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Direct Vision Spectroscope Send for Section J of Catalogue for smaller Direct Vision Spectro- scopes, suitable for laboratory work. I Ins instrument lias a fine micrometer strew with divided drumhead and scale, enabling one to pass through the spectrum and to obtain wave length de- terminations with consider- able accuracy. The prism is of high dispersion, and easily resolves the sodium I > lines A pointer is also fitted into a positive eye- piece. It P... <-,.=;■ I Instrument - *9 10 Hiicts. | stand . .£2 2 DELIVERY FROM STOCK. o o ADAM HILGER, Ltd., 75a, CAMDEN ROAD, LONDON, N.W. Telegrams: "Sphericity, Camroau, London." Telephone: North 1687. fnl ll!lllll]llll||l!l|lllllll!lllilllllllllllllllli|||'llllll!lillilllllll[ OHMS Keep one of our Departments always busy. We manufacture them in the form of RHEOSTATS of all types, values, and carrying capacities, from the SMALLEST SLIDER to the LARGEST LOAD or CALIBRATION Set BRITISH MADE ONLY ISENTHAL & Co. (Department 2> Denzil Works, Neasden, London, N.W. Contractors to the Admiralty. War Office, India Office, Colonial Office, and the Postmaster General. m m Knowledge. With which is incorporated Hardwicke's Science Gossip, and the Illustrated Scientific News. A Monthly Record of Science. Conducted by Wilfred Mark Webb, F.L.S., and E. S. Grew, M.A. APRIL, 1915. CHAPTERS IN SPECTRUM ANALYSIS. By W. MARSHALL WATTS, D. Sc. I. — Law and Order in Spectra. A. Line Spectra. (Continued from page 69.) The absorption spectra of potassium, rubidium, and caesium show long series of regularly arranged pairs of lines similar to those seen in sodium. These three metals are very closely allied in their chemical and physical properties, and their spectra show a most remarkable agreement. In the diagram (see Figure 79) these three spectra are mapped upon a scale of oscillation-frequency — that of caesium at a "height" of 17638, that of rubidium at the "height" of 7301, and that of potassium at the "height " of 1 528, as shown by the scale on the left-hand edge of the diagram, these numbers being the squares of the atomic weights : 132-81 for caesium, 85-45 for rubidium, and 39-1 for potassium. The connecting -lines, marked m = 2>, m=\, m=5, and so on, show the exact correspondence of the spectra line for line. Further, the lines joining corresponding points in caesium and potassium pass almost exactly through the corresponding points in rubidium. The principal series in potassium is set forth' in the following table, with the wave-lengths calculated from the formulae n it iconc u 109675 O.F. = 35005-56 — nA,QCAxa '» + . 293076 -^?) m I for the less refrangible component, and 109675 O.F. = 35005-56 — m + -296228 - I^8)' »i 1 for the more refrangible component of the pairs of lines. Table 18. The Principal Series in Potassium. ill. Observed. Calculated. O— C. O. C. f 7699-23 7699-10 \ 7665-60 / + •13 2 I 7665 27 -•33 3 f 4047 38 4047-51 \ 4044-13 J -13 i. 4ii44 32 + •19 4 r 3447 53 3447-59 \ -06 I 3446 53 3446-56 i -03 _ f 3217 76 3217-83 \ 3217-36/ -07 o \ 3217 31 -05 6 / 3102 37 3102 -27 i 3102 00/ + 10 \ 3102 15 + •15 7 3034 94 / 3035 09 \ X 303500 / -10 8 2992 47 2992-43 + 03 9 2963 37 3-53 -•16 10 2942 8 2942-99 -19 11 292S 0 2927-86 + 14 12 2916 6 2916-38 + .22 13 2907 6 2907-45 + •15 14 2900 4 2900-38 + 02 15 2894 6 2894-67 -07 16 2889 7 2890-00 -•30 17 2885 9 288612 - -22 IS 28S2 9 2882 -87 + •03 19 288d 3 2880-12 + •18 20 2877 9 2877-77 + •13 21 2875 8 2875-75 + -05 22 2874 l 2873-99 + •11 23 2872 5 2872-46 + •04 24 2871 1 2871-12 -02 25 2870 0 2869-93 + 07 N 97 OS KNOWLEDGE. April, 1915. For rubidium the formulae OF. = 33688-20 - Kl«Mi75 (l.r. O.F. = 33688-20 - („+.; ,,•_,;,.„ _±Z3542y line) V m — \ 109675 •l)738()»\" ,: , (m-r- (m + . 365934- '""""'"I Hno \ wi — 1 / give equally p""l results, as shown in the following tabic: Table 19. The Principai Series in Rubidium. III. Observed. Calculated. O— C. 2 i 7949-04 7949-03 \ 7803-13 / + ■01 03-17 + •04 '1 I 4215-72 4215-72 1 4201-99 J 0 .> 1 1201 98 -•01 4 i 3591-74 3591-74 \ 0 I 3587-23 3587-22 J + •01 _ I 3350-99 V 3348-86 3350-94 \ 3348-93 J + •05 s -•07 6 I 3229-26 I 3228- IS 3229-27 \ 3228-10 J -•01 + •08 7 f 3158-47 I 3157-69 3158-39 \ 3157-67 / + ■08 + •02 8 3112-95 3112-95 0 9 3082 -39 3082-34 + •05 10 3060-62 3060-56 + •06 11 3044-33 3044-47 -•14 12 3032-20 3032 -25 - -05 13 3022-70 3022-74 - -04 14 3015-16 3015-20 -•04 15 3009-03 3009-11 -•08 16 3n()4-ll 3004-12 -■01 17 2999-96 2999-98 -•02 18 2996-51 2996-51 0 19 2993-52 2993-57 -•05 20 2991-12 2991-06 + •06 21 2988-94 2988-89 + ■05 22 2987-01 2987 -02 -•01 23 2985-45 2985 -38 + •07 24 2984 -US 2983-94 + •11 25 2982 -68 2982-67 + •01 26 2981-51 2981-53 -•02 27 2980-52 29S0-53 -•01 28 2979-62 2979-62 0 29 2978-81 2978-81 0 30 2978-10 2978-08 + •02 31 2977-39 2977-42 -•03 In caesium the formulae O.F. = 31404-6 109675 O.F. = 31404-6 - m + -418206- 109675 •09002 \a m — 1 ( m + . 449975 _l089294y \ m — 1 / give the following results : Table 20. Tin: Tkincipal Series in Caesium. III. Observed. Calculated. O— C. 2 I 8949-92 8949-92 \ 8527-72 J (I \ 8527-72 ii 3 1 4593-34 4593-34 \ 0 l 1555-44 4555-44 ) 0 4 / 3888-79 I 3876 -53 3888-75 \ + •04 3876-36 / + •17 5 ( 3617-56 3617-44 \ + 13 \ 3611-67 36 1 1 -62 i + •05 6 I 3480-28 l 3477-03 3480-19 \ 3477-13 / + •09 -10 7 f 3400-13 3400131 3398-14 / 0 I 3398-27 + •13 8 / 3348-84 3348-S 3 \ 3347-68/ -•09 I 3347-56 -•12 9 r 3314-16 3314-25 i -•09 l 3313-28 3313-33 / -•05 10 f 3289-25 3289-50 \ 3288-84 J -■25 I 3288-68 -•16 11 3270-56 3270-72 -•16 12 3256-77 3256-92 -•15 13 3246-02 3246-18 -•16 14 3237-58 3237-65 -•07 15 3230-69 3230-78 -•09 16 322511 3225-11 0 17 3220-34 3220 -43 -•09 18 3216-45 3216-48 -•03 19 3213-02 3213-11 -09 20 3210-18 3210-26 -•08 21 3207-78 3207-80 -•02 22 3205-64 3205-66 -•02 23 3203-80 3203-79 + •01 24 3202-13 3202-15 -•02 25 3200-71 3200-70 + •01 26 3199-45 3199-42 + ■03 27 3198-25 3198-26 -•01 28 3197-28 3197-23 + •05 29 3196-20 3196-31 -11 30 3195-42 3195-47 -•05 31 3194-59 3194-72 -13 32 3193-94 3194-04 -■10 The remarkable similarity between the spectra of the alkali metals was noticed by the early observers. In 1869 Lecoq de Boisbaudran remarks that the spectrum of caesium is, like that of potassium, shifted bodily towards the red. Figure 78 is a photographic reproduction of some of the beautiful drawings of spectra published by de Boisbaudran. The caesium and rubidium lines which he marks a, 6 are those of the principal series marked m=3 in Figure 79 (the diagram does not extend far enough to the right to allow of the red lines of the three elements to be shown, i.e., those for which m=2). That there exists some relationship between the atomic weights of allied elements and their spectra is certain. If we knew the precise law of this relationship, the measurement of the wave-lengths of the lines in the spectrum of a new or rare ele- ment, particularly of one difficult to obtain in a April. 1915. KNOWLEDGE. 99 I a. Spectrum of the blue flame of illuminating gas. b. Caesium chloride. Flame spectrum. .?-'.< ■/>'.' '-<■ i >•> j/t'i' tyo //tf /!,,• c. Rubidium chloride. Flame spectrum. (I. Potassium chloride. Flame spectrum. it>o ItO !-■'■ I '■■ Jj,y >■ Potas in::: ulphate (fused). Spark spectrum. ■ z. f. Sodium sulphate (fused). Spark spectrum. I I'.l Rl 100 KNOW I.I D April, i» ,:- b 1' 1 • r * ' : 1 ' 1 •w ,° H V - 11 < V . N I . ;■ 1 21 19 ft, '7 t -i — 1 j 16 N 0 10 «) X) to so tt 10 • e iff » m w no m « wo «o no x x .1 30 v x > M ,tc t B 111 NOTES. ASTRONOMY. I'.y A C. D. Crommelin, B.A., D.Sc, F.R.A.S. llll DISTRIBU1 CON OF ALGOL-STARS IN SPACE. 'I Inn- is .hi article mi tins subject in The Astropk} Journal, December, 1914, by II. N Russell and II. Shapley. The s] " gives the masses, ami tin- type <>i spectrum also gives the probable surface brilliancy. The absolute magnitude can be deduced with some confidence: this compared with the visual magnitude gives the distance u is estimated that the uncertainty is not more than twenty-five per rent.). The mean parallax of the ninety stars discussed is .,,',-/'. implying a distance of 300 parsecs, or 972 I..V. The mean of the distances, however, comes out as 24001 Y ["he method gives 125 L.Y. for Algol, 109 L.Y. for /j Aurigae. Din 1 1 measures of their parallaxes give 67 L.Y. and 95 L.Y. The agreement is tolerably good. \V UrsaeMajoris(164 L.Y.) and R Canis Majoris (180 L.Y.) also seem to lie within a measurable distance, but all the others are very remote. They show a considerable con- centration towards the galactic plane. Thus seventy-five of the ninety stars lie within 30° of this plane — on uniform distribution there would be only forty-five. The same result holds for the linear distances from the galactic plane. The average distance from this plane is about 450 L.Y. The distances have been calculated on the assumption that there is no absorption of light in space. Evidence is accumu- lating that the absorption is sensible but small. Using King's value of the absorption, the three greatest distances of stars from the Sun, which before were given as 17200 L.Y., 12400 L.Y., 7900 L.Y., are reduced to 4900, 4200, 3200 respectively. The average distance of all the stars dis- cussed from the galactic plane is now reduced to 280 L.Y. A similar investigation has been made for the Cepheid variables : this was partly done by Hertzsprung, and has been completed by Russell and Shapley. They prove to be on the average one and a half times the distance of the Algol variables. This is explained by their enormous intrinsic brightness, so that they can be seen at a much greater distance. Both classes of variables agree in in- dicating that our stellar system is comparatively shallow (perhaps not more than 1000 L.Y. in thickness) towards the galactic poles. The median plane of the stellar system appears to be somewhat to the south of the Sun, perhaps some 50 L.Y. distant from it. This is probably the reason of the greater richness of the southern hemisphere in bright stars. There are two other articles by H. Shapley in the same magazine. One deals with additional variables in the cluster Messier 3 (in Canes Venatici). S. Bailey had already found at least one hundred and ten variables in it, their periods being all under eighteen hours. He could not investigate the centre of the cluster, as the star images coalesced there. The great separating power of the sixty-inch mirror at Mount Wilson, when used as a Cassegrain, has now permitted the photographic scrutiny of the central region, and Mr. Shapley now announces at least twenty-three new variables within a minute of arc of the centre. The brightest maxi- mum of these new variables is magnitude 14-3, the faintest minimum is magnitude 17-4. In some cases the range of variation is half a magnitude ; in others nearly two mag- nitudes. Mr. Shapley also discusses Cepheid variables, showing what grave difficulties there are in the way of explaining these by any hypothetical arrangement of pairs of stars. The conclusion is that they are real pulsations in single stars of ellipsoidal figure, either periodic rushes of heated gases from the interior or periodic ebbs and flows of heat, causing th( type of the surface to fluctuate. Mr. II. Shapley also writes in No. 86 of The Contributions of Mount Wilson Observatory on the effei I of the darkening near the limb in Algol stars. It is well known that the disc of our Sun is much less luminous at the edges than in the centre. The effect is probably less in Sirian than in Solar stars, but it would still be sensible. In the Algol system neglect of this darkening makes the bright star the smaller, but taking it into account the diameters may be equal. The Supposed third star which causes a perturbation with period of 1-9 years is also discussed. Its light may amount to one-quarter of that of the whole system, but not more than this. MELLISH'S COMET— The orbit of this comet has been deduced by Messrs. Andersen and Fischer, of Copenhagen. Perihelion 1915, July, 25-109 Berlin M.T. Arc from Node to Perihelion ... 239 13 Ascending STode 75 28 Inclination 51 51 Log. perihelion distance 0-0747 Ephemeris for Berlin midnight — R.A. S. Dec. Log. r. Log A. Mag- h. m. s. o nitude. April 10 ... 18 14 8 3 7 0-2952 01635 8-1 ,, 26 ... 18 31 18 7 39 0-2555 0-0455 7-4 May 12 ... 18 47 50 16 39 0-2138 9-9013 6-4 ,, 28 ... 19 6 25 35 39 01715 9-7428 5-4 June 13 ... 19 49 13 68 53 01314 9-6604 4-9 ,, 29 ... 5 28 56 78 58 0 -0983 9-7365 5-0 July 15 ... 6 31 33 63 11 0-0782 9-8527 5-4 „ 31 ... 6 40 55 55 4 0-0763 9-9432 5-9 Aug. 16 ... 6 40 54 50 42 0-0930 O-0036 6-4 The comet will be visible in England till the middle of May, by which time it will probably be faintly visible to the naked eye. The brightness in June and July will prob- ably be greater than that given above, which takes no account of the physical brightening that usually takes place on approach to perihelion. It is hoped that our readers in the southern hemisphere will be able to obtain satis- factory observations. The recovery ot Metcalf's Periodic Comet, recently announced in " Knowledge," proved to be an error. The object observed was the asteroid Lampetia. BOTANY. By Professor F. Cavers, D.Sc, F.L.S. INDIVIDUALITY OF THE CHROMOSOMES IN PLANT NUCLEI. — A melancholy interest attaches to a recently published paper by Sharp (La Cellule, Volume XXIX), which represents one of the last pieces of biological research done in the University of Louvain before the destruction of that town by the Germans. It deals with the much discussed question of the individuality of the chromosomes of the nucleus, a subject which has during recent years received a large amount of study at the Louvain laboratory by Grdgoire and his pupils, who have maintained that the chromosomes retain their individuality throughout the nuclear divisions that occur in the life of the organism, and are not fused together permanently when the nucleus goes into the resting condition between its divisions. Sharp claims that in many cases, in the cells of the Broad Bean plant which he investigated, the chromo- somes can be identified even in the resting nucleus, and that some of the stages leading up to the splitting of the chromosomes have been misinterpreted by previous investi- gators, who have also overlooked important stages. Accord- ing to Sharp, the actual splitting takes place at a later 112 April, 1915. KNOWLEDGE. 113 stage than has been supposed ; and, if his observations are correct, they strongly support the theory of the individuality of the chromosome — a point of considerable importance in connection with questions of heredity, since it is generally agreed that hereditary qualities are carried by the chromo- somes, while various questions in inheritance depend upon the question whether the chromosomes do or do not retain their individuality. BIOLOGY OF FEGATELLA (CONOCEPHALUM).