\—"ft has been decided from observations made with Whewel's Anemometer, that there is on the average, a general motion of the air, from South to JNorth, two Maxima, and two Minima, have been shown in the force of wind during every twenty four hours, the force increases as the Barometer falls, «nd decreases as it rises. 22 die, and the circumstance of its getting almost vertical at the extreme North, would seem to give some grounds for the hy- pothesis, that the current goes downwards into the »earth to a great depth there at a particular point, and returns through the centre of the globe to the South, where it causes the Nee- dle to rise in proportion as it is depressed to the the North. These two facts, the depression and rise of the Magnet, are strong evidences in support of the supposition, that the cur- rent descends and returns through the crust of the earth to the South, and thus continuing a perpetual current. Electri- city is the rarest fluid yet known; and this has been one great cause of its real nature remaining so long undiscovered; in the manuscript that we hope soon to publish, we will clearly show that Electricity when visible, is nothing else than an accumulation of light, or light condensed and concentrated by mechanical or chemical means, such as friction, compres- sion, or decomposition of any kind of matter. ON THE TIDES OF THE OCEAN. It has been the practice with some authors in every age of the world, when in proposing a theory, or in maintaining an argument—to base their systems, and to draw their conclu- sions from false assumptions—assumptions that have never been thoroughly investigated or admitted as correct, by the general consent of mankind. In the theory we are about to propose, we shall endeavour to avoid this error, and we shall assume nothing but what has been long considered as well established by the great body of modern writers, and what in our judg- ment is highly probable. The diurnal motion of the earth, or more properly speak- ing, the revolution of the earth on its axis, (although only a theory) has never been called in question that I am aware of, as to its correctness, and it has been long received as the most satisfactory way of accounting for the alternation of day and night. But although we are bound to respect a theory, that has for a very long period obtained general belief, (at least until a more plausible one is proposed,) yet it does not follow, that because the principal part of a supposition is very probable, that the whole of the details must be correct; and an individual may very justly entertain doubts and surmises about some of these, and may so express himself, although he has nothing better to propose in their stead. 23 The revolution of the earth on its axis, is a very common mode of expression with philosophers, by which they would designate the motion of the earth; but they have left us en- tirely in the dark as to what kind of an axis it is—whether it is like the axle of a chariot wheel—or whether it remains stationary, and supported at each end. If the latter supposi- tion be the one admitted by learned men, the question natu- rally arises, what becomes of the supports, and what mate- rial is the axle composed of? It must be of a different material from the calcareous fragile substance of the earth, as is it has to undergo a great deal of friction; and the part of the earth in contact with it must be of the same material. These considerations, together with the sound that might be supposed to be produced oy friction, and some other matters philosophers have said nothing at all about. It would appear that this part of their subject they were afraid to touch, and have accordingly passed it over entirely unnoticed, at least no- thing of the kind has come under our observation. This ope- ration appears as difficult a matter to account for as the motion of thefplanets; and indeed it appears to us far too unnatural and artificial, and constantly reminds us of the workshops of the mechanic and factories—instead of the simple and efficient ope- ration of nature. We cannot perceive why it is not just as pro- bable a supposition to suppose that the earth has no axis, and that it is all the time falling into space, revolving as it descends, and that the whole of the planetary system is descending in like manner; but that each by a nice adjustment in density and the action of its own atmosphere, preserves its relative position. I do not propose this theory as free from inconsistencies, although I think it is just as plausible as the one at present established. It would however, be as difficult to account for the regular motion of the earth one way as the other, and in fact the cause of mo- tion is in my judgment very difficult to explain, except we refer it to the direct agency of divine power! In tracing the relation of one thing to another, we always arrive at a point with regard to motion, that is very difficult to comprehend, and are compel- led to acknowledge the existence of a supernatural power, that actually (to use a mechanical phrase,) ," puts his shoulder to the wheel." The cause of Motion then, we consider as a very strik- ing and forcible proof of the existence of a Deity, and leaves the arguments of atheists perfectly untenable. But we do not intend in this place to enter into a discussion concerning the cause of Motion. That the earth is a spherical body, and performs one revolution every twenty four hours, is all that is necessary for our purpose on this subject, and this we presume no one will dispute. There is only one subject more to which we would call the attention of our readers before pro- ceeding with the details of our theory, and that is the density of the atmosphere. It is now we believe, a doctrine very gene- 