclination of the slopes which -we have to ascend. M. de Beaumont has made this very apparent in his memoir, by means of a table containing a large number of the exact measure- ments of different inclines. We shall here quote only a few examples, in order to afford the reader some idea of these results. The street of the Montagne-Sainte-Genevieve, which is perhaps the steepest in all Paris, has nowhere an incline of more than six degrees ; and roads which have an inclination of ten degrees and a half are impracticable for carts. Loaded mules cannot ascend an incline of more than twenty-nine degrees. Sheep cannot reach grass that grows on an ncline of fifty degrees, and a slope of fifty-five degrees is absolutely naccessible. •f [A brief sketch of the labours of M. Elie de Beaumout is given in the Appendix, Note I.] THE COASTS OF SICILY. 77 almost every point from the surrounding plain. Above these heights, which mark the actual limits of the volcano, an arched plateau rises on all sides towards the mountain by an insensible inclination of two or three degrees. This kind of pedestal sup- ports an elliptical cone, which forms the lateral declivities of Etna, and which has a tolerably regular inclination of seven or eight degrees. These lateral slopes abut on the central elevation — the Mongibello of the Sicilians, whose highest part is terminated by a small inclined plane, called the Piano del Lago, which is itself surmounted by the terminal cone in which lies the great crater. From the Piano del Lago, there detach themselves, to the east, two narrow and almost abrupt craters, which form a part of the central elevation, and enclose with two arms, as it were, a great valley known under the name of the Val del Bove* The internal walls of this valley are often perpendicular, while the external walls present an inclination of about thirty-two degrees. Such are the different parts into which modern writers have divided this great mountainous mass; but there is another division, which has long been recognised, and which, as it adapts itself better to the recital of the journey, we shall consequently follow. According to this mode of description there are three zones or concentric regions, which it is very easy to distinguish. The first comprises the level ground; this is the fertile region — regione colta, regione piemontese, which is celebrated for the fertility of the soil, the clearness of the atmosphere, and the salu- brity of the climate. From the earliest historic 78 KAMBLES OF A NATURALIST. ages to our own day, numerous and rich cultiva- tors have occupied this district. And here on this narrow space there are grouped together sixty-five townships or villages, which contain a population of about 300,000.* The second zone is the woody re- gion— il bosco, regione silvosa-, it owes its name to the thick forests with which it was formerly covered, and which still, at different points, give shade and shelter to this part of Etna. This woody region comprises the lateral declivities and a great portion of the central elevation of the mountain. From this region to the summit, there lies a third zone, which is known under the name of the desert region — regione deserta, regione netta, and is in reality nothing more than a vast wilderness, where there is an incessant contest between the fire which smoulders beneath the rocks of the mountain, and the snow which during nearly the whole year covers the summit and declivities. f More than 200 conical eminences, varying in height, but generally of a very regular form, and hollowed in their interior into a sort of funnel-like cavity, are scattered from the extreme limits of * G. Gemellaro. f This contrast strikes all those who visit Etna, and it has furnished poets with several antitheses, which on this occasion at all events express the truth. " Scit niuibus servare fidem, pariterque favillis" CLAUDIAN. Summo canajugo cohilet, mirabile dictu, Vietnam flammis glaciem, aternoque rigore Ar denies horrent scopuli. SILIUS ITALICUS. THE COASTS OF SICILY. 79 the cultivated region as far as the Piano del Lago. These extraneous cones are like so many blow-holes, through which the subterranean fires have made their way at different epochs. The origin of the greater number is lost in the darkness of pre-historic ages, but all belong to the present geological epoch, and appear to be exclusively formed of ashes and scoriae. Most of these are scattered over the woody region, raising far above the trees their summits, which are either green or bare according as their formation is of more or less ancient date. These secondary volcanos diminish in proportion as we ascend the mountain ; and a very small number only are to be met with near the summit. The mode of distribution of these extraneous cones is in complete accordance with the observa- tions which have been made during the eruptions. It is of rare occurrence to find that the great crater is alone in a state of activity. In rising towards the mouth of this gigantic furnace, the lava acts upon the sides of the mountain precisely in the same manner as a hydraulic press, and in general the earth is broken and opened by the action of this enormous force. The burning torrent escapes through this opening at the same time that it carries away with it gaseous emanations, and throws into the air the debris of the soil, which, falling back around the recent volcano, soon invests it with a ne\v cone, the eternal monument of its transitory existence. Of the eighty eruptions whose date is more or less well attested, only twenty-two are looked upon as belonging to the great crater. 80 KAMBLES OF A NATURALIST. And, indeed, in the majority of cases, the moun- tain has at these times ejected only cinders and stones. After having explored Catania and its immediate vicinity, and after having collected numerous facts to which we shall have further occasion to revert, we resolved on an expedition to the volcano itself. The Signor Abate, our host, who is a treasure to those travellers who are anxious to make the ascent, undertook to provide all things necessary for our excursion. Accordingly the three mules which were destined to carry us, were laden with a large assort- ment of travelling cloaks and ample provisions — pre- cautions which, although they seemed to us extremely unnecessary before we began our excursion, were found to be far from useless. It may be said that the ascent of Vesuvius is a mere walk, that of Stromboli a fatiguing excursion, and that of Etna a short, but an invariably arduous journey, which is not unfrequently beset with dangers. On these elevated slopes, where the ice is scarcely ever en- tirely melted, violent tempests and sudden gusts of hail and snow frequently beset the traveller who has begun the ascent under a serene and cloudless sky. Moreover, in quitting Catania to reach the summit of Mount Etna, the variations in the tem- perature and in the atmospheric pressure are very considerable. The thermometer, which during the day and in the plain has stood at 104° F. in the shade, or at about 140° F. in the sun, often falls below the freezing point during the night which the traveller is obliged to spend at the foot of the cone. THE COASTS OF SICILY. 81 In consequence of the weight of the atmosphere, a man of medium height supports at the level of the sea a pressure of about 22,775 Ibs., but when he reaches the margin of the crater this pressure will not exceed 15,258 Ibs. ; thus during this double jour- ney, which generally occupies a space of forty-eight hours, the traveller is twice obliged to support a variation of temperature of at least 72°, and a varia- tion of pressure of 7517 Ibs. We left Catania at break of day, and crossed the cultivated zone by a carriage road. These first gentle acclivities of Mount Etna present an appear- ance which is at once cheering and depressing. At every step we advance, we tread upon a soil covered by rich crops of corn and olive groves. We pass through villages, in which everything announces ease and competency, and we find on the road side charming cottages, or small and comfortable farm- steads, whose white-washed walls are half hidden beneath the luxuriant tendrils of the vine or the foliage of richly laden fruit trees. But the earth we tread upon is a bed of volcanic cinders ; the waving crops, the richly laden cherry orchards, the pomegranate trees, the flowering orange, have all sprung up on lava, which has scarcely been pulve- rised by the slow action of time. The lovely villages through which we passed, the charming country houses which we stopped to admire, are built of lava and cemented with pozzolane. Not unfrequently, indeed, the very verge of an ancient crater has served for the site of some smiling cottage, whose beauty had attracted our attention. At every step VOL. II. G 82 EAMBLES OF A NATURALIST. we take, we are traversing or skirting along some more recent lava bed whose arid and upheaved cheire* covers fields which were once as fertile as those which it now intersects in the form of a huge black dyke. Everywhere, by the side of present happiness and wealth, we see the phantom of past desolation and misery, making us tremble for the future. We more especially experience this feeling when after having passed beyond the little hamlet of Mass-annonziata, we see rising behind the houses of Nicolosi, the double summit of Monti-Rossi. This is the crater which in 1669 buried under a shower of ashes all the neighbouring country, and even threatened Catania with complete destruction, al- though it was situated at more than twelve miles' distance from it. Excavated by the violence of the eruption which produced it, it has preserved the form of two cones in juxta-position to one another, and both rising to a height of nearly a thousand feet, the dark red colour of their scorise contrasting in the most striking manner with the surrounding objects. A stream of gigantic scoriee issues from the base of this mountain, and bending in a southerly direction, falls into the sea to the southwest of Catania, being more than three miles wide in several parts of its course. The whole of this tract is covered with an arid and bare cheire, and among the enormous * Cheire or schiarra, in the Sicilian patois, is the name given to the surface of a lava bed, which has cooled on slightly inclined slopes in such a manner as to become charged with more or less considerable blocks of the same substance. THE COASTS OF SICILY. 83 blocks which have been cooled for more than two hundred years there is scarcely one which exhibits any traces of the action of time. All are of a deep black colour, and their edges and angles are as sharply cut as if they had been cooled and broken up only the day before. Not a blade of grass grows on these rocks, which seem to repulse every form of vegeta- tion, excepting here and there, where a few lichens, in thin and irregular patches, appear to struggle for their very existence.* On our arrival at Nicolosi, we were received by Doctor Mario Gemellaro, one of those three brothers who, not satisfied with having consecrated their lives to the observation of the phenomena of Etna, have endeavoured by every means in their power to faci- litate to travellers the study of their cherished mountain.f Before their time, the tourist who visited Etna was obliged to sleep under an ancient lava bank, where a poor shelter was furnished by a recess in the rock, known as the Grotta delle Capre ; and in order to reach the summit of the cone before * In his letters on Sicily, Von Borch pretends that the lava of 1669 has been covered with one inch of soil. This is an error of observation -which it is very difficult to explain, and which has already been noticed by Spallanzani. See his Viaggi alle due Sicilie. Even in our day the cheire of 1669 possesses no other soil but that which has been transported to it •f The family of Gemellaro numbers amongst its members three brothers, who have all attained to distinction ; one of them, Giuseppi Gemellaro, the author of a plan of Etna, died several years ago. A second brother, Carlo Gemellaro, is still a professor at the University of Catania. Mario Gemellaro, a physician at Nicolosi and a learned naturalist, has published several highly interesting memoirs on the meteorology, botany, and geology of Etna. c 2 84 RAMBLES OF A NATURALIST. sunrise, it was necessary to climb during the greater part of the night the steepest and most dangerous declivities of the mountain. In 1804, the brothers Gemellaro caused a small cottage to be erected at their own expense on the borders of the Piano del Lago, and having furnished it, the key was given in charge to Dr. Gemellaro. This first cottage, or casing was destroyed in 1806, but its place was soon supplied by a second, which was known as the Casino, Gratissima. Five years afterwards, in 1811, a portion of this building was thrown down by an earthquake, and the furniture destroyed. Without suffering themselves to be discouraged by this disaster, the three brothers resolved to erect a larger building in which travellers might find shelter for their mules as well as for themselves. They chose as the site of the new casino, a small hill, covered with lapilli *9 not far from La Gratissima, and sheltered on the side of the volcano by the perpendicular walls of the lava beds of 1754. With the exception of the stone, all the materials had to be carried on the backs of mules for a considerable distance, and as the expense of the undertaking would have far ex- ceeded the limited means of the three brothers, they requested some assistance from Lord Forbes, who was in command of the English troops which at that time occupied Sicily. A subscription was opened, * The term lapilli is applied to fragments of light scoriae, whose average size is about that of a walnut. The same substance, when re- duced to the volume of grains of sand, or when finely pulverised, con- stitutes, properly speaking, the volcanic cinders or ashes, which in no way resemble those of our fires, or even those to be met with in forges. THE COASTS OF SICILY. 85 and under the direction of Doctor Mario Gemellaro a substantial house was soon erected, which has hitherto been spared by the volcano. Nevertheless the perseverance of the brothers Gemellaro was doomed to suffer many other trials. As soon as the house was completed, they supplied it with furniture and an adequate provision of fire- wood. Attracted by these treasures, the herdsmen of Mount Etna broke open the door, and carried away all the furniture, and this damage which was soon repaired, was more than once repeated. At length, in 1820, at the period of the Austrian occu- pation, some of the officers who were garrisoned at Catania, resolved to visit the volcano. As natives of the north, they thought they might dispense with every precaution, and therefore did not condescend to ask for the keys of the Casa Gemellaro. On reaching the summit of the mountain, however, they began to suffer from the intensity of the cold, and breaking open the doors of the house, burnt the furniture as firewood. After this, the brothers yielded to their destiny, and remaining satisfied with having secured a shelter for travellers, they pro- vided the casa with furniture not likely to tempt the cupidity of the mountaineers, and whose low price would enable them to replace it in case of future accidents. We have designated this house under the name of the Casa Gemellaro, which we think it only an act of simple justice to bestow upon it. It is very generally known, however, under the name of the English house, La Casa Inglese* The following o 3 86 K AMBLES OF A NATURALIST. words are inscribed above the entrance: perlustrantibus has cedes Britanni in Sicilia, anno salutis 1811. Not a word is here said of those who took the initiative, who erected the first casine, and who at the present day consecrate their fortune to the maintenance of the casa. It would seem as if Lord Forbes and his officers considered that the merit of having supplied the funds necessary for the completion of the edifice, gave them the right of monopolising to themselves the entire credit of the construction, and the undivided gratitude of tra- vellers. After having received all necessary instructions from Doctor Gemellaro, and having come to an un- derstanding with the guide whom he had engaged for us, we resumed our course. Nicolosi marks the limit of the cultivated region on this side of Etna. The last houses of the village abut upon a hill of black and moving sand, where here and there a large broom, with its pendent branches of golden coloured corollas, rises from the dark soil around it.* Having passed these, we traversed a large plateau of entirely * Notwithstanding their large size, these brooms belong to our common species (Genista scoparia), which in these southern regions attains a height of from twenty to twenty-four feet. This shrub, which has been too much neglected by our horticulturists, might be made very valuable in a commercial point of view from the facility with which it thrives even on land which is very ill adapted for the growth of trees. Its slender and flexible branches furnish textile fibres, which, although they are no doubt inferior to those of flax or hemp, or even to those of the Spanish broom (G. junca\ might, if carefully prepared, furnish a very valuable substance for the manufacture of coarse canvas and linens, and would be found important from its abundance and cheapness. THE COASTS OF SICILY. 87 exposed lava, and here began our fatigues. The sirocco was blowing, and even at Doctor Gemellaro's house the thermometer had stood at 104° F. in the shade. Scorched at once by the direct rays of the sun and by the reflection of these masses of stone, we endeavoured to hasten the tardy pace of our mules, that we might the sooner reach the icoody region, whose sombre verdure seemed to promise from a distance both shade and coolness. Our dis- appointment was, however, great, when on reaching this much desired goal we found only a carpet of ferns, interspersed here and there with a few ancient trunks of branchless oaks. The southern side of Etna presents everywhere the same spectacle.1 In this vast space, which was formerly covered with primeval forests, there remains at the present day scarcely a single tree that has not suffered from the axe or fire. A lawsuit, which has been pending for fifteen years between the Prince of Palermo and the other proprietors, has occasioned all this devastation, for since the beginning of this unfortunate process no watch has been kept over the forest. The mountaineers, profiting by the op- portunity thus thrown in their way, have hacked the trees, or set fire to their roots, in order that they might fall into their hands as dead wood, and owing to this avaricious improvidence, the forest has very nearly disappeared. "We continued to ascend beneath the rays of a burning sun. The path, becoming more and more steep, passed along a loose soil which was almost entirely formed of decomposed lava, and either from G 4 88 RAMBLES OF A NATURALIST. time to time traversed some uncovered lava stream, or wound round the base of some ancient crater, which is now covered by vegetation, and stands forth like a pyramid of verdure. The fruitfulness of the woody region is remarkable, for here the flora of Etna which is so rich in species, seems at every step to dispute possession of the ground with the volcano, which is incessantly threatening it. This struggle gives rise to the most striking contrasts, for absolute sterility is often in immediate juxtaposition with the richest vegetation, as was forcibly exemplified in this portion of our excursion. For here all the slopes situated to the left of our road were concealed beneath a thick covering of green, surmounted here and there by trees, which looked as if they were merely balanced on their denuded roots. A few shepherds, followed by numerous herds, and who watched us pass with an air of indifferent curiosity, imparted animation to the scene. The shallow ground lying to our right presented an equally smiling aspect, but above us lay, like petrified torrents and cascades, the enormous lava beds of the Boccarelle del Fuoco, those twin craters, which in 1766 destroyed, according to the statement of Doctor Gemellaro, more than a million of oaks in this part of the forest. After two hours' march we reached the border of the wood and the Casa del Bosco, a small hut which is built opposite to the Grotta delle Capre. It was past mid-day, but yet the heat was less intolerable. We had already reached a height of 6,233 feet above the point from which we started, and there remained THE COASTS OF SICILY. 89 only about 3,000 feet more to climb in order to reach the Casa Gemellaro. This, however, was the roughest part of the excursion, and in order in some degree to1 renovate our strength, we resolved upon a halt. Our basket of provisions was now opened, and travellers and muleteers sat down together on the fine and close grass which is peculiar to high moun- tains, and here after partaking of a meal, which was seasoned by fatigue, we all fell asleep at the foot of an oak, covered with a few remains of foliage. After a short siesta, we resumed the ascent, and entered the desert region. Here the vegetation decreases so suddenly that it seems almost wholly to disappear. The 477 species of plants, which grow in the woody region, are here reduced to about eighty, among which we must include more than thirty species of lichens *, but not a tree or a shrub is to be seen in these solitudes. The flora of Etna is here only represented by a few of the lowest forms of plants, which are scattered in tufts in the crevices of the rocks, or upon some of the slopes formed by the ancient lapilli. Thus it is impos- sible to conceive anything more desolate than this part of the mountain. Our eyes were wearied with gazing on these slopes, which were uniformly covered * These numbers have been taken from a work, entitled, Chloris JEtnensis, o le quatro florule dell' ^Etna, by Signer C. S. Rafinesque- Schmaltz. The author of this treatise, after having resided for a long time in Sicily, settled in America, and has published amongst other works the Ichthyology of the Ohio, which is often referred to by Cuvier. 