— It has been shown by several writers that Marchantia, Fegatella, and some other members of the Marchantia family of Liverworts are capable of growing in water or in saturated air and in extremely feeble light, and that under these conditions the thallus structure is greatly simplified. The characteristic air-chambers, containing green assimilating filaments, become reduced in extent and simplified in structure in the branches formed in such wet and dark conditions, and the chambers may be absent altogether, the whole thallus also becoming longer and narrower, though chlorophyll is still formed. Miss May- brook (Sew Phytologist, Volume XIII) has studied the modifications in the thallus of plants of Fegatella (Conoce- phalum) conica, a common Liverwort found chiefly beside streams and in other moist places. Her plants were collected from a small cavern in a hedge-bank, and she has worked out, in a very interesting manner, the relation between the structure of plants growing in different light intensities. She concludes from her observations that the absence of air-chambers from the plants found in the wettest and darkest positions is due to the combined effects of darkness and moisture, since in plants growing in decreased intensities of light there is a gradual decrease in the number of chambers per unit of thallus surface and in the size of these chambers. The internal structure of the thallus shows interesting deviations in structure ; for instance, diminished length of the curious beak-like cells which normally terminate the assimilating filaments. The final disappearance of the chambers is apparently dependent upon the moisture factor, for only in those plants showing marked adaptation to a moist habitat were the chambers totally undeveloped, CHEMISTRY. By C. Ainsworth Mitchell, B.A.(Oxon), F.I.C. FLUORINE IN MINERAL WATERS.— Recent in- vestigations of MM. Gautier and Clausmann (Bull. Soc. Chini. de France, 1914, No. 15) have shown that all mineral waters contain fluorine, the proportion being greatest in waters of volcanic origin. Thermal alkali bicarbonate waters are particularly rich in the element, although the proportion does not appear to depend upon the temperature. Speaking generally, mineral waters of the same kind show an increase of fluorine accompanying a rise in the total salts. In the case of calcium sulphate waters, whatever their origin, the amount of fluorine is about two milli- grammes, while sea water contains about three milli- grammes per litre, the proportion varying slightly in different places and at different depths. THE COLOUR OF METALS.— Various facts in support of the theory that all metals are naturally of the colour ol silver are given by Dr. L. Martiouchck in a Russian chemical journal, and his communication is abstracted in the Bulletin, Sociiti Chimique (1914, Volume XVI, page 751). The yellow tint of certain metals, su< b ai i alcium, has been found to be due to the presence of traces "I impurities, the pure metal being silvery white. Heine has also shown that when copper is spcciallv purified it becomes oi a paler tint, the red colour being apparently the result oi oxidation caused by the presence of lead oxide. Moreover, the metals potassium, sodium, and rubidium are of a yellow colour when obtained by reducing their chlorides with calcium in the presence of air. In this case the yellow tint is due to the nitrogen, and not to the oxygen, in the air. POTASH FROM HEDGE CLIPPINGS— Mr. E. J. Russell calls attention in the Journal, Board of Agriculture (1914, Volume XXI, page 694) to the high proportion of potash contained in the ash of bonfires of hedge clippings, weeds, and the like. Samples contained about eleven per cent, of potash (ICO), or nearly as much as kainite. which contains about 12-5 per cent. Hence the ash obtained in normal processes of the form would be worth about forty shillings per ton in normal times, and much more under the present conditions. It is pointed out, however, that precautions must be taken to protect the ash from the rain. since the potassium salts in the ash are readily soluble in water. For example, the potash in a heap of ash was reduced by fifty per cent, after a single night of moderate rain. It is calculated that the hedges from a twenty-acre field would yield an amount of ash equivalent to nearly two hundredweight of kainite, and that the labour of obtaining and burning the clippings would amount to threepence to eightpence per pound of ash. Hence the potash in this form would be expensive if the whole of the operations were specially done for the purpose ; but where the trimming and so on have to be done in any case, the value of the ash would repay the cost of collecting the clippings. AN OXIDISABLE VARIETY OF NITROGEN.— It has been found by Mr. T. M. Lowry(PM. Mag., 1914, XXVIII. 412) that air that has been subjected first to a silent and then to a sparking electric discharge shows the spectrum of nitrogen peroxide, apparentlv formed by the oxidation of a variety of nitrogen produced under the influence of the discharge. After a few seconds this oxidisable kind of nitrogen reverts to a form which can no longer be oxidised either by oxygen or by ozone, and it is suggested that this momentary production of modified nitrogen may play an important part in the technical processes of fixing atmo- spheric nitrogen. The chemically active form of nitrogen discovered by Mr. Strutt, and described at the time in " Knowledge," cannot be oxidised by ozone under the conditions described. GEOGRAPHY. By A. Scott, M.A., B.Sc. LLASSIFICATION OF SE1 UMENTS.— Although the chief characteristics of the various types of sediments are fairly well known, a paper by A. C. Trowbridge (Jour. Geol., May-June, 1914), in which these characteristics are presented in a tabular form, should prove very useful in the examination of the varii ius dep sits now being laid down on the Earth's surface. Sediments arc divided into aeolian, fluvial, pluvial, talus, glacial (including till and lluvio- glacial), lacustrine, and marine deposits including shallow and deep water). Instead of a division into littoral and non- littoral, lacustrine deposits are divided into those of agitated waters, and those of quiet waters. Similarly, shallow-water marine deposits are classified into those >>t major agitation and those of minor agitation, the former resembling the near-shore lacustrine ami the latter the still-water lacustrine, save in the nature of the tossils Emphasis in- laid on the " lens and pocket structure " of fluvial di and on the intermediate nature of Quvio glacial sediments, which are similar texturally to the fluvial, and lithologically to the glacial. STREAM PIRACY -Three interesting case-, showing oi development oi the " int type .•I rivei capture, are described in the Publications of the University oi Virginia N i 20, July. 19141 The first case occurs m a rejuvenated river system, where the main stream is entrenching itself, and at the same time approaching, by lateral Cutting, a tributary, the junction with which is at presenl "in- and .< quartei miles lower down. In the second e.i";e, both the main and tributary streams are Ill KNOWLEDGE. April, 1915. meandering, and two meandei are laterally cutting towards each other, thej have not yet joined on the surface, the intervening rock, which is limestone, has been undercut b .in i mi ut ili.it .1 tunnel has been formed from t ho mi. mi to the other. In the third case, the junction oi two stn n moved one and three-quarter miles upstream 1>\ intercision, due to the cutting through "( .1 ridge of chert winch formerly eparated two meanders. SHAl'l I'l Mil \M\KtTIi i oXTINENT.— Prob- ably the most discussed point in Antarctic physiography has been the que tion as to whether there is one continent or two; that is, whethei there is a continuous range from Graham land to South \ ictoria Land, or whether, as sug- I by Mawson, Graham Land is united to King Edward \ II I and, and separated by a faulted trough or rift valley \ ii toria Land. The evidence has been discussed by i .i lllith . Taylor (Gcog. Join .. ( fctobei , November, December, 1914), who reviews both the geological and physiographic data. The rocks of Prince Leopold Land arc like those of South Victoria Land. Further, a comparison with the Australian coastal type points to the conclusion that the West Antarctic cordillera continues to King Edward VII I ind, with an intermediate broad belt of lowland — the ner— corresponding to the Tasman Sea between Australia and New Zealand. Another point in favour of tins idea is that the Victoria Land mountains belong to the " Atlantic. " or " subsidence " type, whereas Graham Land belongs to the " Pacific " type, which may be continued from the Andes by the South Georgian loop. The Royal Society Range is probably caused by a late Tertiary- fault, while the foothills seem to be a typical " Scnkungsfeld " area. ANTARCTIC GLACIER TYPES.— In the same paper an elaborate account is given oi the ice-fields of the Antarctic continent. Several types of glacier occur in close juxta- position. Of those with large alimentation the great ice- i i p. which is between two thousand and three thousand ei I thick, has been shown to have but little movement. There are several piedmonts, the largest being the Wilson and Putter Point glaciers, which are probably residual from a former glaciation. There are also the large outlet glaciers and numerous small col and dendritic or tributary ones. All the forms of glacial action are well shown by one or other of these types. Thus, the action of the ice-cap and of the piedmont lobes is mainly protective. Glacial erosion, as commonly understood, is evidenced by the outlet glaciers, while " sapping " action, or cirque erosion, generally occurs on the steep slopes of the Royal Society range. An account is also given of the various stages of cirque formation and of glacial deposition. One interesting deduction is that the present conditions in South Antarctica are very unfavourable for glacier erosion, as well as for cirque erosion, which requires rapid alternations of freezing and thawing. THE GULF STREAM. — In the same journal, Commander Hepworth discusses the origin and course of the Gulf Stream. Most ocean currents have a close connection with atmo- spheric currents, though the Earth's rotation is also a power- ful factor. The north-east and south-east trade winds give rise to a drift current, which develops into the north and south equatorial currents. The Gulf Stream is primarily due to components of those which find their way into the Caribbean Sea; thence past Yucatan into the Gulf of Mexico, and finally through the Gulf of Florida. The other hypotheses as to its origin, based on temperature differences, on the silt brought by the Mississippi, and so on, are shown (o be untenable. One interesting fact is the daily and monthly variation in the velocity, which has been correlated with the variation in the heights of the tides. While it has been maintained that the Gulf Stream disappears when it comes into contact with the Labrador current, it is more probable that it can be traced as far north-cast as Spitz- bergen and the Barents Sea. This is borne out by the evidence of the plankton and also by the occurrence, in these regions, oi warm water oi high salinity, such as is typically found in the Cull Stream. The results of a series of investigations of the relations between sea temperature and air temperature, extending over the last ten years, indicate that no important temperature changes have occurred in the North Atlantic within historical times. GEOLOGY. By G. W. Tyrrlll, A.R.C.Sc, F.G.S. THE ORIGIN OF THE BRIGHT AND DULL LAMINAE OF COAL.— In the December number of The Journal of Geology Mr. T. E. Savage discusses the origin of the bright and dull laminae which make up the mass of an ordinary coal, with especial reference to the coals of Illinois. Any theory of origin has to explain the extreme regularity and wide horizontal extent of these laminae (over several hundred square miles in Illinois) ; the alter- nation of the bright and dull layers ; the predominance of mineral charcoal and of plant spores in the dull laminae ; and the numerous pinnae and pinnules of ferns in the midst of mineral charcoal fragments. Mr. Savage's views on the accumulation of coal-beds may be summarised as follows : (1) The vegetable accumulation began in very shallow swamps. (2) That, as the swamps deepened gradually, the accumulation kept pace with the increasing depth. (3) In oft-recurring cycles of drought, successive levels of the vegetable mass were exposed to the air, and were so modified by partial atmospheric decay as to result in the formation of the dull laminae with their mineral charcoal. The bright laminae would thus be formed by decomposition out of contact with air. Quoting Mr. Savage in the above- mentioned paper : " The dull laminae and mineral charcoal partings of the coal-beds are the records of repeated inter- ruptions of accumulation, during which the surface of the vegetable material in the swamp was above water and exposed to atmospheric decay, resulting in the destruction of the softer parts of the plant tissues, leaving them in an indurated and more or less skeletonised and fibrous con- dition. On resubmergence these residual portions of the vegetable materials were not so readily impregnated with the fundamental matter of the bog as were those parts of the mass that had not suffered partial atmospheric decay, and hence are of dull appearance. Such periods of arrested accumulation of the plant material, due to the exposure of the surface of the vegetable matter of the bog, would be favourable for the accumulation on such a surface of a relatively larger proportion of spores than would be mingled with the vegetable mass during periods of submergence and of normal vegetable growth in the bog, and the resistant nature of the spore cases would permit their better pre- servation than the ordinary plant tissues during such times of exposure. These conditions would explain the greater abundance of spores in the dull than in the bright laminae of the coal-beds. The variation in thickness of the dull laminae would be due to the unevenness of the surface of the exposed vegetable matter in the bog." These con- ditions also explain the alternation of the bright and dull layers, and their wide extent, since they were coterminous with the boundaries of the swamp itself. METEOROLOGY. By William Marriott, F.R.Met.Soc. THE WEATHER OF APRIL— Although April is the mid-spring month, when some warm and genial weather may reasonably be expected, yet there is perhaps no other month in which we are exposed to such great and sudden changes of temperature. The increasing power of the sun's rays and drying north-easterly winds cause excessive evaporation. Some days may be warm and genial, while. April, 1915. KNOWLEDGE. 