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- Hydrogeological and Environmental Investigations in Karst Systems
- Karst Hydrogeology and Geomorphology: A virtual field experience using Google Earth, GIS, and TAK
- Karst Geomorphology and Hydrology
- Karst Hydrogeology & Geomorphology
Hydrogeological and Environmental Investigations in Karst Systems
It seems that you're in Germany. We have a dedicated site for Germany. Authors: Ford , D. The karst minerals are all congruent in normal conditions. Incongruent solution of dolomite and precipitation of calcite may occur in some exceptional conditions mentioned later. The sample of congruent minerals in Table 3. Gibbsite is an example that is insoluble to all intents and purposes; even in the most favourable circumstances encountered on the surface of this planet physical processes will disaggregate it and remove it as colloids or larger grains before there is significant solution damage.
Ford and William B. White Author s : Russell S. Harmon, Carol M. Sign In or Create an Account. User Tools. Sign In.
Originally published in , Karst Geomorphology and Hydrology became the leading textbook on karst studies. This new textbook has been substantially revised and updated. The first half of the book is a systematic presentation of the dissolution kinetics, chemical equilibria and physical flow laws relating to karst environments. It includes details of the many environmental factors that complicate their chemical evolution, with a critique of measurement of karst erosion rates. The second half of the book looks at the classification system for cave systems and the influence of climate and climatic change on karst development. The book ends with chapters on karst water resource management and a look at the important issues of environmental management, including environmental impact assessment, environmental rehabilitation, tourism impacts and conservation values. Practical applications of karst studies are explained throughout the text.
Karst Hydrogeology and Geomorphology: A virtual field experience using Google Earth, GIS, and TAK
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Karst Geomorphology and Hydrology
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Karst is a topography formed from the dissolution of soluble rocks such as limestone , dolomite , and gypsum. It is characterized by underground drainage systems with sinkholes and caves. However, in regions where the dissolved bedrock is covered perhaps by debris or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The English word karst was borrowed from German Karst in the late 19th century,  which entered German much earlier.
Karst Hydrogeology & Geomorphology
Resources in this top level collection have received Exemplary or Very Good scores in all five elements of review, and also rate as Exemplary in at least three elements. The five elements included in the peer review process are:. Students will have the opportunity to select and virtually explore the hydrogeology and geomorphology of a karst landscape using Google Earth or perhaps Google Mars or Google Moon if they so choose , lidar data-sourced DEM s , geologic maps, GIS software, and topographic analysis software packages such that they gain an understanding of karst landscapes and their associated hazard risks, access to and analysis of internet-based remote sensing data, design of field strategy, and verbal and written communication of scientific information. If you have already completed the introductory activity, use your results from that activity and continue onto this activity, doing step 2. What field, laboratory, or numerical techniques would be required to obtain the data you need? Please be specific as if you were planning for field work, lab work, or numerical modeling. A walk-through for this activity, including screenshots for each step, is included in the uploaded documents.
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