90 RAMBLES OP A NATUKALIST. with old lava, or with gray ashes. The path now became scarcely perceptible, and the mules, notwith- standing their habitual sure-footedness, stumbled at every step on this soil, which was at once moveable and hard. Nevertheless, we continued to ascend, and the temperature sensibly diminished. At the foot of Montagnuola, one of the most considerable of the secondary cones of Etna, the guides showed us the glaciers of Catania, which consist of vast masses of snow regularly arranged below a thin stratum of sand. A little higher up the snow was completely uncovered*, and here we were obliged to have recourse to our cloaks and wrappers, but very soon even this extra clothing proved insufficient to pro- tect us from the cold, and in order to retain some slight degree of warmth, we were obliged to leave * The German geologist Hoffmann, -who visited Etna in 1830, made some interesting observations on the desert region, -which we give in the subjoined table.1 Feet. Limit of the woody region on the road from Nicolosi to the crater 5470 Extreme limit of vegetation ----- 8628 Limit of the vegetation of the Astragalidse - - 7429 Limit of the vegetation of the Berberidse - - - 7110 Limit of the vegetation of the Pteris aquilina (common bracken or fern) ------- 5619 Limit of the snow under the Montagnuola, Oct. 19th - 7909 Archiv fur Mineralogie, Geognosie, $r., 1839. It ought to be observed that several of the plants mentioned by Hoffmann, rise on Etna to a much greater height than on any other mountain situated in the same latitude, which is probably owing to the internal heat of the soil. 1 [The numbers in the above table have not been reduced to English feet, as it is uncertain whether they represent French or German measurements.] THE COASTS OF SICILY. 91 our mules, and to climb on foot up the last portion of the ascent which separated us from the casa. At the moment of our arrival, the sun which was nearly hid behind the western extremity of the island, cast the shadow of Etna over the Ionian sea, and gilded with its last rays the plains of Catania and Aderno. We paused for a moment to observe this magnificent panorama, which was abruptly inter- rupted towards the north by the cone of the great crater, which rose in the centre of the Piano del Lago to more than a thousand feet above our heads, but the cold did not allow us to remain till the night closed in. The thermometer had fallen below the freezing point, and, as we entered the casa, we showered blessings on the heads of those three brothers who, on a plateau rising about 9600 feet above the level of the sea, have provided travellers with a shelter against the keen north east wind, that had been freezing us to the very heart. Less fortunate than ourselves, our muleteers were obliged to descend to the foot of the Montagnuola in order to find a grotto to shelter their mules, as the stable of the casa was still blocked up by ice and snow. Our guide alone remained in attendance on us, and in a few seconds a narrow plate of lava had been converted into a brasero, on which a charcoal fire was soon blazing, around which we crowded with feelings of intense satisfaction. Our lamps were lighted, and our pro- visions spread on< the coarse, but clean table, and while we were engaged in partaking of our frugal meal, our guide was preparing our bed by spreading a thin paillasse on the somewhat rickety planks 92 RAMBLES OF A NATURALIST. which served for a bedstead. After having filled the brasero, and taken every possible precaution for keep- ing up a good fire, we betook ourselves to our bed, which was certainly very far preferable to the lava floor of the Grotta delle Capre. Covered with our cloaks and wrappers, and huddled close to one another we soon fell asleep, notwithstanding the cold air which passed from the frozen ground through the badly formed frame of our bed. At two hours after midnight the guide awoke us, and each of us grasping a stout staff, we set out by the light of the moon on our road to the crater. We expe- rienced some difficulty in crossing the stream of lava, which in 1838 separated into two branches at the foot of the eminence on which the casa is built. We next passed over a bank of snow which craunched under our feet, and finally descended a gentle slope, covered with scoriae. Here we found ourselves at the base of the cone, and we now began an ascent which was fully as arduous as that of Stromboli. The stones and sand crumbled away at every moment from under our feet, until by the direction of our guide we struck upon a lava bed lying somewhat further west, and here the ascent became less fatiguing. At last we reached the crater, where we stood motion- less, wrapt in the contemplation of the spectacle pre- sented to us. At our feet yawned the great crater. It was not here a simple inverted cone or funnel as we had observed in all the secondary cones, and which is the case even on the summit of Vesuvius itself, nor did we see before us that uniform blackness of the rocks THE COASTS OF SICILY. 03 and ashes which characterises Stromboli. The effects of the eruption of the preceding year were still ap- parent, and the crater of Etna at the period of our visit had the appearance of a deep and irregular valley beset with points and capes, and formed by abrupt slopes, bristling with enormous scoriae and blocks of lava heaped up in masses, or rolled and twisted in a thousand different ways by the force of the volcanic action, or the accidental influences to which they had been subjected in the act of falling. The blue, green, and white lava, stained here and there with broad black patches or streaks of dull red made the livid colour of the surrounding rocks still more striking. A death-like silence reigned over this chaos ; long lines of white vapour were noiselessly escaping from a thousand different fumarolles, and, trailing slowly along the sides of the crater, car- ried to the spot where we were standing suffoca- ting emanations of sulphurous and hydrochloric acids. The pale light of the moon joined to the rising dawn was a fit accompaniment to this wild scene, whose grand and truly supernatural character no language can adequately express. The soil on which we were treading was entirely composed of cinders and scoriae, and was humid and warm, and covered with a white coating that looked like hoar frost. This humidity was, however, in fact the acid emitted from the crater, which moistened and corroded everything that came in contact with it, while the silvery film on which a few crystals were sparkling was a deposit of sulphur sublimated by the volcano, and of salts formed by the chemical re- 94 RAMBLES OF A NATURALIST. actions which were incessantly occurring in this for- midable laboratory.* By following the narrow ridge, which borders the crater to the south, we reached the highest point which is situated on its eastern extremity. Here an indescribable spectacle presented itself to our gaze. The sky was perfectly pure, the air was exquisitely transparent, while the horizon, which from the shortness of the twilight was now brightly illumined, appeared to have no other limits than that which resulted from the curvature of the earth's surface. From our lofty pedestal, we looked down a depth of four or five thousand feet upon the highest summits of the Pelorian and Madonian moun- tains, while the whole of Sicily lay spread before us as on a map. To the west the eye wandered along the summits of Mount Corleone, half hidden by the vapour which concealed Mount Eryx from our view. Beyond this limit, the sea spread far and wide on every side, serving as the frame to this glorious picture of nature. And here we could trace the route we had followed for more than four months in circumnavigating the island in the Santa Rosalia. To the north we saw the mountains of Palermo, and still more clearly Milazzo, the islands of Vulcan, and the black and regular pyramid of Stromboli ; while we could even distinguish every undulation of the soil, and trace every indentation of the coast-line along the straits of Messina on the rocky shores of Calabria. Nearer still, the massive form of Etna presented its three con- * These salts are, according to M. Elie de Beaumont, principally sulphates. THE COASTS OF SICILY. 95 centric zones, all perfectly well defined, with its sixty- five villages lying in the midst of rich campagnas, furrowed and broken up by the lava beds, which diverge from the centre like so many black radia- ting lines. To the south the eye embraced in one glance Augusta, Syracuse, and Cape Passaro, around which the coast seemed to bend back upon itself, as it were, disappearing finally amid the mist which enveloped the coast at Girgenti. Wrapt in mute ad- miration we cast our eyes from one extremity to the other of this immense circle, when suddenly the guide exclaimed, " Eccolo ! ecco il sole," and truly there was the sun, which, raising its ensanguined orb before us, bathed, in one universal tinge of purple, earth, sea, and sky, and projected to the very limits of the horizon, and across the entire island, the gigantic shadow of Etna, which, becoming more and more contracted, grew also more distinct in propor- tion as the sun rose higher above the Ionian Sea. Light vapours were now everywhere curling up- wards from the earth, as it began to be warmed by the rising sun. First thin and airy, they gradually thickened, and soon contracted the horizon on every side. After throwing one last look at the valley of the crater, we left our place of observation and descended towards the foot of a Mamelon which lay to the east. Our guide soon stopped us near a narrow and steep declivity, which was entirely de- tached from the rounded margin of the cone, and abutted upon a precipice which descended to a depth of several hundred feet. Here we saw him roll up the sleeve of his jacket and apply it to his 96 RAMBLES OF A NATURALIST. mouth, a proceeding which he signified by signs that we must imitate, rushing forward across the slope as he exclaimed, "Fate presto." Without hesitation we followed him, and speedily reached the margin of the mouth which in 1842 had thrown its lava into the Val del Bove, and which, being reopened by the eruption of 1843, appeared still to threaten the neighbouring district. It was from hence that the smoke issued which we had seen from Giardini, and it was from the depths of its abysses that we had from time to time heard rolling peals of subterranean thunder. Here all description becomes absolutely impos- sible. A vast irregularly circular enclosure formed by perpendicular walls encircled the chasm. To the left, at the foot of the escarpment, a large blow-hole had opened from which darted forth eddies of fiery red smoke. In the centre, to the right, everywhere lay enormous blocks of lava, that had been shivered, cracked, and torn, some black, others of a dark red, but all exhibiting in their crevices, the vivid tints of the lava from which they had been formed. A thousand streams of white or gray smoke were crossing and recrossing each other in all directions, with a deafening noise and with a whistling sound, similar to that of a locomotive from which the steam is escaping. Unfortunately we could do no more than throw a hasty glance at this strange and ter- rific scene. The hydrochloric acid entered our throats and penetrated to the last ramifications of the bronchial tubes ; and with haste, and almost in- toxicated, as it were, we regained the protecting THE COASTS OF SICILY. 97 slope, where we might breathe more at our ease, and then resting on our staffs, sprang to the edge of the declivity which was solely composed of move- able debris, and in five minutes we had reached the base of the cone, which it had cost us more than an hour to ascend. Our mules were waiting for us at the casa, and no sooner had they received their light load of wrappers, and cloaks, baskets and panniers, than they descended by the straight and nearest track, while we diverged to the left in order to obtain a view of the Val del Bove. This excursion was perhaps the most arduous part of our whole journey. The wind was blowing from the north-east, and in a few minutes it had grown into a perfect hurricane. Its icy breath raised clouds of sand and gravel which pricked and stung our faces and hands as if with so many needles. We found considerable difficulty in reaching the Torre del Filosopho, a small and ancient monument which is now in ruins, but which according to Sicilian legends was the habitation of Empedocles. The probability is, however, that this was once a tomb, most likely dating from a period not earlier than the time of the Roman Emperors. The Torre del Filosopho nearly touches the escarpment of Serre del Solfizio, which bounds the Val del Bove on the side nearest the volcano. Standing upon these perpendicular rocks, we admired this immense circuit, which measures more than six miles in length and more than three miles in breadth, and whose walls, which are almost every- where perpendicular, and formed of masses of lava VOL. II. H 98 RAMBLES OF A NATURALIST. older than the human race, often rise to a height of more than one thousand feet from the base, which is almost entirely composed of recent cheire super- posed upon one another. The hurricane, however, whose violence was now redoubled, soon obliged us to leave our post, and hastening onwards, we passed almost without a moment's pause before the Cisterna, an enormous chasm in shape like an inverted cone, which has opened in the midst of the Piano del Lago. "We at length found shelter behind the Montagnuola where our mules were waiting for us. Three hours afterwards we reached Nicolosi, and after offering our thanks to Doctor Gemellaro, we subscribed our names on his register below the signatures of Leo- pold von Buch*, Elie de Beaumont, Constant Pre- vost, and Adrien de Jussieu. That evening we rested at the house of Abate, and seated round his table, which is the best provided in Sicily, we forgot our fatigues, and thought only of the grand spectacle by which they had been rewarded. After having visited Etna, we are better able to appreciate the enormous power of the forces which are brought into play in this part of the globe, and we no longer regard as exaggerated the recital of those eruptions * Leopold von Buch, a foreign associate of the Institute, who died in 1853, was one of the founders of modern geology. The theory of upheavals owes to him some of the most conclusive proofs on which it is based, and he was the first who referred chains of mountains, which were parallel to one another, to contemporaneous upheavals. It is well known how much M. Elie de Beaumont has extended and enlarged these first data. Among the works which Leopold von Buch has left, we may instance as a model for other writers^, Physikalische Beschreibung der Canarischen Insefa. THE COASTS OF SICILY. 99 which from time to time have shaken the whole island of Sicily, and whose effects have been felt even at Malta and in Calabria. We will endeavour to give some idea of these terrible devastations, by relating the history of the eruption of 1669 as it has been described by Recupero.* Independently of the interest which attaches itself to this disastrous event, we are led to give this narrative with a view of drawing attention to certain facts that have been attested by a great number of eye witnesses, and which have not perhaps been sufficiently re- garded. In perusing these simple narratives which have been so naively written by ignorant monks or village curates, and which have been collected by Recupero, one is surprised to find that they afford a refutation, quite involuntarily indeed, of many errors which have found credence amongst some of our * Storia naturale e generale delV Etna, del Canonico Giuseppe jRecupero, arrischita di noltissime interressanti annotazioni dal suo nepote, tesoriere Agatino Recupero. Catane, 1815. This work, which is too little known out of Italy, contains a large number of original documents, which have been principally extracted from the archives of several towns and convents. The information relating to the eruption of 1669 has been extracted more particularly from a manuscript preserved at Nicolosi, which was written by a certain Don Vincenzo Macri, Chaplain to the Church of Nicolosi. The author reports at great length, and with an irresistible air of truth- fulness, the events which he saw, and to which he nearly fell a victim. Recupero consulted amongst others, the writings of eleven learned Sicilians, a narrative left by the Earl of Winchelsea, English ambassador at Constantinople, and another memoir by the cele- brated Borelli. He has joined his own observation to the testimony of these writers, all of whom were eye witnesses of the events that they record. The facts stated in his work appear to us, therefore, to present every possible guarantee for their accuracy. H 2 100 KAMBLES OF A NATUKALIST. most eminent savants, and which have even been admitted into technical works which are on other accounts most justly esteemed. On the eighth of March, 1669, a terrible hurricane arose suddenly at break of day and continued to rage for about half an hour, shaking all the houses of Nicolosi, and thus serving as a precursor to the disasters which were about to lay waste the country. The following night was ushered in by an earth- quake, and the shocks gradually increased in intensity until the Sunday, when the walls of the houses began to fall in. The terrified population sought safety, in the open country, and during the night of Monday a formidable shock threw down all the houses of the town. The earthquake now became more violent from hour to hour. The trees and the few huts that were still standing, oscillated like so many pieces of wood floating on the surface of a troubled sea, and men, unable to keep their footing on this moving ground, stumbled and fell at every fresh undulation. At this moment the earth opened for a length of twelve miles from the Piano di San- Lio to Monte Frumento, one of the secondary cones which lie the nearest to the summit of Etna. The fissure thus made inclined from south-west to north- east, and was from four to six feet wide, but its depth could not be sounded, notwithstanding the frequent attempts that were made to ascertain it. At length the flames of Etna burst through the soil, which had been so often broken and rebroken. The first mouth was opened to the west of Monte Nu- cilla, and threw into the air a column of sand and THE COASTS OF SICILY. 101 smoke, which was estimated by the inhabitants of Catania to have risen to an elevation of more than 1200 feet. In the space of two hours, six other mouths were opened, all of which were placed in a longitudinal line, and in the same direc- tion as the fissure of which we have spoken. A black and thick smoke issued with a horrible noise from these blow-holes, new craters were formed in the course of the day, and on the Tuesday morning the crater appeared from which arose the Monti Rossi. This last opening at first ejected a thick smoke mixed with burning scoria3, but after the course of a few hours its mouth gave vent to an immense quan- tity of lava, which forming a stream nearly three miles wide and ten feet high, took a southerly direc- tion and struck against the base of Monpilieri, an ancient crater which was then covered with trees and other vegetation. The burning stream penetrated through this somewhat shallow soil, and forcing itself a passage across the mountain, it flowed for some time along this self-made aqueduct, but Monpilieri having partially broken down, the lava flowed round it, encircling it like an island of verdure lost in the midst of flames. Seven secondary mouths opened at the same time round the principal crater. They were at first isolated, and threw up into the air an enormous quantity of burning stones, which struck each other as they fell back and joined the noise of their fall to the terrific artillery of the volcano. At the end of three days they were united into one vast 'and horrible chasm of fully 2500 feet in H 3 102 RAMBLES OP A NATURALIST. circumference, which from the llth of March to the 15th of July never ceased to pour forth its thunder- ing roar, to eject cinders and scoriae, and to vomit forth streams of lava. Up to this moment, the great crater had remained as completely inactive as if its caverns had no com- munication with those of the new volcano ; when all at once, on the 15th of March, towards ten o'clock at night, the entire mountain seemed to shake. First a gigantic column of black smoke and fire darted upwards, and then with a horrible noise the sum- mit fell piece by piece into the abysses of the volcano. On the following day four daring mountaineers ventured to make the ascent. They found the sur- face of the soil depressed round the crater, and all the openings which before had surrounded it engulfed and swallowed up, while the orifice whose circum- ference had formerly not exceeded three miles, now measured double that length.* The torrent of lava which had issued from the Monti Rossi still continued its course in a southerly direction. Its different branches reached a length of nearly four miles. Each day new streams of liquid fire flowed over the substances that had been partially solidified since the previous night, thus widening the beds of the different streams which en- croached upon the various islands of land that had been temporarily spared. Already the villages of Bel- passo, San Pietro, Camporotundo and Misterbianco had been almost entirely destroyed, while their rich * The measurements given by Recupero are probably somewhat exaggerated. THE COASTS OF SICILY. 