Geological facts; or, the crust of the earth, what it is, and what are its usesBarrett, W. G. (William Garland)
Religion
Geological facts; or, the crust of the earth, what it is, and what are its uses
Barrett, W. G. (William Garland)
Geology
The probable size of the Iguanodon was thirty feet in length, though
probably some exceeded these enormous proportions. Seventy species have
been discovered in the quarries opened at Tilgate forest; and this gives
us some idea of the conspicuous part these mighty creatures once played
in the eras happily before man was an inhabitant of this planet. Why
these remains should generally be found in the same locality we cannot
certainly tell, though the previous extract from Alison may shed some
light on this curious fact; but it appears beyond doubt that particular
spots were selected by these beasts as hospitals and dying places,
where, undisturbed by their enemies, they retired to die unseen.
The drawing on page 195, representing the restored fauna of this period,
that is, inclusive of the Lias, Oolite, and Wealden formations, will not
only illustrate our previous remarks, but enable our readers thoroughly
to appreciate the following vivid description of the life of that remote
era, which we do not like to abridge. Should any feel sceptical as to
whether there were ever such “goings on” in this globe of ours,
especially in our eastern counties, now the resort of tourists and
invalids having no dread of such creatures before their eyes, we ask
them not to reject all this as fable until they have gone to the British
Museum, and in Room 3, and in Wall-case C, they will there see some of
the magnificent specimens, obtained by Dr. Mantell, of these extinct
deinosaurians.[102] On reading this description, it seems quite
justifiable to congratulate ourselves upon the era in which we live.
Strange forms and monsters vast have been in the old time before us, and
their disinterred remains teach us again and again the good and
wholesome lesson of the king of Israel, prefixed as a motto to this
chapter.
“Two of these saurians have more especially attracted attention, in
consequence of their great abundance in a fossil state in our own
country, but they are by no means the only ones known. Of these two, one
was more exclusively a tenant of the deep, while the other was probably
more frequently met with on the mud banks or on the shore. Both were
truly marine in their habits, and both seem to have served as the
representatives of the great Cetacean tribe—the whales, the porpoises,
and other similar animals now existing.
“It is not easy to imagine the conditions of existence of such animals.
We know their form, their proportions, their strange contrivances of
structure, their very skin, and the nature of the food which they
devoured; and yet, knowing with absolute certainty these points, we
hardly dare draw the conclusions which are suggested. I will, however,
venture to offer a sketch of the appearance of the sea and its
inhabitants during this portion of the Reptilian epoch.
Public-domain text, read in full here on John Shaqi.
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