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THE discrepancy between the date of Easter, 1954, April 18 as given by the tables in the Book of Common Prayer, and April 25 as given by the formula of Gauss, arises from a purely artificial contrivance of Clavius, who arranged the reformed calendar, which is thus described on p. 55 of "The Prayer Book Interleaved,' 1873, in an account of the calendar founded on a paper by Prof. De Morgan:-"It will never happen as to mean lunations, and rarely as to real ones, that in the same cycle there should be the lunation of a given month beginning on the same day in two different years of the cycle; and such a thing never happened in the unreformed Calendar. Clavius thought it desirable to imitate this in the new Calendar; and he observed that by taking the preceding day whenever the Epact was xxv., and the year of the cycle after the 11th, he could avoid the reiteration, and thus make the desired resemblance. "Whenever the Epact should be xxv., the year of the cycle being upwards of 11, say that the Epact is 26. This is not an astronomical correction, but a mere conventional mode of reconciling the choice which Clavius made of the mode of writing the Epacts with an essential peculiarity of the old cycle of 19 years which that mode of writing would have otherwise destroyed." "In 1954 the Golden Number is 17, the Sunday letter C, and the Epact according to the ordinary rule, XXV. Call it therefore xxvi. Thence April 17 will be the 14th day of the Paschal Moon, April 18, Easter Day. If the Epact xxv. were used April 25 would be Easter Day." The paper by Prof. De Morgan will be found in the "Companion to the British Almanac " for 1845.

My copy of NATURE for April 5 has long since gone to Bolivia, but probably your correspondents will find that Gauss did not take into account this artifice of Clavius. If in this century golden number 6 and Sunday letter C had coincided, Easter would have been set on April 25, because 6 comes in the cycle before 11 instead of after it as 17 does. An inspection of Table III. for finding Easter will show in the two half-lines for April 17 and 18 the arrangement made by Clavius. C. S. TAYLOR.

Banwell Vicarage, June 22.

Musical Thunder.

I

EARLY this morning a storm broke in this neighbourhood accompanied by heavy thunder. During the storm noticed that two of the peals began with a musical note of distinct and definite pitch. The "musical" portion of the peal lasted for about two seconds in each case, and the frequency of the note was both times about 400 per second.

This sound closely resembled a foot-fall in a narrow alley between high walls, and was only heard in two consecutive peals, separated by an interval of about a minute, the first being much more definitely musical than the second. In each case the interval between the flash and the first sound of thunder was about five seconds.

As is well known, a peal of thunder from lightning near at hand frequently sounds like a quick succession of raps or a volley of guns. Can the successive raps have followed one another so rapidly in this case that they combined to form a note?

If so, and if this note was due to a special configuration of reflecting surfaces in the clouds, possibly to others in slightly different positions, considerably different frequencies

may have been observed.

The fact that two peals only sounded in this manner separated by the short interval of about one minute, and that the second was not so decidedly musical as the first, seems to indicate that they were due to some rapidly changing source such as one might expect the reflecting surfaces of a cloud to be. I listened carefully to deter

mine that the note had its origin outside and was not due to resonance within the room, and in the second peal it was certainly outside, and probably had the first had its origin within the room I should have observed it.

I should be very glad to hear if anyone has observed a similar phenomenon. G. H. MARTYN.

1 Marden Road, S. Tottenham, N., June 24.

How do Inquiline Bees find the Nest of their Host>

THE following observation may serve to throw light on the above question, which has doubtless occurred to many entomologists. Yesterday I saw a specimen of the inquiline Coelioxys quadridentata enter the burrow of leaf-cutter bee, Megachile circumcincta. I dug the nest out of the burrow, and in so doing scattered the sand over an area of several square inches, completely destroying all appearance of a burrow. I sat down to await the return of the Megachile, in order to identify the species, and w much astonished to see (and capture) in the course of the next ten minutes two more specimens of Cœlioxys, which came hovering over the spot and alighted on the disturbed soil. I can think of no other explanation than that the cuckoos were attracted to the spot by the scent of the excavated nest. I may add that during several hours spent on the heath where this occurred I saw no other specimens of Cœlioxys, and, further, that there was a fresh south-east breeze blowing at the time, and that the bees came up against the wind.

64

Charterhouse, Godalming, June 24.

IN

OSWALD H. LATTER.