103 territories had wholly disappeared beneath these in- candescent masses. On the 4th of April the lava came within sight of the walls of Catania, and ex- tended on to the Campagna of the Albanelli. Here, as if to show its power, it first lifted up and trans- ported to a considerable distance an argillaceous hill, covered with cornfields, and then an entire vine- yard, which floated for some time on its burning waves. After having levelled various inequalities of land, and destroyed several other vineyards, the lava at length reached a broad and deep valley, called the Gurna di Niceto. The Catanians now believed themselves secure from further danger, for they thought that the volcano would exhaust its forces before it could fill this enormous valley. What must then have been their terror, when they dis- covered that in the short space of six hours the valley was completely filled, while the lava, flowing straight towards them, stopped at a stone's throw from the walls, like an enemy who pitches his camp before the fortress which he is about to assail. The 12th of April seemed destined to witness the ruin of Catania, for a stream of lava nearly a mile and a half wide, and more than thirty feet high, ad- vanced in a direct line towards the town. Being fortunately struck in its course by another current which was flowing westward, it turned aside, and running within a pistol shot of the ramparts it passed beyond the harbour, and finally reached the sea on the 23rd of April. Then began a contest between the water and the fire, which even those who were eye witnesses of these terrible scenes seem to have H 4 104 KAMBLES OF A NATURALIST. felt the impossibility of describing. The lava, which was cooled at its base by contact with the water, presented a perpendicular wall of about 1500 yards in extent, and thirty or forty feet in height. As it slowly advanced, it carried with it, like so many blocks of ice, enormous solidified masses, which were still red-hot. On reaching the extremity of this moving causeway these blocks fell into the sea, and gradually drove back the waves in proportion as the fluid mass advanced. At the point of contact between the two elements, enormous masses of water were converted into vapour, which rising with a horrible whistling sound, hid the sun behind a thick mass of clouds, and then fell in salt rain over the neighbouring country. In the course of a few days the lava had caused the coast line to advance some 900 feet further into the sea. New affluents continued to increase the burning stream, whose current after being incessantly widened, at last reached the ramparts of Catania. Day by day the stream rose higher and higher, until it was even with the top of the walls, which no longer able to support this enormous pressure, gave way on the 30th of April for a space of about 120 feet, and the lava at once entered by the breach which had been thus made. The part of the town that had been broken in was the highest, and Catania now seemed doomed to total destruction, when it was saved by the energy of three men who ventured to contend with the force of the volcano. Doctor Saverio Musmeci and the painter Giacinto Platania, conceived the idea of THE COASTS OF SICILY. 105 constructing walls of dry stones, which being placed in an oblique position before the current, were in- tended to divert its direction. This method was partially successful, but the Dominican brother, Diego Pappalardo, devised another which promised even better success. The beds of lava become en- cased, as it were, in a sort of solid canal, formed of blocks of cooled lava cemented together. The liquid mass protected by this kind of casing, is able to extend its ravages to a greater distance by pre- serving its fluidity. Dom. Pappalardo conceived that by knocking down these natural dykes at some favourable point, he might open a new channel for these burning waves, and thus dry up the torrent at its very source. Followed by about a hundred active and vigorous men, he made an attack upon the stream not far from the crater with hammers, clubs, and sticks. The heat, however, was so intense, that every man was obliged to fall back to recover his breath after he had struck only two or three blows. However, by continued efforts, and by the aid of iron clamps, they contrived to demolish a portion of the dyke, and in accordance with Pappalardo's expectations, the lava diffused itself through this opening. But the new current turned in the direc- tion of Paterno, and the inhabitants of this town in fear of seeing the scourge which had threatened Catania fall upon themselves, sallied forth armed, and attacking Pappalardo, obliged him and his brave companions to retreat. This proceeding was, however, so far successful, that the lava was unable to overwhelm the whole 106 RAMBLES OF A NATURALIST. town, and on the 8th of May it stopped, after having destroyed 300 houses, several palaces and churches, and the garden of the Benedictines.* On the 13th of the same month a small stream flowed over the rampart to the south of the town near the Church della Palma, but a wall of dry stones which had been hastily constructed, sufficed to arrest its further pro- gress. The Catanians were less fortunate some days afterwards, when a new current invaded the castle, filled up its fosses, and speedily reached the level of the ramparts. A dyke was immediately constructed to arrest it, but on the llth of June the lava crossed the wall, and flowed through the town in the direc- tion of the Convent of the Fathers of the Monte Santo. Here a new barrier was opposed to it, which succeeded in arresting it, and thus preserved one of the finest parts of Catania. From this period the lava ceased any longer to threaten the city, and flowed in a direct course into the sea. The eruption, however, continued for some time longer, and Lord Winchelsea tells us that the cinders fell at Catania, and as far as thirty miles out at sea, with such violence and intensity as to be injurious and painful to the eyes. Nevertheless the violence of the volcano was now exhausted. After the 15th of July, it appears to have been limited merely to the ejection of cinders, scoriae, and fragments of lava, * The present garden of the Benedictines has been made up of earth brought at a great expense from a distance to cover this lava, which rises in the present day like an irregular rampart within a few feet of the walls of this monastery, which is undoubtedly the hand- somest building in Catania. THE COASTS OF SICILY. 107 which soon filled up the base of the crater and closed the mouths, which for four months and a half had hurled forth terror and devastation. Such was this mournfully celebrated eruption, which covered about fifty square miles with a stratum of thick lava which at certain points extended to a depth of 100 feet, and which after threatening utterly to annihilate Catania, had destroyed the habitations of 27,000 persons.* Even at the present day, we can trace on the surface of the soil the remains of those terrible phe«- noniena which occurred nearly 200 years ago. We have endeavoured in the preceding pages to describe the cheire which issues from the Monti Rossi, and if time had permitted, we might have found, as Recupero has done, the fifteen accessory mouths which mark, over a space of about 1500 yards, the di- rection of these subterranean forces. We might also have penetrated into the upper portion of that terrific fissure, from which was ejected the enormous quan- tity of sand which covered a space of nearly nine square miles to a depth of three or four feet, and thus spread sterility as far as the Calabrian district. Finally we might have descended into that Grotta Dfi Palombi, which through the exertions of Doctor Mario Gemellaro, may in the present day be ex- plored to a depth of more than 200 feet, where the traveller may contemplate one of the still yawning chasms which has been produced by the dislocation of the ancient strata. * Narrative of the Earl of Winchelsea as given by Recupero. 108 RAMBLES OF A NATURALIST. Without, however, having left the district of Ca- tania we had found ample opportunity of ascertaining the force of the volcano, and verifying the truth of the descriptions which we had read of its destructive action. To the north and to the west of the town we had beheld the lava beds, which threw down and crossed the ramparts, and to the south we had been able to trace the course of those undulating streams which overtopped the walls that had been con- structed by Charles Y. We had seen the for- midable thickness of this destructive stratum on descending the stairs of the Pozzo di Vela, a sort of well hollowed out in the direction of the outer side of this wall, at the base of which Prince Biscari has found the bed of the river Amenano,* which dis- * The river Amenanus of the ancients. This part of the town presents a very curious aspect. The lava, which reached to the level of the parapet, only flowed over it at a few points ; a circum- stance which shows us very plainly the mode in which the stream pro- gressed. The lava did not flow along the wall like a fluid or viscous liquid, but formed a sort of irregular pyramid, whose base rested against the wall, and whose lateral slopes exhibited as great an inclination as a steep flight of stairs. The lava consequently comported itself very much in the same manner as any mass of solid matters when thrown down an incline. These facts do not harmonise with the ideas which are commonly entertained in reference to the nature of lavas generally, more especially with respect to their cohesion. Lava streams very rarely preserve their fluidity for any length of time, for on being brought into contact with the air, their surfaces harden and offer very great resistance, even while they are- flowing with considerable rapidity. M. Blanchard and myself were enabled to confirm these facts within the crater of Vesuvius. On throwing with all our force several porous stones upon a current of lava which had burst forth at a few paces from us, and whose surface appeared perfectly smooth, we THE COASTS OP SICILY. 109 appeared at that fatal epoch. We had also traversed the cheire, which had advanced into the sea beyond the harbour in the form of a promontory, whose surface resembles that of a river on which the ice is breaking up, and whose immoveable and dark blocks frequently present surfaces of several hundred square feet, and are from fifteen to twenty feet in thick- ness. In visiting spots like these, the very aspect saw the stones rebound, and occasionally break in pieces on the surface of this apparently liquid stream. These facts, however, are well known to all those who have been eye witnesses of these terrible phenomena. This special characteristic of the lava explains to us how several venturesome travellers, and amongst others, Hamilton and the Marquis Galliani, were able to cross moving lava beds, without experiencing any inconvenience beyond the sensation of intense heat in the feet and legs. It ought further to be observed that stony substances are bad conductors of heat, which will explain on the one hand how it is that the lava proceeds with so much slowness ; and on the other, why it requires so long a time before it becomes completely solidified and cooled. We have already shown that the burning stream which issued from the Monti Rossi continued its progress for forty-six days before it reached the borders of the sea, at a distance of about twelve miles, and nevertheless in this case the enormous mass of igneous matters that was constantly being ejected from the volcano accelerated its course. In the eruption which continued for ten years, viz. from 1614 to 1624, the current of lava although it was constantly augmented, traversed only a distance of ten miles. On the other hand, the lava of 1819 advanced at the rate of a yard a day nine months after the eruption had ceased. Spallanzani in 1787 saw a walking-stick smoke and catch fire a few minutes after it had been introduced into a fissure, which was still glowing from the presence of a stream of lava, that had been solidified eleven months before. The cheire of the eruption which we have described, continued to smoke, and to give off a very sensible amount of heat eight years after the lava had issued from the Monti Rossi. 110 RAMBLES OF A NATURALIST. of which produces a profound impression, in thinking of the terrible scenes of which it has been, and may again be the theatre, and in reflecting upon the terrific phenomena of which it is the permanent seat, the human mind is unable to limit itself to tranquil and calm observation. Hence endeavours have at all times been made to explain what is passing within this formidable mountain, and for many ages, from the want of better knowledge, recourse was had to supernatural explanations. Thus, according to the ancients, Encelades, struck by a thunderbolt, groans beneath the mountain which is crushing him ; its devouring flames are the breath which issues from his chest, while the earthquakes which have shaken the whole of Sicily, are due to the convul- sive struggles of the giant. To the Christians of the middle ages, Etna became one of the mouths of hell, and even at the present day, many a moun- taineer hears the hopeless cries of the damned blending with the howls of demons within the in- nermost recesses of the mountain. Modern science has in its turn attempted to solve the problem, and supported by experimental inquiry and observation, it now seems very nearly to have attained to its final solution. Considering the enormous quantities of lava, cinders, and scoriae, which are ejected in every eruption of Mount Etna, men were originally led to regard its entire mass as derived solely from the successive accumulation of these materials. This theory which may be traced as far back as the Greek philosophers, long held undivided sway, and THE COASTS OF SICILY. Ill even in the present day it numbers many distin- guished geologists among its supporters. A very partial view of the mountain is of itself sufficient to raise doubts in reference to the truth of this explanation. The slopes which have been formed by the accumulation of moving materials freely obeying the laws of gravity, all present in their contours straight and regular lines. The lateral slopes, the terminal cone of Etna, and the numerous secondary cones on the flanks of the mountain, possess in a high degree this character of regularity. In the most ancient of these cones, and in those which for ages past have been subjected to the action of atmospheric agents, more especially of heavy rains, the declivities may indeed have di- minished, especially at the base, but they still remain regular in form, and their contours join the plain on which they stand by continuous curves. The essential character of the profile of Etna, considered as a whole, is, on the contrary, a want of continuity in its outline. Between the parts which we have designated under the names of lateral declivities and central elevation, there exists a very perceptible break. The same is the case between the central elevation and the terminal cone. These facts appear in themselves to refer these different parts to different origins, and hence M. Elie de Beaumont has been justly led to observe, that a profound knowledge of the outline of Etna was almost a theory in itself. The examination of the lava beds has led us to the same result, and here we will briefly mention 112 RAMBLES OF A NATURALIST. some of the laws which regulate their movements. It will be easily understood that a liquid or viscous mass will not comport itself in the same manner on planes of different inclination. When rapidly carried along a considerable inclination, such a fluid is unable to form a layer of the same thickness as it would attain on an almost horizontal surface. "Wherever the inclination diminished the lava stream would be deep, and wherever the inclination was increased the stream would be shallow. Conse- quently, in order that a stream of lava should pre- sent an equal thickness over a considerable extent, it is necessary that it should flow along a uniform incline. When we examine lava beds with whose origin we are acquainted, we always find that observation is fully in harmony with theory. On slopes of great inclination these lava streams only leave a narrow and thin bed which is almost entirely composed of scoriae, that is to say, of portions already solidified by contact with the air, whilst they accumulate on reaching gently inclined slopes, and here form thick and compact strata. These very simple facts may be verified by the modern streams which intersect the mass of Etna in all directions, and we meet with very frequent examples of this on the road from Nicolosi to the crater, and a little above the Casa del Bosco. Now when we penetrate into the Val del Bove, that strange and celebrated valley which bears in- scribed upon it, in ineffaceable characters, the history of the formation of the volcano, we verify several facts THE COASTS OF SICILY. 113 which appear to be in flagrant contradiction to the laws to which we have just referred. The interior escarpments of the valley are composed of several hundred strata, which are alternately formed by ledges of rocks and beds of fragmentary or pulveru- lent materials. These substances, which are very nearly similar at first sight to the lava of the present geological epoch, exhibit nevertheless a general tinge of grey, to which the deep black colour of the modern streams presents a strong contrast. They are moreover, like the latter, igneous rocks and true lava. All these strata are perfectly regular, and from one extremity of the valley to the other, that is to say, for about a length of six miles, their borders present the most perfect parallelism, without enlarge- ment or constriction. To explain this result, we must necessarily admit that, in issuing from the earth in a liquid state, these lava streams have flowed over a plane and nearly horizontal surface, where they could slowly cool and solidify. But yet, at the present day, their strata ex- hibit determined inclinations ; and on the borders of the Piano del Lagothey begin to dip, burying them- selves under the tuflfa of Etna, not far from the village of Milo. Moreover, in this long course they present various undulations and very great differences of in- clination. At the Rocca del Solfizio they are almost horizontal; but below the Montagnuola, they assume an inclination of seventeen degrees. They again ap- proach the horizontal line under the flanks of Mount Zoccolaro, which forms the southern enclosure of the valley ; and then, after curving suddenly, they take a VOL. II. I 114 RAMBLES OF A NATURALIST. strong inclination downwards, near the Porta di Callana, one of the eastern outlets of the Val del Bove. At some points this inclination amounts to as much as twenty-nine or thirty degrees. If the lava of which they are formed had flowed over surfaces so much inclined as these, they must necessarily have presented considerable variations both in their mode of aggregation and in their thick- ness ; but, as we have already observed, these strata are perfectly regular and parallel at all parts. All these strata rise and fall together, as the leaves of a book would do, if the whole were folded over one another in the same direction. We are, therefore, led to admit that at the epoch of their formation the soil presented a very different configuration from that which we now observe. This conclusion derives confirmation from a still more striking fact. The walls of the Val del Bove are not formed exclusively of those long strata of which we have spoken, for an immense number of veins or lodes, of variable diameter, intersect them from below upwards at very different angles. These veins are composed of the same rock as the strata, and many of them, by intermingling with and follow- ing the direction of the latter, clearly show their real nature. It is evident that they are fissures through which the lava formerly escaped, and which have re- mained filled with the same substances which were ejected from them. On examining one of these veins, abutting upon a lava bed on the middle of even a somewhat steep de- clivity, we find that the stream, without presenting THE COASTS OF SICILY. 115 the slightest irregularity, is continued both above and below the point at which the liquid matter found vent ; and, however numerous these veins may be, the strata are never thicker in the base of the valley than at the level of the Serre del Solfizio. It follows from hence that if, at the epoch of the formation of these strata, the soil had presented the same inclina- tion which it now exhibits, the lava, instead of flow- ing in a mass towards the foot of the volcano, would in part have ascended towards the summit, contrary to the laws of gravity. All these facts admit, on the other hand, of a very natural explanation on the sup- position which we have already advanced, that at the moment of the emission of this lava, the surface of the soil was horizontal, and that consequently these fused matters were able to distribute themselves freely in all directions. We have hitherto only taken into account, in our consideration of the walls of the Val del Bove, those matters which formerly existed in a fluid condition. An examination of the strata which have been formed by ashes and scoriae, would however, lead to the same result. If at the moment of their emission these fragments, which have been thrown into the air by a single mouth in the same manner as the modern lapilli, had fallen back upon inclined planes they would necessarily have comported themselves in the same manner as a mass of sand and loose stones falling down a flight of stairs. They would have smoothed the irregularities of the incline by accu- mulating upon the lesser slopes, and merely covering the steeper declivities by a very thin stratum. This i 2 116 EAMBLES OF A NATURALIST. is precisely what occurs at each eruption on the great cone, the secondary cones, and the lateral slopes. These fragments preserve in the Val del Bove the characteristic parallelism of stratification of which we have already spoken. This fact would, therefore, be inexplicable, if we did not admit that they must have spread in a uniform manner over nearly hori- zontal surfaces. Thus, on examining the profile of Etna, we observed that the regular declivities of the terminal cone and of the lateral slopes were suddenly interrupted by those of the central elevation, of which the Yal del Bove is only a portion. Hence we concluded that this elevation could not be formed by the same pro- cess which gave origin to the cone and to the lateral slopes-. The study of the lava beds leads us to the same conclusion; while, moreover, this observation teaches us that the strata of the Val del Bove must have been solidified on a horizontal surface. To explain how a mountain of more than 10,000 feet in height has taken the place of a plain, and how it is that we meet at Piano del Lago with the same strata which dip below the campagna of Milo, we must admit that some force has upheaved this portion of the earth's crust. Such indeed is the conclusion at which M. de Beaumont has arrived. According to his opinion, the central elevation is the primitive nucleus of Etna, and this nucleus has been formed by upheaval.