
Originally Posted by
Kelly Jessop
I did a study with Georgia DNR and we installed temperature sensors in the cave at about 300ft intervals to a distance to 1200'. When the Flint River started to rise,the spring we were testing reversed. The sensors in this case didn't show a slow change of temperature from sensor to sensor with progressively deeper penetration,but it was similar to a toilet being flushed. Looking at the temperature data revealed this reversal happened through out the system in minutes. A couple years later I went out to dive the system when the river was high,and from the surface I witnessed a swirling vortex of river water syphoning inward. This system wasn't a low flow system like Peacock,but a higher flow system.
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