The International Conference on Remediation of Chlorinated and Recalcitrant Compounds is the world’s largest and most comprehensive meeting on the application of innovative and existing technologies and approaches for characterization, monitoring and management of chlorinated and complex sites. The topic of karst was conspicuously absent at the first eight iterations of this conference. At the 9th Conference, a karst session -- headlined by a presentation by Dr. Derek Ford -- was held and well attended...
The Geological Survey of Spain (IGME) is conducting a research into the Cerro del Cuevon (-1589 m), the deepest cave of Spain and one of the top ten around the world.
International Speleological Congress will be held in 2017 in Sydney, Australia
Contributions are invited for the special issue on the topic of "Geophysical imaging in karst terrain", which will be published in AIMS Geosciences in 2016.
There is ongoing preparation of two interlinked activities relevant to hypogene karst: the DeepKarst 2016 Conference and the book “Selected Hypogene Karst Regions and Caves of the World".
Did you know?
That sepiolite is a cave mineral - mg4si6o15(oh)2.6h2o .?
Checkout all 2699 terms in the KarstBase Glossary of Karst and Cave Terms
Featured article from geoscience journal
The Totes Gebirge is the largest karst massif in the Northern Calcareous Alps (NCA). This paper focuses on the eastern part, where two major multiphase alpine cave systems (Burgunderschacht Cave System and DÖF–Sonnenleiter Cave System) are described with respect to morphology, hydrology, and sediments. The caves consist of Upper Miocene galleries of (epi)phreatic genesis and younger vadose canyon-shaft systems. Morphometrical analyses were used to determine the relevance of (1) cave levels (horizontal accumulations of galleries), (2) slightly inclined palaeo water tables of speleogenetic phases, (3) initial fissures, and (4) inception horizons on the development of the cave systems. (Epi)phreatic cave conduits developed preferentially along vertical faults and along only a restricted number of bedding planes, which conforms to the inception horizon hypothesis. For at least one of the systems, a development under epiphreatic conditions is certain and a hydrological behaviour in the “filling overflow manner” is likely.
Observations in further major cave systems in the Totes Gebirge identify palaeo water tables of speleogenetic phases that show inclinations of 1.5° ± 1°. Analyses of cave levels reveal distinct peaks for each cave but it is hardly possible to correlate these elevation levels between caves of different parts of the karst massif. Therefore, we conclude that cave levels (strictly horizontal) indicate speleogenetic phases or palaeo water tables respectively, but they cannot be correlated with palaeo base levels or on regional scale. An exact correlation between cave development and palaeo base levels at the surface is only possible with inclined palaeo water tables of speleogenetic phases.
For the Totes Gebirge, the inclination directions of the speleogenetic phases imply that palaeo drainage was radial and recharge was autogenic, which is in contrast to observations from other plateaus in the NCA. Differences in fracture properties seem to be the reason for the development of divergent types, according to the Four State Model. A simplified model for cave genesis and surface development in this area since the Upper Miocene is presented.