* * It will be readily understood that in the brief exposition of the facts which justify this conclusion, we have merely adduced some of the most striking. We would, however, refer our readers for THE COASTS OF SICILY. 117 We may now form to ourselves a tolerably exact idea of the successive phenomena to which Etna owes its present shape and proportions. The spot on which the central elevation now rises was originally a nearly horizontal plain, whose soil, broken up by the action of subterranean fires, has at different epochs given passage to currents of very fluid lava. This lava has spread into thin and uniform sheets around these blow-holes, and in solidifying, they have formed ledges of rocks, whose compactness depended upon the thickness of the streams. As in the case of eruptions at the present day, the ejection of these fused substances was accompanied by a violent libe- ration of elastic fluids, which carried with them large quantities of cinders, scorise and lapilli. These substances, which were extremely solid, issued from all the fissures, and falling back in a shower upon the bath of lava, have thus produced these uniform strata of stony and scoriaceous fragments which alternate with those composed of rocks. These phenomena very probably continued to occur for many ages, but at length a moment arrived when the internal forces, which had so many times burst their way through the soil, displayed some ex- traordinary degree of energy, perhaps on account of the ever increasing resistance which was opposed to further particulars to the original memoir of M. Elie de Beaumont. The maps and drawings which accompany the text will remove all doubts, and we more especially recommend to them the study of the plan, which was modelled by that geologist, and of which a copy is exhibited in the Jardin des Plantes. I 3 118 KAMBLES OF A NATURALIST. their action by these strata, which had been con- tinually augmenting in number and solidity. Unable to break through them, the internal forces upheaved them, and this violent movement necessarily broke them, by which a free communication was established between the bowels of the earth and the atmosphere. M. de Beaumont is of opinion that before this event there must have been at this point a multitude of ephemeral volcanoes, which, since that period, have been replaced by a permanent volcano. But we know that in eruptions the ejected matter is not confined solely to solids and liquids, for the quantity of gaseous matter which escapes through the craters very far exceeds the volume of the lava and scoriae. It is, therefore, easy to comprehend that the enormous vault formed by the upheaval of Etna must soon have needed support. Dislocated, moreover, by the very efforts which had given it birth, it must in a great measure have fallen back into the abysses which it had covered, and it is precisely to such a catastrophe as this, that the Val del Bove owes its origin. If this origin be once admitted, we shall be readily able to understand the striking rela- tionship which exists between the craters that sur- round this valley, and the crater of the volcano itself. These craters are evidently continuations of one another, and collectively they form the circumference of the ampulla which had been upheaved on the surface of the soil. The vault, in falling in, exposed a section of the strata of which the escarpments of the valley were all equally composed, and which we again meet with on the Piano del Lago in the inte- THE COASTS OF SICILY. 119 rior of that partial sinking, which we have referred to as la Citerna* There was therefore an epoch in which the primi- tive nucleus of Etna rose solitary in the midst of the plain, towering above the whole island of Sicily with its abrupt and irregular outlines, but this condition of things was necessarily soon subjected to various modi- fications. Dating from the present geological epoch, the eruptions which have occurred upon its sides and round the central elevation have levelled the base of the mountain, and given rise to lateral slopes whose declivities and general aspect plainly reveal their origin. These lava beds, ashes, and scoria?, were a sort of modern vesture, beneath which the volcano concealed its primitive form and veiled its origin. The winds, rain, and streams, have carried into the plain an enormous mass of these moveable substances, and thus gradually formed at different points slight elevations of the soil. We thus see that these se- condary causes have incessantly tended to raise the base, and to level the plains ; and it is to the same * One is naturally led to ask at what epoch those phenomena can have occurred, of which we have endeavoured to give some idea in the preceding remarks. M. de Beaumont regards the upheaval of Etna, as having immediately preceded our present geological epoch. He believes that the outpouring of the ancient lava of the Val del Bove is contemporaneous with the formation of the chains of Atlas, the whole of which form a line bordered to the west by the Canaries and the Peak of Teneriffe, and to the east by Sicily and Etna. These determinations result from the general theory of up- heavals and from the consequences which M. if lie de Beaumont has deduced from them as to the relative age of mountain chains. (See M. de Beaumont's work on Etna, and his article Soulcvements in the Dictionnaire Universelle d' Histoire Naturelle.) I 4 120 RAMBLES OF A NATURALIST. cause that we must more especially attribute that general character of flatness which is exhibited by the entire mass of the mountain, notwithstanding its great height. It may be that, in the course of ages, the surrounding land may in this manner be so much raised, that the greater part of Etna may be buried beneath the products of its own craters. It is not probable, however, that the primitive nucleus will ever wholly disappear. The quantity of matter ejected by the terminal crater is so small, that it scarcely suffices to cover the slightly inclined surface of the Piano del Lago ; while on the steeper declivities this material is only accumulated in the crevices and ravines, in the same manner as we observe in the case of a slight layer of snow. This fact, which at first sight is almost incredible, and which is so strongly opposed to many commonly received opinions, admits nevertheless of a very ready proof. The Torre del Filosopho is only separated from the terminal cone by a distance of about 100 yards. This monument is more than 2000 years old, and yet the volcanic products accumulated round its base had only acquired in 1807 a thickness of nine feet one inch.* The Piano del Lago, which is situ- ated immediately at the foot of the great crater, does not therefore rise each year on an average more than one twenty-fifth of an inch from the accumulation of the direct products of the volcano, together with the materials which atmospheric agents may carry away * These measurements were taken by Dr. Mario Gemellaro, and confirmed by Signer Agatino Recupero. THE COASTS OF SICILY. 121 from the cone and distribute over this nearly hori- zontal surface. Here a curious comparison presents itself to our notice. The mud of the Nile every year raises the soil which it fertilises about one- twentieth of an inch ; and thus, as M. de Beaumont remarks, the monuments of Thebes and of Memphis are being more rapidly buried under the alluvial deposits of this river, than the Torre del Filosopho is being en- tombed by the ashes of Etna. Nevertheless, there is a fact which at first sight appears to be opposed to the preceding views. The terminal cone of Etna is formed with tolerable rapi- dity, for from time to time, as we have already seen, it sinks into the abysses of the volcano, and a few eruptions suffice to restore it to nearly its former di- mensions. In 1702, the Piano del Lago presented the appearance of a plateau, in the centre of which there opened a gigantic funnel. This was the crater, which had been greatly enlarged, and whose orifice opened on a level with the ground, like that of a well which is unprotected by any parapet. The present cone is not more than a century old, yet in 1834 it was ]394 feet in height, while its circum- ference at the base measured 16,410 feet. Have the matters which have been ejected from the vol- cano been the only agents which have contributed to its elevation ? If such were the case, it would be extremely difficult to explain why the Piano del Lago has not been completely overwhelmed by the cone during the course of nearly twenty centuries ; and it would be more especially difficult to under- stand why such abundance of ejected matters should 122 RAMBLES OP A NATURALIST. only have covered the walls of the Torre del Filosopho to the depth of merely a few feet. M. de Beaumont, indeed, admits that the pheno- mena of upheaval, which formerly gave origin to the mountain, are being reproduced in our own day, although with less intensity. He is of opinion that many of the cones, and more particularly the ter- minal cone, probably possess a solid nucleus, formed by upheaval, and that their external shape is due to a covering which is formed by the ejections of the crater, which thus disguise and modify the inequa- lities of the slopes. Finally, according to M. de Beaumont, Etna has not yet attained its greatest altitude, and according to his view, each new erup- tion tending to upheave it, may augment its height to an appreciable extent. This mode of considering the eruptions does away with the apparent contradiction to which we drew attention, and facts are not wanting to justify this extension of his theory. In a great number of eruptions, the fluid lava has reached the very sum- mit of the orifice, and has flowed over the margins of the great crater. The lava could not reach this elevation unless it were upheaved by an enormous power, whose action could not be limited to the vertical tube of the crater, but would necessarily be elsewhere exerted, and perhaps even over the entire mass of the mountain. Thus fissures have several times been observed which formed a sort of radiation along the face of the volcano, the lines all converging towards the crater. After the erup- tion had passed, the margins of some of these fis- THE COASTS OF SICILY. 123 sures were found to exhibit different levels; hence the soil must either have been raised on one side, or depressed on the other. Many other phenomena might be adduced to prove that even in the highest parts of the volcano, the internal agents may produce phenomena of up- heaval, but we will here limit ourselves to a positive example, which has been taken from the narrative of an eye-witness. During the eruption of 1688 there appeared in the highest part of the volcano, accord- ing to the statement of the Padre Massa, a large cupola of perfectly white snow, which rivalled in extent the domes of our largest churches, and in brilliancy the marbles of Faros and of Carara. Recupero justly adds, that this cupola must have resulted from some violent outburst of subterranean fire, which had raised and curved the superficial strata of soil that were at the time covered with snow.* We ought, moreover, to observe that these * These dome-shaped upheavals, which are the direct result of an internal action, which, however, was not powerful enough to break the upheaved strata, were known to the ancients. Strabo and Pausanias have left us details regarding a phenomenon of this nature, which happened 282 years before our era, between Troezen and Epidaurus, and gave rise to the hill of Methone. Baron von Humboldt, from whom we borrow this fact, cites in his Cosmos, the verses in which Ovid recorded and explained this event, and he draws attention to the fact, that modern science fully justifies the description of the Latin poet. The following is the condensed abstract which Baron von Humboldt gives of this passage of Ovid: — " Near Troezen, is a tumulus, steep and devoid of trees, once a plain, now a mountain. The vapours, enclosed in dark caverns, in vain seek a passage by which they may escape ; the heaving earth, inflated by the force of the compressed vapours, expands like a bladder filled with air, or like a goat's skin. The ground has 124 RAMBLES OF A NATURALIST. strata must have been of very considerable thick- ness, since they were able to protect the snow against the heat of the central fire which had caused their upheaval. Without having seen the volcanic forces in all their intensity, we were able to observe, under cir- cumstances which permitted us to distinguish their most minute particulars, the greater number of the phenomena with regard to which there has been so much discussion. On our return from Sicily, M. Blanchard and myself ascended Mount Vesuvius, and before we had advanced very far on this com- paratively easy excursion, we were fully able to ap- preciate the truth of the remark made by Spallanzani, who observed that, " to those who had seen Etna, Vesuvius must appear like a mere cabinet volcano." As if in justification of the words of this celebrated naturalist, Vesuvius exhibited to us a miniature eruption, which struck us somewhat in the light of a laboratory experiment which we could observe at our leisure in all its various phases and details. For the last two years the volcano seems to have been filling up its crater, which is now almost en- tirely full. Forty or fifty feet below the orifice, appeared a crust of black and spongy lava, some- what like a pavement of irregular asphalt, inter- spersed with large blocks of lava, and enclosed by the inner sides of the crater, as by a circular wall. In the middle of this circus, which measured from 500 to 600 feet across, there rose a small cone from remained thus inflated, and the high projecting eminence has been solidified by time into a naked rock." (Cosmos, Vol. I.) THE COASTS OP SICILY. 125 thirty-five to forty feet high, from the mouth of which eddying clouds of fiery smoke, mixed with ashes and scoriae, were being incessantly ejected, accompanied by a noise resembling that of mus- ketry. Every day some opening was made in this lava floor, on the surface of which the liquid matter was freely poured forth, and then solidified. New strata were consequently formed on the top of the older ones, which, after being again partially fused, re-entered into the general mass. At the period of our visit, the crater of Vesuvius was filled almost to its margin with fluid lava covered by a solid crust, the whole resembling a pool of water whose surface has been frozen, and on which we were able to skate as on ice. We had not much difficulty in descend- ing into the interior of the crater, and seated on a large block of lava, lying at ten feet from the small cone, we partook at our leisure of a cold fowl and a bottle of Capri. On reaching the borders of this enclosure, we could perceive, notwithstanding the brightness of the day-light, that the lava in some of the fissures was tinged with a bright red colour ; and we even per- ceived that some of the blocks were shaking, as if they were being moved by the action of an invisible hand. Occasionally, too, a hollow detonation was heard within the body of the mountain. During our dinner the flashes had become more numerous and vivid towards the eastern edge of the crater, at about fifty paces from us. It was evident that some crisis was at hand. The detonations which pealed forth from under our feet became louder and more 126 RAMBLES OF A NATURALIST. frequent ; the scoriee which were thrown up by the small volcano rose to, a greater height, and in their fall they sometimes passed beyond the boundaries of the cone; the solid crust on which we were resting began to emit a crackling noise, and a few of the less steadily poised blocks were thrown over. At this moment the soil began to rise at about forty feet from us, and in an hour's time, instead of presenting a nearly horizontal surface as it had done on our arrival, it formed, in the direction of the eastern margin of the crater, a rounded prominence of about ten or twelve feet in height. Several openings appeared on its side, but these were soon reduced to three, and finally to a single one, from which a perfectly fluid lava issued, and flowed in a straight line towards us. At its origin this burning stream was at most about four or five feet in width, and here it exhibited a beautiful and almost dazzling whiteness; but it gradually acquired a deep red colour as it also became considerably wider in the course of its progress. In about two hours' time it had reached the spot where we were standing, and we now began to retreat step by step before it. At the same time the entire crater seemed to waken into activity. All its fissures and crevices gleamed with light, and the block which had served us for a table began to grow red round its base. Every moment the heat grew more intense. It was a true overflowing, occa- sioned by the afflux of the liquid matters which rose from the abysses of the volcano. It was now necessary to think of retreating, for when we reached the margin, at least one sixth part of THE COASTS OF SICILY. 127 this surface, which had previously been solid, was in a state of fusion; and it was evident that the blocks of lava on which we were standing, although they were still joined together, formed only a simple flooring, supported by this lake of fire, like a piece of ice which is still connected with the shore. These appearances were indeed very different from those which precede the great eruptions of Etna. Nevertheless, the difference is more apparent than real. The phenomena are fundamentally the same, and differ only in the amount of their in- tensity. The small cone of forty feet serves, like the mountain of 10,000 feet, to give issue to the internal agent, and to eject flame, gases, smoke, sand, and scoriae. Each ejection was accompanied by a noise proportionate to the energy of the sub- terranean fires. The stream of lava which was advancing towards us, at one time disturbed and overthrew solid blocks, which lay in its passage, and at other times upheaved and carried away with it the fragments of these masses, which floated on its surface like blocks of ice on a river which is breaking up. It is evident that these disturbances of the strata and these upheavals, which we may actually observe in the crater of Vesuvius, must be reproduced on a much larger scale in all great eruptions generally, and in those of Etna more particularly. The cen- tral elevation and the terminal cone — which are formed of strata which have been upheaved and consequently broken at many points, and of move- able materials which are simply accumulated toge- 128 E AMBLES OF A NATURALIST. ther in masses — cannot possess any great stability. The sinking in, which is visible on the margins of the Piano del Lago and at other points, sufficiently proves how deficient in solidity is this kind of frame- work. When the subterranean furnaces are kindled and the rocks are fused, and an enormous quantity of gas liberated, an outlet must be obtained at some point or other. And if the crater is slow in opening, and the passages of communication should be closed, why should not the boiling lava raise up the vault which accidentally confines it in the same manner as the lava of Vesuvius, acting alone and without any shocks, upheaved before our eyes a hillock of several feet?* The difference of thickness of the strata cannot be adduced in opposition to these conclusions. Is the earth's crust, on which we dwell, and in which the basins of our seas are hollowed out, in reality so solid as we are inclined to imagine ? We will pause to consider this question. Entire provinces have been gradually and con- tinuously raised ; as, for instance, a portion of Scan- dinavia. In other cases they have been suddenly elevated above the ordinary level, as was the case in 1822 with the territories of Valparaiso and Quintero. Considerable islands issuing from the bottom of the * During the whole time that M. Blanchard and myself remained within the crater, that is to say, for more than three hours, we experienced nothing that resembled an earthquake. It was the absence of every indication of this convulsion which enabled us to enjoy entire security, and to observe without the least uneasiness the beautiful eruption which was so well adapted for a subject of study. THE COASTS OF SICILV. 129 sea sometimes vanish as rapidly as they have ap- peared, as those islands of the seas of Iceland and the Azores which rise from the waves, eject flames and then sink into the abysses, from whence they had emerged ; as, for instance, the Isle of Julia, which in 1831 rose in the Sicilian waters, although not a trace of it now remains ; at other times, these islands become solidified and increase in number, as, for instance, in the case of Santorin, the Aleutian Islands, and the Azores, where in 1757 nine new islands were formed in less than a twelvemonth. At one place we find that in a single night plains have been upheaved, bristling with volcanic cones, as was the case atMechoacham at the time of the formation of the volcano of Jorullo in 1759; while, in another place, we find that they are buried in the entrails of the globe, as, for instance, at Sorca, where forty villages disappeared with the land on which they stood. Mountains crumble away and are replaced by lakes, whilst others, on the contrary, rise from the earth, block up the course of rivers, or replace a bay by a cape. Earthquakes cause our fields to undulate, like an agitated sea overthrowing and engulfing our cities, and even at times shaking both hemi- spheres at once. We see therefore that everything teaches us that the crust which we crJl terra Jirma, in reality very little merits that title. We see how thin and fragile is that pellicle which envelopes the fluid part of our globe*, and we learn to understand * A very erroneous idea is generally entertained in reference to VOL. II. K 130 IIAMBLES OF A NATURALIST. how rapidly it might be destroyed if a more or less free outlet to the action of subterranean fires was not always presented by the 550 volcanoes which are disturbed over its surface like so many safety valves.