Over the vast, gently undulating spaces separating these submerged
lines of volcanoes and the ridges of coral, lies a mat of mud of
unknown thickness, which naturalists term “ooze.” It is principally
composed of volcanic dust and of the microscopic “tests,” or flinty
limy skeletons of minute animals, few of which are large enough to be
seen by the unaided eye. “Dwelling in myriads in the superficial parts
of the sea, these foraminifera, as they are termed, sink at death to
the bottom, over which they accumulate a thick coating of minutely
divided limestone powder, forming a layer of ooze as unsubstantial as
the finest snow.”
In regions like the North Atlantic this ooze consists almost wholly of
such animal matter; but in other regions, such as the South Pacific,
where volcanoes prevail, it is constantly and largely increased by an
enormous quantity of mineral matter hurled broadcast by volcanoes,
all of which are on islands or near sea-coasts. A part of this is the
merest dust, which slowly settles from the air, perhaps hundreds of
miles from where it was ejected. A larger part consists of that spongy
lava called pumice, which is so full of holes filled with air and
gases that it may float half way around the globe before it sinks, as
happened after the explosion of Krakatoa.
Into the oceanic ooze, too, sinks so much of all dead fishes and other
mid-sea animals as is not dissolved or devoured before reaching it; and
it forms the grave of thousands of men. It is often said that ships
and other things would not sink far, but would float, suspended by
dense water or some miraculous influence, only a few hundred or a few
thousand feet below the surface, for no one knows how long. But this
eerie notion has no foundation in fact. “No other fate,” we are assured
by those who know, “awaits the drowned sailor or his ship than that
which comes to the marine creatures who die on the bottom of the sea.
In time their dust all passes into the great storehouse of the earth,
even as those who receive burial on land.” Wooden wrecks probably last
much longer than those of iron.
Public-domain text, read in full here on John Shaqi.
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