Alexandria gazette. [volume] (Alexandria, D.C.) 1834-1974, 1901-10-29
DEEHsEA CURRENTS.
MYSTERIES or TIE OCEAN THAT
HAVE PUZZLED THz SCIENTISTS.
A Theory ss,ep ne ostetn and canse
of the c. u aud Other streams-Are
+ They the Product of Immense Sub
martne 0eysersf


They the Product of fmmenss sud-
marine Geysersf
For more than century scian1sts
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 30
called is not apparent as nothing In
fhe gulf OF Mexico is in It's composition.
There have been many theories, which
have been abandoned, some perfectly
absurd, such as It's being caused by the
earth In its revolution on It's axis, for
If It had the power to draw this stream
at the rate of Eve 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
the northeast trade winds drive cur
rent into the Caribbean sea and, aided
by the feeble equatorial stream, heap
ND the water In the gulf Of Mexico,
thence rushing arornd the south OF
Florida from the source Of the gulf
stream. But there is no such heap
ing Of the waters In that gulf. The
waters there are sluggish, and there 10
no perceptible current leading toward
the gulf stream or anywhere else.
This theory has been accepted for
want Of q better, but those who favor
II are not entirely satisfied with it The
gulf stream is an independent body OF
water, having no connection with the
water around or behind the point
where It energies. 1t is warmer and
OF q deeper blue than the surrounding
seap and gushes forth from the start
ing point off Cape Sable at the rate OF
from five to six kuots an hour, with
n temperature Of about 80 degrees,
lessenlng gradually as it proceeds on
its Journey 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
win turn our attention to the great Pa
clfc 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
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 Its
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 1t 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 I'VE TO
six knots an hour from the start.
In its characteristics Of neat, color
and direction It resembles the gulf
stream in every particular, and the
origin Of the two streams must DO 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 OPP
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 of Cape Lagullas. AS a
current, probably part Of 1t is diverted
into a steady set Of the eastern current.
caused by the prevailing westerly
winds In that region. No scientists, so
far as am aware, have attempted to
account for this current Having now
proved beyond REPUTATION that all the
cries advanced as to the cause Of ocean
currents are groundless, II remains to
be proved what the true cause Is.
II must be admitted that the currents
have a similar origin. as they are iden-
teal in every respect as regards color,
heat and velocity, springing 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 its way into the depths Of the
earth under Its crust, where 1t burrows
q channel Of It's own to the surface
again, having received its 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 orifces 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
ly 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
flowing In. and yet the sea remains at
the same level. Evaporation cannot
account for 1t, for what is evaperated
is formed into clouds and is precipitat-
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 incline as II gusbes forth in these
49, ,,otxbtry o,,rrauf0 and caOnOt ha