?« i/&me - jj tf* n ^ijW, ViUCgS ^ C^ Hr* flUQfc . ^ . Jf Tubh.ihcsJ, by Jfcnru J'isht'r. baxton. Zerufan. Jan. 2S2H . > ,4 • I # A HISTORY OF THE EARTH, AND ANIMATED NATURE. IN FOUR VOLUMES. • * BY OLIVER GOLDSMITH. VOL. I. Hontwn : PKINTED BY HENRY FISHER, AT THE CAXTON-PRESS J (Printer in Ordinary to His Majesty.) Published at 38, Newgate-street : Sold by all Booksellers. V ' V ! *r'-- , --<*■ 'L 1 # : ? v, r -- •• ■ -1' -V'v 1 iibi-U t f & !L CONTENTS. VOL. I. PART I. Page CHAP. I. A Sketch of the Universe 9 CHAP. II. A short survey of the Globe, from the light of Astronomy, and Geography 13 CHAP. III. A view of the surface of the Earth. 17 CHAP. IV. A review of the different Theories of the Earth 20 CHAP. V. Fossil-shells and other extraneous Fossils 30 CHAP. VI. The internal structure of the Earth 36 CHAP. VII. Caves and Subterraneous Passages that sink, but not perpendicularly, into the Earth 42 CHAP. VIII. Mines, Damps, and Mineral Vapours 48 CHAP. IX. Volcanoes and Earthquakes 56 CHAP. X. Earthquakes 65 CHAP. XI. The appearance of Islands and Tracts; and of the disappearing of others 76 CHAP. XII. Mountains 82 CHAP. XIII. Water 97 CHAP. XIV. The origin of Rivers 114 CHAP. XV. The Ocean in general ; and of its Saltness 133 CHAP. XVI. The Tides, Motion, and Currents, of the Sea ; with their effects. . . . 145 CHAP. XVII. The changes produced by the Sea upon the Earth 156 CHAP. XVIII. A summary account of the mechanical properties of Air 173 CHAP. XIX. An Essay towards a natural history of the Air 180 CHAP. XX. Winds regular and irregular 194 CHAP . XXI. Meteors, and such appearances as result from a combination of the Elements 211 CHAP. XXII. The Conclusion, 228 IV CONTENTS. PART II. ANIMALS. Page CHAP. I. A comparison of Animals with the inferior ranks of Creation 231 CHAP. II. The generation of Animals 233 CHAP. III. The infancy of Man 253 CHAP. IV. Puberty 268 CHAP. V. The age of Manhood 273 CHAP. VI. Sleep and Hunger 297 CHAP. VII. Seeing 309 CHAP. VIII. Hearing 318 CHAP. IX. Smelling, Feeling, and Tasting 327 CHAP. X. Old Age and Death 335 CHAP. XI. The Varieties in the Human Race 345 CHAP. XII. Monsters 362 CHAP. XIII. Mummies, Wax-works, &c. 375 CHAP. XIV. Animals 386 CHAP. XV. Quadrupeds in general, compared to Man 398 * -*• PREFACE. NATURAL History, considered in its utmost extent, com- prehends two objects. First, that of discovering, ascertain- ing, and naming, all the various productions of Nature. Secondly, that of describing the properties, manners, and relations, which they bear to us, and to each other. The first, which is the most difficult part of this science, is systematical, dry, mechanical, and incomplete. The second is more amusing, exhibits new pictures to the imagination, and improves our relish for existence, by widening the pros- pect of nature around us. Both, however, are necessary to those who would un- derstand this pleasing science in its utmost extent. The first care of every inquirer, no doubt, should be, to see, to visit, and examine, every object, before he pretends to inspect its habitudes or its history. From seeing and observing the thing itself, he is most naturally led to spe- culate upon its uses, its delights, or its inconveniencies. Numberless obstructions, however, are found in this part of his pursuit that frustrate his diligence and retard his curiosity. The objects in nature are so many, and even those of the same kind are exhibited in such a variety of forms, that the inquirer finds himself lost in the exuberance before him, and, like a man who attempts to count the stars, unassisted by art, his powers are all distracted in barren superfluity. ' vol. i. — 83-84. b vi PREFACE. To remedy this embarrassment, artificial systems have been devised, which grouping into masses those parts of nature more nearly resembling each other, refer the in- quirer for the name of the single object he desires to know, to some one of those general distributions, where it is to be found by further examination. If, for instance, a man should in his walks meet with an animal, the name, and consequently the history, of which he desires to know, he is taught by systematic writers of natural history to examine its most obvious qualities, whether a quadruped, a bird, a fish, or an insect. Having determined it, for explanation sake, to be an insect, he ex- amines whether it has wings ; if he finds it possessed of these, he is taught to examine whether it has two or four ; if possessed of four, he is taught to observe, whether the two upper wings are of a shelly hardness, and serve as cases to those under them ; if he finds the wings composed in this manner, he is then taught to pronounce, that this insect is one of the beetle kind : of the beetle kind, there are three different classes distinguished from each other by their feelers ; he examines the insect before him, and finds that the feelers : are clavated or knobbed at the ends ; of beetles, with feelers thus formed, there are ten kinds ; and among those he is taught to look for the precise name of that which is before him. If, for instance, the knob be divided at the ends, and the belly be streaked with white, it is no other than the Dorr, or the May-bug ; an animal, the noxious qualities of which give it a very distinguished rank in the history of the insect creation. In this manner a system of natural history may, in some measure, be com- pared to a dictionary of words. Both are solely intended to explain the names of tilings ; but with this difference, that in the dictionary of words we are led from the name PREFACE. , • • Vll of the thing to its definition; whereas in the system of natural history, we are led from the definition to find out the name. Such are the efforts of writers, who have composed their works with great labour and ingenuity, to direct the learner in his progress through nature, and to inform him of the name of every animal, plant, or fossil substance, that he happens to meet with : but it would be only deceiving the reader to conceal the truth, which is, that books alone can never teach him this art in perfection : and the solitary student can never succeed. Without a master, and a pre* vious knowledge of many of the objects of nature, his book will only serve to confound and disgust him. Few of the individual plants or animals, that he may happen to meet with, are in that precise state of health, or that exact period of vegetation, from whence their descriptions were taken. Perhaps he meets the plant only with leaves, but the systematic writer has described it in flower. Perhaps he meets the bird before it has moulted its first feathers while the systematic description was made in its state of full perfection; He thus ranges without an instructor, confused, and with sickening curiosity, from subject to subject, till at last he gives up the pursuit, in the multi- plicity of his disappointments. Some practice, therefore, much instruction, and diligent reading, are requisite to make a ready and expert natu- ralist, who shall be able, even by the help of a system, to find out the name of every object he meets with. But when this tedious, though requisite, part of study is at- tained, nothing but delight and variety attend the rest of his journey. Wherever he travels, like a man in a country where he has many friends, he meets with nothing but PREFACE. IM vm acquaintances and allurements in all the stages of his way. The mere uninformed spectator passes on in gloomy soli- tude ; but the naturalist, in every plant, in every insect, and every pebble, finds something to entertain his curiosity, and excite his speculation. From hence it appears, that a system may be considered as a dictionary in the study of nature. The ancients, how- ever, who have written most delightfully on this subject, seem entirely to have rejected those humble and mecha- nical helps to science. They contented themselves with seizing upon the great outlines of history, and passing over what was common, as not worth the detail ; they only dwelt upon what was new, great, and surprising, and sometimes even warmed the imagination at the expense of truth. Such of the moderns as revived this science in Europe, undertook the task more methodically, though not in a manner so pleasing. Aldrovandus, Gesner, and Johnson, seemed desirous of uniting the entertaining and rich descriptions of the ancients with the dry and syste- matic arrangement, of which they were the first projectors. This attempt, however, was extremely imperfect, as the great variety of nature was, as yet, but very inadequately known. Nevertheless, by attempting to carry on both ob- jects at once, first directing us to the name of the thing, and then giving the detail of its history, they drew out their works into a tedious and unreasonable length ; and thus mixing incompatible aims, they have left their labours rather to be occasionally consulted, than read with delight, by posterity. The later moderns, with that good sense which they have carried into every other part of science, have taken a different method in cultivating natural history. They have PREFACE. ix been content to give, not only the brevity, but also the dry and disgusting air of a dictionary, to their systems. Ray, Klein, Brisson, and Linnseus, have had only one aim, that of pointing out the object in nature, of discovering its name, and where it was to be found in those authors that treated of it in a more prolix and satisfactory manner. Thus natural history, at present, is carried on in two dis- tinct and separate channels, the one serving to lead us to the thing, the other conveying the history of the thing, as supposing it already known. The following Natural History is written with only such an attention to system as serves to remove the reader’s embarrassments, and allure him to proceed. It can make no pretensions in directing him to the name of every ob- ject he meets with ; that belongs to works of a different kind, and written with very different aims. It will fully answer my design, if the reader, being already possessed of the name of any animal, shall find here a short, though satisfactory, history of its habitudes, its subsistence, its manners, its friendships, and hostilities. My aim has been to carry on just as much method as was sufficient to shorten my descriptions by generalizing them, and never to follow order where the art of writing, which is but another name for good sense, informed me that it would only contribute to the reader’s embarrassment. Still, however, the reader will perceive that I have formed a kind of system in the history of every part of animated nature, directing myself by the great obvious distinctions that she herself seems to have made ; which, though too few to point exactly to the name, are yet sufficient to illu- minate the subject, and remove the reader’s perplexity. Mr. Buffon indeed, who has brought greater talents to this part X PREFACE. of learning than any other man, has almost entirely rejected method in classing quadrupeds. This, with great deference to such a character, appears to me running into the opposite extreme ; and, as some moderns have of late spent much time, great pains, and some learning, all to very little pur- pose, in systematic arrangement, he seems so much dis- gusted by their trifling, but ostentatious efforts, that he describes his animals almost in the order they happen to come before him. This want of method seems to be a fault ; but he can lose little by a criticism which eveiy dull man can make, or by an error in arrangement, from which the dullest are most usually free. In other respects, as far as this able philosopher has gone, I have taken him for my guide. The warmth of his style, and the brilliancy of his imagination, are inimitable. Leav- ing him, therefore, without a rival in these, and only availing myself of his information, I have been content to describe things in my own way ; and though many of the materials are taken from him, yet I have added, retrenched, and altered, as I thought proper. It was my intention at one time, whenever I differed from him, to have men- tioned it at the bottom of the page ; but this occurred so often, that I soon found it would look like envy, and might perhaps convict me of those very errors which I was wanting to lay upon him. I have, therefore, as being every way his debtor, concealed my dissent, where my opinion was different ; but wherever I borrow from him, I take care at the bottom of the page to express my obliga- tions. But though my obligations to this writer are many, they extend to but the smallest part of the work, as he has hitherto completed only the history of quadrupeds. I was, therefore, left to my own reading alone, to make out the history of birds, fishes, and insects, of which the arrange- PREFACE. xi ment was so difficult, and the necessary information so widely diffused, and so obscurely related when found, that it proved by much the most laborious part of the under- taking. Thus having made use of Mr. Buffon’s lights in the first part of the work, I may with some share of confi- dence recommend it to the public. But what shall I say to that part, where I have been entirely left without his assistance ? As I would affect neither modesty nor con- fidence, it will be sufficient to say, that my reading upon this part of the subject has been very extensive ; and that I have taxed my scanty circumstances in procuring books, which are on this subject, of all others, the most expensive. In consequence of this industry, I here offer a work to the public, of a kind which has never been attempted in ours, or any other modern language, that I know of. The ancients, indeed, and Pliny in particular, have anticipated me in the present manner of treating natural history. Like those historians who describe the events of a campaign, they have not condescended to give the private particulars of every individual that formed the army ; they were content with characterizing the generals, and describing their operations, while they left it to meaner hands to carry the muster-roll. I have followed their manner, rejecting the numerous fables which they adopted, and adding the improvements of the moderns, which are so numerous, that they actually make up the bulk of natural history. The delight which I found in reading Pliny, first inspired me with the idea of a work of this nature. Having a taste rather classical than scientific, and having but little employed myself in turning over the dry labours of modern system- makers, my earliest intention was to translate this agreeable writer, and by the help of a commentary to make my work as amusing as I could. Let us dignify natural history never PREFACE. • l Xll so much with the grave appellation of an useful science , yet still we must confess, that it is the occupation of the idle and the speculative, more than of the busy and the ambitious part of mankind. My intention, therefore, was to treat what I then conceived to be an idle subject, in an idle manner ; and not to hedge round plain and simple narratives with hard words, accumulated distinctions, osten- tatious learning, and disquisitions that produced no con- viction. Upon the appearance, however, of Mr. Buffon’s work, I dropped my former plan, and adopted the present, being convinced, by his manner, that the best imitation of the ancients was to write from our own feelings, and to imitate nature. It will be my chief pride, therefore, if this work may be found an innocent amusement for those who have nothing else to employ them, or who require a relaxation from labour. Professed naturalists will, no doubt, find it super- ficial ; and yet I should hope that even these will discover hints and remarks, gleaned from various reading, not wholly trite or elementary. I would wish for their approbation. But my chief ambition is to drag up the obscure and gloomy learning of the cell to open inspection, to strip it from its garb of austerity, and to shew the beauties of that form, which only the industrious and the inquisitive have been hitherto permitted to approach. A HISTORY OF THE EARTH. CHAP. I. A SKETCH OF THE UNIVERSE. The world may be considered as one vast mansion, where man has been admitted to enjoy, to admire, and to be grateful. The first desires of savage nature are merely to gratify the importunities of sensual appetite, and to neglect the contemplation of things, barely satisfied with their enjoyment : the beauties of nature, and all the won- ders of creation, have but little charms for a being taken up in obviating the wants of the day, and anxious for precari- ous subsistence. Philosophers, therefore, who have testified such sur- prise at the want of curiosity in the ignorant, seem not to consider that they are usually employed in making pro- visions of a more important nature ; in providing rather for the necessities than the amusements of life. It is not till our more pressing wants are sufficiently supplied, that we can attend to the calls of curiosity ; so that in every age scientific refinement has been the latest effort of human industry. But human curiosity, though at first slowly excited, be> ing at last possessed of leisure for indulging its propensity becomes one of the greatest amusements of life, and gives higher satisfactions than what even the senses can afford. A man of this disposition turns all nature into a magnifi- cent theatre, replete with objects of wonder and surprise, and fitted up chiefly for his happiness and entertainment : he industriously examines all things, from the minutest insect to the most finished animal ; and, when his limited VOL. i. — 1. B A HISTORY OF 10 organs can no longer make the disquisition, he sends out his imagination upon new inquiries. Nothing, therefore, can be more august and striking than the idea which his reason, aided by his imagination, furnishes of the universe around him. Astronomers tell us, that this earth which we inhabit, forms but a very mi- nute part in that great assemblage of bodies of which the world is composed. It is a million of times less than the sun, by which it is enlightened. The planets also, which, like it, are subordinate to the sun’s influence, exceed the earth a thousand times in magnitude. These, which were at first supposed to wander in the heavens without any fixed path, and that took their name from their apparent devia- tions, have long been found to perform their circuits with great exactness and strict regularity. They have been dis- covered as forming, with our earth, a system of bodies cir- culating round the sun, all obedient to one law, and impelled by one common influence. Modern philosophy has taught us to believe, that, when the great Author of nature began the work of creation, he chose to operate by second causes ; and that, suspending the constant exertion of his power, he endued matter with a quality, by which the universal economy of nature might be continued without his immediate assistance. This quality is called attraction ; a sort of approximating influence, which all bodies, whether terrestrial or celestial, are found to possess ; and which in all increases as the quantity of matter in each increases. The sun, by far the greatest body in our system, is, of consequence, possessed of much the greatest share of this attracting power ; and all the planets, of which our earth is one, are, of course, entirely subject to its superior influence. Were this power, therefore, left uncontrolled by any other, the sun must quickly have attracted all the bodies of our celestial system to itself ; but it is equally counteracted by another power of equal efficacy ; namely, a progressive force, which each planet received when it was impelled forward by the divine Architect, upon its first formation. The heavenly bodies of our system being thus acted upon by two opposing powers ; namely, by that of attraction , which draws them towards the sun ; and that of impulsion , which drives them straight forward into the great void of space ; THE EARTH. 11 they pursue a track between these contrary directions ; and each, like a stone whirled about in a sling, obeying two op- posite forces, circulates round its great centre of heat and motion. In this manner, therefore, is the harmony of our planet- ary system preserved. The sun, in the midst, gives heat, and light, and circular motion, to the planets which sur- round it : Mercury, Venus, the Earth, Mars, Jupiter, Sa- turn, and Herschel, or the Georgium Sidus, perform their constant circuits at different distances, each taking up a time to complete its revolutions proportioned to the great- ness of the circle which it is to describe. The lesser planets also, which are attendants upon some of the greater, are subject to the same laws ; they circulate with the same exact- ness ; and are, in the same manner, influenced by their respective centres of motion. Besides those bodies which make a part of our peculiar system, and which may be said to reside within its great circumference, there are others that frequently come among us, from the most distant tracts of space, and that seem like dangerous intruders upon the beautiful simpli- city of nature. These are Comets, whose appearance was once so terrible to mankind; and the theory of which is so little understood at present : all we know is, that their number is much greater than that of the planets ; and that, like these, they roll in orbits, in some measure obedient to solar influence. Astronomers have endeavoured to calculate the returning periods of many of them ; but ex- perience has not, as yet, confirmed the veracity of their investigations. Indeed, who can tell, when those wan- derers have made their excursions into other worlds and distant systems, what obstacles may be found to oppose their progress, to accelerate their motions, or retard their return ? But what we have hitherto attempted to sketch, is but a small part of that great fabric in which the Deity has thought proper to manifest his wisdom and omnipotence. There are multitudes of other bodies, dispersed over the face of the heavens, that lie too remote for examination : these have no motion, such as the planets are found to possess, and are, therefore, called fixed stars ; and from their extreme brilliancy, and their immense distance. A HISTORY OF 12 philosophers have been induced to suppose them to be suns* resembling that which enlivens our system. As the imagi- nation also, once excited is seldom content to stop, it has furnished each with an attendant system of planets belong- ing to itself ; and has even induced some to deplore the fate of those systems, whose imagined suns, which sometimes happens, have become no longer visible. But conjectures of this kind, which no reasoning can ascertain, nor experiment reach, are rather amusing than useful. Though we see the greatness and wisdom of the Deity in all the seeming worlds that surround us, it is our chief concern to trace him in that which we inhabit. The examination of the earth, the wonders of its contrivance, the history of its advantages, or of the seeming defects in its formation, are the proper business of the natural histo- rian. A description of this earth , its animals, vegetables , and minerals, is the most delightful entertainment the mind can be furnished with, as it is the most interesting and use- ful. I would beg leave, therefore, to conclude these com- mon-place speculations, with an observation which, I hope, is not entirely so. An use, hitherto not much insisted upon, that may re- sult from the contemplation of celestial magnificence, is, that it will teach us to make an allowance for the apparent irregularities we find below. Whenever we can examine the works of the Deity at a proper point of distance, so as to take in the whole of his design, we see nothing but uniformity, beauty, and precision. The heavens present us with a plan, which, though inexpressibly magnificent, is yet regular beyond the power of invention. Whenever, therefore, we find any apparent defects in the Earth, which we are about to consider, instead of attempting to reason ourselves into an opinion that they are beautiful, it will be wiser to say, that we do not behold them at the proper point of distance, and that our eye is laid too close to the objects, to take in the regularity of their connexion. In short, we may conclude, that God, who is regular in his great pro- ductions, acts with equal uniformity in the little. THE EARTH. 13 CHAP. II. A SHORT SURVEY OF THE GLOBE, FROM THE LIGHT OF ASTRONOMY AND GEOGRAPHY. All the sciences are, in some measure, linked with each other, and before the one is ended, the other begins. In a natural history, therefore, of the earth, we must be- gin with a short account of its situation and form, as given us by astronomers and geographers : it will be sufficient, however, upon this occasion, just to hint to the imagina- tion, what they, by the most abstract reasonings, have forced upon the understanding. The earth which we in- habit is, as has been said before, one of those bodies which circulate in our solar system ; it is placed at a happy middle . distance from the centre ; and even seems, in this respect, privileged beyond all other planets that depend upon our great luminary for their support. Less distant from the sun than Herschel, or the Georgium Sidus, Saturn, Jupiter, and Mars, and yet less parched up than Venus and Mer- cury, that are situate too near the violence of its power, the Earth seems in a peculiar manner to share the bounty of the Creator : it is not, therefore, without reason, that man- kind consider themselves as the peculiar objects of his provi- dence and regard. Besides that motion which the earth has round the sun, the circuit of which is performed in a year, it has another upon its own axle, which it performs in twenty-four hours. Thus, like a chariot-wheel, it has a compound motion; for while it goes forward on its journey, it is all the while turning upon itself. From the first of these two arise the grateful vicissitude of the seasons ; from the second, that of day and night. It may be also readily conceived, that a body thus wheeling in circles will most probably be itself a sphere. The earth, beyond all possibility of doubt, is found to be so. Whenever its shadow happens to fall upon the moon, in an eclipse, it appears to be always circular, in whatever position it is projected : and it is easy to prove, that a body which in every position makes a circular shadow, must A HISTORY OF 14 itself be round. The rotundity of the earth may be also proved from the meeting of two ships at sea: the top- masts of each are the first parts that are discovered by both, the under parts being hidden by the convexity of the globe which rises between them. The ships, in this instance, may be resembled to two men who approach each other on the opposite sides of a hill : their heads will first be seen, and gradually as they come nearer they will come entirely into view. However, though the earth’s figure is said to be spheri- cal, we ought only to conceive it as being nearly so. It has been found in the last age to be rather flatted at both poles, so that its form is commonly resembled to that of a turnip. The cause of this swelling of the equator is ascribed to the greater rapidity of the motion with which the parts of the earth are there carried round ; and which, consequently, endeavouring to fly off, act in opposition to central attraction. The twirling of a mop may serve as an homely illustration ; which, as every one has seen, spreads and grows broader in the middle as it continues to be turned round. As the earth receives light and motion from the sun, so it derives much of its warmth and power of vegetation from the same beneficent source. However, the different parts of the globe participate of these advantages in very different proportions, and accordingly put on very different appear- ances ; a polar prospect, and a landscape at the equator, are as opposite in their appearances as in their situation. The polar regions, that receive the solar beams in a very oblique direction, and continue for one half of the year in night, receive but few of the genial comforts which other 0 parts of the world enjoy. Nothing can be more mournful or hideous than the picture which travellers present of those wretched regions. The ground,* which is rocky and bar- ren, rears itself in every place in lofty mountains and in- accessible cliffs, and meets the mariner’s eye at even forty leagues from shore. These precipices, frightful in them- selves, receive an additional horror from being constantly covered with ice and snow, which daily seem to accumu- late, and fill all the vallies with increasing desolation. The * Crantz’s History of Greenland, p. 3. THE EARTH. 15 few rocks and cliffs that are bare of snow, look at a dis- tance of a dark brown colour, and quite naked. Upon a nearer approach, however, they are found replete with many different veins of coloured stone, here and there spread over with a little earth, and a scanty portion of grass and heath. The internal parts of the country are still more desolate and deterring. In wandering through these solitudes, some plains appear covered with ice, that, at first glance, seem to promise the traveller an easy jour- ney.* But these are even more formidable and more im- passable than the mountains themselves, being cleft with dreadful chasms, and every where abounding with pits that threaten certain destruction. The seas that surround these inhospitable coasts are still more astonishing, being covered with flakes of floating ice, that spread like exten- sive fields, or that rise out of the water like enormous mountains. These, which are composed of materials as clear and transparent as glass, -f* assume many strange and fantastic appearances. Some of them look like churches or castles, with pointed turrets ; some like ships in full sail ; and people have often given themselves the fruitless toil to attempt piloting the imaginary vessels into har- bour. There are still others that appear like large islands, with plains, vallies, and hills, which often rear their heads two hundred yards above the level of the sea ; and although the height of these be amazing, yet their depth beneath is still more so ; some of them being found to sink three hun- dred fathom under water. The earth presents a very different appearance at the equa- tor, where .the sun -beams, darting directly downwards, bum up the lighter soils into extensive sandy deserts, or quicken all the moister tracts with incredible vegetation. In these regions, almost all the same inconveniences are felt from the proximity of the sun, that in the former were endured from its absence. The deserts are entirely barren, except where they are found to produce serpents, and that in such quantities, that some extensive plains seem almost entirely covered with them.^ It not unfrequently happens also, that this dry soil, which is so parched and comminuted by the force of the * Crantz’s History of Greenland, p. 22. t Ibid. p. 27 . % Adanson’s Description of Senegal. 16 A HISTORY OF sun, rises with the smallest breeze of wind ; and the sands being composed of parts almost as small as those of water, they assume a similar appearance, rolling onward in waves like those of a troubled sea, and overwhelming all they meet with inevitable destruction. On the other hand, those tracts which are fertile, teem with vegetation even to a noxious degree. The grass rises to such a height as often to require burning ; the forests are impassable from underwoods, and so matted above, that even the sun, fierce as it is, can seldom penetrate.* These are so thick as scarcely to be extirpated ; for the tops being so bound to- gether by the climbing plants that grow round them, though an hundred should be cut at the bottom, yet not one would fall, as they mutually support each other. In these dark and tangled forests, beasts of various kinds, insects in astonish- ing abundance, and serpents of surprising magnitude, find a quiet retreat from man, and are seldom disturbed except by each other. In this manner the extremes of our globe seem equally unfitted for the comforts and conveniences of life : and al- though the imagination may find an awful pleasure in contemplating the frightful precipices of Greenland, 01 the luxurious verdure of Africa, yet true happiness can only be found in the more moderate climates, where the gifts of nature may be enjoyed, without incurring danger in obtaining them. It is in the temperate zone, therefore, that all the arts of improving nature, and refining upon happiness, have been invented: and this part of the earth is, more pro- perly speaking, the theatre of natural history. Although there be millions of animals and vegetables in the unex- plored forests under the line, yet most of these may for ever continue unknown, as curiosity is there repressed by surrounding danger. But it is otherwise in these de- lightful regions which we inhabit, and where this art has had its beginning. Among us there is scarce a shrub, a flower, or an insect, without its particular history; scarce a plant that could be useful, which has not been propa- gated; nor a weed that could be noxious, which has not been pointed out. * Linnaei Amsenit. vol. vi, p. 6J. THE EARTH. 17 CHAP. III. A VIEW OF THE SURFACE OF THE EARTH. When we take a slight survey of the surface of our globe, a thousand objects offer themselves, which, though long known, yet still demand our curiosity. The most obvious beauty that every where strikes the eye is the ver- dant covering of the earth, which is formed by an happy mixture of herbs and trees of various magnitudes and uses. It has been often remarked, that no colour re- freshes the sight so much as green : and it may be added, as a further proof of the assertion, that the inhabitants of those places where the fields are continually white with snow, generally become blind long before the usual course of nature. This advantage, which arises from the verdure of the fields, is not a little improved by their agreeable inequalities. There are scarcely two natural landscapes that offer prospects en- tirely resembling each other ; their risings and depres- sions, their hills and valleys, are never entirely the same, but always offer something new to entertain and refresh the imagination. But to increase the beauties of the face of nature, the landscape is enlivened by springs and lakes, and inter- sected by rivulets. These lend a brightness to the pros- pect; give motion and coolness to the air; and, what is much more important, furnish health and subsistence to animated nature. Such are the most obvious and tranquil objects that every where offer : but there are objects of a more awful and mag- nificent kind ; the Mountain rising above the clouds, and topped with snow ; the River pouring down its sides, in- creasing as it runs, and losing itself, at last, in the ocean ; the Ocean spreading its immense sheet of waters over one half of the globe, swelling and subsiding at well-known in- tervals, and forming a communication between the most distant parts of the earth. If we leave those objects that seem to be natural to our earth, and keep the same constant tenor, we are presented with the great irregularities of nature : the burning mountain ; vol. i. — 1. " C A HISTORY OF 18 the abrupt precipice ; the unfathomable cavern ; the head- long cataract ; and the rapid whirlpool. If we carry our curiosity a little further, and descend to the objects immediately below the surface of the globe, we shall there find wonders still as amazing. We first perceive the earth, for the most part, lying in regular beds or layers, every bed growing thicker in proportion as it lies deeper, and its contents more compact and heavy. W e shall find, almost wherever we make our subterranean in- quiry, an amazing number of shells that once belonged to aquatic animals. Here and there, at a distance from the sea, beds of oyster-shells, several yards thick, and many miles over ; sometimes testaceous substances of various kinds on the tops of mountains, and often in the heart of the hardest marble. These, which are dug up by the pea- sants in every country, are regarded with little curiosity ; for being so very common, they are considered as sub- stances entirely terrene. But it is otherwise with the in- quirer after nature, who finds them, not only in shape, but in substance, every way resembling those that are found in the sea ; and he, therefore, is at a loss to account for their removal. Yet not one part of nature alone, but all her produc- tions and varieties, become the object of the speculative fail’s inquiry : he takes different views of nature from the inattentive spectator ; and scarcely an appearance, how common soever, but affords matter for his contemplation : he inquires how and why the surface of the earth has those risings and depressions which most men call natu- ral ; he demands in what manner the mountains were formed, and in what consists their uses ; he asks from whence springs arise, and how rivers flow round the con- vexity of the globe ; he enters into an examination of the ebbings and flowings, and the other wonders of the deep ; he acquaints himself with the irregularities of nature, and endeavours to investigate their pauses ; by which, at least, he will become better versed in their history. The inter- nal structure of the globe becomes an object of his curio- sity ; and, although his inquiries can fathom but a very little way, yet, if possessed with a spirit of theoiy, his imagination will supply the rest. He will endeavour to account for the situation of the marine fossils that are THE EARTH. 19 found in the earth, and for the appearance of the different beds of which it is composed. These have been the inqui- ries that have splendidly employed many of the philosophers of the last and present age,* and, to a certain degree, they must be serviceable. But the worst of it is, that, as specu- lations amuse the writer more than facts, they may be often carried to an extravagant length ; and that time may be spent in reasoning upon nature, which might be more use- fully employed in writing her history. Too much speculation in natural history is certainly wrong; but there is a defect of an opposite nature that does much more prejudice ; namely, that of silencing all inquiry, by alleging the benefits we receive from a thing, instead of investigating the cause of its production. If I inquire how a mountain came to be formed ; such a rea- soner, enumerating its benefits, answers, because God knew it would be useful. If I demand the cause of an earthquake, he finds some good produced by it, and al- leges that as the cause of its explosion. Thus such an in- quirer has constantly some ready reason for every appear- ance in nature, which serves to swell his periods, and give splendour to his declamation ; every thing about him is, on some account or other, declared to be good; and he thinks it presumption to scrutinize into its defects, or to endeavour to imagine how it might be better. Such writers, and there are many such, add very little to the advance- ment of knowledge. It is finely remarked by Bacon, that the investigation of final causes “f* is a barren study ; and, like a virgin dedicated to the Deity, brings forth nothing. In fact, those men who want to compel every appearance and every irregularity in nature into our service, and expa- tiate on their benefits, combat that very morality which they would seem to promote. God has permitted thousands of natural evils to exist in the world, because it is by their inter- vention that man is capable of moral evil ; and he has per- mitted that we should be subject to moral evil, that we might do something to deserve eternal happiness, by shewing that we had rectitude to avoid it. * Buffon, Woodward, Burnet, Whiston, Kircher, Bourquat, Leibnitz, Steno, Ray, &c. t Investigatio causarum finalium sterilis est, et veluti virgo D$o de- dicata, nil parit. 20 A HISTORY OF CHAP. IV. A REVIEW OF THE DIFFERENT THEORIES OF THE EARTH, Human invention has been exercised for several ages to account for the various irregularities of the earth. While those philosophers, mentioned in the last chapter, see no- thing but beauty, symmetry, and order ; there are others, who look upon the gloomy side of nature, enlarge on its de- fects, and seem to consider the earth, on which they tread, as one scene of extensive desolation.* Beneath its surface they observe minerals and waters confusedly jumbled to- gether ; its different beds of earth irregularly lying upon each other; mountains rising from places that once were level and hills sinking into vallies ; whole regions swal- lowed by the sea, and others again rising out of its bosom. All these they suppose to be but a few of the changes that have been wrought in our globe; and they send out the imagination to describe its primaeval state of beauty. Of those who have written theories describing the manner of the original formation of the earth, or accounting for its present appearances, the most celebrated are Burnet, Whis- ton, Woodward, and Buffon. As speculation is endless, so it is not to be wondered that all these differ from each other, and give opposite accounts of the several changes, which they suppose our earth to have undergone. As the systems of each have had their admirers, it is, in some measure, in- cumbent upon the natural historian to be acquainted, at least, with their outlines ; and, indeed, to know w-hat others have even dreamed in matters of science, is very use- ful, as it may often prevent us from indulging similar delu- sions ourselves, which we should never have adopted, but because we take them to be wholly our own. However, as entering into a detail of these theories is rather furnishing a history of opinions than things, I will endeavour to be as concise as I can. The first who formed this amusement of earth-making into system, was the celebrated Thomas Burnet, a man of polite learning and rapid imagination. His Sacred Theory , * Buffon’s Second Discourse, t Senec. Qusest. lib. vi. cap. 21. THE EARTH. 21 as he calls it, describing the changes which the earth has undergone, or shall hereafter undergo, is well known for the warmth with which it is imagined, and the weakness with which it is reasoned; for the elegance of its style, and the meanness of its philosophy. “ The earth,” says he, “ before the deluge, was very differently formed from what it is at present : it was at first a fluid mass ; a chaos composed of various substances, differing both in density and figure : those which were most heavy, sunk to the cen- tre, and formed in the middle of our globe a hard solid body ; those of a lighter nature remained next ; and the waters, which were lighter still, swam upon its surface, and covered the earth on every side. The air, and all those fluids which were lighter than water, floated upon this also ; and in the same manner encompassed the globe ; so that between the surrounding body of waters, and the cir- cumambient air, there was formed a coat of oil, and other unctuous substances, lighter than water. However, as the air was still extremely impure, and must have carried up with it many of those earthy particles with which it once was intimately blended, it soon began to defecate, and to de- pose these particles upon the oily surface already mentioned, which soon uniting, the earth and oil formed that crust, which soon became an habitable surface, giving life to vegetation, and dwelling to animals. “ This imaginary antediluvian abode was very different from what we see it at present. The earth was light and rich ; and formed of a substance entirely adapted to the feeble state of incipient vegetation ; it was an uniform plain, every where covered with verdure ; without moun- tains, without seas, or the smallest inequalities. It liad no difference of seasons, for its equator was in the plane of the ecliptie, or, in other words, it turned directly opposite to the sun, so that it enjoyed one perpetual and luxuriant spring. However, this delightful face of nature did not long continue in the same state ; for, after a time, it be- gan to crack and open in fissures ; a circumstance which always succeeds when the sun exhales the moisture from rich or marshy situations. The crimes of mankind had been for some time preparing to draw down the wrath of Heaven ; and they, at length, induced the Deity to defer repairing these breaches in nature. Thus the chasms of A HISTORY OF 22 the earth eveiy day became wider, and, at length, they pene- trated to the great abyss of waters ; and the whole earth, in a manner, fell in. Then ensued a total disorder in the uni- form beauty of the first creation, the terrene surface of the globe being broken down : as it sunk the waters gushed out in its place ; the deluge became universal ; all mankind, ex- cept eight persons, were destroyed, and their posterity con- demned to toil upon the ruins of desolated nature.” It only remains to mention the manner in which he re- lieves the earth from this universal wreck, which would seem to be as difficult as even its first formation : “ These great masses of earth falling into the abyss, drew down with them vast quantities also of air ; and, by dashing against each other, and breaking into small parts by the repeated violence of the shock, they, at length, left between them large cavities, filled with nothing but air. These cavities naturally offered a bed to receive the influent waters ; and in proportion as they filled, the face of the earth became once more visible. The higher parts of its broken surface, now become the tops of mountains, were the first that appeared ; the plains soon after came forward, and, at length, the whole globe was delivered from the waters, except the places in the lowest situations ; so that the ocean and the seas are still a part of the ancient abyss, that have not had a place to return. Islands and rocks are fragments of the earth’s former crust; kingdoms and continents are larger masses of its broken substance ; and all the inequalities that are to be found on the surface of the present earth, are owing to the accidental confusion into which both earth and waters were then thrown.” The next theorist was Woodward, who, in his Essay to- wards a Natural History of the Earth, which was only de- signed to precede a greater work, has endeavoured to give a more rational account of its appearances ; and was, in fact, much better furnished for such an undertaking than any of his predecessors, being one of the most assiduous natur- alists of his time. His little book, therefore, contains many important facts, relative to natural history, although his system may be weak and groundless. He begins by asserting that all terrene substances are disposed in beds of various natures, lying horizontally one over the other, somewhat like the coats of an onion ; that A HISTORY OF 300 conjectures of all those that preceded him, ascribes hunger to the united effect of both these causes ; and asserts, that the pungency of the gastric juices, and the attrition of its coats against each other, cause those pains, which nothing but food can remove. These juices continuing still to be sepa- rated in the stomach, and every moment becoming more acrid, mix with the blood, and infect the circulation : the circulation being thus contaminated, becomes weaker, and more contracted ; and the whole nervous frame sympa- thizing, an hectic fever, and sometimes madness, is produced ; in which state the faint wretch expires. In this manner, the man who dies of hunger, may be said to be poisoned by the juices of his own body ; and is destroyed less by the want of nourishment, than by the vitiated qualities of that which he had already taken. However this may be, we have but few instances of men dying, except at sea, of absolute hunger. The de- cline of those unhappy creatures who are destitute of food, at land, being more slow and unperceived. These, from often being in need, and as often receiving an acciden- tal supply, pass their lives between surfeiting and repin- ing; and their constitution is impaired by insensible de- grees. Man is unfit for a state of precarious expectation. That share of provident precaution which incites him to lay up stores for a distant day, becomes his torment, when totally unprovided against an immediate call. The lower race of animals, when satisfied, for the instant moment, are perfectly happy : but it is otherwise with man ; his mind anticipates distress, and feels the pangs of want even before it arrests him. Thus the mind, being continually harassed by the situation, it at length influences the con- stitution, and unfits it for all its functions. Some cruel disorder, but no way like hunger, seizes the unhappy suf- ferer ; so that almost all those men who have thus long lived by chance, and whose every day may be considered as an happy escape from famine, are known at last to die in reality of a disorder caused by hunger; but which, in the common language, is often called a broken heart . Some of these I have known myself, when very little able to relieve them : and I have been told, by a very active and worthy magistrate, that the number of such as die in London for want, is much greater than one THE EARTH. 