© 2005 Gabi Haindl, All Rights Reserved.
In the cavern carbon-dioxide gets in solution in the water until it is saturated. More carbon-dioxide starts to rise the pressure in the chamber till the water starts to rise again. With less hydrostatic pressure in the water column, carbon-dioxide starts to degas in the ascending water and forces the water to ascend faster. The cold geyser erupts.
This happens every 30 minutes, though every second eruption is higher, up to 3-4 meters.
My panorama depicts the smaller of the two eruptions. I liked that version more than the one I took half an hour later. In this one a group of people, who likely attended a funeral before, came by to watch Brubbel and to their opposite some belgian or dutch tourists in shorts.
I also took two additional panoramas, one ten minutes before the eruption and one three minutes after it.