The Medals of Creation, Volumes 1 and 2: First Lessons in Geology and the Study of Organic RemainsMantell, Gideon Algernon
Science
The Medals of Creation, Volumes 1 and 2: First Lessons in Geology and the Study of Organic Remains
Mantell, Gideon Algernon
Geology -- England -- Guidebooks; Paleontology
By a reference to the geological map of England (_Wond._ pl. i.
vol. i.), it will be seen, that the several formations appear on
the surface in a somewhat chronological order, as we pass from the
eastern or south-eastern part of the Island to the west or north-west.
Thus the principal Tertiary deposits are situated in the eastern
and south-eastern parts; and proceeding towards the north-west, we
traverse successively the _Secondary_--the _Chalk_, _Oolite_, _Lias_
and _Trias_; then the _Palæozoic_--_Permian_, _Carboniferous_,
and _Devonian_; next the _Silurian_ and _Cambrian_; and at length
_metamorphic_ and _primary_ rocks appear. It is this distribution
of the strata of the respective formations that has determined
the characters of the physical geography of England. The Alpine or
mountainous districts, which extend north and south along the western
portion of England and Wales, from Cornwall to Cumberland, are formed
by the elevated masses of the Silurian, Cambrian, and Metamorphic
rocks. These are succeeded by a band of the Carboniferous and Triassic
deposits, with a few intrusions of metamorphic and plutonic rocks, that
stretches from the coast of Devonshire, through the midland counties,
by Leicestershire and Derbyshire, to Newcastle. On the south-east
of this tract, the Oolite and Cretaceous formations, chiefly made
up of argillaceous and calcareous strata, constitute a diversified
agricultural district, extending from the southern shores of Hants and
Dorset to the coast of Yorkshire. The Wealden occupies the country
lying between the Chalk Downs of Sussex, Hants, Surrey, and Kent. The
Tertiary deposits lie in basins or depressions of the upper cretaceous
rocks in the south-eastern and eastern maritime districts, and on an
extensive area of these beds stands the metropolis of England; lastly,
irregular accumulations of Drift, containing mammalian remains in some
localities, are spread over the surface of the ancient formations, and
form the immediate subsoil of the most fertile regions.
CHAPTER III.
ON THE NATURE OF FOSSILS, OR ORGANIC REMAINS.
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