Cryoseism

{{Redirect|Ice quake|the 2010 film|Ice Quake (film)|the 2010 novel|SOS Adventures#Ice Quake{{!}}Ice Quake (novel)}}

A cryoseism, ice quake or frost quake,{{Cite journal|last1=Battaglia|first1=Steven M.|last2=Changnon|first2=David|date=2016-01-02|title=Frost Quakes: Forecasting the Unanticipated Clatter|url=https://archive.org/details/BattagliaChangnon2016FrostQuakes|journal=Weatherwise|volume=69|issue=1|pages=20–27|doi=10.1080/00431672.2015.1109984|bibcode=2016Weawi..69a..20B|s2cid=194149546|issn=0043-1672}}{{Citation|last1=Leung|first1=Andrew C. W.|title=Identifying Frostquakes in Central Canada and Neighbouring Regions in the United States with Social Media|date=2017|work=Citizen Empowered Mapping|volume=18|pages=201–222|editor-last=Leitner|editor-first=Michael|url=http://link.springer.com/10.1007/978-3-319-51629-5_9|access-date=2024-01-19|place=Cham|publisher=Springer International Publishing|doi=10.1007/978-3-319-51629-5_9|isbn=978-3-319-51628-8|last2=Gough|first2=William A.|last3=Shi|first3=Yehong|editor2-last=Jokar Arsanjani|editor2-first=Jamal}}{{cite web|url=http://www.uwm.edu/Dept/Geosciences/qketour/frostqke/cryoseis.html|title=Milwaukee Area Frostquakes|date=1994-02-24|publisher=University of Wisconsin–Milwaukee|archive-url=https://web.archive.org/web/20070104124542/http://www.uwm.edu/Dept/Geosciences/qketour/frostqke/cryoseis.html|archive-date=2007-01-04|url-status=dead|access-date=2006-10-22}}{{cite web|url=https://www.maine.gov/dacf/mgs/hazards/earthquakes/quake-cryoseism.htm|title=Cryoseisms in Maine|date=2005-10-06|publisher=Maine Geological Survey|archive-url=https://web.archive.org/web/20180426130312/https://www.maine.gov/dacf/mgs/hazards/earthquakes/quake-cryoseism.htm|archive-date=2018-04-26|url-status=live|access-date=2006-10-21}} is a seismic event caused by a sudden cracking action in frozen soil or rock saturated with water or ice,{{cite journal|author=Lacroix|first=Andrew V.|date=January 1980|title=A Short Note on Cryoseisms|url=http://www.uwm.edu/Dept/Geosciences/qketour/frostqke/lacroix.html|url-status=dead|journal=Seismological Research Letters|volume=51|issue=1|pages=15–21|doi=10.1785/gssrl.51.1.15|bibcode=1980SeiRL..51a..15L|archive-url=https://web.archive.org/web/20070104124323/http://www.uwm.edu/Dept/Geosciences/qketour/frostqke/lacroix.html|archive-date=2007-01-04|access-date=2006-10-21}} or by stresses generated at frozen lakes.

{{Cite journal|last1=Kavanaugh|first1=Jeffrey|last2=Schultz|first2=Ryan|last3=Andriashek|first3=Laurence D.|last4=van der Baan|first4=Mirko|last5=Ghofrani|first5=Hadi|last6=Atkinson|first6=Gail|last7=Utting|first7=Daniel J.|date=2019|title=A New Year's Day icebreaker: icequakes on lakes in Alberta, Canada|url=http://dx.doi.org/10.1139/cjes-2018-0196|journal=Canadian Journal of Earth Sciences|volume=56|issue=2|pages=183–200|doi=10.1139/cjes-2018-0196|bibcode=2019CaJES..56..183K|issn=0008-4077|hdl=1807/93572|hdl-access=free}}

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.{{cite web|url=http://weathernotebook.org/transcripts/2000/04/14.html|title=Cryoseisms Explained|author=Thurlow|first=Dave|work=The Weather Notebook|publisher=Mount Washington Observatory|archive-url=https://web.archive.org/web/20051124034552/http://www.weathernotebook.org/transcripts/2000/04/14.html|archive-date=2005-11-24|url-status=dead|access-date=2006-10-21}}

The requirements for a cryoseism to occur are numerous; 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. Speculation has been made between global warming and the frequency of cryoseisms.