115 on the other hand, days of wintry rigour are experienced, with heavy showers of hail or snow. Hence the old saying " Changeable as an April day." April was a very cold month in the years 1860, 1S79, 1SS1, 1884, 1SSS, and 1908 ; and it was' very mild in the years 1844, 1865, 1869, 1874, 1893, and 1894. The average mean temperature at Greenwich for April is 47°-3 ; in 1865 it was as high as 52:-9; while in 1860 it was as low as 43-3. The average maximum temperature is 57-2; the highest mean was 66"-3, in 1865, and the lowest 51°-7, in 1908. The average minimum temperature is 39° -0 ; the highest mean was 42-5, in 1850, and the lowest 34°-2, in 1852. The absolute highest temperature recorded was 81°-5, in 1865, on the 27th, and the absolute lowest 23° -0, in 1847, on the 17th. The average number of da}"s on which the temperature falls to or below the freezing- point is three. The average rainfall for the month of April is 1 -61 -in. .' the greatest amount was 4-35-in., in 1829, and the leasl 006-in. in 1817. The heaviest fall in one day was 1 50-in.. in 1910, on the 16th. The average number of " rain days " [i.e., on which 01-in. fell) is 12-0 ; the greatest number of days was twenty-one. in 1848, and the least two, in 1852. The average amount of bright sunshine at the Kew Observatory, Richmond, is one hundred and fifty-two hours, or about five hours per day. The average barometric pressure in London for April is 29-933-in. ; the highest mean was 30-308-in., in 1817, and the lowest mean was 29-590-in., in 1829. " April showers bring forth May flowers." THE RAINFALL OF 19 T4— Dr. 11 R. Mill, the Director of the British Rainfall Organisation, in his account of the principal features in last year's rainfall, says that the note- worthy features of the monthly rainfall were the prevailing wetness of the four months February, March, November, and December. Of these February was wettest in Ireland, and December in Great Britain. The rainfall of December was exceptional in all parts of the Kingdom, but especially so in the South of England, where it was probably unpre- cedented in this respect. Of the remaining months, January was everywhere dry. and, following an unusually dry De- cember, gave a character to the midwinter season of 1913- 14 greatly in contrast with that exhibited in the same period of 1914-15. From April to October the rainfall was in general well below the average, though local thunderstorms in England brought the general fall of July slightly above the average, whilst that of August was above the average in Ireland for a similar reason. The persistent dryness of the seven months, and in particular the small rainfall of ( ►ctober, which was the driest month of the year, was probably as abnormal as was the great rainfall ol December. Taking the British Isles as a whole, it appears that the rainfall for the year was six per cent, above the average, and so 1914 must be classed as a moderately wet year. AUSTRALIAN WEATHER, 1911 —The following are the results of some of the observations t"i the year 1911 at several of the principal towns in Australia as given in The Monthly Weather Report recently issued by the Common- wealth Bureau of Meteorology : — Mean Sunshine Temperature Rainfall Evaporation. Hours. in. in. Perth 63-2 ... 23-38 ... 66-34 ... 2961 Alice Springs 70-0 ... 7 09 ... 97 10 ... — Adelaide 62-9 ... 15-99 ... 48-14 ... 2415 Brisbane 69-3 ... 35-20 ... 4l>34 ... 2510 Sydney 63-4 ... 50-24 ... 37-45 ... 1996 Melbourne 58-6 ... 36-61 ... 38-87 ... 1755 Hobart 54-6 ... 26-78 ... 31-98 ... 195(1 MICROSCOPY. By J. E. Barnard, F.R.M.S. LIGHT-FILTERS.— The wave-length of the light used for illuminating purposes has a very definite influence on the resulting microscopic image. A filter may be selected for one of three reasons : to improve the correction of the optical system — and this applies to both the substage condenser and the objective — to increase or decrease con- trast in the image, or to increase resolving power. It is possible to combine, at least in part, all three qualities n one filter, although it is obvious that to obtain the best result each factor must be dealt with independently. In these days, objectives are so well corrected that the visual image is almost free from any very definite colour aberration but under certain exacting conditions it may become evi- dent. A filter which will cut out the particular colours for which the objective is not corrected can easily be made. It may be assumed that objectives are corrected for that part of the spectrum which has the highest visual luminosity, the region of the green, yellow, and blue-green. It follows that if the colours at the extreme ends of the spectrum are eliminated — the red and violet, for instance — the resulting image will be free from any outstanding colour. There is no better filter for this purpose than that known as Gifford's F-line screen. It is made by dissolving malachite or methyl-green in hot glycerine, the strength of solution depending on the thickness of screen used. In addition, a thin piece of signal-green glass must be immersed in the cell, to cut out the outstanding red which otherwise passes. Alternatively, the cell may be made up with one of its sides of signal-green glass, that is, if the cell is of the type which can be taken apart for cleaning purposes. The only objections to the Gilford screen are that the dyes mentioned are not very stable in solution, and that the luminosity of the screen is not high, as its maximum transmission is in the blue-green. A screen that is quite permanent, and that has higher luminosity, is Zetnow's filter. This is perhaps the most useful of any, either for visual or photo- micrographs purposes. It allows light of wave-lengths between five hundred and seventy and five hundred and fifty micro-millimetres to pass. It is made by dissolving ten grammes of pure dry cupric nitrate and cue gramme of chromic acid in fifty cubic centimetres of distilled water. The thickness of liquid should be one centimetre. If it is not convenient to have so thick a cell, the solutions may. of course, be more concentrated, the relative quantities of each substance being maintained. Another method is to keep read}' saturated solutions of copper sulphate and bichromate of potash, and to mix them as required A precipitate is thrown down, which dissolves in glacial acetic acid. The screen may thus be varied from yellow- green to blue-green to suit the objects under examination. The influence of a suitable screen on resolution is well known, although it is perhaps not so thoroughly realised in practice as it might be. Resolution is dependent on the wave-length of the light used in the medium between the object and the front lens of the objective, and on numerical aperture. The latter factor is a constant, that is. assuming that the full aperture of the objective is utilised The former is a variable, and. in the ca>r • •! white light. i> the mean wave-length of the light emitted by the radiant. Reduction of the mean wave-length therefore, by cutting out the red. for instance, increases possible resolution. By using a screen which effectively cuts out the red and yellow, improvement may be effected The method i- tairlv obvious, but further reference to the matter will be made in this column in succeeding numb THE QUEKETT MICROSCOPICAL CLUB.— The five hundred and fifth ordinary, which was also the forty-ninth annual, meeting of the Quekett Microscopical Club was held on Tuesday, February 23rd. at 20, Hanover Square, W., the President, Professor Arthur Dendy. D.Sc, F. R.S., 116 KNOWLKDGK. April. 1915. invited Prt Minchin to occupy the chair, and gave in- annual address. The title wai "The Biological ption "i Individuality. " Professor Dendy observed that probably most ol us think that we can recognise and define an individual, but that, though this is true >>t an individual man or dog, or an individual oak tree 01 cabbage, ii we cans- our investigations below the mii (ace, we find many cases thai are not a little puzzling, and the purpose ol the address "as to enquire whether it i- really possible to frame a definition oi individuality, from a biological point of view, that will be of general applicability throughout the animal and vegetable king- doms. There appeared to be two main paths by which the problem could be approached : the morphological and the physiological, On the one hand, it was possible to enquire what eonsitntes a perfect individual from the point ol view of structure; and. on the other, as to what constitutes ,tn individual as regards function. In the case of the higher animals the question might also be approached in a third way, namely, from the psychological standpoint. The -I i in ture of various unicellular and colonial organisms, and of many of a higher development, was discussed, and diffi- ( nines which arise in deciding their claim to individuality commented upon. Two examples from the higher class may be given. Taking a colonial organism — say an obelia or sertularia — the fertilised egg develops into a single individual, but that individual does not stop developing when it has attained its full growth : it branches out and produces other individuals by a process of budding, and in the colony thus formed it is impossible to say where one individual ends and another begins, though it may be quite possible to say how many individuals there are altogether by simply counting heads. Perhaps the most interesting case was one which well sums up difficulties occurring, especially from the physiological point of view. It may be given in Professor Dendy 's own words : " Many of the higher animals, though they do not form colonies in the morphological sense, have the habit of living together in social communities, which we may regard as colonies of completely separated individuals. The Honey Bee is a familiar example. In a hive of Bees we find individuals of three kinds, easily distinguished from one another both by habits and by structural peculiarities. The Queen is a per- fect female, and is alone capable of laying eggs. The ordinary workers are imperfect females, which have sacri- ficed the power of reproduction, and concentrated their energies upon the collection of food and other important services necessary for the welfare of the community as a whole. The Drones are males : they do no ordinary work ; their sole function is to fertilise the Queen. None of these different kinds of individuals could live a really independent life : they are all mutually dependent upon one another. The morphologist, however, could not refuse to regard them as separate individuals, and probably the physiologist would agree with him. But, if we are to be strictly logical, from the physiological point of view the complete individual can be nothing less than the entire community." . . . " It appears, then, to be hopeless to seek for any biological definition of individuality that can be applied to more than a very limited number of cases : we have constantly to modify our ideas on the subject as we . pass from one group of organisms to another, and every- thing depends upon the point of view." ..." Individu- ality, though a very real, is a very elusive, phenomenon, and one which perhaps lies outside the legitimate domain of the biologist. We can do little more than collect the remarkable facts that confront us so frequently in the course of our investigations, and hand them over to the philosophers to deal with as best they can." PHOTOGRAPHY. By Edgar Senior. PAPIER MINERAL.— One of the most useful of photo- graphic materials is a form of tissue paper, known as " papier mineral," readily obtainable at most photographii dealers. A sheet attached to the glass side ol a negative affords great facilities for alterations and improvements m negatives generally, as it may be worked upon in various ways to modify the effect produced in printing. In land- i ape work, the appearance of distance may be made more real by its means ; and it is also one oi the greatest aids 1 < • successful vignetting. The opening in the vignetting mask, if covered with a pine- oi "papier mineral," will enable a much softer and a more easily controlled vignette to be obtained, and at the same time allow also advantage to be taken of direct sunlight in printing, should it be necessary ; and in a variety of ways it will assist the photographer to improve his work. In almost all cases where ground glass is useful this semi-transparent paper can be made to take its place ; thus a piece stretched over plain glass can be used as a focusing screen, should the latter get broken when travelling. Then, again, in portraiture " papier mineral " is useful for covering light movable screens or pasting direct on to a skylight, and sunlight may be filtered through it, and effects produced, which are in every way satisfactory ; and on dull clays it does not obstruct the light sufficiently to appreciably lengthen the time of exposure. When using " papier mineral " as a means of obtaining the effect of atmosphere in the print from a landscape negative by- causing the more distant objects to appear more or less grey — " the greater the distance the greyer the objects should appear " — it must not be forgotten that the lights of distant objects are grey compared with those in the foreground, and care must be taken that these distant lights do not appear too strong in the print. To obviate this, resort is sometimes made to strengthening those in the foreground and middle distance, but this requires to be done very care- fully. Thus, by means of tissue paper, it is possible to produce in the photographic print an effect more nearly in accord with nature than the negative alone would be able to render, owing to its imperfect gradations. If the photographic process gave a true rendering of all objects depicted, then resort to any such means would not be neces- sary ; but as it usually falls short of doing so, any means may be considered legitimate that will enable the desired end to be obtained, and produce the effect that a perfect process would do. In all cases, however, care must be taken not to overdo it. DEVELOPMENT WITH EIKONOGEN.— The develop- ing properties of this substance were first pointed out in 1881 by Professor R. Meldola, who prepared the acid from which the sodium salt was afterwards obtained, and introduced under the name of "eikonogen," a name derived from the Greek, and signifying "image-producer." In its pure state eikonogen is a white substance. It is the sodium salt of amido-^-naphtholsulphonic acid, its constitution being expressed graphically as follows : — CH CNH„ HC <^\ C /\ COH NaS'O.C CH ^CH CH or doH.OHNHjSOsNa.SHX) The substance is somewhat sparingly soluble in water, but dissolves more readily in the presence of alkalies Sodium sulphite is the best preservative, and acids added to the solution cause the free acid to be precipitated in the form of white needles. It can be recrystallised from solution in sodium sulphite. Eikonogen as a developer was patented in 1889 by Dr. Andresen, of Berlin. It is very quick in its action, and produces soft negatives of a very fine colour, and on this account it is invaluable in portraiture. It is also specially suited for instantaneous work, and it has been claimed that it will give more detail April, 1915. KNOWLEDGE. 