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{{Short description|Earthquake and tsunami in eastern Canada}}
{{Use mdy dates|date=August 2023}}
{{Infobox earthquake {{Infobox earthquake
| timestamp = 1929-11-18 20:32:00
| title = 1929 Grand Banks earthquake
| anss-url = iscgem908394
| isc-event = 908394
| caption = | caption =
| date = {{start-date|November 18, 1929|November 18, 1929}}
| origintime = 20:32 UTC {{Sfn|Engdahl|2016}}
| map2 = {{Location map+ | Canada | relief = 1 | map2 = {{Location map+ | Canada | relief = 1
|places = |places =
Line 10: Line 12:
| float = right | float = right
| caption = }} | caption = }}
| local-date = {{start date text|November 18, 1929|November 18, 1929}}
| magnitude = 7.2 ] {{Sfn|Fine; I.V.|2016}}
| local-time = 17:02
| depth = {{convert|20|km|mi|0|abbr=on}} {{Sfn|Fine; I.V.|2016}}
| location = {{coord|44.54|N|56.01|W}} {{Sfn|Engdahl|2016}} | magnitude = 7.2 ] {{Sfn|Fine|Rabinovich|Bornhold|Thomson|2005}}
|damage = $400,000 {{Sfn|Fine; I.V.|2016}} | depth = {{convert|20|km|mi|0|abbr=on}} {{Sfn|Fine|Rabinovich|Bornhold|Thomson|2005}}
| location = {{coord|44.54|N|56.01|W}} {{Sfn|Engdahl|Vallaseñor|2002}}
| intensity = {{Rfs|VI}}{{Sfn|Natural Resources Canada|2002}}<br/>{{MMI|VIII}}{{Sfn|Natural Resources Canada|2018}}
| tsunami = Yes | tsunami = Yes
| aftershocks = | aftershocks = ~3 {{Sfn|Natural Resources Canada|2002}}
| intensity = ]
| casualties = 27 or 28 killed | casualties = 27 or 28 killed
| title = 1929 Grand Banks earthquake
| countries affected = Newfoundland <br/> Canada <br/> Saint Pierre and Miquelon
|damage = $400,000 {{Sfn|Fine|Rabinovich|Bornhold|Thomson|2005}} ($5.6 million in 2017)
| countries affected = Dominion of Newfoundland <br /> Canada <br />French Republic Saint Pierre and Miquelon
}} }}


The '''1929 Grand Banks earthquake''' (also called the '''Laurentian Slope earthquake''' and the '''South Shore Disaster''') occurred on November 18. The shock had a ] of 7.2 and a maximum ] of VI (''Strong tremor'') and was centered in the Atlantic Ocean off the south coast of ] in the ]. The '''1929 Grand Banks earthquake''' (also called the '''Laurentian Slope earthquake''' and the '''South Shore Disaster''') occurred on November 18, 1929. The shock had a ] of 7.2 and a maximum ] of VI (''Strong tremor'') and was centered in the Atlantic Ocean off the south coast of ] in the ].<ref>{{cite web|url=https://www.cbc.ca/news/canada/newfoundland-labrador/burin-peninsula-tsunami-90th-anniversary-1.5363401|title=90 years later, a tsunami in southern Newfoundland still brings vivid memories|website=Cbc.ca|access-date=December 20, 2021}}</ref>


==Earthquake== ==Earthquake==
The earthquake was centred on the edge of the ], about {{convert|400|km|mi}} south of the island. It was felt as far away as ] and ]. The quake, along two ]s {{convert|250|km|mi}} south of the ], triggered a large ] displaying ({{convert|200|km3|cumi|abbr=on|disp=or}}). It snapped 12 submarine ]s and led to a ] that arrived in three waves.], ] and ] had the largest impact, both from the snapped 12 submarine cables, and the tsunami. This was Canada's largest ] ever recorded, up to 500 times the size of 1894 Saint-Alban subaerial slide.{{Sfn|Fine; I.V.|2016}} The earthquake was centred on the edge of the ], about {{convert|400|km|mi}} south of the island. It was felt as far away as ] and ]. The quake, which occurred along two ]s {{convert|250|km|mi}} south of the ], triggered a large ] displacing ({{convert|200|km3|cumi|abbr=on|disp=or}}). It snapped 12 submarine ]s and led to a ] that arrived in three waves. ], Canada and ] had the largest impact, both from the snapped 12 submarine cables, and the tsunami. This was Canada's largest ] ever recorded, up to 500 times the size of 1894 Saint-Alban subaerial slide.{{Sfn|Fine|Rabinovich|Bornhold|Thomson|2005}}