Effects

Cryoseisms are often mistaken for minor intraplate earthquakes.{{cite report|url=https://dec.vermont.gov/sites/dec/files/geo/HazDocs/Ebell_1995.pdf|title=A Report on the Seismic Vulnerability of the State of Vermont|last1=Ebel|first1=John E.|last2=Bedell|first2=Richard|date=July 1995|publisher=Vermont Emergency Management Agency|last3=Urzua|first3=Alfredo|access-date=2006-10-22|archive-url=https://web.archive.org/web/20170430035840/https://dec.vermont.gov/sites/dec/files/geo/HazDocs/Ebell_1995.pdf|archive-date=2017-04-30|url-status=live}} Initial indications may appear similar to those of an earthquake with tremors, vibrations, ground cracking and related noises, such as thundering or booming sounds. Cryoseisms can, however, be distinguished from earthquakes through meteorological and geological conditions. Cryoseisms can have an intensity of up to VI on the Modified Mercalli Scale. Furthermore, cryoseisms often exhibit high intensity in a very localized area, in the immediate proximity of the epicenter, as compared to the widespread effects of an earthquake. Due to lower-frequency vibrations of cryoseisms, some seismic monitoring stations may not record their occurrence. Cryoseisms release less energy than most tectonic events.{{cite web|url=http://www.ees.nmt.edu/Geop/mevo/seismic/icequakes.html|title=Erebus Icequakes|publisher=Mount Erebus Volcano Observatory|archive-url=https://web.archive.org/web/20060831112521/http://www.ees.nmt.edu/Geop/mevo/seismic/icequakes.html|archive-date=2006-08-31|url-status=dead|access-date=2006-11-16}} Since cryoseisms occur at the ground surface they can cause effects right at the site, enough to jar people awake.

Some reports have indicated the presence of "distant flashing lights" before or during a cryoseism, possibly because of electrical changes when rocks are compressed. Cracks and fissures may also appear as surface areas contract and split apart from the cold. 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.

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.{{Cite journal|last1=Podolskiy|first1=Evgeny A.|last2=Walter|first2=Fabian|date=2016|title=Cryoseismology|url=https://agupubs.onlinelibrary.wiley.com/doi/10.1002/2016RG000526|journal=Reviews of Geophysics|volume=54|issue=4|pages=708–758|doi=10.1002/2016RG000526|bibcode=2016RvGeo..54..708P|issn=8755-1209|hdl=2115/64330|hdl-access=free}}{{Cite journal|last1=Aster|first1=R C|last2=Winberry|first2=J P|date=2017-12-01|title=Glacial seismology|url=https://iopscience.iop.org/article/10.1088/1361-6633/aa8473|journal=Reports on Progress in Physics|volume=80|issue=12|pages=126801|doi=10.1088/1361-6633/aa8473|pmid=28782729|bibcode=2017RPPh...80l6801A|issn=0034-4885}}

Very large calving events in Greenland and Antarctica have been observed to generate seismic events of magnitude 5 or larger.{{Cite journal|last1=Nettles|first1=Meredith|last2=Ekström|first2=Göran|date=2010-04-01|title=Glacial Earthquakes in Greenland and Antarctica|url=https://www.annualreviews.org/doi/10.1146/annurev-earth-040809-152414|journal=Annual Review of Earth and Planetary Sciences|volume=38|issue=1|pages=467–491|doi=10.1146/annurev-earth-040809-152414|bibcode=2010AREPS..38..467N|issn=0084-6597}}

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.