* the thickness and solidity of the earth's crust. The following figures will furnish a more exact idea on this subject. The most superficial strata of the soil participate in all the varia- tions of temperature which depend upon the seasons, and this influence is exerted to a depth which, although it varies with the ati- tude, is never very considerable. Beyond this point, the temperature rises in proportion as we descend to greater depths, and it has been shown by numerous and often repeated experiments that the increase of temperature is on an average one degree (Fahrenheit) for about every 54'5 feet. Hence it results that at a depth of about ?,000 yards from the surface we should reach the temperature of boiling water. In supposing that the heat increases in a uniform ratio, we should have at a depth of twenty miles a temperature which would fuse most of the silicates that enter into the composition of our rocks ; and at a depth of about twelve miles from the surface we should be on the verge of the incandescent mass which constitutes almost the whole of our globe. Now this thickness, when compared with the dimensions of the earth, would represent about one inch for a globe whose diameter was about nine yards. In other terms, it would very nearly equal the thickness of a sheet of ordinary letter paper for one of those globes which are commonly used for geographical studies. With this illustration of the question before us, we cease to be asfonished at the movements which can agitate this pellicle ; and indeed if there is anything to excite our surprise it is rather that the habitable surface of our globe has not more frequently been the theatre of such convulsions, which, although they might be terrible in their results to ourselves, would not the less remain almost inappreci- able on the "vast extent of our planet. * The following table gives the number and the geographical distribution of all the volcanoes and solfataras (semi- extinct volcanoes) whose existence has hitherto been verified. THE COASTS OF SICILY. 131 Man is small and feeble, but full of pride, and he always takes himself as the unit, and as a term of comparison. He measures the globe and the universe by his own stature, and the infinite powers of nature by his own forces. In his eyes, Etna, that blow-hole which is scarcely perceptible upon our planet, which is about 24,000 miles in circumference, is a gigantic mountain, and he starts back in amazement at the forces which are required to upheave it. It is not very difficult, however, to convince oneself that in volcanic phenomena the energy of the cause is fully in harmony with the greatness of the effects. Let us then, by way of illustration, inquire what relation exists between the forces employed at the present day by industrial science and those which slumber within the crater of Etna. Let us suppose, and the assumption is by no means an exaggerated one, that this crater is 500 yards in diameter, and that it penetrates below the earth to a depth equal to the height of the mountain. The magnificent steam engines which exhaust the air on the atmospheric line of Saint-Germain, have ti 400-horse power. They act under a pressure of six atmospheres, and their pistons present a surface of more than three square yards. In approximate calcu- Parts of tho World. Volcanoes Volcanoes of Continents. of Islands. Total. Europe - - - - 4 - 18 - 22 Asia - - - 55 - 71-126 Africa - - - - 13 - 12 - . 25 America- - - - 114 - 90 - 204 The Ocean - - - -183-182 Total 186 373 559 (Nouveau Cours dementaire de Geologic, by J.-J.-N. Iltiot.) K 2 132 RAMBLES OF A NATURALIST. lations like this, the pressure of an atmosphere on a surface whose extent we know, may be regarded as equal to the weight of a column of water of the same base, and of eleven yards in height. Conse- quently the total effect produced by the machines of Saint-Germain may be represented by a weight OA about 150 tons. A column of water raised from the level of the sea to the summit of Etna, would exert a pressure of 300 atmospheres, but the fluid lava is very nearly three times heavier than water. Consequently when this lava flows over the margin of the terminal cone, its pressure at the level of the plain will equal a force of 900 atmospheres, while its force at the bottom of the crater itself will be equal to the pressure of 1,800 atmospheres. The weight of this pressure on every square yard of surface will there- fore be equal to more than 40,000 tons. Now we know that the pressure of liquids is exerted in all directions at once. Consequently each square yard of the vault which supports the volcano is subjected to a force, acting from below upwards, which is 283 times greater than that of the machines of Saint-Germain. In the crater alone, the total force which is solely employed in sustaining the column of lava at the level of the orifice is equal to 53,262,500 times that of these machines. This is a force of more than twenty-one thousands of millions of horses. Hitherto we have supposed that the steam engine was in perfect working order, and that the lava rose easily to the margin of the crater. We know, THE COASTS OF SICILY. 133 however, that this is not always the case. In the steam engine the safety valves become clogged, and are no longer available at the right moment ; innu- merable causes, some of which are still unknown, bring about the sudden evaporation of too large a quantity of water. In this case the boilers burst, and rending the most solid walls throw the fragments far around them. Under circumstances such as these, masses of fused metal weighing two tons have been projected to a distance of 250 yards. Now volcanoes have also their explosions, or, more cor- rectly speaking, their eruptions are to a certain extent one continuous explosion, and the preceding remarks will show how extremely powerful must be their action.* To appreciate completely the forces which are put into action, it will be necessary to add to the pressures that we have already calculated the tumultuous liberation of vapours and gases, and the frightful degree of tension to which these elastic fluids must be subjected at a temperature capable of * The following numerical details will afford some idea of the •volcanic force. M. d'Aubuisson des Voisins estimates the velocity of the matters ejected at the mouth of the crater to be about 400 or 500 yards in a second. This is very nearly the velocity of a ball at the moment it leaves the cannon's mouth. On assuming that this velocity is only 200 yards per second, it has been found that, during certain eruptions, Vesuvius has thrown its artillery of rocks to a height of more than 4,000 feet. Estimates of height are, however, almost always very conjectural, and the volcanic force can be much better estimated by the space which is traversed horizontally. Now the volcano of Cotopaxi has ejected, to a distance of nine miles from its crater, blocks often cubic yards; that is to say, masses of rock weighing about 30 tons. From this we may judge of the force developed in the interior of the volcano. K 3 134 RAMBLES OF A NATUKAL1ST. liquefying the hardest rocks. It would be necessary to multiply the upward pressure resulting from these combined forces, not merely by the surface of the crater, but by the extent of the base, which may perhaps embrace the entire central elevation, and we should then obtain numbers representing a force of which nothing would be able to give us any adequate idea, if the mountain itself did not exist as a monu- ment of this formidable power. 135 CHAP. VII. THE BAY OF BISCAY. BIARRITZ. — G UETT ART. — SAINT • JE AN-DE-LUZ. Departure for the Bay of Biscay. — Bayonne. — The bar of the A dour. — Biarritz. — La chambre (Tumour. — Geological problems relating to the age of neighbouring rocks. — Guettary. — Saint- Jean-de-Luz. — Encroachment of the sea. — Wearing away of the coast; the ground swell. — Hermellas. — Extreme variability in the type of the Annelids. — The Polyophthalmians ; organic compli- cation.— Realisation of some of the fables of mythology. — Independence of the nervous centres in certain of the lower animals ; transposition of the ordinary seat of certain sensations. THE early portion of June 1847 was a period of much enjoyment to me, for after a two years' un- avoidable delay, I was at length enabled to resume my studies at the seaside ; the Bay of Biscay being on this occasion the scene of my exploration*. This expedition was almost like a voyage of^discovery, for only one naturalist had preceded me in the zoological investigation of this portion of the coast of France. In 1794, M. Alexandre Brongniart had on different occasions visited the mouth of the Adour, and ex- plored the neighbourhood of Biarritz. Being in- formed of my intentions, he placed his memoirs and notes most freely at my disposal. Although he was already then labouring under the disease to which he fell a victim a few months afterwards, M. Bron- K 4 136 K AMBLES OF A NATURAL I ST. gniart * laid before me his diaries and the journals in which he had day by day recorded the varied events of his life. For two hours we perused together these memorials of the past, and often the voice of * For more than a century the family of Brongniart has enjoyed the rare privilege of finding that the members of each new genera- tion enhanced by their own eminent merit the splendour of the name which they bore. Alexandre Theodore Brongniart, a member of the Institute, whose fame first rendered this family illustrious, was born in Paris in 1739, and died in the same city in 1815. Having been originally destined for the medical profession, he first directed his attention to scientific pursuits, but yielding soon to his taste for the fine arts, he devoted himself entirely to the study of architecture. We owe to him the erection of some of those princely mansions which are daily being replaced by the humbler houses of the bourgeois, and some of those parks which even more fully manifest the style of living in former times. M. Brongniart was engaged throughout the whole of his life in different public offices ; he also erected many public edifices, among others the Bourse, the exterior of which was partly constructed in accordance with his plans, but on his death the completion of the work was entrusted to an architect who made very great alterations in the original designs. Alexandre Brongniart, a member of the Institute, and professor at the Jardin des Plantes, was the son of Alexandre Theodore Brongniart. He was born in Paris in 1770, and died in the same city in 1847. From, an early period he devoted himself to science, and at the age of twenty he published a work on the means of improving the art of enamelling. While he was attached to the Army of the Pyrenees, in the capacity of a military pharmacien, he devoted his attention specially to zoology, and commenced a memoir on the anatomy of Cephalopodous Molluscs, which, however, he abandoned as soon as he learned that Cuvier was engaged on the same subject. He next studied mineralogy, and published in this department of science a Traite elementaire, which was adopted by the University, and was used in the mineralogical class at the Jardin des Plantes. Brongniart having combined the study of living and fossil animals, THE BAY OF BISCAY. 137 this aged philosopher grew strong, and his eyes glistened at the recollection of those days of his youth, when, as a humble pharmacien attached to the Army of the Pyrenees, he would wander forth at published successively a treatise entitled Essai d'une Classification naturelle des Reptiles, the principal results of which have been uni- versally adopted, and several important memoirs on fossil shells and crustaceans. It is to this last work that we must refer for his ob- servations on the Trilobites — a family whose true nature he was the first to recognise, but which has since then been so much multiplied as to have become the subject of special treatises of considerable extent. At this epoch, Brongniart had become the collaborateur of Cuvier, and it is to their united efforts that we owe the work which was first published under the title of Essai sur la Geographic miner alogigue des environs de Paris (1810), and two years afterwards under that of Description geologique des environs de Paris (1812). Subsequently Brongniart made a great number of geological expe- ditions, traversing every part of France, and a great portion of Europe, and he has fully established a claim to be regarded as one of the founders of modern geology. These different labours did not, however, make him lose sight of a work on which he had been engaged for more than forty years. Having been nominated in 1807 to the directorship of the manufac- tory at Sevres, he wished to bring the light of modern science to bear upon the manufacture of porcelain, and the results of his various investigations were incorporated in a work, entitled Traite des Arts Ceramiques, which appeared only two years before his death. M. Adolphe Brongniart, member of the Institute, and professor at the Jardin des Plantes, is the son of Alexandre Brongniart, and the worthy inheritor of his name. He first devoted his attention to botanical studies, for which he was prepared by his researches in minute anatomy and physiology. Among the works which he has published in this department of science, we may particularly instance his observations on the organisation of leaves and on the fecundation of plants ; but M. Adolphe Brongniart owes more especially the high rank which he occupies in science to his researches on fossil plants. We may say that he is the founder of vegetable palaeontology, as Cuvier was the founder of animal 138 KAMBLES OF A NATURALIST. dawn, provided with a piece of bread, which was to serve for his meal through the day. Exclusively absorbed in the studies which were to render his name illustrious, he was contented and happy if he could return at night with some fossil, some mollusc, or some alga, which he had gathered from the rocks on the shore, or in his wanderings along the sandy beach. M. Brongniart belonged to a generation which is daily passing away. All his life he had loved science for her own sake, and revered her under every form and every manifestation ; he loved her too personified in those young and ardent students of nature who, like himself, had been zealously devoted to her cause, and he ever treated them not as rivals who were to be feared and shunned, but as successors who merited instruction and assistance. A week after my interview with M. Brongniart, I was at Bayonne. In every other place I had always found a sort of separation between the water and the rest of the landscape, but here the country and the sea seemed to approach and blend with one another. Near its source the Adour, which is scarcely wider than the Seine at the Pont des Arts, winds along the foot of lofty hills. Near its mouth dunes covered here and there with pines *, appear palaeontology. Thus both departments of that new science of palaeontology, which teaches us to read the history of the globe in its fossil remains, with as much certainty as we read the history of man on the monuments of the past, is of a wholly French origin. * The kind of pine which grows near Bayonne is the Pinus mari- tima. This tree, whose trunk is often twisted, and whose wood is too soft to be of any great value, has nevertheless become a source THE BAY OF BISCAY. 139 to bar its passage, while within the town itself, the trees of the public walks reach its very banks. Everywhere the black hulls of ships, their tall and slender masts, and their white or reddish sails, stand out against a back ground of verdure. One might almost suppose that one was viewing an inland lake, did not the rising tide indicate the vicinity of the ocean. Twice in the day the waters of the river are driven back, and the direction of the current changed, whilst the bridge of boats which connects Bayonne with its faubourgs as often rises and falls. The Adour presents a somewhat singular pheno- menon in the history of our rivers. At several different epochs its mouth has changed its place. The inhabitants of the district assert that it formerly flowed into the sea between Biarritz and Bidar, to the south of its present outlet, but an examination of the localities does not confirm this tradition. On the other hand, it is quite certain that at different periods this river has made an eruption towards the north. In 1360, the same tempest which destroyed the fleet of Edward III. off the coasts of Normandy, filled up the bed of the Adour and inundated Bayonne and the neighbouring districts. Harvests, cattle, merchandise — everything, in short, perished in the waves. At length the waters found an outlet near Cape Breton, and the river having formed for itself a new bed, fell into the sea at Vieux Boucaut, at of riches to the whole of this district, from the great quantity of turpentine which it produces, and from the facility with which it grows on sandy dunes, which it consolidates, and whose further progress it arrests. 140 KAMBLES OF A NATURALIST. about twenty-four miles distance from its former mouth. For two centuries the Adour followed this direction, until, in 1579, Louis de Foix made a successful attempt to turn it back to its former bed. From this time forth, as in olden times, ships were able to come up to the harbour of Bayonne without the slightest difficulty ; but it would appear that there was soon reason to fear new disasters. Under the continual action of the waves coming from the north- west, the channel, which had at first been tolerably direct, gradually inclined towards the south, and filled up the bed of the river with sand. In 1720, the channel had become almost impracticable. The river was now for the first time embanked, and from thenceforth additions were constantly being made to the magnificent dykes of Touros. The engineering difficulties were, however, far from being removed, and the bar of the Adour has always continued to be a somewhat perilous, and often an impracticable passage, notwithstanding the assistance which is afforded by a tug steamer that is always stationed here for the purpose of towing ships into the harbour. The bar of the Adour always presents the appearance of a restless and troubled sea. I have visited it during one of those splendid autumn days, when all nature seems to repose after the activity of the past season, and to prepare for the torpidity of winter. The breeze that was coming from the east was so slight that it did little more than stir the pennons that were hanging at the mastheads of the many vessels moored along either side of the river, and yet before I left the " Alices THE BAY OF BISCAY. 141 Marines/' those lovely walks which are singularly enough neglected by the Bayonnese for the ramparts of the town, I could hear that distant thundering crash which announces the vicinity of a stormy sea. The half clouded sun was gilding with its rays the whole town of Bayonne and its framework of hills, when I made my way along the narrow jetty of the left bank, which, although it seems a very feeble barrier against the power of the ocean, has hitherto proved sufficient to protect these sandy shores from being worn away. When I approached the village called Boucaut, the noise of the breakers was re- doubled, and at the Quarantine house it became truly formidable. At length I reached the Signal tower, from whose platform I commanded a full view of the mouth of the river and its adjoining banks. On either side the smooth and low beach sloped gradually upwards to the long line of sandy dunes, where many arid points rose above the plantations of pines, which were intended to fix the drifting soil. At my feet lay the low dykes which were planned by MM. de Prony and Sganzin, with a view of gradually contracting the bed of the river, and of acting as a means of flushing the sand and gravel. Before me lay the ocean, whose smooth surface was unruffled by the slight east wind that was then moving over its waters, and yet a broad semicircle of waves and foam separated the sea and the river. This was the bar of the Adour, and here was raging that storm which I had heard for more than an hour. 142 RAMBLES OF A NATURALIST. The tide was rising. Scarcely perceptible waves, which were flowing in from the ocean, rose by degrees as they came in contact with these low embankments, and fell into long undulations like extended lines of walls. Broken at their base by these breast-works, they were twisted upwards in coils, which rapidly descended in a shower of white foam and mist. Being soon again lifted up, not to an equal height, but with a greater force, they rose opposite to the Adour like a quadruple barrier, which was perpetually being destroyed and reproduced, until at length they reached the shore, where they broke with fury into a thousand foam-crested lines, dashing their long and rapid jets of white mist to the very top of the incline which had arrested their progress. At the mouth of the river they rushed precipitously through the narrow channel, dashing to the right and left against the jetties, as if they were endeavouring to open a broader passage for the waters of the ocean, and bearing with them in their course masses of yellowish foam, which looked at the distance almost like floating rocks. Every stranger on arriving at Bayonne makes a point of visiting Biarritz, and as I was anxious not to depart from the ordinary custom, I lost no time in making inquiries as to the means of accomplishing this journey. Formerly this excursion was always made on the back of some animal, either a horse, mule, or donkey, on which was placed an apparatus very much like a set of double panniers, and this mode of travelling was called riding en cacoleL The traveller seated himself on the one side, while on THE BAY OF BISCAY. 