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| local-date = <!-- NZDT -->3 February 1931
| local-date = <!-- NZDT -->3 February 1931
| local-time = 10:46:52 [[Time in New Zealand|NZDT]]
| local-time = 10:46:52 [[Time in New Zealand|NZDT]]
| intensity = {{MMI|9}}<ref name=NGDC>{{Cite web|title=Significant Earthquake Information|url=https://www.ngdc.noaa.gov/hazel/view/hazards/earthquake/event-more-info/3450|author=National Geophysical Data Center / World Data Service (NGDC/WDS)|publisher=[[National Oceanic and Atmospheric Administration|NOAA]] National Centers for Environmental Information|doi=10.7289/V5TD9V7K|year = 1972|type =}}</ref>
| intensity = {{MMI|9}}<ref name=NGDC>{{Cite web|title=Significant Earthquake Information|url=https://www.ngdc.noaa.gov/hazel/view/hazards/earthquake/event-more-info/3450|author=National Geophysical Data Center / World Data Service (NGDC/WDS)|publisher=[[National Oceanic and Atmospheric Administration|NOAA]] National Centers for Environmental Information|doi=10.7289/V5TD9V7K|year = 1972}}</ref>
| magnitude = 7.8 {{M|s|link=y}}<br>7.7 {{M|w|link=yes}}<ref name="Webb_&_Anderson_1998">{{Cite journal |last1=Webb |first1=T.H. |last2=Anderson |first2=H. |date=1998 |title=Focal mechanisms of large earthquakes in the North Island of New Zealand: slip partitioning at an oblique active margin |journal=Geophysical Journal International |volume=134 |issue=1 |pages=40–86 |doi=10.1046/j.1365-246x.1998.00531.x|bibcode=1998GeoJI.134...40W |doi-access= free}}</ref>
| magnitude = 7.8 {{M|s|link=y}}<br>7.7 {{M|w|link=yes}}<ref name="Webb_&_Anderson_1998">{{Cite journal |last1=Webb |first1=T.H. |last2=Anderson |first2=H. |date=1998 |title=Focal mechanisms of large earthquakes in the North Island of New Zealand: slip partitioning at an oblique active margin |journal=Geophysical Journal International |volume=134 |issue=1 |pages=40–86 |doi=10.1046/j.1365-246x.1998.00531.x|bibcode=1998GeoJI.134...40W |doi-access= free}}</ref>
| depth = {{convert|14|km|abbr=on}}
| depth = {{convert|14|km|abbr=on}}
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[[File:Hawkes Bay Tribune 1931.jpg|thumb|Damage to the Hawkes Bay Tribune building]]
[[File:Hawkes Bay Tribune 1931.jpg|thumb|Damage to the Hawkes Bay Tribune building]]


The '''1931 Hawke's Bay earthquake''', also known as the '''Napier earthquake''', occurred in [[New Zealand]] at 10:47 am on 3 February, killing 256,<ref name="deathtoll">The exact number of deaths varies according to different sources; the ''New Zealand Listener'' article cited below gives 258 deaths, but the Bateman ''New Zealand Encyclopedia'' gives 256. The difference is due to two people "missing" and presumed dead. Some articles add these two to the death toll, while others do not.</ref> injuring thousands and devastating the [[Hawke's Bay (region)|Hawke's Bay]] region. It remains New Zealand's deadliest [[natural disaster]]. Centred 15&nbsp;km north of [[Napier, New Zealand|Napier]], it lasted for two and a half minutes and had a magnitude of 7.8 {{M|s|link=y}} (7.7 {{M|w|link=y}}).<ref name="Webb_&_Anderson_1998"/> There were 525 [[aftershock]]s recorded in the following two weeks, with 597 being recorded by the end of February. The main shock could be felt in much of New Zealand, with reliable reports coming in from as far south as [[Timaru]], on the east coast of the [[South Island]].<ref>{{cite web |url= http://www.geonet.org.nz/quakes/region/newzealand/2178228 |title=M 7.4 Hawke's Bay Tue, Feb 3 1931|publisher=GeoNet}}</ref>
The '''1931 Hawke's Bay earthquake''', also known as the '''Napier earthquake''', occurred in New Zealand at 10:47{{Nbsp}}am on 3 February, killing 256,<ref name="deathtoll">The exact number of deaths varies according to different sources; the ''New Zealand Listener'' article cited below gives 258 deaths, but the Bateman ''New Zealand Encyclopedia'' gives 256. The difference is due to two people "missing" and presumed dead. Some articles add these two to the death toll, while others do not.</ref> injuring thousands and devastating the [[Hawke's Bay (region)|Hawke's Bay]] region. It remains New Zealand's deadliest [[natural disaster]]. Centred 15&nbsp;km north of [[Napier, New Zealand|Napier]], it lasted for two and a half minutes and had a magnitude of 7.8 {{M|s|link=y}} (7.7 {{M|w|link=y}}).<ref name="Webb_&_Anderson_1998"/> There were 525 [[aftershock]]s recorded in the following two weeks, with 597 being recorded by the end of February. The main shock could be felt in much of New Zealand, with reliable reports coming in from as far south as [[Timaru]], on the east coast of the [[South Island]].<ref>{{cite web |url= http://www.geonet.org.nz/quakes/region/newzealand/2178228 |title=M 7.4 Hawke's Bay Tue, Feb 3 1931|publisher=[[GeoNet (New Zealand)|GeoNet]]}}</ref>


