Curiosities of Science, Past and Present: A Book for Old and YoungTimbs, John
Science
Curiosities of Science, Past and Present: A Book for Old and Young
Timbs, John
Science
Soon after the completion of the Monument on Fish Street Hill, by Wren,
in 1677, it was used by Hooke and other members of the Royal Society
for astronomical purposes, but abandoned on account of the vibrations
being too great for the nicety required in their observations. Hence
arose _the report that the Monument was unsafe_, which has been revived
in our time; “but,” says Elmes, “its scientific construction may bid
defiance to the attacks of all but earthquakes for centuries to come.”
This vibration in lofty columns is not uncommon. Captain Smythe, in his
_Cycle of Celestial Objects_, tells us, that when taking observations
on the summit of Pompey’s Pillar, near Alexandria, the mercury was
sensibly affected by tremor, although the pillar is a solid.
Geology and Paleontology.
IDENTITY OF ASTRONOMY AND GEOLOGY.
While the Astronomer is studying the form and condition and structure
of the planets, in so far as the eye and the telescope can aid him, the
Geologist is investigating the form and condition and structure of the
planet to which he belongs; and it is from the analogy of the earth’s
structure, as thus ascertained, that the astronomer is enabled to form
any rational conjecture respecting the nature and constitution of the
other planetary bodies. Astronomy and Geology, therefore, constitute
the same science--the science of material or inorganic nature.
When the astronomer first surveys the _concavity_ of the celestial
vault, he finds it studded with luminous bodies differing in magnitude
and lustre, some moving to the east and others to the west; while by
far the greater number seem fixed in space; and it is the business of
astronomers to assign to each of them its proper place and sphere, to
determine their true distance from the earth, and to arrange them in
systems throughout the regions of sidereal space.
In like manner, when the geologist surveys the _convexity_ of his
own globe, he finds its solid covering composed of rocks and beds of
all shapes and kinds, lying at every possible angle, occupying every
possible position, and all of them, generally speaking, at the same
distance from the earth’s centre. Every where we see what was deep
brought into visible relation with what was superficial--what is old
with what is new--what preceded life with what followed it.
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