THE DISTURBANCE OF GREENWICH
OBSERVATIONS.

N the House of Lords on Thursday last, June 21 attention was directed to the threatened danger to the continued efficiency of the Royal Observatory Greenwich, caused by the great electrical generating station erected by the London County Council about half a mile due north of the observatory. The danger was referred to by the Astronomer Royal in his report to the Board of Visitors on May 30, a summary of which appeared in NATURE of June 7 (p. 135). The generating station is situated exactly in the Greenwich meridian, as will be seen from the accompanying photograph of a view looking north over the top of the transit room; and the tall chimneys shown in the picture, as well as the heated air from them, will obviously interfere with some observations of northern stars, which are essential for latitude and refraction. Moreover, from tests already made it appears that the powerful engines which are being installed at the generating station will cause vibrations that will seriously affect the value of observations by reflection from a mercury horizon, required for the fundamental work of the observatory.

This is not the first time that the effects of generating stations and electric tramway systems in the neighbourhood of the observatory have been pointed out. About six years ago the question of the possible effect of disturbances from electric railways on the magnetic work carried on at the observatory was given careful consideration; and the hope was then expressed that in the event of future electric tramways regulations would be laid down by the Board of Trade to secure adequate protection for the magnetic work. The records in this department of the observ. atory have been obtained continuously on a general system for sixty-five years, but the astronomical work extends over more than two centuries and a quarter, and it would be unfortunate if circumstances should arise to break this chain of continuity.

The generating station established at Deptford -nearly a mile from the observatory-to supply the London County Council Tramways with electric

power, has not caused such serious tremors as are produced by the small portion of the engineering plant now available for work at the new station, which is much nearer and larger. It appears, therefore, that if the new station is completed and equipped to supply electric power over London, though it was authorised only for the requirements of tramways, the work of the observatory will be impaired to no slight extent. When the scheme was first put forward, it was not supposed that the works or the engines would assume the gigantic and overpowering proportions now contemplated, and the Astronomer Royal, in referring to this point in his report, remarks:

The question arises why the immediate neighbourhood of the observatory should be selected for the planting of generating stations on an unprecedented scale to supply electric power to distant districts. The very powerful engines required for such a large output are liable to cause

FIG. 1-View of chimneys of the electrical works of the London County Council, looking north over the transit room of the Royal Observatory, Greenwich. The roof of the transit room is shown at the bottom of the picture.

vibrations the extent of which could hardly be anticipated from previous experience of ordinary engineering plant or of railway trains, which have hitherto not affected the work of the observatory.

The question as to the action the Government proposes to take to prevent the Royal Observatory from being injuriously affected by electric stations or other works, either at present or in the future, was asked in the House of Lords by Lord Ellenborough, who remarked that the difficulty which has arisen might have been obviated to some extent by the installation of turbines or triple-expansion horizontal engines instead of vertical engines. The Earl of Crawford pointed out that the interference with observations would arise from the heated air of the chimneys and the tremors due to machinery in motion. He said in the course of his remarks:

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The essentials for observation of an astronomical kind are stability and quietude. Nothing is so dangerous in astronomical observation as the unknown errors which have to be guarded against at the present time. If an error is known no great harm is done. In connection with the meridian, careful observations of the moon require to be made. For very many years the moon has been given over by the scientific world to Greenwich Observatory. The Royal Observatory has specialised on the moon mainly owing to the grand labours of Sir George Airy, the late Astronomer Royal, so that the position of the moon at a given time hence may be fairly accurately predicted. The observations at Greenwich, and the manner in which they have been carried out by the late Astronomer Royal, have led the whole scientific world to say, "Gentlemen, you know your moon so well, pray continue to be responsible for her." If now Greenwich is reduced to the position of saying that its lunar observations have not the weight and value which so far have attached to them, it will be a terrible blow to the reputation of the Royal Observatory and also to our existence as a scientific country. Another difficulty is that disputes as to boundaries between countries are mainly settled by astronomical observation as to the position of the moon, and as the moon is being constantly watched at Greenwich Observatory, applications are frequently received from foreign countries as to the error of the moon at such an hour on such a day. This also shows how extremely important it is that the observations at Greenwich should be trustworthy.