23 they are replete with shells, and other productions of the sea; these shells being found in the deepest cavities, and on the tops of the highest mountains. From these ob- servations, which are warranted by experience, he pro- ceeds to observe, that these shells and extraneous fossils are not productions of the earth, but are all actual re- mains of those animals which they are known to resem- ble; that all the beds of the earth lie under each other, in the order of their specific gravity; and that they are disposed as if they had been left there by subsiding wa- ters. All these assertions he affirms with much earnest- ness, although daily experience contradicts him in some of them; particularly we find layers of stone often over the lightest soils, and the softest earth under the hardest bodies. However, having taken it for granted, that all the layers of the earth are found in the order of their spe- cific gravity, the lightest at the top, and the heaviest next the centre, he consequently asserts, and it will not im- probably follow, that all the substances of which the earth is composed, were once in an actual state of dissolution. This universal dissolution he takes to have happened at the time of the flood. He supposes, that at that time a body of water which was then in the centre of the earth, uniting with that which was found on the surface, so far separated the terrene parts as to mix all together in one fluid mass ; the contents of which afterwards sinking ac- cording to their respective gravities, produced the present appearances of the earth. Being aware, however, of an objection, that fossil substances are not found dissolved, he exempts them from this universal dissolution, and, for that purpose, endeavours to show that the parts of animals have a stronger cohesion than those of minerals ; and that, while even the hardest rocks may be dissolved, bones and shells may still continue entire. So much for W oodward ; but of all the systems which were published respecting the earth’s formation, that of Whiston was most applauded, and most opposed. Nor need we wonder : for being supported with all the parade of deep calculation, it awed the ignorant, and produced the approbation of such as would be thought otherwise; as it implied a knowledge of abstruse learning, to be even thought capable of comprehending what the writer aimed # A HISTORY OF 24 at. In fact, it is not easy to divest this theory of its mathe- matical garb : but those who have had leisure, have found the result of our philosopher’s reasoning to be thus : He supposes the earth to have been originally a comet ; and he considers the history of the creation, as given us in scrip- ture, to have its commencement just when it was, by the hand of the Creator, more regularly placed as a planet in our solar system. Before that time he supposes it to have been a globe without beauty or proportion ; a world in disorder ; subject to all the vicissitudes which comets endure ; some of which have been found, at different times, a thousand times hotter than melted iron ; at others, a thousand times colder than ice. These alterations of heat and cold, conti- nually melting and freezing the surface of the earth, he sup- poses to have produced, to a certain depth, a chaos entirely resembling that described by the poets, surrounding the solid contents of the earth, which still continued unchanged in the midst, making a great burning globe of more than two thousand leagues in diameter. This surrounding chaos, however, was far from being solid : he resembles it to a dense, though fluid atmosphere, composed of substances mingled, agitated, and shocked against each other ; and in this disorder he describes the earth to have been just at the eve of creation. But upon its orbit being then changed, when it was more regularly wheeled round the sun, every thing took its proper place ; every part of the surrounding fluid then fell into a situation, in proportion as it was light or heavy. The middle, or central part, which always remained un- changed, still continued so, retaining* a part of that heat which it received in its primaeval approaches towards the sun ; which heat, he calculates, may continue for about six thousand years. Next to this fell the heavier parts of the chaotic atmosphere, which serve to sustain the lighter : but as in descending they could not entirely be separated from many watery parts, with which they were intimately mixed, they drew down a part of these also with them ; and these could not mount again after the surface of the earth was consolidated : they, therefore, surrounded the heavy first-descending parts in the same manner as these surround the central globe. Thus the entire body of the earth is composed internally of a great burning globe : -I THE EARTH. 25 next which is placed a heavy terrene substance, that encom- passes it; round which also is circumfused a body of water. Upon this body of water, the crust of earth, which we inha- bit, is placed : so that, according to him, the globe is com- posed of a number of coats, or shells, one within the other, all of different densities. The body of the earth being thus formed, the air, which is the lightest substance of all, sur- rounded its surface ; and the beams of the sun, darting through, produced that light which, we are told, first obeyed the Creator’s command. The whole economy of the creation being thus adjusted, it only remained to account for the risings and depressions on the surface of the earth, with the other seeming irregula- rities of its present appearance. The hills and valleys are considered by him as formed by their pressing upon the internal fluid, which sustains the outward shell of earth, with greater or less weight: those parts of the earth which are heaviest sink into the subjacent fluid more deeply, and be- come valleys : those that are lightest, rise higher upon the earth’s surface, and are called mountains. Such was the face of nature before the deluge : the earth was then more fertile and populous than it is at present ; the life of man and animals was extended to ten times its present duration ; and all these advantages arose from the superior heat of the central globe, which ever since has been cooling. As its heat was then in full power, the genial principle was also much greater than at present ; vegetation and animal increase were carried on with more vigour ; and all nature seemed teeming with the seeds of life. But these physical advantages were only productive of moral evil ; the warmth which invigorated the body increased the passions and appetites of the mind; and, as man became more powerful, he grew less innocent. It was found necessary to punish this depravity; and all living creatures were overwhelmed by the deluge in universal destruction. This deluge, which simple believers are willing to as- cribe to a miracle, philosophers have long been desirous to account for by natural causes ; they have proved that the earth could never supply from any reservoir towards its centre, nor the atmosphere by any discharge from above, such a quantity of water as would cover the surface VOL. I. — 1. D 26 A HISTORY OF of the globe to a certain depth over the tops of our highest mountains. Where, therefore, was all this water to be found P Whiston has found enough, and more than a suffi- ciency, in the tail of a comet ; for he seems to allot comets a very active part in the great operations of nature. He calculates, with great seeming precision, the year, the month, and the day of the week, on which this comet (which has paid the earth some visits since, though at a kinder dis- tance,) involved our globe in its tail. The tail he supposed to be a vaporous fluid substance, exhaled from the body of the comet by the extreme heat of the sun, and increasing in proportion as it approached that great luminary. It was in this that our globe was involved at the time of the deluge ; and, as the earth still acted by its natural attraction, it drew to itself all the watery vapours which were in the comet’s tail ; and the internal waters being also at the same time let loose, in a very short space the tops of the highest mountains were laid under the deep. The punishment of the deluge being thus completed, and all the guilty destroyed, the earth, which had been broken by the eruption of the internal waters, was also enlarged by it ; so that, upon the comet’s recess, there was found room suffi- cient in the internal abyss for the recess of the superfluous waters; whither they all retired, and left the earth unco- vered, but in some respects changed, particularly in its figure, which, from being round, was now become ob- late. In this universal wreck of nature, Noah survived, by a variety of happy causes, to re-people the earth, and to give birth to a race of men slow in believing ill-imagined theories of the earth. After so many theories of the earth which have been pub- lished, applauded, answered, and forgotten, Mr. BufFon ventured to add one more to the number. This philosopher was, in every respect, better qualified than any of his prede- cessors for such an attempt, being furnished with more materials, having a brighter imagination to find new proofs, and a better style to clothe them in. However, if one so ill qualified as I am may judge, this seems the weakest part of his admirable work ; and I could wish that he had been con- tent with giving us facts instead of systems ; that, instead of being a reasoner, he had contented himself with being merely an historian. * THE EARTH 27 He begins his system by making a distinction between the first part of it and the last; the one being founded only on conjecture, the other depending entirely upon actual observation. The latter part of his theory may, therefore, be true, though the former should be found erroneous. “ The planets,” says he, “ and the earth among the number, might have been formerly (he only offers this as conjecture) a part of the body of the sun, and adherent to its substance. In this situation, a comet falling in upon that great body, might have given it such a shock, and so shaken its whole frame, that some of its particles might have been driven off like streaming sparkles from red-hot iron ; and each of these streams of fire, small as they wTere in comparison of the sun, might have been large enough to have made an earth as great, nay, many times greater, than our’s. So that in this manner the planets, together with the globe which we inhabit, might have been driven off from the body of the sun by an impulsive force: in this manner also they would continue to recede from it for ever, were they not drawn back by its superior power of attraction ; and thus, by the combination of the two motions, they are wheeled round in circles. “ Being in this manner detached at a distance from the body of the sun, the planets, from having been at first globes of liquid fire, gradually became cool. The earth also, having been impelled obliquely forward, received a rotatory motion upon its axis at the very instant of its formation ; and this motion being greatest at the equator, the parts there acting against the force of gra- vity, they must have swollen out, and given the earth an oblate or flatted figure. “As to its internal substance, our globe, having once belonged to the sun, it continues to be an uniform mass of melted matter, very probably vitrified in its primaeval fusion. But its surface is very differently composed. Having been in the beginning heated to a degree equal to, if not greater, than what comets are found to sustain ; like them it had an atmosphere of vapours floating round it, and which, cooling by degrees, condensed and subsid- ed upon its surface. These vapours formed, according to their different densities, the earth, the water, and the A HISTORY OF 28 air ; the heavier parts falling first, and the lighter remaining still suspended.” Thus far our philosopher is, at least, as much a system- maker as Whiston or Burnet ; and, indeed, he fights his way with great perseverance and ingenuity, through a thousand objections that naturally arise. Having, at last, got upon the earth, he supposes himself on firmer ground, and goes forward with greater security. Turn- ing his attention to the present appearance of things upon this globe, he pronounces from the view, that the whole earth was at first under water. This water he supposes to have been the lighter parts of its former evaporation, which, while the earthy particles sunk downwards by their natural gravity, floated on the surface, and covered it for a considerable space of time. “ The surface of the earth,” says he,* “ must have been in the beginning much less solid than it is at present ; and, consequently, the same causes which at this day produce but very slight changes, must then, upon so complying a substance, have had very considerable effects. We have no reason to doubt but that it was then covered with the waters of the sea ; and that those waters were above the tops of our highest mountains : since, even in such ele- vated situations, we find shells and other marine produc- tions in very great abundance. It appears also that the sea continued for a considerable time upon the face of the earth: for as these layers of shells are found so very fre- quent at such great depths, and in such prodigious quan- tities, it seems impossible for such numbers to have been supported all alive at one time ; so that they must have been brought there by successive depositions. These shells also are found in the bodies of the hardest rocks, where they could not have been deposited, all at once, at the time of the deluge, or at any such instant revolution ; since that would be to suppose, that all the rocks in which they are found, were, at that instant, in a state of dissolution, which would be absurd to assert. The sea, therefore, deposited them wheresoever they are now to be found, and that by slow and successive degrees. “ It will appear also, that the sea covered the whole * Theurie cle la lerrc, vol. i. p. 111. THE EARTH. 29 earth, from the appearance of its layers, which lying re- gularly one above the other, seem all to resemble the se- diment formed at different times by the ocean. Hence, by the irregular force of its waves, and its currents driving the bottom into sand-banks, mountains must have been gradually formed within this universal covering of waters ; and these successively raising their heads above its sur- face, must, in time, have formed the highest ridges of mountains upon land, together with continents, islands, and low grounds, all in their turns. This opinion will receive additional weight by considering, that in those parts of the earth where the power of the ocean is great- est, the inequalities on the surface of the earth are high- est. The ocean’s power is greatest at the equator, where its winds and tides are most constant ; and, in fact, the mountains at the equator are found to be higher than in any other part of the world. The sea, therefore, has pro- duced the principal changes in our earth : rivers, volca- noes, earthquakes, storms, and rain, having made but slight alterations, and only such as have affected the globe to very inconsiderable depths.” This is but a very slight sketch of Mr. Buffon’s theory of the earth ; a theory which he has much more power- fully supported, than happily invented ; and it would be needless to take up the reader’s time from the pursuit of truth in the discussion of plausibilities. In fact, a thou- sand questions might be asked this most ingenious phi- losopher, which he would not find it easy to answer ; but such is the lot of humanity, that a single Goth can in one day destroy the fabric which Caesars were employed an age in erecting. We might ask, How mountains, which are composed of the most compact and ponderous sub- stances, should be the first whose parts the sea began to remove ? We might ask, How fossil- wood is found deeper even than shells ? which argues, that trees grew upon the places he supposes once to have been covered with the ocean. But we hope this excellent man is better employed than to think of gratifying the petulance of incredulity, by answering endless objections. 30 A HISTORY OF CHAP. V. OF FOSSIL-SHELLS, AND OTHER EXTRANEOUS FOSSILS. We may affirm of Mr. Buffon, that which has been said of the chemists of old ; though he may have failed in at- taining his principal aim, of establishing a theory, yet he has brought together such a multitude of facts relative to the history of the earth, and the nature of its fossil pro- ductions, that curiosity finds ample compensation, even while it feels the want of conviction. Before, therefore, I enter upon the description of those parts of the earth which seem more naturally to fall within the subject, it will not be improper to give a short history of those animal productions that are found in such quantities, either upon its surface, or at different depths below it. They demand our curiosity ; and, indeed, there is nothing in natural history that has afforded more scope for doubt, conjecture, and speculation. Whatever depths of the earth we examine, or at whatever distance within land we seek, we most commonly find a number of fossil- shells, which being compared with others from the sea, of known kinds, are found to be exactly of a similar shape and nature.* They are found at the very bottom of quar- ries and mines, in the retired and inmost parts of the most firm and solid rocks, upon the tops of even the highest hills and mountains, as well as in the valleys and plains ; and this not in one country alone, but in all places where there is any digging for marble, chalk, or any other terrestrial matters, that are so compact as to fence off the external injuries of the air, and thus preserve these shells from decay. These marine substances, so commonly diffused, and so generally to be met with, were for a long time consi- dered by philosophers as productions, not of the sea, but of the earth. “ As we find that spars,” said they, “ always shoot into peculiar shapes, so these seeming snails, coc- kles, and mussel-shells, are only sportive forms that na- * Woodward’s Essay towards a Natural History, p. 16. THE EARTH. 31 ture assumes amongst others of its mineral varieties : they have the shape of fish, indeed, but they have always been terrestrial substances.”* With this plausible solution mankind were for a long time content; but upon closer inquiry, they were obliged to alter their opinion. It was found that these shells had in every respect the properties of animal, and not of mineral nature. They were found exactly of the same weight with their fellow shells upon shore. They answered all the che- mical trials in the same manner as sea-shells do. Their parts, when dissolved, had the same appearance to view, the same smell and taste. They had the same effects in medi- cine, when inwardly administered ; and, in a word, were so exactly conformable to marine bodies, that they had all the accidental concretions growing to them, (such as pearls, corals, and smaller shells,) which are found in shells just gathered on the shore. They were, therefore, from these considerations, given back to the sea; but the wonder was, how to account for their coming so far from their own natural element upon land.^ As this naturally gave rise to many conjectures, it is not to be wondered that some among them have been very extraordinary. An Italian, quoted by Mr. Buffon, suppose., them to have been deposited in the earth at the time of the crusades, by the pilgrims who returned from Jerusalem ; who gathering them upon the sea-shore, in their return carried them to their different places of habi- tation. But this conjecturer seems to have but a very inadequate idea of their numbers. At Touraine, in France, more than a hundred miles from the sea, there is a plain of about nine leagues long, and as many broad, whence the peasants of the country supply themselves with marl for manuring their lands. They seldom dig deeper than twenty feet ; and the whole plain is composed of the same materials, which are shells of various kinds, without the smallest portion of earth between them. Here then is a large space, in which are deposited millions of tons of shells, that pilgrims could not have collected, though their whole employment had been nothing else. England * Lowthorp’s Abridgment, Phil. Trans, vol. ii. p. 4 26. f Woodward, p. 43. A HISTORY OF 32 is furnished with its beds, which, 'though not quite so exten- sive, yet are equally wonderful. “ Near Reading, in Berk- shire, for many succeeding generations, a continued body of oyster-shells has been found through the whole circumfer- ence of five or six acres of ground. The foundation of these shells is a hard rocky chalk ; and above this chalk, the oyster-shells lie in a bed of green sand, upon a level, as nigh as can possibly be judged, and about two feet thick- ness.”* These shells are in their natural state, but they were found also petrified, and almost in equal abundance ~j~ in all the Alpine rocks, in the Pyrenees, on the hills of France, England, and Flanders. Even in all quarries from whence marble is dug, if the rocks be split perpendicularly downwards, petrified shells and other marine substances will be plainly discerned. “ About a quarter of a mile from the river Medway, in the county of Kent, after the taking off the coping of a piece of ground there, the workmen came to a blue mar- ble, which continued for three feet and a half deep, or more, and then beneath appeared a hard floor, or pave- v ment, composed of petrified shells crowded closely toge- ther. This layer was about an inch deep, and several yards over ; and it could be walked upon as upon a beach. These stones, of which it was composed, (the describer supposes them to have always been stones,) were either wreathed as snails, or bivalvular like cockles. The wreathed kinds were about the size of a hazel-nut, and were filled with a stony substance of the colour of marie ; and they themselves, also, till they were washed, were of the same colour; but when cleaned, they ap- peared of the colour of bezoar, and of the same polish. After boiling in water they became whitish, and left a ' chalki- ness upon the fingers.”^ In several parts of Asia and Africa, travellers have ob- served these shells in great abundance. In the mountains of Castravan, which lie above the city Barut, they quarry out a white stone, every part of which contains petrified, fishes in great numbers, and of surprising diversity. The} also seem to continue in such preservation, that their fins. * Phil. Trans, vol. ii. p. 427. t Buffon, vol. i. p. 407 x Phil. Trans, p. 426. THE EARTH. 33 scales, and all the minutest distinctions of their make, can be perfectly discerned.* From all these instances we may conclude, that fossils are very numerous ; and, indeed, independent of their situ- ation, they afford no small entertainment to observe them as preserved in the cabinets of the curious. The varieties of their kinds are astonishing. Most of the sea-shells which are known, and many others to which we are entirely strangers, are to be seen either in their natural state, or in various degrees of petrifaction.^ In the place of some we have mere spar, or stone, exactly expressing all the linea- ments of animals, as having been wholly formed from them. For it has happened, that the shells dissolving by very slow degrees, and the matter having nicely and exactly filled all the cavities within, this matter, after the shells have perished, has preserved exactly and regularly the whole print of their internal surface. Of these there are various kinds found in our pits ; many of them resembling those of our own shores ; and many others that are only to be found on the coasts of other countries. There are some shells re- sembling those that are never stranded upon our coasts but always remain in the deep : || and many more there are which we can assimulate with no shells that are known amongst us. But we find not only shells in our pits, but also fishes and corals in great abundance ; together with almost every sort of marine production. It is extraordinary enough, however, that the common red coral, though so very frequent at sea, is scarcely seen in the fossil world ; nor is there any account of its having ever been met with. But to compensate for this, there are all the kinds of the white coral now known, and many other kinds of that substance with which we are unac- quainted. Of animals there are various parts : the ver- tebrae of whales, and the mouths of lesser fishes; these, with teeth also of various kinds, are found in the cabinets of the curious ; where they receive long Greek names, which it is neither the intention nor the province of this work to enumerate. Indeed, few readers would think themselves much improved, should I proceed with enu- * Buffon, vol. i. p. 408. + Hill, p. 646. t Littorales. || Pelagii. VOL. I.— 2. E A HISTORY OF 34 merating the various classes of the Conicthyodontes, Po- lyleptoginglimi, or the Orthoceratites. These names, which mean no great matter when they are explained, may serve to guide in the furnishing a cabinet ; but they are of very little service in furnishing the page of instructive history. From all these instances we see in what abundance pe- trefactions are to be found ; and, indeed, Mr. Buffo n, to whose accounts we have added some, has not been sparing in the variety of his quotations, concerning the places where they are mostly to be found. However, I am sur- prised that he should have omitted the mention of one, which, in some measure, more than any of the rest, would have served to strengthen his theory. We are informed, by almost every traveller,* that has described the pyra- mids of Egypt, that one of them is entirely built of a kind of free-stone, in which these petrified shells are found in great abundance. This being the case, it may be conjec- tured, as we have accounts of these pyramids among the earliest records of mankind, and of their being built so long before the age of Herodotus, who lived but fifteen hun- dred years after the flood, that even the Egyptian priests could tell neither the time nor the cause of their erection ; I say, it may be conjectured that they were erected but a short time after the flood. It is not very likely, therefore, that the marine substances found in one of them, had time to be formed into a part of the solid stone, either during the deluge, or immediately after it ; and, conse- quently, their petrefaction must have been before that pe- riod, And this is the opinion Mr. Buffon has so strenu- ously endeavoured to maintain ; having given specious rea- sons to prove, that such shells were laid in the beds where they are now found, not only before the deluge, but even antecedent to the formation of man, at the time when the whole earth, as he supposes, was buried beneath a covering of waters. But while there are many reasons to persuade us that these extraneous fossils have been deposited by the sea, there is one fact that will abundantly serve to convince us, that the earth was habitable, if not inhabited, before these marine substances came to be thus deposited. For - Hasselqiust, Sarnlys. THE EARTH. 35 we find fossil-trees, which no doubt once grew upon the earth, as deep, and as much in the body of solid rocks, as these shells are found to be. Some of these fallen trees also have lain at least as long, if not longer, in the earth, than the shells, as they have been found sunk deep in a marly substance, composed of decayed shells and other marine productions. Mr. BufFon has proved, that fossil- shells could not have been deposited in such quantities all at once by the flood ; and I think, from the above instance, it is pretty plain, that, howsoever they were deposited, the earth was covered with trees before their deposition ; and, consequently, that the sea could not have made a very per- manent stay. How then shall we account for these extra- ordinary appearances in nature ? A suspension of all assent is certainly the first, although the most mortifying conduct. For my own part, were I to offer a conjecture, and all that has been said upon this subject is but conjecture, instead of supposing them to be the remains of animals belonging to the sea, I would consider them rather as bred in the numer- ous fresh-water lakes, that in primeval times covered the face of uncultivated nature. Some of these shells we know to belong to fresh waters ; some can be assimilated to none of the marine shells now known ;* why, therefore, may we not as w’ell ascribe the production of all to fresh waters, where we do not find them, as we do that of the latter to the sea only, where we never find them ? We know that lakes, and lands also, have produced animals that are now no longer existing ; why, therefore, might not these fossil productions be among the number? I grant that this is making a very harsh supposition ; but I cannot avoid thinking, that it is not attended with so many embarass- ments as some of the former, and that it is much easier to believe that these shells were bred in fresh water, than that the sea had for a long time covered the tops of the highest mountains. * Hill’s Fossils, p. 41 36 A HISTORY OF CHAP. VI. OF THE INTERNAL STRUCTURE OF THE EARTH. Having, in some measure, got free from the regions of conjecture, let us now proceed to a description of the earth as we find it by examination, and observe its in- ternal composition, as far as it has been the subject of ex- perience, or exposed to human inquiry. These inquiries, indeed, have been carried but to a very little depth below its surface, and even in that disquisition men have been conducted more by motives of avarice than of curiosity. The deepest mine, which is that at Cotteberg in Hungary,* reaches not more than three thousand feet deep ; but what proportion does that bear to the depth of the terrestrial globe, down to the centre, which is above four thousand miles ? All, therefore, that has been said of the earth, to a deeper degree, is merely fabulous or conjectural : we may suppose with one, that it is a globe of glass with another, a sphere of heated iron ; J with a third, a great mass of waters; || and with a fourth, one dreadful volcano but let us at the same time shew our consciousness, that all these are but suppositions. Upon examining the earth, where it has been opened to any depth, the first thing that occurs, is the different layers or beds of which it is composed ; these all lying horizontally one over the other, like the leaves of a book, and each of them composed of materials that increase in weight in proportion as they lie deeper. This is, in general, the disposition of the different materials, where the earth seems to have remained unmolested ; but this order is fre- quently inverted ; and we cannot tell whether from its ori- ginal formation, or from accidental causes. Of different substances, thus disposed, the far greatest part of our globe consists, from its surface downwards to the greatest depths we ever dig or mine.^[ The first layer, most commonly found at the surface, is that light coat of blackish mould, which is called by * Boyle, vol. iii. p. 240. f Buffon. J Whiston. || Burnet. § Kircher. Woodward, p. 9. THE EARTH. 37 some garden earth. With this the earth is every where in- vested, unless it be washed off by rains, or removed by some other external violence. This seems to have been formed from animal and vegetable bodies decaying, and thus turning into its substance. It also serves again as a storehouse, from whence animal and vegetable nature are renewed ; and thus are all vital blessings continued with unceasing circulation. This earth, however, is not to be supposed entirely pure, but is mixed with much stony and gravelly matter, from the layers lying immediately beneath it. It generally happens, that the soil is fertile in propor- tion to the quantity that this putrified mould bears to the gravelly mixture ; and as the former predominates, so far is the vegetation upon it more luxuriant. It is this ex- ternal covering that supplies man with all the true riches he enjoys. He may bring up gold and jewels from greater depths ; but they are merely the toys of a capricious being, things upon which he has placed an imaginary value, and for which fools alone part with the more substantial bless- ings of life. “ It is this earth,” says Pliny,* “ that, like a kind mother, receives us at our birth, and sustains us when born.” It is this alone, of all the elements around us, that is never found an enemy to man. The body of waters de- luge him with rains, oppress him with hail, and drown him with inundations. The air rushes in storms, prepares the tempest, or lights up the volcano ; but the earth, gentle and indulgent, ever subservient to the wants of man, spreads his walks with flowers, and his table with plenty ; returns with interest every good committed to her care ; and though she produces the poison, she still supplies the anti- dote ; though constantly teased more to furnish the luxuries of man than his necessities, yet, even to the last, she con- tinues her kind indulgence, and, when life is over, she piously covers his remains in her bosom. Phis external and fruitful layer which covers the earth, is, as was said, in a state of continual change. Vege- tables, which are naturally fixed and rooted to the same place, receive their adventitious nourishment from the sur- rounding earth and water ; animals, which change from place to place, are supported by these, or by each other. * 1’linii Historia Naturalis, lib. ii. cap. 63. A HISTORY OF 38 Both, however, having for a time enjoyed a life adapted to their nature, give back to the earth those spoils, which they had borrowed for a very short space, yet still to be quickened again into fresh existence. But the deposits they make are of very dissimilar kinds, and the earth is very differently enriched by their continuance : those countries that have for a long time supported men and other animals, having been observed to become every day more barren ; while, on the contrary, those desolate places, in which vegetables only are abundantly produced, are known to be possessed of amazing fertility. “ In regions which are uninhabited,” * says Mr. Buffon, “ where the forests are not cut down, and where animals do not feed upon the plants, the bed of vegetable earth is constantly increasing. In all woods, and even in those which are often cut, there is a layer of earth of six or eight inches thick, which has been formed by the leaves, branches, and bark, which fall and rot upon the ground. I have fre- quently observed on a Roman way, which crosses Bur- gundy, for a long extent, that there is a bed of black earth, of more than a foot thick, gathered over the stony pave- ment, on which several trees, of a very considerable size, are supported. This I have found to be nothing else than an earth formed by decayed leaves and branches, which have been converted by time into a black soil. Now as vegetables draw much more of their nourishment from the air and water than they do from the earth, it must follow, that in rotting upon the ground, they must give more to the soil than they have taken from it. Hence, therefore, in woods kept a long time without cutting, the soil be- low increases to a considerable depth ; and such we ac- tually find the soil in those American wilds, where the forests have been undisturbed for ages. But it is other- wise where men and animals have long subsisted: for as they make a considerable consumption of wood and plants, both for firing and other uses, they take more from the earth than they return to it ; it follows, therefore, that the bed of vegetable earth, in an inhabited country, must be always diminishing; and must at length resemble the soil of Arabia Petrea, and other provinces of the East, * Buffon, vol. i. p.353. THE EARTH. 39 which having been long inhabited, are now become plains of salt and sand ; the fixed salt always remaining, while the other volatile parts have flown away.” If from this external surface we descend deeper, and view the earth cut perpendicularly downwards, either in the banks of great rivers, or steepy sea-shores, or, going still deeper, if we observe it in quarries or mines, we shall find its layers regularly disposed in their proper order. We must not expect, however, to find them of the same kind or thickness in every place, as they differ in different soils and situations. Sometimes marl is seen to be over sand, and sometimes under it. The most common dis- position is, that under the first earth is found gravel or sand, then clay or marl, then chalk or coal, marbles, ores, sands, gravels ; and thus an alteration of these sub- stances, each growing more dense as it sinks deeper. The clay, for instance, found at the depth of a hundred feet, is usually more heavy than that found not far from the surface. In a well which was dug at Amsterdam, to the depth of two hundred and thirty feet, the following sub- stances were found in succession :* seven feet of vegetable earth, nine of turf, nine of soft clay, eight of sand, four of earth, ten of clay, four of earth, ten of sand, two of clay, four of white sand, one of soft earth, fourteen of sand, eight of clay mixed with sand, four of sea-sand mixed with shells, then a hundred and two feet of soft clay, and then thirty-one feet of sand. In a well dug at Marly, to the depth of a hundred feet Mr. Buffon gives us a still more exact enumeration of its layers of earth. “ Thirteen of a reddish gravel, two of gravel mingled with a vitrifiable sand, three of mud or slime, two of1 marl, four of marly stone, five of marl in dust mix- ed with vitrifiable sand, six of very fine vitrifiable sand,, three of earthy marl, three of hard marl, one of gravel, one of eglantine, a stone of the hardness and grain of marble, one of gravelly marl, one of stony marl, one of a coarser kind of stony marl, two of a coarser kind still, one of vi- trifiable sand mixed with fossil-shells, two of fine gravel, three of stony marl, one of coarse powdered marl, one of stone calcinable like marble, three of gray sand, two of white sand, one of red sand streaked with white, eight of * Varenius, as quoted by Mr. Buffon, p. 358. 40 A HISTORY OF gray sand with shells, three of very fine sand, three of a hard gray stone, four of red sand streaked with white, three of white sand, and fifteen of reddish vitrifiable sand. In this manner the earth is every wrhere found in beds over beds ; and, what is still remarkable, each of them, as far as it extends, always maintains exactly the same thick- ness. It is found also, that as we proceed to considerable depths, every layer grows thicker. Thus in the adduced instances we might have observed, that the last layer was fifteen feet thick, while most of the others were not above eight ; and this might have gone much deeper, for aught we can tell, as before they got through it the workmen ceased digging. These layers are sometimes very extensive, and often are found to spread over a space of some leagues in circumfer- ence. But it must not be supposed that they are uni- formly continued over the whole globe without any inter- ruption : on the contrary, they are ever, at small intervals, cracked through as it were by perpendicular fissures ; the earth resembling, in this respect, the muddy bottom of a pond, from whence the water has been dried off by the sun, and thus gaping in several chinks, which descend in a direction perpendicular to its surface. These fissures are many times found empty, but oftener closed up with ad- ventitious substances, that the rain, or some other acciden- tal causes, have conveyed to fill their cavities. Their open- ings are not less different than their contents, some being not above half an inch wide, some a foot, and some several hundred yards asunder. Which last form those dreadful chasms that are to be found in the Alps, at the edge of which the traveller stands dreading to look down at the immeasurable gulph below. These amazing clefts are well known to such as have past these mountains, where a chasm frequently presents itself several hundred feet deep, and as many over, at the edge of which the way lies. It often happens also, that the road leads along the bottom, and then the spectator observes on each side frightful pre- cipices several hundred yards above him ; the sides of which correspond so exactly with each other, that they evidently seem torn asunder. But these chasms, to be found in the Alps, are nothing to what Ovalle tells us are to be seen in the Andes. These 'THE EARTH. 41 amazing mountains, in comparison of which the former are but little hills, have their fissures in proportion to their greatness. In some places they are a mile wide, and deep in proportion ; and there are some others, that, running under ground, in extent resemble a province. Of this kind also is that cavern called Eldenhole, in Der- byshire, which Dr. Plott tells us, was sounded by a line of eight and twenty hundred feet, without finding the bottom, or meeting with water : and yet the mouth at the top is not above forty yards over.