The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal lifeGrew, Edwin Sharpe
Science
The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal life
Grew, Edwin Sharpe
Geology; Paleontology
Every one who has been on a chalk cliff or hill has found, and
perhaps thrown, chalk flints. Flints are made of mineral called
silica, and very often these flints, or nodules of silica, surround
some organism like a sponge or a shell. During the formation of the
chalk the sea floor appears to have been covered at intervals by a
growth of sponges, which were composed of siliceous matter, and their
death and decay produced most of the flint. Sometimes flint is found
in bands, in which case it may have been deposited by siliceous water
trickling through fissures or cracks in the chalk.
In the sea which thus existed the Plesiosaurs and Ichthyosaurs still
pursued the even tenor of their way, growing larger and larger.
They were of many shapes, and probably of many habits. Some were
certainly fish-eaters, and with their enormous jaws must have been
most undesirable neighbours. Probably, however, they had plenty of
diversity in their lives, and may have had many a bitter struggle
with equally ferocious sea animals of other types. The scaly
saurians, for example, were beginning to come on; and began in
this era to assume the size and appearance that have occasionally
since been attributed to sea serpents. These reptiles, known as
_Dolichosaurs_, were long-necked, lizard-like reptiles in the
beginning of their career, and grew longer and longer in succeeding
generations, till at last their descendants were so long and snaky
that geologists have called the later specimens "serpents." These sea
serpents were from fifteen to forty-five feet in length, and their
remains have been found in the valley of the Meuse. They do not seem
to have had a very long career, for they do not appear after the
Chalk Age, and no direct descendants are known; but while they lived
they ranged from North and South America to Europe and New Zealand.
The first true sea turtles appeared and lived and extended their
families in great variety. They had broad flat forms, their shells
only just covering their ribs like a short Eton jacket; but they were
very large. The greatest of them, _Archelon_, had a skull larger than
that of a horse, and must have measured fully twelve feet across the
shell.
Public-domain text, read in full here on John Shaqi.
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