This is the
web site of the
International
Journal of
Speleology
Since 1964
ISSN NUMBERS
print
0392 6672
cd-rom
1827-7713
pdf
1827-806X
The International Journal of Speleology has been included in the following ISI Thomson Reuters products beginning with volume 36(1) 2007: Science Citation Index-Expanded including the Web of Science, ISI Alerting Service, Current Contents/Physical, Chemical & Earth Sciences
Special cooperation and joint publications with
Speleogenesis
Bubble trails are subaqueous features in carbonate caves, which are made by the corrosion of ascending carbon dioxide bubbles. Folia are calcite deposits resembling inverted rimstone dams in saturated pools. Based on morphological studies in Adaouste Cave (Provence, France) and on studies elsewhere in the world, we propose a new genetic model for folia, close to the model of Green (1991). The association of bubble trails and folia, occurring on overhanging walls, is interpreted to be an indicator of hypogenic degassing occurring just below the water table. The association is the result of juxtaposed processes composed of corrosion along bubble trails and calcite deposition in calcite-saturated pools.