* This immeasurable cavern runs perpendicularly downward ; and the sides of it seem to tally so plainly as to shew that they once were united. Those who come to visit the place, generally procure stones to be thrown into its mouth; and these are heard for several minutes, falling and striking against the sides of the cavern, producing a sound that resembles distant thunder, dying away as the stone goes deeper. Of this kind also is that dreadful cavern described by iElian ; his account of which the reader may not have met with.'f~ “ In the country of the Arrian Indians, is to be seen an amazing chasm, which is called, The Gulph of Pluto . The depth and the recesses of this horrid place are as extensive as they are unknown. Neither the na- tives, nor the curious who visit it, are able to tell how it was first made, or to what depths it descends. The Indians continually drive thither great multitudes of animals, more than three thousand at a time, of different kinds, sheep* horses, and goats ; and, with an absurd superstition, force them into the cavity, from whence they never return. Their several sounds, however, are heard as they descend; the bleating of sheep, the lowing of oxen, and the neighing of horses, issuing up to the mouth of the cavern. Nor do these sounds cease, as the place is continually furnished with a fresh supply.” There are many more of these dreadful perpendicular fissures in different parts of the earth ; with accounts of which, Kircher, Gaffarellus, and others, who have given histories of the wonders of the subterranean world, abun- dantly supply us. The generality of readers, however. * Phil. Trans, vol. ii. p. 370. t Jiliani Var. Hist. lib. xvi. cap. 16 F VOL. I. — 2. A HISTORY OP 42 will consider them with less astonishment when they are informed of their being common all over the earth ; that in every field, in every quarry, these perpendicular fissures are to be found, either still gaping, or filled with matter that has accidently closed their interstices. The inat- tentive spectator neglects the inquiry, but their being com- mon is partly the cause that excites the philosopher’s at- tention to them ; the irregularities of nature he is often content to let pass unexamined ; but when a constant and a common appearance presents itself, every return of the object is a fresh call to his curiosity ; and the chink in the next quarry becomes as great a matter of wonder as the chasm in Eldenhole. Philosophers have long, therefore, endeavoured to find out the cause of these perpendicular fissures, which our own countrymen, Woodward and Ray, were the first that found to be so common and universal. Mr. BufFon supposes them to be cracks made by the sun, in drying up the earth, immediately after its emersion from the deep. The heat of the sun is very probably a principal cause ; but it is not right to ascribe to one only, what we find may be the result of many. Earthquakes, severe frosts, bursting waters, and storms tearing up the roots of trees, have, in our own times, produced them ; and to this variety of causes we must, at present, be con- tent to assign those that have happened before we had opportunities for observation. CHAP. VII. OF CAVES AND SUBTERRANEOUS PASSAGES THAT SINK, BUT NOT PERPENDICULARLY, INTO THE EARTH. In surveying the subterranean wonders of the globe, besides those fissures that descend perpendicularly, we fre- quently find others that descend but a little way, and then spread themselves often to a great extent below the surface. Many of these caverns, it must be confessed, may be the production of art and human industry; retreats made to protect the oppressed, or shelter the spoiler. The famous labyrinth of Candia, for instance, is supposed to be entirely the work of art. Mr. Tournefort assures us, that it bears the impression of human industry, and that great pains THE EARTH 43 have been bestowed upon its formation. The stone-quarry of Maestricht is evidently made by labour : carts enter at its mouth, and load within, then return, and discharge their freight into boats that lie on the brink of the river Maese. This quarry is so large, that forty thousand peo- ple may take shelter in it : and it in general serves for this purpose, when armies march that way ; becoming then an impregnable retreat to the people that live thereabout. Nothing can be more beautiful than this cavern, when lighted up with torches : for there are thousands of square pillars, in large level walks, about twenty feet high ; and all wrought with much neatness and regularity. In this vast grotto there is very little rubbish ; which shews both the goodness of the stone and the carefulness of the work- men. To add to its beauty, there also are, in various parts of it, little pools of water, for the convenience of the men and cattle. It is remarkable also, that no droppings are seen to fall from the roof, nor are the walks any way wet under foot, except in cases of great rains, where the water gets in by the air-shafts. The salt mines in Poland are still more spacious than these. Some of the cata- combs, both in Egypt and Italy, are said to be very ex- tensive. But no part of the world has a greater number of artificial caverns than Spain, which were made to serve as retreats to the Christians against the fury of the Moors, when the latter conquered that country. How- ever, an account of the works of art does not properly be- long to a natural history. It will be enough to observe, that though caverns be found in every country, far the greatest part of them have been fashioned by the hand of nature only. Their size is found beyond the power of man to have effected, and their forms but ill adapted to the conveniences of a human habitation. In some places, indeed, we find mankind still make use of them as houses ; particularly in those countries where the climate is very severe but in general they are deserted by every race of meaner animals, except the bat ; these nocturnal solitary creatures are usually the only inhabitants ; and these only in such whose descent is sloping, or, at least, not directly perpendicular. * Phil. Trans, vol. ii. p. 36S. A HISTORY OF 44 There is scarcely a country in the world without its na- tural caverns ; and many new ones are discovered every day. Of those in England, Oakey-hole, the Devil’s -hole, and Penpark-hole, have been often described. The former, which lies on the south side of Mendip-hills,* within a mile of the town of Wells, is much resorted to by travel- lers. To conceive a just idea of this, we must imagine a precipice of more than a hundred yards high, on the side of a mountain which shelves away a mile above it. In this is an opening not very large, into which you enter, going along upon a rocky uneven pavement, sometimes ascending, and sometimes descending. The roof of it, as you advance, grows higher; and, in some places, is fifty feet from the floor. In some places, however, it is so low that a man must stoop to pass. It extends itself, in length, about two hundred yards: and from every part of the roof and the.floor, there are formed sparry concretions of various figures, that by strong imaginations have been likened to men, lions, and organs. At the farthest part of this cavern rises a stream of water, well stored with fish, large enough to turn a mill, and which discharges itself near the entrance. Penpark-hole, in Gloucestershire, is almost as remarkable as the former. Captain Sturmy descended into this by a rope, twenty-five fathoms perpendicular, and at the bottom found a very large vault in the shape of a horse- shoe. The floors consisted of a kind of white stone enamelled with lead ore, and the pendant rocks were glazed with spar. Walking forward on this stony pavement, for some time, he came to a great river, twenty fathoms broad, and eight fathoms deep ; and having been informed that it ebbed and flowed with the sea, he remained in this gloomy abode for five hours, to make an exact observation. He did not find, however, any alteration whatsoever in its appear- ance. But his curiosity was ill requited ; for it cost this unfortunate gentleman his life : immediately after his return he was seized with an unusual and violent head- ache, which threw him into a fever, of which he died soon after. But of all the subterranean caverns now known, the * Phil. Trans, vol. ii. p. 368. THE EARTH. 45 grotto of Antiparos is the most remarkable, as well for its extent as for the beauty of its sparry incrustations. This celebrated cavern was first discovered by one Magni, an Italian traveller, about an hundred years ago, at Antipa- ros, an inconsiderable island of the Archipelago.* The account he gives of it is long and inflated, but upon the whole amusing. “ Having been informed,” says he, “ by the natives of Paros, that in the little island of Antiparos, which lies about two miles from the former, of a gigantic statue that was to be seen at the mouth of a cavern in that place, it was resolved that we (the French consul and himself) should pay it a visit. In pursuance of this re- solution, after we had landed on the island, and walked about four miles through the midst of beautiful plains, and sloping woodlands, we at length came to a little hill, on the side of which yawned a most horrid cavern, that with its gloom at first struck us with terror, and almost represt curiosity. Recovering the first surprise, however, we entered boldly ; and had not proceeded above twenty paces, when the supposed statue of the giant presented itself to our view. We quickly perceived, that what the ignorant natives had been terrified at as a giant, was no- thing more than a sparry concretion, formed by the water dropping from the roof of the cave, and by degrees hard- ening into a figure that their fears had formed into a mon- ster. Incited by this extraordinary appearance, we were induced to proceed still farther, in quest of new adventures in this subterranean abode. As we proceeded, new wonders offered themselves ; the spars, formed into trees and shrubs, presented a kind of petrified grove ; some white, some green ; and all receding in due perspective. They struck us with the more amazement, as we knew them to be mere productions of Nature, who, hitherto in solitude, had, in her playful moments, dressed the scene as if for her own amusement. But we had as yet seen but a few of the wonders of the place ; and were introduced only into the portico of this amazing temple. In one corner of this half-illumi- nated recess, there appeared an opening of about three de?c ^h*nd. sub. 112. I have translated a part of Ivircher’s an hvn T’ -ather t^ian ^ ournefort’s, as the latter was written to support A HISTORY OF 46 feet wide, which seemed to lead to a place totally dark, and that, one of the natives assured us, contained nothing more than a reservoir of water. Upon this we tried, by throwing down some stones, which rumbling along the sides of the descent for some time, the sound seemed at last quashed in a bed of water. In order, however, to be more certain, we sent in a Leventine mariner, who, by the promise of a good reward, with a flambeaux in his hand, ventured into this narrow aperture. After continuing within it for about a quarter of an hour, he returned, carrying some beautiful pieces of white spar in his hand, which art could neither imitate nor equal. Upon being informed by him that the place was full of these beautiful incrustations, I ventured in once more with him for about fifty paces, anxiously and cautiously descending by a steep and danger- ous way. Finding, however, that we came to a precipice which led into a spacious amphitheatre, if I may so call it, still deeper than any other part, we returned, and being provided with a ladder, flambeaux, and other things to expedite our descent, our whole company, man by man, ventured into the same opening, and descending one after another, we at last saw ourselves altogether in the most magnificent part of the cavern. “ Our candles being now all lighted up, and the whole place completely illuminated, never could the eye be pre- sented with a more glittering, or a more magnificent scene. The roof all hung with solid icicles, transparent as glass, yet solid as marble. The eye could scarcely reach the lofty and noble ceiling; the sides were regularly formed with spars ; and the whole presented the idea of a magni- ficent theatre, illuminated with an immense profusion of lights. The floor consisted of solid marble ; and in seve- ral places magnificent columns, thrones, altars, and other objects appeared, as if nature had designed to mock the curiosities of art. Our voices, upon speaking or singing, were redoubled to an astonishing loudness ; and upon the firing of a gun, the noise and reverberations were almost deafening. In the midst of this grand amphitheatre rose a concretion of about fifteen feet high, that, in some mea- sure, resembled an altar ; from which, taking the hint, we caused mass to be celebrated there. The beautiful co- lumns that shot up round the altar, appeared like candle- THE EARTH. 47 sticks ; and many other natural objects represented the customary ornaments of this sacrament. “ Below even this spacious grotto there seemed another cavern ; down which I ventured with my former mariner, and descended about fifty paces by means of a rope. I at last arrived at a small spot of level ground, where the bot- tom appeared different from that of the amphitheatre, being composed of a soft clay, yielding to the pressure, and in which I thrust a stick to about six feet deep. In this however, as above, numbers of the most beautiful crys- tals were formed, one of which particularly resembled a table. Upon our egress from this amazing cavern, we perceived a Greek inscription upon a rock at the mouth, but so obliterated by time that we could not read it. It seemed to import that one Antipater, in the time of Alex- ander, had come thither ; but whether he had penetrated into the depths of the cavern, he does not think fit to in- form us.” Such is the account of this beautiful scene, as commu- nicated in a letter to Kircher. We have another, and a more copious description of it, by Tournefort, which is in every body’s hands ; hut I have given the above, both be- cause it was communicated by the first discoverer, and because it is a simple narrative of facts, without any rea- soning upon them. According to Tournefort’s account, indeed, we might conclude, from the rapid growth of the spars in this grotto, that it must every year be growing narrower, and that it must in time be choaked up with them entirely; but no such thing has happened hitherto, and the grotto at this day continues as spacious as we ever knew it. This is not a place for an inquiry into the seeming ve- getation of those stoney substances, with which this and almost every cavern are incrusted : it is enough to observe, m general, that they are formed by an accumulation of that little gritty matter which is carried thither by the waters, and which in time acquires the hardness of marble. What in this place more imports us to know is, how these amazing hollows in the earth came to be formed. And I think, in the three instances above mentioned, it is pretty evident, that their excavation has been owing to water. These finding subterraneous passages under the earth, and by A HISTORY^ OF 48 long degrees hollowing the beds in which they flowed, the ground above them has slipt down closer to their surface, leaving the upper layers of the earth or stone still sus- pended : the ground that sinks upon the face of the waters forming the floor of the cavern ; the ground or rock, that keeps suspended, forming the roof : and, indeed, there are but few of these caverns found without water, either within them, or near enough to point out their formation. CHAP. VIII. OF MINES, DAMPS, AND MINERAL VAPOURS. The caverns, which we have been describing, generally carry us but a very little way below the surface of the earth. Two hundred feet, at the utmost, is as much as the lowest of them is found to sink. The perpendicular fissures run much deeper ; but few persons have been bold enough to venture down to their deepest recesses ; and some few who have tried, have been able to bring back no tidings of the place, for unfortunately they left their lives below. The excavations of art have conducted us much farther into the bowels of the globe. Some mines in Hungary are known to be a thousand yards perpendicular downwards ; and I have been informed, by good authority, of a coal- mine in the north of England, an hundred yards deeper still. It is beside our present purpose to inquire into the pe- culiar contrivance and construction of these, which more properly belongs to the history of fossils. It will be suf- ficient to observe in this place, that as we descend into the mines, the various layers of earth are seen as we have al- ready described them ; and in some of these are always found the metals or minerals for which the mine has been dug. Thus frequently gold is found dispersed and mixed with clay and gravel ;* sometimes it is mingled with other metallic bodies, stones, or bitumens and sometimes united with that most obstinate of all substances, platina, from which scarce any art can separate it. Silver is * Ulloa, vol. ii. p. 470. t Ulloa, ibid. THE EARTH. 49 sometimes found quite pure,* sometimes mixed with other substances and minerals. Copper is found in beds mixed with various substances, marbles, sulphurs, and pyrites. Tin, the ore of which is heavier than that of any other metal, is generally found mixed with every kind of matter lead is also equally common ; and iron we well know can be ex- tracted from all the substances upon earth. The variety of substances which are thus found in the bowels of the earth, in their native state, have a very different appearance from what they are afterwards taught to assume by human industry. The richest metals are very often less glittering and splendid than the most useless marcasites ; and the basest ores are generally the most beautiful to the eye. This variety of substances, which compose the internal parts of our globe, is productive of equal varieties, both above and below its surface. The combination of the different minerals with each other, the heats which arise from their mixture, the vapours they diffuse, the fires which they generate, or the colds which they sometimes produce, are all either noxious or salutary to man ; so that in this great elaboratory of nature, a thousand benefits and calamities are forging, of which we are wholly unconscious ; and it is happy for us that we are so. Upon our descent into mines of considerable depth, the cold seems to increase from the mouth as we descend but after passing very low down, we begin by degrees to come into a warmer air, which sensibly grows hotter as we go deeper, till, at last, the labourers can scarcely bear any covering as they continue working. This difference in the air was supposed by Boyle to pro- ceed from magazines of fire that lay nearer the centre, and that diffused their heat to the adjacent regions. But we now know that it may be ascribed to more obvious causes. In some mines, the composition of the earth all around is of such a nature, that, upon the admission of water or air, it requently becomes hot, and often bursts out into eruptions, i esi es ^ lls> as the external air cannot readily reach the o om, 01 be renewed there, an observable heat is perceived Macquer’s Chymistry, vol. i. p. 316. f Hill’s Fossils, p. 623. + Boyle, vol. iii. p. 232. G VOL. I. 2. A HISTORY OF 50 below, without the necessity of recurring to the central heat for an explanation. Hence, therefore, there are two principal causes of the warmth at the bottom of mines : the heat of the sub- stances of which the sides are composed ; and the want of renovation in the air below. Any sulphureous sub- stance, mixed with iron, produces a very great heat, by the admission of water. If, for instance, a quantity of sulphur be mixed with a proportionable share of iron fil- ings, and both kneaded together into a soft paste, with water, they will soon grow hot, and at last produce a flame. This experiment, produced by art, is very com- monly effected within the bowels of the earth by nature. Sulphurs and irons are intimately blended together, and want only the mixture of water or air to excite their heat ; and this, when once raised, is communicated to all bodies that lie within the sphere of their operation. Those beau- tiful minerals called marcasites and pyrites , are often of this composition ; and wherever they are found, either by imbibing the moisture of the air, or having been bv any means combined with water, they render the mine consi- derably hot.* The want of fresh air also, at these depths, is, as we have said, another reason for their being found much hot- ter. Indeed, without the assistance of art, the bottom of most mines would, from this cause, be insupportable. To remedy this ^inconvenience, the miners are often obliged to sink, at some convenient distance from the mouth of the pit where they are at work, another pit, which joins the former below, and which, in Derbyshire, is called an air- shaft. Through this the air circulates ; and thus the workmen are enabled to breathe freely at the bottom of the place ; which becomes, as Mr. Boyle affirms, very commodious for respiration, and also very temperate as to heat and cold.-f- Mr. Locke, however, who has left us an account of the Mendip mines, seems to present a dif- ferent picture. “ The descent into these is exceedingly difficult and dangerous ; for they are not sunk like wells, perpendicularly, but as the crannies of the rocks happen to run. The constant method is to swing down by a rope * Kircher Mund. Subt. vol. ii. p. 216. f Boyle, vol. iii. p. 238. THE EARTH. 51 placed under the arms, and clamber along by applying both feet and bands to the sides of the narrow passage. The air is conveyed into them through a little passage that runs along the sides from the top, where they set up some turfs, on the lee-side of the hole, to catch and force it down. These turfs being removed to the windy side, or laid over the mouth of the hole, the miners below presently want breath, and faint ; and if sweet-smelling flowers chance to be placed there, they immediately lose their fragrancy, and stink like carrion.” An air so putrifying can never be very commodious for respiration. Indeed, if we examine the complexion of most miners, we shall be very well able to form a judgment of the un- wliolesomeness of the place where they are confined. Their pale and sallow looks shew how much the air is damaged by passing through those deep and winding- ways, that are rendered humid by damps, or warmed with noxious exhalations. But although every mine is unwhole- some, all are not equally so. Coal-mines are generally less noxious than those of tin ; tin than those of copper ; but none are so dreadfully destructive as those of quicksilver. At the mines near the village of Idra, nothing can ade- quately describe the deplorable infirmities of such as fill the hospital there ; emaciated and crippled, every limb contracted or convulsed, and some in a manner transpiring quicksilver at every pore. There was one man, says Dr. Pope,* who was not in the mines above half a year, and yet whose body was so impregnated with this mineral, that putting a piece of brass money in his mouth, or lubbing it between his fingers, it immediately became as white as if it had been washed over with quicksilver. In this manner all the workmen are killed sooner or later; first becoming paralytic, and then dying consumptive : and all this they sustain for the trifling reward of seven pence a day. But these metallic mines are not so noxious from their own vapours, as from those of the substances with which the ores are usually united, sucn as arsenic, cinnabar, bitumen, or vitriol. From the fumes of these, variously combined, and kept inclosed, are produced those various * Phil. Trans, vol. ii. p. 573. 52 A HISTORY OF damps, that put on so many dreadful forms, and are usu- ally so fatal. Sometimes those noxious vapours are per- ceived by the delightful fragrance of their smell,* some- what resembling the pea-blossom in bloom, from whence one kind of damp has its name. The miners are not de- ceived, however, by its flattering appearances ; but as they have thus timely notice of its coming, they avoid it while it continues, which is generally during the whole summer season. Another shews its approach by the burning of the candles, which seem to collect their flame into a globe of light, and thus gradually lessen, till they are quite extinguished. From this, also, the miners fre- quently escape ; however, such as have the misfortune to be caught in it, either swoon away, and are suffocated, or slowly recover in excessive agonies. Here also is a third, called the fulminating damp, much more dangerous than either of the former, as it strikes down all before it like a flash of gunpowder, without giving any warning of its approach. But there is another, more deadly than all the rest, which is found in those places where the vapour has been long confined, and has been, by some accident, set free. The air rushing out from thence, always goes upon deadly errands : and scarce any escape to describe the symp- toms of its operations. Some colliers in Scotland, working near an old mine that had been long closed up, happened, inadvertently, to open a hole into it, from the pit where they were then em- ployed. By great good fortune, they at that time per- ceived their error, and instantly fled for their lives. The next day, however, they were resolved to renew their work in the same pit, and eight of them ventured down, without any great apprehensions ; but they had scarcely got to the bottom of the stairs that led to the pit, but, coming within the vapour, they all instantly dropped down dead, as if they had been shot. Amongst these unfortunate poor men, there was one whose wife was in- formed he was stifled in the mine ; and, as he happened to be next the entrance, she so far ventured down as to see where he lay. As she approached the place, the sight of her husband inspired her with a desire to rescue * * Phil. Trans, vol. ii. p. 375. THE EARTH. 53 him, if possible, from that dreadful situation ; though a little reflection might have shown her it was then too late. But nothing could deter her ; she ventured forward, and had scarce touched him with her hand, when the damp prevailed, and the misguided, but faithful creature, fell dead by his side. Thus, the vapours found beneath the surface of the earth are very various in their effects upon the constitution : and they are not less in their appearances. There are many kinds that seemingly are no way prejudicial to health, but in which the workmen breathe freely ; and yet in these, if a lighted candle be introduced, they immediately take fire, and the whole cavern at once becomes one furnace of flame. In mines, therefore, subject to damps of this kind, they are obliged to have recourse to a very peculiar contrivance to supply sufficient light for their operations. This is by a great wheel ; the circumference of which is beset with flints, which striking against steels placed for that purpose at the extremity, a stream of fire is produced, which affords light enough, and yet which does not set fire to the mineral vapour. Of this kind are the vapours of the mines about Bristol : on the contrary, in other mines, a single spark struck out from the collision of flint and steel, would set the whole shaft in a flame. In such, therefore, every precaution is used to avoid a collision ; the workmen making use only of wooden instruments in digging ; and being cautious, before they enter the mine, to take out even the nails from their shoes. Whence this strange difference should arise, that the vapours of some mines catch fire with a spark, and others only with a flame, is a question that we must be content to leave in obscurity, till we know more of the nature both of mineral vapour and of fire. This only we may observe, that gunpowder will readily fire with a spark, but. not with the flame of a candle; on the other hand, spirits of wine will flame with a candle, but not with a spark : ut even here the cause of this difference as vet remains a secret. As from this account of mines, it appears that the in- ternal parts of the globe are filled with vapours of various 111 ,s’ ^ *s 110t surprising that they should, at different times, reac 1 the surface, and there put on various appearances. A HISTORY OF 54 In fact, much of the salubrity, and much of the unwhole- someness, of climates and soils, is to be ascribed to these vapours, which make their way from the bowels of the earth upwards, and refresh or taint the air with their exhalations. Salt mines, being naturally cold,* send forth a degree of coldness to the external air, to comfort and refresh it : on the contrary, metallic mines are known, not only to warm it with their exhalations, but often to destroy all kinds of vegetation by their volatile corrosive fumes. In some mines, dense vapours are plainly perceived issuing from their mouths, and sensibly warm to the touch. In some places, neither snow nor ice will continue on the ground that covers a mine ; and over others the fields are found destitute of verdure. -f- The inhabitants, also, are rendered dreadfully sensible of these subterraneous 'exhalations, being affected with such a variety of evils proceeding entirely from this cause, that books have been professedly written upon this class of disorders. Nor are these vapours, which thus escape to the sur- face of the earth, entirely unconfined ; for they are fre- quently, in a manner, circumscribed to a spot. The grotto Del Cane, near Naples, is an instance of this ; the noxious effects of which have made that cavern so very famous. This grotto, which has so much employed the attention of travellers, lies within four miles of Naples, and is situated near a large lake of clear wholesome water. ^ Nothing can exceed the beauty of the landscape which this lake affords ; being surrounded with hills covered with forests of the most beautiful verdure, and the whole bearing a kind of amphitheatrical appearance. However, this region, beautiful as it appears, is almost entirely unin- habited ; the few peasants that necessity compels to reside there, looking quite consumptive and ghastly, from the poisonous exhalations that rise from the earth. The famous grotto lies on the side of a hill, near which place a peasant ‘ resides, who keeps a number of dogs for the purpose of shewing the experiment to the curious. These poor animals always seem perfectly sensible of the ap- proach of a stranger, and endeavour to get out of the way. However, their attempts being perceived, they are * Phil. Trans, vol. ii. p. 523 t Boyle, Vol. iii. p. 238 \ Kircher, Mund, Subt. vol. i. p. 101. THE EARTH. taken and brought to the grotto ; the noxious effects of which they have so frequently experienced. Upon entering this place, which is a little cave, or hole rather, dug into the hill, about eight feet high, and twelve feet long, the ob- server can see no visible mark of its pestilential vapour ; only to about a foot from the bottom, the wall seems to be tinged with a colour resembling that which is given by stagnant waters. When the dog, this poor philosophical martyr, as some have called him, is held above this mark, he does not seem to feel the smallest inconvenience ; but when his head is thrust down lower, he struggles to get free for a little ; but in the space of four or five minutes he seems to lose all sensation, and is taken out seemingly without life. Being plunged in the neighbouring lake, he quickly recovers, and is permitted to run home, seemingly without the smallest injury. This vapour, which thus for a time suffocates, is of the humid kind, as it extinguishes a torch, and sullies a look- ing-glass ; but there are other vapours perfectly inflam- mable, and that only require the approach of a candle to set them blazing. Of this kind was the burning well at Brosely, which is now stopped up ; the vapour of which, when a candle was brought within about a foot of the surface of the water, caught flame like spirits of wine, and continued blazing for several hours after. Of this kind, also, are the perpetual fires in the kingdom of Persia. In that province, where the worshippers of fire hold their chief mysteries, the whole surface of the earth, for some extent, seems impregnated with inflammable vapours. A reed stuck into the ground continues to burn like a flambeau ; a hole made beneath the surface of the earth, instantly becomes a furnace, answered all the purposes of a culinary fire. There they make lime by merely burying the stones in the earth ; and watch with veneration the appearances of a flame that has not been extinguished for times immemorial. Plow different are men in various climates ! This deluded people worship these vapours as a deity, which in other parts of the world are considered as one of the greatest evils. 6 56 A HISTORY OF CHAP. IX, OF VOLCANOES AND EARTHQUAKES. Mines and caverns, as we have said, reach but a very little way under the surface of the earth, and ue have hi- therto had no opportunities of exploring further. With- out all doubt, the wonders that are still unknown surpass those that have been represented, as there are depths of thousands of miles which are hidden from our inquiry. The only tidings we have from those unfathomable regions are by means of volcanoes, those burning mountains that seem to discharge their materials from the lowest abysses of the earth.* A volcano may be considered as a cannon of immense size, the mouth of which is often near two miles in circumference. From this dreadful aperture are discharged torrents of flame and sulphur, and rivers of melted metal. Whole clouds of smoke and ashes, with rocks of enormous size, are discharged to many miles dis- tance; so that the force of the most powerful artillery, is but as a breeze agitating a feather in comparison. In the deluge of fife and melted matter which runs down the sides of the mountain, whole cities are sometimes swallowed up and consumed. Those rivers of liquid fire are sometimes two hundred feet deep ; and, when they harden, frequently form considerable hills. Nor is the danger of these confined to the eruption only: but the force of the internal fire struggling for vent, frequently produces earthquakes through the whole region where the volcano is situated. So dread- ful have been these appearances, that men’s terrors have added new horrors to the scene, and they have regarded as prodigies, what we know to be the result of natural causes. Some philosophers have considered them as vents com- municating with the fires of the centre ; and the ignorant, as the mouths of hell itself. Astonishment produces fear, and fear superstition : the inhabitants of Iceland believe the bellowings of Hecla are nothing else but the cries of the damned, and that its eruptions are contrived to increase their tortures. * Buffon, vol. i. p. 291. THE EARTH. 57 But if we regard this astonishing scene of terror with a more tranquil and inquisitive eye, we shall find that these conflagrations are produced by very obvious and natural causes. We have already been apprised of the various mineral substances in the bosom of the earth, and their aptness to burst out into flames. Marcasites and pyrites, in particular, by being humified with water or air, con- tract this heat, and often endeavour to expand with irre- sistible explosion. These, therefore, being lodged in the depths of the earth, or in the bosom of mountains, and being either washed by the accidental influx of waters below, or fanned by air, insinuating itself through per- pendicular fissures from above, take fire at first by only heaving in earthquakes, but at length by bursting through every obstacle, and making their dreadful discharge in a volcano. These volcanoes are found in all parts of the earth : In Europe there are three that are very remarkable ; AEtna in Sicily, Vesuvius in Italy, and Hecla in Iceland. iEtna has been a volcano for ages immemorial. Its eruptions are very violent, and its discharge has been known to cover, for a certain space around, eighty-six feet deep. In the year 1537, an eruption of this mountain produced an earth- quake through the whole island for twelve days, overturned many houses, and at last formed a new aperture, which overwhelmed all within five leagues round. The cinders thrown up were driven even into Italy, and its burnings were seen at Malta, at the distance of sixty leagues. “ There is nothing more awful,” says Kircher, “ than the eruptions of this mountain, nor nothing more dangerous than attempting to examine its appearances, even long after the eruption has ceased. As we attempt to clamber up its steepy sides, every step we take upwards, the feet sink back half way. Upon arriving near the summit, ashes and snow, with an ill-assorted conjunction, present nothing but objects of desolation. Nor is this the worst, for, as all places are covered over, many caverns are en- tirely hidden from the sight, into which, if the inquirer happens to fall, he sinks to the bottom, and meets inevita- ble destruction. Upon coming to the edge of the great crater, nothing can sufficiently represent the tremendous magnificence of the scene. A gulph two miles over, and so VOL. I.— 3. H A HISTORY OF 58 deep that no bottom can be seen ; on the sides pyramidical rocks starting out between apertures that emit smoke and flame ; all this accompanied with a sound that never ceases, louder than thunder, strikes the bold with horror, and the religious with veneration for him that has power to control its burnings.” In the descriptions of Vesuvius or Hecla, we shall find scarcely any thing but a repetition of the same terrible objects, but rather lessened, as these mountains are not so large as the former. The crater of Vesuvius is but a mile across, according to the same author ; whereas that of iEtna is two. On this particular, however, we must place no dependence, as these caverns every day alter; being lessened by the mountain’s sinking in at one erup- tion, and enlarged by the fury of another. It is not one of the least remarkable particulars respecting Vesuvius, that Pliny the naturalist was suffocated in one of its eruptions ; for his curiosity impelled him too near, he found himself involved in smoke and cinders when it was too late to retire; and his companions hardly escaped to give an ac- count of the misfortune. It was in that dreadful eruption that the city of Herculaneum was overwhelmed ; the ruins of which have lately been discovered at sixty feet distance below the surface, and, what is still more remarkable, forty feet below the bed of the sea. One of the most remarkable eruptions of this mountain was in the year 1707, which is finely described by Valetta ; a part of whose description 1 shall beg leave to translate. “ Towards the latter end of summer, in the year 1707, the mount Vesuvius, that had for a long time been silent, now began to give some signs of commotion. Little more than internal murmurs at first were heard, that seemed to contend within the lowest depths of the mountain ; no flame, nor even any smoke, was as yet seen. Soon after some smoke appeared by day, and a flame by night, which seemed to brighten all the campania. At intervals, also, it shot off substances with a sound very like that of artillery, but which, even at so great a distance as we were at, infinitely exceeded them in greatness. Soon after - it began to throw up ashes, which becoming the sport of the winds, fell at great distances, and some many miles. To this succeeded showers of stones, which killed many THE EARTH, 59 of tne inhabitants of the valley, but made a dreadful ravage among the cattle. Soon after a torrent 'of burning matter began to roll down the sides of the mountain, at first with a slow and gentle motion, but soon with increased celerity. The matter thus poured out, when cold, seemed upon inspection to be of vitrified earth, the whole united into a mass of more than stony hardness. But what was particularly observable was, that upon the whole surface of these melted materials, a light spongy stone seemed to float, while the lower body was of the hardest substance of which our roads are usually made. Hitherto there were no appearances but what had been often remarked before ; but on the third or fourth day, seeming flashes of lightning were shot forth from the mouth of the mountain, with a noise far exceeding the loudest thunder. These flashes, in colour and brightness, resembled what we usually see in tempests, but they assumed a more twisted and serpentine form. After this followed such clouds of smoke and ashes, that the whole city of Naples, in the midst of the day, was involved in nocturna* darkness, and the nearest friends were unable to distinguish each other in this frightful gloom. If any person attempted to stir out without torch-light, he was obliged to return, and every part of the city was filled with supplications and terror.’ At length, after a continuance of some hours, about one o’clock at midnight, the wind blowing from the north, the stars began to be seen ; the heavens, though it was night, began to grow brighter; and the eruptions, after a con- tinuance of fifteen days, to lessen. The torrent of melted matter was seen to extend from the mountain down to the shore ; the people began to return to their former dwellings, and the whole face of nature to resume its former appearance.” The famous Bishop Berkeley gives an account of one of these eruptions in a manner something different from the former.* “ In the year 1717, and the middle of April, with much difficulty I reached the top of Mount Vesuvius, in which I saw a vast aperture full of smoke, which hin- dered me from seeing its depth and figure. I heard within that horrid gulph certain extraordinary sounds, which * Phil. Trans, vol. ii. p. 209. 60 A HISTORY OF seemed to proceed from the bowels of the mountain, a sort of murmuring, sighing, dashing sound ; and, between whiles, a noise like that of thunder or cannon, with a clattering like that of tiles falling from the tops of houses into the streets. Sometimes, as the wind changed, the smoke grew thinner, discovering a very ruddy flame, and the circumference of the crater streaked with red and se- veral shades of yellow. After an hour’s stay, the smoke, being moved by the wind, gave us short and partial pros- pects of the great hollow ; in the flat bottom of which I could discern two furnaces almost contiguous ; that on the left seeming about three yards over, glowing with ruddy flame, and throwing up red-hot stones with a hideous noise, which, as they fell back, caused the clattering already taken notice of. — May 8, in the morning, I ascended the top of Vesuvius a second time, and found a different face of things. The smoke ascending upright, gave a full prospect of the crater, which, as I could judge, was about a mile in circumference, and a hundred yards deep. A conical mount had been formed, since my last visit, in the middle of the bottom, which I could see was made by the stones, thrown up and fallen back again into the crater. In this new hill remained the two furnaces already mentioned. The one was seen to throw up every three or four minutes, with a dreadful sound, a vast number of red-hot stones, at least three hundred feet higher than my head, as I stood upon the brink ; but as there was no wind, they fell perpendicularly back from whence they had been discharged. The other was filled with red-hot liquid matter, like that in the furnace of a glass-house, raging and working like the waves of the sea, with a short abrupt noise. This matter would sometimes boil over, and run down the side of the conical hill, appearing at first red hot, but changing colour as it hardened and cooled. Had the wind driven in our faces, we had been in no small danger of stifling by the sulphureous smoke, or being killed by the masses of melted minerals that were shot from the bottom. But as the wind was favourable, I had an opportunity of surveying this amazing scene for above an hour and a half together. On the fifth of June, after a horrid noise, the mountain was seen at Naples to work over ; and, about three days after, its thunders were THE EARTH. 61 renewed so, that not only the windows in the city, but all the houses, shook. From that time it continued to over- flow, and sometimes at night were seen columns of fire shooting upward from its summit. On the tenth, when all was thought to be over, the mountain again renewed its terrors, roaring and raging most violently. One can- not form a juster idea of the noise, in the most violent fits of it, than by imagining a mixed sound made up of the raging of a tempest, the murmur of a troubled sea, and the roaring of thunder and artillery, confused all to- gether. Though we heard this at a distance of twelve miles, yet it was very terrible. I therefore resolved to approach nearer to the mountain ; and, accordingly, three or four of us got into a boat, and were set ashore at a little town situated at the foot of the mountain. From thence we rode about four or five miles, before we came to the torrent of fire that was descending from the side of the volcano ; and here the roaring grew exceedingly loud and terrible as we approached. I observed a mixture of colours in the cloud, above the crater, green, yellow, red, and blue. There was likewise a ruddy dismal light in the air, over that tract where the burning river flowed. These circumstances, set off and augmented by the hor- ror of the night, made a scene the most uncommon and astonishing I ever saw; which still increased as we ap- proached the burning river. Imagine a vast torrent of liquid fire, rolling from the top down the side of the moun- tain, and with irresistible fury bearing down and consum- ing vines, olives, and houses ; and divided into different channels, according to the inequalities of the mountain. The largest stream seemed half a mile broad at least, and five miles long. I walked so far before my companions up the mountain, along the side of the river of fire, that I was obliged to retire in great haste, the sulphureous stream having surprised me, and almost taken away my breath. During our return, which was about three o’clock in the morning, the roaring of the mountain was heard all the way, while we observed it throwing up huge spouts of fire and burning stones, which, falling, resembled the stars in a rocket. Sometimes I observed two or three distinct columns of flame, and sometimes one only, that was large enough to fill the whole crater. These burning 62 A HISTORY OF columns, and fiery stones, seemed to be shot a thousand feet perpendicular above the summit of the volcano ; and in this manner the mountain continued raging for six or eight days after. On the 18th of the same month, the whole appearance ended, and the mountain remained per- fectly quiet, without any visible smoke or flame.” The matter which is found to roll down from the mouth of all volcanoes in general, resembles the dross that is thrown from a smith’s forge. But it is different, perhaps, in various parts of the globe ; for, as we have already said, there is not a quarter of the world that has not its volca- noes. In Asia, particularly in the islands of the Indian Ocean, there are many. One of the most famous is that of Albouras, near Mount Taurus, the summit of which is continually on fire, and covers the whole adjacent coun- try with ashes. In the island of Ternate there is a vol- cano, which, some travellers assert, burns most furiously in the times of the equinoxes, because of the winds which then contribute to increase the flames. In the Molucco islands, there are many burning mountains ; they are also seen in Japan, and the islands adjacent ; and in Java and Sumatra, as well as in other of the Philippine Islands. In Africa there is a cavern, near Fez, which continually sends forth either smoke or flames. In the Cape de Verde islands, one of them, called the Island del Fuego , continually burns ; and the Portuguese, who frequently attempted a settlement there, have as often been obliged to desist. The Peak of Teneriffe is, as every body knows, a volcano, that seldom desists from eruptions. But of all parts of the earth, America is the place where those dread- ful irregularities of nature are the most conspicuous. Ve- suvius, and iEtna itself, are but mere fire-works in eofn- parison to the burning mountains of the Andes ; which, as they are the highest mountains of the world, so also are they the most formidable for their eruptions. The mountain of Arequipa in Peru, is one of the most cele- brated ; Carassa, and Malahallo, are very considerable ; but that of Cotopaxi, in the province of Quito, exceeds any thing we have hitherto read or heard of. The moun- tain of Cotopaxi, as described by Ulloa,* is more than three miles perpendicular from the sea ; and it became a * Ulloa, vol. i. p. 442, THE EARTH. (33 volcano at the time of the Spaniards’ first arrival in that country. A new eruption of it happened in the year 1743, having been some days preceded by a continual roaring in its bowels. The sound of one of these moun- tains is not, like that of the volcanoes in Europe, confined to a province, but is heard at a hundred and fifty miles distance.