The suggestion that the observatory should be moved from Greenwich was considered by Lord Kelvin to be a most undesirable solution of the difficulty. He added:

Even at present we may look forward to possible changes in the arrangement of the works by which the electricity will not seriously disturb or practically cripple the astronomical observations at Greenwich. The disturbance caused at the observatory by the vibration from the electric works may be to some extent avoided by the substitution of steam turbines for reciprocating engines and the use of different electric dynamos. It is no exaggeration to say that the whole world outside, as well as the British Empire, would deplore anything that would injure the great and good work done in the Royal Observatory at Greenwich, and both Houses of Parliament should unite in preserving it.

As further development of the machinery equipment must increase the effects shown by the tests already made, Earl Cawdor considered that powers should be obtained, or set in action, to prevent the County Council from carrying out works that injure the observatory, and that the half a million pounds expended by the Council is a small sum compared with the matter at stake.

Replying on behalf of the Government, Lord Tweedmouth, First Lord of the Admiralty, made the following statement of the case; and his remarks, with those contained in the recent report of the Astronomer Royal to the Board of Visitors, are the only official comments available upon the subject:

Since the subject was raised it has been closely considered at the Admiralty. As to the origin of this generating station, in 1901 the London County Council resolved on it, and in 1902 a Bill was passed through Parliament. In this Bill was inserted a clause, known as the Observatory clause, which gave to the Board of Trade the power, if any use of electrical power was likely to affect injuriously the instruments used in the observatory, to require reasonable and proper precautions to be taken. This proposal was made public and approved by Parliament. It is a pity that the County Council did not more closely apprehend the possibility of danger in choosing this particular site, but some responsibility must also be attached to the various departments and to Parliament. At present, at any rate, no absolute damage has been done, but there is an apprehension of it when the station

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is developed to its fullest power. It will be almost the biggest generating station in the world when completed. Eight engines will work up to 52,000 horse-power, and the electricity generated will be sufficient to work the whole of the London tramway system. At the present time the Astronomer Royal said that no serious effect has as yet arisen in the working of the principal meridian instrument. The Astronomer Royal, however, says that the instrument which has been affected is the portable transit instrument used for determining longitude. From the large generating station at Deptford no damage has resulted, and there is no indication of any disturbance. What the authorities

have to do is to take very careful observation as to what is exactly going on at Greenwich. At present the station is never worked up to more than 3000 horse-power. A trial has been made of two engines, but the experiments are neither complete nor satisfactory. It is proposed to ask Prof. Ewing to represent the Admiralty in the observations to be taken, which must extend over a considerable time. The disturbances vary very much, and there is a great deal to be said as to the possibility of meeting the difficulties by reducing the high chimneys, though the Astronomer Royal does not think that the vapour of the chimneys seriously interferes with the observations. It is proposed also to ask the County Council to appoint a representative of its own for observation in order to have an independent report as to the exact amount of disturbance that might arise. The London County Council will not go on with the two chimneys, which are now only partly erected. Before doing anything it is necessary to discover whether by any re-arrangement of the machinery the threatened damage can be averted. Every effort will be made to make the inquiry a thorough one, and one which should command everyone's respect.

The position then, as stated by Viscount Goschen, is that a mistake has been made a mistake by the Admiralty, by the Astronomer Royal, by the County Council, and by Parliament. The matter affects, not only the Royal Observatory, but the whole world; and the best scientific knowledge available should be utilised to avert any danger which imperils the useful existence of the observatory or interferes with its work.

THE SEA-SERPENT.

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ΤΗ HE narrative of an encounter with the seaserpent" on December last off the coast of Para, given by Messrs. Nicoll and Meade-Waldo at the meeting of the Zoological Society held on June 19, has once more awakened interest in the question as to the possibility of the existence of a large unknown marine vertebrate animal. The appearance of the so-called "sea-serpent" has been recorded from time to time by quite a number of witnesses. Many of these alleged appearances were evidently based on objects other than vertebrate animals unknown to science, but others, as being witnessed by trustworthy and educated observers, are evidently worthy of more serious consideration. The importance of the recent case of which more anon-is that it was witnessed by two gentlemen who have undergone a long training in the observation of animals, and are therefore far less likely to be mistaken than persons who have not specially devoted themselves to the study of natural history.

