The East is old, old! the West, with the exception of the Rocky
Mountains, is of yesterday in comparison. The Hudson was an ancient
river before the Mississippi was born, and the Catskills were being
slowly carved from a vast plateau while the rocks that were to form
many of the Western ranges were being laid down as sediment in the
bottom of the sea. California is yet in her teens, while New England
in comparison is an octogenarian. Just as much geology in the East
as in the West, did I say? Not as much visible geology, not as much
by many chapters of earth history, not as much by all the later
formations, by most of the Mesozoic and Tertiary deposits. The vast
series of sedimentary rocks since the Carboniferous age, to say
nothing of the volcanic, that make up these periods, are largely
wanting east of the Mississippi, except in New Jersey and in some of
the Gulf States. They are recent. They are like the history of our
own period compared with that of Egypt and Judea. It is mainly these
later formations--the Permian, the Jurassic, the Triassic, the
Cretaceous, the Eocene,--that give the prevailing features to the
South-western landscape that so astonish Eastern eyes. From them
come most of the petrified remains of that great army of extinct
reptiles and mammals--the three-toed horse, the sabre-toothed
tiger, the brontosaurus, the fin-backed lizard, the imperial
mammoth, the various dinosaurs, some of them gigantic in form and
fearful in aspect--that of late years have appeared in our museums
and that throw so much light upon the history of the animal life of
the globe. Most of the sedimentary rocks of New York and New England
were laid down before these creatures existed.
Now I am not going to write an essay on the geology of the West, for
I really have little first-hand knowledge upon that subject, but I
would indicate the kind of interest in the country I was most
conscious of during my recent trip to the Pacific Coast and beyond.
Indeed, quite a geologic fever raged in me most of the time. The
rocks attracted me more than the birds, the sculpturing of the
landscapes engaged my attention more than the improvements of the
farms--what Nature had done more than what man was doing. The purely
scenic aspects of the country are certainly remarkable, and the
human aspects interesting, but underneath these things, and striking
through them, lies a vast world of time and change that to me is
still more remarkable, and still more interesting. I could not look
out of the car windows without seeing the spectre of geologic time
stalking across the hills and plains.
Public-domain text, read in full here on John Shaqi.
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