==Tectonic setting==
==Tectonic setting==
New Zealand lies along the boundary between the [[Indo-Australian Plate]] and [[Pacific Plate]]s. In the [[South Island]] most of the relative displacement between these plates is taken up along a single dextral (right lateral) [[strike-slip fault]] with a major [[Dip-slip faults|reverse]] component, the [[Alpine Fault]]. In the [[North Island]] the displacement is mainly taken up along the [[Hikurangi Subduction Zone]], although the remaining dextral strike-slip component of the relative plate motion is accommodated by the [[North Island Fault System]] (NIFS).<ref>{{citation|title=Terminations of large strike-slip faults: An alternative model from New Zealand|journal=Geological Society, London, Special Publications|volume=290|issue=1|pages= 387–415|year=2007|last1=Mouslopoulou|first1=V|last2=Nicol|first2=A|last3=Little|first3=T. A|last4=Walsh|first4=J. J|bibcode=2007GSLSP.290..387M|doi=10.1144/SP290.15|s2cid=129003001}}</ref>
New Zealand lies along the boundary between the [[Indo-Australian plate]] and [[Pacific plate]]s. In the [[South Island]] most of the relative displacement between these plates is taken up along a single dextral (right lateral) [[strike-slip fault]] with a major [[Dip-slip faults|reverse]] component, the [[Alpine Fault]]. In the [[North Island]] the displacement is mainly taken up along the [[Hikurangi Subduction Zone]], although the remaining dextral strike-slip component of the relative plate motion is accommodated by the [[North Island Fault System]] (NIFS).<ref>{{citation|title=Terminations of large strike-slip faults: An alternative model from New Zealand|journal=Geological Society, London, Special Publications|volume=290|issue=1|pages= 387–415|year=2007|last1=Mouslopoulou|first1=V|last2=Nicol|first2=A|last3=Little|first3=T. A|last4=Walsh|first4=J. J|bibcode=2007GSLSP.290..387M|doi=10.1144/SP290.15|s2cid=129003001}}</ref>


The earthquake is thought to have occurred on one of the larger [[Thrust fault|thrust]] faults within the [[accretionary wedge]], at between ca. 5&nbsp;km depth and ca. 20–25&nbsp;km depth (which is the approximate depth of subducted Pacific plate at that location).<ref>{{cite web|url=http://www.gns.cri.nz/gns/Home/News-and-Events/Media-Releases/NZ-s-quake-vulnerability|title=Bay quake highlights NZ's vulnerability|publisher=GNS Science|website=www.gns.cri.nz|access-date=23 June 2011|archive-date=18 February 2013|archive-url=https://web.archive.org/web/20130218235605/http://gns.cri.nz/gns/Home/News-and-Events/Media-Releases/NZ-s-quake-vulnerability|url-status=dead}}</ref>
The earthquake is thought to have occurred on one of the larger [[Thrust fault|thrust]] faults within the [[accretionary wedge]], at between ca. 5&nbsp;km depth and ca. 20–25&nbsp;km depth (which is the approximate depth of subducted Pacific plate at that location).<ref>{{cite web|url=http://www.gns.cri.nz/gns/Home/News-and-Events/Media-Releases/NZ-s-quake-vulnerability|title=Bay quake highlights NZ's vulnerability|publisher=GNS Science|website=gns.cri.nz|access-date=23 June 2011|archive-date=18 February 2013|archive-url=https://web.archive.org/web/20130218235605/http://gns.cri.nz/gns/Home/News-and-Events/Media-Releases/NZ-s-quake-vulnerability|url-status=dead}}</ref>


