What is the Karst Information Portal?

The Karst Information Portal is a digital library linking scientists, managers, and explorers with quality information resources concerning karst environments. The karst research community and its knowledge base are globally distributed and highly interdisciplinary -- information integration and linkages promoting collaboration and connectivity among researchers is essential.

Search the Web for Karst Information

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Browse Conferences & Meetings

***Beta Site Under Construction***
For full access, visit the existing site at www.karstportal.org

New Resources
Go to Demystifying ground-water flow and contaminant movement in karst systems using chemical and isotopic tracers
http://water.usgs.gov/ogw/karst/kig2002/bgk_demystifying.htm...
Conference on the karst and cave research activities of education and research institutions in Hungary: papers: Josvafo 17-19 May 1991
From Northup et al, 1998; review required.
Go to Overview of background resources on karst research emphasizing obscure and "gray area" documents
Overview of background resources on karst research emphasizing obscure and "gray area" documents
From USGS Water-Resources Investigations Report 02-4174. The in-depth understanding of karst is a narrow subspecialty of geology falling within the areas of hydrogeology and/or geomorphology.
http://water.usgs.gov/ogw/karst/kig2002/bfb_overview.html
Go to Application of Seismic Refraction Tomography to Karst Cavities
Application of Seismic Refraction Tomography to Karst Cavities
From U.S. Geological Survey Scientific Investigations Report 2005-5160. For three years we have used synthetic and field data to investigate the effectiveness of commercial refraction tomography...
http://pubs.usgs.gov/sir/2005/5160/PDF/Part1_2.pdf
Go to Records of carbon and oxygen isotopes and paleoclimate reconstruction from a stalagmite from Shuinan Cave, Guilin
Records of carbon and oxygen isotopes and paleoclimate reconstruction from a stalagmite from Shuinan Cave, Guilin
The time sequence of palaeclimatic change from 245.2 ka B.P. to 147.9 ka B.P. has been established by the dating ages of the high precision TIMS-U series and the analysis of oxygen isotopes from...
http://www.pages.unibe.ch/cgi-bin/WebObjects/abstracts.woa/w...

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