The Ascent of Denali (Mount McKinley): A Narrative of the First Complete Ascent of the Highest; Peak in North AmericaStuck, Hudson
History
The Ascent of Denali (Mount McKinley): A Narrative of the First Complete Ascent of the Highest; Peak in North America
Stuck, Hudson
McKinley, Mount (Alaska); Mountaineering -- Alaska -- McKinley, Mount; Stuck, Hudson, 1863-1920 -- Travel -- Alaska -- McKinley, Mount
This great crescent range is, indeed, our rampart against the hateful
humidity of the coast and gives to us in the interior the dry, windless,
exhilarating cold that is characteristic of our winters. We owe it
mainly to this range that our snowfall averages about six feet instead
of the thirty or forty feet that falls on the coast. The winds that
sweep northward toward this mountain range are saturated with moisture
from the warm waters of the Pacific Ocean; but contact with the lofty
colds condenses the moisture into clouds and precipitates most of it on
the southern slopes as snow. Still bearing all the moisture their
lessened temperature will allow, the clouds pour through every notch and
gap in the range and press resolutely onward and downward, streaming
along the glaciers toward the interior. But all the time of their
passage they are parting with their moisture, for the snow is falling
from them continually in their course. They reach the interior, indeed,
and spread out triumphant over the lowlands, but most of their burden
has been deposited along the way. One is reminded of the government
train of mules from Fort Egbert that used to supply the remote posts of
the "strategic" telegraph line before strategy yielded to economy and
the useless line was abandoned. When the train reached the Tanana
Crossing it had eaten up nine-tenths of its original load, and only
one-tenth remained for the provisioning of the post. So these clouds
were being squeezed like a sponge; every saddle they pushed through
squeezed them; every peak and ridge they surmounted squeezed them; every
glacier floor they crept down squeezed them, and they reached the
interior valleys attenuated, depleted, and relatively harmless.
[Sidenote: Aneroids]
The aneroids had kept fairly well with the mercurial barometer and the
boiling-point thermometer until we moved to the ridge; from this time
they displayed a progressive discrepancy therewith that put them out of
serious consideration, and one was as bad as the other. Eleven thousand
feet seemed the limit of their good behavior. To set them back day by
day, like Captain Cuttle's watch, would be to depend wholly upon the
other instruments anyway, and this is just what we did, not troubling to
adjust them. They were read and recorded merely because that routine had
been established. Says Burns:
"There was a lad was born in Kyle,
But whatna day o' whatna style,
I doubt it's hardly worth the while
To be sae nice wi' Robin."
So they were just aneroids: aluminum cases, jewelled movements,
army-officer patented improvements, Kew certificates, import duty, and
all--just aneroids, and one was as bad as the other. Within their
limitations they are exceedingly useful instruments, but it is folly to
depend on them for measuring great heights.
Public-domain text, read in full here on John Shaqi.
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