In 2002 ] and the ], created an intensity map by using the Revised ].{{Sfn|Natural Resources Canada|2018}}


==Tsunami== ==Tsunami==
The tsunami waves had an ] of {{convert|3|-|8|m}}, and a runup of {{convert|13|m|ft}} along the ].{{Sfn|Fine; I.V.|2016}} It destroyed many south coastal communities on the Peninsula, killing 27 or 28 people and leaving 10,000 or more homeless.{{Sfn|Ruffman;Hann|2016}} All means of communication were cut off by the destruction, and relief efforts were further hampered by a blizzard that struck the day after. It was recorded as far away as ] {{convert|4,060|km|mi|abbr=on}}, 06:47 after the earthquake.{{Sfn|Fine; I.V.|2016}}It took 02:23 hrs to strike ], ] {{convert|340|km|mi|abbr=on}} from the epicenter and, only 02:00 hrs; to be observed in ] {{convert|1445|km|mi|abbr=on}}.{{Sfn|Fine; I.V.|2016}} This was Canada's largest ] ever recorded, up to 500 times the size of 1894 ] landslide.{{Sfn|Fine; I.V.|2016}} The tsunami waves had an ] of {{convert|3|-|8|m}}, and a runup of {{convert|13|m|ft}} along the ].{{Sfn|Fine|Rabinovich|Bornhold|Thomson|2005}} It destroyed many south coastal communities on the Peninsula, killing 27 or 28 people and leaving 1,000 or more homeless.{{Sfn|Ruffman|Hann|2006}} All means of communication were cut off by the destruction, and relief efforts were further hampered by a blizzard that struck the day after. It was recorded as far away as ] {{convert|4060|km|mi|abbr=on}} away, 06:47 after the earthquake.{{Sfn|Fine|Rabinovich|Bornhold|Thomson|2005}} It took 2 hours and 23 minutes to strike ], ], {{convert|340|km|mi|abbr=on}} from the epicentre, and only two hours to be observed in ] {{convert|1445|km|mi|abbr=on}}.{{Sfn|Fine|Rabinovich|Bornhold|Thomson|2005}}


{{Quote|text= {{As written}} Tsunami travel times demonstrate the strong ] of the propagating waves. ''The waves reach open ocean islands such as ] in about 2 h (mean speed ~700 km/h) and the ] in about 4 h (~630 km/h).'' At the same time, tsunami wave speeds are much slower in the direction of the North America coast: ''they require 2.7 h to reach ] (~230 km/h) and 4.2 h to reach ] (~380 km/h)''.|author=W.H Berninghausen|source={{Sfn|Fine; I.V.|2016}}}} {{Blockquote|text= {{As written}} Tsunami travel times demonstrate the strong ] of the propagating waves. ''The waves reach open ocean islands such as ] in about 2 h (mean speed ~700 km/h) and the ] in about 4 h (~630 km/h).'' At the same time, tsunami wave speeds are much slower in the direction of the North America coast: ''they require 2.7 h to reach ] (~230 km/h) and 4.2 h to reach ] (~380 km/h)''.|author=W.H Berninghausen|source={{Sfn|Fine|Rabinovich|Bornhold|Thomson|2005}}}}

