The Atlantic Monthly, Volume 12, No. 70, August, 1863: A Magazine of Literature, Art, and PoliticsVarious
History
The Atlantic Monthly, Volume 12, No. 70, August, 1863: A Magazine of Literature, Art, and Politics
Various
American periodicals
These Cretaceous beds were at first divided only into three sets, called
the Neocomian, or lower deposits, the Green-Sands, or middle deposits,
and the Chalk, or upper deposits. The Neocomian, the lower division, was
afterwards subdivided into three sets of beds, called the Lower, Middle,
and Upper Neocomian by some geologists, the Valengian, Neocomian, and
Urgonian by others. These three periods are not only traced in immediate
succession, one above another, in the transverse cut before described,
across the mountain of Chaumont, near Neufchatel, but they are also
traced almost on one level along the plain at the foot of the Jura. It
is evident that by some disturbance of the surface the eastern end of
the range was raised slightly, lifting the lower or Valengian deposits
out of the water, so that they remain uncovered, and the next set of
deposits, the Neocomian, is accumulated along their base, while these in
their turn are slightly raised, and the Urgonian beds are accumulated
against them a little lower down. They follow each other from east to
west in a narrower area, just as the Azoic, Silurian, and Devonian
deposits follow each other from north to south in the northern part of
the United States. The Cretaceous deposits have been intimately studied
in various localities by different geologists, and are now subdivided
into at least ten, or it may be fifteen or sixteen distinct periods, as
they stand at present. This is, however, but the beginning of the work;
and the recent investigations of the French geologist, Coquand, indicate
that several of these periods at least are susceptible of further
subdivision. I present here a table enumerating the periods of the
Cretaceous epoch best known at present, in their sequence, because I
want to show how sharply and in how arbitrary a manner, if I may so
express it, new forms are introduced. The names are simply derived from
the localities, or from some circumstances connected with the locality
where each period has been studied.
_Table of Periods in the Cretaceous Epoch._
Maestrichtian } Chalk.
Senonian }
Turonian } Chalk Marl.
Cenomanian }
Albian }
Aptian } Green Sands.
Rhodanian }
Urgonian }
Neocomian } Wealden.
Valengian }
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