Appletons' Popular Science Monthly, April 1900: Vol. 56, Nov. 1899 to April, 1900Various
History
Appletons' Popular Science Monthly, April 1900: Vol. 56, Nov. 1899 to April, 1900
Various
Science -- Periodicals; Technology -- Periodicals
poles, together with the auroral lights characteristic of those
regions. This, I am well aware, is an audacious theory. It is certainly
a vast extension of the laboratory experiments I have described, but
the electrical radiations developed in electrical discharges are as
competent to produce powerful magnetic whirls as the heat radiations
in our atmosphere to develop cyclones. In the lower regions of our
atmosphere the air is an insulator like glass to the passage of an
electrical current. A layer a foot thick can prevent the circulation of
the most powerful current which is now used to generate horse power.
When this air space is rarefied at a certain degree of rarefaction
the electrical current passes, especially, as we have seen, if it is
illuminated by the X rays. When, therefore, we ascend to a height of
ten or twenty miles the rarefied air becomes an excellent conductor of
electricity of high electro-motive force. To my mind the conditions
exist for developing an electrical state in the earth’s covering of
air, which is competent to explain the electrical manifestations of
the air, the auroral gleam, and the mysterious effect on the magnetic
needle which keeps it directed to the magnetic north. Can not we
conclude that the study of the X rays bids fair to greatly extend
our conceptions of the constitution of matter and of the action and
interaction of Nature’s forces?
* * * * *
A Himalayan explorer reported, a few years ago, that he had seen,
from one of the lofty summits of the Mount Everest district, a peak
which, beheld in the same view with Mount Everest, was evidently
higher than it. Nothing has been heard of the matter since then
till the recent appearance of Major L. A. Waddell’s book, Among
the Himalayas. This author, who has explored the same region,
represents that the Tibetans there say there is another mountain,
due north of Mount Everest, that exceeds that peak in height, thus
confirming the story of the former Alpinist. It appears that Mount
Everest is not called Gaurisankar or Deodunga, as some affirm,
but that the Tibetan name of the culminating peak of the group is
_Jomokang-kar_--“The Lady White Glacier.”
A HUNDRED YEARS OF CHEMISTRY.
BY F. W. CLARKE,
CHIEF CHEMIST, UNITED STATES GEOLOGICAL SURVEY.
Public-domain text, read in full here on John Shaqi.
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