===Newfoundland===
{{Expand section|date=March 2016}}

===Nova Scotia===
{{Expand section|date=March 2016}}


===Prince Edward Island=== ===Prince Edward Island===
Prince Edward Island had felt the earthquake the intensity was rated at the time ] on the Rossi-Forel scale. Natural Resources Canada and the U.S. Geological Survey, created a intensity map by using the Revised ]. In PEI it raged from a intensity of a ].{{Sfn|MMI|2016}} Prince Edward Island felt the earthquake; at the time the intensity was rated at ] on the Rossi-Forel scale.{{Sfn|Natural Resources Canada|2002}} In the province, it ranged from an intensity of ].{{Sfn|Natural Resources Canada|2002}}


===Saint Pierre and Miquelon=== ===Saint Pierre and Miquelon===
On the French islands of ],{{Sfn|Ruffman, Alen|2016}} about {{Convert|18|km}} west of the Burin Peninsula, people were woken around 16:30h by the earthquake that lasted approximately one minute. At 17:20, the tsunami reached the island of Saint-Pierre, submerging the docks. The worst damage was reported on the island then named ] (meaning ''Island of the Dogs till; 1931''), now known as L'Île-aux-Marins (''The Island of the Sailors''). The tsunami hit from the south, rising above the height of the south bank that protects the south coast, flooding the lower part of the island. It damaged and moved some of the houses, there were no reported injuries or casualties from the islands.{{Sfn|Ruffman, Alen|2016}} In the French ] of ],{{Sfn|Ruffman|1992}} about {{Convert|18|km}} west of the ], residents were startled around 16:30h by an earthquake lasting approximately one minute. At 17:20, the subsequent tsunami reached the island of ], submerging the docks. The most destruction was reported on the island formerly known as ] (''The Island of the Dogs'', until 1931–now known as L'Île-aux-Marins, ''The Island of the Sailors''); the tsunami approached from the south, rising above the height of the south bank that protects the south coast, and flooding the lower part of the island upon impact. The waves destroyed (and moved) several residences and structures, but there were no reported injuries or casualties from the islands.{{Sfn|Ruffman|1992}} The quake's intensity on the island was ],{{Sfn|Natural Resources Canada|2002}} and on the revised Modified Mercalli Intensity scale ]{{Sfn|Natural Resources Canada|2018}}


== Aftermath == == Aftermath ==
{{Refimprove section|date=March 2016|small=y}} {{More citations needed section|date=March 2016}}

It took more than three days before the ''SS Meigle'' responded to an SOS signal with doctors, nurses, blankets, and food. Donations from across Newfoundland, Canada, the United States and United Kingdom totaled $250,000.
There was never an accurate official list of the victims produced by any branch of the Newfoundland government. In the report entitled "Loss of Life," the Honourable Dr. Harris Munden Mosdell, Chairman of the Board of Health Burin West, reported: "The loss of life through the tidal wave totals twenty-seven. Twenty-five deaths were due directly to the upheaval. Two other deaths occurred subsequently and were due to shock and exposure." Later research attributed an additional death to the earthquake.{{Sfn|Heezen;Ewing|2016}} In the immediate aftermath of the tsunami, electricity, radio and telegram communications were unavailable for several days. It took three days for the S.S. ''Meigle'' to respond to a distress signal, sending supplies, aid workers, doctors, nurses, blankets, and food. Donations from across Newfoundland, the United States and the United Kingdom totaled around $250k (about CA$4.3 million in 2023). There was never an accurate or official list of victims produced, by any individual or branch of the Newfoundland or Canadian government. In a report entitled "Loss of Life", the Dr. Harris Munden Mosdell (chairman of the board of Health Burin West) reported that "The loss of life through the tidal wave totals twenty-seven. Twenty-five deaths were due directly to the upheaval. Two other deaths occurred subsequently and were due to shock and exposure." Later research attributed an additional death to the earthquake.{{Sfn|Ruffman|Hann|2006}}<ref>{{Cite web |title=The 1929 Magnitude 7.2 "Grand Banks" earthquake and tsunami |url=https://earthquakescanada.nrcan.gc.ca/historic-historique/events/19291118-en.php|publisher=Natural Resources Canada |accessdate=6 August 2023}}</ref>