* “ An aperture was made in the summit of this immense mountain ; and three more about equal heights near the middle of its declivity, which was at that time buried under prodigious masses of snow. The ignited substances ejected on that occasion, mixed with a prodigious quantity of ice and snow, melting amidst the flames, were carried down with such astonishing rapidity, that in an instant the valley from Callo to Latucunga was overflowed ; and besides its ravages in bearing down the houses of the Indians, and other poor inhabitants, great numbers of people lost their lives. The river of Latucunga was the channel of this terrible flood ; till being too small for re- ceiving such a prodigious current, it overflowed the adjacent country, like a vast lake, near the town, and carried away all the buildings within its reach. The inhabitants retired into a spot of higher ground behind the town, of which those parts which stood within the limits of the current were totally destroyed. The dread of still greater devastations did not subside for three days ; during which the volcano ejected cinders, while torrents of melted ice and snow poured down its sides. The eruption lasted several days, and was accompanied with terrible roarings of the wind, rushing through the volcano, still louder than the former rumblings in its bowels. At last all was quiet, neither fire nor smoke to be seen, nor noise to be heard ; till, in the ensuing year, the flames again appeared with recruited violence, forcing their passage through several other parts of the mountain, so that in clear nights the flames being reflected by the transparent ice, formed an awfully magnificent illumi- nation.” Such is the appearance and the effect of those fires which proceed from the more inward recesses of the earth : for that they generally come from deeper regions than man has hitherto explored, I cannot avoid thinking, con- trary to the opinion of Mr. Buffon, who supposes them * Ulloa, vol. i. p. 442. 64 A HISTORY OF .v.4pP®. s\ rooted but a very little way below the bed of the moun- tain. “ We can never suppose,” says this great naturalist, “ that these substances are ejected from any great dis- tance below, if we only consider the great force already required to fling them up to such vast heights above the mouth of the mountain ; if we consider the substances thrown up, which we shall find upon inspection to be the same with those of the mountain below ; if we take into our consideration, that air is always necessary to keep up the flame ; but, most of all, if we attend to one circum- stance, which is, that if these substances were exploded from a vast depth below, the same force required to shoot them up so high, would act against the sides of the vol- cano, and tear the whole mountain in pieces.” To all this specious reasoning, particular answers might be easily given ; as, that the length of the funnel increases the force of the explosion ; that the sides of the funnel are actually often burst with the great violence of the flame ; that air may be supposed at depths at least as far as the perpen- dicular fissures descend. But the best answer is a well- known fact ; nainely, that the quantity of matter discharged from iEtna alone, is supposed, upon a moderate compu- tation, to exceed twenty times the original bulk of the mountain.* The greatest part of Sicily seems covered with its eruptions. The inhabitants of Catanea have found, at the distance of several miles, streets and houses sixty feet deep, overwhelmed by the lava or matter it has discharged. But what is still more remarkable, the walls of these very houses have been built of materials evidently thrown up by the mountain. The inference from all this is very obvious ; that the matter thus exploded cannot belong to the mountain itself, otherwise it would have been quickly consumed ; it cannot be derived from moderate depths, since its amazing quantity evinces, that all the places near the bottom must have long since been exhausted ; nor can it have an extensive, and, if I may so call it, a superficial spread, for then the country round would be quickly under- mined ; it must, therefore, be supplied from the deeper regions of the earth ; those undiscovered tracts where the ' Deity performs his wonders in solitude, satisfied with self- approbation ! * Kircher, Mund. Subt. vol. i. p. 202. THE EARTH \ 65 CHAP. X. OF EARTH&UAKES. Having given the theory of volcanoes, we have in some measure given also that of earthquakes. They both seem to proceed from the same cause, only with this difference, that the fury of the volcano is spent in the eruption ; that of an earthquake spreads wider, and acts more fatally by being confined. The volcano only affrights a province; earth- quakes have laid whole kingdoms in ruin. Philosophers* have taken some pains to distinguish be- tween the various kinds of earthquakes, such as the tremu- lous, the pulsative, the perpendicular, and the inclined; but these are rather the distinctions of art than of nature, mere accidental differences arising from the situation of the country or of the cause. If, for instance, the confined fire* acts directly under a province or a town, it will heave the earth perpendicularly upward, and produce a perpen- dicular earthquake. If it acts at a distance, it will raise that tract obliquely, and thus the inhabitants will perceive an inclined one. Nor does it seem to me that there is much greater reason for Mr. Buffon’s distinction of earthquakes ; one kind of which he supposes^ to be produced by fire in the manner of volcanoes, and confined but to a very narrow circum- ference. The other kind he ascribes to the struggles of confined air, expanded by heat in the bowels of the earth, and endeavouring to get free. For how do these two causes differ ? Fire is an agent of no power whatsoever without air. It is the air, which being at first compressed, and then dilated in a cannon, that drives the ball with such' force. It is the air struggling for vent in a volcano, that throws up its contents to such vast heights. In short, it is the air confined in the bowels of the earth, and acquiring elasticity v heat, that produces all those appearances which are generally ascribed to the operation of fire. When, there- °re, we are told that there are two causes of earthquakes, "e only learn that a greater or smaller quantity of heat produces those terrible effects ; for air is the only active operator in either. Aristotle, Agricola, Buffon. + Buffon, vol. ii. p. 328. voi.r.— 3. I F A . HISTORY OF m Some philosophers, however, have been willing to give the air as great a share in producing these terrible efforts as they could ; and, magnifying its powers, have called in but a very moderate degree of heat to put it in action. Although ex- perience tell us that the earth is full of inflammable mate- rials, and that fires are produced wherever we descend ; although it tells us that those countries where there are volcanoes, are most subject to earthquakes ; yet they step out of their way, and so find a new solution. These only allow but just heat enough to produce the most dreadful phenomena, and, backing their assertions with long cal- culations, give theory an air of demonstration. Mr. Amon- tons* has been particularly sparing of the internal heat in this respect; and has shown, perhaps accurately enough, that a very moderate degree of heat may suffice to give the air amazing powers of expansion. It is amazing enough, however, to trace the progress of a philosophical fancy let loose in imaginary speculations. They run thus : “A very moderate degree of heat may bring the air into a condition capable of producing earth- quakes ; for the air, at the depth of forty-three thousand five hundred and twenty-eight fathom below the surface of the earth, becomes almost as heavy as quicksilver. This, however, is but a very slight depth in comparison of the distance to the centre, and is scarcely a seventieth part of the way. The air, therefore, at the centre, must be infinitely heavier than mercury, or any body that we know of. This granted, we shall take something more, and say, that it is very probable there is nothing but air at the centre. Now let us suppose this air heated, by some means, even to the degree of boiling water, as we have proved that the density of the air is here very great, its elasticity must be in proportion ; a heat, therefore, which at the surface of the earth would have produced but a slight expansive force, must, at the centre, produce one very extraordinary, and, in short, be perfectly irresistible. Hence, this force may, with great ease, produce earth- quakes ; and, if increased, it may convulse the globe ; it may (by only adding figures enough to the calculation) destroy the solar system, and even the fixed stars them- selves.” These reveries generally produce nothing; for, * Memoires de l’Academie de Sciences, An. 1703. THE EARTH. 67 as I have ever observed, increased calculations, while they seem to tire the memoiy, give the reasoning faculty perfect repose. However, as earthquakes are the most formidable minis- ters of nature, it is not to be wondered that a multitude of writers have been curiously employed in their consideration. Woodward has ascribed the cause to a stoppage of the waters below the earth’s surface by some accident. These being thus accumulated, and yet acted upon by fires, which he supposes still deeper, both contribute to heave up the earth upon their bosom. This, he thinks, accounts for the lakes of water produced in an earthquake, as well as for the fires that sometimes burst from the earth’s surface upon those dreadful occasions. There are others who have supposed that the earth may be itself the cause of its own convulsions. “ When,” say they, “ the root or basis of some large tract is worn away by a fluid underneath, the earth sinking therein, its weight occasions a tremor of the adjacent parts, sometimes producing a noise, and sometimes an inundation of water.” Not to tire the reader with a history of opinions instead of facts, some have ascribed them to electricity, and some to the same causes that pro- duce thunder. It would be tedious, therefore, to give all the various opinions that have employed the speculative on this sub- ject. The activity of the internal heat seems alone suffi- cient to account for every appearance that attends these tremendous irregularities of nature. To conceive this distinctly, let us suppose, at some vast distance under the earth, large quantities of inflammable matter, pyrites, bitumens, and marcasites, disposed, and only waiting for the aspersion of water, or the humidity of the air, to put their fires in motion : at last, this dreadful mixture arrives ; waters find their way into those depths, through the perpendicular fissures ; or air insinuates itself through the same minute apertures : instantly new appearances ensue ; those substances, which for ages before lay dor- mant, now conceive new apparent qualities ; they grow hot, produce new air, and only want room for expansion. However, the narrow apertures by which the air or water had at first admission, are now closed up ; yet as new air 18 continually generated, and as the heat every moment A HISTORY OF 68 gives this air new elasticity, it at length bursts, and dilates all round ; and, in its struggles to get free, throws all above it into similar convulsions. Thus an earthquake is pro- duced, more or less extensive, according to the depth or the greatness of the cause. But before we proceed with the causes, let us take a short view of the appearances which have attended the most remarkable earthquakes. By these we shall see how far the theorist corresponds with the historian. The greatest we find in antiquity is that mentioned by Pliny,* in which twelve cities in Asia Minor were swallowed up in one night: he tells us also of another, near the lake Thrasymene, which was not perceived by the armies of the Carthaginians and Romans, that were then engaged near that lake, although it shook the greatest part of Italy. In another place'f- he gives the following account of an earthquake of an extraordinary kind. “ When Lucius Marcus and Sextus Julius were consuls, there appeared a very strange prodigy of the earth, (as I have read in the books of ^Etruscan discipline,) which happened in the province of Mutina. Two mountains shocked against each other, approaching and retiring with the most dreadful noise. They, at the same time, and in the midst of the day, appeared to cast forth fire and smoke, while a vast number of Roman knights and travellers from the iEmilian Way, stood and continued amazed spectators. Several towns were destroyed by this shock ; and all the animals that were near them were killed.” In the times of Trajan, the city of Antioch, and a great part of the adjacent country, was buried by an earthquake. About three hundred years after, in the times of Justinian, it was once more destroyed, together with forty thousand inha- bitants ; and, after an interval of sixty years, the same ill-fated city was a third time overturned, with the loss of not less than sixty thousand souls. In the year 1182, most of the cities of Syria, and the kingdom of Jerusalem, were destroyed by the same accident. In the year 1594, the Italian historians describe an earthquake at Puteoli, which caused the sea to retire two hundred yards from its former bed. But one of those most particularly described in history, * Pirn. lib. ii. cap. 80. f Ibid- lib. iii. cap. 85. THE EARTH. 69 is that of the year 1 693 ; the damages of which were chieflv felt in Sicily, but its motion perceived in Germany, France, and England. It extended to a circumference of two thou- sand six hundred leagues ; chiefly affecting the sea-coast and great rivers ; more perceivable also upon the moun- tains than in the vallies. Its motions were so rapid, that those who lay at their length were tossed from side to side, as upon a rolling billow.* The walls were dashed from their foundations ; and no less than fifty-four cities, with an incredible number of villages, were either destroyed or greatly damaged. The city of Catanea, in particular, was utterly overthrown. A traveller, who was on his way thither, at the distance of some miles, perceived a black cloud, like night, hanging over the place. The sea, all of a sudden, began to roar ; Mount iEtna to send forth great spires of flame ; and soon after a shock ensued, with a noise as if all the artillery in the world had been at once discharged. Our traveller, being obliged to alight, instantly felt himself raised a foot from the ground ; and turning his eyes to the city, he, with amazement, saw nothing but a thick cloud of dust in the air. The birds flew about astonished ; the sun was darkened ; the beasts ran howling from the hills ; and although the shock did not continue above three minutes, yet near nineteen thousand of the inhabitants of Sicily perished in the ruins. — Catanea, to which city the describer was travelling, seemed the principal scene of ruin ; its place only was to be found ; and not a footstep of its former magnificence was to be seen remaining. The earthquake which happened in Jamaica, in 1692, was very terrible, and its description sufficiently minute. “ In two minutes’ time it destroyed the town of Port Royal, and sunk the houses in a gulph forty fathoms deep. It was attended with a hollow rumbling noise, like that of thunder ; and, in less than a minute, three parts of the houses, and their inhabitants, were all sunk quite under water. While they were thus swallowed up on one side of the street, on the other the, houses were thrown into heaps ; the sand of the streets rising like the waves of the sea, lifting up those that stood upon it, and immediately * Phil. Trans. A HISTORY OF 70 overwhelming them in pits. All the wells discharged their waters with the most vehement agitation. The sea felt an equal share of turbulence, and, bursting over its mounds, deluged all that came in its way. The fissures of the earth were, in some places, so great, that one of the streets appeared twice as broad as formerly. In many places, however, it opened and closed again, and continued this agitation for some time. Of these openings, two or three hundred might be seen at a time; in some whereof the people were swallowed up ; in others, the earth closing, caught them by the middle, and thus crushed them instantly to death. Other openings, still more dreadful than the rest, swallowed up whole streets ; and others, more formidable, spouted up whole cataracts of water, drowning such as the earthquake had spared. The whole was attended with the most noisome stench ; while the thundering of the distant falling mountains, the whole sky overcast with a dusky gloom, and the crash of falling habitations, gave unspeak- able horror to the scene. After this dreadful calamity was over, the whole island seemed converted into a scene of desolation ; scarcely a planter’s house was left standing ; almost all were swallowed up ; houses, people, trees, shared one universal ruin ; and in their places appeared great pools of water, which when dried up by the sun, left only a plain of barren sand, without any vestige of former inhabitants. Most of the rivers, during the earthquake, were stopt up by the falling in of the mountains ; and it was not till after some time that they made themselves new channels. The mountains seemed particularly at- tacked by the force of the shock ; and it was supposed that the principal seat of the concussion was among them. Those who were saved got on board ships in the harbour, where many remained above two months ; the shocks con- tinuing, during that interval, with more or less violence every day.” As this description seems to exhibit all the appearances that usually make up the catalogue of terrors belonging to an earthquake, I will suppress the detail of that which happened at Lisbon in our own times, and which is too recent to require a description. In fact there are few par- ticulars in the accounts of those who were present at that scene of desolation, that we have not more minutely and THE EARTH 71 accurately transmitted to us by former writers, wnose nar- ratives I have for that reason preferred. I will therefore close this description of human calamities with the account of the dreadful earthquake at Calabria, in 1638. It is related by the celebrated Father Kircher, as it happened while he was on his journey to visit Mount iEtna, and the rest of the wonders that lie towards the south of Italy. I need scarcely inform the reader, that Kircher is considered, by scholars, as one of the greatest prodigies of learning. “ Having hired a boat, in company with four more, two friars of the order of St. Francis, and two seculars, we launched, on the twenty-fourth of March, from the har- bour of Messina, in Sicily, and arrived the same day at the promontory of Pelorus. Our destination was for the city of Euphsemia, in Calabria, where we had some busi- ness to transact, and where we designed to tarry for some time. However, Providence seemed willing to cross our design ; for we were obliged to continue for three days at Pelorus, upon account of the weather ; and though -we often put out to sea, yet we were as often driven back. At length, however, wearied with the delay, we resolved to prosecute our voyage ; and, although the sea seemed more than usually agitated, yet we ventured forward. The gulph of Charybdis, which we approached, seemed whirled round in such a manner, as to form a vast hol- low, verging to a point in the centre. Proceeding on- ward, and turning my eyes to iEtna, I saw it cast forth large volumes of smoke, of mountainous sizes, which entirely covered the whole island, and blotted out the very shores from my view. This, together with the dreadful noise, and the sulphureous stench, which was strongly perceived, filled me with apprehensions that some more dreadful calamity was impending. The sea itself seemed to wear a very unusual appearance ; those who have seen a lake in a violent shower of rain covered all over with bubbles, will conceive some idea of its agi- tations. My surprise was still increased by the calmness and serenity of the weather ; not a breeze, not a cloud, which might be supposed to put all nature thus into motion. I therefore warned my companions that an earth- quake was approaching ; and, after some time, making for the shore with all possible diligence, we landed at A HISTORY OF 72 Tropae, happy and thankful for having escaped the threaten- ing dangers of the sea. “ But our triumphs at land were of short duration ; for we had scarcely arrived at the Jesuits’ College in that city, when our ears were stunned with a horrid sound, resem- bling that of an infinite number of chariots driven fiercely forward, the wheels rattling, and the thongs cracking. Soon after this, a most dreadful earthquake ensued, so that the whole tract upon which we stood, seemed to vi- brate, as if we were in the scale of a balance that conti- nued wavering. This motion, however, soon grew more violent ; and being no longer able to keep my legs, I was thrown prostrate upon the ground. In the mean time, the universal ruin round me redoubled my amazement. The crash of falling houses, the tottering of towers, and the groans of the dying, all contributed to raise my terror and despair. On every side of me I saw nothing but a scene of ruin, and danger threatening wherever I should fly. I commended myself to God, as my last great refuge. At that hour, O how vain was every sublunary happiness ! wealth, honour, empire, wisdom, all mere useless sounds, and as empty as the bubbles in the deep. Just standing on the threshold of eternity, nothing but God was my pleasure ; and the nearer I approached, I only loved him the more. — After some time, however, finding that I remained unhurt amidst the general concussion, I resolved to venture for safety, and running as fast as I could, reached the shore, but almost terrified out of my reason. I did not search long here till I found the boat in which I had landed, and my companions also, whose terrors were even greater than mine. Our meeting was not of that kind where every one is desir- ous of telling his owp happy escape ; it was all silence, and a gloomy dread of impending terrors. “ Leaving this seat of desolation, we prosecuted our voyage along the coast, and the next day came to Rochetta, where we landed, although the earth still continued in violent agitations. But we were scarcely arrived at our inn, when we were once more obliged to return to the boat, and in about half an hour we saw the greatest part of the town, and the inn at which we had set up, dashed to the ground, and burying all its inhabitants beneath its ruins. “ In this mapner, proceeding onward in our little ves- THE EARTH. 73 sel, finding no safety at land, and yet, from the smallness of our boat, having but a very dangerous continuance at sea, we at length landed at Lopizium, a castle midway between Tropse and Eupheemia, the city to which, as I said before, we were bound. Here, wherever I turned my eyes, nothing but scenes of ruin and horror appeared ; towns and castles levelled to the ground; Strombolo, though at sixty miles distance, belching forth flames in an unusual manner, and with a noise which I could distinctly hear. But my attention was quickly turned from more remote to contiguous danger. The rumbling sound of an approaching earthquake, which we by this time were grown acquainted with, alarmed us for the consequences ; it every moment seemed to grow louder, and to approach more near. The place on which we stood now began to shake most dreadfully, so that being unable to stand, my companions and I caught hold of what- ever shrub grew next us, and supported ourselves in that manner. “ After some time, this violent paroxysm ceasing, we again stood up, in order to prosecute our voyage to Eu- phsemia, that lay within sight. In the mean time, while we were preparing for this purpose, I turned my eyes to- wards the city, but could see only a frightful dark cloud that seemed to rest upon the place. This the more sur- prised us, as the weather was so very serene. We waited, therefore, till the cloud was passed away ; then turning to look for the city, it was totally sunk. Wonderful to tell ! nothing but a dismal and putrid lake was to be seen where it stood. We looked about to find some one that could tell us of its sad catastrophe, but could see none ! All was be- come a melancholy solitude ! a scene of hideous desola- tion ! Thus proceeding pensively along, in quest of some human being that could give us some little information, we at length saw a boy sitting by the shore, and appear- ing stupified with terror. Of him, therefore, we inquired concerning the fate of the city, but he could not be in- duced to give us an answer. We intreated him with every expression of tenderness and pity to tell us : but his senses were quite wrapt up in the contemplation of the danger he had escaped. We offered him some victuals, but he seemed to loathe the sight. We still persisted in °ur offices of kindness ; but he only pointed to the place vol. i.— 3. K A HISTORY OF 74 of the city, like one out of his senses ; and then running up into the woods, was never heard of after. Such was the fate of the city of Euphaemia ! and as we continued our melancholy course along the shore, the whole coast, for the space of two hundred miles, presented nothing but the remains of cities, and men scattered, without an ha- bitation, over the fields. Proceeding thus along, we at length ended our distressful voyage by arriving at Naples, after having escaped a thousand dangers both at sea and land.” The reader, I hope, will excuse me for this long trans- lation from a favourite writer, and that the sooner, as it contains some particulars relative to earthquakes not to be found elsewhere. From the whole of these accounts we may gather, that the most concomitant circumstances are these : A rumbling sound before the earthquake. This proceeds from the air or fire, or both, forcing their way through the chasms of the earth, and endeavouring to get free ; which is also heard in volcanoes. A violent agitation or heaving of the sea, sometimes before and sometimes after that at land. This agitation is only a similar effect produced on the waters with that at land, and may be called, for the sake of perspicuity, a seaquake ; and this also is produced by volcanoes. A spouting up of waters to great heights. It is not easy to describe the manner in which this is performed : but volcanoes also perform the same ; Vesuvius being known frequently to eject a vast body of water. A rocking of the earth to and fro, and sometimes a per- pendicular bouncing, if it may be so called, of the same. This difference chiefly arises from the situation of the place with respect to the subterranean fire. Directly under, it lifts ; at a farther distance, it rocks. Some earthquakes seem to travel onward, and are felt in different countries at different hours the same day. This arises from the great shock being given to the earth at one place, and that being communicated onward by an undulatory motion, successively affects different regions in its progress ; as the blow given by a stone falling in a lake, is not perceived at the chores till some time after the first concussion, THE EARTH. 75 'ilie shock is sometimes instantaneous, like the explosion of gunpowder ; and sometimes tremulous, and continuing for several minutes. The nearer the place where the shock is first given, the more instantaneous and simple it appears. At a greater distance, the earth redoubles the first blow with a sort of vibratory continuation. As waters have generally so great a share in producing earthquakes, it is not to be wondered that they should generally follow those breaches made by the force of fire, and appear in the great chasms which the earthquake has opened. These are some of the most remarkable phenomena of earthquakes, presenting a frightful assemblage of the most terrible effects of air, earth, fire, and water. The valley of Solfatara, near Naples, seems to exhibit, in a minuter degree, whatever is seen of this horrible kind on the great theatre of nature. This plain, which is about twelve hundred feet long, and a thousand broad, is embo- somed in mountains, and has in the middle of it a lake of noisome blackish water, covered with a bitumen, that floats upon its surface. In every part of this plain, caverns ap- pear smoking with sulphur, and often emitting flames. The earth, wherever we walk over it, trembles beneath the feet. Noises of flames, and the hissing of waters, are heard at the bottom. The water sometimes spouts up eight or ten feet high. The most noisome fumes, foetid water, and sulphureous vapours, offend the smell. A stone thrown into any of the caverns, is ejected again with considerable violence. These appearances generally prevail when the sea is any way disturbed ; and the whole seems to exhibit the appearance of an earthquake in miniature. However, in this smaller scene of wonders, as well as in the greater, there are many appearances for which, perhaps, we shall never account ; and many questions may be asked, which no conjectures can thoroughly resolve. It was the fault of the philosophers of the last age, to be more inquisitive after the causes of things than after the things themselves. They seemed to think that a confession of ignorance can- celled their claims to wisdom ; they, therefore, had a solution for every demand. But the present age has grown, if not more inquisitive, at least more modest ; and none are now ashamed of that ignorance, which labour can neither remedy nor remove. 76 A HISTORY OF CHAP. XI. OF THE APPEARANCE OF NEW ISLANDS AND TRACTS ; AND OF THE DISAPPEARING OF OTHERS. Hitherto we have taken a survey only of the evils which are produced by subterranean fires, but we have mentioned nothing of the benefits they may possibly produce. They may be of use in warming and cherishing the ground, in promoting vegetation, and giving a more exquisite flavour to the productions of the earth. The imagination of a person who has never been out of our own mild region, can scarcely reach to that luxuriant beauty with which all nature appears clothed in those very countries that we have but just now described as desolated by earthquakes, and under- mined by subterranean fires. It must be granted, therefore, that though in those regions they have a greater share in the dangers, they have also a larger proportion in the benefits of nature. But there is another advantage arising from subterranean fires, which, though hitherto disregarded by man, yet may one day become serviceable to him ; I mean, that while they are found to swallow up cities and plains in one place, they are also known to produce promontories and islands in another. We have many instances of islands being thus formed in the midst of the sea, which though for a long time barren, have afterwards become fruitful seats of hap- piness and industry. New islands are formed in two ways ; either suddenly, by the action of subterraneous fires ; or more slowly, by the deposition of mud, carried down by rivers, and stop- ped by some accident.* With respect particularly to the first, ancient historians, and modern travellers, give us such accounts as we can have no room to doubt of. Se- neca assures us, that in his time the island of Therasia appeared unexpectedly to some mariners, as they were employed in another pursuit. Pliny assures us, that thir- teen islands in the Mediterranean appeared at once emerging from the water ; the cause of which he ascribes rather to the retiring of the sea in those parts, than to any subterraneous elevation. However, he mentions the island * Buffon, vol. ii. p. 343. THE EARTH. 77 of Hiera, near that of Therasia, as formed by subterraneous explosions ; and adds to his list several others formed in the same manner. In one of which he relates that fish in great abundance were found, and that all those who ate of them died shortly after. “ On the twenty-fourth of May,* in the year 1707, a slight earthquake was perceived at Santorin ; and the day following, at sun-rising, an object was seen by the inhabi- tants of that island, at two or three miles distance at sea, which appeared like a floating rock. Some persons, desirous either of gain, or incited by curiosity, went there, and found, even while they stood upon this rock, that it seemed to rise beneath their feet. They perceived also, that its sur- face was covered with pumice-stones and oysters, which it had raised from the bottom. Every day after, until the fourteenth of June, this rock seemed considerably to in- crease ; and then was found to be half a mile round, and about thirty feet above the sea. The earth of which it was composed seemed whitish, with a small proportion of clay. Soon after this the sea again appeared troubled, and steams arose which were very offensive to the inha- bitants of Santorin. But on the sixteenth of the succeeding month, seventeen or eighteen rocks more were seen to rise out of the sea, and at length to join together. All this was accompanied with the most terrible noise, and fires which proceeded from the island that was newly formed. The whole mass, however, of all this new- formed earth, uniting, increased every day, both in height and breadth, and, by the force of its explosions, cast forth rocks to seven miles distance. This continued to bear the same dreadful appearances till the month of November in the same year; and it is at present a volcano, which sometimes renews its explosions. It is about three miles in circumference ; and more than from thirty-five to forty feet high.” It seems extraordinary, that, about this place in parti- cular, islands have appeared at different times, particularly that of Hiera, mentioned above, which has received con- siderable additions in succeeding ages. Justin tells us,-}- that at the time the Macedonians were at war with the Homans, a new island appeared between those of Thera- * Hist, de l’Acad. an. 1708. p. 23. f Justin, lib. xxx. cap. 4. A HISTORY OF 78 menes and Therasia, by means of an earthquake. We are told that this became half as large again about a thousand years after, another island rising up by its side, and joining to it, so as scarcely at present to be distinguished from the former. A new island was formed, in the year 1/20, near that of Tercera, near the continent of Africa, by the same causes. In the beginning of December, at night, there was a terrible earthquake at that place, and the top of a new island ap- peared, which cast forth smoke in vast quantities. rIhe pilot of a ship, who approached it, sounded on one side of this island, and could not find ground at sixty fathom : at the other side the sea was totally tinged of a different colour, exhibiting a mixture of white, blue, and green ; and was very shallow. This island, on its first appearance, was larger than it is at present ; for it has since that time sunk in such a manner, as to be scarcely above water.* A traveller, whom these appearances could not avoid affecting, speaks of them in this manner:^ “What can be more surprising than to see fire not only break out of the bowels of the earth, but also to make itself a passage through the waters of the sea ! What can be more extra- ordinary, or foreign to our common notions of things, than to see the bottom of the sea rise up into a mountain above the water, and become so firm an island as to be able to resist the violence of the greatest storms ! I know that subterraneous fires, when pent in a narrow passage, are able to raise up a mass of earth as large as an island : but that this should be done in so regular and exact a manner that the water of the sea should not be able to * In the spring of 1783, a volcanic island was formed about 30 miles from the south-west point of Iceland. The discoverer. Captain Von Lowenhorn, in the Danish service, who arrived just at the time of the first eruption, when smoke and flames ascended out of the sea, relates that no island or any land could be seen, from which these flames could originate. No wonder, then, that he fell into the greatest consternation, when, as he expresses himself, he saw the waves on fire. The following year, the Danish government directed, that all ships bound to Iceland should examine the new- formed island ; but so entirely had it vanished’, that none of them either saw or could discover the smallest trace ot it. However, towards the end of the next year, a Danish ship of war, of 64 guns, was wrecked on this rock 5 which is now no longer visible, but re- mains a most dangerous rock, nearly level with the surface of the water. f Phil. Trans, vol. v. p. 1 97. THE EARTH. 79 penetrate and extinguish those fires ; that after having made so many passages, they should retain force enough to raise the earth ; and, in fine, after having been ex- tinguished, that the mass of earth should not fall down, or sink again with its own weight, but still remain in a manner suspended over the great arch below ! This is what to me seems more surprising than any thing that has been related of Mount AEtna, Vesuvius, or any other volcano.” Such are his sentiments : however, there are few of these appearances any way more extraordinary than those at- tending volcanoes and earthquakes in general. We are not more to be surprised that inflammable substances should be found beneath the bottom of the sea, than at similar depths at land. These have all the force of fire giving expansion to air, and tending to raise the earth at the bottom of the sea, till it at length heaves above water. These marine volcanoes are not so frequent ; for, if we may judge of the usual procedure of nature, it must very often happen, that before the bottom of the sea is elevated above the surface, a chasm is opened in it, and then the water pressing in, extinguishes the volcano before it has time to produce its effects. This extinction, however, is not effected without very great resistance from the fire beneath. The water, upon dashing into the cavern, is very probably at first ejected back with great violence ; and thus some of those amazing water-spouts are seen, which have so often astonished the mariner, and excited curiosity. But of these in their place. Besides the production of those islands by the action of fire, there are others, as was said, produced by rivers or seas carrying mud, earth, and such like substances, along with their currents ; and at last depositing them in some particular place. At the mouths of most great rivers, there are to be seen banks, thus formed by the sand and mud carried down with the stream, which have rested at that place, where the force of the current is diminished by its junction with the sea. These banks, by slow de- giees, increase at the bottom of the deep : the water in those places, is at first found by mariners to grow more shallow ; the bank stfon heaves up above the surface ; it 18 considered, for a while, as a tract of useless and barren A HISTORY OF 80 sand ; but the seeds of some of the more hardy vegetables are driven thither by the wind, take root, and thus bind- ing the sandy surface, the whole spot is clothed in time with a beautiful verdure. In this manner there are de- lightful and inhabited islands at the mouths of many rivers, particularly the Nile, the Po, the Mississippi, the Ganges, and the Senegal. There has been, in the memory of man, a beautiful and large island formed in this manner at the mouth of the river Nanquin, in China, made from depo- sitions of mud at its opening; it is not less than sixty miles long, and about twenty broad. La Loubere informs us,* in his voyage to Siam, that these sand-banks increase every day, at the mouths of all the great rivers in Asia : and hence, he asserts, that the navigation up these rivers becomes every day more difficult, and will, at one time or other, be totally obstructed. The same may be remarked with regard to the Wolga, which has at present seventy openings into the Caspian sea ; and of the Danube, which has seven into the Buxine. We have had an instance of the formation of a new island not very long since at the mouth of the Humber, in England. “ It is yet within the memory of man,” says the relator, 'f' “ since it began to raise its head above the ocean. It began its appear- ance at low water, for the space of a few hours, and was buried again till the next tide’s retreat. Thus succes- * sively it lived and died, until the year 1666, when it began to maintain its ground against the insult of the waves, and then first invited the aid of human industry. A bank was thrown about its rising grounds, and being thus de- fended from the incursions of the sea, it became firm and solid, and, in a short time, afforded good pasturage for cattle. It is about nine miles in circumference, and is worth to the proprietor about eight hundred pounds a year.” It would be endless to mention all the islands that have been thus formed, and the advantages that have been derived from them. However, it is frequently found, that new islands may often be considered as only turning the rivers from their former beds ; so that in proportion as land is gained at one part, it is lost by the overflowing of some other. * Lettres Curieuses et Edifiantes, sec. xi. p. 234 f Phil. Trans, vol. iv. p. 251, THE EARTH. 81 Little, therefore, is gained by such accession ; nor is there much more by the new islands which are sometimes formed from the spoils of the continent. Mariners assure us, that there are sometimes whole plains unrooted from the main lands, by floods and tempests. These being carried out to sea, with all their trees and animals upon them, are frequently seen floating in the ocean, and exhi- biting a surprising appearance of rural tranquillity in the midst of danger. The greatest part, however, having the earth at their roots at length washed away, are dispersed, and their animals drowned ; but now and then some are found to brave the fury of the ocean, till being stuck either among rocks or sands, they again take firm footing, and become permanent islands. As different causes have thus concurred to produce new islands, so we have accounts of others, that the same causes have contributed to destroy. We have already seen the power of earthquakes exerted in sinking whole cities, and leaving lakes in their room. There have been islands, and regions also, that have shared the same fate ; and have sunk with their inhabitants never more to be heard of. Thus Fausanias* tells us of an island called Chryses, that was sunk near Lemnos. Pliny mentions several ; among others, the island of Cea, for thirty miles, having been washed, away, with several thousands of its inhabitants. But of all the noted devastations of this kind, the total submersion of the island of Atalantis, as mentioned by Plato, has been most the subject of speculation. Mankind, in general, now consider the whole of his description as an ingenious fable ; but when fables are grown famous by time and authority, they become an agreeable, if not a necessary, part of literary information. “ About nine thousand years are passed,” says Plato, ■'f* “ since the island of Atalantis was in being. The priests of Egypt were well acquainted with it ; and the first heroes of Athens gained much glory in their wars with the inhabitants. This island was as large as Asia Minor and kyria united; and was situated beyond the Pillars of Her- cules, in the Atlantic ocean. The beauty of the buildings, and the fertility of the soil, were far beyond any thing a! * Pausanias, L 8. in Arcad. p. 509. f Plato in Critia. VOL. I. 4. L 32 A HISTORY OF • modern imagination can conceive: gold and ivory were every where common ; and the fruits of the earth offered themselves without cultivation. The arts and the cou- rage of the inhabitants, were not inferior to the happiness of their situation ; and they were frequently known to make conquests, and overrun the continents of Europe and Asia.” The imagination of the poetical philosopher riots in the description of the natural and acquired ad- vantages, which they long enjoyed in this charming re- gion. “ If,” says he, “ we compare that country to our own, ours will appear a mere wasted skeleton, when op- posed to it. Their mountains, to the very tops, were clothed with fertility, and poured down rivers to enrich the plains below.” However, all these beauties and benefits were destroyed in one day by an earthquake sinking the earth, and the sea overwhelming it. At present not the smallest vestiges of such an island are to be found ; Plato remains as the only authority for its existence ; and philosophers dispute about its situation. It is not for me to enter into the controversy, when there appears but little probability to support the fact ; and, indeed, it would be useless to run back nine thousand years in search of difficulties, as we are surrounded with objects that more closely affect us, and that demand admi- ration at our very doors. When I consider, as Lactantius suggests, the various vicissitudes of nature ; lands swallowed by yawning earthquakes, or overwhelmed in the deep ; rivers and lakes disappearing, or dried away ; mountains levelled into plains ; and plains swelling up into mountains ; I cannot help regarding this earth as a place of very little stability ; as a transient abode of still more transitory beings. CHAP. XII. OF MOUNTAINS. Having at last, in some measure, emerged from the deeps of the earth, we come to a scene of greater splen- dour; the contemplation of its external appearance. In this survey, its mountains are the first objects that strike the imagination, and excite our curiosity. There is not> perhaps, any thing in all nature that impresses an imac- THE EARTH. 