To attempt to record on the present occasion all the trustworthy cases of the alleged appearance of the sea-serpent (for the sake of convenience we may discard the inverted commas) would much exceed our limits of space, and we may therefore refer our readers to the volume by Mr. A. C. Oudemans entitled the "Great Sea Serpent," published in 1892, where all the more important ones up to that date will be found mentioned. It may be profitable to

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"The sea-serpent, however, is always open to criticism. This wonderful animal has hardly ever been seen alike by any two observers. It is nearly always easy to a naturalist to understand the stories told. Sometimes it is a pair of whales that is seen; sometimes a long mass of floating seaweed deceives the distant observer; sometimes the serpent has large eyes and a crest behind the head; then it is a ribbonfish. I myself am one of the few professed naturalists who have seen the serpent. It was on a voyage to Rotterdam from the Thames. . . . It was a flock of cormorants, which were flying in line behind the waves, and which were viewed in the intervals between them with a sort of thaumoscopic effect."

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Clearly Mr. Moseley was not "on the side of the angels"; neither Sir Richard Owen, who attempted to explain the undermentioned appearance seen by the officers of the Daedalus by the seaweed theory; and that some of the appearances can be explained by Moseley's suggestions, or by a school of porpoises, may be candidly admitted.

Mr. F. A. Lucas, on the other hand, in his "Animals of the Past," although confessing himself an "agnostic" in regard to this subject, takes up a somewhat less uncompromisingly hostile attitude.

"Like the fossil man,'" he writes, "the seaserpent flourishes perennially in the newspapers, and despite the fact that he is now mainly regarded as a joke, there have been many attempts to rehabilitate this mythical monster and place him on a foundation of firm fact. The most earnest of these was that of M. Oudemans, who expressed his belief in the existence of some rare and huge seal-like creature whose occasional appearance gave rise to the reports of the sea-serpent. Among other possibilities it has been suggested that some animal believed to be extinct had really lived to the present day. Now there are a few waifs, spared from the wrecks of ancient faunas, stranded on the shores of the present, such as the Australian ceratodus and the gar-pikes of North America. If a fish of such ancient lineage as the gar-pike is so common, why may there not be a few plesiosaurs or a mosasaur in the depths of the ocean? The argument was a good one, the more that we may suppose' almost anything; but it must be said that no trace of any of these creatures has so far been found outside of the strata in which they have long been known to occur, and all the probabilities are opposed to this theory.'

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The event recorded by Messrs. Nicoll and MeadeWaldo took place in the forenoon of December 7, 1905, when they were on board the yacht Valhalla off the coast of Para. At a distance of about 100 yards from the vessel the two observers saw what appeared to be the vertical dorsal fin of some large animal, and a short time afterwards the head and neck of an animal was raised above the water some distance in advance of the fin. The head was compared to that of a turtle, while the neck appeared to be about 6 feet in length. The description, so far as we can judge, suggests a creature of not more than about 20 feet or 25 feet in length. Although the vessel was subsequently put about, no further signs of the seaserpent were seen during daylight. It is, however, noteworthy that during the night two of the ship's officers became aware of the presence of some large animal swimming alongside the yacht at a rapid pace; the two officers, it is stated, had no cognisance of the events of the morning.

R. L.

THE ROYAL SOCIETY CONVERSAZIONE.

A most significant feature in this circumstantial Without offering any suggestion as to what the account is that it tallies to some extent with the nature of the object seen by Messrs. Nicoll and Meadenarrative given by the officers of H.M.S. Daedalus Waldo really was, it may be pointed out that the testiof the appearance of the sea-serpent seen by them in mony of two such trained observers (supplemented by the year 1848 in the Atlantic. that of the officers of the Daedalus and by the two In the figures given by Oudemans the (double)" apparitions" off Tonkin) cannot possibly be brushed back-fin is very low, and the neck seems relatively aside in the light-hearted manner with which Prof. short and ill-defined. Revised restorations, however, Moseley treated the evidence available in his time. give a longer neck and no back-fin. It is possible, if a fin was present, that its apparent difference in height in the two instances was due to the animal swimming faster in one case than the other. Megophias megophias, it appears, is a name which has been suggested for the creature... In 1903 Prof. Racovitza (Bull. Soc. Zool, Paris, xxviii., p. 11) gave an account of a sea-serpent seen by Lieut. Lagresille in 1898 in Along Bay, Tonkin, and in 1904 M. Vaillant (Bull. Mus. Paris, x., p. 217) mentioned another apparition of an apparently similar creature in the same locality. In this second account the animal is described as being probably scaled, with a head like that of a turtle or a seal, and as "spouting" from terminally placed nostrils. It was also stated to move in undulations at one time vertical, at another horizontal. Two occurrences in the same locality are very noteworthy.

