Appletons' Popular Science Monthly, February 1900: Vol. 56, November, 1899 to April, 1900Various
Science
Appletons' Popular Science Monthly, February 1900: Vol. 56, November, 1899 to April, 1900
Various
Science -- Periodicals; Technology -- Periodicals
These conclusions are not reached by physical reasonings alone, but are
also confirmed by experimental investigations. For example, a plumb
line on the plains of India is deflected indeed toward the Himalayas,
as it ought to be, but much less than it would be if the mountain and
sub-mountain mass were not less dense and the sub-oceanic material
more dense than the average.[G] Again, gravitative determinations by
pendulum oscillations, undertaken by the United States along a line
from the Atlantic shore to Salt Lake City, show that the largest
inequalities, such as the Appalachian bulge, the Mississippi-basin
hollow, and the Rocky Mountain bulge, are in gravitative
equilibrium--i. e., the mountain and sub-mountain material is as much
lighter as the mountain region is higher than the Mississippi-basin
region.
[G] Pratt, Philosophical Magazine, vol. ix, p. 231, 1855; vol.
x, p. 340, 1855; vol. xvi, p. 401, 1858.
Now, so sensitive is the earth to changes of gravity that, given time
enough, it responds to increase or decrease of pressure over large
areas by corresponding subsidence or elevation. Hence, all places where
great accumulations of sediment are going on are sinking under the
increased weight, and, contrarily, all places where excessive erosion
is going on, as, for example, on high plateaus and great mountain
ranges, are rising by relief of pressure.
This principle of isostasy is undoubtedly a valuable one, which must be
borne in mind in all our reasonings on crust movements, although its
importance has been exaggerated by some enthusiastic supporters. Its
greatest importance is not as a cause _initiating_ crust movements or
determining the features of the earth, but rather as conditioning and
modifying the results produced by other causes. The idea belongs wholly
to the latter half of the present century. Commencing about 1840, it
has grown in clearness and importance to the present time.
[_To be concluded._]
THE APPLICATIONS OF EXPLOSIVES.
BY CHARLES E. MUNROE,
PROFESSOR OF CHEMISTRY, COLUMBIAN UNIVERSITY.
[_Concluded._]
[Illustration: GUN COTTON SHELL AFTER IMPACT.]
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