83 customed spectator with such ideas of awful solemnity, as these immense piles of Nature’s erecting, that seem to mock the minuteness of human magnificence. In countries where there are nothing but plains, the smallest elevations are apt to excite wonder. In Holland, which is all a flat, they shew a little ridge of hills, near the sea-side, which Boerhaave generally marked out to his pupils, as being mountains of no small consideration. What would be the sensations of such an auditory, could they at once be presented with a view of the heights and precipices of the Alps or the Andes ! Even among us in England, we have no adequate ideas of a mountain-pros- pect ; our hills are generally sloping from the plain, and clothed to the very top with verdure : we can scarcely, therefore, lift our Imaginations to those immense piles, whose tops peep up behind intervening clouds, sharp and precipi- tate, and reach to heights that human avarice or curiosity have never been able to ascend. We, in this part of the world, are not, for that reason, so immediately interested in the question which has so long been agitated among philosophers, concerning what gave rise to these inequalities on the surface of the globe. In our own happy region, we generally see no inequalities but such as contribute to use and beauty; and we therefore are aipazed at a question, inquiring how such necessary inequalities came to be formed, and seeming to express a wonder how the globe comes to be so beautiful as we find it. But though with us there may be no great cause for such a demand, yet in those places where mountains deform the face of nature, where they pour down cataracts, or give fury to tempests, there seems to be good reason for inquiry either into their causes or their uses. It has been, therefore, asked by many, in what manner moun- tains have come to be formed ; or for what uses they are designed ? To satisfy curiosity in these respects, much reasoning has been employed, and very little knowledge propagated. With regard to the first part of the demand, the manner ln which mountains were formed, we have already seen the conjectures of different philosophers on that head. One supposing that they were formed from the earth’s broken shell at the time of the deluge ; another, that they 84 A HISTORY OF existed from the creation, and only acquired their defor- mities in process of time ; a third, that they owed their original to earthquakes ; and still a fourth, with much more plausibility than the rest, ascribing them entirely to the fluctuations of the deep, which he supposes in the be- ginning to have covered the whole earth. Such as are pleased with disquisitions of this kind, may consult Bur- net, Whiston, Woodward, or Buffon. Nor would I be thought to decry any mental amusements, that at worst keep us innocently employed ; but, for my own part, I cannot help wondering how the opposite demand has never come to be made ; and why philosophers have never asked how we come to have plains ? Plains are sometimes more prejudicial to man than mountains. Upon plains, an inundation has greater power ; the beams of the sun are often collected there with suffocating fierceness ; they are sometimes found desert for several hundred miles together, as in the country east of the Caspian sea, although otherwise fruitful, merely because there are no risings or depressions' to form reservoirs, or collect the smallest rivulet of wrater. The most rational answer, therefore, why either moun- tains or plains were formed, seems to be that they were thus fashioned by the hand of Wisdom, in order that pain and pleasure should be so contiguous, as that morality might be exercised either in bearing the one, or communicating the other. Indeed, the more I consider this dispute respecting the formation of mountains, the more I am struck with the futility of the question. There is neither a straight line, nor an exact superficies, in all nature. If we consider a circle, even with mathematical precision, we shall find it formed of a number of small right lines, joining at angles together. These angles, therefore, may be considered in a circle as mountains are upon our globe ; and to demand the reason for the one being mountainous, or the othei angular, is only to ask, why a circle is a circle, or a globe is a globe. In short, if there be no surface without inequality in nature, why should we be surprised that the earth has such ? It has often been said, that the inequalities of its surface are scarce distinguishable, if compared to its mag- nitude ; and I think we have every reason to be content with the answer. THE EARTH. 85 Some, however, have avoided the difficulty by urging the final cause. They allege, that mountains have been formed merely because they are useful to man. This carries the inquirer but a part of the way ; for no one can affirm, that in all places they are useful. The contrary is known, by horrid experience, in those vallies that are sub- ject to their influence. However, as the utility of any part of our earthly habitation is a very pleasing and flattering speculation to every philosopher, it is not to be wondered that much has been said to prove the usefulness of these. For this purpose many conjectures have been made, that have received a degree of assent even beyond their evi- dence ; for men were unwilling to become more miserably wise. It has been alleged, as one principal advantage that we derive from them, that they serve, like hoops or ribs, to strengthen our earth, and to bind it together. In con- sequence of this theory, Kircher has given us a map of the earth, in this manner hooped with its mountains ; which might have a much more solid foundation, did it entirely correspond with truth. Others have found a different use for them, especially when they run surrounding our globe ; which is, that they stop the vapours which are continually travelling from the equator to the poles ; for these being urged by the heat of the sun, from the warm regions of the line, must all be accumulated at the poles, if they were not stopped in their way by those high ridges of mountains which cross their direction. But an answer to this may be, that all the great mountains in America lie lengthwise, and therefore do not cross their direction. But to leave these remote advantages, others assert, that not only the animal but vegetable part of the crea- tion would perish for want of convenient humidity, were it not for their friendly assistance. Their summits are, by these, supposed to arrest, as it were, the vapours which float in the regions of the air. Their large inflections and channels are considered as so many basons prepared for the reception of those thick vapours, and impetuous rains, which descend into them. The huge caverns be- neath are so many magazines or conservatories of water for the peculiar service of man ; and those orifices by A HISTORY OF 86 which the water is discharged upon the plain, are so situated as to enrich and render them fruitful, instead of returning through subterraneous channels to the sea, after the per- formance of a tedious and fruitless circulation.* However this be, certain it is, that almost all our great rivers find their source among mountains ; and, in general, the more extensive the mountain, the greater the river : thus the river Amazon, the greatest in the world, has its source among the Andes, which are the highest mountains on the globe ; the river Niger travels a long course of several hundred miles from the Mountains of the Moon, the highest in all Africa ; and the Danube and the Rhine proceed from the Alps, which are probably the highest mountains of Europe. It needs scarcely be said, that, with respect to height, there are many sizes of mountains, from the gently rising upland, to the tall craggy precipice. The appearance is in general different in those of different magnitudes. The first are clothed with verdure to the very tops, and only seem to ascend to improve our prospects, or supply us with a purer air : but the lofty mountains of the other class have a very different aspect. At a distance their tops are seen, in wavy ridges, of the very colour of the clouds, and only to be distinguished from them by their figure ; which, as I have said, resembles the billows of the sea.'f-' As we approach, the mountain assumes a deeper colour ; it gathers upon the sky, and seems to hide half the horizon behind it. Its summits also are become more distinct, and appear with a broken and perpendicular line. What at first seemed a single hill, is now found to be a chain of continued mountains, whose tops running along in ridges, are embosomed in each other ; so that the curva- tures of one are fitted to the prominences of the opposite side, and form a winding valley between, often of several miles in extent ; and all the way continuing nearly of the same breadth. Nothing can be finer, or more exact, than Mr. Pope’s description of a traveller straining up the Alps. Every mountain he comes to he thinks will be the last ; he finds, however, an unexpected hill rise before him ; and that * Nature Displayed, vol. iii. p. 88. t Lettres Philosophiques sur la Formation, &c. p. 106. THE EARTH. 87 being scaled, he finds the highest summit almost at as great a distance as before. Upon quitting the plain, he might have left a green and fertile soil, and a climate warm and pleasing. As he ascends, the ground assumes a more russet colour ; the grass becomes more mossy, and the weather more moderate. Still as he ascends, the weather becomes more cold, and the earth more barren. In this dreary passage he is often entertained with a little valley of surprising verdure, caused by the reflected heat of the sun collected into a narrow spot on the surrounding, heights. But it much more frequently happens that he sees only frightful precipices beneath, and lakes of amaz- ing depths ; from whence rivers are formed, and fountain derive their original. On those places next the highest summits, vegetation is scarcely carried on ; here and there a few plants of the most hardy kind appear. The air is in- tolerably cold ; either continually refrigerated with frosts, or disturbed with tempests. All the ground here wears; an eternal covering of ice, and snows that seem constantly accumulating. Upon emerging from this war of the ele- ments, he ascends into a purer and a serener region, where vegetation is entirely ceased ; where the precipices, com- posed entirely of rocks, rise perpendicularly above him while he views beneath him all the combat of the ele- ments ; clouds at his feet, and thunders darting upwards; from their bosoms below.* A thousand meteors, which are never seen on the plain, present themselves. Circular rainbows ^ mock suns the shadow of the mountain pro- jected upon the body of the air and the traveller’s own image, reflected as in a looking-glass, upon the opposite cloud. § Such are, in general, the wonders that present them- selves to a traveller in his journey either over the Alps or the Andes. But we must not suppose that this picture exhibits either a constant or an invariable likeness of those stupendous heights. Indeed, nothing can be more capri- cious or irregular than the forms of many of them. The tops of some run in ridges for a considerable length, with- out interruption ; in others, the line stems indented by great vallies to an amazing depth. Sometimes a solitary * fJlloa, vol. i | Phil. Trans, vol. v. p. 152. t Ibid, § Ulloa, vol. i. A HISTORY OF 88 and a single mountain rises from the bosom of the plain ; and sometimes extensive plains, and even provinces, as those of Savoy and Quito, are found embosomed near the tops of mountains. In general, however, those countries that are most mountainous, are the most barren and un- inhabitable. If we compare the heights of mountains with each other, we shall find that the greatest and highest are found under the line.* It is thought by some, that the rapidity of the earth’s motion in these parts, together with The great- ness of the tides there, may have thrown up those stupend- ous masses of earth. But, be the cause as it may, it is a remarkable fact, that the inequalities of the earth’s surface are greatest there. Near the poles, the earth, indeed, is craggy and uneven enough ; but the heights of the mountains there are very inconsiderable. On the contrary, at the equator, where nature seems to sport in the amazing size of all her productions, the plains are extensive, and the mountains remarkably lofty. Some of them are known to rise three miles perpendicular above the bed of the ocean. To enumerate the most remarkable of these, according to their size, we shall begin with the Andes, of which we have an excellent description by Ulloa, who went thither by com- mand of the king of Spain, in company with the French Academicians, to measure a degree of the meridian. His journey up these mountains is too curious not to give an extract from it. After many incommodious days sailing up the river Guayaquil, he arrived at Caracol, a town situated at the foot of the Andes. Nothing could exceed the inconveni- ences which he experienced in this voyage, from the flies and moschetoes, (an animal resembling our gnat.) “ We were the whole day,” says he, “ in continual motion to keep Our our sufficient defence for the rest of our bodies ; for their stings penetrating through the cloth, caused a very painful and fiery itching. One night, in coming to an anchor near a large and handsome house that was uninhabited, we had no * Buffon, passim. them off ; but at night our torments were excessive, gloves, indeed, were some defence to our hands ; but faces were entirely exposed ; nor were our clothes a THE EARTH. 89 sooner seated ourselves in it, than we were attacked on all sides by swarms of moschetoes, so that it was impossible to have one moment’s quiet. Those who had covered themselves with clothes made for this purpose, found not the smallest defence ; wherefore, hoping to find some relief in the open fields, we ventured out, though in danger of suffering in a more terrible manner from the serpents. But both places were equally obnoxious. On quitting this in- hospitable retreat, we the next night took up our quarters in a house that was inhabited ; the host of which being informed of the terrible manner we had past the night be- fore, gravely told us, that the house we so greatly com- plained of, had been forsaken on account of its being the purgatory of a soul. But we had more reason to believe that it was quitted on account of its being the purgatory of the body. After having journeyed for upwards of three days, through boggy roads, in which the mules at every step sunk up to their bellies, we began at length to per- ceive an alteration in the climate ; and having been long accustomed to heat, we now began to feel it grow sensibly colder. “It is remarkable, that at Tariguagua we often see in- stances of the effects of two opposite temperatures, in two persons happening to meet ; one of them leaving the plains below, and the other descending from the mountain. The former thinks the cold so severe, that he wraps himself up in all the garments he can procure ; while the latter finds the heat so great, that he is scarce able to bear any clothes whatsoever. The one thinks the water so cold, that he avoids being sprinkled by it ; the other is so delighted with its warmth, that he uses it as a bath. Nor is the case very different in the same person, who experiences the same diversity of sensation upon his journey up, and upon his return. This difference only proceeds from the change naturally felt at leaving a climate to which one has been accustomed, and coming into another of an opposite tem- perature. “ The ruggedness of the road from Tariguagua, leading UP the mountain, is not easily described, In some parts, tfte. declivity is so great, that the mules can scarcely keep their footing ; and in others, the acclivity is equally diffi- cult. The trouble of having people going before to mend VOL. I.— 4. M A HISTORY OF 90 the road, the pains arising from the many falls and bruises, and the being constantly wet to the skin, might be sup- ported, were not these inconveniences augmented by the sight of such frightful precipices, and deep abysses, as must fill the mind with ceaseless terror. There are some places where the road is so steep, and yet so narrow, that the mules are obliged to slide down, without making any use of their feet whatsoever. On one side of the rider, in this situation, rises an eminence of several hundred yards ; and on the other, an abyss of equal depth ; so that if he in the least checks his mule, so as to destroy the equilibrium, they both must unavoidably perish. “ After having travelled about nine days in this manner, slowly winding along the side of the mountain, we began to find the whole country covered with an hoar frost ; and an hut, in which we lay, had ice on it. Having escaped many perils, we at length, after a journey of fifteen days, arrived upon the plain, on the extremity of which stands the city of Quito, the capital of one of the most charming regions upon earth. Here, in the centre of the torrid zone, the heat is not only very tolerable, but in some places the cold also is painful. Here they enjoy all the temperature and advantages of perpetual spring ; their fields being always covered with verdure, and en- amelled with flowers of the most lively colours. How- ever, although this beautiful region be higher than any other country in the world, and although it took up so many days of painful journey in the ascent, it is still over- looked by tremendous mountains ; their sides covered with snow, and yet flaming with volcanoes at the top. These seemed piled one upon the other, and rise to a most astonishing height, with great coldness. However, at a determined point above the surface of the sea, the conge- lation is found at the same height in all the mountains. Those parts which are not subject to a continual frost, have here and there growing upon them a rush, resem- bling the genista, but much more soft and flexible. To- wards the extremity of the part where the rush grows, and the cold begins to increase, is found a vegetable, with a round bulbous head, which, when dried, becomes of amazing elasticity. Higher up, the earth is entirely bare of vegetation, and seems covered with eternal snow. The THE EARTH. 91 most remarkable mountains are, that of Cotopaxi (already described as a volcano,) Chimborazo, and Pichincha. Cotopaxi is more than three geographical miles above the surface of the sea : the rest are not much inferior. On the top of the latter was my station for measuring a de- gree of the meridian ; where I suffered particular hard- ships, from the intenseness of the cold, and the violence of the storms. The sky round was, in general, involved in thick fogs, which, when they cleared away, and the clouds, by their gravity, moved nearer to the surface of the earth, they appeared surrounding the foot of the moun- tain, at a vast distance below, like a sea, encompassing an island in the midst of it. When this happened, the horrid noises of tempests were heard from beneath, then discharg- ing themselves on Quito, and the neighbouring country. I saw the lightnings issue from the clouds, and heard the thunders roll far beneath me. All this time, while the tempest was raging below, the mountain top, where I was placed, enjoyed a delightful serenity ; the wind was abated; the sky clear; and the enlivening rays of the sun moderated the severity of the cold. However, this was of no very long duration, for the wind returned with all its violence, and with such velocity as to dazzle the sight; whilst my fears were increased by the dread- ful concussions of the precipice, and the fall of enormous rocks ; the only sounds that were heard in this frightful situation.” Such is the animated picture of these mountains, as given us by this ingenious Spaniard : and I believe the reader will wish that I had made the quotation still longer. A passage over the Alps, or a journey across the Pyre- nees, appear petty trips or excursions in the comparison ; and yet these are the most lofty mountains we know of in Europe. If we compare the Alps with the mountains already described, we shall find them but little more than one half of the height of the former. The Andes, upon being measured by the barometer, are found above three thou- sand one hundred and thirty-six toises or fathoms above the surface of the sea.* Whereas the highest point of the Alps is not above sixteen hundred. The one, in other * Ulloa, vol, i. p. 442. A HISTORY OF 92 words, is above three miles high ; the other about a mile and a half. The highest mountains in Asia are Mount Taurus, Mount Immaus, Mount Caucasus, and the moun- tains of Japan. Of these, none equals the Andes in height; although Mount Caucasus, which is the highest of them, makes very near approaches. Father Verbiest tells of a mountain in China, which he measured, and found a mile and a half high.* In Africa, the mountains of the Moon, famous for giving source to the Niger and the Nile, are rather more noted than known. Of the Peak of Teneriffe, one of the Canary Islands that lie off this coast, we have more certain information. In the year 1727, it was visited by a company of English merchants, who travelled, up to the top, where they observed its height, and the volcano on its very summit.-^ They found it a heap of mountains, the highest of which rises over the rest like a sugar-loaf, and gives a name to the whole mass. It is computed to be a mile and a half perpendicular from the surface of the sea. Kircher gives us an estimate of the heights of most of the other great mountains in the world ; but as he has taken his calculations in general from the ancients, or from modern travellers, who had not the art of measuring them, they are quite incredible. The art of taking the heights of places by the barometer, is a new and an ingenious invention. As the air grows lighter as we ascend, the fluid in the tube rises in due proportion : thus the instrument being properly marked, gives the height with a tolerable degree of exactness ; at least enough to satisfy curiosity. Few of our great mountains have been estimated in this manner ; travellers having, perhaps, been deterred, by a supposed impossibility of breathing at the top. However, it has been invariably found, that the air in the highest that our modern travellers have ascended, is not at all too fine for respiration. At the top of the Peak of Teneriffe, there was found no other inconvenience from the air, except its coldness ; at the top of the Andes, there was no diffi- culty of breathing perceived. The accounts, therefore, of those who have asserted that they were unable to breathe, although at much less heights, are greatly to be suspected. In fact, it is very natural for mankind to paint those * Verbiest, a la Chine. f Phil. Trans, vol. v. THE EARTH. 93 obstacles as insurmountable, which they themselves have not had the fortitude or perseverance to surmount. The difficulty and danger of ascending to the tops of mountains, proceeds from other causes, not the thinness of the air. For instance, some of the summits of the Alps have never yet been visited by man. But the reason is, that they rise with such a rugged and precipitate ascent, that they are utterly inaccessible. In some places they appear like a great wall of six or seven hundred feet high ; in others, there stick out enormous rocks, that hang upon the brow of the steep, and every moment threaten destruction to the traveller below. In this manner almost all the tops of the highest moun- tains are bare and pointed. And this naturally proceeds from their being so continually assaulted by thunders and tempests. All the earthy substances with which they might have been once covered, have for ages been washed away from their summits ; and nothing is left remaining but immense rocks, which no tempest has hitherto been able to destroy. Nevertheless, time is every day, and every hour, making depredations ; and huge fragments are seen tumbling down the precipice, either loosened from the summit by frost or rains, or struck down by lightning. Nothing can exhibit a more terrible picture than one of these enormous rocks, commonly larger than a house, falling from its height, with a noise louder than thunder, and rolling down the side of the mountain. Doctor Plot tells us of one in particular, which being loosened from its bed, tumbled down the precipice, and was partly shattered into a thousand pieces. Notwithstanding, one of the largest fragments of the same, still preserving its motion, travelled over the plain below, crossed a rivulet in the midst, and at last stopped on the other side of the bank ! These fragments, as was said, are often struck off by lightning, and sometimes undermined by rains ; but the most usual manner in which they are disunited from the mountain, is by frost : the rains in- sinuating between the interstices of the mountain, continue there until there comes a frost, and then, when converted into ice, the water swells with an irresistible force, and produces the same effect as gunpowder, splitting the most solid rocks, and thus shattering the summits of the mountain. A HISTORY OF 94 But not rocks alone, but whole mountains are, by various causes, disunited from each other. We see in many parts of the Alps, amazing clefts, the sides of which so exactly correspond with the opposite, that no doubt can be made of their having been once joined together. At Cajeta,* in Italy, a mountain was split in this manner by an earth- quake ; and there is a passage opened through it, that appears as if elaborately done by the industry of man. In the Andes these breaches are frequently seen. That at Thermopyle, in Greece, has been long famous. The moun- tain of the Troglodytes, in Arabia, has thus a passage through it : and that in Savoy, which nature began, and which Victor Amadeus completed, is an instance of the same kind. We have accounts of some of these disruptions, imme- diately after their happening. “ In the month of June,^ in the year 1714, a part of the mountain of Diableret, in the district of Valais, in France, suddenly fell down be- tween two and three o’clock in the afternoon, the weather being very calm and serene. It was of a conical figure, and destroyed fifty-five cottages in the fall. Fifteen per- sons, together with about a hundred beasts, were also crushed beneath its ruins, which covered an extent of a good league square. The dust it occasioned instantly covered all the neighbourhood in darkness. The heaps of rubbish were more than three hundred feet high. They stopped the current of a river that ran along the plain, which is now formed into several new and deep lakes. There appeared, through the whole of this rubbish, none of those substances that seemed to indicate that this disruption had been by means of subterraneous fires. Most probably, the base of this rocky mountain was rotted and decayed ; and thus fell, without any extraneous violence.” In the same manner, in the year 1618, the town of Pleurs, in France, was buried beneath a rocky mountain, at the foot of which it was situated. These accidents, and many more that might be enume- rated of the same kind, have been produced by various causes : by earthquakes, as in the mountain at Cajeta ; or by being decayed at the bottom, as at Diableret. But the most general way is, by the foundation of one part * Buffon, vol. ii. p. 364. f Hist, de l’Acad6mie des Sciences, p. 4. an, 1715 THE EARTH. 95 of the mountain being hollowed by waters, and thus wanting a support, breaking from the other. Thus it generally has been found in the great chasms in the Alps ; and thus it almost always is known in those disruptions of hills, which are known by the name of land-slips. These are nothing more than the slidings down of a higher piece of ground, disrooted from its situation by subterraneous inundations, and settling itself upon the plain below. There is not an appearance in all nature that so much astonished our ancestors, as these land-slips. In fact, to behold a large upland, with its houses, its corn, and cattle, at once loosened from its place, and floating, as it were, upon the subjacent water ; to behold it quitting its ancient situation, and travelling forward like a ship in quest of new adventures ; this is certainly one of the most extraordinary appearances that can be imagined ; and to a people, ignorant of the powers of nature, might well be considered as a prodigy. Accordingly, we find all our old historians mentioning it as an omen of approaching calamities. In this more enlightened age, however, its cause is very well known ; and, instead of exciting ominous apprehensions in the populace, it only gives rise to some very ridiculous law-suits among them, about whose the property shall be ; whether the land which has thus slipt shall belong to the original possessor, or to him upon whose grounds it has encroached and settled. What has been the determination of the judges, is not so well known, but the circum- stances of the slips have been minutely and exactly described. In the lands of Slatberg,* in the kingdom of Iceland, there stood a declivity, gradually ascending for near half a mile. In the year 1713, and on the 10th of March, the inhabitants perceived a crack on its side, somewhat like a furrow made with a plough, which they imputed to the effects of lightning, as there had been thunder the night before. However, on the evening of the same day, they were surprised to hear an hideous confused noise issuing &11 round from the side of the hill ; and their curiosity being raised, they resorted to the place. There, to their amazement, they found the earth, for near five acres, all ln gentle motion, and sliding down the hill upon the * Phil. Trans, vol. iv. p. 250. 96 A HISTORY OF subjacent plain. This motion continued the remaining part of the day, and the whole night ; nor did the noise cease during the whole time ; proceeding, probably, from the attrition of the ground beneath. The day following, how- ever, this strange journey down the hill ceased entirely ; and above an acre of the meadow below xvas found covered with what before composed a part of the declivity. However, these slips, when a whole mountain’s side seems to descend, happen but very rarely. There are some of another kind, however, much more common ; and, as they are always sudden, much more dangerous. These are snow- slips, well known, and greatly dreaded by travellers. It often happens, that when snow has long been accumulated on the tops and on the sides of mountains, it is borne down the precipice, either by means of tempests, or its own melting. At first, when loosened, the volume in motion is but small ; but gathers as it continues to roll ; and, by the time it has reached the habitable parts of the mountain, is generally grown of enormous bulk. Wherever it rolls, it levels all things in its way ; or buries them in unavoidable de- struction. Instead of rolling, it sometimes is found to slide along from the top ; yet even thus it is generally as fatal as before. Nevertheless, we have had an instance, a few years ago, of a small family in Germany, that lived for above a fortnight beneath one of these snow-slips. Al- though they were buried, during that whole time, in utter darkness, and under a bed of some hundred feet deep, yet they were luckily taken out alive ; the weight of the snow being supported by a beam that kept up the roof ; and nourishment being supplied them by the milk of an ass, if I remember right, that was buried under the same ruin. But it is not the parts alone that are thus found to sub- side, whole mountains have been known totally to dis- appear. Pliny tells us,* that in his own time the lofty mountain of Cybotus, together with the city of Eurites, were swallowed by an earthquake. The same fate, he says, attended Phlegium, one of the highest mountains in Ethiopia; which, after one night’s concussion, was never seen more. In more modern times, a very noted moun- tain in the Molucca islands, known by the name of the * Plin. lib. ii. cap. 93. THE EARTII. 97 Peak, and remarkable for being seen at a very great dis- tance from sea, was swallowed by an earthquake; and nothing but a lake was left in the place where it stood. Thus, while storms and tempests are levelled against moun- tains above, earthquakes and waters are undermining them below. All our histories * talk of their destruction ; and very few new ones (if we except mount Cenere, and one or two such heaps of cinders,) are produced. If moun- tains, therefore, were of such great utility as some philo- sophers make them to mankind, it would be a very me- lancholy consideration that such benefits were diminish- ing every day. But the truth is, the valleys are fertilized by that earth which is washed from their sides ; and the plains become richer, in proportion as the mountains CHAP. XIII. OF WATER. In contemplating nature, we shall often find the same substances possessed of contrary qualities, and producing opposite effects. Air, which liquefies one substance, dries up another. That fire which is seen to burn up the desert, is often found, in other places, to assist the luxuriance of vegetation ; and water, which, next to fire, is the most fluid substance upon earth, nevertheless gives all other bodies their firmness and durability ; so that every element seems to be a powerful servant, capable either of good or ill, and only awaiting external direction, to become the friend or the enemy of mankind. These opposite qualities, in this sub- stance in particular, have not failed to excite the admiration and inquiry of the curious. That water is the most fluid penetrating body, next to fire, and the most difficult to confine, is incontestibly proved by a variety of experiments. A vessel through which water cannot pass, may be said to retain any thing, ft may be objected, indeed, that syrups, oils, and honey, ftak through some vessels that water cannot pass through ; hut this is far from being the result of the greater tenuity a*rd fineness of their parts ; it is owing to the rosin where- with the wrood of such vessels abounds, which oils and vol. i. — 4. N A HISTORY OF 98 syrups have a power of dissolving; so that these fluids, instead of finding their way, may more properly be said to eat their way through the vessels that contain them. How- ever, water will at last find its way even through these ; for it is known to escape through vessels of every sub- stance, glass only excepted. Other bodies may be found to make their way out more readily indeed ; as air, when it finds a vent, will escape at once ; and quicksilver, be- cause of its weight, quickly penetrates through whatever chinky vessel confines it : but water, though it operates more slowly, yet always finds a more certain issue. As, for instance, it is well known that air will not pass through leather ; which water will very readily penetrate. Air also may be retained in a bladder ; but water will quickly ooze through. And those who drive this to the greatest de- gree of precision, pretend to say, that it will pass through pores ten times smaller than air can do. Be this as it may, we are very certain that its parts are so small, that they have been actually driven through the pores of gold. This has been proved by the famous Florentine experi- ment, in which a quantity of water was shut up in a hol- low ball of gold, and then pressed with a huge force by screws, during which the fluid was seen to ooze out through the pores of the metal, and to stand, like a dew, upon its surface. As water is thus penetrating, and its parts thus minute, it may easily be supposed that they enter into the compo- sition of all bodies, vegetable, animal, and fossil. This every chymist’s experience convinces him of ; and the mix- ture is the more obvious, as it can always be separated, by a gentle heat, from those substances with which it had been united. Fire, as was said, will penetrate where water cannot pass ; but then it is not so easily to be separated. But there is scarce any substance from which its water cannot be divorced. The parings or filings of lead, tin, and antimony, by distillation, yield water plentifully: the hardest stones, sea-salt, nitre, vitriol, and sulphur, are found to consist chiefly of water ; into which they resolve by force of fire. “ All birds, beasts, and fishes,” says Newton, “ insects, trees, and vegetables, with their parts, grow from water; and, by putrefaction, return to water again.” In short, almost every substance that we see. THE EARTH. 99 owes its texture and firmness to the parts of water that mix with its earth ; and, deprived of this fluid, it becomes a mass of shapeless dust and ashes. From hence we see, as was above hinted, that this most fluid body, when mixed with others, gives them consistence and form. Water, by being mixed with earth or ashes, and formed into a vessel, when baked before the fire, becomes a coppel, remarkable for this, that it will bear the utmost force of the hottest furnace that art can contrive. So the Chinese earth, of which porcelain is made, is nothing more than an artificial composition of earth and water, united by heat ; and which a greater degree of heat could easily separate. Thus we see a body, extremely fluid of itself, in some measure assuming a new nature, by being united with others : we see a body, whose fluid and dissolving qualities are so obvious, giving consistence and hardness to all the substances of the earth. From considerations of this kind, Thales, and many of the ancient philosophers, held that all things were made of water. In order to confirm this opinion, Helmont made an experiment, by divesting a quantity of earth of all its oils and salts, and then putting this earth, so prepared, into an earthen pot, which nothing but rain-water could enter, and planting a willow therein ; this vegetable, so planted, grew up to a considerable height and bulk, merely from the accidental aspersion of rain-water; while the earth, in which it was planted, received no sensible diminution. From this experiment, he concluded, that water was the only nourishment of the vegetable tribe; and that vege- tables, being the nourishment of animals, all organized substances, therefore, owed their support and being only to water. But this has been said by Woodward to be a mistake: for he shews, that water being impregnated with earthy particles, is only the conveyer of such sub- stances into the pores of vegetables, rather than an in- creaser of them by its own bulk : and likewise, that water is ever found to afford so much less nourishment, in propor- tion as it is purified by distillation. A plant in distilled water will not grow so fast as in water not distilled : and if the same be distilled three or four times over, the ‘ plant will scarcely grow at all, or receive any nourishment from it. So that water, as such, does not seem the proper nou- A HISTORY OF 100 rishment of vegetables, but only the vehicle thereof, which contains the nutritious particles, and carries them through all parts of the plant. Water, in its pure state, may suffice to extend or swell the parts of a plant, but affords vegetable matter in a moderate proportion. However this be, it is agreed on all sides, that water, such as we find it, is far from being a pure simple sub- stance. The most genuine we know is mixed with exha- lations and dissolutions of various kinds ; and no expedient that has been hitherto discovered, is capable of purifying it entirely. If we filter and distil it a thousand times, ac- cording to Boerhaave, it will still depose a sediment : and by repeating the process we may evaporate it entirely away, but can never totally remove its impurities. Some, however, assert, that water, properly distilled, will have no sediment ;* and that the little white speck which is found at the bottom of the still, is a substance that enters from without. Kircher used to shew, in his Museum, a phial of water that had been kept for fifty years, hermeti- cally sealed ;-f~ during which it had deposed no sediment, but continued as transparent as when first it was put in. How far, therefore, it may be brought to a state of purity by distillation, is unknown ; but we very well know, that all such water as we every where see, is a bed in which plants, minerals, and animals, are all found confusedly floating together. Rain-water, which is a fluid of Nature’s own distilling, and which has been raised so high by evaporation, is never- theless a very mixed and impure substance. Exhalations of all kinds, whether salts, sulphurs, or metals, make a part of its substance, and tend to increase its weight. If we gather the water that falls, after a thunder-clap, in a sultry summer’s day, and let it settle, we shall find a real salt sticking at the bottom. In winter, however, its im- pure mixtures are fewer, but still may be separated by distillation. But as to that which is generally caught * Hill’s History of Fossils. t Hermetically sealing a glass vessel, means no more than heating the mouth of the phial red hot ; and thus when the glass is become pliant, squeezing the mouth together with a pair of pincers, and then twisting it six or seven times round, which effectfully closes it up. THE EARTH. 101 pouring from the tops of houses, it is particularly foul, being impregnated with the smoke of the chimnies, the vapour of the slates or tiles, and with other impurities that birds and animals may have deposited there. Besides, though it should be supposed free from all these, it is mixed with a quantity of air, which, after being kept for some time, will be seen to separate. Spring-water is next in point of purity. This, according to Dr. Halley, is collected from the air itself ; which being sated with water, and coming to be condensed by the evening’s cold, is driven against the tops of the mountains, where being condensed and collected, it trickles down by the sides, into the cavities of the earth ; and running for a while underground, bubbles up in fountains upon the plain. This having made but a short circulation, has generally had no long time to dissolve or imbibe any foreign substances by the way. River-water is generally more foul than the former. — Wherever the stream flows, it receives a tincture from its channel. Plants, minerals, and animals, all contribute to add to its impurities : so that such as live at the mouths of great rivers, are generally subject to all those disorders which contaminated and unwholesome waters are known to produce. Of all the river-water in the world, that of the Indus and the Thames is said to be the most light and wholesome. The most impure fresh water that we know, is that of stagnating pools and lakes, which, in summer, may be more properly considered as a jelly of floating insects, than a collection of water. In this, millions of little reptiles, undisturbed by any current, which might crush their frames to pieces, breed and engender. The whole teems with shapeless life, and only grows more fruitful by increasing putrefaction. Of the purity of all these waters, the lightness, and not the transparency, ought to be the test. Water may be extremely clear and beautiful to the eye, and yet very much impregnated with mineral particles. In fact, sea- water is the most transparent of any, and yet it is well known to contain a large mixture of salt and bitumen. On the contrary, those waters which are lightest, have the fewest dissolutions floating in them ; and may, therefore. A HISTORY OF 102 be the most useful for all the purposes of life. But, after all, though much has been said upon this subject, and although waters have been weighed with great assiduity, to determine their degree of salubrity, yet neither this, nor their curdling with soap, nor any other philosophical stan- dard whatsoever, will answer the purposes of true informa- tion. Experience alone ought to determine the useful or noxious qualities of every spring; and experience assures us, that different kinds of water are adapted to different constitutions. An incontestible proof of this, are the many medicinal springs throughout the world, whose peculiar benefits are known to the natives of their respective coun- tries. These are of various kinds, according to the dif- ferent minerals with which they are impregnated; hot, saline, sulphureous, bituminous, and oily. But the account of these will come most properly under that of the several minerals by which they are produced. After all, therefore, we must be. contented with but an impure mixture for our daily beverage. And yet, perhaps, this very mixture may often be more serviceable to our health than that of a purer kind. We know that it is so with regard to vegetables : and why not, also, in general, to man ? Be this as it will, if we are desirous of having water in its greatest purity, we are ordered, by the curious in this particular, to distil it from snow, gathered upon the tops of the highest mountains, and to take none but the outer and superficial part thereof. This we must be satisfied to call pure water; but even this is far short of the pure unmixed philosophical element; which, in reality, is no where to be found. As water is thus mixed with foreign matter, and often the repository of minute animals, or vegetable seeds,, we need not be surprised that, when carried to sea, it is always found to putrefy. But we must not suppose that it is the element itself which thus grows putrid and offensive, but the substances with which it is impregnated. It is true, the utmost precautions are taken to destroy all vegetable and animal substances that may have previously been lodged in it, by boiling ; but, notwithstanding this, there are some that will still survive the operation, and others that find their way during the time of its stowage. Seamen, therefore, assure us, that their water is generally found to THE EARTH. 103 putrefy twice, at least, and sometimes three times, in a long voyage. In about a month after it has been at sea, when the bung is taken out of the cask, it sends up a noisome and dangerous vapour, which would take fire upon the application of a candle.