bottle. This mist is composed of water-drops, drawn out of the
air of the room, because the cold glass chilled the air all round
it, so that it gave up its invisible water to form dew-drops.
Just in this same way the cold blades of grass chill the air
lying above them, and steal its vapour.

But try the experiment, some night when a heavy dew is expected,
of spreading a thin piece of muslin over some part of the grass,
supporting it at the four corners with pieces of stick so that it
forms an awning. Though there may be plenty of dew on the grass
all round, yet under this awning you will find scarcely any. The
reason of this is that the muslin checks the heat-waves as they
rise from the grass, and so the grass-blades are not chilled
enough to draw together the water-drops on their surface. If you
walk out early in the summer mornings and look at the fine cobwebs
flung across the hedges, you will see plenty of drops on the
cobwebs themselves sparkling like diamonds; but underneath on the
leaves there will be none, for even the delicate cobweb has been
strong enough to shut in the heat-waves and keep the leaves warm.

Again, if you walk off the grass on to the gravel path, you find
no dew there. Why is this? Because the stones of the gravel can
draw up heat from the earth below as fast as they give it out,
and so they are never cold enough to chill the air which touches
them. On a cloudy night also you will often find little or no dew
even on the grass. The reason of this is that the clouds give
back heat to the earth, and so the grass does not become chilled
enough to draw the water-drops together on its surface. But after
a hot, dry day, when the plants are thirsty and there is little
hope of rain to refresh them, then they are able in the evening