The Story of the Atlantic TelegraphField, Henry M. (Henry Martyn)
History
The Story of the Atlantic Telegraph
Field, Henry M. (Henry Martyn)
Transatlantic cables
is easy to see that it is not dragging through the water, but over the
ground. "I often went to the bow," says Mr. Field, "and sat on the
rope, and could tell by the quiver that the grapnel was dragging on the
bottom two miles under us."
And thus, with its fishing line set, the great ship moves slowly down
over where the cable lies. As the grapnel drags on the bottom, one of
the engineer's staff stands at the dynamometer to watch for the moment
of increasing strain. A few hours pass, and the index rises to eight,
ten, or twelve tons, sure token that there is something at the end of
the line--it may be the lost cable, or a sunken mast or spar, the
fragment of a wreck that went down in a storm that swept the Atlantic a
hundred years ago. And now the engine is set in motion to haul in. As
the rope comes up, it passes over a five-foot drum, every revolution
bringing up three fathoms. Thus it takes some hours to haul in over two
miles' length, perhaps at last to find nothing at the end!
Success in hooking the cable depends on the accuracy of their
observations. These were sometimes verified in a remarkable manner. When
the nights were very dark and thick with fog, so that they could not see
the stars above nor their lights on the ocean, they had to go almost by
the sense of feeling. Yet so exactly had they taken their bearings, that
they could almost grope over the ground with their hands. A singular
proof of this was given one night, when, just as the line began to
quiver, showing that the cable had been hooked, one of the buoys--which
had not been seen in the darkness--thumped against the side of the ship.
So exactly had it been placed over the prescribed line, that the ship
struck the buoy just as the grapnel struck the cable! The accident,
which startled them at first, when it occurred in the gloom of night,
furnished the strongest proof of the accuracy of their observations; and
the officers were very proud of it, as they well might be, as a victory
in nautical astronomy!
These different experiments revealed some secrets of the ocean. Its
bottom proved to be generally ooze, a soft slime. When the rope went
down, one or two hundred fathoms at the end would trail on the sea
floor; and when it came up, this was found coated with mud, "very fine
and soft like putty, and full of minute shells." But it was not _all_
ooze at the bottom of the sea, even on this telegraphic plateau. There
were hidden rocks--perhaps not cliffs and ledges, but at least scattered
boulders, lying on that mighty plain. Sometimes the strain on the
dynamometer would suddenly go up three or four tons, and then back
again, as if the grapnel had been caught and broken away. Once it came
up with two of its hooks bent, as if it had come in contact with a huge
rock. At one time it brought up in the mud a small stone half the size
of an almond; and at another a fragment as large as a brick. This was a
piece of granite.
Public-domain text, read in full here on John Shaqi.
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