at the limit of the influence of the eastern tide, according to what was said in article 8. Will the interference of the tides explain such a change?

It obviously will do so; for the two tides at their meeting differ by twelve hours in the extent of their course, the one which has come round the northern extremity of Scotland and down the east coast being so much older than the channel tide. If, therefore, one of the two be a morning tide (when referred to its origin), the other must be an afternoon tide; and each compound tide being made up of such a pair, will show no peculiar character of either one or the other. Thus we may expect that, as far as the interference of the tides extends, the diurnal difference will disappear.

Taking the two considerations of Article 8. and this article together, I think it cannot be doubted that the sea, from the Isle of Wight to the Downs, and probably further, is affected by both the western and the northern tide.

11. It is natural to inquire whether we can, from our observations, discover the nature of the effect which the form of the coast produces on the time and height of the tide. On this subject I can offer some reply, though a more complete discussion of the existing returns, and of future observations, is desirable to confirm and extend our views.

The principal feature which appears in the observations of June is, that the tidehour varies very rapidly in rounding the main promontories of the coast, and very slowly in passing along the shores of the intervening bays. Thus, along the whole of the great bay formed by the coast of Devonshire and Dorsetshire, from Prawle Point to Portland Bill, the tide hour is nearly the same, ranging only from about 6h 5m to 6h 20m. But in passing round into Weymouth Bay the hour becomes 7, and on going round St. Alban's Head into Swanage Bay, it becomes suddenly 9h.

If we draw the cotidal lines so as to correspond with these conditions, it is clear that the ends of these lines will be brought close together at the promontories, and that the lines will run along nearly parallel to the shore. Thus, the extremity of the 6h cotidal line is near Prawle Head, the line itself following nearly the coast of the bay to Portland Bill. The 7h cotidal line ends at Portland Bill, and the 8h and 9h lines end at St. Alban's Head. The 10h and 11h lines appear to meet the coast near St. Catherine's Head in the Isle of Wight; and, agreeably with what has already been stated, the 11 line runs at a little distance from the coast through the straits of Dover. The cotidal lines drawn in my Essay printed in 1833 require to be modified according to these remarks.

12. At points of the coast where the cotidal lines are brought near together, the place of high water moves slowly; so that it is high water at one point, while at another point not far off, the water is still considerably deficient from its greatest height. Hence there will be a difference of level and a rapid tide-stream in such cases. Thus the peculiarity just noticed in the reference of cotidal lines to promontories is con

nected with the occurrence of strong currents governed by the tide, like the Race of Portland and the similar current which is found off St. Alban's Head.

I abstain from making any further remarks till the reduction of the whole of the returns of last June shall give me more complete materials. I am the more desirous to draw attention to the results which such observations may supply, on account of its being intended to repeat the observations at the Coast Guard stations in the ensuing June, from the 9th to the 27th. I am also glad to be able to state, that the subject having been laid before the Lords of the Admiralty by CAPTAIN BeauTheir Lordships expressed their wish that application should be made to foreign maritime states, with a view to induce them to make contemporaneous observations on their coasts; and that such applications are now in the course of being made. The extension of such results as have been stated in the present paper to other coasts, and the discovery of other similar laws, cannot but be looked upon as a valuable and interesting addition to our knowledge.

FORT,

VI. On certain Peculiarities in the Double Refraction and Absorption of Light exhibited in the Oxalate of Chromium and Potash. By Sir DAVID BREWSTER, K.H. LL.D. F.R.S.

Received January 27,-Read February 12, 1835.

THIS remarkable salt was put into my hands about the end of the year 1832, by Dr. WILLIAM GREGORY, of Edinburgh, to whom I have been indebted for much kind assistance in carrying on my inquiries respecting the action of coloured bodies in absorbing definite rays of the spectrum. A very brief examination of its optical properties was sufficient to indicate its more obvious peculiarities, and a short notice of these was published at the time. Having received, however, from Dr. GREGORY a very fine group of well formed crystals, and having had an opportunity in the spring of 1833 of observing their action upon the spectrum, both in their solid state and in the state of aqueous solution, I am now able to present to the Society a general view of the results which I obtained.

The oxalate of chromium and potash occurs in flat, irregular, six-sided prisms. The two broadest faces are inclined to each other like the faces of a wedge, whose sharp edge is the summit of the crystal. These faces are considerably rounded, being parallel near the base, and inclined to each other about three degrees at the apex of the prism. The incidence of the broad faces upon the adjacent faces of the prism is about 140°, and therefore these faces are inclined to one another at an angle of 180° — 148° x 2 = 64°. The crystal is terminated by four minute planes equally inclined to the broad face and the axis of the prism, but two of these faces often disappear, and the crystal terminates in an oblique edge in place of a triangular apex.