* The whole body of the water then is found replete with little worm-like insects, that float, with great briskness, through all its parts. These generally live for about a couple of days ; and then dying, by depositing their spoils, for a while increase the putrefac- tion. After a time, the heavier parts of these sinking to the bottom, the lighter float in a scum, at the top ; and this is what mariners call, the water’s purging itself. There is still, however, another race of insects, which are bred, very probably, from the spoils of the former ; and produce, after some time, similar appearances : these dying, the water is then thought to change no more. However, it very often happens, especially in hot climates, that nothing can drive these nauseous insects from the ship’s store of water. They often increase to a very disagreeable and frightful size, so as to deter the mariner, though parching with thirst, from tasting that cup which they have contaminated. This water, as thus described, therefore, is a very different fluid from that simple elementary substance upon which philosophical theories have been founded; and concerning the nature of which there have been so many disputes. Elementary water is no way compounded ; but is without taste, smell, or colour; and incapable of being discerned by any of the senses, except the touch. This is the famous dissolvent of the chymists, into which, as they have boasted, they can reduce all bodies ; and which makes up all other substances, only by putting on a different disguise. In some forms, it is fluid, transparent, and evasive of the touch ; in others, hard, firm, and elastic. In some, it is stiffened by cold ; in others, dissolved by fire. According to them, it only assumes external shapes from accidental causes ; but the mountain is as much a body of water, as the cake of ice that melts on its brow ; and even the philosopher himself is composed of the same materials with the cloud or meteor which he contemplates. * Phil. Trans, vol v. part ii. p. 71. A HISTORY OF 104 Speculation seldom rests when it begins. Others, dis- allowing the universality of this substance, will not allow that in a state of nature there is any such thing as water at all. “ What assumes the appearance,” say they, “ is nothing more than melted ice. Ice is the real element of Nature’s making; and when found in a state of fluidity, it is then in a state of violence. All substances are natu- rally hard; but some more readily melt with heat than others. It requires a great heat to melt iron ; a smaller heat will melt copper; silver, gold, tin, and lead, melt with smaller still ; ice, which is a body like the rest, melts with a very moderate warmth ; and quicksilver melts with the smallest warmth of all. Water, therefore, is but ice hept in continual fusion ; and still returning to its former state, when the heat is taken away.” Between those op- posite opinions, the controversy has been carried on with great ardour, and much has been written on both sides ; and yet, when we come to examine the debate, it will pro- bably terminate in this question, whether cold or heat first began their operations upon water? This is a fact of very little importance, if known ; and, what is more, it is a fact we can never know. Indeed, if we examine into the operations of cold and heat upon water, we shall find that they produce somewhat similar effects.. Water dilates in its bulk, by heat, to a very con- siderable degree ; and, what is more extraordinary, it is like- wise dilated by cold in the same manner. If water be placed over a fire, it grows gradually larger in bulk, as it becomes hot, until it begins to boil ; after which no art can either increase its bulk or its heat. By increasing the fire, indeed, it may be more quickly evapo- rated away ; but its heat and its bulk still continue the same. By the expanding of this fluid, by heat, philoso- phers have found a way to determine the warmth or the coldness of other bodies ; for if put into a glass tube, by its swelling and rising, it shews the quantity of heat in the body to which it is applied ; and by its contracting and sinking, it shews the absence of the same. Instead of using water in this instrument, which is called a thermo- meter, they now make use of spirit of wine, which is not apt to. freeze, and which is endued even with a greater expansion, by heat, than water. The instrument consists THE EARTH. 105 of nothing more than a hollow ball of glass, with a long tube growing out of it. This being partly filled with spirits of wine tinctured red, so as to be seen when it rises, the ball is plunged into boiling water, which making the spirit within expand and rise in the tube, the water marks the greatest height to which it ascends ; at this point the tube is to be broken off, and then hermetrically sealed, by melting the glass with a blow-pipe: a scale being placed by the side, completes the thermometer. Now as the fluid expands or condenses with heat or cold, it will rise and fall in the tube in proportion ; and the degree or quantity of ascent or de- scent will be seen in the scale. No fire, as was said, can make water hotter, after it begins to boil. We can, therefore, at any time be sure of an equa- ble certain heat ; which is that of boiling water, which is in- variably the same. The certainty of such a heat is not less useful than the instrument that measures it. It affords a standard, fixed degree of heat over the whole world ; boiling water being as hot in Greenland as upon the coast of Guinea. One fire is more intense than another ; of heat there are vari- ous degrees ; but boiling water is a heat every where the same, and easily procurable. As heat thus expands water, so cold, when it is violent enough to freeze the same, produces exactly the same effect, and expands it likewise. Thus water is acted upon in the same manner by two opposite qualities ; being di- lated by both. As a proof that it is dilated by cold, we have only to observe the ice floating on the surface of a pond, which it would not do were it not dilated, and grown more bulky, by freezing, than the water which remains unfroze. Mr. Boyle, however, put the matter past a doubt, by a variety of experiments.* Having poured a proper quantity of water into a strong earthen vessel, he exposed it, uncovered, to the open air, in frosty nights ; and observed, that continually the ice reached higher than the water before it was frozen. He filled also a tube with water, and stopped both ends with wax : the water, when frozen, was found to push out the stopples from both ends ; and a rod of ice appeared at each end of the tube, which shewed how much it was swollen by the cold within. vol. i. — 5. * Boyle, vol. i. p. 610. o A HISTORY OF 106 From hence, therefore, we may be very certain of the cold dilating of the water; and experience also shews, that the force of this expansion has been found as great as any which heat has been found to produce. The touch-hole of a strong gun-barrel being stopped, and a plug of iron forcibly driven into the muzzle, after the bar- rel had been filled with water, it was placed in a mixture of ice and salt; the plug, though soldered to the barrel, at first gave way, but being fixed in more firmly, within a quarter of an hour the gun -barrel burst with a loud noise, and blew up the cover of the box wherein it lay. Such is its force in an ordinary experiment. But it has been known to burst cannons, filled with water, and then left to freeze ; for the cold congealing the water, and the ice swelling, it became irresistible. The bursting of rocks by frost, which is frequent in the northern climates, and is sometimes seen in our own, is an equal proof of the ex- pansion of congealed water. For having by some means insinuated itself into the body of the rock, it has remained there till the cold was sufficient to affect it by congelation. But when once frozen, no obstacle is able to confine it from dilating ; and, if it cannot otherwise find room, the rock must burst asunder. This alteration in the bulk of water might have served as a proof that it was capable of being compressed into a narrower space than it occupied before; but, till of late, water was held to be incompressible. The general opinion was, that no art whatsoever could squeeze it into a nar- rower compass ; that no power on earth, for instance, could force a pint of water into a vessel that held an hair’s-breadth less than a pint. And this, said they, ap- pears from the famous Florentine experiment ; where the water, rather than suffer a compressure, was seen to ooze through the pores of the solid metal ; and, at length, mak- ing a cleft in the side, spun out with great vehemence. But later trials have proved that water is very compressi- ble, and partakes of that elasticity which every other body possesses in some degree. Indeed, had not mankind been dazzled by the brilliancy of one inconclusive experi- ment, there were numerous reasons to convince them of its having the same properties with other substances. Ice, which is water in another state, is very elastic. A stone. THE EARTH. 107 flung slantingly along the surface of a pond, bounds from the water several times ; which shews it to be elastic also. But the trials of Mr. Canton have put this past all doubt ; which being somewhat similar to those of the great Boyle, who pressed it with weights properly applied, carry sufficient conviction. What has been hitherto related, is chiefly applicable to the element of water alone; but its fluidity is a property that it possesses in common with several other sub- stances, in other respects greatly differing from it. That quality which gives rise to the definition of the fluid, namely, that its parts are in a continual intestine motion, seems extremely applicable to water. What the shapes of those parts are, it would be vain to attempt to discover. Every trial only shews the futility of the attempt; all we find is, that they are extremely minute ; and that they roll over each other with the greatest ease. Some, indeed* from this property alone, have not hesitated to pronounce them globular ; and we have, in all our hydrostatical books, pictures of these little globes in a state of sliding and roll- ing over each other. But all this is merely the work of imagination ; we know that substances of any kind, re- duced very small, assume a fluid appearance, somewhat resembling that of water. Mr. Boyle, after finely pow- dering and sifting a little dry powder of plaster of Paris, put it in a vessel over the fire, where it soon began to boil fixe water, exhibiting all the motions and appearances of a boiling liquor. Although but a powder, the parts of which we know are very different from each other, and just as accident has formed them, yet it heaved in great waves like water. Upon agitation, a heavy body will sink to the bottom, and a light one emerge to the top. There is no reason, then, to suppose the figure, of the parts of water round, since we see their fluidity very well imitated by a composition, the parts of which are of vari- ous forms and sizes. The shape of the parts of water, there- fore, we must be content to continue ignorant of. All we know is, that earth, air, and fire, conduce to separate the parts from each other. Earthy substances divide the parts from each other, and keep them asunder. This division may be so great, that me water will entirely lose its fluidity thereby. MudL A HISTORY OF 108 potter’s clay, and dried bricks, are but so many different combinations of earth and water ; each substance in which the parts of water are most separated from each other, appearing to be the most dry. In some substances, in- deed, where the parts of water are greatly divided, as in porcelain, for instance, it is no easy matter to recover and bring them together again ; but they continue in a manner fixed and united to the manufactured clay. This circum- stance led Doctor Cheney into a very peculiar train of thinking. He suspected that the quantity of water, on the surface of the earth, was daily decreasing. For, says he, some parts of it are continually joined to vegetable, animal, and mineral substances, which no art can again recover. United with these, the water loses its fluidity ; for if, con- tinues he, we separate a few particles of any fluid, and fasten them to a solid body, or keep them asunder, they will be fluid no longer. To produce fluidity, a considerable num- ber of such particles are required ; but here they are close, and destitute of their natural properties. Thus, according to him, the world is growing every day harder and harder, and the earth firmer and firmer : and there mav come a time , j when every object around us may be stiffened in universal frigidity ! However, we have causes enough of anxiety in this world already, not to add this preposterous concern to the number. That air also contributes to divide the parts of water, we can have no manner of doubt ; some have even dis- puted whether water be not capable of being turned into air. However, though this cannot be allowed, it must be granted, that it may be turned into a substance which greatly resembles air (as we have seen in the experiment of the seolipile) with all its properties ; except that, by cold, this new-made air may be condensed again into water. But of all the substances which tend to divide the parts of water, fire is the most powerful. Water, when heated into steam, acquires such force, and the parts of it tend to fly off from each other with such violence, that no earthly substance we know of is strong enough to confine them. A single drop of water, converted into steam, has been found capable of raising a weight of twenty tons ; and would have raised twenty thousand, were the vessel con- THE EARTH. 109 fining it sufficiently strong, and the fire below increased in proportion. From this easy yielding of its parts to external pres- sure, arises the art of determining the specific gravity of bodies by plunging them in water ; with many other use- ful discoveries in that part of natural philosophy, called hydrostatics . The laws of this science, which Archimedes began, and Pascal, with some other of the moderns, have much improved, rather belongs to experimental than to natural history. However, I will take leave to mention some of the most striking paradoxes in this branch of science, which are as well confirmed by experiment, as rendered universal by theor\ . It would, indeed, be un- pardonable, while discoursing on the properties of water, to omit giving some account of the manner in which it sustains such immense bulks as we see floating upon its soft and yielding surface: how some bodies, that are known to sink at one time, swim with ease, if their sur- face be enlarged : how the heaviest body, even gold itself, may be ' made to swim upon water ; and how the lightest, such as cork, shall remain sunk at the bottom : how the pouring in of a single quart of water, will burst a hogshead hooped with iron : and how it ascends, in pipes, from the valley, to travel over the mountain : these are circumstances that are at first surprising ; but, upon a slight consideration, lose their wonder. *In order to conceive the manner in which all these wonders are effected, we must begin by observing that water is possessed of an invariable property, which has not hitherto been mentioned; that of always keeping its surface level and even. Winds, indeed, may raise it into waves, or art spurt it up in fountains ; but ever, when left to itself, it sinks into a smooth even surface, of which no one part is higher than another. If I should pour water, for instance, into the arm of a pipe of the shape of the letter U, the fluid would rise in the other arm just to the same height; because, otherwise, it would not find its level, which it invariably maintains. A pipe bending * In the above sketch, the manner of demonstrating used by Monsieur D Alembert is made use of, as the most obvious, and the most satisfac- tory, Vide Essai sur, &c. A HISTORY OF no from one hill down into the valley, and rising by another, may be considered as a tube of this kind, in which the water, sinking in one arm, rises to maintain its level in the other. Upon this principle all water-pipes depend ; which can never raise the water higher than the fountain from which they proceed. Again, let us suppose for a moment, that the arms of the pipe already mentioned, may be made long or short at pleasure ; and let us still further suppose, that there is some obstacle at the bottom of it, which prevents the water poured into one arm, from rising in the other. Now it is evident, that this obstacle at the bottom will sustain a pressure from the water in one arm, equal to what would make it rise in the other ; and this pressure will be great, in proportion as the arm filled with water is tall. We may, therefore, generally conclude, that the bottom of every vessel is pressed by a force, in proportion to the height of the water in that vessel. For instance, if the vessel filled with water be forty feet high, the bottom of that vessel will sustain such a pressure as would raise the same water forty feet high, which is veiy great. From hence we see how extremely apt our pipes, that convey water to the city, are to burst ; for descending from a hill of more than forty feet high, they are pressed by the water contained in them, with a force equal to what would raise it to more than forty feet high ; and that this is sometimes able to burst a wooden pipe, we can have no room to doubt of. Still recurring to our pipe, let us suppose one of lts arms ten times as thick as the other ; this will produce n° effect whatsoever upon the obstacle below, which we sup* posed hindering its rise in the other arm ; because, ho thick soever the pipe may be, its contents would only A® ; and it will, therefore, press the obstac to its own level ally with a force equal thereto. We may, therefore, univers ^ conclude, that the bottom of any vessel is pressed by ^ water, not as it is broad or narrow, but in proportioti it is high. Thus the water contained in a vessel not t than my finger, presses its bottom as forcibly as the ^ contained in an hogshead of an equal height; and, made holes in the bottoms of both, the water wou . out as forceful from the one as the other. Hence THE EARTH. Ill with great ease, burst an hogshead with a single quart of water; and it has been often done. We have only,* for this, to place an hogshead on one end, filled with water : we then bore a hole in its top, into which we plant a narrow tin pipe, of about thirty feet high : by pouring a quart of water into this, at the top, as it continues to rise higher in the pipe, it will press more forcibly on the bottom and sides of the hogshead below, and at last burst it. Still returning to our simple instrument of demonstration. If we suppose the obstacle at the bottom of the pipe to be moveable, so as that the force of the water can push it up into the other arm ; such a body as quicksilver, for instance. Now, it is evident, that the weight of water weighing down upon this quicksilver in one arm, will at last press it up in the other arm ; and will continue to press it upwards, until the fluid in both arms be upon a par. So that here we actually see quicksilver, the heaviest substance in the world, except gold and platina, floating upon a water, which is but a very light substance. When we see water thus capable of sustaining quick- silver, we need not be surprised that it is capable of float- lng much lighter substances, ships, animals, or timber. When any thing floats upon water, we always see that a part of it sinks in the same. A cork, a ship, a buoy, each buries itself in a bed on the surface of the water ; this bed niay be considered as so much water displaced ; the water ’ therefore, lose so much of its own weight, as is equal u the weight of that bed of water which it displaces. If . e body be heavier than a similar bulk of water, it will ^ink; if lighter, it will swim. Universally, therefore, a ea ‘Vi ^unSed in water, loses, as much of its weight as is glUa to the weight of a body of water of its own bulk. tbeh-6 • ^ bodies, therefore, such as cork, lose much of bodi and therefore swim; other more ponderous ivat;rS Slnb> because they are heavier than their bulk of s*mP*e theorem entirely depends the art of instanclb Petals . hydrostatically. I have a guinea, for have We’. ana desire to know whether it be pure gold ; I find it ev. i ** *n usual way with another guinea, and act y of the same weight, but still I have some * Nollet’s Lectures. A HISTORY OF 112 suspicion, from its greater bulk, that it is not pure. In order to determine this, I have nothing more to do than to weigh it in water with that same guinea that I know to be good, and of the same weight ; and this will instantly shew the difference ; for the true ponderous metal will sink, and the false bulky one will be sustained in proportion to the greatness of its surface. Those whose business it is to examine the purity of metals, have a balance made for this purpose, by which they can precisely determine which is most ponderous, or, as it is expressed, which has the greatest specific gravity. Seventy-one pound and a half of quick- silver, is" found to be equal in bulk to a hundred pound weight of gold. In the same proportion sixty of lead, fifty- four of silver, forty-seven of copper, forty-five of brass, forty-two of iron, and thirty-nine of tin, are each equal to an hundred pound of the same most ponderous of all metals. This method of precisely determining the purity of gold, by weighing in water, was first discovered by Archimedes, to whom mankind have been indebted for many useful discoveries. Hiero, king of Sicily, having sent a certain quantity of gold to be made into a crown, the workman, it seems, kept a part for his own use, and supplied the deficiency with a baser metal. His fraud was suspected by the king, but could not be detected ; till he applied to Archimedes, who weighed the crown in water ; and, by this method, informed the king of the quantity of gold which was taken away. It has been said, that all fluids endeavour to preserve their level; and, likewise, that a body pressing on the surface, tended to destroy that level. From hence, there- fore, it will easily be inferred, that the deeper any body sinks, the greater will be the resistance of the depressed fluid beneath. It will be asked, therefore, as the resist- ance increases in proportion as the body descends, how comes the body, after it has got a certain way, to sink at all ? The answer is obvious : From the fluid above pressing it down with almost as great a force as the fluid beneath presses it up. Take away, by any art, the pressure of the fluid from above, and let only the resistance of the fluid from below be suffered to act, and after the body *s gone down very deep, the resistance will be insuper- THE EARTH. 113 able. To give an instance : A small hole opens in the bottom of a ship at sea, forty feet we will suppose below the surface of the water ; through this the water bursts up with great violence ; I attempt to stop it with my hand, but it pushes the hand violently away. Here the hand is, in fact, a body attempting to sink upon water, at a depth of forty feet, with the pressure from above taken away. The water, therefore, will overcome my strength; and will continue to burst in till it has got to its level : if I should then dive into the hold, and clap my hand upon the opening, as before, I should perceive no force acting against my hand at all ; for the water above presses the hand as much down against the hole, as the water with- out presses it upward. For this reason, also, when we dive to the bottom of the water, we sustain a very great pressure from above, it is true, but it is counteracted by the pressure from below ; and the whole acting uniformly on the surface of the body, wraps us close round without injury. As I have deviated thus far, I will just mention one or two properties more, which water, and all such like fluids, is found to possess. And, first, their ascending in vessels which are emptied of air, as in our common pumps for instance. The air, however, being the agent in this case, we must previously examine its properties, before we un- dertake the explanation. The other property to be men- tioned is, that of their ascending in small capillary tubes. This is one of the most extraordinary and inscrutable appearances in nature. Glass tubes may be drawn, by means of a lamp, as fine as a hair ; still preserving their hollow within. If one of these be planted in a vessel of water, or spirit of wine, the liquor will immediately be seen to ascend ; and it will rise higher, in proportion as the tube is smaller ; a foot, two feet, and more. How does this come to pass ? Is the air the cause ? No : the liquor rises, although the air be taken away. Is attrac- tion the cause P No : for quicksilver does not ascend, which it otherwise would. Many have been the theories °f experimental philosophers to explain this property. Such as are fond of travelling in the regions of conjec- ture, may consult Hawksbee, Morgan, Jurin, or Watson, who have examined the subject with great minuteness. VOL. I, — 5. F 114 A HISTORY OP Hitherto, however, nothing but doubts, instead of know- ledge, have been the result of their inquiries. It will not, therefore, become us to enter into the minuteness of the inquiry, when we have so many greater wonders to call oui attention away.# CHAP. XIV. OF THE ORIGIN OF RIVERS. The sun ariseth, and the sun goeth down, and pants u for the place from whence he arose. All things are filled “ with labour, and man cannot utter it. All rivers run “ into the sea, yet the sea is not full. Unto the place “ whence the rivers come, thither they return again. The “ eye is not satisfied with seeing, nor the ear with hear- “ ing.”-'f~ Thus speaks the wisest of the Jews. And at so early a period was the curiosity of man employed in observing these great circulations of nature. Every eye attempted to explain those appearances ; and every phi- losopher who has long thought upon the subject, seems to give a peculiar solution. The inquiry whence rivers are produced ; whence they derive those unceasing stores of water, which continually enrich the world with fertility and verdure ; has been variously considered, and divided the opinions of mankind more than any other topic in natural history. In this contest the various champions may be classed under two leaders ; Mr. De la Hire, who contends that rivers must be supplied from the sea, strained through * This phenomenon, which has so long embarrassed philosophers, is easily soluble upon the principle, that the attraction between the particles of glass and water is greater than the attraction between the particles of water themselves : for, if a glass tube be held parallel to the horizon, and a drop of water be applied to the under side of the tube, it will adhere to it : nor will it fall from the glass, till its bulk and gravity are so far increased as to overbalance the attraction of the glass. Hence it is easy to conceive, how sensibly such a power must act on the surface of a fluid not viscid, as water, contained within the cavity of a small glass tube ; as also that the quantity of the fluid raised, will be as the surface of the bore which it fills, that is, as the diameter of the tube. f Ecclesiastes, chap, i. ver. 5, 7, 8. THE EARTH. 115 the pores of the earth ; and Dr. Halley, who has endea- voured to demonstrate that the clouds alone are sufficient for the supply. Both sides have brought in mathematics to their aid ; and have shewn that long and laborious cal- culations can at any time be made to obscure both sides of a question. De la Hire* begins his proofs, that rain-water, evapo- rated from the sea, is insufficient for the production of rivers ; by shewing that rain never penetrates the surface of the earth above sixteen inches. From thence he infers, that it is impossible for it, in many cases, to sink so as to be found at such considerable depths below. Rain-water, he grants, is often seen to mix with rivers, and to swell their currents ; but a much greater part of it evaporates. “ In fact,” continues he, “ if we suppose the earth every where covered with water, evaporation alone would be sufficient to carry off two feet nine inches of it in a year : and yet we very well know, that scarcely nineteen inches of rain-water falls in that time ; so that evaporation would carry off a much greater quantity than is ever known to descend. The small quantity of rain-water that falls is, therefore, but barely sufficient for the purposes of vegeta- tion. Two leaves of a fig-tree have been found, by ex- periment, to imbibe from the earth, in five hours and a half, two ounces of water. This implies the great quantity of fluid that must be exhausted in the maintenance of one single .plant. Add to this, that the waters of the river Rungis will, by calculation, rise to fifty inches ; and the whole country from whence they are supplied never receives fifty inches in the year by rain. Besides this, there are many salt springs, which are known to proceed immediately from the sea, and are subject to its flux and reflux. In short, wherever we dig beneath the surface of the earth, except in a very few instances, water is to be found : and it is by this subterraneous water that springs and rivers, nay, a great part of vegetation itself, is supported. It is this subterraneous water which is raised into steam, by the internal heat of the earth, that feeds plants. It is this subterraneous water that distils through interstices ; and there, cooling, forms fountains. * Hist, de l’Acad. 1713, p. 56. A HISTORY OF 116 It is this, that by the addition of rains, is increased into rivers, and pours plenty over the whole earth.” On the other side of the question,* it is asserted, that the vapours which are exhaled from the sea, and driven by the winds upon land, are more than sufficient to sup- ply not only plants with moisture, but also to furnish a sufficiency of water to the greatest rivers. For this pur- pose, an estimate has been made of the quantity of water emptied at the mouths of the greatest rivers ; and of the quantity also raised from the sea by evaporation ; and it lias been found, that the latter by far exceeds the former. This calculation was made by Mr. Marriotte. By him it was found, upon receiving such rain as fell in a year, in a proper vessel fitted for that purpose ; that, one year with another, there might fall about twenty inches of water upon the surface of the earth, throughout Europe. It was also computed that the river Seine, from its source to the city of Paris, might cover an extent of ground, that would supply it annually with above seven millions of cubic feet of this water, formed by evaporation. But upon computing the quantity which passed through the arches of one of its bridges in a year, it was found to amount only to two hundred and eighty millions of cubic feet, which is not above the sixth part of the former num- ber. Hence it appears, that this river may receive a sup- ply, brought to it by the evaporated waters of the sea, six times greater than what it gives back to the sea by its cur- rent ; and, therefore, evaporation is more than sufficient for maintaining the greatest rivers, and supplying the purposes also of vegetation. In this manner, the sea supplies sufficient humidity .to the air, for furnishing the earth with all necessary mois- ture. One part of its vapours fall upon its own bosom, before they arrive upon land. Another part is arrested by the sides of mountains, and is compelled, by the rising stream of air, to mount upward towards the summits. Here it is presently precipitated, dripping down by the crannies of the stone. In some places, entering into the caverns of the mountain, it gathers in those receptacles, which being once filled, all the rest overflows ; and break- ing out by the sides of the hills, forms single springs. * Phil. Trans, vol. ii. p. 128. THE EARTH 117 Many of these run down by the vallies or guts between the ridges of the mountain, and, coming to unite, form little rivulets or brooks ; many of these meeting in one common valley, and gaining the plain ground, being grown less rapid, become a river ; and many of these uniting, make such vast bodies of water as the Rhine, the Rhone, and the Danube. There is still a third part, which falls upon the lower grounds, and furnishes plants with their wonted supply. But the circulation does not rest even here ; for it is again exhaled into vapour By the action of the sun ; and after- wards returned to that great mass of waters whence it first arose. “ This,” adds Dr. Halley, “ seems the most rea- sonable hypothesis ; and much more likely to be true, than that of those who derive all springs from the filtering of the sea-waters, through certain imaginary tubes or passages within the earth ; since it is well known that the greatest rivers have their most copious fountains the most remote from the sea.”* This seems the most general opinion ; and yet, after all, it is still pressed with great difficulties ; and there is still room to look out for a better theory. The perpetuity of many springs, which always yield the same quantity when the least rain or vapour is afforded, as well as when the greatest, is a strong objection. Derham^ mentions a spring at Upminster, which he could never perceive by his eye to be diminished, in the greatest droughts, even when all the ponds in the country, as well as an adjoining brook, have been dry for several months together. In the rainy seasons, also, it was never overflowed ; except sometimes, perhaps, for an hour or so, upon the immission of the external rains. He, therefore, justly enough concludes, that had this spring its origin from rain or vapour, there would be found an mcrease or decrease of its water, corresponding to the causes of its production. Thus the reader, after having been tossed from one hypothesis to another, must at last be content to settle in conscious ignorance. All that has been written upon this subject, affords him rather something to say, than some- thing to think ; something rather for others than for him- Self. Varenius, indeed, although he is at a loss for the * Phil. Trans, vol. ii. p. 128. f Derham Physico-Theol. A HISTORY OF 118 origin of rivers, is by no means so as to their formation. He is pretty positive that all rivers are artificial. He boldly asserts, that their channels have been originally formed by the industry of man. His reasons are, that when a new spring breaks forth, the water does not make itself a new channel, but spreads over the adjacent land. “ Thus,” says he, “ men are obliged to direct its course ; or, other- wise, Nature would never have found one.” He enumerates many rivers that are certainly known, from history, to have been dug by men. He alleges, that no salt-water rivers are found, because men did not want salt-water ; and as for salt, that was procurable at less expence than digging a river for it. However, it costs a speculative man but a small expence of thinking to form such an hypothesis. It may, perhaps, engross the reader’s patience to detain him longer upon it. Nevertheless, though Philosophy be thus ignorant, as to the production of rivers, yet the laws of their motion, and the nature of their currents, have been very well explained. The Italians have particularly distinguished themselves in this respect ; and it is chiefly to them that we are indebted for the improvement.* All rivers have their source either in mountains, or elevated lakes ; and it is in their descent from these that they acquire that velocity which maintains their future current. At first their course is generally rapid and headlong ; but it is retarded in its journey, by the continual friction against its banks, by the many obstacles it meets to divert its stream, and by the plains generally becoming more level as it ap- proaches towards the sea. If this acquired velocity be quite spent, and the plan1 through which the river passes is entirely level ; it will) notwithstanding, still continue to run, from the perpen- dicular pressure of the water, which is always in exact proportion to the depth. This perpendicular pressure 1S nothing more than the weight of the upper waters pressing the lower out of their places ; and, consequently, driving them forward, as they cannot recede against the stream* As this pressure is greatest in the deepest parts of * river, so we generally find the middle of the stream rapid ; both because it has the greatest motion * 11 * S. Guglielmini della Natura de Fiumi, passim. THE EARTH. 119 communicated by the pressure, and the fewest obstructions from the banks on either side. Rivers thus set into motion are almost always found to make their own beds. Where they find the bed elevated, they wear its substance away, and deposit the sediment in the next hollow, so as in time to make the bottom of their channels even. On the other hand, the water is con- tinually gnawing and eating away the banks on each side ; and this with more force as the current happens to strike more directly against them. By these means it always has a tendency to render them more straight and parallel to its own course. Thus it continues to rectify its banks, and enlarge its bed; and, consequently, to diminish the force of its stream, till there becomes an equilibrium be- tween the force of the water, and the resistance of its banks, upon which both will remain without any further mutation. And it is happy for man that bounds are thus put to the erosion of the earth by water ; and that we find all rivers only dig and widen themselves but to a certain degree.* In those plains-^ and large vallies where great rivers flow, the bed of the river is usually lower than any part of the valley. But it often happens, that the surface of the water is higher than many of the grounds that are adjacent to the banks of the stream. If, after inundations, we take a view of some rivers, we shall find their banks appear above water, at a time that all the adjacent valley is overflowed. This proceeds from the frequent deposition of ^ud, and such like substances, upon the banks, by the rivers frequently overflowing ; and thus, by degrees, they become elevated above the plain ; and the water is often Seen higher also. Rivers, as every body has seen, are always broadest at le mouth, and grow narrower towards their source. But nat is less known, and probably more deserving curio- is, that they run in a more direct channel as they immediately leave their sources ; and that their sinuosities • a turnings become more numerous as they proceed. It th t ,certa*n sign among the savages of North America, they are near the sea, when they find the rivers wind- * Guglielmini della Natura de Fiumi, passim. t Buffon, de Fleuves, passim, vol. ii. A HISTORY OF 120 ing, and every now and then changing their direction. And this is even now become an indication to the Europeans themselves, in their journeys through those trackless forests. As those sinuosities, therefore, increase as the river approaches the sea, it is not to be wondered at that they sometimes divide, and thus disembogue by different channels. The Danube disembogues into the Euxine by seven mouths ; the Nile by the same number ; and the Wolga by seventy. The currents* of rivers are to be estimated very differently from the manner in which those writers, who have given us mathematical theories on this subject, represent them. They found their calculations upon the surface being a perfect plain from one bank to the other : but this is not the actual state of nature ; for rivers, in general, rise in the middle ; and this convexity is greatest in proportion as the rapidity of the stream is greater. Any person, to be con- vinced of this, need only lay his eye, as nearly as he can, on a level with the stream, and looking across to the opposite bank, he will perceive the river in the midst to be elevated considerably above what it is at the edges. This rising, in some rivers, is often found to be three feet high ; and is ever increased in proportion to the rapidity of the stream. In this case, the water in the midst of the current, loses a part of its weight, from the velocity of its motion ; while that at the sides, for the contrary reason, sinks lower. W sometimes, however, happens, that this appearance . is reversed ; for when tides are found to flow up with violence against the natural current of the water, the greatest rapidity is then found at the sides of the river, as the water there least resists the influx from the sea. 0° those occasions, therefore, the river presents a' concave rather than a convex surface ; and, as in the former case, the middle waters rose in a ridge, in this case they sink m furrow. The stream of all rivers is more ra channel is diminished. For instai™, — - swifter where it is ten yards broad, than where it is twen for the force behind still pushing the water forward, when ^ comes to the narrow part, it must make up by velocity w it wants in room. * Buffon, de Fleuves, passim, vol. ii. pid in proportion as nn*. it will be mucn THE EARTH. 121 It often happens that the stream of a river is opposed by one of its jutting banks, by an island in the midst, the arches of a bridge, or some such obstacle. This produces not unfrequently a back current ; and the water having passed the arch with great velocity, pushes the water on each side . of its direct current. This produces a side current, tending to the bank; and not unfrequently a whirlpool; in which a large body of waters, are circulated in a kind of cavity, sinking down in the middle. The central point of the whirlpool is always lowest, because it has the least motion : the other parts are supported, in some measure, by the violence of theirs, and consequently rise higher as their motion is greater; so that towards the extre- mity of the whirlpool, must be higher than towards the centre. If the stream of a river be stopped at the surface, and yet be free below ; for instance, if it be laid over by a bridge of boats, there will then be a double current ; the water at the surface will flow back, while that at the bottom will proceed with increased velocity. It often happens that the current at the bottom is swifter than at the top, when, upon violent land-floods, the weight of waters towards the source presses the waters at the bottom, before it has had time to communicate its motion to the surface. However, in all other cases, the surface of the stream is swifter than the bottom, as it is not retarded by rubbing over the bed of the river. It might be supposed that bridges, dams, and other ostacles in the current of a river, would retard its velocity.5 ut the difference they make is very inconsiderable. The ob,er’ by .tnese stoPPages> gets an elevation above the ject ; which, when it has surmounted, it gives a velocity ^ recompenses the former delay. Islands and turnings o retard the course of the stream but very inconsiderably ; y cause which diminishes the quantity of the water, streamSenSlbly dindn*shes the f°rce and the velocity of the increL *ncIease# > °f water in the bed of the river . always ‘bstantfi ltS .raPidity » except in cases of inundation. The e uver has overflowed its banks, the velocity of v '* Buffon, vol. li. p. 62. 122 • A HISTORY OF its current is always turned that way, and the inundation is perceived to continue for some days ; which it would not otherwise do, if, as soon as the cause was discontinued, it acquired its former rapidity. A violent storm, that sets directly up against the course of the stream, will always retard, and sometimes entirely stop its course. I have seen an instance of this, when the bed of a large river was left entirely dry for some hours, and fish were caught among the stones at the bottom. Inundations are generally greater towards the source of rivers than farther down ; because the current is generally swifter below than above ; and that for the reasons already assigned. A little river* may be received into a large one, without augmenting either its width or depth. This, which at first view seems a paradox, is yet very easily accounted for. The little river, in this case, only goes towards increasing the swiftness of the larger, and putting its dormant waters into motion. In this manner the Venetian branch of the Po, was pushed on by the Ferrarese branch and that of Panaro, without any enlargement of its breadth or depth from these accessions. A river tending to enter another, either perpendicularly, or in an opposite direction, will be diverted by degrees from that direction ; and be obliged to make itself a more favour- able entrance downward, and more conspiring with the stream of the former. The union of two rivers into one, makes it flow the swifter ; since the same quantity of water, instead of rubbing against four shores, now only rubs against two. And, besides, the current being deeper, becomes, of consequence, more fitted for motion. ^ i With respect to the places from whence rivers proceed, it may be taken for a general rule, that the largest^ &n highest mountains supply the greatest and most extensive rivers. It may also be remarked, in whatever direction tie jridge of the mountain runs, the river takes an opp^51 course. If the mountain, for instance, stretches h° ^ north to south, the river runs from east to west ; and contrariwise. These are some of the most generally * ceived opinions with regard to the course of rivers ; 11 * Gugllelmini. f Doctor Halley. THE EARTH. 123 ever, they are liable to many exceptions ; and nothing but an actual knowledge of each particular river can furnish us with an exact theory of its current. The largest rivers of Europe are, first, the Wolga, which is about six hundred and fifty leagues in length, extending from Reschow to Astrachan. It is remarkable of this river, that it abounds with water during the summer months of May and June ; but all the rest of the year is so shallow as scarce to cover its bottom, or allow a passage for loaded vessels that trade up its stream. It was up this river that the English attempted to trade into Persia, in which they were so unhappily disappointed, in the year 1741. The next in order is the Danube. The course of this is about four hundred and fifty leagues, from the mountains of Switzerland to the Black Sea. It is so deep between Buda and Belgrade, that the Turks and Christians have fleets of men of war upon it ; which frequently engaged during the last war between the Ottomans and the Austrians : however, it is unnavigable further down, by reason of its cataracts, which prevent its commerce into the Black Sea, The Don, or Tanais, which is four hundred leagues from the source of that branch of it called the Softna, to its mouth in the Euxine Sea. In one part of its course, it approaches near the Wolga; and Peter the Great had actuallv begun a canal, by which he intended joining those two rivers ; but this he did not live to finish. The Nieper, or Boristhenes, which rises in the middle of Muscovy, and runs a course of three hundred and fifty leagues, to empty itself into the Elack Sea. The Old Cossacks inhabit the banks and elands of this river ; and frequently cross the Black Sea, to plunder the maritime places on the coasts of Turkey. The . ma, which takes its rise in a province of the same name ln Russia, that runs a course of three hundred leagues, and disembogues into the White Sea, a little below Arch- angel. . largest rivers of Asia are, the Hohanho, in China, ich is eight hundred and fifty leagues, in length, corn- el lng from its source at Raja Ribron, to its mouth in ^hangi. The Jenisca of Tartary, about t0b tj hundred leagues in length, from the lake Selinga, sun 1 l0y Sea‘ This river is, by some, supposed to P y most of that great quantity of drift wood which A HISTORY OF 124 is seen floating in the seas near the Arctic circle. The Oby, of five hundred leagues, running from the lake of Kila into the Northern Sea. The Amour, in Eastern Tartary, whose course is about five hundred and seventy- five leagues, from its source to its entrance into the sea of Kamtschatka. The Kiam, in China, five hundred and fifty leagues in length. The Ganges, one of the most noted rivers in the world, and about as long as the for- mer. It rises in the mountains which separate India from Tartary ; and running through the dominions of the Great Mogul, discharges itself by several mouths into the bay of Bengal. It is not only esteemed by the Indians for the depth and pureness of its stream, but for a supposed sanctity which they believe to be in its waters. It is visited annually by several hundred thousand pilgrims, who pay their devotions to the river as to a god : for sa- vage simplicity is always known to mistake the blessings of the Deity, for the Deity himself. They carry their dying friends from distant countries, to expire on its banks ; and to be buried in its stream. The water is lowest in April or May; but the rains beginning to fall soon after, the flat country is overflowed for several miles, till about the end of September ; the waters then begin to retire, leaving a prolific sediment behind, that enriches the soil, and, in a few days time, gives a luxuriance to vegetation, beyond what can be conceived by an Euro- pean. Next to this may be reckoned the still more cele- brated river Euphrates. This rises from two sources, northward of the city Erzerum, in Turcomania, and unites about three days’ journey below the same ; from whence, after performing a course of five hundred leagues, it fall® into the gulph of Persia, fifty miles below the city o Bassora in Arabia. The river Indus is extended, from 1 source to its discharge into the Arabian Sea, four hundre( leagues. . « The largest rivers of Africa are, the Senegal, whic^ runs a course of not less than eleven hundred leagu comprehending the Niger, which some have suppose ' fall into it. However, later accounts seem to affirm the Niger is lost in the sands, about three hundred up from the western coasts of Africa. Be this as 1 ^all the Senegal is well known to be navigable for more THE EARTH. 