{{Cite journal|last1=Martin|first1=Seelye|last2=Drucker|first2=Robert|last3=Aster|first3=Richard|last4=Davey|first4=Fred|last5=Okal|first5=Emile|last6=Scambos|first6=Ted|last7=MacAyeal|first7=Douglas|date=2010|title=Kinematic and seismic analysis of giant tabular iceberg breakup at Cape Adare, Antarctica|url=https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2009JB006700|journal=Journal of Geophysical Research: Solid Earth|volume=115|issue=B6|doi=10.1029/2009JB006700|bibcode=2010JGRB..115.6311M|issn=0148-0227}}

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.{{cite web|url=http://amos.indiana.edu/library/scripts/icequake.html|title=Ice Quake!|author=Orem|first=William|date=2004-09-14|work=A Moment of Science|publisher=Indiana University|archive-url=https://web.archive.org/web/20080227051716/http://amos.indiana.edu/library/scripts/icequake.html|archive-date=2008-02-27|url-status=dead|access-date=2006-11-16}}{{cite web|url=http://www.postnormaltimes.net/blog/archives/2006/03/climate_and_eco.html|title=Climate and economic models|author=Tognetti|first=Sylvia S.|date=2006-03-27|work=The Post-Normal Times|access-date=2006-11-16|archive-url=https://web.archive.org/web/20070928102722/http://www.postnormaltimes.net/blog/archives/2006/03/climate_and_eco.html|archive-date=2007-09-28|url-status=dead}} This type of cryoseism can be very brief, or may last for many minutes.{{cite web|url=http://www.vibrationdata.com/Newsletters/June2006_NL.pdf|title=Ice Quakes|author=Irvine|first=Tom|date=June 2006|work=Vibrationdata Newsletter|archive-url=https://web.archive.org/web/20180504021145/http://www.vibrationdata.com/Newsletters/June2006_NL.pdf|archive-date=2018-05-04|url-status=live|access-date=2006-11-16}}

= Location =

== United States ==

Image:US states with reported cryoseisms - updated.PNG

Geocryological processes were identified as a possible cause of tremors as early as 1818. In the United States, such events have been reported throughout the Midwestern, Northern and Northeastern United States.{{cite news|date=31 Jan 2019|title=Ground-shaking frost quakes: They're Indiana's latest polar vortex phenomenon|url=https://www.indystar.com/story/news/local/hamilton-county/2019/01/31/indianas-latest-polar-vortex-phenomenon-ground-shaking-frost-quakes/2732546002/|last=Tuohy|first=John|work=Indianapolis Star}}

== Canada ==

Cryoseisms also occur in Canada, especially along the Great Lakes/St. Lawrence corridor, where winter temperatures can shift very rapidly.{{Cite news|url=https://www.cbc.ca/news/canada/toronto/frost-quakes-wake-toronto-residents-on-cold-night-1.2482615|title='Frost quakes' wake Toronto residents on cold night|date=2014-01-03|work=CBC News|archive-url=https://web.archive.org/web/20170215233214/http://www.cbc.ca/news/canada/toronto/frost-quakes-wake-toronto-residents-on-cold-night-1.2482615|archive-date=2017-02-15|url-status=live}}{{cite web|url=http://www.earthquakescanada.nrcan.gc.ca/info-gen/faq-eng.php#temperature|title=Frequently Asked Questions about Earthquakes (FAQ)|publisher=Natural Resources Canada|archive-url=https://web.archive.org/web/20190105204019/http://www.earthquakescanada.nrcan.gc.ca/info-gen/faq-en.php|archive-date=2019-01-05|url-status=live}} They have surfaced in Ontario, Quebec, Alberta and the Maritime Provinces.{{cite journal|last=Burke|first=Kenneth B. S.|title=Historical Seismicity in the Central Highlands, Passamaquoddy Bay, and Moncton Regions of New Brunswick, Canada, 1817–1961|url=https://archive.org/details/HistoricalSeismicityInTheCentralHighlands|journal=Seismological Research Letters|date=May 2004|volume=75|issue=3|pages=419–431|doi=10.1785/gssrl.75.3.419|bibcode=2004SeiRL..75..419B}}{{cite news|url=https://calgary.ctvnews.ca/possible-epicenter-of-frost-quake-found-in-northwest-schoolyard-1.1722711|title=Possible epicenter of frost quake found in northwest schoolyard|last=Lawrence|first=Erin|date=2014-03-10|work=CTV News Calgary|archive-url=https://web.archive.org/web/20170726025109/https://calgary.ctvnews.ca/possible-epicenter-of-frost-quake-found-in-northwest-schoolyard-1.1722711|archive-date=2017-07-26|url-status=live}}