In 1952, American scientists from Columbia University put together the pieces of the sequentially broken cables that led to the discovery of the landslide and the first documentation of a ].{{Ref|Heezen;Ewing|2016}} Scientists have examined other layers of sand believed to be deposited by other tsunamis in an effort to determine the occurrence rates of large earthquakes.{{citation needed|date=March 2016}} One sand layer, thought to be deposited by the 1929 tsunami, at Taylor's Bay was found {{convert|13|cm}} below the turf line.{{citation needed|date=March 2016}} The occurrences of large tsunamis, such as the one in 1929, are dependent upon deposition of sediments offshore because it was the landslide that made the tsunami so powerful. The deposition of such a large volume of sediments will take a while before there is enough to form an underwater landslide the same size as that in 1929.{{citation needed|date=March 2016}} In 1952, scientists from ] put together the pieces of the sequentially-broken cables, leading to the discovery of the landslide and the first documentation of a ].{{sfn|Heezen|Ewing|1952}} Scientists have examined layers of sand, believed to be deposited by other tsunamis, in an effort to determine the regional frequency of large earthquakes.{{citation needed|date=March 2016}} One sand layer, thought to be deposited by the 1929 tsunami at ], was found {{convert|13|cm}} below the turf line.{{citation needed|date=March 2016}} The frequency of large tsunamis varies according to the deposition of sediments offshore, as it was the submarine landslide's power that triggered the wave.<ref>{{Cite web |url=https://www.heritage.nf.ca/articles/politics/tsunami-1929.php |title=The Tsunami of 1929|website=heritage.nf.ca |accessdate=6 August 2023}}</ref>


==See also== ==See also==
*] *]
*] *]
*] *]


