
At the Mountains of Madness
quickly with strata of varying hardness. Steel head, jointed rods, gasoline motor,
collapsible wooden derrick, dynamiting paraphernalia, cording, rubbish-removal auger,
and sectional piping for bores five inches wide and up to one thousand feet deep all
formed, with needed accessories, no greater load than three seven-dog sledges could
carry. This was made possible by the clever aluminum alloy of which most of the metal
objects were fashioned. Four large Dornier aeroplanes, designed especially for the
tremendous altitude flying necessary on the antarctic plateau and with added fuel-
warming and quick-starting devices worked out by Pabodie, could transport our entire
expedition from a base at the edge of the great ice barrier to various suitable inland
points, and from these points a sufficient quota of dogs would serve us.
We planned to cover as great an area as one antarctic season - or longer, if absolutely
necessary - would permit, operating mostly in the mountain ranges and on the plateau
south of Ross Sea; regions explored in varying degree by Shackleton, Amundsen, Scott,
and Byrd. With frequent changes of camp, made by aeroplane and involving distances
great enough to be of geological significance, we expected to unearth a quite
unprecedented amount of material - especially in the pre-Cambrian strata of which so
narrow a range of antarctic specimens had previously been secured. We wished also to
obtain as great as possible a variety of the upper fossiliferous rocks, since the primal life
history of this bleak realm of ice and death is of the highest importance to our knowledge
of the earth's past. That the antarctic continent was once temperate and even tropical, with
a teeming vegetable and animal life of which the lichens, marine fauna, arachnida, and
penguins of the northern edge are the only survivals, is a matter of common information;
and we hoped to expand that information in variety, accuracy, and detail. When a simple
boring revealed fossiliferous signs, we would enlarge the aperture by blasting, in order to
get specimens of suitable size and condition.
Our borings, of varying depth according to the promise held out by the upper soil or rock,
were to be confined to exposed, or nearly exposed, land surfaces - these inevitably being
slopes and ridges because of the mile or two-mile thickness of solid ice overlying the
lower levels. We could not afford to waste drilling the depth of any considerable amount
of mere glaciation, though Pabodie had worked out a plan for sinking copper electrodes
in thick clusters of borings and melting off limited areas of ice with current from a
gasoline-driven dynamo. It is this plan - which we could not put into effect except
experimentally on an expedition such as ours - that the coming Starkweather-Moore
Expedition proposes to follow, despite the warnings I have issued since our return from
the antarctic.
The public knows of the Miskatonic Expedition through our frequent wireless reports to
the Arkham Advertiser and Associated Press, and through the later articles of Pabodie and
myself. We consisted of four men from the University - Pabodie, Lake of the biology
department, Atwood of the physics department - also a meteorologist - and myself,
representing geology and having nominal command - besides sixteen assistants: seven
graduate students from Miskatonic and nine skilled mechanics. Of these sixteen, twelve
were qualified aeroplane pilots, all but two of whom were competent wireless operators.
Eight of them understood navigation with compass and sextant, as did Pabodie, Atwood,