24 rally acquiesced in, that it is the pressure of the air on the sur- face of the earth, that prevents every thing from being detached. And were it not for this action, all substances not adhering, would fall or bound off, such as stones and animals, streams ot water, and even the ocean itself. It is the force of the circum. ambient air, that is known to be equal in weight to a column ot water thirty three feet high, that confines all objects to the sur- face of this globe, and hence, in obedience to this law, water is compelled to find its own level, and instead of rising upwards, or falling downwards as the case may be, it moves along the surface from the impetus it receives. Having made these remarks, we will proceed to detail a the^ ory, accounting for the tides and currents of the ocean, and that on a different principle from the one which now obtains. The spherical figure of the earth, its diurnal revolution, the compres- sion of the atmosphere, are the subjects on which we found our theory; and these we consider highly probable, and have ob- tained the general consent of mankind for a long period of time. The last mentioned subject, the weight of the air we consider as completely demonstrated. Before proceeding with our details, we will make a few re- marks designed to shew the improbability of the present theory of the tides, and these will be confined to one particular, the supposed influence of the Moon. The coincidence between the Moon and the Tides, was observed we believe long before Sir Isaac New- ton's time but it was he who first pointed out the mode in which that planet was supposed to act on the great body of the .ocean. After the best consideration that we are capable of giving the sub- ject, we do not perceive any relation established between the Moon and the Tides, and that the whole subject has been inferred from mere coincidence only. This mode of reasoning is to our minds far from being satisfactory, without its being taken in con- junction with some analogous circumstances—which are entirely wanting in the present case. It is inferred that because the Tides are higher at the full, than the wane of the Moon, and other coincidences, that she must exert an influence on them; and then the manner in which this is done is particularly described. This mode of reasoning has been a fruitful source of error in every age of the world, and the foundation of a great amount of su- perstition. If we were to reason from mere coincidence alone, a great many other operations of nature, besides the flux and re-flux of the waters of the ocean, might be attributed to the influence of the Moon, with as much probability as the said theory. Ani- mals are sometimes much agitated during full Moon. Chancel- lor Bacon, (it is recorded,) was subject to Syncope during the full Moon. Hoffman reports a young girl that labored under a painful swelling of the leg, beginning and ending with the in- crease and decrease of the Moon. These occurrences, together 25 with others that are unnecessary to mention, might with afl much propriety be ascribed to the influence of the Moon as the Tides. Yet there are but few learned men who believe in such influences, and still fewer who can trace or point out any con- nection ; and the bare isolated fact of the coincidence only, is all that remains to propound a theory upon. It is not denied but that the Moon may exert some power on this earth; her light may accelerate the ripening of grain, and promote the growth of plants, as some agriculturists uniformly affirm, but that she could exercise such a powerful attraction, as to lift the waters of the great deep to such an extent as is imagined in the case of the Tides,—is in our judgment extremely improbable, without its being felt equally on the earth as well as the ocean. All substances not permanently fixed to the surface would be immediately detached, and attracted towards that planet, and this would be effected much easier than with water, for in the latter case the additional circumstance of resistance, a natural tenden- cy to find its own level would have to be overcome. This part of the theory we consider as the most improbable of the whole system. The following is our hypothesis, which we offer as being more rational, and liable to fewer exceptions than any other. Philo- sophers have asserted that there are seven tenths of the whole earth covered with water, and the remaining three tenths only are dry land. Although this statement may be perfectly cor- rect, in the sense in which they understand it, yet there cannot be a doubt but that there is more land than water; for the . ocean itself, and all large bodies of water whatever, have land for their base, or rest upon land. I think it very probable how- ever, that there are exceptions to this remark, and these excep- tions I consider as the real cause of the rising and subsiding of the waters of the ocean: in other words, I presume that there are two vast openings at the bottom of the sea through the whole diameter of the earth, (crossing each other at right an- gles, and acting independent, or meeting in the centre as the case may be,) by which the waters are connected, and that du- ring the revolution of this globe, which is performed once in twenty four hours; each end of the opening will be uppermost alternately every six hours, and the waters of the uppermost end will press or sink towards the lower, causing a flow at the higher, and a full tide also at the lower; and of course there would be a flux and re-flux at the same place every twelve hours If this supposition were correct, we should of course have double the number of tides as days during the year; but a great many circumstances interfere to prevent this regularity, and it would only be in