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its sides, and bending it over its body so as to be partially hidden.

"In all these operations no material was collected by the animal for its nest, but only the growing grass was either pressed down, or arranged so as to form a complete retreat.

"Unfortunately, the Frog soon disappeared altogether."

It is very probable that other functions, as yet unnoticed, may be performed by these members, since though the observation just above related is the first known observation of the kind, yet the manoeuvre recorded is no doubt a constant habit of the animal.

Doubtless, also, the very singular actions performed by the male Pipa and Obstetricans are performed by the help of the hinder extremities.

At the same time that the Frog shows so startling a resemblance in its leg muscles to higher animals, it shows

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Kici. 65.—Muscles of Ventral Surface of MtHoiraiuhut. On the right side, superficial muscles; on the left side, deeper muscles, the mylohyoidei, pectoralis, and external oblique being removed. Also superficial flexor muscles of right pectoral limb of Menobranchiis. B, biceps; CBl and CB2, coraco-brachiahs ; CHE, cerato-hyoidcus cxternus; EO, external oblique; PL, flexor longus; GH, genio-hyoid; JlfH' and AfH2, mylo-hyoideus ; _ OH, omo-nyoid: P, Pi, and P-, pectoralis; F, rectus; 5", subclavitis; SH, stcrno-hyoid; SL, supinator longus;' T, triceps.

as striking a difference from the leg muscles of animals with which it is nearly allied,—namely, with those of its class-fellows, the Urodela.

In Reptiles we meet with a muscle which takes origin from beneath the joints of the tail, and is inserted with the thigh-bone, and which has no certain representation amongst mammals, and is called ihe/emorocauda/.

In the Urodela we also meet with a femoro caudal, but no such structure exists in the Anoura. This is not so surprising when we recollect the abortive condition of the tail of the Frog. It might, however, have been expected that in the Tadpole, during the co-existence of the tai with the hind legs, and while it thus externally resemble

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Fie. 68. -Deeper Muscles of Extensor Surface ot Right Leg of Menopomi. B. biceps j.SB, extensor brevis; EH, extensor hallucis: ELD. extensor longus digitorum ; FC, lemoro-caudal: C.lfrfand G.Vi, muscles like the lesser glutei ; GMx and RF, great extensors of the thigh ; /, muscle resembling the iliacus . lie, ilio-caudal; IP, ilio-peroneal; SM and ST, muscles like the semimembranosus andsemi-tcndinosus respectively; TA, tibialis amicus.

the use of the members, as novel and interesting as the one just cited with regard to the nest-building actions of the Frog.

St. George Mivart {To be continued)



T^E have now to consider the complementary side of the phenomena. A stratum of air, 3 miles thick, on a perfectly calm day, has been proved competent to stifle both the cannonade and the horn-sounds emoloyed at the South Foreland; while the observations just recorded, one and all, point to the

mixture of air and aqueous vapour as the cause of this extraordinary Dhenomenon. Such a mixture could fill the atmosphere with an impervious acoustic cloud on a day of perfect optical transparency. But, granting this, it is incredible that so gieat a body of sound could utterly disappear in so short a distance, without rendering any account of itself. Supposing, then, instead of placing ourselves behind the acoustic cloud, we were to place ourselves in front of it, might we not, in accordance with the law of conservation, expect to receive by reflection the sound which had failed to reach us by transmission? The case


[A tunnel 2 in, square, 4 ft. S in. long, open at both ends, and having a glass front, runs through the box a b. The space above and below is divided into cells opening into the tunnel by oblong orifices exactly corresponding vertically. Each alternate cell of the upper series—the 1st, 3rd, 5th, &c.—communicates by a tube (Jil) with the upper reservoir (g), its counterpart in the lower series having a free outlet into the air. In like manner the 2nd, 4th, 6th, &c, of the lower series of cells are connected with the lower reservoir (/) ; and each has its direct passage into the air through the cell immediately above it. The gas distriDutors are filled from both ends at the same time; the upper with carbonic acid gas, the lo^er with coal-gas, by branches from their respective supply pipes {/, /;). A well-padded box (/) opening upon the end of the tunnel forms alittle cavern, whence the sound-waves are sent forth by an electric bell. A few feet from the other end of the tunnel, in a direct line, is a sensitive flam; {/:), provided with a funnel as sound collector, and guarded from chance currents by a shade.