==Damage and effects==
==Damage and effects==
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=== Fires ===
=== Fires ===
Within minutes fires broke out in a few chemist shops in Hastings Street, Napier.<ref name=":0">{{Cite web |title=The 1931 Earthquake {{!}} Napier City Council |url=https://www.napier.govt.nz/napier/about/history/napier-earthquake-1931/ |access-date=2024-05-11 |website=www.napier.govt.nz}}</ref><ref name=":5" /> The fire brigade almost had the first fire under control when the second broke out in a shop at the back of the Masonic Hotel.{{Citation needed|date=May 2024}} The fire continued to spread through adjoined wooden buildings, which led to the entire town being engulfed in flames by the afternoon.<ref name=":0" /> The wind at this point also picked up strength and began blowing from the east, pushing the fires back over the city.{{Citation needed|date=May 2024}} The day was hot and dry which increased the fire's ability to spread. With water mains broken, the brigade was unable to save many buildings. Attempts were made at pumping water from the sea, but these failed.<ref name=":0" /> Fire engines at Napier's central fire station were covered in debris from the earthquake which made them unavailable for use.<ref name=":5" /> Pumping water from Clive Square, they were able to stop the fires spreading south. Only a few buildings in the central Napier area survived. Some withstood the earthquake only to be gutted by fire. Trapped people had to be left to burn as people were unable to free them in time.{{Cn|date=May 2024}} It took until the following afternoon for the main fires to go out,<ref name=":0" /> but the ruins still smouldered for several days.{{Citation needed|date=May 2024}}
Within minutes fires broke out in a few chemist shops in Hastings Street, Napier.<ref name=":0">{{Cite web |title=The 1931 Earthquake {{!}} Napier City Council |url=https://www.napier.govt.nz/napier/about/history/napier-earthquake-1931/ |access-date=2024-05-11 |website=napier.govt.nz}}</ref><ref name=":5" /> The fire brigade almost had the first fire under control when the second broke out in a shop at the back of the Masonic Hotel.{{Citation needed|date=May 2024}} The fire continued to spread through adjoined wooden buildings, which led to the entire town being engulfed in flames by the afternoon.<ref name=":0" /> The wind at this point also picked up strength and began blowing from the east, pushing the fires back over the city.{{Citation needed|date=May 2024}} The day was hot and dry which increased the fire's ability to spread. With water mains broken, the brigade was unable to save many buildings. Attempts were made at pumping water from the sea, but these failed.<ref name=":0" /> Fire engines at Napier's central fire station were covered in debris from the earthquake which made them unavailable for use.<ref name=":5" /> Pumping water from Clive Square, they were able to stop the fires spreading south. Only a few buildings in the central Napier area survived. Some withstood the earthquake only to be gutted by fire. Trapped people had to be left to burn as people were unable to free them in time.{{Citation needed|date=May 2024}} It took until the following afternoon for the main fires to go out,<ref name=":0" /> but the ruins still smouldered for several days.{{Citation needed|date=May 2024}}


In Hastings, the fires were quickly brought under control.{{Citation needed|date=May 2024}}
In Hastings, the fires were quickly brought under control.{{Citation needed|date=May 2024}}


=== Utilities ===
=== Utilities ===
The entire east coast of the North Island lost electricity during the quake, although power was restored to [[Masterton]], [[Pahiatua]], [[Dannevirke]] and [[Waipukurau]] within two hours, and to [[Gisborne, New Zealand|Gisborne]] within ten hours. At Napier substation, the transformers were tipped over by the force of the quake and the high-voltage switchgear damaged, while the Napier to [[Tuai]] transmission line was taken out of service after a landslide caused a tower to collapse. A limited supply was restored to Napier and Hastings on 4 February; due to the damage at Napier substation, the Waipukurau to Napier transmission line was jumpered to the low-voltage switchgear at both ends. The Napier to Tuai line was repaired and put back into service on 12 February, while full supply to Napier substation was restored on 29 March.<ref>{{Cite web|date=1931|title=AtoJs Online Appendix to the Journals of the House of Representatives 1931 Session I-II D-01 PUBLIC WORKS STATEMENT (BY THE RIGHT HON. J. G. COATES, MINISTER OF PUBLIC WORKS).|url=https://atojs.natlib.govt.nz/cgi-bin/atojs?a=d&d=AJHR1931-I-II.2.2.2.1&pg=101&e=-------10--1---bySH---0-AJHR_1931_IZz-II_DZz-I-|access-date=26 February 2021|website=atojs.natlib.govt.nz|language=en-NZ}}</ref>
The entire east coast of the North Island lost electricity during the quake, although power was restored to [[Masterton]], [[Pahiatua]], [[Dannevirke]] and [[Waipukurau]] within two hours, and to [[Gisborne, New Zealand|Gisborne]] within ten hours. At Napier substation, the transformers were tipped over by the force of the quake and the high-voltage switchgear damaged, while the Napier to [[Tuai]] transmission line was taken out of service after a landslide caused a tower to collapse. A limited supply was restored to Napier and Hastings on 4 February; due to the damage at Napier substation, the Waipukurau to Napier transmission line was jumpered to the low-voltage switchgear at both ends. The Napier to Tuai line was repaired and put back into service on 12 February, while full supply to Napier substation was restored on 29 March.<ref>{{Cite web|date=1931|title=AtoJs Online Appendix to the Journals of the House of Representatives 1931 Session I-II D-01 PUBLIC WORKS STATEMENT (BY THE RIGHT HON. J. G. COATES, MINISTER OF PUBLIC WORKS).|url=https://atojs.natlib.govt.nz/cgi-bin/atojs?a=d&d=AJHR1931-I-II.2.2.2.1&pg=101&e=-------10--1---bySH---0-AJHR_1931_IZz-II_DZz-I-|access-date=26 February 2021|website=atojs.natlib.govt.nz}}</ref>


