A Manual of Elementary Geology: or, The Ancient Changes of the Earth and its Inhabitants as Illustrated by Geological MonumentsLyell, Charles, Sir
Science
A Manual of Elementary Geology: or, The Ancient Changes of the Earth and its Inhabitants as Illustrated by Geological Monuments
Lyell, Charles, Sir
Geology
_floetz_, or "a level floor;" and every deposit more modern than the chalk,
which was classed as the uppermost of the floetz series, was designated "the
overflowed land," an expression which may be regarded as equivalent to
alluvium, although under this appellation were confounded all the strata
afterwards called tertiary, of which Werner had scarcely any knowledge. As
the followers of Werner soon discovered that the inclined position of the
"transition beds," and the horizontality of the floetz, or newer
fossiliferous strata, were mere local accidents, they soon abandoned the
term floetz; and the four divisions of the Wernerian school were then named
primitive, transition, secondary, and alluvial.
As to the trappean rocks, although their igneous origin had been already
demonstrated by Arduino, Fortis, Faujas, and others, and especially by
Desmarest, they were all regarded by Werner as aqueous, and as mere
subordinate members of the secondary series.[91-A]
This theory of Werner's was called the "Neptunian," and for many years
enjoyed much popularity. It assumed that the globe had been at first
invested by an universal chaotic ocean, holding the materials of all rocks
in solution. From the waters of this ocean, granite, gneiss, and other
crystalline formations, were first precipitated; and afterwards, when the
waters were purged of these ingredients, and more nearly resembled those of
our actual seas, the transition strata were deposited. These were of a
mixed character, not purely chemical, because the waves and currents had
already begun to wear down solid land, and to give rise to pebbles, sand,
and mud; nor entirely without fossils, because a few of the first marine
animals had begun to exist. After this period, the secondary formations
were accumulated in waters resembling those of the present ocean, except at
certain intervals, when, from causes wholly unexplained, a partial
recurrence of the "chaotic fluid" took place, during which various trap
rocks, some highly crystalline, were formed. This arbitrary hypothesis
rejected all intervention of igneous agency, volcanos being regarded as
modern, partial, and superficial accidents, of trifling account among the
great causes which have modified the external structure of the globe.
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