The bell was set ringing. The flame, with quick response to each blow of the hammer, emitted a sort of musical roar, so regular were its alternate shortenings and lengthenings as the successive sound-pulses reached it. The gases were then admitted. Twenty-five flat jets of coal gas ascended from the tubes below, and twenty-five cascades of carbonic acid poured down from the tubes above. That which was a homogeneous medium had now fifty limiting surfaces, from each of which a portion of the sound was thrown back. In a few moments these successive reflections became so effective that not a single sound-wave having sufficient power to affect a flame so sensitive as to be knocked down, crushed, as it were, by a chirrup, or jingle, at twenty feet distance, could pierce the clear, optically-transparent, but acoustically-opaque atmosphere in the tunnel. So long as the gases continued to flow, the flame remained perfectly tranquil. When the supply was cut off, the gases rapidly diffused into tbe air. The atmosphere of the tunnel became again homogeneous, and therefore acoustically transparent, and the flime bowed down to each sound-pulse as before. Alternate layers of common air and air saturated with various vapours produce the same effect]

would then be strictly analogous to the reflection of light from an ordinary cloud to an observer placed between it and the sun. My fir.-t c»re, in the early part of the day in question, was to assure myself that our inability to hear the sound did not arise from any derangement of the instruments. At one P.M. I was

* Royal Institution, Friday evening Discourse by Prof. Tyndall, D.C. T,. Ml1 F. R.S. Jan. 16. (Continued from page 253.)

rowed to the shore, and landed at the base 01 the South Foreland cliff. Ths body of air which had already shown such extraordinary power to intercept sound, and which manifested this power still more impressively later in the day, was now in front of us. On it the sonorous wave3 impinged, and from it they were sent back to us with astonishing intensity. The instruments, hidJcn from vi-;\v, were,on the summit of a cliff

235 feet above us, the sea was smooth and clear of ships, the atmosphere was without a cloud, and there was no object in sight which could possibly produce the observed effect. From the perfectly transparent air the echoes came, at first with a strength apparenUy but Utile less than that of the direct sound, and then dying gradually and continuously away. The remark of my companion, Mr. Edwards, was: "Beyond saying that the echoes seemed to come from the expanse of ocean, it did not appear possible to indicate any more definite point of reflection." Indeed, no such point was to be seen; the echoes reached us as if by magic, from absolutely invisible walls. Arago's notion that clouds are necessary to produce atmospheric echoes is therefore untenable.

The reflection fiom aerial surfaces has never been experimentally demonstrated. It is wholly a matter of inference, and I wished very much lo reduce it to demonstration. I made one or two rough experiments on the transmission of sound through a series ol flames; and no doubt by proper arrangement such experiments might be made successful. I then thought that alternate layers of carbonic acid and coal £as, the one rising by its lightness, the other falling by its weight, would supply a heterogeneous medium suitable for the demonstration. To my assistant, Mr. Cottrell, who possesses in an eminent degree the skill of devising appara'us, I communicated this idea, leaving the realisation of it wholly to him, and he has carried it out in the most admirable manner. (For a sketch and description of the apparatus, see previous page).