There was also severe damage to sewerage systems, gas supply and telegraph systems.{{sfn|Dowrick|1998|p=145}}
There was also severe damage to sewerage systems, gas supply and telegraph systems.{{sfn|Dowrick|1998|p=145}}
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The earthquake caused great damage to Napier's roads, railways,<ref name="teara1966" /> bridges and wharves. Rails were badly twisted.{{sfn|Dowrick|1998|p=142-143}} The city's [[tram]] tracks were also twisted, and were never restored.<ref>{{cite web |title=Napier Earthquake |url=http://library.christchurch.org.nz/Kids/NZDisasters/Napier.asp |url-status=live |archive-url=https://web.archive.org/web/20080216185652/http://library.christchurch.org.nz/kids/nzdisasters/napier.asp |archive-date=16 February 2008 |access-date=13 February 2008 |work=Christchurch City Libraries}}</ref>
The earthquake caused great damage to Napier's roads, railways,<ref name="teara1966" /> bridges and wharves. Rails were badly twisted.{{sfn|Dowrick|1998|p=142-143}} The city's [[tram]] tracks were also twisted, and were never restored.<ref>{{cite web |title=Napier Earthquake |url=http://library.christchurch.org.nz/Kids/NZDisasters/Napier.asp |url-status=live |archive-url=https://web.archive.org/web/20080216185652/http://library.christchurch.org.nz/kids/nzdisasters/napier.asp |archive-date=16 February 2008 |access-date=13 February 2008 |work=Christchurch City Libraries}}</ref>


New Zealand's first commercial air disaster occurred six days after the quake, when a [[Dominion Airlines]] [[Desoutter]] monoplane crashed near Wairoa. The small airline had been making three return trips a day between Hastings and Gisborne, carrying passengers and supplies. All three on board were killed.<ref>{{Cite web |title=First fatal accident on a scheduled air service in New Zealand |url=https://nzhistory.govt.nz/first-fatal-air-accident-in-nz |access-date=2024-04-15 |website=nzhistory.govt.nz |language=en}}</ref>
New Zealand's first commercial air disaster occurred six days after the quake, when a [[Dominion Airlines]] [[Desoutter]] monoplane crashed near Wairoa. The small airline had been making three return trips a day between Hastings and Gisborne, carrying passengers and supplies. All three on board were killed.<ref>{{Cite web |title=First fatal accident on a scheduled air service in New Zealand |url=https://nzhistory.govt.nz/first-fatal-air-accident-in-nz |access-date=2024-04-15 |website=nzhistory.govt.nz}}</ref>


=== Et cetera ===
=== Et cetera ===
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== Casualties ==
== Casualties ==
The official death toll was 256 although the Napier earthquake memorial lists 258 names.<ref name=":3">{{Cite web |title=Deadly Hawke's Bay earthquake |url=https://nzhistory.govt.nz/hawkes-bay-earthquake |access-date=2024-05-11 |website=nzhistory.govt.nz |language=en}}</ref> Of these, 161 people were in [[Napier, New Zealand|Napier]], 93 in [[Hastings, New Zealand|Hastings]], and two in [[Wairoa]].<ref name="deathtoll" /> Thousands more were injured, with over 400 hospitalised.<ref name=":0" /> Places with several deaths include 17 deaths due to Roach's department store collapsing, 15 in an old men's home,<ref name=":3" /> nine students in Napier Technical College,<ref name="historicplacesaotearoa2">{{Cite web |date=1 May 2014 |title=H B Heritage News |url=https://historicplacesaotearoa.org.nz/assets/HPHB-NEWSLETTER-1-May-2014.pdf |access-date=11 May 2024 |website=historicplacesaotearoa.govt.nz}}</ref> eight from Grand Hotel, and seven at the [[Greenmeadows, New Zealand|Greenmeadows]] seminary.<ref name=":3" />
The official death toll was 256 although the Napier earthquake memorial lists 258 names.<ref name=":3">{{Cite web |title=Deadly Hawke's Bay earthquake |url=https://nzhistory.govt.nz/hawkes-bay-earthquake |access-date=2024-05-11 |website=nzhistory.govt.nz}}</ref> Of these, 161 people were in [[Napier, New Zealand|Napier]], 93 in [[Hastings, New Zealand|Hastings]], and two in [[Wairoa]].<ref name="deathtoll" /> Thousands more were injured, with over 400 hospitalised.<ref name=":0" /> Places with several deaths include 17 deaths due to Roach's department store collapsing, 15 in an old men's home,<ref name=":3" /> nine students in Napier Technical College,<ref name="historicplacesaotearoa2">{{Cite web |date=1 May 2014 |title=H B Heritage News |url=https://historicplacesaotearoa.org.nz/assets/HPHB-NEWSLETTER-1-May-2014.pdf |access-date=11 May 2024 |website=historicplacesaotearoa.govt.nz}}</ref> eight from Grand Hotel, and seven at the [[Greenmeadows, New Zealand|Greenmeadows]] seminary.<ref name=":3" />


