Chapter 1
I
am forced into speech because men of science have refused to follow
my advice without knowing why. It is altogether against my will that
I tell my reasons for opposing this contemplated invasion of the
antarctic—with its vast fossil hunt and its wholesale boring and
melting of the ancient ice caps. And I am the more reluctant because
my warning may be in vain.Doubt
of the real facts, as I must reveal them, is inevitable; yet, if I
suppressed what will seem extravagant and incredible, there would be
nothing left. The hitherto withheld photographs, both ordinary and
aerial, will count in my favor, for they are damnably vivid and
graphic. Still, they will be doubted because of the great lengths to
which clever fakery can be carried. The ink drawings, of course, will
be jeered at as obvious impostures, notwithstanding a strangeness of
technique which art experts ought to remark and puzzle over.In
the end I must rely on the judgment and standing of the few
scientific leaders who have, on the one hand, sufficient independence
of thought to weigh my data on its own hideously convincing merits or
in the light of certain primordial and highly baffling myth cycles;
and on the other hand, sufficient influence to deter the exploring
world in general from any rash and over– ambitious program in the
region of those mountains of madness. It is an unfortunate fact that
relatively obscure men like myself and my associates, connected only
with a small university, have little chance of making an impression
where matters of a wildly bizarre or highly controversial nature are
concerned.It
is further against us that we are not, in the strictest sense,
specialists in the fields which came primarily to be concerned. As a
geologist, my object in leading the Miskatonic University Expedition
was wholly that of securing deep–level specimens of rock and soil
from various parts of the antarctic continent, aided by the
remarkable drill devised by Professor Frank H. Pabodie of our
engineering department. I had no wish to be a pioneer in any other
field than this, but I did hope that the use of this new mechanical
appliance at different points along previously explored paths would
bring to light materials of a sort hitherto unreached by the ordinary
methods of collection.Pabodie's
drilling apparatus, as the public already knows from our reports, was
unique and radical in its lightness, portability, and capacity to
combine the ordinary artesian drill principle with the principle of
the small circular rock drill in such a way as to cope 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, and I. In addition, of course,
our two ships—wooden ex–whalers, reinforced for ice conditions
and having auxiliary steam—were fully manned.The
Nathaniel Derby Pickman Foundation, aided by a few special
contributions, financed the expedition; hence our preparations were
extremely thorough, despite the absence of great publicity. The dogs,
sledges, machines, camp materials, and unassembled parts of our five
planes were delivered in Boston, and there our ships were loaded. We
were marvelously well–equipped for our specific purposes, and in
all matters pertaining to supplies, regimen, transportation, and camp
construction we profited by the excellent example of our many recent
and exceptionally brilliant predecessors. It was the unusual number
and fame of these predecessors which made our own expedition— ample
though it was—so little noticed by the world at large.As
the newspapers told, we sailed from Boston Harbor on September 2nd,
1930, taking a leisurely course down the coast and through the Panama
Canal, and stopping at Samoa and Hobart, Tasmania, at which latter
place we took on final supplies. None of our exploring party had ever
been in the polar regions before, hence we all relied greatly on our
ship captains—J. B. Douglas, commanding the brig Arkham, and
serving as commander of the sea party, and Georg Thorfinnssen,
commanding the barque Miskatonic—both veteran whalers in antarctic
waters.As
we left the inhabited world behind, the sun sank lower and lower in
the north, and stayed longer and longer above the horizon each day.
At about 62° South Latitude we sighted our first icebergs—table–like
objects with vertical sides—and just before reaching the antarctic
circle, which we crossed on October 20th with appropriately quaint
ceremonies, we were considerably troubled with field ice. The falling
temperature bothered me considerably after our long voyage through
the tropics, but I tried to brace up for the worse rigors to come. On
many occasions the curious atmospheric effects enchanted me vastly;
these including a strikingly vivid mirage—the first I had ever
seen—in which distant bergs became the battlements of unimaginable
cosmic castles.Pushing
through the ice, which was fortunately neither extensive nor thickly
packed, we regained open water at South Latitude 67°, East Longitude
175°. On the morning of October 26th a strong land blink appeared on
the south, and before noon we all felt a thrill of excitement at
beholding a vast, lofty, and snow–clad mountain chain which opened
out and covered the whole vista ahead. At last we had encountered an
outpost of the great unknown continent and its cryptic world of
frozen death. These peaks were obviously the Admiralty Range
discovered by Ross, and it would now be our task to round Cape Adare
and sail down the east coast of Victoria Land to our contemplated
base on the shore of McMurdo Sound, at the foot of the volcano Erebus
in South Latitude 77° 9'.The
last lap of the voyage was vivid and fancy–stirring. Great barren
peaks of mystery loomed up constantly against the west as the low
northern sun of noon or the still lower horizon–grazing southern
sun of midnight poured its hazy reddish rays over the white snow,
bluish ice and water lanes, and black bits of exposed granite slope.