During my recent visit to the United States I accompanied General Woodruff, the engineer in charge of two of the lighthouse districts, to the establishments at Staten Island and Sandy Hook, with the express intention of observing the performance of the steam-syren, which, under the auspices of Prof. Henry, has been introduced into the lighthouse system of the United States. Such experiments as were possible to make under the circumstances were made, and I carried home with me a somewhat vivid remembrance of the mechanical effect of the sound of the steam syren upon my ears and body generally. This I considered to be greater than the similar effect produced by the horns of Mr. Holmes ; hence the desire, on my part, to see the syren tried at the South Foreland. The formal expression of this desire was anticipated by the Elder Brethren, while their wishes were in turn anticipated by the courteous kindness of the Lighthouse Board at Washington. Informed by Major Elliott that our experiments had begun, the Board forwarded to the Corporation, for trial, the noble instrument now mounted at the South Foreland. The principle of the syren is easily understood. A musical sound is produced when the tympanic membrane is struck periodically with sufficient rapidity. The production of these tympanic shocks by puffs of air was first realised by Dr. Robison. But the syren itself is the invention of Cagniard de la Tour. He employed a box with a perforated lid, and above the lid a similarly perlora'ed disc, capable of rotation. The perforations were oblique, so that when wind was driven through the disc was set in motion. When the perforations coincided a puff escaped, when they did not coincide the current of air was cut off. The regular succession of impulses thus imparted to the air produce a musical note. Even in its small form, the instrument is capable of producing sounds of great intensity. The syren has been improved upon by Dove, and notably developed by llelmholtz.

In the steam syren patented by Mr. Brown of New York, a fixed disc and a rotatory disc are also employed, radial slits being cut in both discs instead of circular apertures. One disc is fixed across the throat of a trumpet-shaped tube, i6J ft. long, 5"in. diameter where the disc crosses it, and gradually opening out till at the other extremity it reaches a diameter of 2 ft. 3 in. Behind the fixed disc is the rotating one, which is driven by separate mechanism. The trumpet is mounted on a boiler. In our experiments steam of "o lbs. pressure has for the most part been employed. Just as in the air-syren, when the radial slits of the two discs coincide, a puff of steam escapes. Sound-waves of great intensity are thus sent through the air; the pitch of the note produced depending on the rapidity with which the puffs succeed each other; in other words, upon the velocity of rotation.

On October 8 I remained some lime at the Foreland, listening to the echoes. Of the horn-echoes I have already spoken : those of the syren were still more extraordinary. Like the others they were perfectly continuous, and faded as if into the distance gra

dually away. The single sound seemed rendered complex and multitudinous by its echoes, which resembled a band of trumpeters first responding close at hand, and then retreating ratiidly from us towards the coast of France. The syren echoes had eleven seconds duration, those of the horn eight seconds. With sorisdi of the same pitch the duration of the echo might be taken ts 4 measure of the penetrative power of the sound.

I moved away from the station so as to lower the power of the direct sound. This was done by dropping into the soundshadow behind an adjacent eminence. The echoes heard thus were still more wonderful than before. In the case of the syren, moreover, the reinforcement of the direct sound by the echo was distinct. One second after the commencement of the syren lilast, the echo struck in as a new sound. This fir.>t echo, therefore. must have been flung back by a body of air not more than 600 or 700 ft. in thickness.

There appears to be a direct connection between the duration of the echoes and the distance penetrated by the sound. Oa October 17 the perfect clearness of the afternoon caused me to choose it for the examination of the echoes. The echoes of that day, when our transmitted sound reached its maximum, exceeded in duration those of all other days. We heard the syren fifteen miles off. On the close of the day we found its echoes fourteen to fifteen seconds in duration, this long duration indicating the distance from which they were thrown back.

The visual clearness of the atmosphere on the morning of Oct. S, wasverygreat, the coast of France was very plainlysern, iheGrisna lighthouse, and the monument and cathedral of Jioulogne, were distinctly visible to the naked eye. At j) miles from the station, the horn was heard feebly, the syren clearly. At 2.30 P.m., .1 densely black scowl overspread the heavens to the W.S.W. At this hour, the distance being 6 miles, the horn wis heard very feebly, the syren more distinctly, all being hushed on board during the observations. A squall now approached us from the west. In the Alps, or elsewhere, I have rarely seen the beirens blacker. Vast cumuli floated in the X.E. and S.E.; vast streamers of rain were seen descending W.N. W. ; huge scrolls of cloud to the N.

At 7 miles distance the syren was not strong, and the hom was very feeble.

