It w ould be outside the scope of this essay to at¬
 tempt to discuss fully and systematically the varied
 and complex colour effects seen at sea, but, beyond the
 general outline which wehavepresented, atewremarks
 on some special features will not be out of place.
 
The waters of the Mediterranean are rich in colour¬
 ing, and will furnish illustration of certain points. At
 some distance from land, the churning of the screw
 or the foam of the breakers shows an almost pure
 blue, but nearer shore (probably owing to contamina¬
 tion of some kind) the water assumes a greenish
 tinge, which becomes still more marked in the har¬
 bours. This brilliant colour, it need hardly be said, is
 
 
Dover that often greets us on our return to English
 waters from sunnier seas. Looking down into the
 clear depths of the Mediterranean, however, the water
 often seems to be of a slightly purplish or violet blue,
 and does not show any sign of green. Even ona dull
 day, when looked at perpendicularly from the deck
 or in the near sides of the waves, it still appears of
 this beautiful deep ultramarine,—so that the colour
 is evidently not due to reflexion from the blue sky,—
 whilst the farther sides of the waves, being tilted away
 from us, reflect strongly the gray light from the clouds.
 The most probable explanation of this difference is
 that sea water, in common with many other liquids,
 possesses the property of showing a somewhat differ¬
 ent colour according as one is looking through a thick
 or a thin layer of it." In this case the particles in the
  
‘ A solution of Prussian blue, with which the sea water was
 matched in Threlfall’s experiments, described on page 84, has this