== Response ==
== Response ==
Shortly after the earthquake, people escaped to the Marine Parade Beach. After noticing that the shoreline had receded, they ran away in panic under the expectation that a tsunami was on its way. There was, however, no tidal wave; the receded shoreline was caused by the land moving upwards.<ref>{{Cite news |last=Fowler |first=Michael |date=27 November 2016 |title=1931 quake sparked tidal-wave fear |url=https://www.nzherald.co.nz/hawkes-bay-today/news/1931-quake-sparked-tidal-wave-fear/FJDGAEWDELHBC64YVESUTJDZHA/ |access-date=16 May 2024 |work=[[Hawke's Bay Today]] |via=[[The New Zealand Herald]]}}</ref><ref name=":5" />[[File:1931_Hawkes_Bay_Earthquake_-_Telegram_from_King_George_V_(24290801269).jpg|thumb|Telegram from [[King George V]] to Governor-General of New Zealand, 3 February 1931]]On 4 February over 5,000 people evacuated Napier,<ref name=":5">{{Cite web |title=Hawke's Bay earthquake |url=https://my.christchurchcitylibraries.com/hawkes-bay-earthquake |access-date=15 May 2024 |website=my.christchurchcitylibraries.com |language=en-NZ}}</ref> mainly women and children. Men were expected to stay to help out with the recovery. The army and navy also arrived in Napier to help with the recovery. [[Nelson Park, Napier|Nelson Park]] served as Napier's "evacuation centre" which was the site of many tents and was able to cater for over 1,000 people from a [[field kitchen]]. Many people also lived in tents in [[Marine Parade, New Zealand|Marine Parade]] and other places. There were several places that gave out free food in Napier and Hawke's Bay, such as in several schools. Water barrels were also kept full to allow for people to take from them, after losing water access from their homes.<ref name=":0" />
Shortly after the earthquake, people escaped to the Marine Parade Beach. After noticing that the shoreline had receded, they ran away in panic under the expectation that a tsunami was on its way. There was, however, no tidal wave; the receded shoreline was caused by the land moving upwards.<ref>{{Cite news |last=Fowler |first=Michael |date=27 November 2016 |title=1931 quake sparked tidal-wave fear |url=https://www.nzherald.co.nz/hawkes-bay-today/news/1931-quake-sparked-tidal-wave-fear/FJDGAEWDELHBC64YVESUTJDZHA/ |access-date=16 May 2024 |department=[[Hawke's Bay Today]] |work=[[The New Zealand Herald]]}}</ref><ref name=":5" />[[File:1931_Hawkes_Bay_Earthquake_-_Telegram_from_King_George_V_(24290801269).jpg|thumb|Telegram from [[King George V]] to Governor-General of New Zealand, 3 February 1931]]On 4 February over 5,000 people evacuated Napier,<ref name=":5">{{Cite web |title=Hawke's Bay earthquake |url=https://my.christchurchcitylibraries.com/hawkes-bay-earthquake |access-date=15 May 2024 |website=my.christchurchcitylibraries.com}}</ref> mainly women and children. Men were expected to stay to help out with the recovery. The army and navy also arrived in Napier to help with the recovery. [[Nelson Park, Napier|Nelson Park]] served as Napier's "evacuation centre" which was the site of many tents and was able to cater for over 1,000 people from a [[field kitchen]]. Many people also lived in tents in [[Marine Parade, New Zealand|Marine Parade]] and other places. There were several places that gave out free food in Napier and Hawke's Bay, such as in several schools. Water barrels were also kept full to allow for people to take from them, after losing water access from their homes.<ref name=":0" />


Within four days of the quake, cinemas around New Zealand offered news specials about the disaster.{{Citation needed|date=May 2024}}
Within four days of the quake, cinemas around New Zealand offered news specials about the disaster.{{Citation needed|date=May 2024}}
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[[File:Tin town, napier.jpg|thumb|The temporary shopping centre known as "Tin Town"]]
[[File:Tin town, napier.jpg|thumb|The temporary shopping centre known as "Tin Town"]]


{{Anchor|Tin Town}}Several temporary structures were built following the earthquake, including the shopping centre commonly referred to as Tin Town in Clive Square.<ref name=":0" /><ref name=":2">{{Cite web |last=McSaveney |first=Eileen |date=12 June 2006 |title=Rebuilding Napier |url=https://teara.govt.nz/en/historic-earthquakes/page-8 |access-date=11 May 2024 |website=[[Te Ara: The Encyclopedia of New Zealand]]}}</ref> It remained for about two years,<ref name=":1">{{Cite news |last=Heather |first=Ben |date=31 October 2011 |title=Napier's 'Tin Town' did it first |url=https://www.stuff.co.nz/the-press/5878800/Napiers-Tin-Town-did-it-first |access-date=11 May 2024 |work=[[The Press]] |via=[[Stuff (website)|Stuff]]}}</ref> housed over 50 businesses, and was created with a £10,000 loan<ref name=":0" /> which did not have to be paid back. According to ''[[The Press]]'', it was the world's first "pop-up mall".<ref name=":1" />
{{Anchor|Tin Town}}Several temporary structures were built following the earthquake, including the shopping centre commonly referred to as Tin Town in Clive Square.<ref name=":0" /><ref name=":2">{{Cite web |last=McSaveney |first=Eileen |date=12 June 2006 |title=Rebuilding Napier |url=https://teara.govt.nz/en/historic-earthquakes/page-8 |access-date=11 May 2024 |website=[[Te Ara: The Encyclopedia of New Zealand]]}}</ref> It remained for about two years,<ref name=":1">{{Cite news |last=Heather |first=Ben |date=31 October 2011 |title=Napier's 'Tin Town' did it first |url=https://www.stuff.co.nz/the-press/5878800/Napiers-Tin-Town-did-it-first |access-date=11 May 2024 |work=[[The Press]] |publisher=Stuff|location=New Zealand}}</ref> housed over 50 businesses, and was created with a £10,000 loan<ref name=":0" /> which did not have to be paid back. According to ''[[The Press]]'', it was the world's first "pop-up mall".<ref name=":1" />