==References== ==References==
Line 62: Line 63:
=== Sources === === Sources ===
{{refbegin|30em}} {{refbegin|30em}}
*{{cite web|ref={{SfnRef|RossiForel|2016}}title=Le séisme de magnitude 7,2 et le tsunami de 1929 sur les "Grands Bancs"|url=http://www.earthquakescanada.nrcan.gc.ca/historic-historique/events/19291118-en.php|website=Naturl Resoues Canada|publisher=Government of Canada|accessdate=6 March 2016}}</ref> *{{cite web|ref={{SfnRef|Natural Resources Canada|2002}}|title=Le séisme de magnitude 7,2 et le tsunami de 1929 sur les "Grands Bancs"|url=http://www.earthquakescanada.nrcan.gc.ca/historic-historique/events/19291118-en.php|publisher=Natural Resources Canada|access-date=6 March 2016}}
*{{cite web|ref={{SfnRef|MMI|2016}}|title=Revised Modified Mercalli intensities for the Magnitude 7.2 1929 Grand Banks earthquake|url=http://www.earthquakescanada.nrcan.gc.ca/historic-historique/events/19291118-revmmi-en.php|website=Natural Resources Canada|publisher=Government of Canada|accessdate=6 March 2016}} *{{cite web|ref={{SfnRef|Natural Resources Canada|2018}}|title=Revised Modified Mercalli intensities for the Magnitude 7.2 1929 Grand Banks earthquake|url=http://www.earthquakescanada.nrcan.gc.ca/historic-historique/events/19291118-revmmi-en.php|publisher=Natural Resources Canada |date=19 October 2018 |access-date=22 November 2016}}
*{{cite book|ref={{SfnRef|Engdahl|2016}}|title=International Handbook of Earthquake & Engineering Seismology|series=Part A, Volume 81A|chapter=Global seismicity: 1900-1999|first=E. R.|last=Engdahl|first2=A.|last2=Vallaseñor|url=http://wayback.archive.org/web/20060414112957/http://earthquake.usgs.gov/research/data/centennial.pdf|publisher=]; (Sept. 12, 2002)|edition=First|isbn=978-0124406520|page=675}} *{{cite book |title=International Handbook of Earthquake & Engineering Seismology |series=Part A, Volume 81A |chapter=Global seismicity: 1900–1999 |first1=E. R. |last1=Engdahl |first2=A. |last2=Vallaseñor |chapter-url=https://earthquake.usgs.gov/data/centennial/centennial.pdf |publisher=] |date=September 12, 2002 |edition=First |isbn=978-0124406520 |page=675 }}
*{{cite journal|ref={{SfnRef|Fine;Rabinovich|2016}}|first=I. V.|last=Fine|first2=A. B.|last2=Rabinovich|first3=B. D.|last3=Bornhold|first4=R. E.|last4=Thomson|first5=E. A.|last5=Kulikov|year=2005|title=The Grand Banks landslide-generated tsunami of November 18, 1929: preliminary analysis and numerical modeling|journal=Marine Geology|publisher=]|volume=215|issue=1–2|pages=45-57|doi=10.1016/j.margeo.2004.11.007|url=https://web.archive.org/web/20070630105626/http://www.pac.dfo-mpo.gc.ca/SCI/osap/projects/tsunami/documents/1929.pdf}} *{{cite journal |first1=I. V. |last1=Fine |first2=A. B. |last2=Rabinovich |first3=B. D. |last3=Bornhold |first4=R. E. |last4=Thomson |first5=E. A. |last5=Kulikov |year=2005 |title=The Grand Banks landslide-generated tsunami of November 18, 1929: preliminary analysis and numerical modeling |journal=Marine Geology |publisher=] |volume=215 |issue=1–2 |pages=45–57 |doi=10.1016/j.margeo.2004.11.007 |url=http://www.pac.dfo-mpo.gc.ca/SCI/osap/projects/tsunami/documents/1929.pdf |url-status=dead |archive-url=https://web.archive.org/web/20070630105626/http://www.pac.dfo-mpo.gc.ca/SCI/osap/projects/tsunami/documents/1929.pdf |archive-date=June 30, 2007 |bibcode=2005MGeol.215...45F }}
*{{cite journal | url=http://www.ajsonline.org/content/250/12/849.extract | title=Turbidity Currents and Submarine Slumps, and the 1929 Grand Banks Earthquake | last1=Heezen |first1=B.C. |last2= Ewing |first2= M. | journal=American Journal of Science | year=1952 | volume=250 | pages=849–873| doi=10.2475/ajs.250.12.849 | doi-access=free }}
*{{cite journal|ref={{SfnRef|Ruffman;Hann|2016}}|title=The Newfoundland Tsunami of November 18, 1929: An Examination of the Twenty-eight Deaths of the “South Coast Disaster”|url=http://www.seismescanada.rncan.gc.ca/historic-historique/events/Ruffman_Hann2006_NLSv21.pdf|first=A.|last=Ruffman|first2=V.|last2=Hann|pages=57|year=2006|accessdate=5 March 2016|journal=Newfoundland and Labrador Studies}} *{{cite journal|title=The Newfoundland Tsunami of November 18, 1929: An Examination of the Twenty-eight Deaths of the "South Coast Disaster"|url=http://www.seismescanada.rncan.gc.ca/historic-historique/events/Ruffman_Hann2006_NLSv21.pdf|first1=A.|last1=Ruffman|first2=V.|last2=Hann|pages=57|year=2006|access-date=5 March 2016|journal=Newfoundland and Labrador Studies}}
*{{cite journal|ref={{SfnRef|Ruffman, Alen|2016}}|last1=Ruffman|first1=Alan|title=Archiving Content The 1929 Tsunami In St. Lawrence, Newfoundland|journal=Tsunami Runup Mapping As An Emergency Preparedness Planning Tool:|date=1992|volume=2-Appendices and Enclosures|pages=294|url=https://www.publicsafety.gc.ca/lbrr/archives/gc%20222.n6%20r84%201996%20v.2-eng.pdf|accessdate=4 March 2016|publisher=Emergency Preparedness Protection civile Canada|language=English}} *{{cite journal|last1=Ruffman|first1=Alan|title=Archiving Content The 1929 Tsunami In St. Lawrence, Newfoundland|journal=Tsunami Runup Mapping as an Emergency Preparedness Planning Tool|date=1992|volume=2-Appendices and Enclosures|pages=294|url=https://www.publicsafety.gc.ca/lbrr/archives/gc%20222.n6%20r84%201996%20v.2-eng.pdf|access-date=4 March 2016|publisher=Emergency Preparedness Protection civile Canada}}
*{{cite journal|ref={{SfnRef|Heezen;Ewing|2016}}|url=http://www.ajsonline.org/content/250/12/849.extract|title=Turbidity Currents and Submarine Slumps, and the 1929 Grand Banks Earthquake|author=Heezen B.C. & Ewing M.| journal=American Journal of Science | year=1952 | volume=250 | pages=849–873}}