The heavy rain at length reached us, but although it was falling all the way between us and the Foreland, the sound, instead of being deadened, rose perceptibly in power. Hail was now added to the rain, and the shower reached a tropical violence. We stopped. In the midst of this furious squall both the hom and ihe syren were distinctly heard, and as the shower lightened, thus lessening the local pattering, the sounds so rose in power that we heard them at a distance of 7 J miles distinctly louder than they had been heard through the rainless atmosphere at 5 miles. This observation is entirely opposed to the statement of Derham, which has heen repeated by all writers since his time, regarding the stifling influence of falling rain upon sound. Hut it harmonises perfectly with our experience of July 3, which proved water in a state of vapour so mixed wiih air as to form non-homogeneous parcels, to be a most potent influence as regards the stoppage of sound. Prior to the violent shower, the nir had been in this flocculcnt condition, but the descent of the rain and hail restored in part the homogeneity of the atmosphere, and augmented its transmissive power. There may be states of the atmosphere associated with rain unfavourable to sound, but to rain itself I have never been able to trace the slightest deadening effect.

The observations continued till November 25. Up to that date we had no fog, but the experience of July I and of October 30, entirely destroy the notion that optical transparency and acoustic transparency go hand-in-hand. Both were days of ha:e sufficiently thick to hide the cliffs of the Foreland, but on the former the sounds reached 12 J. and on the latter 11J miles.

Keflection from the particles of fog and ha/.e has been hitherto held to blot out sound. The late dense fog in London enabled experiments to be made which entirely controvert this conclusion. On December 10 I made some experiments over the Serpentine. The fog was verydense. Mr. Cotterell stood on the walk below the south-west end of the bridge dividing Hyde Park from Kensington Gardens, while I went to the eastern end of the Serpentine. He blew a dog-whistle, and an organ-pipe sounding Mi3, which corresponds to 380 waves a second. I heard both distinctly. I then changed places with him, and listening attentively at the 1 ridge, heard for a time the distinct blast of the whistle only. The organ-pipe at length sent its deeper note to me across the water. It sometimes rose to great '■ istinctness, and sometimes fell to inaudibility. These fluctuations of which various striking examples have been observed, are due to the drifting of acoustic clouds, which act upon a source of sound, as the drifting of ordinary clouds upon the sun. The whistle showed the same intermittence as to period, but in the opposite sense for when the whistle was faint the pipe was strong, and vice versd.

There seemed to be an extraordinary amount of sound in the air. It was filled with a resonant roar from the Bayswater and Knightsbridge roads. The railway whistles were extremely distinct, while the fog-signals exploded at the various metropolitan stations kept up a loud and almost constant cannonade. I could by no means reconcile this state of things with the statements so categorically made regarding the influence of fog.

The water was on this day warmer than the air, and the ascending vapour was instantly in part condensed, thus revealing its distribution. Instead of being uniformly diffused, it formed wreaths and stria?. I am pretty confident that had the vapour been able to maintain itsell as such, the air would have been far more opaque to sound. In other words, I believe that the very cause which diminished the optical transparency of the atmosphere augmented its acoustical transparency.

This conclusion was confirmed by numerous observations made while the fog lasted.*

On Dec. 13 the fog was displaced by a thin haze. We could plainly see from one bank of the S .rpentine to the other, and far into Hyde Park beyond. There was a wonderful subsidence of the sound of the carriages, church bells, &c. Being at the bridge I listened for the sounds excited at the end of the Serpentine. With the utmost stretch of attention I could hear nothing. I walked along the edge of the water towards Mr. Cottrcll, and when I had lessened the distance by one half, the sound of his whistle was not so distinct as it had been at the bridge on the day of the densest fog. Hence the optical cleansing of the air by the melting of the fog had so darkened it acoustically, that a sound generated at the end of the Serpentine was lowered to at least one-fourth of its intensity at a point midway between the end and the bridge.

This opportune fog enabled me to remove the last of a congeries of errors which, ever since the year 1708, have attached themsdves to this question. As regards phonic coast-jignals, we now know exactly where we stand.