In each of these four instances it can scarcely be doubted that the object seen was a living creature (or creatures) of some kind, and that it (or they) was of the same general type. If the object were formed by more than one animal, cadit quaestio. If, on the other hand, it consisted of a single individual, furnished with a dorsal fin, a long, snake-like neck, and a head like a turtle, it could scarcely be any known living animal. Neither, it may be suggested, could it be even an unknown type of seal, especially since all the known members of that group come ashore to breed. The next question is, Could it have been a survivor of some Mesozoic reptilian? Two arguments, so far as they go, are against this. Firstly, the one referred to by Mr. True as to the absence of the remains of any such creature in Tertiary deposits, and secondly (on the hypothesis that it is an air-breathing vertebrate, and if not, why should it come to the surface at all?), the rarity of the seaserpent's appearance, the latter argument being applicable whether the creature is considered to belong to a supposed extinct group or not.

With regard to the fossil theory, it might be urged that the creature is an inhabitant of the deep sea, and consequently that its remains should not be expected to occur in Tertiary deposits, which belong for the most part, at any rate, to more or less shallow water. For what it is worth, it may be mentioned in reply that no traces of the creature have been found on the ocean bottom, where sharks' teeth and cetacean ear-bones are common. A more forcible objection is that, if the creature is in the habit of coming to the surface (as on the hypothesis of its existence it must), it cannot be a denizen of the abysses, no animal (despite the old belief in regard to whales) being able to live under such diversities of pressure. Ergo, its remains ought to occur in Tertiary deposits. Its stranded carcase ought also to have been found. If the creature be a "living fossil," the plesiosaurian group has the strongest claim to its ownership, as, although the zeuglodont cetaceans are the latest in time of possible extinct representatives, the smallness of its head prevents the reference of the sea-serpent (as described) to that group. As to the rarity of its appearance, it can scarcely be urged that only two or three (or even half a dozen) examples of the creature are in existence.

MANY of the exhibits of scientific apparatus and
objects at the second, or ladies', conversazione
held at the Royal Society on June 20 were the same
as those shown at the gentlemen's conversazione on
May 9.
As these have already been described
(May 17, p. 59), it is only necessary to refer now to
the new exhibits. During the evening demonstra-
tions, with lantern illustrations, were given by Dr.
Tempest Anderson, Sir William Crookes, and Mr.
Fred. Enock. Dr. Tempest Anderson described the
recent eruption of Vesuvius, his photographs showing
the phenomena during the later stages of the erup-
tion, as well as some of the results. In several cases
the views afforded a comparison with the conditions
of the same places as previously observed. Sir
William Crookes gave a short address with experi-
ments in illustration of some properties of the
diamond; and Mr. Fred. Enock described slides show-
ing by means of colour photography (Sanger Shep-
herd process) the adaptability of lepidopterous insects.
to their environment.

In the subjoined summary of the official catalogue, the exhibits are arranged roughly in groups of related subjects.

Dr. H. Forster Morley on behalf of the International Catalogue Committee: A map of the world was shown upon which thirty-one countries or regions were coloured. Each of these has established a Regional Bureau for indexing its scientific literature. The literature indexed is that published since January 1, 1901. Each annual issue of the catalogue contains seventeen volumes, dealing with seventeen sciences. A copy of the second annual issue was shown. The Regional Bureaus for France, Germany, and that for Polish literature employ the material prepared for the International Catalogue for the compilation of bibliographies of their own scientific literature. Specimens of these bibliographies were shown.-Prof. H. McLeod on behalf of the Committee of the Royal Society's Catalogue of Scientific Papers: An exhibit illustrating the course of operations in the preparation of the catalogue, which was fully described in an appendix to the descriptive programme of the conversazione.