Through the desolate summits swept ranging, intermittent gusts of the
terrible antarctic wind; whose cadences sometimes held vague
suggestions of a wild and half–sentient musical piping, with notes
extending over a wide range, and which for some subconscious mnemonic
reason seemed to me disquieting and even dimly terrible. Something
about the scene reminded me of the strange and disturbing Asian
paintings of Nicholas Roerich, and of the still stranger and more
disturbing descriptions of the evilly fabled plateau of Leng which
occur in the dreaded Necronomicon of the mad Arab Abdul Alhazred. I
was rather sorry, later on, that I had ever looked into that
monstrous book at the college library.On
the 7th of November, sight of the westward range having been
temporarily lost, we passed Franklin Island; and the next day
descried the cones of Mts. Erebus and Terror on Ross Island ahead,
with the long line of the Parry Mountains beyond. There now stretched
off to the east the low, white line of the great ice barrier, rising
perpendicularly to a height of two hundred feet like the rocky cliffs
of Quebec, and marking the end of southward navigation. In the
afternoon we entered McMurdo Sound and stood off the coast in the lee
of smoking Mt. Erebus. The scoriac peak towered up some twelve
thousand, seven hundred feet against the eastern sky, like a Japanese
print of the sacred Fujiyama, while beyond it rose the white,
ghostlike height of Mt. Terror, ten thousand, nine hundred feet in
altitude, and now extinct as a volcano.Puffs
of smoke from Erebus came intermittently, and one of the graduate
assistants—a brilliant young fellow named Danforth—pointed out
what looked like lava on the snowy slope, remarking that this
mountain, discovered in 1840, had undoubtedly been the source of
Poe's image when he wrote seven years later:
— the
lavas that restlessly roll Their sulphurous currents down Yaanek In
the ultimate climes of the pole — That groan as they roll down
Mount Yaanek In the realms of the boreal pole.Danforth
was a great reader of bizarre material, and had talked a good deal of
Poe. I was interested myself because of the antarctic scene of Poe's
only long story—the disturbing and enigmatical Arthur Gordon Pym.
On the barren shore, and on the lofty ice barrier in the background,
myriads of grotesque penguins squawked and flapped their fins, while
many fat seals were visible on the water, swimming or sprawling
across large cakes of slowly drifting ice.Using
small boats, we effected a difficult landing on Ross Island shortly
after midnight on the morning of the 9th, carrying a line of cable
from each of the ships and preparing to unload supplies by means of a
breeches–buoy arrangement. Our sensations on first treading
Antarctic soil were poignant and complex, even though at this
particular point the Scott and Shackleton expeditions had preceded
us. Our camp on the frozen shore below the volcano's slope was only a
provisional one, headquarters being kept aboard the Arkham. We landed
all our drilling apparatus, dogs, sledges, tents, provisions,
gasoline tanks, experimental ice–melting outfit, cameras, both
ordinary and aerial, aeroplane parts, and other accessories,
including three small portable wireless outfits—besides those in
the planes—capable of communicating with the Arkham's large outfit
from any part of the antarctic continent that we would be likely to
visit. The ship's outfit, communicating with the outside world, was
to convey press reports to the Arkham Advertiser's powerful wireless
station on Kingsport Head, Massachusetts. We hoped to complete our
work during a single antarctic summer; but if this proved impossible,
we would winter on the Arkham, sending the Miskatonic north before
the freezing of the ice for another summer's supplies.I
need not repeat what the newspapers have already published about our
early work: of our ascent of Mt. Erebus; our successful mineral
borings at several points on Ross Island and the singular speed with
which Pabodie's apparatus accomplished them, even through solid rock
layers; our provisional test of the small ice–melting equipment;
our perilous ascent of the great barrier with sledges and supplies;
and our final assembling of five huge aeroplanes at the camp atop the
barrier. The health of our land party— twenty men and fifty–five
Alaskan sledge dogs—was remarkable, though of course we had so far
encountered no really destructive temperatures or windstorms. For the
most part, the thermometer varied between zero and 20° or 25°
above, and our experience with New England winters had accustomed us
to rigors of this sort. The barrier camp was semi–permanent, and
destined to be a storage cache for gasoline, provisions, dynamite,
and other supplies.Only
four of our planes were needed to carry the actual exploring
material, the fifth being left with a pilot and two men from the
ships at the storage cache to form a means of reaching us from the
Arkham in case all our exploring planes were lost. Later, when not
using all the other planes for moving apparatus, we would employ one
or two in a shuttle transportation service between this cache and
another permanent base on the great plateau from six hundred to seven
hundred miles southward, beyond Beardmore Glacier. Despite the almost
unanimous accounts of appalling winds and tempests that pour down
from the plateau, we determined to dispense with intermediate bases,
taking our chances in the interest of economy and probable
efficiency.Wireless
reports have spoken of the breathtaking, four–hour, nonstop flight
of our squadron on November 21st over the lofty shelf ice, with vast
peaks rising on the west, and the unfathomed silences echoing to the
sound of our engines. Wind troubled us only moderately, and our radio
compasses helped us through the one opaque fog we encountered. When
the vast rise loomed ahead, between Latitudes 83° and 84°, we knew