143 the opposite side of the animal, by way of balance, sat the cacolettiera, a sprightly black eyed Basque damsel of lively wit and quick repartee, whose engaging conversation no doubt contributed very materially to compensate the traveller for the length and weariness of the route. The progress of civilisation, and the necessity of more rapid and frequent communications, have, how- ever, put an end to these romantic journeyings. A tolerably good road now joins Biarritz to Bayonne. Various omnibuses and minibuses, decorated with the name of diligences, now carry on an active traffic, which is rendered more exciting by the competition of cabs and other carriages ; but I have no doubt that many a traveller, when seated within these dusty and ill-adjusted vehicles, has often regretted the cacolet of former days. Nevertheless a journey to Biarritz is well worth an hour's exposure to dust and the jolting of a rough vehicle. This village is the very realisation of some lovely and picturesque scene in an opera. Imagine a small plateau terminating in a deep gorge, sloping rapidly towards the sea, and surrounded by mountains and rocks, interspersed with precipices and ravines ; the whole scene being abrupt and wild, although on a very miniature scale ; such was Biarritz before it became one of the most celebrated bathing places of southern France. Its two lines of hills advance into the sea in the form of a double-horned cape. To the left at the Pointe des Basques, begins a high range of cliffs, which stretch far towards the south, while to the right the Cote des Fous is dotted over 144 RAMBLES OF A NATURALIST. with the perforated rocks of the Attala'i, whose isolated pinnacles have been strangely fashioned into various shapes by the waves that are rapidly wearing them away. Between the Pointe des Basques and Attalai lies Port-Vieux, from whence many whalers were wont to set sail year by year in former times, although the harbour, which is constantly being con- tracted, can now do little more than give shelter to a few stray fishing smacks. Encased as it were within this charming framework, lie the picturesque habita- tions of Biarritz. Some of the houses occupying the plateau and the bottom of the valley constitute the village and its principal street, whilst others are grouped here and there, by chance, as it were, and in accordance with the nature and character of the ground. The green blinds and dazzlingly white walls of these cottages, give them an air of cleanli- ness and comfort, which is well adapted to attract visitors, arid each year the nomad population which flocks to Biarritz tends more and more to convert it into a fashionable watering-place, to the loss of the invalids who formerly resorted to it. The coasts of the Bay of Biscay are extremely dangerous, even to the most skilful swimmers, except at a few sheltered spots. The Port-Vieux is, however, perfectly adapted for bathing, for it seems like a basin artificially formed by the hand of man for the very purpose. On either side, the two points of the cape break the force of the waves and neutralise the effect of the currents. The sandy bottom slopes gently upwards towards the shore, which is overlooked by the last houses of the village, THE BAY OF BISCAY. 145 and a few of the principal establishments which have lately been erected for the accommodation of travellers. Narrow paths run in a zig-zag direction all round the harbour, and at the hour for bathing these walks are crowded with the promenaders, who for the moment have deserted the rocks of Attala'i, or the beach of Les Basques. Thanks to the patriarchal traditions of Biarritz, no artificial barrier separates the male and female bathers. Men and women here adopt a costume, to which the most scrupulous prudery could not object, but which varies some- what according to individual taste, and thus conver- sations or even flirtations are as agreeably conducted in the bath as on the promenade. It afforded me no little pleasure to watch this scene of enjoyment and sport, in which harmless defiances were giren and returned amid cries of joy and shouts of laughter. Every one is ambitious of outvying his neighbours, and even the most timid lady is desirous of reaching, at least once, the line which is slung across the entrance of the harbour. In order to attain this desired goal, most of the fair bathers are obliged to have recourse to the aid of some attendant cavalier, or to accept the less agreeable support of a rude swimming belt, composed of a pair of large gourds. I have, however, seen several daring lady swimmers, chiefly Basques or Spaniards, who, without the slightest apparent effort, would bring up a handful of gravel from a depth of ten feet, or would take a header with all the ease and security of a proficient swimmer. At about a mile from Biarritz lies la Chamlrc VOL. II. L 146 KAMBLES OF A NATUEALIST. d? Amour, a deep recess hollowed out in a semicircle, and surrounded by inaccessible cliffs. The only access to it is by a narrow tongue of sand which is left dry by the retiring tide at the base of the northern cliffs. Formerly the shore was everywhere very low, and at high tides the waves beat the precipitous rocks of the bay in every direction, and sometimes penetrated into the grotto which had been excavated in the cliff. According to tradition it once served as the rendez-vous of two lovers. For a long time the ocean appears to have respected and protected their try sting place ; but one day, \\ hen the waves were driven violently against the rocks by a strong north-west wind, the waters rose above their usual level, and the next day a fisherman, on pene- trating into this rocky recess, found the bodies of the lovers clasped in each other's arms. A similar catastrophe need no longer be appre- hended. For many years past the repeated shock of the waves has crumbled away a portion of the cliffs, and the sand which has been washed in from the open sea has covered these debris, and obstructed the entrance to the grotto. At the present day, if the traveller were surprised by the tide and imprisoned Avithin the Chambre d' Amour, the worst that could befall him would be imprisonment for a few hours in the open air, or perhaps, if the sea were running very high, he might be compelled to take refuge on the summit of the little hillock which covers the tomb of the two lovers. The naturalist feels perhaps even a greater interest than the poet in the Chambre d'Amour, for the un- THE BAY OF BISCAY. 147 dulation of the soil surrounding it marks the extreme boundary of the chain of the Pyrenees. At a few feet from this little bay, the cliffs sink to rise no more, their last rocks dipping below the sea of sand, which extends as far as La Gironde, exhibiting in the midst of our richest provinces a miniature representation of an African desert. Biarritz, with the surrounding district, which is thus situated on the limit of one of those great geological formations which give to our globe its existing configuration, presents very curious problems, regarding whose solution geolo- gists are by no means agreed. We will endeavour to give some idea of this subject, by taking for our guides the magnificent Atlas* and the special Memoirs of MM. Dufrenoy f and Elie de Beaumont. * In 1811, M. Brochant de Villiers, professor of mineralogy and geology at the School of Mines, first proposed to construct a geological atlas of France. The execution of this project, after many delays, was resumed in 1822, under MM. Dufrenoy and Elie de Beaumont, who shared in the responsibility and labours of the undertaking. They devoted themselves for nineteen years to this great work, which appeared in 1841. It is unfortunately very difficult to procure copies of this splendid atlas, in consequence of the government having reserved to themselves the absolute monopoly of the work. f M. Dufrenoy a member of the Institute, professor at the Jardin des Plantes, and Director of the Ecole des Mines, has raised himself to the first place among contemporary geologists by the publication of numerous works, among which we will only instance those which refer to the geological atlas of France and to Mount Vesuvius, the latter of which is to a certain degree the pendant to that of M. Elie de Beaumont on Etna. M. Dufrenoy has especially endeavoured to restore to mineralogy its character as a science of observation, which it had partly lost by the introduction of almost exclusively chemical methods. His TraitG de Mincralogie, which is L 2 148 RAMBLES OF A NATURALIST. It is well known that our globe has only gradually attained its present configuration. Before it pre- sented the elevations and depressions which are now figured on our geographical maps, its surface under- went numerous convulsions which were separated from one another by long intervals of repose. During these periods of rest, whole tracts of land were heaped up upon one another, and strata superposed on other strata at the bottom of the vast seas of those geological periods, but when the moment of a new cataclysm arrived, the forces which had been tem- porarily dormant in the centre of the globe were again awakened, and thrusting the subjacent rocks through more recent deposits, caused hitherto sub- merged continents and new chains of mountains to be upheaved. Vast dislocations, twistings, ruptures, and disturbances of strata accompanied each of these upheavals, and it is from these disturbed masses, and the relations by which they are connected, that modern science has succeeded in tracing, with an almost incredible degree of certainty, the history of these vast revolutions. At the period when the land surrounding the Bay of Biscay first appeared, Europe generally, and France more especially, bore no resemblance to their present condition. Twelve upheavals or cata- clysms had already taken place.* Auvergne, the accompanied by a magnificent atlas, has become a standard work 011 the subject to which it refers. * These numbers have been given by M. Elie de Beaumont in one of his recent publications on the subject. Article SYSTEMES DE MONTAGNES in the Dictionnaire Universel (THistoire Naturelle. We ought however, to observe that the author himself merely THE BAY OF BISCAY. 149 Black Mountain, and the Cevennes formed a sort of continent, which extended as far as the Ardennes and the Yosges; Brittany, a portion of Normandy, Maine, and La Vendee were prolonged into a sort of irregular isthmus, and were connected by Poitou with this central plateau, while Flanders, Picardy, Cham- pagne, the Paris basin, Upper Normandy, Touraine, the south of France, and the north of Spain were all one vast sea, in the midst of which rose a fe\v scattered islands. At tlje bottom of this sea were deposited the last strata of the secondary or creta- ceous formations, which by their thickness and variety attest the long period during which this condition of things must have existed. This state of repose was disturbed for the first time by the thirteenth upheaval, namely, that of Mont Viso, which gave origin to the French Alps. Then, after another period of tranquillity, came the fourteenth cataclysm, which was one of the most considerable of which we have any traces on the earth's surface. It extended from the western extre- mity of Europe as far as North America, through the whole of Asia ; and it is especially to this up- heaval that the Pyrenees owe their present eleva- tion.* The eruption of the primary rocks which regards these numbers as provisional, and as representing only the present condition of science. No one could be less disposed than M. Elie de Beaumont to assign impassable limits to the progress of knowledge, and on this account he has always designated every recognised upheaval by a name, borrowed either from the principal chains which have resulted from it, or from the districts in which it has occurred. * The present form of mountain chains is r.ot owing to a single L 3 150 RAMBLES OF A NATURALIST formed the central axis of these mountains, uplifted the chalk strata of which we have just spoken. On either side of this chain we find that the strata are inclined in a direction parallel to this axis, and they constitute all the littoral rocks of the Basque pro- vinces. If the geological phenomena that occurred round the Bay of Biscay had stopped at this epoch, their explanation would have presented very slight diffi- culties; but such is by np means the case. The chalk strata which have been raised and thrust to the south by the appearance of the Pyrenees, and retained towards the north by the ancient formations on which they rested, had been bent in the middle, and hollowed into a vast depression, which had been immediately filled up by the waves. The Pyrenees were thus separated from France by a broad arm of the sea, which extended to the west from Biarritz to La Gironde, and to the east from Carcassonne to the mouth of the Rhone. Tertiary strata were suc- cessively deposited in this basin, and many distin- guished geologists, guided principally by the study of the fossils of the district, have referred the neigh- bourhood of Biarritz from the Chambre d'Amour to upheaval. M. de Beaumont admits that the Alps, such as we see them in the present day, have been as it were modelled by at least five upheavals, and the Vosges by as many as twelve. According to M. Durocher we find in the Pyrenees superposed traces of seven successive cataclysms. Often, in a somewhat limited space, different systems of mountains, differing in age and direction, appear to have been accumulated, as it were at will. Thus MM. Boblaye and Virlet recognised in the More a as many as nine distinct upheavals. Article SYSTEMES DE MONTACNES. THE BAY OF BISCAY. 151 the Mill of Sopite to these formations. In accord- ance with this view, the Pyrenees must have been upheaved subsequently to the formation of these strata ; and consequently they would be more recent than has generally been supposed.* A special circumstance complicates the question and renders its solution still more difficult. Very long after the appearance of the Pyrenees, and after the deposition of the tertiary strata, a new cataclysm occurred which convulsed the whole region, changing the primary inclination of the strata, and occasion- ally modifying their relations to one another. Ser- pentine, a kind of porphyritic rock, penetrated through all the preceding formations, and gave rise at several points to centres of partial upheaval. M. Dufrenoy had drawn attention to this remarkable fact, and he made a sketch of one of these masses of serpentine surrounded by gypsum, which had exerted an upheaving action on the cliffs lying between Biarritz and Bidar.f I did not fail to visit this remarkable locality; but twenty years had passed since M. Dufrenoy had made the sketch which accompanies his memoir, and the aspect of the district had been strangely changed since that time. The gypsum had almost entirely * Among those geologists who have maintained this opinion, -we must especially mention M. d'Archiac, who amongst other works has published a very important memoir on the fossils of Biarritz (Mcmoires de la Societe geoloyique de France, 1846), and M. Alcide d'Orbigny, a geologist who has most strenuously maintained the principle of the characterisation of strata by fossils. f Mcmoires pour servir a une description geologique de la France, by MM. Dufrenoy and Elie de Beaumont, t ii. pi. 7. L 4 152 RAMBLES OF A NATURALIST. disappeared under the incessant action of the waves, and the cliffs had retreated at least 150 feet farther inland. The serpentine, from its extreme hardness, had alone been able to resist this continued action of the waters, and it now stood forth in the midst of the beach as an evidence of the destructive power of the waves. M. de Collegno, who had made his obser- vations long before my visit, estimates the annual encroachment of the sea to be about ten feet.* This fact, which is observable in a more or less marked degree along the whole length of the coast, depends upon the very nature and structure of the rocks. The cliffs here are generally formed of a marly or sandy limestone, which becomes disintegrated under the action of atmospheric agents. It is almost everywhere divided into laminae, which are occasion- ally separated by layers of clay. This earth on being carried away by the waters becomes changed into a sort of foliaceous crust, which yields to the slightest shock of the waves ; and, indeed, from the Chambre d'Amour as far as the bay of Saint-Jean- de-Luz the whole line of the shore affords ample proof of a gradual and progressive disintegration. On every side deep crevices, crumbling earth, and * Bulletin de la Societe geologique de France, 1839. M. de Collegno, being implicated in the political troubles of Piedmont, was obliged to leave his country. He learned, however, to seek consolation for the pains of exile in the pursuits of science, and during his residence in France he was appointed professor in the Faculty of Sciences at Bordeaux. Having been subsequently recalled to his native country, he continued to take an active and earnest part in politics, and he even returned to Paris as the representative of the country from which he had once been banished. THE BAY OF BISCAY. 153 recently fractured rocks, meet the eye. Science alone can profit by a state of things which threatens the future stability of these districts. The rent and fractured sides of the cliffs bring to view innumerable fossils, the remains of those animal and vegetable races which once peopled these ancient seas, and every storm prepares a new harvest for the naturalist. In order to avail myself of this opportunity, I lost no time in providing myself with a geologist's hammer and a quarryman's chisel, and thus equipped, I was enabled, under the direction of the expe- rienced guide * who accompanied me on my explora- tions, to make a large collection of fossils in the course of a very few days. Biarritz, therefore, presents sufficient attractions for the tourist and the geologist, but it is not equally favourable to the pursuits of the zoologist. The rocks of la Pointe, which are isolated between two long tracts of sandy beach incessantly worn by the waves, afford a very precarious and limited retreat to marine animals. Indeed, some small Molluscs, now and then an Annelid, and a few of the commonest Zoophytes are the sole representa- tives of their fauna. I saw, therefore, that it would be mere loss of time to remain longer at this station, and after consulting M. Beautemps-Beaupre's Atlas, I determined to fix my quarters at the little village of Guettary, which is situated about six miles from the town of Saint-Jean-de-Luz. Guettary, which is a true type of a Basque vil- * M. Darrac of Bayonne, who is well known to all naturalists who have visited this part of France. 154 RAMBLES OF A NATURALIST. lage, consists of a church, round which are grouped ten or a dozen white houses furnished with red or green blinds, and perhaps some fifty similar habi- tations scattered over a space of about two square miles, and enclosing within its limits several low hills and small valleys, dotted over with clumps of trees, and corn, and maize fields, which are every- where intersected by narrow paths, shaded by haw- thorn and wild plum trees. The cliffs, which are broken by a sort of platform at about the elevation of one of the principal groups of houses, sinks in a rapid slope towards a small sandy harbour, which is protected by two long ledges of rocks, which extend on either side of it like natural jetties. On this account Guettary is also well adapted for bathing, and the cheapness of provisions, and the quiet and isolation of the village, attract to it many of those who dread being involved in the luxurious habits of Biarritz, and who visit the sea rather for purposes of health than pleasure. The primitive simplicity and customs of the olden times still prevail at Guettary, where the bathing is carried on in the most social and familiar manner. The beach, which is exposed to the sea, receives the full force of the waves, which often roll in with considerable violence. For the sake of making a better stand against the onset of the breakers as they dash against the shore, it is customary for the lady bathers, both young and old? to advance hand in hand into the water ; and it is truly a pleasant sight to watch the sort of joyous anxiety with which they await the arrival of the waves, each one springing aside to avoid the ad- THE BAY OF BISCAY. 155 vancing mass of waters, although occasionally dis- appearing almost entirely under some high wave. There is not, however, the slightest cause of alarm on these occasions, nor is any real danger to the fair bathers to be apprehended, for a master diver, an old sailor, who has been bronzed by exposure to the sun and winds in every climate, is always present to watch over the general safety, and to afford as- sistance in case of need. There is, however, no instance on record of any bather having been drowned at Guettary, and there is no doubt that bathing in this manner in the open sea must be doubly effi- cacious from the amount of exercise which it neces- sitates. All the men of Guettary are sailors, or, at all events, lead a seafaring life. The greater number of them generally ship themselves on board vessels bound for Newfoundland, and after the season they return to their homes with a sum of money varying from 800 to 1,500 francs each. The others are en- gaged in fishing, more especially in the tunny fishery; but this is not conducted here in the same manner as in the Mediterranean, for the abysses, rocks, and tempests of the Bay of Biscay do not allow of the establishment of madrayuas. The fish too is different in the two seas. The tunny of the Mediterranean may be known by its short pectoral fins, but the species which is caught at Guettary has very long fins, and is, moreover, of much smaller size, although its flesh is more delicate, and hence it is most esteemed in a commercial point 156 RAMBLES OF A NATURALIST. of view.