Base-ball : $b How to become a player, with the origin, history and explanation of the gameWard, John Montgomery
History
Base-ball : $b How to become a player, with the origin, history and explanation of the game
Ward, John Montgomery
Baseball
The discovery of the curve itself was purely an accident. During the
years from 1866 to 1869 the theory was held by many pitchers that the
more twist imparted to a pitched ball, the more difficult it would be to
hit it straight out. It was thought that even if it were struck fairly,
this twist would throw it off at an angle to the swing of the bat. One
writer on the game declared strongly against this practice of the
pitchers on the ground that, though this twist did do all that was
claimed for it, it at the same time caused the ball, when hit, to bound
badly, and thus interfered with good fielding. Of course, both of these
theories become absurd in the light of the present, but it was doubtless
the belief in the former that led to the introduction of the curve. In
1869 Arthur Cummings, pitching for the Star Club, noticed that by giving
a certain twist to the ball it was made to describe a rising, outward
curve, and his remarkable success with the new delivery soon led to its
imitation by other pitchers, and finally to the general introduction of
curve pitching.
The philosophy of the curve is, in itself, quite simple. A ball is
thrown through the air and, at the same time, given a rotary motion upon
its own axis, so that the resistance of the air, to its forward motion,
is greater upon one point than upon another, and the result is a
movement of the ball away from the retarded side. Suppose the ball in
the accompanying cut to be moving in the direction of the arrow, B C, at
the rate of 100 feet per second. Suppose, also, that it is rotating
about its vertical axis, E, in the direction of I to H, so that any
point on its circumference, I H D, is moving at the same rate of 100
feet per second. The point I is, therefore, moving forward at the same
rate as the ball's centre of gravity, that is, 100 feet per second, plus
the rate of its own revolution, which is 100 feet more, or 200 feet per
second; but the point D, though moving forward with the ball at the rate
of 100 feet per second, is moving backward the rate of rotation, which
is 100 feet per second, so that the forward motion of the point D is
practically zero. At the point I, therefore, the resistance is to a
point moving 200 feet per second, while at D it is zero, and the
tendency of the ball being to avoid the greatest resistance, it is
deflected in the direction of F.
In the Scientific American of August 28th, 1886, a correspondent gave a
very explicit demonstration of the theory of the curve, and, as it has
the virtue of being more scientific than the one given above, I append
it in full.
Public-domain text, read in full here on John Shaqi.
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