== Other places ==

Glacier-related cryoseism phenomena have been reported in Alaska,{{cite web|url=http://www.alaska.org/glaciers/advice-know-what-to-look.htm|title=Alaska Glacier Tours – Know What To Look For|website=Alaska.org|archive-url=https://web.archive.org/web/20120722025223/http://www.alaska.org/glaciers/advice-know-what-to-look.htm|archive-date=2012-07-22|url-status=live|access-date=2006-11-16}} Greenland,{{cite web|url=http://facts.bigli.ru/2/fact-348/|script-title=ru:Гренландские ледники трещат по швам|access-date=2006-10-22|work=Bigli Facts|publisher=Bigli Web|language=ru|url-status=dead|archive-url=https://web.archive.org/web/20070116195326/http://facts.bigli.ru/2/fact-348/|archive-date=2007-01-16}} Iceland (Grímsvötn),{{cite web|url=http://library.thinkquest.org/03oct/00421/izland_k_eng.htm|title=The Icelandic "Icy Flood"|last=Gyula|first=Honyek|date=October 2003|work=ThinkQuest Library|archive-url=https://web.archive.org/web/20061115072803/http://library.thinkquest.org/03oct/00421/izland_k_eng.htm|archive-date=2006-11-15|url-status=dead|access-date=2006-11-16}} Finland,{{Cite web|title=New Data Helps Researchers Demystify 'Frost Quakes'|url=https://www.insidescience.org/news/new-data-helps-researchers-demystify-frost-quakes|access-date=2022-10-20|website=Inside Science|date=11 November 2020}} Ross Island, and the Antarctic Prince Charles Mountains.{{cite news|url=http://abc.net.au/news/specials/antarcticsummer/stories/pcmega.htm|title=Surveying the Icy Peaks|author=Johnston|first=Nicole|date=2002-11-29|work=Antarctic Summer|access-date=2006-11-16|archive-url=https://web.archive.org/web/20051119154630/http://www.abc.net.au/news/specials/antarcticsummer/stories/pcmega.htm|archive-date=November 19, 2005|url-status=dead|publisher=ABC News|location=Australia}}

= Precursors =

There are four main precursors for a frost quake cryoseism event to occur:

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 {{convert|6|in|cm}})
A rapid temperature drop from approximately freezing to near or below {{convert|-18|C}}, which ordinarily occurred on a timescale of 16 to 48 hours.

Cryoseisms typically occur when temperatures rapidly decrease from above freezing to subzero, and are more than likely to occur between midnight and dawn (during the coldest parts of night). However, due to the permanent nature of glacial ice, glacier-related cryoseisms may also occur in the warmer months of summer. In general, cryoseisms may occur 3 to 4 hours after significant changes in temperature.{{cite web|url=http://www.uwm.edu/Dept/Geosciences/qketour/frostqke/willis2.html|title=Icequake Precursors|last1=Willis|first1=D. E.|last2=Taylor|first2=R. W.|date=October 1979|work=51st Annual Meeting of the Eastern Section of the Seismological Society of America|publisher=Dept of Geological Sciences, University of Wisconsin–Milwaukee|archive-url=https://web.archive.org/web/19990921075700/http://www.uwm.edu/Dept/Geosciences/qketour/frostqke/willis2.html|archive-date=1999-09-21|url-status=dead|access-date=2006-11-16|last3=LeNoble|first3=M.|last4=Yellin|first4=S.}} 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. Geologically, areas of permeable materials like sand or gravel, which are susceptible to frost action, are likelier candidates for cryoseisms. Following large cryoseisms, little to no seismic activity will be detected for several hours, indicating that accumulated stress has been relieved.