If we call A A' the broad faces of the crystal, m, m', m, m' the other four faces of the prism, and o, o', p, p' the faces on the summit, the following are the angles which they form with each other.

Incidence of A upon A in a line passing through the axis of the prism

A upon m, and A' upon m'

5° 10'

A

upon A' over o, o' or p,p′ ·

50 10

4 36

The crystals of oxalate of chromium and potash are, generally speaking, opake; and at thicknesses not much greater than the twenty-fifth of an inch they are abso

lutely impervious to the sun's rays. In this state their colour, seen by reflected light, is nearly black; but their powder is green in daylight, and of a French grey colour by candlelight. In the smaller crystals, which are generally the best formed, the colour both of reflected and transmitted daylight is blue, but that of candlelight is purple. I have not been able to find any distinct traces of cleavage.

axes.

This salt possesses a powerful double refraction, which is no doubt related to two In reference to the axis of the prism the double refraction is negative, like that of calcareous spar. The greatest refractive index is about 1.605, and the least about 1.506, reckoning from a line near the boundary of the blue and green rays.

One of the most remarkable properties of this salt is the difference of colour in the two images formed by double refraction. At a certain small thickness the least refracted image is bright blue, and the most refracted image bright green, in daylight, or bright pink in candlelight. The blue contains an admixture of green when analysed by the prism, and the green an admixture of red, the red predominating over the green in candlelight. At greater thicknesses the blue becomes purer and fainter, and the green passes into red; and at a certain thickness the least refracted blue image disappears altogether, and the most refracted image is olive green. At still greater thicknesses this image disappears also, and absolute opacity ensues.

When the crystal is exposed to polarized light, with its axis in the plane of polarization, the transmitted light is green; but when the axis of the crystal is perpendicular to that plane, the transmitted light is blue.

When the oxalate of chromium and potash is dissolved in water its double refraction disappears, in consequence of the particles being released from the force of aggregation by which they are held together in the solid state, and by which double refraction is produced. The solution, however, exhibits the same general action upon light as the solid. At moderate thicknesses its colour is a dark blueish green by daylight, and a bright blood red by candlelight; but when we increase the thickness of the fluid it becomes of a blueish pink by daylight, and of a deeper blood red by candlelight, the red rays continuing to increase both in day- and candle-light, as we lengthen the path of the ray through the solution.

The most remarkable property of the oxalate of chromium and potash, and the one on account of which I have submitted this paper to the Royal Society, is its specific action upon a definite red ray lying near the extremity of the red portion of the spectrum. This is a property which is not possessed by any solid or fluid body with which I am acquainted, although I have submitted some hundreds of coloured bodies to direct experiment. Like all coloured bodies, the oxalate under our consideration exercises a general absorbent action on the spectrum. The smallest thickness of it, in which colour is scarcely discernible, attacks the yellow rays of the spectrum on the more refrangible side of the line D of FRAUNHOFER. As the thickness of colour of the solution increases, the violet rays are absorbed, and also all the yellow, orange, and less refrangible green, till the whole space D E, and part of the spaces on the other

side of the lines D, E, are wholly destroyed. In this state the prism gives two distinct images of objects, viz. a red and a greenish blue image, which are considerably separated. As the absorption advances, the green on the blue side of E, and the blue on the violet side of F, gradually disappear, till a pure blue image about F alone remains, and this too wholly vanishes by an increased thickness of the solution, leaving the red rays unabsorbed.

While these changes are going on throughout the spectrum, a specific action is exerted upon a red ray between A and B of FRAUNHOFER, and in that very part of the spectrum over which the solution exercises no general absorptive action. The sharp and narrow black band which is thus formed constitutes a fixed line in all artificial lights, and also in solar and day light, which will enable philosophers to measure the refractive powers of all bodies in reference to this line with an accuracy which could not otherwise be obtained, unless by the use of fine prisms of the refracting substances, which in most cases are unattainable.

In order to render this line or band of real use in practical optics, I have endeavoured to fix its place with as great accuracy as possible. Between the lines A, B of FRAUNHOFER there is a group of lines nearly bisecting the space A B, which he has marked a in his map. The dark band lies in the space Ba; and if we designate it by the letter X, its position is such that BX = 3 Ba, or the index of refraction in the Water spectrum, of the rays which are absorbed at the band X is almost exactly 1-330701, the temperature of the water being 65° of FAHRENHEIT.

The relations of this salt to common and polarized light may be readily examined and finely exhibited by placing upon a plate of glass a few drops of a saturated solution of it in water. If the crystals are slowly formed they will be found of various thicknesses, each thickness exhibiting a different colour, varying from perfect transparency, through all shades of pale yellow, green, and blue, in daylight, and through all shades of pale yellow, pale orange, red, and blue, in candlelight.

BELLEVILLE, by Kingussie,

March 21st, 1835.