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
Between Land and Ocean a ceaseless contest is carried on.
The land is always endeavouring to keep its present state unchanged.
The ocean is ever trying to tear down and demolish the land. Yet the
very object of the ocean in so doing seems to be that new land may be
raised up with the stolen materials.
There are Continents and Islands, moulded long ago, which we see as
finished structures, that have reached the meridian of their existence
and entered upon their decadence. With many of these Ocean’s efforts
are chiefly employed for destruction. Indeed, in all cases, the power
which once erected an island or a continent is at work upon it still,
not always and only for destruction, but sometimes for modification,
altering its shape, making it larger or smaller, rounding a curve here,
adding a protuberance there, giving finishing touches, and in the end,
if not from the beginning, acting also as spoliator.
But the work of building has not ceased; it never does cease. Through
the ages it has gone on, and it goes on yet. There are embryo islands,
perhaps embryo continents, being now slowly fashioned in Ocean’s
workshops, not ready for use.
A great part of the work of land-building takes place in darkness. It
is carried on, not merely from day to day, but from century to century,
never hasting, never pausing. The materials are brought often from
far distances, not by men, but by streams, by rivers, by glaciers, by
ocean-waters; and the weight of those waters helps to weld the gathered
materials into a solid whole.
Anybody who watches the results of even one heavy downpour of rain on
land may gain some notion of what is going on everywhere.
If your house has a soft-water tank, you can hardly have failed to note
how black the water becomes, after a pelting shower, following upon a
drought.
No wonder, for the rain has washed the roof, and has carried off a
supply of collected dust and soot. Not the roofs of houses alone, but
the streets, the walls, the pavements, in a town--the trees, hedges,
grass, roads, in the country--are all relieved of dusty layers, while,
if the rain be heavy enough, sand and soil also are swept away.
Sometimes they are only taken to a lower level in the same
neighbourhood, but large quantities find their way into the drains or
streamlets, which join bigger brooks, and thus reach the nearest river,
finally joining the sea.
Any moving stream is able to carry along floating materials, which
in still water would sink to the bottom. The faster the current the
heavier is the weight which it can support. A mountain torrent conveys
pebbles, grinding them to a smaller size as it rushes along; and some
of the more powerful torrents transport even great stones.
Public-domain text, read in full here on John Shaqi.
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