| 770 | 771 | 772 | 773 | 774 |
| 1 | 306 | 613 | 919 | 1225 |
|
allowed to the course of rivers in general, we shall find that the
Nile must have its mouth ten miles lower than its source. Again, we
see the Rhine, the Rhone and the Danube starting from the German
parts, almost the centre of Europe, and having a course one to the
East, the other to the North, and the last to Southern seas. And if
you consider all this you will see that the plains of Europe in
their aggregate are much higher than the high peaks of the maritime
mountains; think then how much their tops must be above the sea
shores.
Theory of the elevation of water within the mountains.
9
41.
OF THE HEAT THAT IS IN THE WORLD.
Where there is life there is heat, and where vital heat is, there is
movement of vapour. This is proved, inasmuch as we see that the
element of fire by its heat always draws to itself damp vapours and
thick mists as opaque clouds, which it raises from seas as well as
lakes and rivers and damp valleys; and these being drawn by degrees
as far as the cold region, the first portion stops, because heat and
moisture cannot exist with cold and dryness; and where the first
portion stops the rest settle, and thus one portion after another
being added, thick and dark clouds are formed. They are often wafted
about and borne by the winds from one region to another, where by
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