* The fishermen, who pursue the tunny to a distance of from sixty to ninety miles off the shore, use long handlines baited with a piece of canvas roughly painted so as to resemble a sardine. It requires all the proverbial intrepidity of the Basque sailor to venture out to such great distances in small undecked boats, and that upon a sea which is sur- rounded on every side by this formidable iron-bound coast, which is certain destruction to every ship that strikes upon it; but when the fishing is good the profits are very considerable. I have seen one of these boats return to Guettary loaded with more than eighty tunnies, weighing on an average more than thirty pounds each. In their cruise of two days, the crew, consisting of five men and a boy, had gained more than 1,000 francs. The Newfoundland trade together with the Tunny and Sardine fisheries (the latter of which is more especially practised by the fishermen of the Socoa) is quite sufficient to diffuse plenty, and even riches, among the population of this coast. My landlord at Guettary was a striking instance of what may be done here by order and economy. At the age of twenty, Cazavan was a common sailor, poor, and with no prospect of ad- vancement. He thgn married a woman as poor as himself, and immediately afterwards sailed for New- * This difference in the length of the fins joined to several other characteristics has led to the separation into two distinct genera of these two fishes, which we have designated in the text by their ordinary appellation. That which is caught in the Mediter- ranean is the only true Tunny, the Thynnus Mediterraneus of naturalists. The other is the Orcynus da longa. THE BAY OF BISCAY. 157 foundland. At the present day he is a landowner, and one of the first master sailmakers of Bayonne. Unhappily, however, his case is an honourable ex- ception to the general rule, for recklessness and dissipation keep up a constant state of poverty amongst this population, which might so easily attain to a state of competence ; and strangely enough it is to the women more especially that this sad result is to be attributed. Surrounded by sailors, they seem to have adopted their character and manners. The greater number give themselves up to drinking, and when the father or sons return from some distant cruise, there is always a bread or tavern bill to be paid for with their earnings. The little that remains from their wages is soon dissipated in the same manner. It is thus that Guettary, which of itself sends forth more than 200 men to the cod fisheries, and which consequently receives annually from this sole branch of commerce from 200,000 to 250,000 francs in hard money, suffers misery notwithstanding this source of wealth, which would rapidly enrich the neighbouring communities. There is certainly no doubt that the Basques of the plain and of .the moun- tains are very different in this respect from their brothers of the coast, and it is very easy at compara- tively short distances to obtain striking evidences of the moralising influence of agricultural pursuits. To the right of the little harbour of which I have already spoken, extends the sandy beach which con- nects Guettary, Bidar and Biarritz. To the left begin the rocks which run along the base of the cliffs to the very mouth of the Bidassoa, and are un- 158 RAMBLES OF A NATURALIST. covered at every tide. This was the field of my operations, and I certainly found it very hard ground to work upon. The chalk rocks, which have been incessantly broken by the waves, are worn down to the level of high water, forming a sort of irregular causeway, which extends to a width of several hun- dred yards. The strata, which have been bent and twisted in all directions like the leaves of a book that had been purposely crumpled, form a coast line bristling with points and narrow ledges, and inter- sected to a greater extent than I had ever observed with openings and fissures. In the midst of this disorder there was no veo-eta- o tion, and no mud suitable to the abode of marine animals, or adapted to their nourishment. On every side lay pure sand, which was consequently unsuited to animal life, or solid rocks, which showed between their laminae the various creatures which I was anxious to obtain to aid me in my zoological inqui- ries. An ordinary pickaxe would have been of very little use to me here ; but, knowing the nature of the ground, I had provided myself with a very strong spade, tipped with steel and terminated below by a sharp point, and with this instrument I attacked the foliaceous lamina of the compact limestone, which was frequently superposed on quartz. Besides this I had a hammer, and by the help of these tools my flasks and bottles were soon tolerably well filled. However, both here and at Biarritz, no less than at Saint- Jean- de-Luz and at Saint Sebastian, I missed that superabundance of marine animals to which I had been accustomed in iny former excursions. The THE BAY OF BISCAY. 159 coasts of the Channel, which perhaps are exceptional in this respect, had spoiled me for the Bay of Biscay. Guettary then had become my head-quarters for the time being. Sometimes I explored the neighbour- hood, intent on zoological investigations ; at other times I visited the cliffs of Bidar, provided with a large canvas bag, which was very soon filled with vegetable treasures, or with some fossil molluscs or zoophytes, intended for the Museum of the Jardin des Plantes. On several occasions I extended my excursions as far as the fort of the Socoa, which is situated at the southern extremity of Saint-Jean-de- Luz, and, the better to profit by my distant explora- tions, I usually carried with me a double supply of collecting apparatus. On these occasions I was equipped somewhat after the Robinson Crusoe fashion. At my right shoulder hung a bag for fossils ; over my left arm was suspended a long tin box intended to receive large animals. My hammer was passed through a belt somewhat in the fashion of a poignard, whilst my tubes and bottles, whose wide mouths protruded from all my pockets, personated inoffensive cartridge boxes, or very harmless pistols. My double pickaxe with its strong ash handle com- pleted my strange equipment, and no doubt made me appear a most singular object ; indeed the fisher- men and labourers, on seeing me pass, regarded me with a look of the most intense curiosity, whilst more than once I was pursued by the entire juvenile po- pulation of Saint- Jean- de-Luz. This town, which is the last on this frontier of France, has more than one claim to the notice of the 160 RAMBLES OF A NATUKALIST. traveller. Its roadstead, which affords the only safe anchorage along the whole line of coast from the Gironde to the Bidassoa, presents a view which chal- lenges admiration from those who have seen the Gulf of Palermo and the Bay of Naples. All that is lovely or stern in the characteristics of Basque scenery is concentrated in this view. From the summit of Point Saint Barbara, whose batteries, which are now in ruins, formerly exchanged fire with those of Fort Socoa, the eye in turning towards the south, encounters a line of rounded hills, irre- gularly interspersed with trees and small white- washed cottages. To the east, the bay expands into a semicircle, margined at its base by the houses of Saint-Jean-de-Luz, which, seen from a distance, has all the appearance of a large town. A narrow opening, contracted between two granite dykes, marks the entrance of the harbour and the mouth of the Nivelle. Beyond, this little river flows through a charming valley, which is overhung by the abrupt declivities and barren summit of the Rune ; to the west, the bay curves into a crescent, and gliding below a triple series of hills terminates at the large grey tower of the Socoa. On every side, the Pyrenees exhibit their deep gorges and rugged rocks, whose outlines are softened by distance, their picturesquely indented summits gradually va- nishing in the direction of the coasts of Spain, until they are lost in the horizon, amid the double azure of the sea and sky. Saint- Jean-de-Luz contains now only about 2,000 inhabitants, but in its days of prosperity it numbered THE BAY OF BISCAY, 161 a population of fully 10,000. Its seamen had for a long time no rivals in the whale and cod fisheries ; and, as late as the middle of the last century, it enjoyed a state of the greatest commercial pros- perity. Louis XIV. and the Spanish Infanta re- ceived the nuptial benediction in the principal church of Saint-Jean-de-Luz, and this event is still referred to with considerable pride by the inha- bitants. Elated at the honour of having lodged the king within their walls*, whilst his suite and equipages remained at Bayonne, they contemptuously designate this latter town as the stables of Saint- Jean-de-Luz. This, however, must be but a mourn- ful source of consolation ; for the real struggle, which once existed between these two towns, has for many years past been a mere tradition, and Ba- yonne has nothing now to fear from her old rival. The ocean even seems to have taken part with her, and every year this formidable auxiliary is carrying away, piece by piece, some fragment of Saint- Jean-de-Luz. This is no exaggeration, for I simply express a fact which is but too evident. If you go to the rocks which form the left bank of the mouth of the Ni- velle, you will everywhere see traces of foundations and a few fragments of broken walls ; yet this was once one of the ancient quarters of the town. If you proceed along the sandy beach at the foot of the bay, you will find at fifty feet or more in advance * The inhabitants of the district always speak of this event as if it were an occurrence of a very recent date. They never refer to this king as Louis XIV., but they always speak of him as le roi, VOL. II. M 162 RAMBLES OF A NATUEALIST. of the present pier a circle of mason work, which is the only trace now existing of a well wrhich in 1820 watered the gardens which lay at the back of a street of which not a vestige now remains. If you return to the town, you will find, behind the mole which is intended to protect it, uninhabited houses, falling in and crumbling to pieces in consequence of neglect. This state of things is owing to the long and cruel experience which has taught the inha- bitants that all means of defence against the enemy which is thundering at their gates are alike una- vailing, and that the wisest and safest plan is to retreat before its advances. Saint- Jean-de-Luz formerly possessed natural dykes of its own. The entrance of the bay was narrower, and while a ledge of rocks served the purpose of a breakwater, the mouth of the Nivelle was as it were embanked between the mountain of Bordagain and a high tract of sandy dunes. Towards the seventeenth century, the Points of Socoa and of Saint Barbara yielded little by little, the plateau of Arta sank more and more, and the waves, which were then able to reach the beach without any serious obstacle, began to wear it away. A wall was now constructed to stop their further advance, but the sea encroached daily more and more upon the land, and on the 22nd of February, 1749, a tempest carried away this first dyke, together with several houses. Since this time the most skilful engineers have vainly attempted to struggle against the fatality which seems to be impending over Saint- Jean-de-Luz. Works which to all appearance were of the most THE BAY OF BISCAY. 163 solid kind have been thrown down, and their complete destruction by the storms of 1822 appears definitely to prove the inutility of all further attempts. In the hope of opposing the advance of the waves, M. de Baudres improved upon the works of his predecessors, and in the additions which he made to the former embankments he appears to have exhausted all the resources of engineering art. A dyke of earthwork was erected on the embankments formed by the sea itself, and strengthened in the interior by massive sup- ports of masonry. With a view of offering the greatest opposition to the force of the waves, its exterior was covered by a steeply inclined wall of a yard in thick- ness, composed of large blocks of freestone. Enormous masses of rock bound down by three tiers of deeply sunken piles protected the base of the dyke, and yet in the course of a few days the piles were all torn up, the pieces of rock washed away, and the whole so entirely destroyed, that after the tempest there remained not a single vestige of the embankment for a length of more than 140 yards.* The ocean had passed its levelling touch over the whole of the ruins which it had made, and entombed them in a bed of sand. A new pier has now replaced those which the sea had destroyed, but we scarcely dare to hope that it will be able to afford better resistance than its predeces- sors. The sand has already begun to accumulate at its base, and with every storm of wind the waves pass over it, and break into the town, carrying masses of sand and gravel with them through the streets. * Nouveau Cours clementaire de Geologic, by M. J.-J.-N. Huot. M 2 164 KAMBLES OF A NATUKALIST. To save Saint- Jean-de-Luz by any direct means of defence would, therefore, appear to be impossible, and experience seems to show that a more successful result would hardly be attained by attempting to defend it by a line of advanced works. Vauban pro- posed to close the bay by means of two moles which, resting upon the rocks of Saint Barbara and Point Socoa, would have left only a very narrow passage between them. Towards the end of the last century an attempt seems to have been made to put this plan into execution, but after several fruitless trials it was found necessary to relinquish the project. The dyke of Saint Barbara, which had been advanced about two hundred yards, is now entirely abandoned, while that of the Socoa has been adapted to a wholly local purpose, and now merely serves to protect the fort with a small harbour adjoining it. Thus Saint-Jean- de-Luz, or at least all the portion of the town which separates the bay from the harbour, is irretrievably doomed to destruction. Such was already the opinion of Napoleon when he visited the town, and far from thinking it expedient to pursue this struggle with the ocean, he rather wished to yield to it at certain points in order the better at others to avail himself of its power. Ac- cording to the plans which were drawn up under his own immediate direction, the town was to be destroyed as far inland as the church, by which a free passage would be opened to the sea in the direction of the low and shallow land, through which the Nivelle takes its course. A harbour dug out behind the mountain of Siboure would have afforded safe shelter THE BAY OF BISCAY. 165 to shipping, and, finally, for nothing checked this genius who delighted in colossal schemes, the Adour was to have been diverted from its present bed, and its waters turned into the new roadstead, which would thus have been kept free from sand. It re- mains for engineers to determine whether so desirable a project, which would have afforded to our coasts a harbour of refuge, which they so greatly need, is practicable and deserves to be put into execution. One cannot contemplate the devastation which has been caused by the sea along the whole line of this coast, and more especially at Saint-Jean-de-Luz, without inquiring to what special cause we must at- tribute this destructive action of the ocean. A very simple experiment will suffice to solve this problem. If we take an inverted funnel and plunge it rapidly into a vessel filled with water, taking care not to submerge the mouth, we shall perceive at every movement the liquid will rise within the funnel very much above the external level, darting upwards in a jet thro ugh the orifice. If the funnel remain motion- less, and we let the vessel of water be rapidly moved from below upwards, a precisely similar result will be brought about. The Bay of Biscay, which is formed by the union of the coasts of France and Spain, which intersect one another almost at right angles, forms a sort of gigantic funnel whose base opens towards the north- west. Besides this, the coast dips into the sea on almost every part of the bay below slopes which become more and more steep in proportion as we advance towards the bottom of the bay, whilst the M 3 166 KAMBLES OF A NATUEALIST. depth of the water at a short distance from the shore increases in a similar proportion. Thus the waves, urged by the north-west wind, traverse the whole of the Atlantic as far as the entrance to the Bay of Biscay without having encountered any ob- stacle to their course. But being now compressed between coasts, which gradually approximate more and more closely to one another, they exhibit on a large scale the same phenomenon as the water in the funnel, and flow towards the bottom with a con- stantly increasing velocity. It is only at short dis- tances from the shore that the deep waves striking against the submarine escarpments tend to shoot upwards in an eddying current, like those which we observe to be formed at the water's level along our dykes ; but having been stopped and turned aside by the strata of water which cover them, these ascend- ing currents become changed into a ground swell, which moves with frightful rapidity and strikes against the shore with an irresistible force. During the storm of 1822 the waves which were dashed from the rocks of Arta had a breadth of more than 400 yards, and moved at the rate of twenty yards a second. Their progress was therefore nearly twice as rapid as that of a locomotive which is going at the rate of thirty miles an hour. According to Colonel Emy, the ground swell plays a very considerable part in the greater number of the remarkable phenomena exhibited by the ocean.* * Du mouvement des ondes et des travaux hydrauliques maritimes, by Colonel Emy. M. de Caligny, who is well known in the scientific world for his able experiments on hydraulics, has opposed THE BAY OF BISCAY. 167 It occurs in all seas, but the disposition of the coast- line influences its intensity. It is by this ground swell and not by the superficial waves that boulders, pebbles, sand, and all submerged objects are thrown on the shore, and this is also the cause of those breakers occurring above submarine shoals, which are so much dreaded by sailors, and which render many channels impracticable even during the calmest weather, as we see amongst other places at the entrance to the bay of Saint-Jean-de-Luz. To the same kind of ground swell we must also ascribe that O perpetual tempest which seems to prevail at the bar of the Adour, and at several other points of this coast. Colonel Emy also refers to it the singular phenomenon which I have observed on a small scale in the river of St. Sebastian, but which is much more fully developed in almost all large rivers. It is known to the English by the name of the bore, to the bargemen of the Seine as la barre, to those of the Dordogne as le mascaret, and to the boatmen of the Amazon as la pororoca. At the mouth of the latter river, during spring tides at the periods of new and full moon, the sea, instead of continuing to rise for six hours, attains its greatest elevation in the theory of Colonel Emy in relation to the formation of the ground swell, and he regards it as owing to the action of waves, which are formed not by simple undulations, but by a real transportation of liquid. All the effects attributed to the ground swell are ascribed by him to the back stroke. The views which we have here expressed correspond very nearly with those of M. de Caligny, although we agree with Colonel Emy in attributing a very decided influence to submarine rocks in the formation of the ground swell. U 4 168 KAMBLES OP A NATURALIST. the course of two or three minutes. A wave of twelve or fifteen feet in height extends across the entire breadth of the river. This is very soon fol- lowed by two or three similar waves, all of which ascend the stream with a terrific noise, and with such rapidity that they destroy every thing that opposes their passage, uprooting trees and carrying away vast tracts of land. The pororoca extends its in- fluence sometimes as far as 600 miles inland. In the open sea, the ground swell is not the less power- ful where it encounters sharp and perpendicular rocks in its passage. These ground waves have often been known to dart their eddying lines of water to the very top of Lot's Wife ; a rock which is situ- ated in the Archipelago of the Philippines, and which rises to an elevation of more than 360 feet. Colonel Emy asserts that these waves act at a depth of 130 yards, and that they will raise above the level of the sea columns of water more than 50 yards in height, of 2,000 or 3,000 cubic yards in bulk, and weighing from 2,000 to 3,000 tons. With such figures as these before us, we can no longer feel surprised at the ravages which these waves have committed at Saint- Jean-de-Luz, and we may now more readily believe in the possibility of blocks of stone which weighed four tons, and formed part of the masonry of the pier, having been uplifted and carried to the top of the dyke. It is also in a great measure to this ground swell that we must attribute the relative poverty of the coasts of Guettary, Saint-Jean-de-Luz, and Saint Sebastian in respect to marine animals. These THE BAY OF BISCAY. 1G9 laminated rocks are so constantly penetrated by the waves to their very innermost fissures and indenta- tions that they cannot nourish a very numerous population ; but as the animals which live in these recesses belong to a warmer sea than the Channel, they were to a certain extent new to me, and on this account they were the more highly valued. It must, moreover, be remembered that in the present state of science no real interest can attach itself to super- ficial studies embracing a very large number of animals. A single species thoroughly and systema- tically studied will teach more than a hundred that have been cursorily examined. The great matter, however, is to make a judicious choice, and in this respect I was very fortunately situated. At Guettary I found an abundance of those Polyophthalmians which I h#d already studied in Sicily together with the same Hermellas which I had casually seen at Granville. These two types were represented here by species which differed from those with which I was already acquainted. I lost no time in testing my past re- searches by a new and severe revision, while at the same time I entered upon fresh inquiries, and the results of these investigations, of which I shall en- deavour to give some idea, fully recompense me for all my labours. On these coasts, which are so violently beaten by the waves, we often observe small hillocks of sand pierced by an infinite number of minute openings half covered by a thin projecting margin. These mounds are either found behind some large rock or in some deep fissure, although occasionally they are 170 RAMBLES OF A NATURALIST. fixed on an entirely uncovered point. These little hillocks or mounds which look very much like a thick piece of honeycomb are in reality villages or popu- lous cities, in which live in modest seclusion certain tubicolous Annelids, known by the name of Hermel- las — creatures as curious as any that fall under the notice of the naturalist. Their body, which is about two inches in length, is terminated anteriorly by a bifurcated head, bearing a double bright golden- coloured crown of strong, sharp, serrated silken threads.