Cryoseism
A cryoseism, ice quake or frost quake,
Effects
Cryoseisms are often mistaken for minor
Some reports have indicated the presence of "distant flashing lights" before or during a cryoseism, possibly because of
Occurrences
Glacial cryoseisms
A glacial cryoseism or glacial ice quake is a non-tectonic seismic event of the glacial cryosphere. A large variety of seismogenic glacial processes arising from internal, ocean calving, or basal processes have been identified and studied.[12][13] Very large calving events in Greenland and Antarctica have been observed to generate seismic events of magnitude 5 or larger.[14] Extremely large icebergs can also generate seismic signals that are observable at distances up to thousands of kilometers when they collide or grind across the ocean floor.[15] Basal glacial motion be enhanced due to water accumulation underneath a glacier sourced from surface or basal ice melt. Hydraulic pressure of subglacial water can reduce the friction at the bed, allowing the glacier to suddenly shift and generate seismic waves.[10][16] This type of cryoseism can be very brief, or may last for many minutes.[8]
Location
United States
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][7][17]
Canada
Cryoseisms also occur in Canada,
Other places
Glacier-related cryoseism phenomena have been reported in Alaska,[22] Greenland,[23] Iceland (Grímsvötn),[24] Finland,[25] Ross Island,[11] and the Antarctic Prince Charles Mountains.[26]
Precursors
There are four main precursors for a frost quake cryoseism event to occur:[1][2]
- A region must be susceptible to cold air masses
- The ground must undergo saturation from thaw or liquid precipitation prior to an intruding cold air mass
- 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 (15 cm))
- A rapid temperature drop from approximately freezing to near or below −18 °C (0 °F), which ordinarily occurred on a timescale of 16 to 48 hours.[1]
Cryoseisms typically occur when temperatures rapidly decrease from above freezing to
See also
References
- ^ S2CID 194149546.
- ^ ISBN 978-3-319-51628-8, retrieved 2024-01-19
- ^ "Milwaukee Area Frostquakes". University of Wisconsin–Milwaukee. 1994-02-24. Archived from the original on 2007-01-04. Retrieved 2006-10-22.
- ^ 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.
- ^ doi:10.1785/gssrl.51.1.15. Archived from the originalon 2007-01-04. Retrieved 2006-10-21.
- ^
Kavanaugh, Jeffrey; Schultz, Ryan; Andriashek, Laurence D.; van der Baan, Mirko; Ghofrani, Hadi; Atkinson, Gail; Utting, Daniel J. (2019). "A New Year's Day icebreaker: icequakes on lakes in Alberta, Canada". Canadian Journal of Earth Sciences. 56 (2): 183–200. ISSN 0008-4077.
- ^ 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.
- ^ a b Irvine, Tom (June 2006). "Ice Quakes" (PDF). Vibrationdata Newsletter. Archived (PDF) from the original on 2018-05-04. Retrieved 2006-11-16.
- ^ 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.
- ^ 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.
- ^ a b "Erebus Icequakes". Mount Erebus Volcano Observatory. Archived from the original on 2006-08-31. Retrieved 2006-11-16.
- ISSN 8755-1209.
- PMID 28782729.
- ISSN 0084-6597.
- ^
Martin, Seelye; Drucker, Robert; Aster, Richard; Davey, Fred; Okal, Emile; Scambos, Ted; MacAyeal, Douglas (2010). "Kinematic and seismic analysis of giant tabular iceberg breakup at Cape Adare, Antarctica". Journal of Geophysical Research: Solid Earth. 115 (B6). ISSN 0148-0227.
- ^ 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.
- ^ Tuohy, John (31 Jan 2019). "Ground-shaking frost quakes: They're Indiana's latest polar vortex phenomenon". Indianapolis Star.
- ^ a b "'Frost quakes' wake Toronto residents on cold night". CBC News. 2014-01-03. Archived from the original on 2017-02-15.
- ^ "Frequently Asked Questions about Earthquakes (FAQ)". Natural Resources Canada. Archived from the original on 2019-01-05.
- .
- ^ 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.
- ^ "Alaska Glacier Tours – Know What To Look For". Alaska.org. Archived from the original on 2012-07-22. Retrieved 2006-11-16.
- ^ Гренландские ледники трещат по швам. Bigli Facts (in Russian). Bigli Web. Archived from the original on 2007-01-16. Retrieved 2006-10-22.
- ThinkQuest Library. Archived from the originalon 2006-11-15. Retrieved 2006-11-16.
- ^ "New Data Helps Researchers Demystify 'Frost Quakes'". Inside Science. 11 November 2020. Retrieved 2022-10-20.
- ^ 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.
- ^ 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.
External links
- Media related to Cryoseisms at Wikimedia Commons
- Google Maps-based reporting website