Now I understand a spring being covered, even reversing, but why would Bozel 1 be dead, while 30 ft away Bozel 2 was pumping. Low, but pumping. We distinctly did not get the impression that there was any flow occuring under the layer of pooh, and as Bozel divers know, this spring basin is like a strainer as the water is pushed out about 10 different holes (only one of which leads under the land bridge to Bozel 2). So what gives? Has anyone else been here when this has happened? My theory is that the flow seen in Bozel 2 is actually artifact of what would normally be downstream, through too small fissure, backflowing up to Bozel 2 and creating the little discharge that was evident. I say this only because, inexplicably, the normally downstream vents are seemingly flowing at an increased rate. This was observed about mid-July. If anyone has been there after that please let me know what you saw. ty
Another possibility is that a cave-in or slide has blocked a passage feeding "Bozel 1", and the flow has been re-routed to the other springs. Especially since you noticed a collapse in one location, and droughts are more likely to cause cave-ins.