* These brilliant crowns are not mere orna- ments, but, to speak more correctly, are the two sides of a solid door or rather a true portcullis, which her- metically closes the entrance of the habitation, when, at the least alarm of danger, the Annelid darts with the rapidity of lightning within its house of sand. From the edges of the cephalic opening, issue about fifty or sixty light violet-coloured slender filaments, which are incessantly moving about like numerous minute serpents. These are so many arms which can be lengthened or shortened at will, and which seizing the prey as it passes, bring it into the hollow funnel- shaped mouth at the base of the depression. It is by means of these arms that one by one the grains of quartz or hard limestone are collected, and put into their proper places, to serve in the composition of the tubes, the different parts being solidly cemented together by a sort of mortar-like mucosity, which is furnished by the animal itself. On the sides of its * These Setae replace the calcareous or horny operculura, which in the ordinary Tubicula, similarly serves to close the orifice of the tube* TUE BAY OF BISCAY. 171 body appear little projections, from whence issue bundles of sharp and cutting lances or broad fans, serrated like semicircular saws. These are the feet of the Hermella. Finally, the back is furnished with cirrhi, recurved like sickles, and whose colour varies from dark red to grass green ; these organs re- present the branchiae, which, by an exception that has hitherto been found to be unique in this group, are distributed over every ring instead of being united to the head like the petals of a flower. These external characters are in themselves suffi- cient to attract the attention of the naturalist to the Hermellas, and most keenly to excite his curiosity. Their internal organisation is not less remarkable. These singular animals realise in their actual ana- tomical details a theoretical view which might hitherto have been justly regarded as a mere abstract idea. In the Articulata generally, the two sides of the body are similar to one another, so that these animals may be regarded as formed by the reunion of two symmetrical halves, cemented together along the median line, and attempts were long since made to confirm this view by the study of their embryology ; and Newport, one of the most distinguished compa- rative anatomists of England, had shown that in the young Myriapods *, the abdominal nervous centres, the ganglia, are developed in two halves, which become subsequently united. I had made a similar observation in respect to a Eunice sanguinea, which * This class is nearly allied to that of insects, and it includes amongst others the Centipedes and Millipedes. 172 RAMBLES OP A NATURALIST. was in the act of producing the posterior segments of the body, which had been lost by some accident, but no adult animal had hitherto been met with which presented any very apparent traces of this original division. In the Hermella, however, this division exists throughout the greater portion of the body. Throughout the whole length of the abdomen, the muscles, vessels, and nerves are all double, and the two halves are only held together by the skin and by the digestive canal, which is single. Here, then, the Annelid is actually cleft in two; both before and behind all parts of the muscular and vascular appa- ratus meet along the middle of the body, but the ventral nervous system remains divided from the one extremity to the other, and its two halves only com- municate together by delicate threads or excessively thin bands.* At the period when I made these observations, this division of the nervous system in the Hermellas was regarded as an entirely exceptional mode of arrange- ment ; but in the course of my investigations I found that the Annelids exhibited many other equally re- markable phenomena. This is incontestably the most interesting group to which the zoologist can at the present day devote his attention ; for it appears to be * I would here observe, that in the Articulata the principal nervous centre is situated in the head above the digestive tube. This ganglion is considered as the representative of the brain in the Vertebrata, because it usually furnishes nerves to the organs of the senses. This brain is united by two connecting filaments to the abdominal nervous system, which is placed below the digestive tube, and consists essentially of a chain of nervous centres or ganglia united by other connecting filaments. THE BAY OF BISCAY. 173 more especially distinguished by the infinite varia- bility of characters which in all other cases exhibit the greatest constancy. In the Annelids the organs of motion and of circulation vary in the most marked degree in the different species. The respiratory system is sometimes developed in an almost exagge- rated manner, whilst in other cases it is found to have completely disappeared, and that even in ani- mals which are apparently very nearly allied to one another. The nervous system itself, that system which Cuvier characterised as the entire animal) pre- sents no exception to this common law, for, in a spe- cial memoir on this important question, I have been able to demonstrate that this apparatus exhibits the most singular variations. Thus I found in other Tubicolous Annelids, and even in the Errantia, these abdominal nervous chains cleft into two halves, which were widely separated from each other ; while on the other hand, I found in other species that this same chain formed along the median line merely a narrow and uniformly equal band, in the thickness of which the ganglia seemed as it were embedded ; and between these two extremes I moreover discovered a great number of intermediate .forms. Thus those premature generalisations which have more especially originated from the exclusive study of animals belonging to a fixed type, vanish one by one before an examination which is daily becoming more and more severe ; and thus we learn day by day more thoroughly to appreciate the scientific import- ance of the study of the lower animals. In this respect, botanists are in the same condition as zoologists. In 174 KAMBLES OF A NATURALIST. ohlcr to solve the most difficult problems of their own science, they no longer turn to the oak or the palm- tree for their information, but rather to the Algse and the lower plants. In no other animals does creation exhibit itself so completely in the light of a veritable Proteus as in the Annelids, which are at every moment assuming new forms, and surprising the observer by the mani- festation of the most unexpected modifications. The Polyophthalmians exhibit one of the most curious examples of these metamorphoses ; but here a few historical details become necessary, in order to show the great interest which attaches itself to the study of a small worm which is only a fraction of an inch in length. The splendid discoveries of Ehrenberg revived in 1830 a discussion of originally a much more ancient date. Among naturalists, some, adopting the views of the illustrious Berlin microscopist, maintain that even the smallest animals, those, for instance, which in our scientific classifications are placed in the very lowest position of the zoological scale, present an or- ganisation which is fully as complicated as those of the higher animals. Others, on the contrary, follow- ing the steps of the celebrated founder of the Natur- Philosophie, maintain with Oken that the organisation is simplified in a progressive manner the lower we descend in this scale ; so that entire groups, composed to a certain extent of rudimentary animals, are almost entirely devoid of organisation. The latter class of observers agreed with Reaumur in regarding the Medusae, for example, as nothing more than masses THE BAY OF BISCAY. 175 of living jelly, whilst the Planarias and the greater number of Intestinal Worms in their estimation con- sist of little else than Parenchyma. In their eyes, this simplification of the organisms was carried to such an extent that whole classes of animals were regarded as altogether devoid of a nervous system. In France and Germany, these opposite doctrines were attacked and supported with much heat and asperity. The discussion was commenced without a clear understanding on either side as to what is to be understood by the expression inferior animals ! and consequently it soon led to much exaggeration and error. Various works published during the last few years present the subject in its true aspect. Many points of detail undoubtedly still need elucidation, but it may be stated generally, that wherever we study even the lowest animals with care and exact- ness, the results of our investigations will show us that even in their case a very decided organic com- plication is apparent. The advocates of organic sim- plicity are daily losing ground, and at present they are unable to defend themselves except by having recourse to the negative results yielded by the Infu- soria ; that is to say, by beings whose excessive minuteness places the majority beyond our means of investigation. Amongst the most warmly discussed points of fact or theory in this quarrel, we must place that of the existence of distinct organs of the senses, and more especially of eyes, in a great number of animals which belong to the three divisions of the Mollusca, Articulata, and Radiata, 176 RAMBLES OF A NATURALIST. Ehrenberg had regarded as organs of vision certain coloured points which are met with in the margin of the umbrella in the Medusae, at the extremities of the rays in the Star-fishes, in the head among the Annelids, Planarias, Rotifers, &c., and at one of the extremities of the body in certain of the Infu- soria. The accuracy of most of these statements was denied in the most positive manner, although often very unjustly. In proportion as these creatures have been more profoundly studied, it has been found, in the case of those animals whose size rendered them accessible to our methods of examination, that the greater number actually possessed true organs of vision. The most abundant evidence on this point has been contributed by naturalists of every Euro- pean nation. The Annelids more especially furnished me with a very striking example of this fact. One of the species, which lives in the Sicilian seas, possesses eyes which are almost as complete as those of a fish. I have succeeded in enucleating the crystalline lens, and in examining it separately ; and I found that when it was placed upon a piece of thin glass which received the parallel rays transmitted to it by a plane mirror, it formed perfectly achromatic images. These images repeated and magnified by the microscope enabled me to distinguish with perfect clearness the very smallest details of the neighbouring coast, and by means of the crystalline lens of an Annelid my microscope was thus converted into a telescope. The opposition which Ehrenberg met with was even more strongly marked when he announced that THE BAY OF BISCAY. 177 he had discovered an Annelid, the Amphicora, which carried at the end of its tail two eyes, which were perfectly similar to those which were upon its head. How, it was asked, were we to admit such a trans- position of the senses ? how was it to be supposed that eyes could exist at so great a distance from the brain, and without having any probable connection with it? The question was thus made a general one, and consequently acquired a very high degree of physiological importance. It was no longer suffi- cient to ascertain whether eyes did or did not exist, but it was now further necessary to decide if any one portion of the nervous system, excepting the brain, could become the seat of sensorial perception. If by the word eye we must understand an Organ which is always the same, and everywhere similar to that which we find in Man or Birds, Annelids, Ne- mertes, Planarias, and Medusas are certainly blind animals, but, like every organic apparatus, the visual organ may be simplified and degraded, without, on that account, changing its nature. Even in this state of degradation it maintains its fundamental parts, and these parts are generally easy of recognition. Although destined to fulfil an entirely physiological function, the eye is a true physical apparatus. It always consists of a camera obscura, in which a con- verging lens concentrates the light, and throws the image of external objects on a screen which is placed in its focus. But here the lens instead of being formed of inert matter is organised, and is known as the crystalline lens. The screen is also living, and bears the name of the retina, and it is through the VOL. n. N 178 RAMBLES OF A NATURALIST. latter that the impression received from images is transmitted to the brain. However varied may be the degree of complication in an eye, its fundamental parts always consist of a crystalline lens and a retina. We are therefore on the other hand bound to consi- der as a true eye every organ which possesses these characteristic elements ; for it could not fulfil any other functions but those of which we have spoken. To decide this general question advanced by Ehren- berg, and to ascertain whether in fact the visual organ can be thus transposed, or, in other words, whether it can exist elsewhere than in the head, we must necessarily find in the Amphicora, or in every other animal presenting analogous facts, the crystal- line lens and retina of the eyes.* In this respect my investigations continued for a long time to be unsuccessful. On the coasts of the Channel and of Sicily, I had found many Annelids allied to the Amphicora, and bearing on the posterior extremity of their bodies the coloured points in question. In some of the species that I had disco- vered, these coloured points were moreover strangely multiplied. There were several of them on the head, four at the extremity of the tail, and two on each ring of the body. This multiplication seemed to me to present in itself a very serious objection to the views of Ehrenberg. How was it possible to believe in such a profusion of visual organs ? Yet the study of the living animals seemed to confirm this determi- nation. I saw the tail fulfilling all the functions of * The term crystalline lens is here used to express generally the whole refractive apparatus of the eye. THE BAY OF BISCAY. 179 the head, and this with evident proofs of spontaneity and intelligence. In moving, the tail went first, explored the objects without touching them, and turned aside from obstacles that lay in its path ; in a word, it acted as if it were the seat of distinct vision, and as if it were directed by a clear will. Neverthe- less, notwithstanding the many hours which I devoted to these observations, I was unable to discover either a crystalline lens or a retina ; and hence my convic- tion in reference to so delicate a question as this could not be conclusive. At length, among the Coralline?, those small Algse which cover the rocks with their closely com- pressed tufts as the moss mantles over the stone, I discovered the Polyophthalmians (Polyophthtdmia). Here there was no longer any room for doubt; the fable of Argus was realised before me on the most incontestible evidence. Imagine to yourself a nearly cylindrical little worm, of a golden yellow, about an inch in length, and armed with two rows of seta?, whose length increased from before backwards, and you may perhaps form some idea of the aspect pre- sented by the Polyophthalmians in a state of repose. In the sand where it passes its life this animal moves with incredible rapidity, by means of the general contractions of its body and the setaB which serve it in place of feet, but as soon as it wishes to swim freely in the water, or merely to place itself in such a manner that the little animals with which it is nourished may be within reach of its mouth, two large ciliated structures, which are placed on N 2 180 RAMBLES OP A NATURALIST. the sides of its head, are protruded and act like the two paddle-wheels of a steam-boat. With the view of directing its course, the Poly- ophthalmian is provided on its head with three eyes, each of which is furnished with two or three volu- minous crystalline lenses, very easy of recognition. Besides this, on each side of the rings of its body there appears on either side a red point, very similar to those of certain of the Amphicorae. On dissection, we find that each of these points receives a large nerve issuing from the ganglion or ventral nervous centre corresponding to it. By the help of the microscope, we can see that this nerve penetrates into a mass of pigment, which encloses a spherical crystalline lens, and we now see that the textures lying before it have undergone a modification by which they are rendered more completely and equa- bly transparent. In a word, we can no longer doubt that these red points, which are placed on the sides and along the whole length of the body, are true eyes, receiving their optic nerves from the abdominal nervous centres, and having no direct connection with the brain. This result, however strange it may appear, is not the only one of the kind by which modern science has been enriched. The Mollusca furnish us with several facts of the same nature. Most of our readers are no doubt acquainted with the Pecten, which is com- monly known as St. James's or the pilgrim's shell. The animal which inhabits this shell somewhat re- sembles the oyster, and possesses like the latter a mantle or thin covering of living tissue, which lines THE BAY OF BISCAY. 181 the interior of its habitation. The Pecten, which is as restless as the oyster is sedentary, possesses organs of vision, and these organs are not placed upon the head, nor are they connected with a brain, but they occupy the margins of the mantle, and derive their optic nerves from the great ventral ganglion. These very curious facts were published more than ten years ago in Germany.* I have been able to verify these observations at different times, and I have detected in these eyes in the mantle of a Mol- lusc almost all the parts which are present in the eyes of a Mammal, including even the eyelashes and eyebrows, which are here represented by fleshy cirrhi which surround and protect the delicate organ of vision. Three German naturalists, Grube f , Krohn, and Will, have extended these researches to other genera of Acephalous Molluscs, and they have detected a similar organisation in the Spondyli, Tellings, Pinnae, Arcae, Pectunculi, &c. In the pre- sence of such precise and abundant evidence, our observations on the Polyophthalmians lose their apparent improbability. Indeed, the multiplication of eyes, their lateral position, and their relations with other nervous centres than the brain, are per- haps less singular in this little Annelid than in the Molluscs of which we have just spoken. Indeed, as in the case of all animals belonging to * The existence of these eyes appears to have been long known; but no detailed anatomical description of them was published until 1840. f Grube, a professor at Dorpat, has devoted himself, with much success, to the history of the Annelids. He has published several zoological and anatomical memoirs on this subject, K 3 182 RAMBLES OF A NATURALIST. the group of Annelids, the body of the Polyoph- thalmians is formed of a series of rings, joined toge- ther piece by piece, and presenting very great resem- blance to one another. In the largest Annelids one may easily convince oneself of the slightness of the connection which exists between these rings. A certain number of them may even be killed or affected by gangrene, while the others, and more es- pecially those which precede them, do not appear to suffer in any way. Each of them is to a certain extent a complete animal, having as it were its own life, while the entire body may be considered as a kind of colony, of which the head would be the chief, or rather the guide. This is the portion which usually possesses organs of the senses. On cutting it off, the body can undoubtedly no longer see, and it also becomes deprived of organs of touch, but as far as we can judge, it still experiences tolerably precise sensations, and manifests a will. Thus, for instance, severed portions of the Eunice evidently avoid the light and bury themselves in the mud by a succession of movements which exhibit no appear- ance of confusion. What, then, can be wanting to these severed seg- ments, to these isolated rings, to render them so many complete animals? Assuredly, they can only need organs of sensation generally, and more particularly organs of sight. Now we find that both the Amphicorge and the Polyophthalmia are Anne- lids, in which each ring, by receiving these organs, and consequently by presenting so much the greater resemblance to the head, most completely realises one THE BAY OF BISCAY. 183 of the most characteristic tendencies of the group. Considered in this respect, they are only Annelids which possess a greater degree of perfection than the others. This remarkable independence of the different parts of the body of the same animal, and the strange diffusion of the faculties of perception and of a reasoning will through all parts of the nervous sys- tem, are not exclusively exhibited by the Annelids. The same thing is to be met with in insects, animals whose organic complication exceeds in many respects even that of man himself.* The experiments of Duges leave no doubt on this point. If you imitate this skilful and lamented na- turalist, and if you successively remove from a Praying Mantis the head and the posterior part of the body, the prothorax which remains will live for more than an hour, although it now only contains a single ganglion. If you attempt to seize it, you will find that the aggressive feet of the animal will be directed towards your fingers, into which it will bury the powerful hooks with which they are armed. The abdominal ganglion, which alone animates the ring, has therefore /