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
In this period, which is called the Triassic (the name given to it
by the German geologist Bronn because of the three distinct beds
he found in it, though the middle of these, a shelly limestone,
does not exist in Great Britain), there was a wide development of
large reptiles and amphibians. We cannot enumerate them all, for
not one chapter nor one volume would suffice to deal adequately
with the reptiles of the Trias formations and of the Jurassic rocks
which followed them, and of the Permian which preceded them. But
we may speak of some of them. One of the most striking was the
_Pareiasaurus_, which has been found in the Jurassic sandstones and
limestones of South Africa, of Russia, of India and Scotland, and of
middle England. The skeleton of the Pareiasaurus looks like that of a
gigantic pug dog eight feet long; but it was a comparatively harmless
animal, the teeth of which show that it largely fed on vegetable food.
In Sir E. Ray Lankester's lectures on "Extinct Animals" he described
the finding of a great many of these fossil reptiles by Professor
Amalitzky on the banks of the River Dwina, near Archangel. There is a
cliff of Permian strata on the banks of the Dwina, and in this cliff
there is a peculiar pocket or accumulation of sandy matter with large
hard nodules embedded in it. These nodules are removed and broken up
for mending the roads. The pocket seems to be in a fissure and of
Triassic age, later, that is to say, than the Permian rocks on either
side of it. However that may be, the nodules are usually removed
for road-mending, and four or five years ago Professor Amalitzky on
visiting the spot was astounded and delighted to find that when
broken each nodule was seen to contain the skeleton or skull of
a great reptile. The Russian geologist determined to make a most
thorough investigation of this wonderful deposit, and for years spent
several thousand pounds in having the nodules dug out by the peasants
after the year's farming work was over, and in removing them to the
University of Warsaw, where with the finest instruments and greatest
care the nodules are opened, and each bone removed in fragments is
put together from its more or less broken parts, and firmly cemented
and set up in its natural position as a complete skeleton.
Public-domain text, read in full here on John Shaqi.
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