The earthquake prompted a thorough review of New Zealand [[building code]]s,<ref>{{Cite book |last1=Hicks |first1=Geoffrey R. F. |url=https://www.wikidata.org/wiki/Q126174593 |title=Awesome Forces: The Natural Hazards That Threaten New Zealand |last2=Campbell |first2=Hamish |date=2012-01-01 |publisher=Te Papa Press |isbn=978-1-877385-87-2 |pages=51 |language=English}}</ref> which were found to be totally inadequate.<ref>{{Cite journal |url=https://ojs.aut.ac.nz/interstices/index.php/Interstices/article/view/260/262 |last=Walker |first=Paul |date=1992 |title=Shaky Ground |journal=Interstices: Journal of Architecture and Related Arts |pages=25–44 |language=en-US |doi=10.24135/ijara.v0i0.260 |doi-broken-date=14 June 2024 |doi-access=free }}</ref> The first earthquake building code was created in 1935.{{sfn|Dowrick|1998|p=141}} Many buildings built during the 1930s and 1940s are heavily reinforced, although more recent research has developed other strengthening techniques. Building regulations established as a result of this event mean that to this day, there are only four buildings in Hawke's Bay taller than five storeys, and as most of the region's rebuilding took place in the 1930s when [[Art Deco]] was fashionable, Hawke's Bay architecture is regarded today as being one of the finest collections of Art Deco in the world.<ref>{{cite web
The earthquake prompted a thorough review of New Zealand [[building code]]s,<ref>{{Cite book |last1=Hicks |first1=Geoffrey R. F. |url=https://www.wikidata.org/wiki/Q126174593 |title=Awesome Forces: The Natural Hazards That Threaten New Zealand |last2=Campbell |first2=Hamish |date=2012-01-01 |publisher=Te Papa Press |isbn=978-1-877385-87-2 |pages=51}}</ref> which were found to be totally inadequate.<ref>{{Cite journal |url=https://ojs.aut.ac.nz/interstices/index.php/Interstices/article/view/260/262 |last=Walker |first=Paul |date=1992 |title=Shaky Ground |journal=Interstices: Journal of Architecture and Related Arts |pages=25–44|doi=10.24135/ijara.v0i0.260 |doi-broken-date=1 November 2024 |doi-access=free }}</ref> The first earthquake building code was created in 1935.{{sfn|Dowrick|1998|p=141}} Many buildings built during the 1930s and 1940s are heavily reinforced, although more recent research has developed other strengthening techniques. Building regulations established as a result of this event mean that to this day, there are only four buildings in Hawke's Bay taller than five storeys, and as most of the region's rebuilding took place in the 1930s when [[Art Deco]] was fashionable, Hawke's Bay architecture is regarded today as being one of the finest collections of Art Deco in the world.<ref>{{cite web
| url = https://www.smithsonianmag.com/travel/earthquake-helped-turn-city-art-deco-capital-world-180958081/ | title = How an Earthquake Turned This New Zealand Town into the Art Deco Capital of the World | last = Nalewicki | first = Jennifer | date = 19 February 2016 | website = SmithsonianMag.com | access-date = 16 November 2023}}</ref>
| url = https://www.smithsonianmag.com/travel/earthquake-helped-turn-city-art-deco-capital-world-180958081/ | title = How an Earthquake Turned This New Zealand Town into the Art Deco Capital of the World | last = Nalewicki | first = Jennifer | date = 19 February 2016 | website = SmithsonianMag.com | access-date = 16 November 2023}}</ref>


