Brian Frank (United States) |
|
Contact by email
|
| Address: | Atlanta, GA |
|---|---|
| Affiliation: | NSS, SCCI, Dogwood Grotto |
Member of Speleogenesis.info since 2012-01-01
Community news
Speleology in Kazakhstan
Shakalov on 04 Jul, 2018
Hello everyone!
I pleased to invite you to the official site of Central Asian Karstic-Speleological commission ("Kaspeko")
There, we regularly publish reports about our expeditions, articles and reports on speleotopics, lecture course for instructors, photos etc. ...New publications on hypogene speleogenesis
Klimchouk on 26 Mar, 2012
Dear Colleagues, This is to draw your attention to several recent publications added to KarstBase, relevant to hypogenic karst/speleogenesis: Corrosion of limestone tablets in sulfidic ground-water: measurements and speleogenetic implications Galdenzi,The deepest terrestrial animal
Klimchouk on 23 Feb, 2012
A recent publication of Spanish researchers describes the biology of Krubera Cave, including the deepest terrestrial animal ever found:
Jordana, Rafael; Baquero, Enrique; Reboleira, Sofía and Sendra, Alberto. ...Caves - landscapes without light
akop on 05 Feb, 2012
Exhibition dedicated to caves is taking place in the Vienna Natural History Museum
The exhibition at the Natural History Museum presents the surprising variety of caves and cave formations such as stalactites and various crystals. ...Did you know?
That phreatic zone is 1. those parts of the earth's crust in which all voids are filled with water under pressure greater than atmospheric [22]. 2. that part of the earth's crust beneath the regional water table in which all voids, large and small, are ideally filled with water under pressure greater than atmospheric [22]. when discussing a karst setting, it is preferable to use the term, phreatic zone, so as to avoid confusion regarding chemical saturation. synonym: saturated zone. see also zone of saturation.?
Checkout all 2699 terms in the KarstBase Glossary of Karst and Cave Terms