It is worth observing he e that the solution of the deportment of bail, rain, snow, haze, and log, as regards sound, der ends entirely upon observations made on the 3rd of July, which was about the last day that one would have chosen lor experiments on fog-signali Indeed, it had been distinctly laid down that observations on such a day would be useless; that they might indeed cnab'e us to weed away bad instruments from good ones, but could throw no light whatever on the quest in of fogsignaling. That the contrary is the case, is an illus'ration of the fact that the solution of a question often lies in a direction diametrically opposed to that in which it appears to lie. t


T HAVE advisedly, not thoughtlessly, used the expression ■*■ "terrestrial electricity." It is not an expression we are accustomed to. We are accustomed to "terrestrial magnetism;" we are accustomed to atmospheric electricity. The electric telegraph forces us to combine our ideas with reference to terrestrial magnetism and atmospheric electricity. We must link upon the earth and the air as a whole—a globe of eirlh and air—and consider its electricity whether in test or in motion. Then, as to terrestrial magnetism, of what its relation may be to perceptible electric manifestations we at present know nothing.

You all know that the earth acts as a great magnet. Dr. Ciilbert, of Colchester, made that clear nearly 300 years ago; but how the earth acts as a great magnet—how it is a magnet,— whether an electro magnet in \irtue of currents revolving round under the upper surface, or whether it is a magnet like a mass of steel or load-stone, we do not know. This we do know, that

* Since the first notices of this lecture appeared in the newspapers, strong confirmatory evidence has been received.

t The 'Oregoing report vat compiled from the notes of Prof. Tyndall. It if published with Prof. Tyndall's sanction, but was not written by himvelf.

it is a variable magnet, and that a first approximation to the variation consists in a statement of motion round the axis of figure—motion of the magnetic poles, round the axis of figure, in a period of from 900 to 1,000 years. The earth is not a uniformly magnetised magnet with two ]>olcs. and with circles of symmetry round those poles. But a first expression—as we should say in mathematical language the first "harmonic term" —in the full expression of terrestrial magnetism is an expression of a regular and symmetrical distribution such as I have indicated. Now, this is quite certain, that the axis of this first term, so to speak, or this first approximation, which, in fact, we might call the magnetic axis of the earth, does revolve round the axis of figure.

When the phenomena of terrestrial magnetism were first somewhat accurately observed about three hundred years ago, the needle pointed here in England a little to the east of north; a few years later it pointed due north; then, until about the year 1820, it went to the west of north ; and now it has come back towards the north. The dip has experienced corresponding variations. The dip was first discovered by the instrument maker, Robert Norman, an illustration, I may mention in passing, of the benefits which abstract science derives from practical applications—one of the most important fundamental discoveries of magnetism brought back to theory by an instrument maker who made mariner's compasses. Robert Norman, in balancing his compass cards, noticed that after they were magnetised one end dipped, and he examined the phemonenon and supported a needle about the centre of gravity, magnetised it, and discovered the dip. When the dip was first so discovered by Robert Norman it was less than it is now. The dip has gone on increasing, and is still increasing ; but abcut 50 years ago the deviation from true north was greatest. Everything goes on as if the earth had a magnetic pole revolving from west to east round the true North Pole, at a distance of 200 fiom it. About three hundred years ago its azimuth from V ngland was a little to the east of the north pole: then it came round, moving eastwards on the far side of the north pole, and round in a circle towards us on the left-hand side of the north pole, as looked to from England. That motion in a circle round the north pole has already been experienced within the period during which somewhat accurate measurements have been made—has been experienced to the extent of rather more than a quarter of the whole revolution; and we may expect that about 200 years from the present lime the magnetic pole will be between England and the North Pole; so that the needle will thus point due north, and the dip be greater than it has been for I,coo years, or will be for another. It is one of the greatest mysteries o' science, a mystery which 1 might almost say is to myself a subject of daily contemplation— what can be the cause of this magnetism in the interior of the earth? Rigid magnetisation, like that of steel or the loadstone, has no quality in itself in virtue of which we can cjneeive it to migrate round in the magnetised bar. Electric currents afford the more favoured hypothesis; they are more mobile. If we can conceive electric currents at all, we may conceive them flitting about. But what sustains the electric currents? People sometimes say, heedlessly or ignorantly, that thermoelectricity does it. Wc have none of the elements of the problem of thermo-electricity in the state of underground temperature which could possibly explain, in accordance with any knowledge we have of thermo-electricity, how there could so be sustained currents round the earth. And if there were currents round the earth, regulated by some cause so as to give them a definite direction at one time, we are as far as ever from explaining how the channel of those currents could experience that great secular variation which we know it does. Thus we have merely a mystery. It would be rash to suggest even an explanition. I may say that one explanation has been suggested. It was suggested by the great astronomer, Halley, that there is a nucleus in the interior of the earth, and that the mystery is explained simply by a magnet not rigi ily connected with the upper crust of the earth, but revolving round an axis differing from the axi? of roation of the outer crust, and exhibiting agradual precrssional motion independent of the precessional motion of the outer rigid crust. I merely say that has been suggested. I do not ask }ou to judge of the pr ibability: I would not ask myself to judge of the probability of it. No other explanation has been suggested.

