Cave in
Cave-in
A cave-in occurs when a geological formation collapses, causing the ground to sink or a structure to fall. This phenomenon is often associated with mining, tunneling, and construction activities, but can also occur naturally in karst landscapes where limestone is dissolved by water, creating underground voids.
Causes[edit | edit source]
Cave-ins can be caused by a variety of factors, including:
- Natural Erosion: The dissolution of soluble rocks such as limestone, gypsum, and salt by water can create underground voids that eventually collapse.
- Mining Activities: The removal of material from underground mines can lead to instability and collapse.
- Construction: Excavation and tunneling without proper support can result in cave-ins.
- Seismic Activity: Earthquakes and other seismic events can destabilize the ground, leading to cave-ins.
Prevention[edit | edit source]
Preventing cave-ins involves several strategies:
- Proper Support: Using shoring, bracing, and other support systems during excavation and construction.
- Monitoring: Regularly monitoring ground conditions and using geotechnical engineering techniques to assess stability.
- Regulations: Adhering to safety regulations and guidelines set by organizations such as the Occupational Safety and Health Administration (OSHA).
Notable Incidents[edit | edit source]
Several notable cave-ins have occurred throughout history, including:
- The Quecreek Mine Rescue in 2002, where nine miners were trapped underground in Pennsylvania.
- The San José Mine collapse in 2010, which trapped 33 miners in Chile for 69 days.
Related Pages[edit | edit source]
- Sinkhole
- Subsidence
- Geotechnical engineering
- Mining safety
- Occupational Safety and Health Administration
See Also[edit | edit source]
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Contributors: Prab R. Tumpati, MD