The mighty deep : $b and what we know of it — John Shaqi
The mighty deep : $b and what we know of itGiberne, Agnes
Science
The mighty deep : $b and what we know of it
Giberne, Agnes
Marine biology; Nature study
People often grow to like best that to which they are accustomed. A
lady, who had spent most of her life on the borders of that brown
Channel, once assured me that she infinitely preferred it to the “deep
blue sea.” She had been to stay by the latter, and had found its
monotony of tint so uninteresting that she was charmed to get back to
her old friend.
Tastes differ, certainly. Not many would agree with her. Yet it is a
fact that the great Turner went to the Bristol Channel, with all its
mud, for many of his marvellous sea and cloud effects.
“Deeply, darkly, beautifully blue,” sang Byron of the ocean, and he
sang truly, even though the ocean itself, putting aside the Bristol
Channel, is not always and uniformly azure. Near land the tint is often
greenish. Sometimes it is pure green. Often it is a pale and watery
blue. At other times we have a leaden grey. The genuine ocean-blue,
which resembles nothing else on Earth, can seldom be enjoyed till one
gets on really deep water, far from land. Or--till one is looking at
the Mediterranean.
Why should the sea be blue? And why should the sky be blue? For the
matter of that, why should anything be blue? What do we mean by
colour?--whether blue or green, red or yellow?
We mean that particular tint--or sensation--which the object in
question causes us to see--or feel. The object receives sunlight,
and reflects it to our eyes. And since sunlight is white or
yellowish-white, one might expect that everything we look upon would
appear to us white or yellowish-white.
But everything does not. And the reason is that a ray of sunlight is
really a bundle of lesser rays, each of which has its own colour. If
a ray of light is made to pass through a prism, these lesser sub-rays
are spread out upon wall or floor, always in the same order, from
violet at one end to red at the other end. Light is believed to be due
to enormous numbers of most minute wavelets; and for each colour the
wavelets have a definite but different size. They are smallest at the
violet end, and largest at the red end.
Now when a ray of sunlight falls upon anything--leaf or flower, earth
or water--some of the sub-rays are absorbed or taken in, and some are
rejected or refused admission. A healthy leaf, for instance, absorbs
the red, the yellow, the blue, the violet, and refuses the green, which
is therefore thrown back from the leaf-surface to our eyes, making it
green to us. A ripe tomato absorbs the yellow and green, the blue and
violet, and reflects the red. A lump of blacklead absorbs greedily all
the rays, reflecting none, and so to our eyes it is black or without
colour. The petals of a white rose, on the contrary, absorb so little
colour of any kind, that practically the entire ray is sent again to us
as white light.
If this is the manner in which the ocean is blue, it means that
sea-water, and indeed water generally, must in itself be actually blue,
as a cake of ultramarine, a sapphire, a corn-flower, a forget-me-not,
are blue.
Public-domain text, read in full here on John Shaqi.
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