The Clarksburg telegram. [volume] (Clarksburg, W. Va.) 1874-1926, 1901-10-25
DEEP SEA CURRENTS.
nysTER,es or THE OCEAN THAT
HAVE PUZZLED THE SCIENTISTS

NANAAN wv
For more than a century scientists
and philosophers have been vainly try.
ing to discover the origin and cause Of
the mysterious current in the Atlantic
ocean called the gulf stream. Why 50
called is not apparent, as nothing in
the gulf OF Mexico is in its composition.
There have been many theories. which
have been abandoned, some perfectly
absurd. such as It's being caused by the
garth in It's revolution on Its axis. Tor
IL II had the power TO draw this stream
NJ the rate OF tive miles an hour from
the coast OF Florida It would draw all
the water from the east coasts OF
North and South America at the same
velocity. The prevailing theory is that
,he northeast trade winds drive q cur.
rent into the Caribbean sea and, aided
Inv the feeble equatorial stream, heap
mn the water in the gulf OF Mexico,
thence rushing around the south OF
Florida from the source OF the gun
stream. But there is no such heap
ING OF the waters In that gulf. The
waters there. ARE sluggish, and there Is
no perceutible current leading toward
the gulf stream or anywhere else.
This theory has been accepted for
want OF better, but those who favor
II are not entirely satisfied with II. The
gulf stream is an independent body oil
water, having no connection with the
water around or behind the point
where 1t energies 1t is warmer and
Of n deeper blue than the surrounding
seas md gushes forth from the start.
ing poiut on Cape Sable at the rate OF
from five to six kuots an hour, with
a temperature of about 90 degrees
lessening gradually as it proceeds on
It's tourney Of thousands of-miles across
the Atlantic ocean, warming the west
ern shores OF Europe.
Having seen the fallacy Of the the
cries concerning the gulf stream, We
will turn our attention to the great Pa
cIfic current, identical in all respects
with its sister current OF the Atlantic
and concerning which there are no the
cries to contend with.
1t starts spontaneously from spot n
few miles from the south end OF the
island of Formosa, in the Banshee
channel, following the coast OF For
mosa northeasterly, past and through
the Loochoo Islands. skirting the coast
of Japan; thence turns eastward on It's
long Journey across the wide Pacific,
warming the coast of America from
Puget sound to Mexico. Its dark blue
waters are In striking CONTRAST TO the
surrounding seas, giving II the name OF
Murra Suar, or black water. 1t Is an
independent stream where no combina-
ton OF winds or currents can possibly
cause the mighty rush OF warm blue
water with a velocity Of from five 10
six knots an hour from the start.
In it's characteristics of heat, color
and direction it resembles the gulf
stream in every particular. and the
origin of the two streams must be the
same, whatever they may be, which /
shall endeavor to show later on. There
is another ocean current similar in all
respects to the other two, with the ex.
ception that 1t runs in an exactly op-
posIte direction. Starting from the vi
cinity of the south end of the island OF
Madagascar, 1t runs sOuthwesterly
around the Cape of Good Hope, where
It disappears off Cape Lagullas. As a
current, probably part Of 1t Is diverted
into steady set of the eastern current,
caused by the prevailing westerly
winds in that region. No scientists, 81
far as am aware, have attempted to
account for this current. Having now
proved beyond refutation that all the
cries advanced as to the cause of ocean
currents are groundless, it remains to
be proved what the true cause Is.
It must be admitted that the currents
have a similar origin, as they are iden-
teal in every respect as regards color.
heat and velocity, sprInEIuR forth In
the same manner spontaneously from
the earth In some mysterious way.
There Is no place on the surface of the
earth where the water can be heated
to furnish the heat contained in these
streams that gush forth from the
depths OF the sea; consequently the
forces must be subterranean and can
only be accounted for by large bodies
OF clear, blue water from the ocean
forcing. It's way Into the depths Of the
earth under its crust, where It burrows
a channel Of its own to the surface
again, having received itB warmth on
the way by contact with the Internal
heat of the lower regions Of the earth,
forced on by continual pressure from
behind.
That there are orihces in the earth's
crust cannot be denied. also what be-
comes of the vast volume of water that
cannot be computed which is constant.
" running at the rate Of from four to
six knots an hour from the Atlantic
ocean, through the strait OF Gibraltar
into the Mediterranean sea. The nu-
merous rivers. too, are continually
howing in. and yet the sea remains at
the same level. Evaporation cannot
account for, II, for what Is eVaporated
is formed into clouds and is precipltat-
ed again into the sea by the medium Of
storms and frequent rains.
/, The water must enter the earth from
the ocean through these apertures on
an tIncllne as 1t gushes forth IN these
three mighty currents and cannot be
discovered by soundIngs; consequently
these three mighty currents are moth