At the time of the earthquake, there were no national emergency response organisations or legal provisions in case of such disaster, which was a hindrance to recovery. As a result, new legislation had to be passed quickly,<ref>{{Cite web |last=McSaveney |first=Eileen |date=12 June 2006 |title=The Hawke's Bay Earthquake Act 1931 |url=https://teara.govt.nz/en/document/4569/the-hawkes-bay-earthquake-act-1931 |access-date=12 May 2024 |website=[[Te Ara: The Encyclopedia of New Zealand]]}}</ref> such as the Hawke's Bay Earthquake Act 1931 which received assent on 28 April to give out loans for the rebuild. The [[Great Depression]] caused difficulty gathering funds however, so a large portion came from charity.<ref>{{Cite web |date=2024-05-21 |title=Major New Zealand earthquakes since 1855 - New Zealand Parliament |url=https://www.parliament.nz/mi/pb/research-papers/document/00PLEcoRP2016031/major-new-zealand-earthquakes-since-1855 |access-date=2024-05-11 |website=www.parliament.nz |language=en}}</ref>
At the time of the earthquake, there were no national emergency response organisations or legal provisions in case of such disaster, which was a hindrance to recovery. As a result, new legislation had to be passed quickly,<ref>{{Cite web |last=McSaveney |first=Eileen |date=12 June 2006 |title=The Hawke's Bay Earthquake Act 1931 |url=https://teara.govt.nz/en/document/4569/the-hawkes-bay-earthquake-act-1931 |access-date=12 May 2024 |website=[[Te Ara: The Encyclopedia of New Zealand]]}}</ref> such as the Hawke's Bay Earthquake Act 1931 which received assent on 28 April to give out loans for the rebuild. The [[Great Depression]] caused difficulty gathering funds however, so a large portion came from charity.<ref>{{Cite web |date=2024-05-21 |title=Major New Zealand earthquakes since 1855 New Zealand Parliament |url=https://www.parliament.nz/mi/pb/research-papers/document/00PLEcoRP2016031/major-new-zealand-earthquakes-since-1855 |access-date=2024-05-11 |website=parliament.nz}}</ref>


On the tenth anniversary of the earthquake, the ''[[New Zealand Listener]]'' reported that Napier had risen from the ashes like a phoenix. It quoted the 1931 principal of [[Napier Girls' High School]] as saying "Napier today is a far lovelier city than it was before".{{Citation needed|date=May 2024}}
On the tenth anniversary of the earthquake, the ''[[New Zealand Listener]]'' reported that Napier had risen from the ashes like a phoenix. It quoted the 1931 principal of [[Napier Girls' High School]] as saying "Napier today is a far lovelier city than it was before".{{Citation needed|date=May 2024}}


The New Napier Carnival was held in January 1933 to celebrate the rebuild of the town,<ref name=":0" /><ref>{{Cite web |date= |title=New Napier Week Carnival |url=https://collection.mtghawkesbay.com/objects/73138/new-napier-week-carnival |access-date=14 May 2024 |website=[[MTG Hawke's Bay]]}}</ref> which officially declared it reborn.<ref name=":2" />
The New Napier Carnival was held in January 1933 to celebrate the rebuild of the town,<ref name=":0" /><ref>{{Cite web |title=New Napier Week Carnival |url=https://collection.mtghawkesbay.com/objects/73138/new-napier-week-carnival |access-date=14 May 2024 |website=[[MTG Hawke's Bay]]}}</ref> which officially declared it reborn.<ref name=":2" />

== Memorials ==
== Memorials ==
[[File:Hastings Clock Tower.jpg|thumb|The [[Hastings Clock Tower]] was built in 1935 to symbolise the recovery of the earthquake.]]
[[File:Hastings Clock Tower.jpg|thumb|The [[Hastings Clock Tower]] was built in 1935 to symbolise the recovery of the earthquake.]]
A [[common grave]] was created on 5 February 1931 to bury 101 of the earthquake's victims. Architect [[J. A. Louis Hay]] started designing a memorial for the site in 1932, which consists of an obelisk, a garden, the text "Their sun is gone down while it is yet day", and a written list of the victims known to be buried there.<ref>{{Cite web |title=Napier Earthquake Memorial |url=https://nzhistory.govt.nz/media/photo/napier-earthquake-memorial |access-date=2024-05-11 |website=nzhistory.govt.nz |language=en}}</ref> [[Hastings Clock Tower|A clock tower]] memorial was built in Hastings in 1935, which serves the purpose of symbolising recovery rather than being a memorial.<ref>{{Cite web |title=Hastings clock tower memorial |url=https://nzhistory.govt.nz/media/photo/hastings-clock-tower-memorial |access-date=2024-05-11 |website=nzhistory.govt.nz |language=en}}</ref>
A [[common grave]] was created on 5 February 1931 to bury 101 of the earthquake's victims. Architect [[J. A. Louis Hay]] started designing a memorial for the site in 1932, which consists of an obelisk, a garden, the text "Their sun is gone down while it is yet day", and a written list of the victims known to be buried there.<ref>{{Cite web |title=Napier Earthquake Memorial |url=https://nzhistory.govt.nz/media/photo/napier-earthquake-memorial |access-date=2024-05-11 |website=nzhistory.govt.nz}}</ref> [[Hastings Clock Tower|A clock tower]] memorial was built in Hastings in 1935, which serves the purpose of symbolising recovery rather than being a memorial.<ref>{{Cite web |title=Hastings clock tower memorial |url=https://nzhistory.govt.nz/media/photo/hastings-clock-tower-memorial |access-date=2024-05-11 |website=nzhistory.govt.nz}}</ref>