{{refend}} {{refend}}


==External links== ==External links==
* – CBC
* - ] * ]
* *
* *
* – ] * – ]
* International Journal of ], ] and ] (2004) {{ISSN|0025-3227}} * International Journal of ], ] and ] (2004) {{ISSN|0025-3227}}
*{{EQ-isc-link|908394}}


===Further reading=== ===Further reading===
*''Tsunami: The Newfoundland Tidal Wave Disaster'' - ] (2004) ISBN 1-894463-63-3 *''Tsunami: The Newfoundland Tidal Wave Disaster'' ] (2004) {{ISBN|1-894463-63-3}}
{{Earthquakes in the 1920s}}


{{DEFAULTSORT:1929 Grand Banks Earthquake}} {{DEFAULTSORT:1929 Grand Banks Earthquake}}
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Latest revision as of 13:17, 14 November 2024

Earthquake and tsunami in eastern Canada

1929 Grand Banks earthquake
1929 Grand Banks earthquake is located in Canada1929 Grand Banks earthquake
UTC time1929-11-18 20:32:00
ISC event908394
USGS-ANSSComCat
Local dateNovember 18, 1929 (1929-11-18)
Local time17:02
Magnitude7.2 Mw
Depth20 km (12 mi)
Epicenter44°32′N 56°01′W / 44.54°N 56.01°W / 44.54; -56.01
Areas affectedDominion of Newfoundland
Canada
French Republic Saint Pierre and Miquelon
Total damage$400,000 ($5.6 million in 2017)
Max. intensityRFS VI (Strong tremor)
MMI VIII (Severe)
TsunamiYes
Aftershocks~3
Casualties27 or 28 killed

The 1929 Grand Banks earthquake (also called the Laurentian Slope earthquake and the South Shore Disaster) occurred on November 18, 1929. The shock had a moment magnitude of 7.2 and a maximum Rossi–Forel intensity of VI (Strong tremor) and was centered in the Atlantic Ocean off the south coast of Newfoundland in the Laurentian Slope seismic zone.

Earthquake

The earthquake was centred on the edge of the Grand Banks of Newfoundland, about 400 kilometres (250 mi) south of the island. It was felt as far away as New York City and Montreal. The quake, which occurred along two faults 250 kilometres (160 mi) south of the Burin Peninsula, triggered a large submarine landslide displacing (200 km or 48 cu mi). It snapped 12 submarine transatlantic telegraph cables and led to a tsunami that arrived in three waves. Newfoundland, Canada and Saint Pierre and Miquelon had the largest impact, both from the snapped 12 submarine cables, and the tsunami. This was Canada's largest submarine landslide ever recorded, up to 500 times the size of 1894 Saint-Alban subaerial slide.

In 2002 Natural Resources Canada and the United States Geological Survey, created an intensity map by using the Revised Modified Mercalli scale.

Tsunami

The tsunami waves had an amplitude of 3–8 metres (9.8–26.2 ft), and a runup of 13 metres (43 ft) along the Burin Peninsula. It destroyed many south coastal communities on the Peninsula, killing 27 or 28 people and leaving 1,000 or more homeless. All means of communication were cut off by the destruction, and relief efforts were further hampered by a blizzard that struck the day after. It was recorded as far away as Lagos, Portugal 4,060 km (2,520 mi) away, 06:47 after the earthquake. It took 2 hours and 23 minutes to strike Burin, Newfoundland, 340 km (210 mi) from the epicentre, and only two hours to be observed in Bermuda 1,445 km (898 mi).

