surindas in diameter. They grew upon the margins of vast stagnant lakes which I was compelled to navigate by means of rude rafts made from their trunks lashed together with vines.
In the fauna of the region that I had traversed I had noted changes corresponding to those in the flora. On the upper slope there was nothing but the mountain sheep, but I passed successively through the habitats of the bear, the deer and the horse. This last mentioned creature, which our naturalists have believed long extinct, and which Dorbley declares our ancestors domesticated, I found in vast numbers on high table lands covered with grass upon which it feeds. The animal answers the current description of the horse very nearly, but all that I saw were destitute of the horns, and none had the characteristic forked tail. This member, on the contrary, is a tassel of straight wiry hair, reaching nearly to the ground—a surprising sight. Lower still I came upon the mastodon, the lion, the tiger, hippopotamus and alligator, all differing very little from those infesting Central Europe, as described in my “Travels in the Forgotten Continent.”
In the lake region where I now found myself, the waters abounded with ichthyosauri, and along the margins the iguanodon dragged his obscene bulk in indolent immunity. Great flocks of pterodactyls, their bodies as large as those of oxen and their necks enormously long, clamored and fought in the air, the broad membranes of their wings making a singular musical humming, unlike anything that I had ever heard. Between them and the ichthyosauri there was incessant battle, and I was constantly reminded of the ancient poet’s splendid and original comparison of man to dragons of the prime
That tare each other in their slime.
When brought down with my electric rifle and properly roasted, the pterodactyl proved very good eating, particularly the pads of the toes.
In urging my raft along the shore line of one of the stagnant lagoons one day I was surprised to find a broad rock jutting out from the shore, its upper surface some ten coprets above the water. Disembarking, I ascended it, and on examination recognized it as the remnant of an immense mountain which at one time must have been 5,000 coprets in height and doubtless the dominating peak of a long range. From the striations all over it I discovered that it had been worn away to its present trivial size by glacial action. Opening my case of instruments, I took out my petrochronologue and applied it to the worn and scratched surface of the rock. The indicator at once pointed to K 59 xpc 1/2! At this astonishing result I was nearly overcome by excitement: the last erosions of the ice-masses upon this vestige of a stupendous mountain range which they had worn away, had been made as recently as the year 1945! Hastily applying my nymograph, I found that the name of this particular mountain at the time when it began to be enveloped in the mass of ice moving down upon it from the north, was “Pike’s Peak.” Other observations with other instruments showed that at that time the country circumjacent to it had been inhabited by a partly civilized race of people known as Galoots, the name of their capital city being Denver.
That evening at the hour of 23 I set up my aerial isochronophone[3] and reported to his gracious Majesty the Ahkoond as follows: [3] This satire was published in the San Francisco Examiner many years before the invention of wireless telegraphy; so I retain my own name for the instrument.—A.B.
“Sire: I have the honor to report that I have made a startling discovery. The primeval region into which I have penetrated, as I informed you yesterday—the ichthyosaurus belt—was peopled by tribes considerably advanced in some of the arts almost within historic times: in 1920. They were exterminated by a glacial period not exceeding one hundred and twenty-five years in duration. Your Majesty can conceive the magnitude and violence of the natural forces which overwhelmed their country with moving sheets of ice not less that 5,000 coprets in thickness, grinding down every eminence, destroying (of course) all animal and vegetable life and leaving the region a fathomless bog of detritus. Out of this vast sea of mud Nature has had to evolve another creation, beginning de novo, with her lowest forms. It has long been known, your Majesty, that the region east of the Ultimate Hills, betwen them and the Wintry Sea, was once the seat of an ancient civilization, some scraps and shreds of whose history, arts and literature have been wafted to us across the gulf of time; but it was reserved for your gracious Majesty, through me, your humble and unworthy instrument, to ascertain the astonishing fact that these were a pre-glacial people—that between them and us stands, as it were, a wall of impenetrable ice. That all local records of this unfortunate race have perished your Majesty needs not to be told: we can supplement our present imperfect knowledge of them by instrumental observation only.”
To this message I received the following extraordinary reply: “All right—another bottle of—ice goes: push on— this cheese is too—spare no effort to—hand me those nuts—learn all you can—damn you!”
His most gracious Majesty was being served with dessert, and served badly.
I now resolved to go directly north toward the source of the ice-flow and investigate its cause, but examining my barometer found that I was more than 8,000 coprets below the sea-level; the moving ice had not only ground down the face of the country, planing off the eminences and filling the depressions, but its enormous weight had caused the earth’s crust to sag, and with the lessening of the weight from evaporation it had not recovered.
I had no desire to continue in this depression, as I should in going north, for I should find nothing but lakes, marshes and ferneries, infested with the same primitive and monstrous forms of life. So I continued my course eastward and soon had the satisfaction to find myself meeting the sluggish current of such streams as I encountered in my way.
By vigorous use of the new double-distance telepode, which enables the wearer to step eighty surindas instead of forty, as with the instrument in popular use, I was soon again at a considerable elevation above the sea-level and nearly 200 prastams from “Pike’s Peak.” A little farther along the water courses began to flow to the eastward. The flora and fauna had again altered in character, and now began to grow sparse; the soil was thin and arid, and in a week I found myself in a region absolutely destitute of organic life and without a vestige of soil. All was barren rock. The surface for hundreds of prastams, as I continued my advance, was nearly level, with a slight dip to the eastward. The rock was singularly striated, the scratches arranged concentrically and in helicoidal curves. This circumstance puzzled me and I resolved to take some more instrumental observations, bitterly regretting my improvidence in not availing myself of the Ahkoond’s permission to bring with me such apparatus and assistants as would have given me knowledge vastly more copious and accurate than I could acquire with my simple pocket appliances.
I need not here go into the details of my observations with such instruments as I had, nor into the calculations of which these observations were the basic data. Suffice it that after two months’ labor I reported the results to his Majesty in Sanf Rachisco in the words following:
“Sire: It is my high privilege to apprise you of my arrival on the western slope of a mighty depression running through the center of the continent north and south, formerly known as the Mississippi Valley. It was once the seat of a thriving and prosperous population known as the Pukes, but is now a vast expanse of bare rock, from which every particle of soil and everything movable, including people, animals and vegetation, have been lifted by terrific cyclones and scattered afar, falling in other lands and at sea in the form of what was called meteoric dust! I find that these terrible phenomena began to occur about the year 1860, and lasted, with increasing frequency and power, through a century, culminating about the middle of that glacial period which saw the extinction of the Galoots and their neighboring tribes. There was, of course, a close connection between the
