The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal lifeGrew, Edwin Sharpe
Science
The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal life
Grew, Edwin Sharpe
Geology; Paleontology
For ten years Professor Agassiz took observations concerning a very
deep mine in the United States called the Calumet and Hecla Mine.
He and Professor Chamberlin, after examining all the observations
very carefully, came to the conclusion that in going down from the
earth's surface the temperature rose at a rate of about 1° of heat
(Fahrenheit) for every 125 feet.
At the North Garden Gully Mine, Bendigo, Australia, and at the New
Chum Mine a temperature of 99° F. was reached at 3000 feet, and 107°
at 3645 feet. The rate of increase of temperature was reckoned to be
1° of heat (Fahrenheit) for every 80 feet.
This rate of 1° for 80 feet was also found at a South German mine,
Maldon, as well as at a Ballarat mine, and at a mine near Port
Jackson.
In a French mine more than 3000 feet deep, at the collieries of
Ronchamp, the rate of increase was as high as 1° in 50 feet.
In the North Staffordshire mines Mr. Atkinson, H.M. Inspector of
Mines, found the increase to be on the average 1° in 65 feet; whereas
in the South Staffordshire Hamstead Colliery Mr. F. G. Meachem found
that the increase was 1° F. for every 110 feet. The same rate was
obtained at the Baggeridge Wood Colliery, South Staffordshire.
In South Wales, in the neighbourhood of Rhondda and Aberdare, the
rate is 1° for 95 feet; at Dowlais, in the Merthyr coalfield, it
was 1° in 93 feet; at the Niddrie Collieries, near Edinburgh, the
increase is at the rate of 1° in 99 feet.
It will thus be seen that all over the world there is an increase of
temperature at a rate which, on the average, is about 1° for every
100 feet. There are 5280 feet in a mile; therefore, if this rate of
increasing temperature were maintained, at a depth of 100 miles the
temperature would be perhaps 5000° F.; a temperature at which steel
would melt and boil away into vapour. At a depth of 200 miles the
heat would be greater than that of the surface of the sun.[2]
[Footnote 2: According to the calculations made by the late Mr. W.
E. Wilson, F.R.S., in Ireland, 5773° Centigrade above the lowest
temperature which is possible in space, or about 10,500° F.]
Public-domain text, read in full here on John Shaqi.
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