This preview shows pages 1–2. Sign up to view the full content.
This preview has intentionally blurred sections. Sign up to view the full version.View Full Document
Unformatted text preview: the Garber sandstone and Wellington formation to do Chase, Council Grove, and admire Groups possible contamination which would could cause harm to thousands in the population. Locally intense pumping has the adverse effect of causing saline water to up rise. This can cause numerous problems with the fresh water. To prevent from such matter occurring, the GWA was set up to protect the groundwater. Oklahoma government has also recommended ways of protecting the aquifer in such ways as using less fertilizers, prohibit industrialization in possible high potential of pollution of groundwater, and also to protect wetlands. Mark Sullivan Geology 1014 Section 24 October 22, 2007 Works Cited Morris, Kyle E. “Central Oklahoma Aquifer.” 2005 <http://academic.emporia.edu/schulmem/hydro/TERM %20PROJECTS/Morris/Wetland%20Soils%20history.htm>...
View Full Document
This essay was uploaded on 04/18/2008 for the course ENG 1113 taught by Professor Watkins during the Spring '08 term at Oklahoma State.
- Spring '08