Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 2 - By Alexander Von Humboldt And Aime Bonpland.
- Page 10 of 777 - First - Home
Whenever We Find
This Equilibrium Broken, It Will Be Well Rather To Examine Whether The
Rupture Be Not Owing To Causes Merely Local, And Of Very Recent Date,
Than To Admit An Uninterrupted Diminution Of The Water.
This reasoning
is conformable to the more circumspect method of modern science.
At a
time when the physical history of the world, traced by the genius of
some eloquent writers, borrowed all its charms from the fictions of
imagination, the phenomenon of which we are treating would have been
adduced as a new proof of the contrast these writers sought to
establish between the two continents. To demonstrate that America rose
later than Asia and Europe from the bosom of the waters, the lake of
Tacarigua would have been described as one of those interior basins
which have not yet become dry by the effects of slow and gradual
evaporation. I have no doubt that, in very remote times, the whole
valley, from the foot of the mountains of Cocuyza to those of Torito
and Nirgua, and from La Sierra de Mariara to the chain of Guigue, of
Guacimo, and La Palma, was filled with water. Everywhere the form of
the promontories, and their steep declivities, seem to indicate the
shore of an alpine lake, similar to those of Styria and Tyrol. The
same little helicites, the same valvatae, which now live in the lake
of Valencia, are found in layers of three or four feet thick as far
inland as Turmero and La Concesion near La Victoria.
Enter page number
PreviousNext
Page 10 of 777
Words from 2442 to 2696
of 211397