The Rice belt journal. (Welsh, Calcasieu Parish, La.) 1900-19??, 1914-07-31

mine the rgldity of the earth are intensely Inter
esting. Science has long needed to know the
physical properties Of this globe. 1t is imposs
bic to learn this directly, as the deepest mines
yet sunk penetrate less than two miles below the
surface, distance proportionately no greater
than the thickness of the Varnsh on twofoot
globe. The interior of the earth is believed to
be intensely hot. This theory is based on the
fact that molten lava is thrown forth by eTuphng
volcanoes Also, in descending mine there is
rise in temperature, amounting to SO degrees per
mile of descent. If this rate of increase is con
slant the temperature at only 100 miles down is
above the melting point of all substances under
conditions as they exist on the surface of the
earth. However, despite the high temperature
the interior of the earth may be held IN solid
state by the tremendous pressure to which it is
subjected.
Under the now accepted theory Of the celestial
mechanics, scientists assume that a heavenly
body is held In its course by the attractive force
exepted by the other heavenly bodies on all sides
of IT, In this way is determined the earths
course around the sun and the motion of the
entire solar system through space. Assuming
that the earth Is not solid mass scientists have
long struggled to discover how it resisted the at
tractye forces exerted by other planets and stars
whether as ytscous mass or as a perfectly
elastic body
They have long known that the earth did re-
sist these forces in some degree The ocean
tides which sweep our shores twice daily are
proof Of this. It has long been known that the
tides are caused by the attraction of the sun and
the moon. If the earth offered no resistance to
this attraction. the whole earth would respond
quickly to lt and there would be no tides On
the other hand, If the earth were perfectly rigid
body II would resist this attraction completely.
and the tides would reach their maximum height
The amount that the tides fall short of their
theoretical maximum height would measure the
degree of rlgidty which the earth possesses
The next step was to determine the actual
height OF The tides. This long proved the STUN
bling block. II shore lines were perfectly straight
and the floor OF the ocean perfectly level, the
height of the tides could be measured directly;
but crooked shore lines and shelving beaches re.
slst the motion of the tides and make It impos-
sible to determine their height with the accuracy
demanded by science
Sir George Darwin made elaborate experiments
to determine the height OF the tides, but was
Obliged to give up the problem IN despair Pro
fessor Nicholson solved this difficulty by laying
two lengths Of pipe, each FIVE hundred feet long,
and measuring the rise and fall OF the water in
them One length of pipe was laid north and
south, and the other length east and west, In
order to measure the tides In both directions
The pipes we're buried six feet under ground to
obtain a uniform temperature
st both ends Of the pipes tees were inserted
having glass windows for observatory purposes
The pipes we're half filled with water; and the
changes in the height Of the water were obtained
hV measuring through Lnirrescope the distanna
between pointer inserted Just under the surface
Of the water and the image Of the pointer reflect
ca above the water