| previous |
4 of 4 |
Ground water in karst terrains is contaminated easily because the surface waters are channeled rapidly into the subsurface at sinkholes and swallowholes. These waters then flow underground without the benefit of filtration or exposure to sunlight, which might remove or kill some organic contaminants. Eventually, the ground water exits at springs. Contaminants from livestock feeder lots, agricultural pesticides, poorly managed industrial plants, leaking gasoline tanks or spills, septic fields, and sewage plants may be discharged at these springs without being adequately diluted. Wastes located in sinkholes, including dead livestock, discarded chemical containers, waste oil, and batteries also can be washed into the underground conduit and cavern systems.
|
| previous |
4 of 4 |
Geology | GIS/Maps | About Us | Bookstore | Interactive Maps | Licensing
IGSInfo@indiana.edu / 812-855-7636
Accessibility Information
Copyright, Map Disclaimer, and Limitation of Warranties and Liability