But now, I say, we loo'* with hopefulness to the practical telegraphist for data towards a solu ion of this grand p-obl-n.. The terrestri d m gnet is subject, as a whole, to the grand secular variation which I have indicated. But, besides that, there are annual variations and diurnal variations. Every day the needle varies from a few minu'es on one side to a few minutes on the other side of its mean position, and at times there are much greater variations. What are called "magnetic storms" are of not very unfrequent occurrence. In a magnetic storm the needle will often fly twenty minutes, thirty minutes, a degree, or even as much as two or three degrees sometimes, from its proper position—if I may use that term—its proper position lor the time; that is, the position which it might be expected to have at the time according to the statistics of previous observations. I speak of the needle in general. The ordinary observation of the horizontal needle shows these phenomena. So does observation on the dip of the needle. So does observation on the total intensity of the terrestrial magnetic force.

The three elements, deflection, dip, and total intensity, all vary every day with the ordinary diurnal variation, and irregularly with the magnetic storm. The magnetic storm is always associated with a visible phenomenon, which we call, habitually, electrical;—aurora borealis, and, no doubt, also aurora of the southern polar regions. We have the strongest possible reasons for believing tha.t aurora consists of electric currents, like the electric phenomena presented by currents of electricity through what are called vacuum tubes, through the space occupied by vacuums of different qualities in the well-known vacuum tubes. Of course, the very expression, "vacuums of different qualities" is a contradiction in terms. It implies that there are small quantities of matter of different kinds left in those nearest approaches to a perfect vacuum which we can make.

Well now, it is known to you all that aurora borealis is properly comparable with the phenomena presented by vacuum tubes. The appearance of the light, the variations which it presents, and the magnetic accompaniments, are all confirmatory of this view, so that we may accept it as one of the truths of science. Well now—and htre is a point upon which, I think, the practical telegraphist not only can, but will, before long give to abstract science data forjudging—is the deflection of the needle a direct effect of the auroral current, or are the auroral current and the deflection of the needle common results of another cause?

With reference to this point, I must speak of underground currents. There again I have named a household word to everyone who has anything to do with the operation of working the electric telegraph, and not a very pleasing household word I must say. I am sure most practical telegraphers would rather never hear of earth currents again. Still we have got earth currents; let us make the best of them. They are always with us; let us see whether we cannot make something of them, since they have given us so much trouble. Now, if we could have simultaneous observations of the underground currents, of the three magnetic elements, and of the aurora, we should have a mass of evidence from which, I believe, without fail, we ought to be able to conclude an answer more or less definite to the question I have put. Are we to look in the regions external to our atmosphere for the cause of the underground currents, or are we to look under the earth for some unknown cause affecting terrestrial magnetism, and giving rise to an induction of those currents? The direction of the effects, if we can only observe those directions, will help us most materially to judge as to what answer should be given.

