OF WHAT IS WATER.

Among the four elements water is the second both in weight and in
instability.

932.

THE BEGINNING OF THE BOOK ON WATER.

Sea is the name given to that water which is wide and deep, in which
the waters have not much motion.

[Footnote: Only the beginning of this passage is here given, the
remainder consists of definitions which have no direct bearing on
the subject.]

Of the surface of the water in relation to the globe (933-936).

933.

The centres of the sphere of water are two, one universal and common
to all water, the other particular. The universal one is that which
is common to all waters not in motion, which exist in great
quantities. As canals, ditches, ponds, fountains, wells, dead
rivers, lakes, stagnant pools and seas, which, although they are at
various levels, have each in itself the limits of their superficies
equally distant from the centre of the earth, such as lakes placed
at the tops of high mountains; as the lake near Pietra Pana and the
lake of the Sybil near Norcia; and all the lakes that give rise to
great rivers, as the Ticino from Lago Maggiore, the Adda from the
lake of Como, the Mincio from the lake of Garda, the Rhine from the
lakes of Constance and of Chur, and from the lake of Lucerne, like
the Tigris which passes through Asia Minor carrying with it the
waters of three lakes, one above the other at different heights of
which the highest is Munace, the middle one Pallas, and the lowest
Triton; the Nile again flows from three very high lakes in Ethiopia.

[Footnote 5: _Pietra Pana_, a mountain near Florence. If for Norcia,
we may read Norchia, the remains of the Etruscan city near Viterbo,
there can be no doubt that by '_Lago della Sibilla_'--a name not
known elsewhere, so far as I can learn--Leonardo meant _Lago di
Vico_ (Lacus Ciminus, Aen. 7).]

934.

OF THE CENTRE OF THE OCEAN.

The centre of the sphere of waters is the true centre of the globe
of our world, which is composed of water and earth, having the shape
of a sphere. But, if you want to find the centre of the element of
the earth, this is placed at a point equidistant from the surface of
the ocean, and not equidistant from the surface of the earth; for it
is evident that this globe of earth has nowhere any perfect
rotundity, excepting in places where the sea is, or marshes or other
still waters. And every part of the earth that rises above the water
is farther from the centre.

935.

OF THE SEA WHICH CHANGES THE WEIGHT OF THE EARTH.

The shells, oysters, and other similar animals, which originate in
sea-mud, bear witness to the changes of the earth round the centre
of our elements. This is proved thus: Great rivers always run
turbid, being coloured by the earth, which is stirred by the
friction of their waters at the bottom and on their shores; and this
wearing disturbs the face of the strata made by the layers of
shells, which lie on the surface of the marine mud, and which were
produced there when the salt waters covered them; and these strata
were covered over again from time to time, with mud of various
thickness, or carried down to the sea by the rivers and floods of
more or less extent; and thus these layers of mud became raised to
such a height, that they came up from the bottom to the air. At the
present time these bottoms are so high that they form hills or high
mountains, and the rivers, which wear away the sides of these
mountains, uncover the strata of these shells, and thus the softened
side of the earth continually rises and the antipodes sink closer to
the centre of the earth, and the ancient bottoms of the seas have
become mountain ridges.

936.

Let the earth make whatever changes it may in its weight, the
surface of the sphere of waters can never vary in its equal distance
from the centre of the world.

Of the proportion of the mass of water to that of the earth (937.
938).

937.

WHETHER THE EARTH IS LESS THAN THE WATER.

Some assert that it is true that the earth, which is not covered by
water is much less than that covered by water. But considering the
size of 7000 miles in diameter which is that of this earth, we may
conclude the water to be of small depth.

938.



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