Dinosaurs, with Special Reference to the American Museum CollectionsMatthew, William Diller
Science
Dinosaurs, with Special Reference to the American Museum Collections
Matthew, William Diller
Dinosaurs
Aroused from sleep on a clear evening in camp by the heavy rumble of
a passing Union Pacific freight-train[21], I shall never forget my
meditations on the contrast between the imaginary picture of the great
Age of Dinosaurs, fertile in cycads and in a wonderful variety of
reptiles, and the present age of steam, of heavy locomotives toiling
through the semi-arid and partly desert Laramie Plains.
So many animals had already been removed from these bluffs that we
were not very sanguine of finding more; but after a fortnight our
prospecting was rewarded by finding parts of skeletons of the
long-limbed dinosaur _Diplodocus_ and of the heavy-limbed dinosaur
_Brontosaurus_. The whole summer was occupied in taking these animals
out for shipment to the East, the so-called "plaster method" of
removal being applied with the greatest success. Briefly, this is a
surgical device applied on a large scale for the "setting" of the
much-fractured bones of a fossilized skeleton. It consists in setting
great blocks of the skeleton, stone and all, in a firm capsule of
plaster subsequently reinforced by great splints of wood, firmly drawn
together with wet rawhide. The object is to keep all the fragments and
splinters of bone together until it can reach the skilful hands of the
museum preparator.
_The Rock Waves Connecting the Bluffs and the Quarry._ The Como Bluffs
are about ten miles south of the Bone-Cabin Quarry; between them is a
broad stretch of the Laramie Plains. The exposed bone layer in the two
localities is of the same age, and originally was a continuous level
stratum which may be designated as the "dinosaur beds;" but this
stratum, disturbed and crowded by the uplifting of the not far-distant
Laramie range of mountains and the Freeze Out Hills, was thrown into a
number of great folds or rock waves. Large portions, especially of the
upfolds, or "anticlines," of the waves, have been subsequently removed
by erosion; the edges of these upfolds have been exposed, thus
weathering out their fossilized contents, while downfolds are still
buried beneath the earth for the explorers of coming centuries.
Public-domain text, read in full here on John Shaqi.
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