Sir James Dewar, F.R.S.: (1) New charcoal calorimeter and thermoscope. Charcoal at the temperature of liquid hydrogen that has absorbed at atmospheric pressure considerable quantities of helium or hydrogen-or alternatively of nitrogen, oxygen, or air at their respective boiling points -is utilised in this instrument as a material that, by reason of changes in the volume of the occluded gas, exhibits great sensibility to heat and light radiation, and can be used in calorimetry at the temperature of solid hydrogen. (2) Charcoal vacua. Electric discharge tubes showing gradual gas absorption by charcoal cooled in liquid air until, after the Röntgen radiation stage, the electric resistance becomes so great that a discharge will not pass. (3) Spectrum tubes. (a) The less condensable gases of the atmosphere-helium and neon. (b) The more condensable gases of the atmosphere-krypton and xenon, each set of gases being separated by the charcoal method. (4) Some scientific uses of liquid air. (a) Electric ice crystals. (b) Rough measures of relative thermal conductivities in metals and alloys, by observing the height of the deposited ice cap when similar wires are placed alongside each other

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and the ends immersed in liquid air. The relative conductivities are as the squares of the height of the ice columns. (c) Spheroidal state of liquid air on the surface of different fluids and solutions, showing changes of volatility from the varying amount of vapour condensation; at the same time exhibiting interesting rotatory and translatory movements.-Department of Applied Mathematics, versity College, London: (1) Investigation into the stresses in masonry dams, Prof. Karl Pearson, F.R.S., and Mr. A. F. C. Pollard. The investigation suggested that the shear distribution should in each case be found from a model dam, before the stresses are determined by graphical methods. The existence of stretch in the tail of dams of ordinary type is confirmed by the experiments illustrated. (2) Solution of the problem of the random walk, Prof. Karl Pearson, F.R.S., and Mr. J. Blakeman. The diagrams shown give the sections of the frequency surface for two, three, four, five, six, and seven stretches or flights, and show the passage of the discontinuous function into Lord Rayleigh's continuous surface. The problem is of considerable importance from the standpoint of the migration of species, and was suggested by Major Ross's investigations into the infiltration of mosquitoes into a cleared district. The solution has been obtained by successive mechanical integration from the first case by using the functional relation between successive flights.-Mr. A. A. C. Swinton: Visibly luminous electrical discharges in vacuo obtained with comparatively low electrical pressures. Edison, Fleming, and others have shown that the passage of the electric discharge in vacuo is much facilitated by heating the kathode. Owen and Wehnelt have proved that this effect is enormously increased if the heated kathode be coated with oxides of the alkaline metals. The

present experiments show that similar results can be obtained by coating the kathode with radium, and that the effect will be greater when the kathode is heated than obtains without heating.-Mrs. Watts-Hughes and Mr. Richard Kerr: Floral, geometric, and other forms produced by the human voice in singing. Moistened water-colour is spread on paper attached to an india-rubber disc stretched over a cup-shaped vessel. The sound vibrations are communicated to the under side of the india-rubber through a tube in the side of the cup.-Mr. Oliver S. Dawson : Photographic prints in natural colours (Smith-Merckens process).-Messrs. Carl Zeiss, Jena: Photomicrographic apparatus for ultra-violet light (designed by Dr. Köhler).

A.

Mr. R. G. Durrant: Evidence to show that ionic separation occurs when solutions of acids or of salts are allowed to diffuse into sensitised jellies or solutions. Dr. O. Silberrad and Dr. R. C. Farmer: Stability test for cordite. This exhibit illustrated a method recently devised at the Chemical Research Department, Royal Arsenal, Woolwich, for the determination of the stability of cordite and other propellant explosives. It is well known that these explosives decompose gradually on storage, and may eventually ignite spontaneously, if their stability be not tested from time to time. The principle of the new test is based upon the results of several thousand experiments, and is the only method known which gives trustworthy results with cordites. The test has been adopted by the Service, and will shortly be made use of as a safeguard against spontaneous explosions in powder magazines, particularly in the tropics, where the deterioration takes place most rapidly. In examining cordites the procedure is briefly as follows:-50 grams of the explosive are maintained at 70° C. in a glass vessel fitted with a mercury manometer; the alteration in pressure is measured at intervals. A contraction takes place at first owing to the absorption of oxygen from the air; subsequently a gradual expansion occurs; the former of these phenomena has never previously been observed.-Dr. F. D. Chattaway: Copper mirrors obtained by the deposition of metallic copper upon glass. The method of silvering glass by depositing the metal in a thin film by reduction of some soluble silver compound has long been employed in the production of mirrors, but hitherto no method of similarly depositing copper in a brilliant film has been discovered. The exhibit showed a number of glass vessels on which copper had been thus deposited by a slow reduction of the black

oxide. The metal being protected from the air, such mirrors retain their lustre permanentiv.

