Last
weekend it was hot outside, the temperature was in the lower 80o’s F
(around 27o C), I was hiking when suddenly, I felt a cold breeze, which
must have been about 50o F (10o
C)! I followed the breeze and saw a
cave, a “breathing cave”.
A
breathing cave, what’s that?
This cave, if it is the
same as the one mentioned in the history of Armstrong County, Pennsylvania,
by J.H. Beers & Co, would likely have two openings, since constant water
erosion would explain the sandy floor that was discovered inside.
In any case, the cave
layout, whether it has an upper and lower entrance separated by a difference in
elevation, and the temperature contrast between the internal cave air and the
outside air, is what creates the cave respiration.
In the winter, the cave’s
air temperature is usually warmer than the outside air temperature, this causes
the warmer, less dense to rise and flow out along the roof of the cave’s
entrance creating a warm breeze. In the
summer this pattern reverses, with the cave’s internal air temperature being
lower than the outside air temperature causing the cooler, more dense cave air
to sink and flow out along the floor of the cave’s entrance crating a cool
breeze. This pattern of cave breathing
also happens daily as the outside air temperatures rises and falls above and
below 50o F (10o C), since according to the U.S. National
Park Service caves in the United States, remain a constant 52o to 55o
F (11o to 13o C) year around. Daily two-way cave airflow is most common
during the spring and fall, since outside air temperatures during those seasons
most often rise and fall above and below the cave’s constant internal
temperature.
Today, the “chimney
effect” and the physics of cave airflow is just a curious and interesting
mental tidbit, but in the past, this was a vital bit of survival information
for our cave dwelling ancestors and for pre-steam engine miners, who used this effect
and fires both for warmth and to draw cool fresh air into the underground.
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That
is all for now, and as always, until next time, Happy Trails!
Sources
J.H. Beers & Co;
Armstrong County, Pennsylvania, Vol. 1, [J.H. Beers & Co, Chicago,
1914], https://archive.org/details/armstrongcountyp01jhbe/page/40/mode/2up,
accessed September 6, 2024
Kedar, Yafit and Barkai, Ran;
“The Significance of Air Circulation and Hearth Location at Paleolithic Cave
Sites”, Open Quaternary, Vol. 5, No. 4, pages 1 to12, https://openquaternary.com/articles/52/files/submission/proof/52-1-985-1-10-20190612.pdf,
accessed September 7, 2024
McGee,
W. J.; “Ice
Caves and Frozen Wells”, The National Geographic Magazine, December
1901, Volume 12, page 434 to 435, https://books.google.com/books?id=-z4PAAAAIAAJ&pg=PA432&dq=%22it+is+very+desirable+that+this+boundary+be+resurveyed%22&hl=en&newbks=1&newbks_redir=0&sa=X&ved=2ahUKEwj2n8fdkqqIAxUrGVkFHeIaGYUQ6AF6BAgHEAI#v=onepage&q=%22it%20is%20very%20desirable%20that%20this%20boundary%20be%20resurveyed%22&f=false,
accessed September 6, 2024
National Speleological
Society; Journal Of Cave And Karst Studies, March 2021, Volume 83,
Number 1, pages 8-9, https://caves.org/wp-content/uploads/Publications/JCKS/v83/cave-83-01-fullr.pdf,
accessed September 6, 2024
Unknown; A Description
of Howe’s Cave, [Weed, Parsons and Company, Albany, 1865], pages 10 to 11, https://books.google.com/books?id=JOXu0KCTX4wC&pg=PA10&dq=blowing+caves+temperature&hl=en&newbks=1&newbks_redir=0&sa=X&ved=2ahUKEwiH_5Xe96uIAxUaF1kFHR5VJ38Q6AF6BAgPEAI#v=onepage&q=blowing%20caves%20temperature&f=false,
accessed September 6, 2024
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