we had reached Beardmore Glacier, the largest valley glacier in the
world, and that the frozen sea was now giving place to a frowning and
mountainous coast line. At last we were truly entering the white,
aeon–dead world of the ultimate south. Even as we realized it we
saw the peak of Mt. Nansen in the eastern distance, towering up to
its height of almost fifteen thousand feet.The
successful establishment of the southern base above the glacier in
Latitude 86° 7', East Longitude 174° 23', and the phenomenally
rapid and effective borings and blastings made at various points
reached by our sledge trips and short aeroplane flights, are matters
of history; as is the arduous and triumphant ascent of Mt. Nansen by
Pabodie and two of the graduate students—Gedney and Carroll—on
December 13—15. We were some eight thousand, five hundred feet
above sea–level, and when experimental drillings revealed solid
ground only twelve feet down through the snow and ice at certain
points, we made considerable use of the small melting apparatus and
sunk bores and performed dynamiting at many places where no previous
explorer had ever thought of securing mineral specimens. The
pre–Cambrian granites and beacon sandstones thus obtained confirmed
our belief that this plateau was homogeneous, with the great bulk of
the continent to the west, but somewhat different from the parts
lying eastward below South America—which we then thought to form a
separate and smaller continent divided from the larger one by a
frozen junction of Ross and Weddell Seas, though Byrd has since
disproved the hypothesis.In
certain of the sandstones, dynamited and chiseled after boring
revealed their nature, we found some highly interesting fossil
markings and fragments; notably ferns, seaweeds, trilobites,
crinoids, and such mollusks as linguellae and gastropods—all of
which seemed of real significance in connection with the region's
primordial history. There was also a queer triangular, striated
marking, about a foot in greatest diameter, which Lake pieced
together from three fragments of slate brought up from a deep–blasted
aperture. These fragments came from a point to the westward, near the
Queen Alexandra Range; and Lake, as a biologist, seemed to find their
curious marking unusually puzzling and provocative, though to my
geological eye it looked not unlike some of the ripple effects
reasonably common in the sedimentary rocks. Since slate is no more
than a metamorphic formation into which a sedimentary stratum is
pressed, and since the pressure itself produces odd distorting
effects on any markings which may exist, I saw no reason for extreme
wonder over the striated depression.On
January 6th, 1931, Lake, Pabodie, Danforth, the other six students,
and myself flew directly over the south pole in two of the great
planes, being forced down once by a sudden high wind, which,
fortunately, did not develop into a typical storm. This was, as the
papers have stated, one of several observation flights, during others
of which we tried to discern new topographical features in areas
unreached by previous explorers. Our early flights were disappointing
in this latter respect, though they afforded us some magnificent
examples of the richly fantastic and deceptive mirages of the polar
regions, of which our sea voyage had given us some brief foretastes.
Distant mountains floated in the sky as enchanted cities, and often
the whole white world would dissolve into a gold, silver, and scarlet
land of Dunsanian dreams and adventurous expectancy under the magic
of the low midnight sun. On cloudy days we had considerable trouble
in flying owing to the tendency of snowy earth and sky to merge into
one mystical opalescent void with no visible horizon to mark the
junction of the two.At
length we resolved to carry out our original plan of flying five
hundred miles eastward with all four exploring planes and
establishing a fresh sub–base at a point which would probably be on
the smaller continental division, as we mistakenly conceived it.
Geological specimens obtained there would be desirable for purposes
of comparison. Our health so far had remained excellent—lime juice
well offsetting the steady diet of tinned and salted food, and
temperatures generally above zero enabling us to do without our
thickest furs. It was now midsummer, and with haste and care we might
be able to conclude work by March and avoid a tedious wintering
through the long antarctic night. Several savage windstorms had burst
upon us from the west, but we had escaped damage through the skill of
Atwood in devising rudimentary aeroplane shelters and windbreaks of
heavy snow blocks, and reinforcing the principal camp buildings with
snow. Our good luck and efficiency had indeed been almost uncanny.The
outside world knew, of course, of our program, and was told also of
Lake's strange and dogged insistence on a westward—or rather,
northwestward—prospecting trip before our radical shift to the new
base. It seems that he had pondered a great deal, and with alarmingly
radical daring, over that triangular striated marking in the slate;
reading into it certain contradictions in nature and geological
period which whetted his curiosity to the utmost, and made him avid
to sink more borings and blastings in the west– stretching
formation to which the exhumed fragments evidently belonged. He was
strangely convinced that the marking was the print of some bulky,
unknown, and radically unclassifiable organism of considerably
advanced evolution, notwithstanding that the rock which bore it was
of so vastly ancient a date—Cambrian if not actually
pre–Cambrian—as to preclude the probable existence not only of
all highly evolved life, but of any life at all above the unicellular
or at most the trilobite stage. These fragments, with their odd
marking, must have been five hundred million to a thousand million
years old.