Sinkhole
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This article originated from the Critical Issues Program authored by the American Geosciences Institute. To learn more about AGI or the Critical Issues Program, visit http://www.americangeosciences.org/critical-issues. |
Most sinkholes occur in places where water can dissolve the rock below the surface, for example where the bedrock is limestone, salt, or gypsum. They can collapse very quickly, or slump slowly over time. Many sinkholes occur naturally, but human activities can also cause them. Over-pumping of groundwater and leaking pipes beneath roads and buildings are common causes of artificial sinkholes.
Contents
Why do sinkholes matter?
Like landslides, sinkholes can devastate small areas. Natural sinkholes are a potential threat throughout 20% of the United States.[1] Florida, Texas, Alabama, Missouri, Kentucky, Tennessee, and Pennsylvania are most sinkhole-prone because of their bedrock. Human-induced sinkholes can develop anywhere due to careless practices.
How does geoscience help?
Geoscientists study how sinkholes form in order to warn the public. They make maps identifying the types of bedrock where sinkholes are likely to form so that homeowners and public officials can understand their local risks.
Introductory resources
- Living with Karst - A Fragile Foundation, American Geosciences Institute
- This booklet illustrates what karst is and why karst areas are important. It also discusses karst-related environmental and engineering concerns, guidelines for living with karst, and highlights sources of additional information.
Frequent questions
References
- ↑ U.S. Geological Survey, 2013, The Science of Sinkholes, Web Feature, http://www.usgs.gov/blogs/features/usgs_top_story/the-science-of-sinkholes/?from=textlink
See also
- Sinkhole Basics, American Geosciences Institute
- Drought
- Earthquake
- Flood
- Landslide
- Tsunami
- Volcano
- Waste management
- Weather hazards
External links
| find literature about Sinkhole |
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