Mr. G. F. Herbert Smith: Precious stones and simple methods for their identification. This exhibit illustrated the variety of precious stones which are available for ornamental purposes. A gem stone must be hard enough to resist the abrasive action of ordinary dust, and at the same time be either transparent or, if opaque, of pleasing colour. The number of mineral species suitable for the purpose is not so restricted as popularly supposed. The names employed by jewellers frequently differ considerably from the scientific nomenclature, being often associated with certain colours rather than particular species, r.g. topaz (yellow), sapphire (blue), ruby (red), emerald (green), and amethyst (violet). The colour, though the most obvious character of a stone, is the least trustworthy; and the hardness, while of immense importance as regards its durability, is of little discriminative value. On the other hand, the optical characters (refractivity, double refraction, and dichroism) and the specific gravity may be easily and accurately determined, and lead to the precise identification of the stone. In the case of practically all faceted transparent stones the refractivity and double refraction are sufficient for the purpose, and the stone need not be removed from its setting.-Sir William Crookes, F.R.S.: (1) Occurrence of the diamond. (a) Example of "blue ground in which diamonds are found, from the 1320-feet level, De Beers Mine; (b) diamantiferous gravel from the Pulsator, De Beers Mine; (c) selected stones from the Pulsator, De Beers Mine. (2) Models of crystals of diamond. (3) Cut and polished section of a piece of silicified wood found about twelve years ago in the untouched "blue ground of the Du Toits Pan Diamond Mine, Kimberley. (4) Polished section of the Cañon Diablo meteorite in which diamonds have been found.-Prof. W. Gowland (1) Portion of a meteorite containing diamonds found near Cañon Diablo, Arizona, and specimens of diamonds extracted from it. (2) Alloys of copper and calcium. A series of alloys ranging from 0.8 per cent. to 61.5 per cent. of calcium. All are brittle, and those containing 6 per cent. to 7 per cent. calcium extremely hard. The higher alloys decompose water, and are readily oxidised in the air. Specimens were also exhibited showing the effects of calcium on lead, tin, bismuth, aluminium, and coinage bronze.-Miss Rhodes: Stereoscopic views of the Victoria Falls and the Batoka Gorge of the Zambezi, and of the Batoka country east of the Falls. Photographed by the late Colonel F. W. Rhodes.

The Director, Royal Gardens, Kew: Sturt's desert pea (Clianthus Dampieri). A prostrate herbaceous plant, native of West Australia, first collected by Captain William Dampier. Under cultivation it is very delicate, but when grafted on the bladder senna (Colutea arborescens) it grows with vigour and flowers freely.-Dr. F. E. Fritsch: Method of colonisation of free surfaces by subaërial Alga (Cyanophyceae) in the tropics.-Mr. E. A. Newell Arber. Miss M. Benson, Miss W, Brenchley, Prof. F. W. Oliver. F.R.S., Dr. D. H. Scott, F.R.S., and Prof. F. E. Weiss: Fossil plants from the English Coal-measures.-Mr. W Saville-Kent: Stereoscopic and other natural-colour photographic transparencies illustrating the fauna of the Polynesian coral reefs. This series of natural-colour photographs was more particularly illustrative of the coralfrequenting fishes of Polynesia. A notable genus of mostly minute percoid fishes, Tetradachnum, represented in the series, habitually make isolated bushy coral stocks their headquarters. They cruise around these coral growths in sport and in search of food, retreating within the coral's ramifications to rest or to escape from any

enemy.

The Solar Physics Observatory, South Kensington: Recent photographs of some British stone circles.-Dr. W. M. Flinders Petrie, F.R.S.: (1) Hyksos fortress model. and pottery, 2000 B.C., Egypt. (2) Model of the temple and city of Onias, Egypt. (3) Photographs, enlarged, from Sinai. The Egyptian turquoise mines were worked from 5000 B.C. The oldest rock sculptures are those of the middle of the first dynasty of kings. Both centres of mining, Wady Maghara and Serabit el Khadem, were shown.

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