117 with a short exposure than many of the alkaline developers. This, however, appears doubtful, as it is believed that the detail brought out is similar, whatever be the developer employed. The advantage of eikonogen is that it prevents that excessive contrast that is likely to be obtained at times with "pyro" and still further with hydroquinone ; and the great difficulty often experienced by those who have been used to either pyro- or hydroquinone as a developer has been that of not getting sufficient density in the image with eikonogen. But the entire absence of fog allows of the image being afterwards intensified to the required extent without difficulty. Then eikonogen may be mixed with either " pyro " or hydroquinone, or may be used after these at any stage of development, so long as the alkali employed as the accelerator is a carbonate. Thus, suppose that, with pyro as the developer, there is the appearance that the high lights are becoming too dense before the details in the less illuminated portions of the subject are well out; then these may be developed without any further perceptible increase of density by washing off the "pyro" solution, and applying one of eikonogen and carbonate of soda, the quantities being regulated according to the stage that the negative has reached. It should also be mentioned that the solution of eikonogen should be kept as near as possible at a temperature of 65° F., as it is very insoluble in cold water, and will crystallise out, and therefore lose nearly all its developing power. With this developer the quantity of sulphite required appears to vary with the nature of the subject and the plate used ; it must, however, be at least equal to that of the eikonogen, and may often with advantage be increased to twice, or even three times, that. Except for very quick exposures, a small quantity of bromide- should be used in the developer, as it appears to have the effect of producing greater density in the negative. As, however, restrainers act much more powerfully than with pyro, only three or four drops of a ten-per-cent solution should be added to each ounce of developer ; and the bro- mide must be potassium, and not ammonium. Develop- ment with eikonogen may also be conducted tentatively by adding the alkali in small quantities at a time. A saturated solution of potassium carbonate should be made, which may be added in drops as development proceeds. The developer may also be allowed to remain stationary upon the plate without markings of any kind appearing, provided that the solution is quite free from any deposit ; and, if required, further development can be instantly checked by immersion of the plate in a one-per-cent. solution of either acetic or citric acid. Over-exposure can, to an extent, be corrected by increasing the quantity of sulphite in the developer, although eikonogen cannot be said to allow of much latitude in this direction. Oi the many formulae that have been given from time to time the following will be found useful for portrail oi" landscape work generally : — Portraits and I. ami'-' mi rains Eikonogen... ... ... ... ,5 Soda sulphite 22 Soda carbonate ... ... ... 16-5 Water (distilled) ... ... 1 ounce For very quick exposures the following formula is to be recommended : — For Very Short Exposures. Eikonogen 14 grains Soda sulphite ... ... ... 75 Potassium carbonate ... ... 30 Water (distilled) ... ... ... 1 ounce Then, again, eikonogen is especially suitable for use with isochromatic plates, and, when mixed with hydroquinone, yields results on these plates that arc excellent in ever] way. The following formulae, which were originally published by Carbutt, are for a developer of this nature which the writer has used repeatedly with great success : — Carbutt's Formula. For Snapshots on Isochromatic Plates. Eikonogen... ... ... ... 2 grains Hydroquinone ... ... ... 1 grain Soda sulphite ... ... ... 12 grains Potassium carbonate ... ... 6 ,, Water (distilled) ... ... 1 ounce For Portraits on Isochromatic Platks. Eikonogen... ... ... ... 1-6 grains Hydroquinone ... ... ... 0-8 grain Soda sulphite ... ... ... 10 grains Potassium carbonate ... ... 5 Water (distilled) ... ... 1 ounce For Landscapes ox Isochromatic Plates. Eikonogen... ... ... ... 1-9 grains Hydroquinone ... ... ... 0-95 grain Soda sulphite ... ... ... 11 grains Potassium carbonate ... ... 3-6 Water (distilled) ... ... ... 1 ounce Care should be taken not to over-expose the plates, when these mixed developers will be found to do everv- thing required, if the development is carried far enough. Sufficient has now been said as to the value of eikonogen alone, as well as when mixed with hydroquinone ; and, as the substance can be obtained at a cost less than that of pyro at the present time in many cases, it is worth while giving it a trial. PHYSICS. By J. H. Vincent, M.A., D.Sc, A.R.C.Sc. THE COOLIDGE AT-RAY TUBE.— This tube diners very much from the usual form of .t-ray bulb, both in con- struction and in the principles underlying its operation. It is manufactured by the British Thomson-Houston Company, which has communicated a detailed account of Dr. Coolidge's invention to The Electrician (Januarv 15th, 1915). The usual concave cathode is replaced in the new tube by a spiral of thin tungsten wire, which is heated to incandescence by a small battery. This wire gives out the necessarv stream oi corpuscles, which, when they strike the anti-cathode, givi- rise to the i-ravs. Tin- anti-cathode also serves as the anode, and is made of wrought tungsten. When the tungsten wile is cold the tube is capable of with- standing an electrical pressure oi one hundred thousand volts without the insulation of the vacuum breaking down, so perfect is the exhaustion. When, however, the wire is hot, the tube becomes conducting in one direction, namely, through the space from the tungsten plate to the spiral, the current being carried entirely by the stream of corpuscles issuing from the hot wire. It is claimed for the new tube that its action is more easily controlled than that of the old tube, anil in particular that the conditions ,,f working are more readily reprodu VICKY SHORT-WAVED ULTRA-VIOLET LIGHT.— The wave-length oi the light in the middle of the visible i 'i ■> brum is about six thousand tenth metres, a tenth metre being 10 -,° metres. Stokes fust studied the ultra-violet region Ol the spectrum, and carried his work as far as length 1800 oi so The region lying between 4000 and 2000 may be called the ordinary ultra-violet region Tins radiation is remarkable for us photographic and fluorescent effects. Schumann many years ago earned the knowledge ol the ultra-violet up to the estimated wave- length 1000 The whole work had to be executed in a rOSCOpe which could be evacuated, as air is opaque to these shorl wavi Special photographic plates had to be used, and the prisms and lenses construct) fluorite. By the use oi a concave grating in a vacuum, Lyman has recently pushed the limit ol the spectrum up to nine hundred tenth metres, and has hopes oi still further invading the unexplored region lying between the shortest known ultra-violet waves and the longest waves oi the X-rayS. These have a wave-length ot the order of one tenth metre, while shorter still are the y-waves given out by radio-active bodies. 118 KNOWLEDGE April. 1915. A M \\ Ml I HOD OF COUNTING TI1K MOLECULES OF A GAS In ihe Astrophysicai Journal for December. h»l4, Fowle describes a new method i>>i determining the number of molecules v0 in a cubic centimetre of a gas at norma] temperature and pressure. The method consists in determining the transmissibility oi light of various wave- lengths through the dry air vertically above Mount Wilson, and computing the results by a formula due to Rayleigh, This formula gives the coefficient of transmission in terms of the refraction and oi the number of the particles in unit volume Rayleigh was the first to regard the molecules of .in .!•- capable ol acting as scattering particles, and considers that, while as seen from the Earth's surface, much of the light from the sky is tine to comparatively gross suspended matter, yet an appreciable proportion is attributable to the ulesol the air themselves, and that at high elevations where the blue is purer the latter part may become pre- dominant Fowle's result is w„ = (2-70± -02) x 1019, which is in close ai < ord with the best determinations of this con- stant by other methods. FRICTIONAL ELECTRICITY.— Very little is known about electrification by friction, so that a paper on this subject by Morris Jones is very welcome (Phil. Mag., February, 1915). Measurements were made of the charge produced on a surface by friction and of the frictional work spent in generating it. The specimens were insulated, and pressed against a rotating wheel covered with various materials. The charge generated was measured by a quadrant electrometer, and the work done could also be determined. It was found necessary to give the insulators a rest alter each rub, lor, if an insulator was rubbed a number of times in succession, the deflexions rose to the maximum, though the work done was the same for each rub, and less than that required to give the maximum for a first rub. When the normal pressure between the specimen and the rubber was maintained constant, it was found that for each pair of materials the charge reached a maximum as the quan- tity of work was increased. The sign of the charge was plus on quartz, glass, fluor-spar, Iceland spar, and heavy spar when rubbed on flannel, silk, and chamois leather, but negative on ebonite, amber, and sealing-wax when rubbed on the same materials. When specimens of various metals were rubbed against silk, the results were more complicated, the charge varying both in magnitude and sign with the state of the surface ; the maximum charge proved to be independent of the pressure and velocity. A tentative mathematical theory of the effects is given based on the assumption that the friction removes electrons from either the rubber or the specimen at a speed proportional to the rate of working. QUARTZ GLASS. — This material is surpassed only by invar in respect to its invariability of size with temperature. It was discovered by Professor C. V. Boys, who used threads of this material to support the deflected masses in his classical research on the Newtonian constant of gravitation. Boys showed how to prepare these threads by the bow and arrow and other methods, and also prepared small pieces of rods and tubes before the oxy-hydrogen blowpipe. When once quartz has been fused it is very easy to work, as it does not crack with sudden change of temperature. This is partly owing to its low coefficient of expansion, but also probably to its great mechanical strength. Shenstone still further unproved the methods of making fused silica, and the material is now a commercial article, being obtain- able in two grades : one perfectly clear and colourless, the other being silky and translucent in appearance. The methods of manufacture have been so far perfected that complicated apparatus of quartz glass can now be easily made, and a preliminary difficulty as regards sealing the leading in wires for electrical purposes has been overcome completely. This wonderful and beautiful product has already been applied to some commercial purposes, such as for making electric lamps, and the extension of its uses to various other fields is certain. RADIO-ACTIVITY. By Alexander Elf.ck, B.Sc. ANNUAL REPORT— The report issued annually by tin Chemical Society always devotes a section to the progress made in radio-activity during the past year. Most of the questions raised in the section of the report which has ]ust been issued have been mentioned from time to time in these columns The three following subjects, dealt with more fully in the report are, however, of some importance, and may briefly be referred to now. NEW WORK ON THE DISINTEGRATION SERIES. — Fajans and Towara have announced, in the Natiowissen- schaflen (1914, page 685), that they have discovered a radio-active substance which they have not been able to separate from bismuth, and which gives a-rays. The activity of the bismuth which has thus been obtained is five times as active as an equal quantity of uranium ; and, deducing its period from the range of its a-rays, the period of average life of this " radium-H " is between one hundred thousand and one million years. THORIUM ACTIVE DEPOSIT.— It has been generally accepted that when a radio-active element underwent dual disintegration we had a homogeneous collection of atoms which had the faculty of choosing in which of two ways they could disintegrate. If the experiments of Wood (Proceedings Physical Society, Volume XXVI, page 248) are confirmed, a large modification either of our views on dual disintegration or on the evolution of the radio-elements through the Periodic Table will be required. The experiments in question dealt with the volatilisation of thorium active deposit, and seemed to show that the substance hitherto referred to as thorium-C is composed of two elements, one of which commences to volatilise about 200° C. below the other. ATOMIC- WEIGHT DETERMINATIONS OF RADIUM AND URANIUM. — Despite the most careful atomic-weight determinations, there is still a greater discrepancy between the values obtained for these elements than there should be if the three o - particles emitted between uranium-I and radium had the same atomic weight as helium derived from the atmosphere, namely, 3-99. The writer of the report — Professor Soddy — therefore suggests that it is an open question whether the law of the conservation of mass accurately holds in radio-active change. To the present writer it seems that a more probable explanation would be that radio-active helium is an " isotope " of atmospheric helium, but of a slightly higher atomic weight, just in the same way as Ashton's meta-neon had an atomic weight of 22 compared to that of 20 for atmospheric neon. ACQUIRED RADIO-ACTIVITY.— Sir W. Crookes has recently published a paper (Philosophical Transactions of the Royal Society, Volume CCXIV, page 433) describing the behaviour of diamonds when buried in a radiferous salt or exposed to radium emanation. As is to be expected, the gems, just like any other material similarly placed, are coated with the active deposit, and so possess the " acquired activity." The author, however, finds this difference, that the material producing the activity so obtained can easily be dissolved from glass ; while, when it is obtained on dia mond, it can withstand the most vigorous chemical agents. The activity is, so far as can be ascertained, constant over a period of years. In the paper referred to Sir W. Crookes does not attempt to explain the phenomena observed, although it would be easy to suggest a number of explanations capable of expert mental verification. April, 1915. KNOWLEDGE. 