It is my desire to make a suggestion which may reach members of this society, ami associates in distant parts of the world. 1 make it not merely to occupy a little time in an inaugural address, but with the most earnest desire and expectation that something may be done in the direction of my suggestion. I do not venture to say that something may come from my suggestion, because, perhaps, without any suggestion from me, the acute and intelligent operators whom our great submarine telegraph companies have spread far and wide over the earth, are fully alive to the importance of such observations as I am now speaking of. I would just briefly say that this kind of observation is what ■would be of value for the scientific problem—to observe the indication of an electrometer at each end of a telegraph line at any time, whether during a magnetic storm or not, and at any time of the night or day. If the line be worked with a condenser at each end, this observation can be made without in the slightest degree influencing, and therefore without in the slightest degree disturbing, the practical work throughout the line. Put on an electrometer in direct connection with the line, connect the outside of the electrometer with a proper earth connection, and it may be observed quite irrespectively of the signalling; when the

signalling is done, as it very frequently is at submarine line*, with a condenser at each end. The saentiric observation mil be disturbed undoubtedly, and considerably distorted by the sending of messages, but the disturbance is only transient, and in the very pause at the end of a wor.i there will !>e a surheiently near approach to steadiness in the potential at the end of a «t>: connected with the electrometer to allow a careful observer to estimate with practical accuracy the indication that he would tar; were there no working of the line going on at the lime. A rnignetic storm of considerable intensity does not stop the working, does indeed scarcely interfere with the working, of a submarine line in many instances when a con lenser is used at each end.

Thus, observations, even when the line is working, may be made during magnetic storms, and again, during hours when the line is not working, if there are any, and even the very basic*: lines have occasional hours of rest. Perhaps, then, however, the operators have no time or zeal left, or, rather, 1 am sure they have always zeal, but I am not sure that theie is always time left, and it may be impossible for them to bear the strain longer than their office hours require them. But when there is an operator, or a superintendent, or a mechanic, or an extra operator who may have a little time on his hands, then, I say, any single observation or any series of observations that he can make on the electric potentials at one end of an insulated line will give valuable re uIts. When arrangements can be made for simultaneous observations of the potentials by an electrometer at the two ends of the line, the results will be still more valuable.

And, lastly, I may just say that when an electrometer is not available, a galvanometer of very large resistance may be employed. This will not in the slightest decree interfere with the practical working any more than would an electrometer, nor will it be more difficult to get results of the scientific observations not overpoweringly disturbed by the practical working if a galvanometer is used than when an electrometer is available. Tie more resistance that can be put in between the cable ani the earth in circuit with the galvanometer the better, and the sensibility of the galvanometer wilt still be found perhaps more than necessary. Then, instead of reducing it by a shunt, let steel magnets, giving a more powerlul direction to the needle, be applied for adjusting it. The resistance in circuit with the galvanometer between cable-end and earth ought tu be at least twenty-times the cable's copper-resistance to make the galvanometer observations as valuable as those to be had by electrometer.

I should speak also of the subject of atmospheric electricity. The electric telegraph brings this phenomenon into connection with terrestrial magnetism with earth current-, and through them with aurora borealis, in a manner for which observations made before the time of the electric telegraph, or without the aid of the electric telegraph, had aot given us any data whatever. Scientific observations on terrestrial magnetism, and on the aurora, and on atmospheric electricity, had shown a connection between the aurora and terrestrial magnetism in the shape of the disturbances that I have alluded to at the time of magnetic storms; but no connection between magnetic storms and atmospheric electricity, thunderstorms, or generally the state of the weather—what is commonly called meteorology—has vet been discovered.

The one common link connecting these phenomena hitherto known to us is exhibited in the electric telegraph. A telegraphic line—an air line more particularly, but a submarine line also— shows us unusually great disturbances, not only when there are auroras and variations of terrestrial magnetism, but when the atmospheric electricity is in a disturbed state. That it should be so electricians here present will readily understand. They will understand when they consider the change of electrification of the earth's surface which a lightning discharge necessarily produces.

1 fear I might occupy too much of your time, or else I would just like to say a word upon atmospheric electricity, and to call your attention to the quantitative relations which questions 10 connection with this subject bear to those of ordinary earth currents and the phenomena of terrestrial magnetism. In fair weather, the surface of the earth is always, in these countries it all events, found negatively electrified. Now the limitation to these countries that I have made suggests a point for the practical telegraphists all over the world. Let us know whether it is only in England, France, and Italy that in fine weather the earth's surface is negatively electrified.

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