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A cryoseism, also known as an ice quake or a frost quake,[1][2][3][4] is a seismic event that may be caused by a sudden cracking action in frozen soil or rock saturated with water or ice.[5] As water drains into the ground, it may eventually freeze and expand under colder temperatures, putting stress on its surroundings. This stress builds up until relieved explosively in the form of a cryoseism.[1][6]

Another type of cryoseism is a non-tectonic seismic event caused by sudden glacial movements. This movement has been attributed to a veneer of water which may pool underneath a glacier sourced from surface ice melt. Hydraulic pressure of the liquid can act as a lubricant, allowing the glacier to suddenly shift position.[7][8] This type of cryoseism can be very brief, or may last for several minutes.[9]

The requirements for a cryoseism to occur are numerous;[1][2] therefore, accurate predictions are not entirely possible and may constitute a factor in structural design and engineering when constructing in an area historically known for such events.[5] Speculation has been made between global warming and the frequency of cryoseisms.[2][9]


Cryoseisms are often mistaken for minor intraplate earthquakes.[5][10] Initial indications may appear similar to those of an earthquake with tremors, vibrations, ground cracking and related noises,[4] such as thundering or booming sounds.[6] Cryoseisms can, however, be distinguished from earthquakes through meteorological and geological conditions.[5] Cryoseisms can have an intensity of up to VI on the Modified Mercalli Scale.[5] Furthermore, cryoseisms often exhibit high intensity in a very localized area,[4] in the immediate proximity of the epicenter,[10] as compared to the widespread effects of an earthquake.[5] Due to lower-frequency vibrations of cryoseisms,[7] some seismic monitoring stations may not record their occurrence.[10] Cryoseisms release less energy than most tectonic events. [11] Since cryoseisms occur at the ground surface they can cause effects right at the site, enough to jar people awake.[4]

Some reports have indicated the presence of "distant flashing lights" before or during a cryoseism, possibly because of electrical changes when rocks are compressed.[6] Cracks and fissures may also appear as surface areas contract and split apart from the cold.[4][10] The sometime superficial to moderate occurrences may range from a few centimeters to several kilometers long, with either singular or multiple linear fracturing and vertical or lateral displacement possible.[5]



United States[edit]

US States with reported cryoseisms.

Geocryological processes were identified as a possible cause of tremors as early as 1818.[1][5] In the United States, such events have been reported throughout the Midwestern, Northern and Northeastern United States.[1][6][12]


Cryoseisms also occur in Canada,[1][2] especially along the Great Lakes/St. Lawrence corridor, where winter temperatures can shift very rapidly.[13][14] They have surfaced in Ontario, Quebec and the Maritime Provinces.[13][15] They are also observed in Calgary.[16]

Other Places[edit]

Glacier-related cryoseism phenomena have been reported in Alaska,[17] Greenland,[18] Iceland (Grímsvötn).,[19] Ross Island,[11] and the Antarctic Prince Charles Mountains.[20]


There are four main precursors for a frost quake cryoseism event to occur:[1][2] (1) a region must be susceptible to cold air masses, (2) the ground must undergo saturation from thaw or liquid precipitation prior to an intruding cold air mass, (3) most frost quakes are associated with minor snow cover on the ground without a significant amount of snow to insulate the ground (i.e., less than 6 inches), and (4) a rapid temperature drop from approximately freezing to near or below zero degrees Fahrenheit, which ordinarily occurred on a timescale of 16 to 48 hours.[1]

Cryoseisms typically occur when temperatures rapidly decrease from above freezing to subzero,[4][10] and are more than likely to occur between midnight and dawn (during the coldest parts of night).[1][5] [However, due to the permanent nature of glacial ice, glacier-related cryoseisms may also occur in the warmer months of summer.][7] In general, cryoseisms may occur 3 to 4 hours after significant changes in temperature.[21] Perennial or seasonal frost conditions involved with cryoseisms limit these events to temperate climates that experience seasonal variation with subzero winters. Additionally, the ground must be saturated with water, which can be caused by snowmelt, rain, sleet or flooding.[5] Geologically, areas of permeable materials like sand or gravel, which are susceptible to frost action, are likelier candidates for cryoseisms.[5] Following large cryoseisms, little to no seismic activity will be detected for several hours, indicating that accumulated stress has been relieved.[21]

See also[edit]