119 CONDENSATION OF THORIUM AND RADIUM EMANATIONS.— In The Philosophical Magazine for March the present writer also contributes a paper on the condensa- tion of these two emanations. The object of the research was to find out whether isotopes had or had not the same temperature of condensation. It was found that in a mixture of the two emanations at atmospheric pressure, thorium emanation appeared to be condensed before radium emanation ; while, if the experiment was made in a vacuum, the reverse was the case. From theoretical considerations it was shown that results of this nature are to be ex- pected, even if individual atoms of each emanation had identical condensation points. The difference in behaviour is in all probability due to the different periods of average life. Indirect evidence was obtained in one ex- periment that the two emanations behaved identically in respect to their condensation and volatilisation. By altering the external conditions the condensation point of either emanation can be varied between — 150° C. and - 185° C. RELATION BETWEEN X-RAY WAVE-LENGTHS AND ABSORPTION.— A paper on this subject, by Pro- fessor W. H. Bragg, appears in The Philosophical Magazine for March. It deals with the absorption of rays emitted by substances when these are bombarded with cathode or .r-rays. It is well known that secondary rays are of two types, and are characteristic of individual elements. The main conclusion reached is that it is probable that " the characteristic rays of a substance form a system which can only be excited as a whole." In the meantime this result has been proved to be correct for some six or so elements ; if, however, further work enables it to be stated in a generalised form applicable to all the elements, an important step will have been made in our knowledge, not only of the material, using the word in its widest sense, inside an atom, but also of how that material is held together. ZOOLOGY. By Professor J. Arthur Thomson, M.A., LL.D. RELATIVE LENGTHS OF OUR TOES.— Onera A. Merritt Hawkes finds that there are three types of feet, of which two are common. The first or great toe may project beyond all the others (L type). The second toe may pro- trude, not only beyond the third, fourth, and fifth, but also beyond the first (S type). This is much less common than L. The first and second toes are of the same length, and longer than the others (E type). This is very unusual. There is some limitation in regard to sex, the S type occur- ring more commonly in females than in males. As the S type is commonest in the foetus, it may be said that in this, as in some other features, woman is a more youth- ful type than man. In inheritance the L type is irregularly dominant over the S type of foot. PHEASANTS AND MUTATION.— Mr. C. William Beebe, the Curator of Birds to the New York Zoological Society, has been studying pheasants for some years, and his opinion on the factors of evolution is well worth having. He says that he began with some prejudice against the " mutation theory " (of brusque, discontinuous, or saltatory variations), but that the more he observed such species as the golden and Amherst pheasants (Chrysolophus piclus and amhersiiae), the colour relations in both sexes, and the results of hybridism, the more necessary some such phe- nomena as saltations appeared to be in these particular instances. The genus Phasianus seems to afford good illustrations of continuous variation, and the genus Euplocomus of saltatory variations. Both forms have been operative in nature. CROCODILE'S NEST.— Mr. \V. Schultze, of the Bio- logical Laboratory at Manila, describes the nest of a crocodile (Crocodilus paluslris) near Taytay, Palawan. A peculiar mound of grass on the shore of a lake attracted attention, and it was found to be a crocodile's nest. A space about eight metres long and five metres wide had been cleared of the coarse, wiry grass {Ischaemum) which grew there, and a mound had been made 2-5 metres in diameter at the base and 1-5 metres in height. The grass was mixed with sand, and was moist. About the centre of the mound there were thirty eggs in several layers. The egg is oblong ellipsoidal, with a very hard porous shell, a high porcelain lustre, and a strongly marked opaque white band around the middle (girth). It was found that the time of incubation in the Philippines is between seven- teen and eighteen weeks. HOW A STING -RAY PROTECTS ITS EYE.— It is well known that the eyes of fishes are lidless, and cannot be closed like those of most higher vertebrates. Sometimes, however, they are well protected from injury, and B. Sun- dara Raj gives a good example in Trygon kuhlii, one of the sting-rays. It lies buried in the sand with the eyes, the spiracles, and a portion of the formidable spined tail pro- jecting. If sand or other particles be dropped down, the upper margin of the spiracle nearest the eye forms a pro- jecting fold which serves both to protect the eye and to exclude foreign objects from the spiracle. SIZES OF RED BLOOD CORPUSCLES.— An interest- ing suggestion has been made by Dr. J. Burton Cleland that specialisation is attended with a reduction of the size of the red blood cells. Thus, among fishes, those of Ceratodus are 39 x 23 to 25/i, which is " cumbersome " ; those of Elasmobranchs vary from 18 x 12-5 to 23 x 13 -5m : those of Teleosteans range from 9x7 to 13-5 x 10-3m- In Therapion unicolor they are almost spherical, 6 to 8^- Similarly in birds the Emu has 15-5 to 16-5x8-5 to 9-S^i ; the Grebes, Penguins, Herons, Pelicans, and the like have approximately 1 4 x 8/i ; in Passerine birds (except Cor- vidae) there is a definite tendency to smaller cells, 10 to 12x5 to7M. STINGS OF JELL YFISHES— The stinging threads of the common jellyfish (Aurelia aurita) are not strong enough to pierce the ordinary human skin, but bathers on British coasts have sometimes painful experience of the virulence of the orange or the blue species of Cyanea. In other waters there are much more formidable jellyfishes. Thus Mr. S. F. Light, in describing Philippine medusae, notes of Chiropsaimus qiiadrigatus that the sting of the tentacles is very dangerous. Swelling and inflammation begin almost immediately, blisters form, the heart action is impaired, respiratory spasms and nervous twitchings of the muscles ensue, and there is intense general pain. The natives of Palawan reported that the sting may be fatal. Another dangerous form is Daciylometra quinquecirrha, which causes severe poisoning. The native remedy is sugar solution taken internally and applications of vinegar externally. NESTS OF FALSE SCORPIONS— A very fine piece of observational work has been done by Mr. II. Wallis Kew, who has for the first time described the whole process of nest- making in the little creatures known as false scorpions, or pseudoscorpions, which are moderately well represented in Britain. Nests are made by all individuals of both for moulting, for brood purposes, and sometimes for hibernation, The interior is lined with dense spun tissue, almost like silk paper, which takes days or even weeks to make. There may be an external covering of earthy or ible m.itt rials attached by silk. The silk is formed by glands in the cephalothorax, and is conveyed by dm the tips of the chelii erae, or first pair of appendages. The silk is drawn out in separate viscid threads, which may coalesce or remain separate. There are five or six from each chelicera, but these may form one. The spinning is asso- ciated with continuous forward and backward movements of the body, and with lateral movements of the cheliccrae. 120 KNOWLEDGE. April, 1915. HYBRID COCKATOOS— Dr. Ernest Warren, of the Natal Museum, describes a very interesting case oi hybridism. The male bird was the common Sulphur-crested Cockatoo itua galsrita), the female the so-called Slender-billed Ltoo {Licmetis nasiea). The hybrid seemed to be a thorough Mind. Out of ten characters it was nearer Cacatua in five, nearer Licmetis in one. and almost exactly intermediate in four. In even,' character examined, with the possible exception of the coloured and non-coloured lores, there is very obvious blending of the male and female tics. There was no evidence of Mcndelian inheritance. HABITS OF TESTACELLA.— The Testacellid Slugs widely from the other British Slugs: Limacidae and Aiionidae. They retain a small external shell, visible on the surface, near the posterior end, whereas in the others the shell is either a hidden vestige or quite absent. Again, while most British Slugs are omnivorous, the Testacellids are essentially carnivorous, and feed largely on Earthworms caught by night. Mr. Charles Oldham writes : " The Earthworm is seized by a sudden, rapid extrusion of the Slug's odontophore or lingual ribbon, a structure provided with close-set rows of long, slender, barbed teeth, which afford an excellent hold on the Worm's soft body, and the whole of this stupendous meal, in bulk perhaps three times that of the Slug, is gradually ingested." In its early struggles the Earthworm often dashes the Slug about, but the bull-dog grip is not relaxed. In hot, dry weather and in the cold of winter Testacella lies inactive in a cocoon- like cell made of earth and mucus. The elliptical eggs, about five millimetres in longer axis, are deposited under- ground. There are three British species. STRENGTH OF SPONGE-CURRENTS.— Ever since Robert Grant discovered the currents produced in water by living sponges the hidden activity of these often very vegetable-like animals has excited interest. The last con- tribution to the subject is Professor G. H. Parker's estimate of the strength and volume of the currents. In Stylotella the pressure is equal to a column of water 3-5-4 millimetres in height. In seven others it was less, usually a little over two millimetres. In Spitwsella sororia, the common Ber- muda finger-sponge, a tube put into an exhalent aperture, or osculum, showed that the rate of flow is about four millimetres per second, and the rate of discharge about seventy-eight litres per day from each osculum — over four hundred and fifteen gallons for the whole sponge. As the experiments were made in the laboratory, the esti- mate is probably under the mark. An undisturbed specimen of Spirastrella at low water was found capable of over- coming a pressure of four millimetres of sea water. Big sponges often produce deformations of the surface of the sea above them, as a vigorous spring does ; but Professor Parker's interesting investigations indicate that the cur- rents flow at low pressure. COMPANIONS OF J 1 l.l.YFISHES.— It is well known that some medusae swim about with horse-mackerels (Carangidae) in the shelter of their Sowing lips. Mr. S. F. Light describes this in a Philippine jellyfish, Rhopilema visayana, with which a species of Caranx has established a companionship. " The fish would be seen playing about among the mouth, arms, and appendages, and on being alarmed would disappear under the edge of the bell, between the arms or in the subgenital porticus." A similar condition was found in the case of Lobonema mayeri. Inside the Rhopilema there was usually a crab (Char ibdis crucij era) , considerably paler than is typical for the species, which suggests a prolonged residence within the medusa. It is interesting to notice Light's observation that the companion fishes were seen eating dead specimens of Rhopilema visayana, though their relation with the living forms seemed to be quite friendly. " I am told," Mr. Light adds, " that R. visayana, which is closely related to the common edible medusa of Japan (R. esculenta), is used for food by the inhabitants of the east coast of Leyte, where it is preserved in vinegar." COLOUR CHANGE OF NEWTS.— The colour changes of the Palmated Newt (Molge palmata) are well described by Mr. Charles Oldham. " Individuals living in a pond with a dark, muddy bottom are dark green in colour, and in consequence when at rest are almost invisible from above ; similarly those in a pond with a bottom of yellow clay are yellowish in colour and alike inconspicuous. If, how- ever, one of the dark green Newts be placed in a glass vessel upon a white surface, it will, in the course of a few hours, become yellowish-drab in colour, but often paler in tint than the Newts which rested on the yellow clay; whilst, if one of the yellow-skinned Newts be taken from the pond with the bottom of yellow clay and placed into a glass vessel, it will be seen presently to exhibit greenish spots and marblings over the whole of the upper surface, and ultimately, by the expansion of these green areas, to acquire an almost uniform dark-green tint over the whole of the surface exposed to view from above. The green will, indeed, be darker in tint, provided the glass vessel stands upon some dead-black surface, than in the Newt which was taken from the pond with the bed of dark mud." (Trans. Hertfordshire Nat. Hist. Soc, Volume XV, 1915, page 207.) The colour-change depends on the contraction and expansion of the living matter of the pigment cells, which are under the control of peripheral nerves. The stimulus from the coloured environment first affects the eye, for blind animals do not change. NUMBER OF SPORES IN A MYXOMYCETE. By W. B. GROVE, M.A. In November, following the directions of Mr. S. P. Bolton, I found on a tree-stump a huge mass ot aethalia of the Myxomycete (Brefeldia maxima). The crowded aethalia covered a space of about six square feet, and were just ripening their spores. As the number of spores was evi- dently enormous, it was thought it would be interesting to make an estimate. For this purpose a gramme of spores and capillitium was taken and shaken up in two hundred cubic centimetres of water, with a little ether to loosen the spores from one another. After thorough shaking, the number of spores was counted, in the ordinary way, by a blood- corpuscle-counting apparatus of Zeiss. Allowing about six per cent, for capillitium, the number worked out at 10s in a cubic centimetre. Thus, in the whole mass covering the stump, roughly estimated at about five hundred cubic centimetres, there were half a million million spores. This result can be checked by geometrical considerations. The aethalium contains nothing but spores and capillitium ; the size of the spores varies from 9 to 12^. Taking 10/i as an average, the volume of a spherical spore is approximately \ • (j^)6 cubic millimetres. If equal spheres are packed as tightly as possible in a given space, geometry teaches us that about twenty-six per cent, must be allowed for the spaces between the spheres ; if, then, we allow six per cent., as before, for capillitium, and a further eighteen per cent, for the obvious loose packing and occasional larger spores (this last amount is, of course, a mere guess), we get a total allowance of fifty per cent. Therefore the number of spores in one cubic centimetre = 50% of 2xl0°xl0s = 109. THE FACE OF THE SKY FOR MAY. By A. C. D. CROMMELIN, B.A., D.Sc, F.R.A.S. Table 21. Date. Greenwich Noon. May , „ 6 ii ii ,, 16 .... , 21 ,. 