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Various

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

"
This was the usual testimony of the residents. Winds of great velocity
never occur there. In summer there is always an evening breeze,
commencing at 4 to 6 o'clock, and continuing until after sunrise
the next morning. In times of rain, clouds hang low over the ridge
occasionally, but they never have fogs there.
The range of the thermometer is less on the Tablelands than in the
adjacent valleys. I have had access to the carefully taken observations
of the Lookout Mountain Educational Institute, such published accounts
as have been made by Professor Safford, State Geologist, Mr. Killebrew,
the thorough and painstaking private record of Captain John P. Long,
of Chattanooga, and many more of less length of time. From all these I
deduce the fact that the summer days are seven or eight degrees cooler
on the mountains than in the Tennessee Valley at Chattanooga, and five
or six degrees cooler than in the Sequatchee Valley, as far up as Dunlay
and Pikeville. The nights on the table are cooler than in the lower
lands by several more degrees than the days; how much I have thus far
not been able to state.


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