125 three hundred leagues up the country; and how much higher it may reach is not yet discovered, as the dread- ful fatality of the inland parts of Africa, not only deters curiosity, but even avarice, which is a much stronger pas- sion. At the end of last war, of fifty Englishmen that were sent to the factory at Galam, a place taken from the French, and nine hundred miles up the river, only one returned to tell the fate of his companions, who were de- stroyed by the climate. The celebrated river Nile is said to be nine hundred and seventy leagues, from its source among the Mountains of the Moon, in Upper .Ethiopia, to its opening into the Mediterranean Sea. The sources of this river were considered as inscrutable by the ancients ; and the causes of its periodical inundation were equally un- known. They have both been ascertained by the mis- sionaries who have travelled into the interior parts of -Ethiopia. The Nile takes its rise in the kingdom of Gojam,* from a small aperture on the top of a mountain, which, though not. above a foot and a half over, yet was unfathomable. This fountain, when arrived at the foot of the mountain, expands into a river; and being joined by others, forms a lake thirty leagues long, and as many road; from this, its channel, in some measure, winds back to the country where it first began; from thence, precipitating by frightful cataracts, it travels through a vAan^y of desert regions, equally formidable, such as bara, Olaca, Damot, and Xaoa. Upon its arrival in e kingdom of Upper Egypt, it runs through a rocky cafa1116^ some latc travellers have mistaken for its aracts. In the . beginning of its course, it receives ess.er rivers into it ; and Pliny was mistaken in say- cou tlat- ^ received none. In the beginning also of its but> for above three hun- ann eagues from the sea, it runs in a direct line. Its A-hich * °VPenS in °Ur summer> so the Nile is at that Egyjr TV1?‘ ^rom> these inundations, the inhabitants P enve happiness and plenty; and, when the * Kircher, Mund. Subt. vol. ii. d. 7<2. A HISTORY OF 126 river does not arise to its accustomed heights, they prepare for an indifferent harvest. It begins to overflow about the seventeenth of June ; it generally continues to augment for forty days, and decreases in about as many more. The time of increase and decrease, however, is much more inconsiderable now than it was among the ancients. He- rodotus informs us, that it was an hundred days rising, and as many falling ; which shews that the inundation was much greater at that time than at present. Mr. Buffo n* has ascribed the present diminution, as well to the lessen- ing of the Mountains of the Moon, by their substance having so long beep washed down with the stream, as to the rising of the earth in Egypt, that has for so many ages received this extraneous supply. But we do not find, by the buildings that have remained since the times of the ancients, that the earth is much raised since then. Be- sides the Nile in Africa, we may reckon the Zara, and the Coanza, from the greatness of whose openings into the sea, and the rapidity of whose streams, we form an estimate of the great distance from whence they come. Their courses, however, are spent in watering deserts and savage countries, whose poverty or fierceness have kept strangers away. $ But of all parts of the world, America, as it exhibits the most lofty mountains, so also it supplies the largest rivers. The foremost of these is the great river Amazon, which, from its source in the lake of Lauricocha, to its discharge into the Western Ocean, performs a course of more than twelve hundred leagues. The breadth and depth of this river are answerable to its vast length ; and, where its width is most contracted, its depth is augmented in proportion. So great is the body of its waters, tha other rivers, though before the objects of admiration, arC lost in its bosom. It proceeds, after their junction, w1 its usual appearance, without any visible change m 1 breadth or rapidity ; and, if we may so express it, renialjtg great without ostentation. In some places it displays ^ whole magnificence, dividing into several large branc ^ and encompassing a multitude of islands ; and, at *elhjin. discharging itself into the oeean, by a channel of an 1 ^ dred and fifty miles broad. Another river, that may * Buffon, vol. ii. p. 82. t Ulloa, vol. i. P-.388* THE EARTH. 127 most lival the former, is the St. Lawrence, in Canada, which rising in the lake Assiniboils, passes from one lake to another, from Christinaux to Alempigo ; from thence to lake Superior ; thence to the lake Hurons ; to lake Erie ; to lake Ontario ; and, at last, after a course of nine hundred leagues, pours . their collected waters into the Atlantic Ocean. The river Mississippi is of more than seven hun- dred leagues in length, beginning at its source near the lake Assiniboils, and ending at its opening into the gulph of Mexico. The river Plate runs a length of more than eight hundred leagues from its source in the river Parana, to its mouth. . The river Oroonoko is seven hundred and fifty leagues in length, from its source near Pasto, to its discharge into the Atlantic Ocean. Such is the amazing length of the greatest rivers ; and even in some of these, the most remote sources very pro- bably yet continue unknown. In fact, if we consider the number of rivers which they receive, and the little ac- quaintance we have with the regions through which they nin, it is not to be wondered at that geographers are divided concerning the sources of most of them. As among a number of roots by which nourishment is con- veyed to a stately tree, it is difficult to determine precisely t vat by which the tree is chiefly supplied ; so among the many branches of a. great river, it is equally difficult to f Much is the original. Hence it may easily happen, vat a similar branch is taken for the capital stream ; and * s runnings are pursued, and delineated, in prejudice of ome other branch that better deserved the name and the esciipticm. In this manner,* in Europe, the Danube is own to receive thirty lesser rivers ; the Wolga, thirty- five ^ ,thirty-three- In Asia, the Hohanho receives thirty- > the Jenisca above sixty; the Oby as many; the the °r ak°ut forty > the Nanquin receives thirty rivers ; Afric ail]feS twenty ; and the Euphrates about eleven. In h’ile a’ * ^ ^ene£al receives more than twenty rivers ; the and Jeceives n°t one for five hundred leagues upwards, Arnaz en ° v twelve or thirteen. In America, the river ble; th 1^ceives ahove sixty, and those very considera- e nvei St. Lawrence about forty, counting those * Buffon, vol. ii. p. 74. A HISTORY OF 128 which fall into its lakes; the Mississippi receives foxty; and the river Plate above fifty. I mentioned the inundations of the Ganges and the Nile; but almost every other great river, whose source lies within the tropics, have their stated inundations also. The river Pegu has been called, by travellers, the Indian Nile, because of the similar overflowings of its stream: this it does to an extent of thirty leagues on each side ; and so fertilizes the soil, that the inhabitants send great quantities of rice into other countries, and have still abundance for their own consumption. The river Sene- gal has likewise its inundations, which cover the whole flat country of Negroland, beginning and ending much about the same time with those of the Nile ; as, in fact, both rivers rise from the same mountains. But the dif- ference between the effects of the inundations in each river is remarkable: in the one, it distributes health and plenty; in the other, diseases, famine, and death. The inhabitants along the torrid coasts of the Senegal, can receive no benefit from any additional manure the river may carry down to their soil, which is by nature more than sufficiently luxuriant; or, even if they could, they have not industry to turn it to any advantage. The banks, therefore, of the rivers, lie uncultivated, overgrown with rank and noxious herbage, and infested with thousands of animals of various malignity. Every new flood only tends to increase the rankness of the soil, and to pro- vide fresh shelter for the creatures that infest it. If the flood continues but a few days longer than usual, the improvident inhabitants, who are driven up in the higher grounds, want provisions, and a famine ensues. When the river begins to return into its channel, the humiditv and heat of the air are equally fatal ; and the carcases 0 infinite numbers of animals, swept away by the inunda tion, putrefying in the sun, produce a stench that is most insupportable. But even the luxuriance of vegetation becomes a nuisance. I have been assure^ by persons of veracity who have been up the river fce^ gal, that there are some plants growing along the o° ^ the smell of which is so powerful, that it is hardly j®. ^ endured. It is certain, that all the sailors and so ^ ivho have been at any of our factories there, ascri THE EARTH 129 unwholesomeness of the voyage up the stream, to the vegetable vapour. However this be, the inundations of the rivers in this wretched part of the globe, contribute scarce any advantage, if we except the beauty of the pros- pects which they afford. These, indeed, are finished beyond the utmost reach of art : a spacious glassy river, with its banks here and there fringed to the very surface by the man grove -tree, that grows down into the water, presents itself to view ; lofty forests of various colours, with openings between, carpeted with green plants, and the most gaudy flowers ; beasts and animals, of various kinds, that stand upon the banks of the river, and, with a sort of wild curiosity, survey the mariners as they pass, contribute to heighten the scene. This is the sketch of an African prospect ; which delights the eye, even while it destroys the constitution . Besides these annually periodical inundations, there are many rivers that overflow at much shorter intervals. Thus most of those in Peru and Chili have scarce any motion by night ; but upon the appearance of the morning sun, they resume their former rapidity : this proceeds from the moun- tain snows, which, melting with the heat, increase the stream, and continue to drive on the current while the sun continues to dissolve them. Some rivers also flow with an even steady current, from their source to the sea ; others flow with greater rapidity, their stream being poured down Jn a cataract, or swallowed by the sands, before they reach the sea. The rivers of those countries that have been least in- . ahited, are usually more rocky, uneven, and broken lnt0 water-falls or cataracts, than those where the indus- JT man has been more prevalent. Wherever man ®es, nature puts on a milder appearance : the terrible us f i^16 su^me> are exchanged for the gentle and the andl cataract *s sl°Ped away into a placid stream ; hav t le k.anks become more smooth and even.* It must rec^r^ ages to render the Rhone or the Loire na- their ^ 1 beds must have been cleaned and directed ; flustrv^iv113^^68 removed i and, by a long course of in- • ’ ^ature must have been taught to conspire with vol. t* — 6. * BufFon, vol. ii, p. 90. R A HISTORY OF 130 the desires of her controller. Every one’s experience must have supplied instances of rivers thus being made to flow more evenly, and more beneficially to mankind ; but there are some whose currents are so rapid, and falls so precipi- tate, that no art can obviate ; and that must for ever remain as amazing instances of incorrigible nature. Of this kind are the cataracts of the Rhine ; one of which I have seen exhibit a very strange appearance ; it was that at Schathausen, which was frozen quite across, and the water stood in columns where the cataract had formerly fallen. The Nile, as was said, has its cataracts. The river Vologda, in Russia, has two. The river Zara, in Africa, has one near its source. The river Velino, in Italy, has a cataract of above an hundred ,and fifty feet perpendicular. Near the city of Gottenburgh, * in Sweden, the river rushes down from a prodigious high precipice, into a deep pit, with a terrible noise, and such dreadful force, that those trees designed for the masts of ships, which are floated down the river, are usually turned upside down in their fall, and often are shattered to pieces, by being dashed against the surface of the water in the pit ; this occurs if the masts fall sideways upon the water ; but if they fall endways, they dive so far under water, that they disappear for a quarter of an hour, or more : the pit, into which they are thus plunged, has been often sounded with a line of some hundred fathoms long, but no ground has been found hitherto. There is also a cataract at Powers- court, in Ireland, in which, if I am rightly informed,, the water falls three hundred feet perpendicular ; which is a greater descent than that of any other cataract in any palt of the world. There is a cataract at Albany, in the province of New York, which pours its stream fifty feet perpendicular- But of all the cataracts in the world, that of Niagfefo in Canada, if we consider the great body of water t falls, must be allowed to be the greatest, and the R1 astonishing. .. This amazing fall of water is made by the riverc®| Lawrence, in its passage from the lake Erie into the Ontario. We have already said that the St. was one of the largest rivers in the world ; and ye * Phil. Trans, vol. ii. p. 325. THE EARTH. 131 whole of its waters are here poured down, by a fall of an hundred and fifty feet perpendicular. It is not easy to bring the imagination to correspond with the greatness of the scene; a river, extremely deep and rapid, and that serves to drain the waters of almost all North America into the Atlantic ocean, is here poured precipitately down a ledge of rocks, that rise, like a wall, across the whole bed of its stream. The width of the river, a little above, is near three quarters of a mile broad ; and the rocks, where it grows narrower, are four hundred yards over. Their direction is not straight across, but hollowing inwards like a horse-shoe ; so that the cataract, which bends to the shape of the obstacle, rounding inwards, presents a kind of theatre the most tremendous in nature. Just in the middle of this circular wall of waters, a little island, that has braved the fury of the current, presents one of its points, and divides the stream at top into two ; but it unites again long before it has got to the bottom. The noise of the fall is heard at several leagues distance ; and the fury of the waters at the bottom of their fall is inconceivable. The dashing produces a mist that rises to the very clouds ; and that produces a most beautiful rainbow, when the sun shines. It may easily be conceived, that such a cataract quite destroys the navigation of the stream ; and yet some Indian canoes, as it is said, have been known to venture down it with safety. Of those rivers that lose themselves in the sands, or are swallowed up by chasms in the earth, we have vari- 0Us information. What we are told by the ancients, ot the river Alpheus, in Arcadia, that sinks into the ground, and rises again near Syracuse in Sicily, where it takes the jiame of Arethusa, is rather more known than credited. ut we have better information with respect to the river ^gris being lost in this manner under mount Taurus ; of fe, Ouadalquiver, in Spain, being buried in the sands ; an 1 • r-1Ver ^r^ataIh in Yorkshire, running under ground, p C nsing again ; and even of the great Rhine itself, a f ot which is no doubt lost in the sands, a little above But it ought to be observed of this river, that f^yden. by altii^f1 £r.eatest Part arrives at the ocean ; for, Bttlo 1 ?16 ancient channel which fell into the sea, a 0 the west of that city, be now entirely choked up, A HISTORY OF 132 yet there are still a number of small canals, that carry a great body of water to the sea ; and, besides* it has also two veiy large openings, the Lech and the Waal, below Rotter- dam, by which it empties itself abundantly. Be this as it will, nothing is more common in sultry and sandy deserts, than rivers being thus either lost in the sands, or entirely dried up by the sun. And hence we see, that under the line, the small rivers are but few ; for such little streams as are common in Europe, and which with us receive the name of rivers, would quickly evaporate, in those parching and extensive deserts. It is even confi- dently asserted, that the great river Niger is thus lost before it reaches the ocean ; and that its supposed mouths, the Gambia and the Senagal, are distinct rivers, that come a vast way from the interior parts of the country. It appears, therefore, that the rivers under the Line are large ; but it is otherwise at the Poles,* where they must necessarily be small. In that desolate region, as the mountains are covered with perpetual ice, which melts but little, or not at all, the springs and rivulets are furnished with a very small Supply. Here, therefore, men and beasts would perish, and die for thirst, if Providence had not ordered, that in the hardest winter, thaws should intervene, which deposit a small quantity of snow-water in pools under the ice ; and from this source the wretched inhabitants drain a scanty beverage. Thus, whatever quarter of the globe we turn to, we shall find new reasons to be satisfied with that part of it in which we reside. Our rivers furnish all the plenty of the African stream, without its inundation ; they have all the coolness of the polar rivulet, with a more constant supply; they may want the terrible magnificence of huge cataracts, or extensive lakes, but they are more navigable, and more transparent ; though less deep and rapid than the rivers of the torrid zone, they are more manageable and only wait the will of man to take their direction. rivers of the torrid zone, like the monarchs of the cou try,' rule with despotic tyranny ; profuse in their bounty > and ungovernable in their rage. The rivers of Enr0Py like their kings, are the friends, and not the oppress0 * Crantz’s History of Greenland, vol. i. p- 41. THE EARTH. 133 of the people ; bounded by known limits, abridged in the power of doing ill, directed by human sagacity, and only at freedom to distribute happiness and plenty. CHAP. XV. OF THE OCEAN IN GENERAL; AND OF ITS SALTNESS. If we look upon a map of the world, we shall find that the ocean occupies considerably more of the globe, than the land is found to do. This immense body of waters is diffused round both the Old and New Continent, to the south ; and may surround them also to the north, for what we know, but the ice in those regions has stopped our inquiries. Although the ocean, properly speaking, is but one extensive sheet of waters, continued over every part of the globe, without interruption, and although no part of it is divided from the rest, yet geographers have distinguished it by different names ; as, the Atlantic or Western Ocean, the Northern Ocean, the Southern Ocean, the Pacific Ocean, and the Indian Ocean. Others have divided it differently, and given other names ; as, the Iiozen Ocean, the Inferior Ocean, or the American Ocean, hut all these being arbitrary distinctions, and not of feature’s making, the naturalist may consider them with ^difference. In this vast receptacle, almost all the rivers of the earth ^ tlmately terminate ; nor do such great supplies seem to please its stores ; for it is neither apparently swollen by eir tribute, nor diminished by their failure ; it still con- °f UpS same. Indeed, what is the quantity of water co f • rivers and lakes in the world, compared to that rtl^! aiaed in this great receptacle ?* If we should offer to the G a rU^e esttmate, we shall find that all the rivers in tinuVV°rid, flowing into the bed of the sea, with a con- ance of their present stores, would take up at least * Buffon, vol. ii. p. 70. A HISTORY OF 134 eight hundred years to fill it to its present height. For, supposing the sea to be eighty-five millions of square miles in extent, and a quarter of a mile, upon an average, in depth, this, upon calculation, will give about twenty- one millions of cubic miles of water, as the contents of the whole ocean. Now, to estimate the quantity of water which all the rivers supply, take any one of them ; the Po, for instance, the quantity of whose discharge into the sea is known to be one cubic mile of water in twenty-six days. Now it will be found, upon a rude computation, from the quantity of ground the Po, with its influent streams, covers, that all the rivers of the world furnish about two thousand times that quantity of water. In the space of a year, therefore, they will have discharged into the sea about twentv-six thousand cubic miles of water ; and not till eight hundred years, will they have discharged as much water as is contained in the sea at present. I have not troubled the reader with the odd numbers, lest he should imagine I was giving precision to a subject that is incapable of it. Thus great is the assemblage of waters diffused round our habitable globe ; and yet, immeasurable as they seem, they are mostly rendered subservient to the necessities and the conveniences of so little a being as man. Never- theless, if it should be asked whether , they be made for him alone, the question is not easily resolved. Some philosophers have perceived so much analogy to man in the formation of the ocean, that they have not hesitated to assert its being made for him alone. The distribution of land and water,* say they, is admirable; the one be- ing laid against the other so skilfully, that there is a just equipoise of the whole globe. Thus the Northern Ocean balances against the Southern ; and the New Continent is an exact counterweight to the Old. As to any objec- tion from the ocean’s occupying too large a share of the globe, they contend, that there could not have been a smaller surface employed to supply the earth with a du share of evaporation. On the other hand, some take gloomy side of the question ; they either magnify^ its parent defects ; or assert, that what seems defects to » f Burnet’s Theory, passim- * Derham’s Physico-Theol. THE EARTH. 135 may be real beauties to some wiser order of beings.* They observe, that multitudes of animals are concealed in the ocean, and but a small part of them are known ; the rest therefore, they fail not to say, were certainly made for their own benefit, and not for ours. How far either of these opinions be just, I will not presume to determine; but of this we are certain, that God has endowed us with abilities to turn this great extent of waters to our own advantage. He has made these things, perhaps, for other uses ; but he has given us faculties to convert them to our own. This much agi- tated question, therefore, seems to terminate here. We shall never know whether the things of this world have been made for our use ; but we very well know that we have been made to enjoy them. Let us then boldly affirm, that the earth, and all its wonders, are ours ; since we are furnished with powers to force them into our service. Man is the lord of all the sublunary crea- tion ; the howling savage, the winding serpent, with all the untameable and rebellious offspring of Nature, are destroyed in the contest, or driven at a distance from his habitations. The extensive and tempestuous ocean, instead of limiting or dividing his power, only serves to assist his industry, and enlarge the sphere of his enjoy- ments. Its billows, and its monsters, instead of present- ing a scene of terror, only call up the courage of this little intrepid being ; and the greatest danger that man now fears on the deep, is from his fellow creatures. In- deed, when I consider the human race as Nature has formed them, there is but very little of the habitable globe that seems made for them. But when I consider them as accumulating the experience of ages, in commanding the earth, there is nothing so great or so terrible. What a poor contemptible being is the naked savage, standing on e beach of the ocean, and trembling at its tumults ! ow little capable is he of converting its terrors into be- ^ ts ; or of saying, Behold an element made wholly for y onjoymejH ! He considers it as an angry deity, and it the homage of submission. But it is very different en he has exercised his mental powers ; when he has * Pope’s Ethic Epistles, passim. A HISTORY OP 136 learnt to find his own superiority, and to make it subservient to his commands. It is then that his dignity begins to appear, and that the true Deity is justly praised for having been mindful of man ; for having given him the earth for his habitation, and the sea for an inheritance. This power which man has obtained over Ahe ocean, was at first enjoyed in common ; and none pretended to a right in that element where all seemed intruders. The sea, therefore, was open to all till the time of the emperor Justinian. His successor Leo granted such as were in possession of the shore, the sole right of fishing before their respective territories. The Thracian Bosphorus was the first that was thus appropriated ; and from that time it has been the struggle of most of the powers of Europe to obtain an exclusive right in this element. The republic of Venice claims the Adriatic. The Danes are in pos- session of the Baltic. But the English have a more ex- tensive claim to the empire of all the seas encompassing the kingdoms of England, Scotland, and Ireland ; and although these have been long contested, yet they are now considered as their indisputable property. Every one knows that the great power of the nation is exerted on this element; and that the instant England ceases to be superior upon the ocean, its safety begins to be precarious. It is in some measure owing to our dependence upon the sea, and to our commerce there, that we are so well ac- quainted with its extent and figure. The bays, gulphs, cur- rents, and shallows, of the ocean, are much better known and examined than the provinces and kingdoms of the earth itself. The hopes of acquiring wealth by commerce, has carried man to much greater length than the desire of gaining information could have done. In consequence of this, there is scarce a strait or an harbour, scarce a rock or a quicksand, scarce an inflection of the shore, or the jut' ting of a promontory, that has not been minutely describ- ed. But as these present very little entertainment to the imagination, or delight to any but those whose pursuits are lucrative, they need not be dwelt upon here. Wvlle the merchant and the mariner are solicitous in describing currents and soundings, the naturalist is employed observing wonders, though not so beneficial, yet to h11 THE EARTH. 137 of a much more important nature. The saltness of the sea seems to be foremost. Whence the sea has derived that peculiar bitterish salt- ness which we find in it, appears, by Aristotle, to have exercised the curiosity of naturalists in all ages. He sup- posed (and mankind were for ages content with the solution) that the sun continually raised dry saline ex- halations from the earth, and deposited them upon the sea ; and hence, say his followers, the waters of the sea are more salt at top than at bottom. But, unfortunately for this opinion, neither of the facts is true. Sea-salt is not to be raised by the vapours of the sun ; and sea- water is not salter at the top than at the bottom. Father Bohours is of opinion, that the Creator gave the waters of the ocean their saltness at the beginning ; not only to prevent their corruption, but to enable them to bear greater burthens. But their saltness does not prevent their corruption ; for stagnant sea-water, like fresh, soon grows putrid : and, as for their bearing greater burthens, fresh water answers all the purposes of navigation quite as well. The established opinion, therefore, is that of Boyle,* who supposes, “ That the sea’s saltness is sup- plied not only from rocks or masses of salt at the bottom of the sea, but also from the salt which the rains and nvers, and other waters, dissolve in their passage through many parts of the earth, and at length carry with them to the sea.” But as there is a difference in the taste of rock-salt found at land, and that dissolved in the waters of the ocean, this may be produced by the plenty of nitrous- ari(l bituminous bodies that, with the salts, are likewise gashed into that great receptacle. These substances oemg thus once carried to the sea, must for ever remain lei'e ; for they do not rise by evaporation, so as to be returned back from whence they came. Nothing but the resh waters of the sea rise in vapours ; and all the saltness remains behind. From hence it follows, that every year cm ^6a must become more and more salt ; and this spe- ation Dr. Halley carries so far, as to lay down a e od of finding out the age of the world by the salt- Ss of its waters. “ For if it be observed,” says he, V0L‘ — 6. * Boyle, vol. lii. p. 221. S A HISTORY OF 138 “ what quantity of salt is at present contained in a certain weight of water taken up from the Caspian Sea for example, and, after some centuries, what greater quantity of salt is contained in the same weight of water, taken from the same place ; we may conclude, that in proportion as the saltness has increased in a certain time, so much must it have increased before that time ; and we may thus, by the rule of proportion, make an esti- mate of the whole time wherein the water would acquire the degree of saltness it should be then possessed of.”* All this may be fine: however, an experiment, begun in this century, which is not to be completed till some centuries hence, is rather a little mortifying to modern curiosity ; and, I am induced to think, the inhabitants round the Caspian Sea will riot be apt to undertake the inquiry. This saltness is found to prevail in every part of the ocean ; and as much at the surface as at the bottom. It is also found in all those seas that communicate with the ocean ; but rather in a less degree. The great lakes, likewise, that have no outlets nor com- munication with the ocean, are found to be salt ; but some of them in less proportion. On the contrary, all those lakes through which rivers run into the sea, however extensive they be, are, notwithstanding, very fresh : for the rivers do not deposit their salts in the bed of the lake, but carry them with their currents into the ocean. Thus the lakes Ontario and Erie, in North America, although for magni- tude they may be considered as inland seas, are, never- theless, fresh-water lakes ; and kept so by the river St. Lawrence, which passes through them. But those lakes that have no communication with the sea, nor any rivers going out, although they be less than the former, are, how ever, always salt. Thus, that which goes by the name 0 the Dead Sea, though very small, when compared to tho already mentioned, is so exceedingly salt, that its wa seem scarcely capable of dissolving any more. The lak®-s ' Mexico and of Titicaca, in Peru, though of no great exte are nevertheless salt; and both for the same reason. Those who are willing to turn all things to the best, * Phil. Trans, vol. v. P. 218. THE EARTH. ' not failed to consider this saltness of the sea as a peculiar blessing from Providence, in order to keep so great an ele- ment sweet and wholesome. What foundation there may be in the remark, I will not pretend to determine ; but we shall shortly find a much better cause for its being kept sweet, namely, its motion. On the other hand, there have been many who have considered the subject in a different light, and have tried every endeavour to make salt-water fresh, so as to sup- ply the wants of mariners in long voyages, or when ex- hausted of their ordinary stores. At first it was sup- posed simple distillation would do ; but it was soon found that the bitter part of the water still kept mixed. It was then tried by uniting salt of tartar with sea-wrater, and distilling both ; but here the expence was greater than the advantage. Calcined bones were next thought of ; but a hogshead of calcined bones, carried to sea, would take up as much room as a hogshead of water, and was more hard to be obtained. In this state, therefore, have the attempts to sweeten sea-water rested ; the chymist satis- fied with the reality of his invention, and the mariner convinced of its being useless. I cannot, therefore, avoid mentioning a kind of succedaneum which has been lately conceived to answer the purposes of fresh water, when mariners are quite exhausted. It is well known, that persons who go into a warm bath, come out several ounces heavier than they went in ; their bodies having imbibed :i correspondent quantity of water. This more particularly happens, if they have been previously debarred from drinking, or go in with a violent thirst ; which they quickly find quenched, and their spirits restored. It was opposed, that in case of a total failure of fresh water at sea, a warm bath might be made of sea-water, for the use of Mariners ; and that their pores would thus imbibe the fluid, ^thout any of its salts, which would be seen to crystallize the surface .of their bodies. In this manner, it is sup- posed, a sufficient quantity of moisture may be procured to stain life, till time or accident furnish a more copious SUpply. k°wever ^is be, the saltness of the sea can by no ns he considered as a principal cause in preserving its rs hom putrefaction. The ocfean has its currents, like A HISTORY OF 140 rivers, which circulate its contents round the globe ; and these may be said to be the great agents that keep it sweet and wholesome. Its saltness alone would by no means an- swer this purpose : and some have even imagined, that the various substances with which it is mixed, rather tend to promote putrescence than impede it. Sir Robert Hawkins, one of our most enlightened navigators, gives the following- account of a calm in which the sea continuing for some time without motion, began to assume a very formidable appearance. “ Were it not,” says he, “ for the moving of the sea, by the force of winds, tides, and currents, it would corrupt all the world. The experiment of this I saw in the year 1590, lying with a fleet about the islands of Azores, almost six months ; the greatest part of which time we were becalmed. Upon which all the sea became so replenished with several sorts of jellies, and forms of serpents, adders, and snakes, as seemed wonderful : some green, some black, some yellow, some white, some of divers colours ; and many of them had life ; and some there were a yard and a half, and two yards long ; which, had I not seen, I could hardly have believed. And hereof are witnesses all the company of the ships which were then present ; so that hardly a man could draw a bucket of water clear of some corruption. In which voyage, towards the end thereof, many of every ship fell sick, and began to die apace. But the speedy passage into our country was a remedy to the crazed, and a preservative for those that were not touched.” This shews, abundantly, how little the sea’s saltness was capable of preserving it from putrefaction : but to put the matter beyond all doubt, Mr. Boyle kept a quantity of sea-water, taken up in the English Channel, for some time barrelled up ; and, in the space of a few weeks, it began to acquire a fetid smell.* He was also assured, by one of his acquaintance, who Wets becalmed for twelve or fourteen days in the Indian Sea, that the water, for want of motion, began to stink ; and that had it continued much longer, the stench would probably have poisoned him. It is the motion, therefore, and not * saltness of the sea, that preserves it in its present sta * * Boyle, vol. iii. p, £22. THE EARTH. 141 of salubrity; and this, very probably, by dashing and breaking in pieces the rudiments, if I may so call them, of the various animals that would otherwise breed there, and putrify. There are some advantages, however, which are derived from the saltness of the sea. Its waters being evaporated, furnish that salt which is used for domestic purposes ; and although in some places it is made from springs, and in others dug out of mines, yet the greatest quantity is made only from the sea. That which is called bay salt , (from its coming to us by the Bay of Biscay,) is a stronger kind, made by evaporation in the sun ; that called common salt , is evaporated in pans over the fire, and is of a much inferior quality to the former. Another benefit arising from the quantity of salt dis- solved in the sea, is, that it thus becomes heavier, and consequently more buoyant. Mr. Boyle, who examined the difference between sea-water and fresh, found that the former appeared to be about a forty-fifth part heavier than the latter. Those, also, who have had opportunities of bathing in the sea, pretend to have experienced a much greater ease in swimming there than in fresh water. How- ever, as we see they have only a forty-fifth part more of their weight sustained by it, I am apt to doubt whether so minute a difference can be practically perceivable. Be this as it may, as sea-water alters in its weight from fresh, so it is found also to differ from itself in different parts of the ocean. In general, it is perceivable to be heavier, and consequently salter, the nearer we approach the Line.* But there is an advantage arising from the saltness of ffe waters of the sea, much greater than what has been yet mentioned ; which is, that their congelation is thus retarded. Some, indeed, have gone so far as to say, that sea- water never freezes but this is an assertion con- r^dicted by experience. However, it is certain that it requiies a much greater degree of cold to freeze it than es water ; so that, while rivers and springs are seen inerted \n^° one solid body of ice, the sea is- always fit navigation, and no way affected by the coldness of the * Phil. Trans, vol. ii, p. 297. t Macrobius. 142 A HISTORY OF severest winter. It is, therefore, one of the greatest bless- ings we derive from this element, that, when at land all the stores of nature are locked up from us, we find the sea ever open to our necessities, and patient of the hand of industry. But it must not be supposed, because in our temperate climate we never see the sea frozen, that it is in the same manner open in every part of it. A very little acquaintance with the accounts of mariners, must have informed us, that at the polar regions it is embarrassed with mountains and moving sheets of ice, that often render it impassable. These tremendous floats are of different magnitudes ; sometimes rising more than a thousand feet above the surface of the water ;* sometimes diffused into plains of above two hundred leagues in length ; and, in many parts, sixty or eighty broad. They are usually divided by fissures ; one piece following another so close, that a person may step from one to the other. Sometimes mountains are seen rising amidst these plains, and presenting the ap- pearance of a variegated landscape, with hills and valleys, houses, churches, and towers. These are appearances in which all naturalists are agreed ; but the great contest is respecting their formation. Mr. Buffon asserts,^ that they are formed from fresh water alone, which congealing at the mouths of great rivers, accumulate those huge masses that disturb navigation. However, this great naturalist seems not to have been aware that there are two sorts of ice floating in these seas ; the flat ice and the mountain ice : the one formed of sea- water only ; the other of fresh. J The flat, or driving ice, is entirely composed of seaj water ; which, upon dissolution, is found to be salt ; is readily distinguished from the mountain, or fresh-wa / ice, by its whiteness, and want of transparency. *. , ice is much more terrible to mariners than that, w rises up in lumps : a ship can avoid the one, as it 1S s5j^ at a distance ; but it often gets in among the other, w sometimes closing, crushes it to pieces. This, w manifestly has a different origin from the fresh-water * Crantz’s History of Greenland, vol. i. p- SR t Buffon, vol. ii. p. 91. + Crantz. THE EARTH. 143 may perhaps have been produced in the Icy Sea, beneath the pole ; or along the coasts of Spitzbergen or Nova- Zembla. The mountain ice, as was said, is different in every respect, being formed of fresh water, and appearing hard and transparent ; it is generally of a pale green colour, though some pieces are of a beautiful sky-blue ; many large masses also appear gray, and some black. If exa-\ mined more nearly, they are found to be incorporated with earth, stones, and brush-wood, washed from the shore. On these also are sometimes found, not only earth, but nests with birds’ eggs, at several hundred miles from land. The generality of these, though almost totally fresh, have nevertheless a thick crust of salt-water frozen upon them, probably from the power that ice has sometimes to pro- duce ice. Such mountains as are here described, are most usually seen at spring-time, and after a violent storm, driving out to sea, where they at first terrify the mariner, and are soon after dashed to pieces by the continual washing of the waves ; or driven into the warmer regions of the south, there to be melted away. They sometimes, however, strike back upon their native shores, where they seem to take root at the feet of mountains ; and, as Martius tells us, are sometimes higher than the mountains them- selves. Those seen by him were blue, full of clefts and cavities made by the rain, and crowned with snow, which alternately thawing and freezing every year, augmented their size. These, composed of materials more solid than that driving at sea, presented a variety of agreeable figures to the eye, that with a little help from fancy assumed the aPpearance of trees in blossom ; the inside of churches, Wlth arches, pillars, and windows ; and the blue-coloured 7S> darting from within, presented the resemblance of a ti Tf it we inquire into the origin and formation of these, tVi’ as we see’ are very different from the former, I ink we have a very satisfactory account of them in rantz s History of Greenland ; and I will take leave to ^Ve the passage with a very few alterations. “ These ^ anta^ns of ice,” says he, “ are not salt, like the sea- exce^ swee<: > anch therefore, can be formed no where Pt on the mountains, in rivers, in caverns, and against A HISTORY OF 144 the hills near the sea-shore. The mountains of Greenland are so high, that the snow which falls upon them, parti- cularly on the north-side, is in one night’s time wholly converted into ice: they also contain clefts and cavities, where the sun seldom or never injects his rays ; besides these, are projections, or landing-places, on the declivities of the steepest hills, where the rain and snow-water lodge, and quickly congeal. When now the accumulated flakes of snow slide down, or fall with the rain from the emi- nences above on these prominences ; or, when here and there a mountain-spring comes rolling down to such a lodging-place, where the ice has already seated itself, they all freeze, and add their tribute to it. This, by degrees, waxes to a body of ice, that can no more be overpowered by the sun ; and which, though it may indeed, at certain seasons, diminish by a thaw, yet, upon the whole, through annual acquisitions, it assumes an annual growth. Such a body of ice is often prominent far over the rocks. It does not melt on the upper surface, but underneath ; and often cracks into many larger or smaller clefts, from whence the thawed water trickles out. By this it becomes at last so weak, that being overloaded with its own pon- derous bulk, it breaks loose, and tumbles down the rocks with a terrible crash. Where it happens to over- hang a precipice on the shore, it plunges into the deep with a shock like thunder ; and with such an agitation of the water, as will overset a boat at some distance, as many a poor Greenlander has fatally experienced.” Thus are these amazing ice-mountains launched forth to sea, and found floating in the waters round both the poles- It is these that have hindered mariners from discovering the extensive countries that lie round the South P°le» and that probably block up the passage to China by t*16 North. I will conclude this chapter, with one effect in°re produced by the saltness of the sea ; which is the lumin® appearance of its waves in the night. All who have bee spectators of a sea by night, a little ruffled with wi ^ seldom fail of observing its fiery brightness. In places it shines as far as the eye can reach at ^ * Boyle, vol. i. p. 294, THE EARTH. 