26 .. 31 Su R.A. Dec. h. m. 2 30-5 249-6 3 9'° 328-7 348-6 4 87 4 29-0 N.i4-8 16-3 ■7"7 18 g 2D"0 2I'0 N.2I-8 Moon. R.A. Dec. h. m. o 16 i8"o S. 26*3 21 23-3 S. 15-7 1 9-8 N.I2'0 5 15-8 N.27-s 9 33-6 N.14'5 13 44-7 S. 15-9 19 9-6 S. 25-4 Mercury. R.A. Dec 2 29-6 N.14-5 3 "'6 >8'5 3 54-4 21-8 4 35'4 *4'i 5 "2'5 25'3 5 44 '3 25'° 6 9-6 N.25'2 Venus. R.A. Dec. h. m. o O 22"! N. 0"6 0 44-2 2-9 1 64 5-1 1 28-7 7'4 1 5i'3 9'6 2 14*2 1 1 '7 2 37'5 N-"3'7 Jupiter. R.A. Dec. h. m. 23 24"2 23 277 23 31-1 23 34 '4 23 37'4 23 40-3 23 43'° 5"o 46 4'3 3 '9 36 3 '3 3'1 Saturn. R.A. Dec. in. h 5 SS'3 5 57'5 5 59-8 6 2*2 6 4-8 6 7-3 6 10 'o N.22'7 22"7 22*7 22*7 22*7 22 7 N.22'7 Uranus. R.A. Dec 21 12*7 S.i6'8 21 13*0 16*8 21 132 168 21 i3'3 i6"3 2i 13*4 i6'8 ai 13*3 i6'8 21 13*2 S.i6*8 Neptune. R.A. Dec h. m 0 759*2 N.20*3 7 59"5 7 59'8 8 0*2 8 0*7 8 i*i 8 i*7 20*3 20 *3 20"2 20 "2 20 '2 N.20*2 Table 22. Date. Greenwich Noon. Greenwich Midnight. Sun. P B L Moon. P Jupiter. P B L L T T, 121 2 O 0 o - 24'4 -4'I 309-3 *3'4 3'6 243-3 22-3 3-0 177-1 ao'g a'5 iii'o I9'S 1 '9 44"9 '7'8 l'3 338-7 — 16*1 -o*7 272*6 + 7-3 — i8-o — 20 '9 - 2-6 +18-5 + i9'" - 8-4 a 0 a oh. ni. h. m. — 253 +i*s 129-6 267-7 8 27 e 4 36 e 23'3 16 1540 238-7 7 47' S 24 ' 25-4 1-7 178-6 209*8 7 te 6 i:f 25-4 1-7 203-2 iSi'o 6 26 e 7 oe 25-4 i-8 228-0 152-4 5 45' 7 47' 6 „ 8 „ 16 P Is the position angle of the North end of the body's axis measured eastward from the North point of the disc. B, L are the helio-(planeto-)graphical latitude and longitude of the centre of the disc. In the case of Jupiter System I refers to the rapidly rotating equatorial zone, System II to the tem- perate zones, which rotate more slowly. To find intermediate passages of the zero meridian of either system across the centre of the disc, apply to Ti T2 multiples of 9h 50m-6, 9h 55m-7 respectively. The data for the Moon and Planets in the Second Table are now given for Greenwich Midnight, i.e., the Midnight at the end of the given day. The letters m, e stand for morning, evening. The day is taken as beginning at midnight The Sun is moving Northwards at a slackening pace. Its semi-diameter diminishes from 15' 54" to 15' 48". Sunrise changes from 4" 36m to 3n 52m ; sunset from 7" la™ to 8h 4m. The Sun's surface is likely to repay careful scrutiny, owing to the recrudescence of activity. Mercury is in superior conjunction with the Sun on 1st; then it is an evening star, well placed for observation. East Elongation, 23° from Sun on 31st. Semi-diameter increases from 2k" to 4". Illumination diminishes from Full to g. VENUS is a morning star. Illumination increases from | to ?. Semi-diameter diminishes from 6\" to 6". The Moon.— Last quarter 6d 5h 23m m. New 14d 3h 5\m tn. First quarter 22d 4" 50m m. Full 28" 9b 55™ c. Apogee 14 respectively. Maximum librations 6" 7° W., 14" 7° S„ 22" 8" E., 27 7° N. The letters indicate the region of the Moon's limb brought into view by libration. E., W. are with reference to our sky, not as they would appear to an observer on the Moon (see Table 24). Mars is still badly placed, near Venus on 14th. Jupiter was in conjunction with the Sun on Feb. 24th, and is still difficult to observe. Equatorial diameter 36", Polar 34". Configurations of satellites at 3h 30™ a.m. Jupiter's Satellites. Day. West. East. I )ay. West. East. May I 2 O 134 M »y 17 Oi 243 „ 2 I 0 234 , 18 21 0 34 » .i 0 1234 . >9 23 0 14 . 4 21 0 34 , 20 3' 0 24 . S 3 c 14 '• , 21 0 214 , 6 3' 0 24 . 22 23' 0 4 . 7 32 0 1 • 23 Oi 2 34 , s ii 0 I* . 24 4 0 2> >• . 9 41 u 23 . 25 421 0 3 , io 4 0 123 . ZQ 42 0 1 i II 421 u 3 ■ 27 43' 0 2 . 12 432 0 1 , 2S 43 0 21 • '3 431 V1 2 . 29 423' 0 . 14 43 y 1 , ;o 4 0 '3 -'• . «5 343> u • 51 4 0 2? • , lb 0 243 The following satellite phenomena are visible at Greenwich, all in the morning hours : — ld 3h 30m I. Oc. R ■ 14d 3h 59™ 51* I. Fc. D. ; 16d 2b 30m I. Tr. I.. 3h 36™ I. Sh. I.; 21d 3h 44™ II. Tr. I.; 23d 3h llm I. SIi. I. ; 24d 3h 55m d 9h e. Perigee 28 6 e, semi-diameter 14 43 , 16 46" |, Qc. K. ; 2S'1 3b 47m II. Sh. I.; 31d 2b 16*° 35' 1 Ec P The Northward motion of Jupiter will make this year's opposition (which ocean on September 17th* mote favourable for European observers than those of the last four years, in which it has been verv low down. 121 122 KNOWLEDGE. April, 1915. Saturn is an evening star in Gemini. Is now approaching conjunction with the Sun. 2i° South of Mercury on 31st. Polar semi-diameter 8". Major axis of ring 38", minor 17". Angle P-6°-2. The Satellite positions are not given, owing to the planet's proximity to the Sun. Uranus is a morning star, but badly placed. In quadrature with Sun on Sth. Near Moon on 6th, 7h m. Neptune is an evening star in Cancer; diameter 2". Double Stars and Clusters. — The tables of these, given three years ago, are again available, and readers are referred to the corresponding month of three years ago. Variable Stars. — Stars reaching their maxima in or near May, 1915, are included. The lists in recent months may also be consulted (see Table 23). Meteor Showers (from Mr. Denning's List) : Date. Radian!. Remarks. K.A. 1 Dec. Mar. — M. iv 263 + 6°2 Ralher swift. A pi. 19 May 9 201 + 8 Slow. Apl.— Mav ... ■93 + 5S Slow, yellow. Apl. — May ... 296 0 Swift, streaks. .May 16 338 — 2 Aquaria's, swift, streaks. „ 7 246 + 3 Slow, bright. ,, II-lS ... 231 + 27 Slow, small. ,, 3010 Aug 3.33 + 28 Swift, streaks. May — lune ... 2S0 + 32 Swift. May July ... 252 - 21 Slow, trains. „ 181031... 245 + 29 Swift, white. The May Aquarids are of special interest from their asso- ciation with Halley's Comet. Accurate observations of their paths are desirable. Table 23. Long-period Variable Stars. Star. Right Ascension. Declination. Magnitudes. Period. Date of Maximum. T Camelop. ... R Auri^ae K Comae R Serpentis RU Herculis li. m. s. 4 3' 48 5 10 25 11 59 54 15 46 47 16 6 41 +65 59 + 53 3° + 19 16 + 15 23 +25 17 7'0 to 13- 5 6-510 13-3 7'3 <° i4'6 5'8to 135 70 to 142 d. 370 448 362 357 483 1915— Apr. 19 „ Apr. 4 „ June 1 ,, May 2 „ May 16 Night Minima of Algol ld 0h-4m, 3d 9m-2e, 18d 5h-3m, 21d 2h • 1 111, 23d llh-9e, 26d 8h -7 c. Period 2d 20h 48m-9. Principal Minima of /3 Lyrae 5d 9hm, 18d 7h m, 31d 5h m. Period 12d 21h 47m-5. Table 24. Occultations of Stars by the Moon visible at Greenwich. Disappearance. Reappearance. Dale. Star's Name. Magnitude. Time. Angle from Time. Angle from N. to E. N. to E. I9I5- h. m. h. m. * May 1 4 Scorpii . . 5 6 1 45 '" 57 2 35 '" 329 ,, 2 WZC 1098 67 — 3 28 m 247 , 3 BAC6I27 47 0 30 111 108 1 38 m 252 , 7 WZC 1466 7'l — — 3 11 "' 182 , 9 13 Piscium 6-5 2 53"' 354 3 '6 m 309 , 16 BACI754 57 7 5°' 97 8 46 < 278 , 16 BD + 26-884 6-8 9 6 e 179 — . 24 WZC 802... 71 9 34 « 100 , 26 WZC 849 7-0 0 52 m 94 — , 27 WZC 96s 7-2 11 15 « 41 — , 31 Lacaille 7849 7-0 1 36 '" 222 From New to Full disappearances occur at the Dark Limb, from Full to New reappearances. POLLARDS. The making of pollards ensures a supply from time to time of long poles suitable for fencing and other purposes, in much the same way as they are obtained in the under- wood of copses. There is this advantage, however, about the former method, that pollards can be grown in odd cor- ners, along the sides of streams (as in the case of willows), or in hedgerows. Where we find pollards in woods or scattered about common land, it seems likely that they were produced in connection with common rights, and that they were cut legitimately or otherwise by cottagers who were not supposed to touch the forest trees. There is no doubt but that old pollards which have been left alone for many years, such as those at Burnham Beeches, become very picturesque, but their conservation is a matter of difficulty. The old trunk becomes hollow, and often a mere shell has to support a large number of solid branches (see Figure 93), each of wh'ch may weigh several tons. Our illustrations (see Figures 93 to 97) show how, in the slightest wind or in the still air, the pollards may break up, and many of them have to be cut somewhat drastically in order to save them at all. April. 1915. KNOWLEDGE. 123 FlGL'KE y3. A Beech Pollard, showing the large mass of heavy branches, which if not removed will destroy the hollow trunk. Figure y-t. A Pollard that has lost one side, and to pn which the limbs must be lopped. Win and prop i" prevent the Pollard from breaking up. 124 KNOWLEDGE. April, 1915. F 1GURE 96. Limb of a Pollard that has been broken off by the wind. Figure 97. A Pollard cut back to preserve it from utter ruin. STONYHURST COLLEGE OBSERVATORY. By FRANK C. DENNETT. The Annual Report of this institution for 1914 has just been issued by its able Director, the Rev. Walter Sidgreaves, S. J., F.R.A.S. The year has proved remarkably mild and cloudy. The mean barometric pressure was 0-041 inch below the average, and the mean temperature l°-5 above the average. The rainfall proved to be 3-113 inches in excess of the mean quantity. Only one " record " seems to have occurred : January 8th had the heaviest fall of rain — 2-074 inches — for a January day that has occurred Y£Afl IS H 13 It 1/ 10 0 S 7 6 S t 3 2 1 isie ^ v iSOQ V. -T 1900 \ 1901 ) 1902 ri 1903 ^** 190* 1105 < -.-,-" 1906 / » * 1907 < < 100? s ^ x% 1909 > v^ IQ'O- < •«._ 191/ •• 10^ » 10/.? r > |9/» PCD . 4 Figure 98. Magnetic Mean Declination Range. Mean Daily Spot Area. during the previous sixty-seven years. May was the only month with a mean temperature below the average, and cloudiness is shown by the fact that the total hours of sun- shine registered are three hundred and twenty-eight less than the average of the past thirty-four years. September gave a record of thirty sunny days, with 176-5 bright hours. The wind record is below the annual average to the extent of two thousand three hundred and eighty-six miles. The strongest gale reached only forty-four miles in the hour on February 22nd. The rainfall of the year shows an excess of three inches above the usual record. January. March, May, July, September, November, and December each yielded a rainfall above the average, especially the last two, which together had a rainfall of 14-46 inches, or 5-392 inches in excess of the mean. In August and October little over half the usual amount fell. Magnetic records appear to be missing on five days — January 5th to 8th and June 29th. Of the remainder, one hundred and twenty-two are marked as calm, two hundred and ten as small, and twenty-five as moderate ; three days only are marked as greater, April 5th and 6th — when the fine sun-spot group No. 5 was crossing the central meridian — and September 27th ; but no very great disturbances occurred. The magnetic conditions during the year have been remarkably quiet. Solar observations were made on two hundred and seventeen days, and drawings made on one hundred and thirty-three : only nineteen of these showed faculae, and one hundred and fourteen spots and faculae. The mean disc area of spots (in units of one five-thousandth of the visible surface) appears at 0-82, and the mean daily range of the magnetic declination (in minutes of arc) at 10 '-2. These are included in the diagram constructed by the writer (see Figure 98), showing the variations since 1898, as given in the Stonyhurst reports, and are worth studv. The present report is additionally interesting in that it gives a record of the expedition organised by the Joint Permanent Eclipse Committee of the Royal and Royal Astronomical Societies to Hernosand, in Sweden, to observe the total eclipse of the Sun, August 21st, 1914. Originally it was arranged for Professor A. Fowler and Father Cortie, accompanied by Major Hills and Father O'Connor, with Dr. Fowler's assistant, to go to Kiev, in Russia. The Rus- sian Government, however, would not at first grant the necessary permission to the Jesuit Fathers. This objection, however, was withdrawn later at the intervention of Dr. Backlund, the Imperial Astronomer at Pulkova, but by good fortune the news did not reach the party. The out- break of War would have stopped the party at Riga, as, indeed, was the case with Professor Fowler. Had they reached Kiev the clouds would have prevented observations. As it was, they, through the good offices of Professor B. Hasselberg, found a capital site, with exceptional con- veniences, at Hernosand, in a field at the rear of the Technical School. Moreover, on the day of the eclipse they were favoured with fine skies. The equipment was good, and the observations successful. One photograph of the corona, taken with the twenty-foot objective — four inches aperture — is given in the report. A study of the rays in the corona makes it apparent that some of them are due to the great sun-spot (No. 24 in the " Knowledge" List). The corona was generally of the minimum type, the beautiful short radiations around the poles, the arc extending for 75° about the North and 65' about the South Pole. A long " fish-tail " extended away from the western limb, and spreading rays of the " intermediate " type from the eastern. Eight pro- minences appear on the plates, some being fine ones. Like other observers, they found what is usually known as the " characteristic coronal radiation " at wave-length 5303 to be barely traceable on the photographic plates. This appv to be weak at the times of sun-spot minimum, as it was faint in 1900. For more minute details the reader is referred to the report itself, which is well worthy of study. REVIEWS. BIOGRAPHY. Life of Sir John Lubbock {Lord Avebury) I [y HoRACl G. Hutchinson. 2 volumes. 338 and 334 pages. 