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Underground Rivers - University of New Mexico

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Chapter 9 -- Thermodynamic Engines<br />

A fire smoldering within a cavern nicely, if incorrectly, explains<br />

the report in Adams County [Iowa] Free Press, October 18,<br />

1913.<br />

A peculiarity <strong>of</strong> some <strong>of</strong> the streams on Switzerland is that a<br />

number <strong>of</strong> them have their source from canyons which are<br />

underground passages. One at Ragaz, known as the<br />

Taminaschlucht, comes out at the foot <strong>of</strong> a mountain, and a<br />

foot way has been constructed so that it may be entered for a<br />

distance <strong>of</strong> about half a mile to a place where the stream<br />

gushes our <strong>of</strong> a subterranean opening to its full capacity, and<br />

at one side there is a second opening from which hot water<br />

flows.<br />

The Taminaschlucht gorge is 100 meters deep and 10 meters<br />

wide. A tunnel leads to a grotto having a 37°C thermal spring.<br />

In at least this instance, hypothesizers <strong>of</strong> hot and cold<br />

subterranean plumbing were close to the mark.<br />

What we now know <strong>of</strong> geophysics supports in loose degree even a transmutational basis for<br />

springflow, if one allows chemical reactions to count as transmutation. Some hot-spring effluent<br />

is "juvenile," newly formed by volcanic or tectonic processes.<br />

While condensation may be inconsequential in most groundwater<br />

environments, again the early speculators were onto a legitimate idea.<br />

The micro-hydrologic water balance in large cave systems -- especially<br />

ones in which there are large differences in temperature -- can be<br />

significant. In certain Crimean and Caucasian karst regions, between<br />

0.1 and 20 percent <strong>of</strong> dry-season run<strong>of</strong>f is said to be derived from<br />

subterranean condensate, the illustration to the right serving as an<br />

illustration.<br />

The heat <strong>of</strong> the earth does not drive underground rivers uphill, but in limited cases, geothermal<br />

energy plays a role in groundwater flow. The hydrophylacia so well advertised by Kircher do not<br />

exist, but again in limited cases, Chapters 51 and 42 containing examples, mammoth<br />

subterranean caverns evidence subterranean streamflow.<br />

And we're not done with subterranean hydrologic engines, or at least imaginative propositions for<br />

the task.<br />

DRAFT 1122//66//22001122<br />

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90

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