some situations where a perfect unifor- mity could take place. The parts of the earth at a distance from the opening, would have the tides less frequent during a vear than those situated near it, and the inequalities at the bot- tom of the ocean, would cause considerable irregularity m the motion of the tides. Mariners assert, that it is very difficuli 26 amongst islands to ascertain which way the tides flow; and this is doubtless caused by the uneven bottom obstructing the passage of the current. Where the bed of the ocean is smooth or nearly so, the tides would be more uniform and regular. This may account in some measure, for the irregularity of the tides in different parts of the world. But there is another cir- cumstance to be considered which would also tend to this result. In all likelihood, there are a number of these openings in differ- ent parts of the ocean remote from each other, in a different parallel of latitude, and of course, there would be a difference in the time of the rise and depression of their waters, owing to the motion of the earth, and where their tides meet, there would be a confused agitation of the sea. We have been informed by seafaring men, that there are different places in the ocean, where the waters have a rough boisterous appearance without any storm or wind'—may it not be owing to this circumstance, as much as to the action of the wind impelling a greater body of water in that direction. In order to convey as clear and distinct an idea as possible of these great hydraulic communications, we will endeavour to il- lustrate the operation in a very simple manner, so that it may be understood by persons of almost any capacity. If two funnels were soldered together at the small ends, then held in a perpendicular position, and filled at the upper end with water, it would immediately pass through, without spreading out at the funnel or flange below; because in this instance, the weight of the atmosphere presses everything towards the sur- face of the earth; and the gravity of the water itself, without the air, would effect this; but supposing that the soldered fun- nels were an isolated object, and were placed in the actual posi- tion of the earth itself, and encompassed like it by the pressure of the air equally on all sides,—it is evident then, that the gravity of the water of the upper funnel, independently of any other circumstance, would force the water to spread out towards the flange or edge of the lower funnel, instead of dropping from it; for in this instance, the atmosphere would prevent it; and this obpet as it gradually revolved round, would cause a flow and an ebb at the same place alternately, during one revolu- tion. If we now take a second pair of funnels and proceed with them in the same manner, placing them at right angles to the former, we shall have a complete example of the mode of ope- ration that is intended to be conveyed. This we imagine, is the mode of operation of these great water communications at the bottom of the sea, and we can perceive nothing in it at variance with the strictest principles of sound philosophy. It would be very foolish in us to attempt to state the dimen- sions of these openings; but if there is only one location of them, it must be very large, if there are a number of them, the dimensions will of course be less; still they must all be large ac- cording to our conceptions of objects; since their length through the whole diameter of the earth is very great, being generally 27 stated at seven thousand miles. Were I to hazard a conjecture about their locality, I should say that there may be one, and that probably the largest at the equator. We have been in- formed by a gentleman acquainted with nautical affairs, that the tides commence first at the equator, and proceed in every direc- tion, as if from a common centre. 1 do not consider this gen- tleman very good authority, but I am not aware of any circum- stance that militates against this observation.. It has been long a common remark with mankind, that the sea had no bottom; this idea doubtless originated in conse- quence of their unavailing efforts to fathom it, but it will be a singular circumstance, if this observation should prove correct. If we examine an American Almanac of 1841, containing calculations for the United States, and beginning with the month of January, we shall find the high water quoted for Boston, at 4 hours 14 minutes, and for New-York at 1 hour 14 minutes; here is a difference of 3 hours, and so on with other places; and in looking over the whole month, we find the returning full tide 1^ hours later each time, and sometimes only half an hour, or va- rying from half an hour, to one hour and fifty minutes. We have ascribed this difference to the distance the waters have to travel,—the inequalities at the bottom of the sea, and peculiar position of places. But there is still another circumstance to be accounted for, that is, the frequent occurrence of very high tides, and very low, or neap tides. In the present received theory, the Moon is held insufficient to account for that circumstance, and the aid of the Sun was called in. It is well known that the wind is a powerful agent in forcing the waters of the ocean in the direction in which it blows, and very high tides are sometimes the consequence of this; a storm of wind will also retard the flow of the tide when opposed to each other. Examples of both these statements are of very frequent occurrence, and sometimes they produce disas- trous results. It would seem to be the intention of nature, and no doubt a very provident law in her economy—that there should be a body of water continually in motion, adapted for different operations in that great element,—and where there is a surplus at one