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Introduction: the initial conditions. Progressive permeability / porous aquifers5 conditions:Soluble and fissured rock (limestone?)Water (solvent, transport)Acidity (CO2 from vegetation)Hydraulic headand time?Large karst development in:Wet regions (rain vegetation)Mountains (topographic
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2. Introduction: the initial conditions Progressive permeability / porous aquifers
5 conditions:
Soluble and fissured rock (limestone
)
Water (solvent, transport)
Acidity (CO2 from vegetation)
Hydraulic head
and time
Large karst development in:
Wet regions (rain + vegetation)
Mountains (topographic gradient) / plateau (long evolution)
3. Karst development and speleogenesis 1 An organized aquifer
2 An evolutive dynamic
3 Vertical cave pattern
4. An organized aquifer1.1. Karst inception
5. An organized aquifer1.2. Vertical organization
6. An organized aquifer1.2. Vertical organization
7. An organized aquifer1.3. Perched vs. dammed karst
8. 2. An evolutive dynamic2.1. Information from recession curves
9. 2. An evolutive dynamic2.2. Exchanges: drain ? annex systems
10. 2. An evolutive dynamic2.3. Karst aquifers classification [after Mangin]
11. 3. Vertical cave pattern3.1. Main types of vertical cave pattern
12. 3. Vertical cave pattern3.1. Main types of vertical cave pattern
13. 3. Vertical cave pattern3.1. Main types of vertical cave pattern
14. 3. Vertical cave pattern3.1. Main types of vertical cave pattern
15. 3. Vertical cave pattern3.1. Main types of vertical cave pattern
16. 3. Vertical cave pattern3.2. Influence of base level changes
17. 3. Vertical cave pattern3.2. Influence of base level changes (lowering)
18. 3. Vertical cave pattern3.2. Influence of base level changes (rising)
19. 3. Vertical cave pattern3.2. Influence of base level changes (rising)
20. 3. Vertical cave pattern3.2. Influence of base level changes (rising)
21. Conclusion