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Page 28
"Now look at my map. This inner circle represents the present area of
boiling lava, which, as I have said, is about fifteen miles in
diameter--the South Pole, according to the natives, being at about the
point corresponding to this dot, marked 'a.' The ring next without the
circle I have made to represent a zone of lava which is at its inner
edge white-hot, and at its outer edge red-hot, its width, let us say, as
the division is arbitrary, about four miles. The second circle
represents a zone of lava which is dull red at its inner edge, and
black, but hot, at its outer. Of course the lava blends away from
white-hot within, to barely warm without; but I thus map it, the better
to picture reigning conditions. The next circle, some four or five miles
in width, represents a ring of cold lava-blocks, masses of rock-salt,
and animalculine remains, from twenty-five to two hundred feet high.
Outside of this last-mentioned zone, we have several rings of volcanic
mountains with intervening valleys, and many active craters at the
summit of mountains; while on the mountain-sides lie numerous masses of
rock-salt, thrown from below by eruptive action, glistening in the
brilliant volcanic light, and slowly deliquescing. This zone of
mountains and valleys is from ten to twenty miles in width, and whilst
in the main its mountains are not more than from half a mile to a mile
high, it contains peaks of five or six miles in height, and there is one
peak which rises nine miles above the sea-level.
"I want you to look particularly at these larger mountain-ranges, one at
the right, the other at the left side of my map--each of which as it
stretches out into the sea divides into two smaller chains. Upon these
ranges, and the comparatively diminutive height of the intervening
mountains, in connection with the fact that there is a constant
wind-current from the lower Pacific (generally speaking, from the west
of longitude 74 W.), depends the habitability of this large island, the
Island of Hili-li (here represented in about longitude 75 E.), and many
other islands which stretch out in the same direction from this enormous
active surface-crater. I say that upon such conditions depends the
habitability of these islands, and so I believe; but there is another
cause for their greater than tropical warmth: If you will glance here on
the right of this map, in the midst of the mountain zone you will see
represented a bay, which, winding among mountains, makes its way very
close to the zone of hot lava--in fact, is divided from it by little
more than the ring of lava-blocks, rock-salt, and animal remains, which
at this point is narrowed to a width of about two miles. The temperature
of the water of this bay at its inner extremity is probably about 180
F.--say 32 below the boiling-point of distilled water; and it flows in a
steady current past the Island of Hili-li. This bay is undoubtedly fed
from the opposite side of the great crater, and its supply flows for
miles in contact with hot lava. It is probable that this extremely warm
water current greatly assists the hot-air current in creating the
super-tropical climate of Hili-li.
"And now, as I have in part satisfied your curiosity, and as I am
somewhat exhausted with my two days' and nights' experience with Peters,
I know you will permit me to rest at so suitable a stopping-point.
To-morrow evening I will take up the story of Dirk Peters where it joins
the sudden break in Pym's journal, and will carry you along to the time
when the inhabitants of Hili-li thought that the atmosphere of some
other land would be more conducive to Peters' longevity and health, as
well as to their own tranquillity. And I assure your Sultanship, that
the story I shall relate to you to-morrow night will be more interesting
than the dry physical facts which I have this evening imparted, and
which it seemed best that you should know before hearing in consecutive
detail the particulars of Peters' voyage."
I assented to his suggestions, thanking him for the clear description
which he had given of that strange region, and for the pains he had
taken to draft of it so accurate a map--which map he allowed me to
retain. I was about to ask a question, when the door opened, and Doctor
Castleton rushed into the room.
"Well, how's the old man?" he asked.
We described Peters' condition; and I even recounted a few of the facts
which Bainbridge had just imparted to me. Then I asked the question
which Castleton's abrupt entry had delayed.
"But," I asked, "has not Peters' imagination, owing to the
administration of drugs, been unnaturally stimulated? There are drugs
which it is commonly believed may have a wonderful effect in stimulating
the imagination to flights of marvellous grandeur."
"No," said Bainbridge. "The doctor here will say the same. No drug on
earth could produce even an approach to such an effect."
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