place, there is a deficiency at another, and in fact, this must of necessity be the case, according to the strictest logi- cal principles; for if there is a certain quantity of water on this earth, the removal of any portion from one place to another, must cause a flow at the one and an ebb at the other. It can- not be supposed that the Deity creates water at one place, and annihilates it at another. It is a much more reasonable conclu- sion, deducibletoo from well established principles, that there is not one drop more or less of water in the world since the creation; and the removal and replacing of it, causes that pleasing vari- ety that is so striking a trait in the works of nature. But it may be objected here, that these very high and very low tides, have an uniform character, occur every month, and of course must have a regular cause. We have already stated, that stropg 28 winds blowing for a length of time in one direction, might be one cause in producing the above effect. In confirmation of this, we will here state a simple case or two. It is evident that were a powerful wind blowing in the direction of North, a superabun- dance of the waters of the ocean would be driven in that direc- tion ; and if this should happen to be at a distance from any opening, of course there would less descend through, the wind preventing in a great degree its return to the great gulph, as it may be called, until one end had passed in revolving. If the wind continued long enough, the next high tide would also be very high at the same place, causing a succession of high tides, while at another situation, there wold be a succession of low^tides. In describing the revolution of the two openings, we have re- marked that there would be a flux and re-flux at the same place every 12 hours, or in other words, that there would be an ebb in 6 hours, and a flow in 6 hours more—alternately. This re- quires some explanation which we will proceed to give, as it is our intention to consider it fully in all its bearings. These two openings we have stated to pass through the whole diameter of the earth, crossing each other at right angles, and acting inde- pendent of each other; or they may be supposed to meet in the centre, which circumstance would make no difference as to the operation, as the waters would pass through the one only, that was perpendicular, in preference to taking any of the two pas- sages at the sides. These two passages would constitute four openings, or one at each side, supposing the circumference of the globe were divided into four parts, or if divided by time, it would leave 6 hours for each to change its location. There must then be an ebb and a flow alternately, which we suppose to be effected in this manner. While one opening is uppermost, there must of course be one directly under, the waters of the ocean will flow into the upper, and pass through to the lower, causing a flow at both places, or a full tide at the same time both with us and our antipodes. The openings at each side would have an ebb at the same time, causing a re-flux at the same instant both with us and our antipodes. Some people may nor conceive how the waters could flow from the sides to the upper cavity, as in that case they would have to rise from their level. To this objection it may be remarked, that the sea would flow towards the place where it had found an opening, and a current would be created, tending to that situation; and and besides, the spherical figure of the earth is so little at' short distances, that it has never been considered as opposing any ob- stacle to the passage of the waters either way. And indeed if we allow for the sake of argument that it does offer resistance we must also admit that there would be great facilities for its' descent, and the whole of the waters of the ocean where they encompassed the globe, would subside towards the lowest part with a vengeance, at every revolution of the earth. In the pre- sent received theory, and in that part of it that relates to the influence of the tides,—it is affirmed that that planet raises the 29 waters of the ocean at the same instant of time with us, as it does with our antipodes; and the arguments that they adduce to enforce this supposition, are in our judgment much more appli- cable to our theory than to the one just stated. At a first consideration, it would seem that these great hy- draulic communications could exist only where the ocean encompasses the globe from east to west, or any other direction; but this is not necessary in the fullest sense of the term, for large spaces of dry land might intervene between the cavities, provided there were a small opening for the egress and ingress of the waters, and a narrow space of two or three hundred miles could afford passage for a vast body of waters. All the great seas are found to be connected with each other. We consider that these explanations will afford a sufficiently clear idea of our theory to a common reader, without exhibiting a drawing; for he has only to conceive the upper cavity, (which he may call >»o. 1 if he chooses,) being filled to overflowing, in consequence of the rush of waters from both sides, and in the places of the earth adjacent to these sides or openings, there would be an ebb of the waters ; while at the places of the earth contiguous to No. 1, there would be a flow; as the earth revolved round in 6 hours, No. 1 would be at the side where it would have an ebb. In the third place, in 6 hours more, it would be right under where it would have a flow in consequence of the descent of the waters; in another 6 hours, it would be at the opposite side, where it would ebb; and in the last 6 hours, it would again arrive at the upper situation, having completed the circumference of