2 illus- trations in each volume 8J-in. -,5.1-in. (Macmillan & Co. Price 30/- nel | It Mr. Hutchinson is not concerned with apportii to Lord Avebury his precise niche in Fame's temple, tin- volumes be lore us bring home to the reader the (act that the niche, wherever it may be situated, must be a very import. nit one. Mr. Hutchinson mentions more than once the comment th.it bankers considered l ord Avebury to be a good scientific man. while men i 't science looked upon him .is ,i i;o(xl banker , and. though we agree that the biography " dispos ever ol that ill-considered criticism, it may lx- well to look Eoj a moment at the reasons which may have led to it. It is not recorded, apparently, who is responsible for the epigram, but we should imagine that it was not made by a banker. Scientific men who specialise are prone to the very human 125 126 KNOWLEDGE. April, 1915. ailment known as " gutting into a groove," and look askance upon versatility which Lord Avebury possessed to a very remarkable degree. They seem to forget the necessity of broadmindedness, and fail to appreciate that he who makes known to the World what is being done in science is doing a very important work, with the help most probably of talents winch they do not themselves possess. Science is ignored far too greatly by the powers that be and by the commercial classes in this country ; and the mere fact that a man who has distinguished himself as a financier, a politician, and an administrator has also made a mark in science is of very great value to science. At one time there was a tendency to belittle Lord Ave- bury's scientific work because some of the observations which he used were earned out by others. Nobody objects to the fact that an architect does not with his own hands build the houses which lie plans, or that a modern sculptor puts only the finishing touches to the marble. Many scientific men have become famous through using the observations of others which they did not originate, and many a zoological professor has added his name to that of a demonstrator on the title pages of a paper written by the latter to the mutual advantage of both. Lord Avebury, who wasted very little of his time, planned out the work which he wanted done, and it was by delegating part of this that he was able to do so much. Mr. Hutchinson's book recalls that, besides being a banker, Lord Avebury was a member of Parliament, where he played no small part ; was Chairman of the London County Council, president of nearly all the scientific societies at one time or another. Warden of Birmingham University, and Rector of St. Andrews ; but even the two volumes before us are not sufficient to record a very great deal of the useful work which Lord Avebury did. We are reminded of his support of Darwin, and that we owe the terms " palaeolithic " and " neolithic " — now household words in science — to Lord Avebury. Educational movements in this country have profited by the help of Lord Avebury, which he was ever ready to give, and not the least of his endeavours was that to preserve something of the beauties and anti- quities of our land. The biography of Lord Avebury strengthens one's feeling gained from the lives of other famous men, whose career at school was cut short, that our system of education is not calculated to encourage individuality, and that those who go through the ordinary school course, and make their way in the world, succeed in spite of it. In conclusion, we may say that every thinking person would be the better for carefully reading Sir John Lubbock, Lord Avebury's life. W. M. W. CHEMISTRY. Photo-Chemistry.- — By S. E. Sheppard, D.Sc. 461 pages. 47 illustrations. 7£-in. x 5-in. (Longmans, Green & Co. Price 12/6.) This is the latest addition to the series of text-books of physical chemistry edited by Sir William Ramsay, and it fills a distinct gap in chemical literature. Most of the previous treatises on the subject have dealt, in the main, with the reactions of light in its special adaptation of photography, and there was no convenient handbook discussing the other aspects of photo-chemistry. The boundaries of this division of chemistry are not well-defined, for some of the radio-active phenomena also fall within its scope, and are therefore briefly touched upon in this book. It has been the author's aim, not to describe all the known photo-chemical changes, but rather to discuss typical instances at sufficient length to illustrate the theory. The book thus fulfils the true function of a practical handbook, of throwing sidelights upon the meaning of new phenomena met with by the student, and full references to original papeis are given on every page. The branches of the subject discussed include the measurement of quantities of light, the absorption of light, dynamics of photo-chemical change, special photo-chemistry, genesis of light in chemical change, and organic photo-synthesis (including the chemistry of chlorophyll). It is a book that should find a warm welcome from the chemist, the photographer, and the botanist with a knowledge of chemistry. C. A. M. GEOGRAPHY. A Little Book on Map-Projection. — By M. Adams. 108 pages. 41 figures. 8J-in. x 5J-in. (George Philip & Son. Price 2/- net.) To the non-mathematical student of geography no part of the subject presents so many difficulties as the study of map-projection. Although several excellent books on the latter subject have been written, the treatment in these is, without exception, mathematical, and hence incompre- hensible to many. For this reason alone this book by Miss Adams should be found exceedingly useful. The subject is treated in a strictly non-mathematical fashion, and even the simple trigonometric ratios only appear in some non- essential paragraphs. As is to be expected, the arrangement of the subject-matter is not strictly logical, but this does not in any way diminish the lucidity of the explanations. The first part of the book treats of the principles of map-projection, and of the various geometrical concepts connected therewith ; while in the second part is given a description of the types commonly in use. Sundry mathe- matical notes on certain of the latter are given in an appen- dix. A number of diagrams illustrative of the different projections are of much assistance in the comprehension of the descriptive parts (the diagram of the gnomonic projection is a trifle confusing, however.) In view of the great development of modern geographical teaching, this book should prove valuable, both to teachers and students, and it can be recommended as an attractive pre- sentation of a subject usually considered somewhat " dry." A. S. FORESTRY. Elements of Forestry. — By F. F. Moon, Professor of Forest Engineering, and N. C. Brown, Professor of Forest Utilisation, New York State College of Forestry, Syracuse, N.Y. 392 pages. 8J-in. x6J-in. (New York : John Wiley & Sons. London : Chapman & Hall. Price 8/6 net.) We have watched with interest the growth of State forestry in the United States from its beginning under Dr. F. B. Hough, in 1876, to the present day. In 1882 Dr. Hough published a work with the same title as that now before us — an excellent work, but based necessarily on the experience of European countries. Not till 1891 was Presi- dent Harrison empowered to reserve national forest land ; but the thirteen million acres that he set aside, to which President Cleveland added twenty-two million, rose under President Roosevelt to one hundred and ninety-four and a half million acres, " under the control of an efficient, non-political, technically trained " Forest Service. Deservedly, therefore, is this book dedicated to the last- named ex-President as the man who " aroused the American people to the importance of forestry as a national issue." This importance is categorically demonstrated by the authors under the following four reasons : — " First. — We are cutting our timber about three times as fast as it is growing. " Second. — Our per capita consumption is unnecessarily high, being two hundred and sixty cubic feet against forty cubic feet in Germany and twelve cubic feet in Great Britain. " Third. — Our per-acre production has sunk so low under the poor forest management until it is only about one-fourth of the possible yield. " Fourth. — Already the end is in sight for some species of timber, and the virgin supply of forest material in the April, 1915. KNOWLEDGE. 127 United States will be practically exhausted by the year 1950." This being so, it was clearly opportune that an up-to-date textbook on the general subject should appear ; and the present work is in marked contrast to Dr. Hough's book of 1882, in that it is the exposition of a complete system of forestry of purely national growth and character. Al- though, of course, the general principles of the physiology of the tree, of what the authors term " silvics," and even of sylvicultural management, forest protection, mensuration, and technology, are the same everywhere, the application of these principles to American species and American con- ditions gives a thoroughly local colour to the entire work. These principles, including also those of wood utilisation, wood preservation, and forest finance, are so clearly set forth as to render the book useful to anyone concerned with timber or forestry in any land ; while the map and the second half of the text give a more succinct and intelligible account of the forest regions of the United States than we remember to have met with anywhere else. A tolerably full glossary of technical terms is given ; but the English reader might be glad of an explanation of a good many words, such as " burlap," " duff," " excelsior," " kerf," " ross," and " tierce," which find no place in it. As, how- ever, the title-page bears the (to us) unusual inscription, " First Edition First Thousand," we r.iay well look forward to seeing all such terms explained in some future reissue. A bibliography — mainly of United States Government publications — is added to each chapter ; and the apparent ambiguity of such names as Yellow, Hard or Norway Pine, Red Cedar, and so on, is obviated by an appendix in which the scientific names are given. G. S. BOULGER. LOGIC. Logic : Deductive and Inductwe. — By Carveth Read, M.A. 417 pages. 7£-in. x 5-in. (Alexander Moring. Price 6 /-) This, the fourth edition of Mr. Read's " Logic," has been completely revised, and some new sections have been added. In the main, the author follows Mill, though not without occasionally criticising his position. The first part of the book, dealing with deductive logic, seems very satisfactory on the whole, the author's presentation being straightforward and clear, though the determination of the nineteen moods of the syllogism and their reduction to the first figure are treated rather briefly. The latter part of the book, dealing with inductive logic and allied topics, is of more questionable value, the writer, it seems to me, lacking something of Mill's precision. Some of the sections are, indeed, excellent, such as those on " The Canons of Direct Induction " and " Definition of Common Terms." But the defects in the chapters on " Transition to Induction " and " Causation," and elsewhere, are so serious that one hesitates to recommend the book to students. In metaphysics, " causation," and consequently " explanation," has an entirely different connotation from that with which it is used in logic and the natural sciences. It is very necessary, therefore, in a treatise on logic to make this difference quite plain, especially as the common use of these words has a vague idea of their metaphysical meanings behind it. Now, Mr. Read not only fails to do this, but habitually writes of " physical " causes as though they were " efficient " cm i a well. Great stress, moreover, is laid upon the principles of conservation of matter and conservation of energy. But to base logic on the principles of physical science, which themselves must seek their justification in logic, is surely to argue in a circle ; and the danger of this particular circle is the more evident now that the principle of the conservation of mattei has been called in question. Moreover, such a fallacious statement as "... all Times and all Spaces are com- mensurable, although in certain relations of space (as «•) the unit of measurement must be infinitely small," is surely remarkable in a book on logic, ^"hat, in fact, does the necessity for an infinitely small unit imply but that the things so needing to be measured are incommensurable ? In the chapter on " Hypotheses " the author appears to be straining after an unattainable ideal. As Poincare has pointed out, every phenomenon permits of infinite hypo- theses valid in the scientific sense of the term. The pragmatic criterion is the only one that offers us any escape from this burden of infinity ; and using that criterion we should adopt that hypothesis which is simplest, and there- fore most useful. There is no hint, however, of anything of this in Mr. Read's treatment of the subject. These defects are the more regrettable because of the commend- able quality of much else in the book. There are thirteen pages of examination questions at the end, but no index. H. S. REDGROVE. PHYSICS. The Principle of Relativity. — By E. Cunningham, M.A. 221 pages. 8§-in. x5i-in. (Cambridge University Press. Price 9/- net.) The subject of this treatise has received a large degree of attention since Einstein, ten years ago, brought the theory of Relativity into prominence. The doctrine itself may be regarded as teaching the futility of all experimentation with a view to determining the motion of matter with respect to the ether, if one is assumed to exist. If one does not postulate any ether, then the principle resolves itself into a denial of the possibility of determining absolute velocity in a physical sense. Although beginning with a negative hypothesis, the results are by no means limited to negations. As the author unfolds the results of the theory, one is reminded of the consequences flowing from the denial of a perpetual motion, or of the statement that heat will not of itself move from a place of lower to a place of higher temperature. The author is a well-known mathematician, a fellow and lecturer of St. John's College, Cambridge, and it is therefore natural to expect a highly mathematical treatment of the subject ; but the mathematical part has been compressed so as to leave room for very clear accounts of the optical and electrical experiments bearing on the subject. In fact, a large portion of the work will be read with ease and pleasure by the non-mathematical reader. The usual table of con- tents is reinforced by a very lucid and well-written summary of each chapter, which will be especially useful to serious students. The references given to the chief original papers will form a vers- welcome guide to the voluminous literature of the subject. J. H. V. Introduction to Physical Metallurgy. — By Walter Rosen- hain, B.A., D.Sc, F.R.S. 368 pages, 53 figures in the text. 88 figures on 32 plates. 