Ice jacking

Ice jacking occurs when water invades a confined space in a structural support, or geologic formation, and upon freezing causes structural fracture as the ice expands.[1]

Geologic engineering

Rock slope failures can occur due to the presence of water; ice jacking occurs when water between joint or fissure surfaces freezes and expands. This type of failure is progressive, resulting in incremental weakening over time, often requiring several cycles before failure.[2] Ice jacking is one form of rock erosion.

See also

References

  1. Whistler reopens as officials blame ice damage for collapsed tower
  2. Xanthakos, Petros P.; Abramson, Lee W.; Bruce, Donald A. (1994). Ground Control and Improvement. New York: John Wiley. p. 737. ISBN 9780471552314.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.