145 times, only when the waves boom against the side of the vessel, or the oar dashes into the water. Some seas shine often ; others more seldom ; some, ever when particular winds blow ; and others, within a narrow compass ; a long tract of light being seen along the surface, whilst all the rest is hid in total darkness. It is not easy to account for these extraordinary appearances: some have supposed that a number of luminous insects produced the effect, and this is in reality sometimes the case ; in general, how- ever, they have every resemblance to that light produced by electricity ; and, probably, arise from the agitation and dashing of the saline particles of the fluid against each other. But the manner in which this is done, for we can produce nothing similar by any experiments hitherto made, remains for some happier accident to discover. Our progress in the knowledge of nature is slow ; and it is a mortifying consideration, that we are hitherto more indebted for success to chance than industry. CHAP. XVI. °F THE TIDES, MOTION, AND CURRENTS, OF THE SEA; WITH THEIR EFFECTS. It was said in the former chapter, that the waters of he sea were kept sweet by their motion ; without which jhey would soon putrefy, and spread universal infection. we look for final causes, here indeed we have a great tj an obvious one that presents itself before us. Had 'e sea been made without motion, and resembling a pool w ffgnant water, the noble races of animated nature shortly be at an end. Nothing would then be ln0ralu:e^t swarms of ill-formed creatures, with scarcely tl;ayi vegetable life; and subsisting by putrefaction. rpii|-e tllS ex*ens^ve bed of waters entirely quiescent, propp,nS ^le smader reptile kinds would there find a *here j retrea.t to breed and multiply in ; they would find fluid t^° agitation, no concussion in the parts of the Vo 0 crush their feeble frames, or to force them from • o. t 146 A HISTORY OP the places where they were bred: there they would mul- tiply, in security and ease, enjoy a short life, and putrefying, thus again give nourishment to numberless other, as little worthy of existence as themselves. But the motion of this great element effectually destroys the number of these viler creatures ; its currents and its tides produce continual agitations, the shock of which they are not able to endure ; the parts of the fluid rubbing against each other, destroy all viscidities ; and the ocean, if I may so express it, acquires health by exercise. The most obvious motion of the sea, and the most ge- nerally acknowledged, is that of its tides. This element is observed to flow for certain hours, from the south towards the north ; in which motion or flux, which lasts about six hours, the sea gradually swells ; so that entering the mouths of rivers, it drives back the river-waters to their heads. After a continual flux of six hours, the sea seems to rest for a quarter of an hour ; and then begins to ebb, or retire back again, from north to south, for six hours more ; in which time the waters sinking, the rivers resume their natural course. After a seeming pause of a quarter of an hour, the sea again begins to flow as before : and thus it has alternately risen and fallen, twice a day, since the creation. This amazing appearance did not fail to excite the cu- riosity, as it did the wonder, of the ancients. After some wild conjectures of the earliest philosophers, it became well known in the time of Pliny, that the tides were en- tirely under the influence, in a small degree, of the sun ; but in a much greater of the moon. It was found that of there was a flux and reflux of the sea, in the space twelve hours fifty minutes, which is exactly the time of a lunar day. It was observed, that whenever the moon wis in the meridian, or, in other words, as nearly as possible over any part of the sea, that the sea flowed to that parj’ and made a tide there ; on the contrary, it was f°un ’ that when the flow back again be said to ebb. Thus far the waters of the sea ^ ^ very regularly to attend the motions of the moon. & ^ it appeared, likewise, that when the moon was ,n ^ opposite meridian, as far off on the other side of the g : moon left the meridian, the sea begaI1^J tin from whence it came ; and there nlV . THE EARTH. H7 that there was a tide on this side also ; so that the moon produced two tides, one by her greatest approach to us, and another by her greatest distance from us : in other words, the moon, in once going round the earth, produced two tides, always at the same time ; one on the part of the globe directly under her ; and the other, on the part of the globe directly opposite. Mankind continued for several ages content with know- ing the general cause of these wonders, hopeless of dis- covering the particular manner of the moon’s operation. Kepler was the first who conjectured that attraction was the principal cause ; asserting, that the sphere of the moon’s operation extended to the earth, and drew up its waters. The precise manner in which this is done, was discovered by Newton. The moon has been found, like all the rest of the planets, to attract and to be attracted by the earth. This attraction prevails throughout our whole planetary system. The more matter there is contained in any body, the more it attracts ; and its influence decreases in proportion as the distance, when squared, increases. This being premised, let us see what must ensue upon supposing the moon in the meridian of any tract of the sea. The surface of the water imme- diately under the moon, is nearer the moon than any other part of the globe is ; and, therefore, must be more subject to its attraction than the waters any where else. The waters will, therefore, be attracted by the moon, and rise in a heap ; whose eminence will be the highest where the attraction is greatest. In order to form this eminence, it is obvious that the surface, as well as the depths, will be agitated; and that wherever the water runs from one part, succeeding waters must run to fill up the space it has left. Thus the "aters of the sea, running from all parts to attend the motion °/ the moon, produce the flowing of the tide ; and it is high hde at that part wherever the moon comes over it, or to its Pridian. But when the moon travels onward, and ceases to point ?Ver the place where the waters were just risen, the cause tlT,e their rising ceasing to operate, they will flow back by natural gravity into the lower parts from whence they Pu. travelled ; and this retiring of the waters will form the ebbln§ of the sea 148 A HISTORY OF Thus the first part of the demonstration is obvious; since, in general, it requires no great sagacity to conceive that the waters nearest the moon are most attracted, or raised highest by the moon. But the other part of the demonstration, namely, how there come to be high tides at the same time, on the opposite side of the globe, and where the waters are farthest from the moon, is not so easy to conceive. To comprehend this, it must be observed, that the part of the earth and its waters that are farthest from the moon, are the parts of all others that are least attracted by the moon ; it must also be observed, that all the waters, when the moon is on the opposite side of the earth, must be attracted by it in the same direction that the earth itself attracts them ; that is, if I may so say, quite through the body of the earth, towards the moon itself. This, therefore, being conceived, it is plain that those waters which are farthest from the moon, will have less weight than those of any other part, on the same side of the globe ; because the moon’s attraction, which conspires with the earth’s attraction, is there least. Now, therefore, the waters farthest from the moon, having less weight, and being lightest, will be pressed on all sides, by those that, having more attraction, are heavier : they will be pressed, I say, on all sides ; and the heavier waters flowing in, will make them sw'ell and rise, in an eminence directly opposite to that on the other side of the globe, caused by the more immediate influence of the moon. In this manner the moon, in one diurnal revolution, produces two tides ; one raised immediately under the sphere of its influence, and the other directly opposite to it. As the moon travels, this vast body of waters rears upward, as if to watch its motions ; and pursues the same constant rotation. However, in this great work of raising the tides, the sun has no small share ; it produces its own tides constantly every day, just as the moon does, but i a much less degree, because the sun is at an immense greater distance. Thus there are solar tides, and. him tides. When the forces of these twro great luinina^ concur, which they always do when they are either n1.^ same, or in opposite parts of the heavens, they ^ produce a much greater tide, than when they a situated in the heavens, as each to make peculiar ! THE EARTH. 149 their own. To express the very same thing technically; in the conjunctions and oppositions of the sun and moon, the attraction of the sun conspires with the attraction of the moon ; by which means the high spring-tides are formed. But in the quadratures of the sun and moon, the water raised by the one is depressed by the other ; and hence the lower neap-tides have their production. In a word, the tides are greatest in the syzigies, and least in the quadratures. This theory we. understood, and the astronomical terms previously knowr, it may readily be brought to explain the various appearances of the tides, if the earth were covered with a deep sea, and the waters uninfluenced by shoals, currents, straits, or tempests. But in every part of the sea, near the shores, the geographer must come in to correct the calculations of the astronomer. For, by reason of the shallowness of some places, and the narrowness of the straits in others, there arises a great diversity in the effect, not to be accounted for without an exact knowledge of all the circumstances of the place. In the great depths of the ocean, for instance, a very slow and imperceptible motion of the whole body of water will suffice to raise its surface several feet high ; but if the same increase of water is to be conveyed through a narrow channel, it must rush through it with the most impetuous rapidity. Thus, in the English Channel, and the German Ocean, the tide is found to flow strongest in those places that are narrowest ; the same quantity of water being, in this case, driven through a smaller passage. It is often seen, therefore, pouring through a strait with great force ; and, by its rapidity, con- ^derably raised above the surface of that part of the ocean 111 to which it runs. This shallowness and narrowness in many parts of the Sea> give also rise to a peculiarity in the tides of some P»rts of the world. For in many places, and in our own ?as ln particular, the greatest swell of the tide is not while !e m°on is in its meridian height, and directly over the ;j,jlce> but some time after it has declined from thence. "itK SGa’ ln case’ being obstructed, pursues the moon wate dispatch it can, but does not arrive with all its Lastl ^ f1^ *0n? a^ter ^e. moon has ceased to operate. y> hoin this shallowness of the sea, and from its beinsr A HISTORY OF 150 obstructed by shoals and straits, we may account for the Mediterranean, the Baltic, and the Black Sea, having no sensible tides. These, though to us they seem very ex- tensive, are not however large enough to be affected by the influence of the moon ; and as to their communication with the ocean, through such narrow inlets, it is impossible in a few hours’ time that they should receive and return water enough to raise or depress them in any considerable degree. In general, therefore, we may observe, that all tides are much higher, and more considerable, in the torrid zone, than in the rest of the ocean ; the sea in those parts being generally deeper, and less affected by changeable winds, or winding shores.* The greatest tide we know of, is that at the mouth of the river Indus, where the water rises thirty feet in height. How great, therefore, must have been the amazement of Alexander’s soldiers at so strange an appearance ! They wrho always before had been ac- customed only to the scarcely perceptible risings of the Mediterranean, or the minute intumescene of the Black Sea, when made at once spectators of a river rising and falling thirty feet in a few hours, must, no doubt, have felt the most extreme awe, and, as we are told,~f~ a mixture of curiosity and apprehension. The tides are also remarkably high on the coasts of Malay, in the straits of Sunda, in the Red Sea, at the mouth of the river St. Lawrence, along the coasts of China and Japan, at Panama, and in the gulph of Bengal. The tides at Tonquin, however, are the most remarkable in the world. In this part there is but one tide, and one ebb, in twenty-four hours ; whereas, »s we have said before, in other places there are two. Be' sides, there, twice in each month, there is no tide at all. when the moon is near the equinoctial, the water being hu some time quite stagnant. These, with some other od appearances attending the same phenomena, were con sidered by many as inscrutable ; but Sir Isaac with peculiar sagacity, adjudged them to arise from concurrence of two tides, one from the South Sea, and other from the Indian Ocean. Of each of these there come successively two every day; two at one * Buffon, vol. ii. p. 187. f Quintus Curtius. THE EARTH. 151 greater, and two at another that are less. The time be- tween the arrival of the two greater, is considered by him as high tide ; the time between the two lesser, as ebb. In short, with this clue, that great mathematician solved every appearance, and so established his theory as to silence every opposer. This fluctuation of the sea from the tides, produces another, and more constant rotation of its waters, from the east to the west, in this respect following the course of the moon. This may be considered as one great and general current of the waters of the sea ; and although it be not every where distinguishable, it is nevertheless every where existent, except when opposed by some particular current or eddy, produced by partial and local causes. This tendency of the sea towards the west, is plainly per- ceivable in all the great straits of the ocean ; as, for instance, in those of Magellan, where the tide running in from the east, rises twenty feet high, and continues flowing six hours ; whereas the ebb continues but two hours, and the current is directed to the west. This proves that the flux is not equal to the reflux ; and that from both results a motion of the sea westward, which is more powerful during the time of the flux than the reflux. But this motion westward has been sensibly observed by navigators, in their passage back from India to Madagascar, and so on to Africa. In the great Pacific Ocean also it is very perceivable ; but the places where it is most obvious, as was said, in those straits which join one ocean to another. In the straits between the Maldivia islands, in the gnlph of Mexico, between Cuba and Jucatan. In the straits °f the gulph of Paria, the motion is so violent, that it hath Reived the appellation of the Dragon’s Mouth. North - ward, in the sea of Canada, in Waigat’s straits, in the straits 1 Java, and, in short, in every strait where the ocean on one Part pours into the ocean on the other. In this manner, erefore, is the sea carried with an unceasing circulation tile globe ; and, at the same time that its waters are P 8 led backward and forward with the tide, they have thus a ^gressive current to the west, which though less observa- not the less real. oth eS1^es .these two general motions of the sea, there are 18 which are particular to many parts of it, and are 152 A HISTORY OF called currents. These are found to run in all directions* east, west, north, and south ; being formed, as was said above, by various causes ; the prominence of the shores, the narrowness of the straits, the variations of the wind, and the inequalities at the bottom. These, though no great object to the philosopher, as their causes are generally local and obvious, are nevertheless of the most material consequence to the mariner ; and without a knowledge of which he could never succeed. It often has happened, that when a ship has unknowingly got into one of these, every thing seems to go forward with success, the mariners suppose themselves every hour approaching their wished -for port, the wind fills their sails, and the ship’s prow seems to divide the water ; but, at last, by miserable experience they find, that instead of going forward, they have been all the time receding. The business of currents, therefore, makes a considerable article in navigation ; and the direction of their stream, and their rapidity, has been carefully set down. This some do by the observation of the surface of the current ; or by the driving of the froth along the shore ; or by throwing out what is called the log-line , with a buoy made for that purpose, and by the direction and motion of this, they judge of the setting and the rapidity of the current. These currents are generally found to.be most violent under the equator, where indeed ah the motions of the ocean are most perceivable Along the coasts of Guinea, if a ship happens to overshoot the mouth r-f any river if is bound to, the current prevents its return ; so that it is obliged to steer out to sea, and take a very large compass, in order to correct the former mistake. These set in a contrary direction to the general motion of the sea west- ward ; and that so strongly, that a passage which, with the current, is made in two days, is with difficulty performe in six weeks against it. However, they do not exten above twenty leagues from the coast : and ships going t0 the East Indies, take care not to come within the sphere, of their action. At Sumatra, the currents, which are tremely rapid, run from south to north ; there are a ^ strong currents between Madagascar and the GaPe ^ Good Hope. On the western coasts of America, the ^ rent always run from the south to the north, w THE EARTH. 153 south wind, continually blowing, most probably occasions this phenomenon. But the currents that are most re- markable, are those continually flowing into the Medi- terranean sea, both from the ocean by the straits of Gib- raltar, and at its other extremity, from the Euxine sea by the Archipelago. This is one of the most extraordinary appearances in nature ; this large sea receiving not only the numerous rivers that fall into it, such as the Nile, the Rhone, and the Po, but also a very great influx from the Euxine sea. on one part, and the ocean on the other. At the same time, it is seen to return none of those waters it is thus known to receive. Outlets running from it there are none ; no rivers but such as bring it fresh sup- plies; no straits but what are constantly pouring their waters into it : it has, therefore, been the wonder of man- kind in every age, how, and by what means, this vast concourse of waters are disposed of ; or how this sea, which is always receiving, and never returning, is no way fuller than before. In order to account for this, some have said, that the water was re-conveyed by subter- raneous passages into the Red Sea.* There is a story told of an Arabian cailiff, who caught a dolphin in this sea; admiring the beauty of which, he let it go again, having previously marked it by a ring of iron. Some tune after a dolphin was caught in the Red Sea, and quickly known by the ring to be the same that had been taken in the Mediterranean before. Such, however, as ave not been willing to found their opinions upon a smry, have attempted to account for the disposal of the Raters of the Mediterranean by evaporation. For this Purp°se they have entered into long calculations upon the *nt i°f ifc.S surface’ and the quantity of water that the ^ rfdsed fr°m sucdl a surface in a year. They strait C°^pUte h°W much water runs in bv its rivers and by evS ln that time ’ and find> that the quantity exhausted river<; aJ)01'atlon> greatly exceeds the quantity supplied by tisfactor*! ?5fs’ ^is solution, no doubt, would be sa- .as Weji ^ ’ dld not the ocean, and the Euxine, evaporate the j • Mediterranean : and as these are subject to e iam, it must follow, that all the seas will in Vn. * Kircher, Mund. Subt. vol. i. 0l- w. u A HISTORY OF ‘ 154 tliis respect be upon a par ; and, therefore, there must be some other cause for this unperceived drain, and continual supply. This seems to be satisfactorily enough accounted for by Dr. Smith, who supposes an under current running through the straits of Gibraltar, to carry out as much water into the ocean, as the upper current continually carries in from it. To confirm this, he observes, that nearer home, between the North and the South Foreland, the tide is known to run one way at top, and the ebb another way at bottom. This double current he also confirms by an experiment communicated to him by an able seaman, who being with one of the king’s frigates in the Baltic, found he went with his boat into the mid- stream, and was carried violently by the current ; upon which a basket was sunk, with a large cannon-ball, to a certain depth of water, which gave a check to the boat’s .notion : as the basket sunk still lower, the boat was driven, by the force of the water below, against the upper current ; and the lower the basket was let down, the stronger the under current was found, and the quicker was the boat’s motion against the upper stream, which seemed not to be above four fathom deep. From hence we may readily infer, that the same cause may operate at the straits of Gibraltar; and that while the Mediterranean seems replenishing at top, it may be emptying at bottom. The number of the currents at sea are impossible to be recounted, nor indeed are they always known ; new' ones are daily produced by a variety of causes, and as quickly disappear. When a regular current is opposed by another in a narrow strait, or where the bottom of the sea is very uneven, a whirlpool is often formed. These were formerly considered as the most formidable ob- structions to navigation ; and the ancient poets and his- torians speak of them with terror ; they are described as swallowing up ships, and dashing them against the. roc^ at the bottom ; apprehension did not fail to add inl8t^ nary terrors to the description, and placed at the of the whirlpool a dreadful den, fraught with rIlon1s_i,_ whose howlings served to add new horrors to the ings of the deep. Mankind at present, however, these eddies of the sea with very little appre hive ^ and some have wondered how the ancients could a THE EARTH. 155 much overcharged their descriptions. But all this is very naturally accounted for. In those times when navigation was in its infancy, and the slightest concussion of the waves generally sent the poor adventurer to the bottom, it is not to be wondered at that he was terrified at the violent agitations in one of these. When his little ship, but ill fitted for opposing the fury of the sea, was got within the vortex, there was then no possibility of ever leturning. To add to the fatality, they were always neai the shore ; and along the shore was the only place where this ill-provided mariner durst venture to sail. These were, therefore, dreadful impediments to his navi- gation ; for if he attempted to pass between them and the shore, he was sometimes sucked in by the eddy; and if he attempted to avoid them out at sea, he was often sunk by the storm. But in our time, and in our present im- proved state of navigation, Charybdis, and the Euripus, * with all the other irregular currents of the Mediterranean* are no longer formidable. Mr. Addison, not attending to this train of thinking, upon passing through the straits ol bicily, was surprised at the little there was of terror 111 the present appearance of Scylla and Charybdis; and seems, to be. of opinion, that their agitations are much diminished since the times of antiquity. In fact, from the reasons above, all the wonders of the Mediterranean sea are described in much higher colours than they merit, 0 us who are acquainted with the more magnificent terrors the ocean. The Mediterranean is one of the smoothest u most gentle seas in the world : its tides are scarcely L?i!Vab C’ , exCePt in the SulPh of Venice, and ship- "0rld S aiG eSS known there than in any other part of the Ti • , are nV”, ocean’ therefore, that these whirlpools and 1;)ltlcl,Iarly dangerous, where the tides are violent, railed m ^S68? fierce* To mention only one, that "Inch : Maehtroom, upon the coasts of Norway, 'n wn u°n" as th.e most dreadful and voracious *'gnifies It ’ ^he name it has received from the natives, tfreat shar ^ ^ the sea ; since ^ey suppose that a d'arged R6 °’+ t iC wa^er the sea is sucked up and dis- mal p J ! s vortex. A minute description of the in- s is not to be expected, since none who were A HISTORY OF there ever returned to bring back information. The body o the waters that form this whirlpool, are extended in a circle above thirteen miles in circumference.* In the midst of this stands a rock, against which the tide in its ebb is dashed with inconceivable fury. At this time it instantly swallows up all things that come within the sphere of its violence, trees, timber, and . shipping. No skill m the manner, nor strength of rowing, can work an escape : the sailor at the helm finds the ship at first go in a current opposite to his intentions ; his vessel’s motion, t ough slow in the beginning, becomes every moment more rapid ; it goes round in circles still narrower, and narrower, till at last it is dashed against the rocks, and instantly disappears: nor is it seen again for six hours; till the tide flowing, it is vomited forth with the same vio- lence with which it was drawn in. The noise of this dreadful vortex still farther contributes to increase its terror, which, with the dashing of the waters, and the dreadful valley, if it may be so called, caused by their circulation, makes one of the most tremendous objects in nature. J CHAP. XVII. OF THE CHANGES PRODUCED BY THE SEA UPON THE EARTH. From what has been said, as well of the earth as of the sea, they both appear to be in continual fluctuation. I he earth, the common promptuary that supplies sub- sistence to men, animals, and vegetables, is continually furnishing its stores to their support. But the matter which is thus derived from it, is soon restored and laid down again to be prepared for fresh mutations. The transmi' gi ation of souls is, no doubt, false and whimsical ; but nothing can be more certain than the transmigration of bodies : the spoils of the meanest reptile may go to the formation of a prince ; and, on the contrary, as the p°e* * Kircher, Mund, Subt. vol, i. p. 156. THE EARTH. 157 has it, the body of Caesar may be employed in stopping a beer-barrel.. From this, and other causes, therefore, the earth is in continual change. Its internal fires, the deviation of its rivers, and the falling of its mountains, are daily altering its surface ; and geography can scarcely recollect the lakes and the vallies that history once described. But these changes are nothing to the instability of the ocean. It would seem that inquietude was as natural to it as its fluidity. It is first seen with a constant and equable motion going towards the west; the tides then interrupt this progression, and for a time drive the waters in a con- trary direction : beside these agitations, the currents act their part in a smaller sphere, being generally greatest where the other motions of the sea are least; namely, nearest the shore : the winds also contribute their share in this universal fluctuation ; so that scarcely any part of the sea is wholly seen to stagnate. Nil enim quiescit, undis impellitur unda, Et spiritus et calor toto se corpore miscent. As this great element is thus changed, and continually labouring internally, it may be readily supposed that it produces correspondent changes upon its shores, and those parts of the earth subject to its influence. In fact, it is every day making considerable alterations, either by overflowing its shores in one place, or deserting them in others; by covering over whole tracts of country that !vere cultivated and peopled, at one time ; or by leaving its bed to be appropriated to the purposes of vegetation, a»d to supply a new theatre for human industry, at another. In this struggle between the earth and the sea for do- minion, the greatest number of our shores seem to defy e whole rage of the waves, both by their height, and the acky materials of which they are composed. The coasts of Ira’ f°r *?stance>* are bordered with rocks of marble j: .• 1 e^e,nt kinds, the quarries of which may easily be Pen!r^Ui1S at a d*stance fr°m sea, and appear like per- * cular columns of the most beautiful kinds of marble. * Buffon, vol, ii. p, 199. A HISTORY OF 158 ranged along the shore. In general, the coasts of France, from Brest to Bourdeaux, are composed of rocks ; as are also those of Spain and England, which defend the land, and only are interrupted, here and there, to give an egress to rivers, and to grant the conveniences of bays and harbours to our shipping. It may in general be re- marked, that wherever the sea is most violent and furious, there the boldest shores, and of the most compact ma- terials, are found to oppose it. There are many shores several hundred feet perpendicular, against which the sea, when swollen with tides or storms, rises and beats with inconceivable fury. In the Orkneys,* where the shores are thus formed, it sometimes, when agitated by a storm, rises two hundred feet perpendicular, and dashes up its spray, together with sand and other sub- stances that compose its bottom, upon land, like showers of rain. From hence, therefore, we may conceive how the violence of the sea, and the boldness of the shore, may be said to have made each other. Where the sea meets no obstacles, it spreads its waters with a gentle intu- mescence, till all its power is destroyed, by wanting depth to aid the motion. But when its progress is checked in the- midst, by the prominence of rocks, or the abrupt elevation of the land, it dashes with all the force of its depth against the obstacle, and forms, by its repeated violence, that abruptness of the shore which confines its impetuosity. Where the sea is extremely deep, or very much vexed by tempests, it is no small obstacle that can confine its rage ; and for this reason we see the boldest shores projected against the deepest waters ; all less impediments having long before been surmounted and washed away. Perhaps of all the shores in the world, there is not one so high as that on the west of St. Kilda, which, upon a late admeasurement,^ was found to be six hundred fathoms perpendicular above the surface of the sea. Here also, the sea is deep, turbulent, and stormy; so that it requires great force in the shore to oppose its violence. In many parts of the world, and particularly upon the coasts of the East Indies, the shores, though not * Buffon, vol. ii. p. 191. t Description of St, Hilda. THE EARTH. 159 high above water, are generally very deep, and con- sequently the waves roll against the land with great weight and irregularity. This rising of the waves against the shore, is called by mariners the surf of the sea ; and in shipwrecks is generally fatal to such as attempt to swim on shore. In this case no dexterity in the swimmer, no float he can use, neither swimming-girdle nor cork- jacket, will save him ; the weight of the superincumbent waves breaks upon him at once, and crushes him with certain ruin. Some few of the natives, however, have the art of swimming and of navigating their little boats near those shores, where an European is sure of instant destruction. In places where the force of the sea is less violent, or its tides less rapid, the shores are generally seen to descend with a more gradual declivity. Over these, the waters of the tide steal by almost imperceptible degrees, covering them for a large extent, and leaving them bare on its recess. . Upon these shores, as was said, the sea seldom beats with any great violence, as a large wave has not depth sufficient to float it onwards, so that here only are to be seen gentle surges making calmly towards land, and lessening as they approach. As the sea, in the former description, is generally seen to present prospects of tumult and uproar, here it more usually exhibits a scene of repose and tranquil beauty. Its waters which, when surveyed from the precipice, afforded a muddy greenish hue, arising from their depth and position to the eye,* when regarded horn a shelving shore, wear the colour of the sky, and seem rising to meet it. The deafening noise of the deep sea, is here converted into gentle murmurs ; instead of the waters dashing against the face of the rock, it advances and recedes, still going forward, but with just force enough to push its weeds and shells, by insensible approaches, to the shore. There are other shores, beside those already described, which either have been raised by art, to oppose the sea’s aPproaches, . or, from the sea’s gaining ground, are threat- ened with imminent destruction. The sea’s being thus 6en *° S*ve and take away lands at pleasure, is, without * Newton’s Optics, p. 163—16T. A HISTORY OF 160 question, one of the most extraordinary considerations in all natural history. In some places it is seen to ob- tain the superiority by slow and certain approaches ; or to burst in at once, and overwhelm all things in un- distinguished destruction ; in other places it departs from its shores, and where its waters have been known to rage, it leaves fields covered with the most beautiful verdure. The formation of new lands by the sea’s continually bringing its sediment to one place, and by the accumula- tion of its sands in another, is easily conceived. We have had many instances of this in England. The island of Oxney, which is adjacent to Romney-marsh, was pro- duced in this . manner. This had for a long time been a low level, continually in danger of being overflown by the river Rother ; but the sea, by its depositions, has gra- dually raised the bottom of the river, while it has hol- lowed the mouth ; so that the one is sufficiently secured from inundations, and the other is deep enough to admit ships of considerable burthen. The like also may be seen at that bank called the Dogger-sand^, where two tides meet, and which thus receives new increase every day, so that in time the place seems to promise fair for being habitable earth. On many parts of the coasts of France, England, Holland, Germany, and Prussia, the sea has been sensibly known to retire.* Hubert Thomas asserts, in his Description of the Country of Liege, that the sea formerly encompassed the city of Tongres, which, however, is at present thirty-five leagues distant from it: this assertion he supports by many strong reasons ; and among others, by the iron rings fixed in the walls of the town, for fastening the ships that came into the port. In Italy there is a considerable piece of ground gained at the mouth of the river Arno ; and Ravenna, that once stood by the sea-side, is now considerably removed from it* But we need scarcely mention these, when we find that the whole republic of Holland seems to be a conquest upon the sea, and in a manner rescued from its bosom. The surface of the earth, in this country, is below the level of the bed of the sea; and I remember, upon approaching * Buffon, vol. vi. p. 434. the earth. 161 the coast, to have looked down upon it from the sea, as into a valley: however, it is every day rising higher by the depositions made upon it by the sea, the Rhine, and the Meuse ; and those parts which formerly admitted large men or war, are now known to be too shallow to receive ships of very moderate burthen.* The province' of Jucatan, a peninsula m the gulph of Mexico, was formerly a part of the sea. This tract, which stretches out into the ocean a hundred leagues, and which is above thirty broad, is every where, at a moderate depth below the surface, composed of shells, which evince that its land once formed the bed of the sea. In Fiance, the town of Aigues Mortes was a port in the times of St. Louis, which is now removed more tnan four miles from the sea. Psalmodi, in the same kingdom, was an island in the year 815, but is now more than six miles from the shore. All along the coasts of Norfolk I am very well assured, that in the memory of man tne sea has gained fifty yards in some places, and has lost as much in others. Thus numerous, therefore, are the instances of new land* having been produced from the sea, which, as we see, is brought about two different ways : first, by the waters raising banks of sand and mud where their sediment is deposited • sec.ondly> by tbeir relinquishing the shore entirely, and having it unoccupied to the industiy of man. Lut as the sea has been thus known to recede from some hds, so has it, by fatal experience, been found to encroach of °rers ’ and Probably these depredations on one part for n S 10ie> may account f°r their dereliction from another : ie current which rested upon some certain bank having uPon eg/eSS 111 _S0JneI otber Place> it no longer presses new former bed> but Pours a11 its stream into the be atten ^iaaCe-;i 80 that evei7 inundation of the sea may shore. ^ Wlth S°me colTesPondent dereliction of another seafc; *his be> ,we. have numerous histories of the bosom " a 10ns, and. its burying whole provinces in its bear co.untnes that have been thus destroyed, file ton- r>f Wltness to the truth of history ; and shew leir houses, and the spires of their steeples. V0L* * Buffon, vol. vi. p. 424. X A HISTORY OF 162 still standing at the bottom of the water. One of the most considerable inundations we have in history, is that which happened in the reign of Henry I. which overflowed the estates of the Earl Godwin, and forms now that bank called the Goodwin Sands. In the year 1546, a similar irruption of the sea destroyed a hundred thousand persons in the territory of Dort ; and yet a greater number round Dullart. In Friezland, and Zealand, there were more than three hundred villages overwhelmed ; and their ruins continue still visible at the bottom of the water in a clear day. The Baltic Sea has, by slow degrees, covered a large part of Pomerania ; and, among others, destroyed and overwhelmed the famous port of Vineta. In the same manner, the Norwegian Sea has formed several little islands from -the main land, and still daily advances upon the continent. The German Sea has advanced upon the shores of Holland, near Catt ; so that the ruins of an ancient citadel of the Romans, which was formerly built upon this coast, are now actually under water. To these accidents several more might be added ; our own historians, and those of other countries, abound with them ; almost every flat shore of any extent, being able to shew something that it has lost, or something that it has gained from the sea. There are some shores on which the sea has made tem- porary depredations ; where it has overflowed, and after remaining perhaps some ages, it has again retired of its own accord, or been driven back by the industry of man.* There are many lands in Norway, Scotland, and the Mai* livia Islands, that are at one time covered with water, and at another free. The country round the isle of Ely, in the times of Bede, about a thousand years ago, was one of the most delightful spots in the whole kingdom : it ^as not only richly cultivated, and produced all the necessaries of life, but grapes also, that afforded excellent wine, TJ1^ accounts of that time are copious in the description of 1 s verdure and fertility ; its rich pastured covered flowers and herbage ; its beautiful shades, anjJ wl10^01^ air. But the sea, breaking in upon the land, overwlie. lr» the whole country, took possession of the sctfl, and toW4> * Buffon, vol. ii. p, 425. THE EARTH. 163 destroyed one of the most fertile vallies in the world. Its air, from being dry and healthful, from that time became most unwholesome, and clogged with vapours ; and the small part of the country that, by being higher than the rest, escaped the deluge, 'was soon rendered uninhabitable, from its noxious vapours. Thps this country continued under water for some centuries ; till at last the sea, by the same caprice which had prompted its invasions, began to abandon the earth in like manner. It has continued for some ages to relinquish its former conquests ; and although the inhabitants can neither boast the longevity, nor the luxuries, of their former pre-occupants, yet they find ample means of subsistence; and if they happen to survive the first years of their residence there, they are often known to arrive at a good old age. But although history be silent as to many other inun- dations of the like kind, where the sea has overflowed the country, and afterwards retired, yet we have numberless testimonies of another nature, that prove it beyond the possibility of a doubt : I mean those numerous trees that are found buried at considerable depths in places where either rivers or the sea has accidently overflown.* At the mouth of the river Ness, near Bruges, in Flanders, at the depth of fifty feet, are found great quantities of trees lying as close to each other as they do in a wood : the trunks, the branches, and the leaves, are in such perfect preservation, that the particular kind of each tree may instantly be known. About five hundred years ago, this Very ground was known tfo have been covered by the sea5 nor is there any history or tradition of its having been dry ground, which we can have no doubt must have been the case. Thus we see a country flourishing in verdure, producing large forests, and trees of various kinds, overwhelmed by the sea. We see this element depositing its sediment to a height of fifty feet; and its Raters must, therefore, have risen much higher. We see e same, after it has thus overwhelmed and sunk the so deep beneath its slime, capriciously retiring from vvje. ^ine coasts, and leaving that habitable once more, !ch it had formerly destroyed. All this is wonderful ; * Buffon, vol. ii. p. 403. 164 A HISTORY and, perhaps, instead of attempting to inquire after the cause, which has hitherto been inscrutable, it will best become us to rest satisfied with admiration. At the city of Modena in Italy, and about four miles round it, wherever it is dug, when the workmen arrive at the depth of sixty-three feet, they come to a bed of chalk, which they bore with an’ auger five feet deep : they then withdraw from the pit, before the auger is removed, and upon its extraction, the water bursts up through the aperture with great violence, and quickly fills this new- made well, which continues full, and is affected neither by rains nor droughts. But that which is most remark- able in this operation, is the layers of earth as we descend. At the depth of fourteen feet are found the ruins of an ancient city, paved streets, houses, floors, and different pieces of Mosaic. Under this is found a solid earth, that would induce one to think had never been removed ; how- ever, under it is found a soft oozy earth, made up of ve- getables ; and at twenty-six feet depth, large trees entire, such as walnut-trees, with the walnuts still sticking on the stem, and their leaves and branches in exact preservation. At twenty-eight feet deep, a soft chalk is found, mixed with a vast quantity of shells ; and this bed is eleven feet thick. Under this, vegetables are found again, with leaves, and branches of trees as before ; and thus alter- nately chalk and vegetable earth to the depth of sixty- three feet. These are the layers wherever the workmen attempt to bore ; while in many of thexn they also find pieces of charcoal, bones, and bits of iron. From this de- scription, therefore, it appears, that this country has been alternately overflowed and deserted by the sea, one age after another : nor were these overflowings and retirings of trifling depth, or of short continuance. When the sea burst in, it must have been a long time in overwhelming the branches of the fallen forest with its sediment ; and still longer in forming a regular bed of shells eleven feet over them. It must have, therefore, taken an age, at least, to make any one of these layers ; and we may con- clude, that it must have been many ages employed in the production of them all. The land also, upon being de- serted, must have had time to grow compact, to gat 1(; fresh fertility, and to be drained of its waters befoie THE EARTH. 165 could be disposed to vegetation, or before its trees could have shot forth again to maturity. We have instances nearer home of the same kind given us in the Philosophical Transactions ; one of them by Mr. Derham. An inundation of the sea, at Dagenham, in Essex, laying bare a part of the adjacent pastuie for above two hundred feet wide, and, in some places, twenty deep, it discovered a number of trees that had lain there for many ages before : these trees, by laying long under ground, were become black and hard, and their fibres so tough, that one might as easily break a wire, as any of them : they lay so thick in the place where they were found, that in many parts he could step from one to another : he conceived also, that not only all the adjacent marshes, for several hundred acres, were covered underneath with such timber, but also the marshes along the mouth of the Thames, for several miles. The meeting with these trees at such depths, he ascribes to the sediment of the river, and the tides, which constantly washing over them, have always left some part of their substance behind, so as, by repeated alluvions, to work a bed of vegetable earth over them, to the height at which he found it. The levels of Hatfield- Chace, in Yorkshire, a tract of above eighteen thousand acres, which was yearly over- flown, was reduced to arable and pasture-land, by one Sir Cornelius Vermusden, a Dutchman. At the bottom of this wide extent, are found millions of the roots and bodies of trees, of such as this island either formerly did, or does at present, produce. The roots of all stand in their proper postures ; and by them, as thick as ever they could grow, the respective trunks of each, some above thirty yards long. The oaks, some of which have been sold for fifteen pounds a piece, are as black as ebony, very lasting, and close-grained. The ash-trees are as soft as oarth, and are commonly cut in pieces by the workmen’s spades, and as soon as flung up into the open air, turn to dust. But all the rest, even the willows themselves, which ^re softer than the ash, preserve their substance and tex- llre to this very day. Some of the firs appear to have 'egetated, even after they were fallen, and to have, from eir branches, struck up large trees, as great as the parent runk. It is observable, that many of these trees have A HISTORY OF 166 been burnt, some quite through, some on one side, some have been found chopped and squared, others riven with great wooden wedges ; all sufficiently manifesting, that the country which was deluged had formerly been inhabited. Near a great root of one tree, were found eight coins of the Roman emperors ; and, in some places, the marks of the ridge and furrow were plainly perceivable, which testified that the ground had formerly been patient of cultivation. The learned naturalist who has given this description,* has pretty plainly evinced, that this forest in particular, must have been thus levelled by the Romans and that the falling of the trees must have contributed to the ac- cumulation of the waters. “ The Romans,” says he,