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 chemical erosion is processes partially synonymous with chemical dissolution, but including any other form of rock breakdown accelerated by chemical changes of the constituent minerals .?
Checkout all 2699 terms in the KarstBase Glossary of Karst and Cave Terms
Featured article from karst/cave journal
Flank margin caves have been observed in Quaternary Bridgewater Formation eolianites on Kangaroo Island, South Australia. Horizons of flank margin cave development at 25 m, 30 m, and 35 m elevation demonstrate tectonic uplift of tens of meters during the Quaternary, as the cave elevations are higher than any reported Quaternary glacioeustatic sea-level highstand. Distinct cave horizons indicate that episodic uplift was possible. Wave-cut notches at Hanson Bay, at 30 to 35 m elevation, also support the interpretation from caves that relative sea level was once at the ,30-m- elevation range. Admirals Arch, previously presented as forming solely by wave erosion, is a flank margin cave breached and modified by wave erosion. Point Ellen contains a Late Pliocene subtidal carbonate unit that formed within the reach of wave base, was uplifted and cliffed by wave processes, and then was karstified before being buried by Quaternary Bridgewater Formation eolianites. A possible flank margin cave developed at Point Ellen at 3 m above modern sea level is consistent with earlier interpretations of notching of the nearby coast at a similar elevation during the last interglacial sea-level highstand (MIS 5e); and therefore, no tectonic uplift in the last 120 ka. In contrast, the tafoni of Remarkable Rocks present a cautionary note on evidence of cave wall morphological characteristics as proof of dissolutional origin.