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Various

"Scientific American Supplement, No. 433, April 19, 1884"

The late fall months, the winter, and early
spring are not so much colder than the valleys as the summer months, the
difference between the average temperature of the mountains and valleys
being at that time four or five degrees less than in the summer. There
is no record of so hot a day ever having occurred on the Cumberladd
Mountains as to cause mercury to run so high as 95 deg. F., or so cold a day
as to cause it to run so low as 10 deg. below zero.
In the average winter the ground rarely freezes to a greater depth than
2 or 3 inches, and it remains frozen but a few days at a time. Ice has
been known to form 8 inches thick, but in ordinary winters, 3 or 4
is the maximum. Snow falls every winter, more or less, and sometimes
remains for a week. Old people have a remembrance of a foot of snow
which lasted for a week.
Walden's Ridge has a total population of a little more than 4,000,
scattered over 600 square miles of surface. The number of dwellings is
about 800. Ninety per cent. of these are log houses; 70 per cent.


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