Tsunami travel times demonstrate the strong anisotropy of the propagating waves. The waves reach open ocean islands such as Bermuda in about 2 h (mean speed ~700 km/h) and the Azores in about 4 h (~630 km/h). At the same time, tsunami wave speeds are much slower in the direction of the North America coast: they require 2.7 h to reach Halifax (~230 km/h) and 4.2 h to reach Atlantic City (~380 km/h).

— W.H Berninghausen,

Prince Edward Island

Prince Edward Island felt the earthquake; at the time the intensity was rated at IV (Slight tremor) – VI (Strong tremor) on the Rossi-Forel scale. In the province, it ranged from an intensity of III (Weak) – V (Moderate).

Saint Pierre and Miquelon

In the French Overseas territory of Saint Pierre and Miquelon, about 18 kilometres (11 mi) west of the Burin Peninsula, residents were startled around 16:30h by an earthquake lasting approximately one minute. At 17:20, the subsequent tsunami reached the island of Saint-Pierre, submerging the docks. The most destruction was reported on the island formerly known as Île-aux-Chiens (The Island of the Dogs, until 1931–now known as L'Île-aux-Marins, The Island of the Sailors); the tsunami approached from the south, rising above the height of the south bank that protects the south coast, and flooding the lower part of the island upon impact. The waves destroyed (and moved) several residences and structures, but there were no reported injuries or casualties from the islands. The quake's intensity on the island was V (Moderate tremor) – VI (Strong tremor), and on the revised Modified Mercalli Intensity scale IV (Light) – V (Moderate)

Aftermath

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In the immediate aftermath of the tsunami, electricity, radio and telegram communications were unavailable for several days. It took three days for the S.S. Meigle to respond to a distress signal, sending supplies, aid workers, doctors, nurses, blankets, and food. Donations from across Newfoundland, the United States and the United Kingdom totaled around $250k (about CA$4.3 million in 2023). There was never an accurate or official list of victims produced, by any individual or branch of the Newfoundland or Canadian government. In a report entitled "Loss of Life", the Dr. Harris Munden Mosdell (chairman of the board of Health Burin West) reported that "The loss of life through the tidal wave totals twenty-seven. Twenty-five deaths were due directly to the upheaval. Two other deaths occurred subsequently and were due to shock and exposure." Later research attributed an additional death to the earthquake.

In 1952, scientists from Columbia University put together the pieces of the sequentially-broken cables, leading to the discovery of the landslide and the first documentation of a turbidity current. Scientists have examined layers of sand, believed to be deposited by other tsunamis, in an effort to determine the regional frequency of large earthquakes. One sand layer, thought to be deposited by the 1929 tsunami at Taylor's Bay, was found 13 centimetres (5.1 in) below the turf line. The frequency of large tsunamis varies according to the deposition of sediments offshore, as it was the submarine landslide's power that triggered the wave.

See also

References

Citations

  1. ^ Fine et al. 2005.
  2. Engdahl & Vallaseñor 2002.
  3. ^ Natural Resources Canada 2002.
  4. ^ Natural Resources Canada 2018.
  5. "90 years later, a tsunami in southern Newfoundland still brings vivid memories". Cbc.ca. Retrieved December 20, 2021.
  6. ^ Ruffman & Hann 2006.
  7. ^ Ruffman 1992.
  8. "The 1929 Magnitude 7.2 "Grand Banks" earthquake and tsunami". Natural Resources Canada. Retrieved August 6, 2023.
  9. Heezen & Ewing 1952.
  10. "The Tsunami of 1929". heritage.nf.ca. Retrieved August 6, 2023.

Sources

External links

Further reading

Earthquakes in the 1920s
1920
1921
1923
1925
1927
1928
1929
indicates earthquake resulting in at least 30 deaths
indicates the deadliest earthquake of the year
Categories: