Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
Hence, it is impossible to deny, that the masses which now constitute
our highest mountains, have been originally in a liquid state; and
that they have for a long time been covered by waters in which
no living beings existed. Thus, it has not been only since the
appearance of life that changes have been operated in the nature of
the matters which have been deposited; for the masses formed previous
to that event, have varied, as well as those which have been formed
since. They have also experienced violent changes in their position,
and a part of these changes must have taken place at the period when
these masses existed by themselves, and were not covered over by
the shelly masses. The proof of this lies in the overturnings, the
disruptions, and the fissures, which are observable in their strata,
as well as in those of more recent formations, and which are in the
ancient strata even in greater number and better defined.
But these primitive masses have also undergone other revolutions
since the formation of the secondary strata, and have, perhaps,
given rise to, or at least have partaken of, some of those changes
which these strata themselves have experienced. There are actually
considerable portions of the primitive formations uncovered, although
placed in lower situations than many of the secondary formations;
and we cannot conceive how it should have so happened, unless the
primitive strata in those places had forced themselves into view,
after the secondary strata had been formed. In certain countries, we
find numerous large blocks of primitive substances scattered over
the surface of secondary formations, and separated by deep valleys,
or even by arms of the sea, from the peaks or ridges from which they
must have been derived. We must necessarily conclude, therefore,
either that these blocks have been ejected by eruptions, or that the
valleys (which must have stopped their course) did not exist at the
time of their being transported; or, lastly, that the motions of the
waters by which they were transported, exceeded in violence any thing
that we can imagine at the present day[6].
Here, therefore, we have a collection of facts, a series of epochs,
anterior to the present time, of which the successive steps may
be perfectly ascertained, although the duration of their intervals
cannot be defined with precision. They are so many fixed points,
which serve to regulate and direct our inquiries respecting this
ancient chronology.
_Examination of the Causes which act at present on the surface of the
Globe._
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account