8J-in. x5i-in. (Constable & Co. Price 10/6 net.) The arts of winning metals from their ores, and of fashion- ing these mi't.ils into weapons and implements, have been practised from prehistoric times, but the systematic study 0l the internal constitution and physical properties of metals and alloys- the science oi Physical Metallurgy — can l>r said to date only from 1864, when Sorby first noted the striking similarity in the nature oi the microstructures of steel and minerals in fact, nearly all the names uso- ciated with tins branch oi science are those oi men suii alive, and actively conducting investigations at the present day. This state of things naturally implies a large output of original work which only .i fortunate few have tune to follow closely. It implies, moreover. special methods of investigation, and even .i special nomenclature, which make it difficult, or even impossible, for those not familiar with 128 KNOWLEDGE. April, 1915. the science to understand the papers in which the results of investigations are described. The value of a book, therefore, which, while not over- burdened with detail, yet gives a clear survey of the methods of investigation and of the results so far achieved, cannot easily be overrated ; and Dr. Rosenhain is to be congratu- lated on having given us in the present volume just such a book. The microscopic examination of metals, from the selection and preparation of the specimen to the interpreta- tion of the structures revealed, is discussed with the sure touch of one with considerable experience, whilst the lucidity with which the construction of constitutional diagrams is described, and several typical alloy systems — and notably the iron-carbon system — are discussed, reveals the born teacher. The second half of the book is devoted to " the properties of metals as related to their structure and constitution." In this part are dis- cussed the mechanical testing of metals, the effect of strain, and the thermal and mechanical treatments of metal. The final chapter deals with " Defects and Failures in Metals and Alloys." The book is illustrated with numer- ous excellent reproductions of photomicrographs, but the omission of all details as to subject and magnification on the plates themselves, and in most cases of the page number of a given plate in the text, is a constant source of annoy- ance to the reader, necessitating repeated references to the list of plates at the beginning of the book. It is unfortunate also that the chapter on " The Thermal Study of Metals and Alloys " should be marred by several typographical errors. With these exceptions, however, we have nothing but praise for a book which can be unreservedly recom- mended to all who are beginning the study of physical mi'tallnrgy, and to those who, as manufacturers or users, are chiefly interested in the properties of metals from the " practical " side T. S. POND LIFE. /'"/.<:l Reserve Claims under life policies intimated and in course "I ; Annuities duo and unpaid ... Balance of bonus under life policies reserved tor distril 87.687.071 4 1 1.750.000 0 0 300.000 0 0 233.518 0 7 3.171 13 4 228.582 15 10 £91.202.343 13 10 ASSETS. Mortgages on property within the United Kingdom 8,882,496 5 4 Mortgage- on property out of the L'nit. .1 Kn .^ 1- ni 336.449 2 9 Loans on parochial and other puUi' in. - ... ... ... 13.412,347 14 8 Loans on Life interests 1,193.287 0 11 Loans on Reversions 96,502 18 3 Loans on stocks and shares ... ... ... ... ... 76,385 2 0 Loans on Company's policies within their surrender values ... 3,221,385 7 9 Pel ional security ... ... Loans to Educational institutions sc 43.969 19 1 Investments : — it with the High Court (£24,400 2}% C olidati 17,568 0 0 Carried forward £27.280.391 10 9 ASSETS Invcsti ■ K.ulu.i - Life inl Agents' balaw :.230.391 10 9 1.41 3. 36S 143.117 4.621.551 • 5.411.862 IS 11 I S 10 11 4.115.S13 0 6 1 5 2 10 10 7 12 10 IS 11 5 21.S47.943 3.193.674 4,783.46! 9.143 4.200.467 :. 8.4 1 115.010 52^.743 14 S 4 I 6 6 11 7 19 11 10 7 16 0 11 S 1 0 The values of the Stoi kl middle mark - than provided ter by the Investments Ri We certify that in our bclicl the Ass. I therein less thi I business to which it is ap] A. C. THOMPSON, Cm, " ' 20.000 1.241. 167 0 0 17 5 £91.202.34; 13 10 port th.it with the assistant e ol the t hai explanati ins that wc haw n quired, an I in our opinion such m of the state ol the Company's affairs according to tht i!v for any purp »c otha tl 1*1111.1 * l We have « • I mil paymcnl we find the sai VYc have al out in tl lUDti ' ■ " ■ . 1915. ~ M I on il , n ; KNOWLEDGE. April, 1915. CLARKSON'S SECOND-HAND OPTICAL MART. TELESCOPES. 4$>in, W'rny.ni r i : i massif c oak lath siaml with hers, liori- 7oni.il and vertical moi ;n t s by I [i ioke's joint, slow mi i in dei . .1 astro, ami i .i.i\ ' \ epiei es £-40 4-in..full,Nejpretti & Zumbra.ili.i/.. finder, 1 day, ; . ase :.'..in. Baker, altaz., hoi izontal and vertical motions, findei . da} ami .■ astros, 1 -in. Casella, altaz., 1 daj . ■ astros. Steward, on altaz. with equatoi ial rcles), 1 day, 2 astros. Wood, 1 astro, and 1 day eyepie* es Mans ■'' Also Eyepieces, Finders, Diagonals, etc. MICROSCOPES. Ituctil , 1(1 15 is 14 14 o I.! 15 0 IS MICROSCOPY. SECOND-HAND DEPARTMENT. Watson eyepieces, 1 -in., 1/6, oil immersion oltjccm 1 triple 1 piece, universal con- denser . - \\ ;itn . tives, triple nosepiece, spiral Abbe and iris, me< hanical stage, as new Baker "D.P.H." No. 1, 2 eyepieces, Leii/ ; ami 7 objectives, triple n -■ piece, Vbbe condenser Watson "Fram," eyepiece, spiral, \ i- ; .' mble nosepiei e 1 \ and 10 . . Leitz Mb, eyepiece, 3 and 7 objectives, d< mbli piral A h and ins Heck Small "London," spiral, \Ki" and iris, double nosepiece, 2/3 and 1/6 Sw ift " Discovery," eyepiece, 2/3, 1 6, double nosepiece .. Beck ".Star," sliding coarse and micro- meter line adjustments. 1 eyepiece. 2/3 and 1/6 objectives, di mble n use piece. spiral Abbe and in-, no case 3 5 o Many others. Also Objectives (a large stock by all the ending makers), Kyepieces. Double and Triple- Nose- ,■ . 1 ■■ . ( Condensers, Lamps, Spectroscopes, Miootoines, PRISM BINOCULARS BY ROSS. ZEISS, GOERZ. etc., FOR SALE AND WANTED. 338 HIGH HOLBORN (I Ipp site Gray's l"n Road), LONDON. SPECIALLY ATTRACTIVE SLIDES FOR POPULAR EXHIBITION V STUDY. Zoology, Marine and Freshwater. Unique preparations, wit/tout pressure^ in their natural form and beauty foi Dark Ground (■>■ transparent), 1 ,v\, M,-i tentacles; ffofothurians with wheel plates, etc.; ■> ■ in of th< curious Salfa and other Tunicata ; youn developing in their eggs ; the celebrated (W ; also the Radiolarian Spheerozoum^ the "Volvox of the sea," etc., etc. Insects and Parts. I.arvaof /7«;>/(-,/<,'/i«/ (also for polariscope). Superb tongues of the rare Sylvan Wasp and Hornet, also piercing organs of the Gaafly, etc.) etc. Special Cements, Forceps. - 1 etc, etc., for Mounting and Dissecting. SECOND-HAND INSTRUMENTS, OBJECTIVES, &c. NEW LIST NOW READY. Post free on request. To Beginners."— Expert advice freely given on ^election of suitable equipment; much time and needless expense can thereby be saved. Write 01 call. WuNTFD Microscopes, Objectives, etc., or whole Outfits purchased for Cash. EXCHANGES M* CLARKE & PAGE, 25, Thavies Inn, Holborn Circus, LONDON. LIVING SPECIMENS FOR THE MICROSCOPE. Vol vox globator, Desinids, Diatoms, Spirogyra, Amceba, Actinophrys, Spongilla, Vorticella, Stentor, Hydra Cordylopohra, Stephanoceros, Melicerta, Polyzoa, and other forms of Pond Life, 1s. per tube, with printed drawing, post free. Thomas Hoi. ton, Naturalist, 25, lialsall Heath Road, Birmingham. MINERALOGY AND GEOLOGY. JAMES R. GREGORY & Co., Mineralogists, &c. Are in .1 better position than ever for supplying Collections of Minerals, Fossils & Rocks, A* they hav ateriaj. LISTS AS USUAL. 139, Fulham Road, South Kensington, S.W. Tele Telegri Western '2X41. 1 Meteorite:.. Londo Microscopes, Telescopes, Spectroscopes, Binoculars, Surveying Instruments, 4c, BY THE BEST MAKERS AT MODERATE PRICES. Lists sent post free on request. Scientific Instruments Sought, Exchanged and Sold on Commission. JOHN BROWNING, 146 STRAND, and 72 New Oxford St.. LONDON. Telegrams : 'AUKS," LONDON. Telephone 884 GERRARD. Established Stevens' Auction Rooms, 38, KING ST., COVENT GARDEN, LONDON, W.C. Every FRIDAY at 12.30, Sales are held at the Rooms of Microscopes and Slides, Telescopes, Si rveving Instruments, Electrical and Scien- riFic Apparatus, Cameras and Lenses, Lanterns and Slides, Cinematographs and Films, in great variety, Lathes and Tools, Etc. Goods may be sent for inclusion in early Sales. Settlements made one week after disposal. Catalogues and all Particulars Post Free. Valuations for Probate or Transfer, and Sales con- ducted in any part of the Country. FOR ALL KINDS OF EDUCATIONAL Mineral Material, COMMON ORES, and SELECT CRYSTALLIZED SPECIMENS, at ALL PRICES. G. H. RICHARDS & Co., Dealers 'n all kinds of British and Foreign Mineral Specimens. PRICE LISTS FREE. 4£ Sydney Street Fulham Road, South Kensington London, S.W. F. WIGGINS & SONS, 102, 103, 104, Minories, LONDON, E Contractors to H.M. Government. FOR LAMPS. STOVES. VENTILATORS, ELECTRICAL WORK AND ALL PURPOSES. Largest Stock in the World. Tel. No. 2248 Avenue. Printer of ' Knowledge. JOHN KING, Uxbridge, Southall, and Ealing, T s favourably equipped for the PRI NTI NG of *■ Scientific Hooks, Brochures, Catalogues, &c, ami will be pleased to submit estimates. Address all Communications to 213, UXBRIDGE ROAD, EALING, LONDON, W. "Phone: 1144 Ealing. Binding Cases for Knowledge Volume, 1914. IN BLUE CLOTH, WITH GILT DESIGN AND LETTERING. 9d. net each : by post, Knowledge Office: AVENUE CHAMBERS, BL00MSBURY SQUARE, LONDON, W.C. A most acceptable Girt at any time. KNOWLEDGE VOLUME FOR 19 14. Container; 440 Pages m'Ii 425 Illustrations, many being Full Page Plate'.. ... .i in Blue Cloth. AAjn x . jnstruinellt- CONVENIENT '. Eiery necessary movement is embodied. STABLE " With either tripod or horseshoe foot. PRACTICAL : Intended fur hard work. LAST A LIFETIME. The "RESEARCH" Microscope. Specification : — Mechanical Stage — Giving move- ments 2" X If. Both milled heads on same axis. Fine Adjustment — Side limb, vertical lever type. Coarse Adjustment — Diagonal rack, long range, enables 3" objective to be focussed when on nosepiece. Compound Substage — Rack and pinion focussing with centering screws for condenser. Movements are slotted and sprung throughout, and wear can be at once compensated. Tripod foot giving stability in any position. Guaranteed for 5 years. Fop the Amateur op Professional this instrument embodies every desirable movement, and ,is at once the cheapest and the best obtainable. Prices: — , Research Microscope ... £12 10 0 00. 00. with eyepieces No. 2 and No. 4, objectives 1" and .11 mm. working distance for pond life or blood counts), aplanatised Abbe illuminator with iris diaphragm. In mahogany case 17 17 6 Full details of the above, and also of 32 Different Models at all prices, will be found in Watson's Micro- scope Catalogue, No, 2 k, which will be forwarded gratis on application. APPARATUS FOR:— PHOTOMICROGRAPHY. POND LIFE. METALLURGY. PETROLOGY. BACTERIOLOGY. PROJECTION. HEMATOLOGY, &c, &c. W. WATSON & SONS, LTD., Contractors to fx/ny eovetnments, 313 HIGH HOLBORN, LONDON, W.C. Branches : 16 Forrest Road, Edinburgh; I96 Great Portland Strew, London, W. Dki-6ts : 2 Easy Row, llirminiiham; 78 Swanston Street, Melbourne, Australia: 2I2 Notre Dame Street West, Montreal, Canada. Optical Works— HIGH BARNET, HERTS. ESTABLISHED 1837. The BECK BINOCULAR BECK BINOCULAR MICROSCOPE. No. 1081 P.S. (Patent applied for) Not only an advance on previous Binoculars, but better tban a Monocular with all powers. 1. Resolution equal to that of a Monocular. 2. Equal illumination in both eyes. 3. Short tube length, mak- ing Microscope com- pact. 4. No special object- glasses or eyepieces required. 5. Standard angle of con- vergence. 6. Stereoscopic vision. 7. Binocular vision, saving eyestrain and giving better results than Monocular vision. 8. Converted into a Mon- ocular by a touch. Full descriptive Booklet and Price List on application. R. & J. BECK, Ltd- 68 Cornhill, London, E.C. DENTS CLOCKS WATCHES AND CHRONOMETERS FOR SCIENTIFIC USE. Sidereal op Mean Time Clocks for Observatories, £21 and upwards. THREE GRAND PRIZES and ONE GOLD MEDAL ill! FRANCO-BRITISH EXHIBITION. The only Grand Prize awarded to a British Firm for Watches, Clocks and Chronometers. The only Grand Prize awarded for Astronomical Regulators. Chronographs, and Ship's Compasses. TRADE MARK 61, STRAND, and 4, ROYAL EXCHANGE, LONDON. Telephone So. 61 City. UXB PR Address JOH RIDGE If NTING and wi N KING Printer of •' r%ir»\J» "Knowledge," , SOUTHALL, AND EALING, favourably equipped for the OF SCIENTIFIC BOOKS, BROCHURES, Ac, 1 be pleased to submit Estimates. Road, Ealing, London, W. Tn.l«NOal . 114* |UI CAUTION. The Proprietors of SCHWEITZER'S "COCOATINA, "FAIRY COCOA," &c, beg to inform their clients that XOXE of their products are manufactured in Germany ; that they are a private E\GLISH COMPANY man- aged by a Board of EXGLISH DIRECTORS; and that all shares are held by relatives and con- nections by marriage of the late sole proprietor. Captain Thomas Edward Symons, R.N. KNOWLEDGE. April, 1915. FOR Zoology & Botany Classes & Forestry Work. Adopted by Agricultural!} and other Colleges under various Government Departments. [Jauscfi [omf> DISSECTING MICROSCOPE. The best Instrument of its kind. Has hinged base provided with suitable receptacles for imuj instruments used in the work. and dissecting Complete with two Coddlngton lenses, 38mm. and 19mm., Inland parcel post, Cd. ^^^_^_^_-______ ITS. 6d. Foreign, Is. Ctl. MICROSCOPES FOR AIL REQUIREMENTS UP TO THE MOSTADVANCED RESEARCH. OVER 100,000 SOLD, WHICH ARE IN USE THROUGHOUT THE WORLD. Call and Inspect at our New Showrooms, or ask for List "A 2" (Microscopes) post free. Also particulars of MICROTOMES, PHOTO-MICROGRAPHIC and DRAWING APPARATUS, PROJECTION APPARATUS, CENTRIFUGES, GANONG'S APPARATUS lor PLANT PHYSIOLOGY, VISCOSIMETEUS, Sc, on application. N.B.— ALL OUR INSTRUMENTS BEING MADE AT OUR OWN FACTORY IN ROCHESTER, N.Y., THERE WILL BE NO DELAY IN DELIVERY, AND WE HAVE JUST RECEIVED LARGE STOCKS. Trade Mark. BAUSCH & LOMB OPTICAL CO. Contractors to British and Foreign Governments, 37-38, HATTON GARDEN, LONDON, E.G. [Telephone: Holborn 2640.] OR THROUGH ALL DEALERS. [Telegrams: "Optibalof, London: Trade Ma Dr. A. HUTCHINSON'S NEW UNIVERSAL GONIOMETER For the Examination 0! Small Crystals and Mineral Grains. This instrument can be used lor any of the following purposes : — As an Ordinary Goniometer for the Measurement of Angles. As an Axial-angle Apparatus. As a Kohlrausch Tolal-rerlectometer. For Determining Refractive Indices by the Prism Method. For Experimental U'oik in Mineralogy. Descriptive PatrplUct on Application. JAMES SWIFT & SON, UNIVERSITY OPTICAL WORKS, 81, TOTTENHAM COURT ROAD, LONDON. Pastorelu & Rapkin, (Estab. 1750.) Ltd. 46, HATTON GARDEN, LONDON E.C. GLASS-TOP BOXES, BOTH CARD &. WOOD, FOR COLLECTORS. MUSEUMS. &c, for STORING SHELLS. EGGS, COINS OR OTHER OBJECTS. In all sizes, both pound and rectangular. FLATTERS & GARNETT, Ltd., MAKERS OF LANTERN AND MICROSCOPE SLIDES, 309, OXFORD ROAD (%££'). MANCHESTER. ACTUAL MANUFACTURERS of all kinds of Meteorological Instruments. STANDARD INSTRUMENTS. (With Kern Certificates, if dr. id.) Fort in's Barometers. Maximum Thermometers. Minimum Thermometers. Hygrometers. Earth Thermometers. Sunshine Recorders. Rain Gauges. Anemometers. Self-registering Rain Gauges. , Barometers. _ .. Thermometers. Self-recording Rajn Gauges 1 Anemometers. Etc. Illustrated Price List Post Free. ContractOPS to H.M. Government. Telephone: 1981 Holborn. Telegrams: Rapkin, London. \* We pay carriage and guarantee safe delivery within U.K. on all our Instruments. Printed for the Proprietors (Knowledge Publishing Company, Limited), by John King, Ealing and Uxbridge. — April, 1915.