The book “Hypogene Karst Regions and Caves of the World” is going to be published by Springer, in its series “Cave and Karst Systems of the World”.
There will be a karst session at the AGU Fall 2016 Meeting in San Francisco, USA in December 12-16: Characterization, Modeling, and Remediation of Fissured, Carbonate, and Karst Groundwater Systems
A book "Höhlen und Karst in Österreich" (Caves and karst in Austria; Editors: Christoph Spötl, Lukas Plan & Ehrad Christian) will be printed until mid of July. Subscription is available.
Many inspiring ideas on caves can be found in images created by children, generated by the International Contest of Kid’s Drawing "Caves in the Eyes of our Children".
A call to submit an abstract to a session devoted to karst aquifers, which will be held in September in Montpellier during the 43rd IAH Congress
Did you know?
That active glacier is glacier in the stage of actively enlarging and moving as a result of accumulation of precipitation that exceeds the rate of ablation.?
Checkout all 2699 terms in the KarstBase Glossary of Karst and Cave Terms
Featured article from karst/cave journal
Free surface streams in caves and their surface infeeders often contain pebbles and cobbles coated with black manganese oxide minerals. Coating thicknesses vary from fractions of a millimeter to a few millimeters. In addition, a few caves contain loose masses of black oxide material. The results reported here are based on examination of 39 specimens and detailed chemical analyses of 18 of them. Most of the coatings are amorphous to x-rays, with at best, only a few broad diffraction lines. Infrared spectroscopy shows that most of the specimens are birnessite, with evidence for romanechite, ranceite, and pyrolusite in a few specimens. All specimens contain both iron and manganese, but the Mn/Fe ratio varies widely. Many specimens are enriched in Ba but depleted in Sr. The manganese and iron oxides contain the transition metals Co, Cu, Ni, V, and Zn in concentrations greater than 0.5 wt% in some specimens. Minor Cr and Mo also occur. Given the extremely low concentrations of these elements expected in freshwater streams in carbonate terrains, the manganese oxides exert a dramatic amplifying effect over the expected background. Manganese oxides appear to act as a dosimeter for heavy metals in karst waters.