Capitolo 38
external crust of this the particular one of the one small planet of ours. While the
astronomers went in for the evolution of solos, stars and worlds, Lyell
and his/her brothers geologic it went in for the evolution of the earth
surface. As theirs was stellar, so his was worldly. If the world started
being an incandescent mass of the planetary matter in a tall state of inside
excitement, boiling and dancing with the heat of his/her emotions it,
gradually him cooled with age and it experiments, for old increasing it is
increasing cold as every one of us in duration, alas, it discovers. As it passed
from his/her ardent and volcanic youth to his/her staider and soberer middle age,
a solid crust started to form in way clouded on its surface of cooling.
The aqueous vapor around which as vapor had been floating for first its heated
mass condensed with time in a wide ocean on the hull now hardened.
This ocean gradually moved its mass in two or three principal bodies that
sunk in it digs some crust of viscid the precursors of Atlantic,,
Pacific and the Indian Seas. Wrinklings of the crust, produced from the
refreshing and consequent contraction, produced before mountain of child for
series, and later to the more first raw draughts of the he/she anchors a lot
vague and rough continents. The world grew daily more complex and more
different; it advanced, in agreement with the law of Spencerian, from the
homogeneous to the heterogeneous one, and so before, as aforesaid, with
delicious regularity.
Finally, from long changes and graduates, seas and earths, peninsulas and
islands, lakes and rivers, hills and mountains were beaten out of
inside or external energies on the crust so generally shaped.
Evaporation from the oceans produced clouds and rain and hailstorms;
the water that is fallen on the mountain overcomes cut out the valleys and river
basins; brooks gathered in brooks, brooks in brooks the brooks in
primaeval Nile and Horsewoman and Mississippis. Volcanic strengths lifted
here an Alpine chain, or depressed there a deep-sea cable. Sediment