  1. ^ a b c d e f g h i Battaglia, Steven M.; Changnon, David (2016-01-02). "Frost Quakes: Forecasting the Unanticipated Clatter". Weatherwise. 69 (1): 20–27. doi:10.1080/00431672.2015.1109984. ISSN 0043-1672.
  2. ^ a b c d e Battaglia, Steven M.; Changnon, David (2016-06-01). "Frost Quake Events and Changing Wintertime Air Mass Frequencies in Southeastern Canada". doi:10.13140/RG.2.2.22351.48803.
  3. ^ "Milwaukee Area Frostquakes". University of Wisconsin–Milwaukee. 1994-02-24. Archived from the original on 2007-01-04. Retrieved 2006-10-22.
  4. ^ a b c d e f "Cryoseisms in Maine". Maine Geological Survey. 2005-10-06. Archived from the original on 2018-04-26. Retrieved 2006-10-21.
  5. ^ a b c d e f g h i j k Lacroix, Andrew V. (January 1980). "A Short Note on Cryoseisms". Seismological Research Letters. 51 (1): 15–21. doi:10.1785/gssrl.51.1.15. Archived from the original on 2007-01-04. Retrieved 2006-10-21.
  6. ^ a b c d Thurlow, Dave. "Cryoseisms Explained". The Weather Notebook. Mount Washington Observatory. Archived from the original on 2005-11-24. Retrieved 2006-10-21.
  7. ^ a b c Orem, William (2004-09-14). "Ice Quake!". A Moment of Science. Indiana University. Archived from the original on 2008-02-27. Retrieved 2006-11-16.
  8. ^ Tognetti, Sylvia S. (2006-03-27). "Climate and economic models". The Post-Normal Times. Archived from the original on 2007-09-28. Retrieved 2006-11-16.
  9. ^ a b Irvine, Tom (June 2006). "Ice Quakes" (PDF). Vibrationdata Newsletter. Archived (PDF) from the original on 2018-05-04. Retrieved 2006-11-16.
  10. ^ a b c d e Ebel, John E.; Bedell, Richard; Urzua, Alfredo (July 1995). A Report on the Seismic Vulnerability of the State of Vermont (PDF) (Report). Vermont Emergency Management Agency. Archived (PDF) from the original on 2017-04-30. Retrieved 2006-10-22.
  11. ^ a b "Erebus Icequakes". Mount Erebus Volcano Observatory. Archived from the original on 2006-08-31. Retrieved 2006-11-16.
  12. ^ Tuohy, John (31 Jan 2019). "Ground-shaking frost quakes: They're Indiana's latest polar vortex phenomenon". Indianapolis Star.
  13. ^ a b "'Frost quakes' wake Toronto residents on cold night". CBC News. 2014-01-03. Archived from the original on 2017-02-15.
  14. ^ "Frequently Asked Questions about Earthquakes (FAQ)". Natural Resources Canada. Archived from the original on 2019-01-05.
  15. ^ Burke, Kenneth B. S. (May 2004). "Historical Seismicity in the Central Highlands, Passamaquoddy Bay, and Moncton Regions of New Brunswick, Canada, 1817–1961". Seismological Research Letters. 75 (3): 419–431. doi:10.1785/gssrl.75.3.419.
  16. ^ Lawrence, Erin (2014-03-10). "Possible epicenter of frost quake found in northwest schoolyard". CTV News Calgary. Archived from the original on 2017-07-26.
  17. ^ "Alaska Glacier Tours – Know What To Look For". Archived from the original on 2012-07-22. Retrieved 2006-11-16.
  18. ^ Гренландские ледники трещат по швам. Bigli Facts (in Russian). Bigli Web. Archived from the original on 2007-01-16. Retrieved 2006-10-22.
  19. ^ Gyula, Honyek (October 2003). "The Icelandic "Icy Flood"". ThinkQuest Library. Archived from the original on 2006-11-15. Retrieved 2006-11-16.
  20. ^ Johnston, Nicole (2002-11-29). "Surveying the Icy Peaks". Antarctic Summer. ABC News. Archived from the original on November 19, 2005. Retrieved 2006-11-16.
  21. ^ a b Willis, D. E.; Taylor, R. W.; LeNoble, M.; Yellin, S. (October 1979). "Icequake Precursors". 51st Annual Meeting of the Eastern Section of the Seismological Society of America. Dept of Geological Sciences, University of Wisconsin–Milwaukee. Archived from the original on 1999-09-21. Retrieved 2006-11-16.

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