the globe. It does not seem to have occurred to philosophers, that there might exist vast chasms extending through the whole diameter of the earth. The circumstance however, in our judgment, is very probable ; and independently of its being a very plausible me- thod of accounting for the cause of the motions of the waters, it is the most simple and rational [theory that we have as yet seen proposed. There are no other operations in nature that we are acquainted with, that has any resemblance to this, from which we might trace some analogy; "but there are some colla- teral circumstances that may be considered as having a ten- dency that way. We have read of the existence of vast chasms in the earth, on dry land—and there is one mentioned by Goldsmith in his Natural History, of which he says, " the in- habitants of the place where it is situated, have been in the habit of paying it a kind of adoration; they believed it had no bottom; and for a great length of time, they had been in the practice (at stated intervals,) of turning into the chasm, large droves of cattle and sheep by way of propitiatory sacrifice." We are also informed by the same author, and by other na- tural historians, " that there are fresh water lakes in different places of the world, that are subject to a flux and re-flux." May not this so happen in consequence of these waters commu- nicatino* through the whole diameter of the earth, to another 30 body of water, immediately under, or opposite; and as the earth revolved, the uppermost would press towards the lower, caus- ing an ebb at the one, and a flow at the other; for in this in- stance, there would be no water to flow from the sides, owing to the small area of the lake; and of course, there would only be a flow and an ebb every 24 hours ; whether such is the fact or not, I have not been able to learn. A writer in the New-York Mail, gives the following account of a remarkable pond in Sussex Co. State of New-York. " White Lake is situated about one mile west of the Paleres Rill, in the town of Stillwater. It is nearly circular, and about one third of a mile in diameter; it has no visible inlet, but its outlet is a never failing stream of considerable magnitude. From the centre, or dark portion of the lake at stated seasons, innume- rable quantities of shells are thrown up, of various sizes and forms, but all perfectly white, these float to the shore, and are thrown out upon the beach, or sink into shallow water; the soil around the lake is formed of them. In the centre of the lake, bottom has never been found; although it has been sounded to the depth of several hundred feet." The inference that may be deduced from the above extract, is this. That this pond may have a communication through the whole diameter of the earth, to another body of water contain- ing large quantities of these shells; and the circumstance of their being thrown up in the pond, in greater quantities at one time than another, might be owing to the body of water oppo- site, being carried by the action of the wind,*in that direction more so at one time than another, and of course would carry into the openings a larger quantity of shells. The following is extracted from a New-York Newspaper. Tide Wells.—" Seve- ral wells in Morris Co. New Jersey, regularly ebb and flow about six feet twice in twenty four hours, one of which is on the farm of Stephen Dickerson, near Whippany, the highest land in the vicinity. The water is said to be cool and refreshing." I have seen a statement going the rounds of the newspapers purporting to be related by a sea captain of truth and veracity^ that " he had known a vessel lost and sunk in one sea, and was found floating in another." Any of these statements taken se- parately, may not be considered very conclusive evidence in favor of our theory; but taken altogether they afford good ground for believing that the waters communicate through the whole diameter of the earth. There is one circumstance to which we will advert before taking our leave of the tides. It raav not appear clear to some readers, notwithstanding what we have alreadv remarked in what manner the waters of the ocean can rise from each side of the earth, and cause a flow at the top. To this we would remark, that the waters near the cavity would be absorbed first but the rush from the sides to supply their place would cause an overflow; and it must be remembered that the earth is a sphe- rical body, and whatever way the waters came, they would 31 have to come from the sides; that is if they had to come from a great distance; and of course there would be an ebb at the place from which the waters receded. This idea involves no greater inconsistency than the current of rivers, which flow up or down as the case may be, owing to the revolutions of the earth; for all streams of water flowing west or east, must be in that situation once in 24 hours. A river having its course di- rected to the west, the part of the earth where it is situated, must be descending'at one time, and rising at another. I confess that this doctrine may appear very singular to some people, who have not bestowed much attention on these subjects, and it may seem so to some people who have, as they are apt to conclude, that because water will fall off from a ball, or circle of any kind, instead of running round with it,—that it ought to do so with the earth; I explained this circumstance before, but I may remark again here, that the circle or ball alluded to, in order to be sub- ject to the same laws as the earth, would require to be placed in some sphere by itself; endowed with a rotary motion, and hav- ing an atmosphere of its own pressing against, and surrounding it on every side. We will here conclude our description of the tides, by reca- pitulating the principles that we think we have discovered. 