Franklin noticed many similarities between electricity and lightning.
For instance, both produced zigzag sparks, both were conducted by
metals, both set fire to inflammable materials, and both were capable
of killing animals. These resemblances appeared to him so striking that
he was convinced that the two were the same, and he resolved to put the
matter to the test. For this purpose he hit upon the idea of using a
kite, to the top of which was fixed a pointed wire. At the lower end of
the flying string was tied a key, insulated by a piece of silk ribbon.
In June 1752, Franklin flew his kite, and after waiting a while he
was rewarded by finding that when he brought his knuckle near to the
key a little spark made its appearance. This spark was exactly like
the sparks obtained from electrified bodies, but to make things quite
certain a Leyden jar was charged from the key. Various experiments were
then performed with the jar, and it was proved beyond all doubt that
lightning and electricity were one and the same.
Lightning is then an enormous electric spark between a cloud and the
Earth, or between two clouds, produced when opposite charges become so
strong that they are able to break down the intervening non-conducting
layer of air. The surface of the Earth is negatively electrified,
the electrification varying at different times and places; while the
electricity of the air is usually positive, but frequently changes to
negative in rainy weather and on other occasions. As the clouds float
about they collect the electricity from the air, and thus they may be
either positively or negatively electrified, so that a discharge may
take place between one cloud and another, as well as between a cloud
and the Earth.
Lightning flashes take different forms, the commonest being forked or
zigzag lightning, and sheet lightning. The zigzag form is due to the
discharge taking the easiest path, as in the case of the spark from
a Wimshurst machine. Sheet lightning is probably the reflection of a
flash taking place at a distance. It may be unaccompanied by thunder,
as in the so-called “summer lightning,” seen on the horizon at night,
which is the reflection of a storm too far off for the thunder to be
heard. A much rarer form is globular or ball lightning, in which the
discharge takes the shape of a ball of light, which moves slowly along
and finally disappears with a sudden explosion. The cause of this form
of lightning is not yet understood, but it is possible that the ball of
light consists of intensely heated and extremely minute fragments of
ordinary matter, torn off by the violence of the lightning discharge.
Another uncommon form is multiple lightning, which consists of a number
of separate parallel discharges having the appearance of a ribbon.
Public-domain text, read in full here on John Shaqi.
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