or 80 deg.below the freezing point.
The cause of this absolute dependence of terrestrial temperatures upon density of the air-envelope is seldom discussed in text-books either of geography or of physics, and there seems to be still some uncertainty about it.

Some impute it wholly to the thinner air being unable to absorb and retain so much heat as that which is more dense; but if this were the case the soil at great altitudes not having so much of its heat taken up by the air should be warmer than below, since it undoubtedly _receives_ more heat owing to the greater transparency of the air above it; but it certainly does not become warmer.

The more correct view seems to be that the loss of heat by radiation is increased so much through the rarity of the air above it as to _more_ than counterbalance the increased insolation, so that though the surface of the earth at a given altitude may receive 10 per cent.

more direct sun-heat it loses by direct radiation, combined with diminished air and cloud-radiation, perhaps 20 or 25 per cent.

more, whence there is a resultant cooling effect of 10 or 15 per cent.