1st. That there are two vast openings penetrating through the whole diameter of the earth, and crossing each other at right angles; and these openings, including their commencement and termina- tion, make four cavities, situated at regular intervals in the cir- cumference of the globe, at the bottom of the sea; and are the cause of the tides of the ocean. 2d.—The circumstance of each returning tide being later than its predecessor, we have ascribed to the distance the tide has to travel from its opening.- 3rd. The difference in time of the tides visiting different situations that might be supposed equal in distance, is owing to inequali- ties at the bottom of the sea, and the peculiar disposition ot pla- ces not being favorable to the advance of the waters. Lastly ; .1 will here elucilte this sta-enl,nt hy^ Iitt.e farthe.^^^J^^^ZTJ^Si est spot on the earth's.urfag, to t^ ^T^J^'^ m{leB . tbe third, 2000, and the fourth place had only begun to flow. ™™*>^*™^n n't this place two full tides in would approach the nearest spot in 12 hours or nearly so,. ™al""= ll \ l £d th next tide M hours, or double the ^*«*™*ZZZZ^^it°^^£ M the third*tt might be i of an hour later ^"^.^^^yi^XrMiy little ebb or flow, for the might be 4 an hour later= ^"J^J^^ begun to ebb. According to this returning f^^^^fSSXthi number of tides are about equal t» the calculaiion, there are some qarterslot »ew0"u W,V ig about j 0f an hour later than us prede- Jays and nights: at «her parte. e«h ^urmng tide is mo■ j» ^ ^ ^ rf cessor. At others again, it would be 4 Mnouriaier. b » produce 8tatcments in globe where the ebb and flow is bard,' P«f «P*W£ JJJ '*&f«a« being equal to the number of £r0of of all these assertions, «W.^^o^fSa Ion has not yet enabled us to ascer- days and night, m the year our lmnedmemis ot n each retuming t,de 13 tain whether such is the fact M.^ .^^L^L^S Winter Island, in the year 1821, '22, re- aboutjan hour later. Accotding to crt«ervauin. £ ™'rnetBrnl t'ide was about 20 minutes corded in Capt. Parry's Voyage, the average time^o eaont 0 Jf then there w „ter; and at the Mediterranean ^J™*^£ %X%&?miV\f it some places there . difference of time of ^to'Sj^^^Jtlm* parts of the earth, the tides will returi scarcely any tide at all, it is but.f«r tointe , wai i canJ.here possib.y be a full tide at, lea scarcely any tide at all it is but.to* to into; ™l"J°™n^rr pcSrbly be a full tide at, less at regular intervals of 12 hours only, whUe at no place cd.v H distances from the centre, to Ume^han 12 hours In the «W»>»™ ^'^ miteT W? »«» !"• supposition I do not ^&^™*1^™<$ « a»umPtion,for the purpose of elucidatm* our ideas 32 The spring and neap tides are owing to the action of the wind retarding or accelerating the advance of the waters, either at places very remote or very near. I may remark here, with" regard to the currents of the ocean, that the most plausible idea is, that these currents are rivers, flow- ing at the bottom of the sea; and have formed to themselves chan- nels, and that they preserve their course in these channels, and keep the great body of water at each side at abeyance—just as a river flowing through a lake will form a current in the middle, while the waters at each side will be perfectly still. It may be thought singular why the large body of waters does not rush in- to the current, and mix with it. But the fact is, the current has received its impetus, and always maintains its position; and the still waters on each side can no more prevent it, than a gentle breeze of wind can prevent a hurricane; the same result un- doubtedly obtains at the bottom of the sea. These currents, or rivers, occupy their channels, and are urged on in their course by the impetus they have received; the great body of sea wa- ter presenting but little obstacle. We may here introduce a fact to support this conclusion. It is asserted by mariners, that the course of some rivers may be perceived in the sea for some hundreds of miles. We will set this subject in a clear light, by asking and answering a question. What would be the result with regard to rivers, supposing the whole earth were overflow- ed with water—is it not very probable that all the greater would maintain their course, and flow as they at present do, they have formed to themselves channels, and would still di- rect their course in them, notwithstanding the great body of wa- ters with which they might be surrounded? It is true the wa- ters would mix in some degree, but the current would still be preserved, There cannot be a doubt but that the bottom of the present ocean was once dry land, and that the same aspect and general appearance with regard to rivers and inequalities exist there as on our earth-we think there can be no doubt of this, and therefore conclude that we have good grounds for believing that the currents existing in the sea are nothing but rivers If we take for an example the river St. Lawrence, that forms' the boundary line in some places between Canada and the United states—we shall perceive but very little current in the waters at the outlet of Lake Ontario, on commencement of the river • but it is sensibly known to sailors who make the passage much quicker down than up. Now supposing the river wire aug- mented to six times its present quantity of water, so as to have superadded a depth of 100 fathoms, and encompassed by still water to a great depth; is it not very probable that with all theae additions to its bulk, it would still maintain its current with considerable force We have not the least doubt, but that this would be the case, but where the stream is very rapid it would be more apparent No superincumbent mass of waters could rXr^itextremeagitated state °f the river at ^