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Ground Water
| Term | Definition |
|---|---|
| Permeable Rocks | Rocks that allow water to percolate freely through them. |
| Impermeable Rocks | Rocks that are made of particles so tightly packed that water can not pass through them. |
| Water Table | The upper level of the saturated ground water zone. It does not remain at a constant level. |
| Water Table Rises | After heavy rain falls. |
| Water Table Falls | During a heavy drought. |
| Spring | Any natural flow of water from the ground. Springs are held up by impermeable rock ledges. |
| Artesian Well | A well where water is naturally pushed from the ground by surface pressure. Popular in dry areas where there is little rain. |
| Oasis | A small area of water found in the desert when the water table lies close to the surface. |
| Karst | Regions that have distinctive surface features which are the result of the interaction of water and limestone. |
| Limestone | A rock composed largely of calcium carbonate that dissolves in acid. Ground water, a very weak acid dissolves limestone. As the water seeps down into the limestone, it dissolves more soluble materials. This increases the permeability of the rock. |
| Swallow Hole/Sinkhole | Holes that link caverns to the surface. |
| Doline | Steep sided depression formed when swallow holes on the surface collapse. |
| Stalagmite | A build up of calcium carbonate on the floor of a cavern. |
| Stalactite | A build up of calcium carbonate on the roof of a cavern. |
| Column/Pillar | When a stalagmite and a stalactite connect. |
| Polje | An extensive depression with a flat floor and steep walls. Formed by the coalescence of several sinkholes. Serbo-Croation word for field. |
| Terra Rossa | A type of red clay like soil produced my the weathering of limestone. Good soil for vineyards. |
| Disappearing and Reappearing Streams | Streams that meet a sinkhole and go down into a cavern and reappear in a polje or a red clay valley. |