Hastings holds a commemoration every year on 3 February for the earthquake, which starts at 10.30am and has clock towers ring at 10.47, which was the same time the earthquake struck.<ref>{{Cite web |title=Earthquake Commemoration {{!}} Hastings District Council |url=https://www.hastingsdc.govt.nz/hastings/about-hastings/earthquake-commemoration/ |access-date=2024-05-11 |website=www.hastingsdc.govt.nz}}</ref>
Hastings holds a commemoration every year on 3 February for the earthquake, which starts at 10.30am and has clock towers ring at 10.47, which was the same time the earthquake struck.<ref>{{Cite web |title=Earthquake Commemoration {{!}} Hastings District Council |url=https://www.hastingsdc.govt.nz/hastings/about-hastings/earthquake-commemoration/ |access-date=2024-05-11 |website=hastingsdc.govt.nz}}</ref>


The HMS ''Veronica'' Sunbay memorial is located on Marine Parade, which remembers the crew of the ship ''Veronica''. It was built in 1934 and named in 1937 after the ship was decommissioned. The ship's bell is used for community services. The council decided in 2024 that the memorial will be restored again after it was deemed potentially unsafe.<ref>{{Cite news |date=7 August 2024 |title=Sunbay repairs: Napier City Council to start restoration on HMS Veronica Memorial that honours 1931 quake heroes |url=https://www.nzherald.co.nz/nz/sunbay-repairs-napier-city-council-to-start-restoration-on-hms-veronica-memorial-that-honours-1931-quake-heroes/LKQPOJ7N2RE3XP26FIPMINVTNI/ |access-date=10 August 2024 |work=[[The New Zealand Herald]]}}</ref>
The HMS ''Veronica'' Sunbay memorial is located on Marine Parade, which remembers the crew of the ship ''Veronica''. It was built in 1934 and named in 1937 after the ship was decommissioned. The ship's bell is used for community services. The council decided in 2024 that the memorial will be restored again after it was deemed potentially unsafe.<ref>{{Cite news |date=7 August 2024 |title=Sunbay repairs: Napier City Council to start restoration on HMS Veronica Memorial that honours 1931 quake heroes |url=https://www.nzherald.co.nz/nz/sunbay-repairs-napier-city-council-to-start-restoration-on-hms-veronica-memorial-that-honours-1931-quake-heroes/LKQPOJ7N2RE3XP26FIPMINVTNI/ |access-date=10 August 2024 |work=[[The New Zealand Herald]]}}</ref>


==Gallery==
==Gallery==
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* [[2011 Christchurch earthquake]]
* [[2011 Christchurch earthquake]]

* [[List of earthquakes in 1931]]
* [[List of earthquakes in 1931]]
* [[List of earthquakes in New Zealand]]
* [[List of earthquakes in New Zealand]]

Latest revision as of 08:03, 24 November 2024

1931 Hawke's Bay earthquake
Hastings Post Office
1931 Hawke's Bay earthquake is located in New Zealand
1931 Hawke's Bay earthquake
1931 Hawke's Bay earthquake (New Zealand)
UTC time1931-02-02 22:46:52
ISC event906607
USGS-ANSSComCat
Local date3 February 1931
Local time10:46:52 NZDT
Duration2:20 seconds
Magnitude7.8 Ms
7.7 Mw[1]
Depth14 km (8.7 mi)
Epicentre39°18′S 177°00′E / 39.3°S 177.0°E / -39.3; 177.0
Areas affectedNapier, Hastings, Hawkes Bay
Total damagearound 2000 buildings
Max. intensityMMI IX (Violent)[2]
Casualties256 dead, thousands injured
Damage to the Hawkes Bay Tribune building

The 1931 Hawke's Bay earthquake, also known as the Napier earthquake, occurred in New Zealand at 10:47 am on 3 February, killing 256,[3] injuring thousands and devastating the Hawke's Bay region. It remains New Zealand's deadliest natural disaster. Centred 15 km north of Napier, it lasted for two and a half minutes and had a magnitude of 7.8 Ms (7.7 Mw).[1] There were 525 aftershocks recorded in the following two weeks, with 597 being recorded by the end of February. The main shock could be felt in much of New Zealand, with reliable reports coming in from as far south as Timaru, on the east coast of the South Island.[4]

Tectonic setting

[edit]

New Zealand lies along the boundary between the Indo-Australian plate and Pacific plates. In the South Island most of the relative displacement between these plates is taken up along a single dextral (right lateral) strike-slip fault with a major reverse component, the Alpine Fault. In the North Island the displacement is mainly taken up along the Hikurangi Subduction Zone, although the remaining dextral strike-slip component of the relative plate motion is accommodated by the North Island Fault System (NIFS).[5]

The earthquake is thought to have occurred on one of the larger thrust faults within the accretionary wedge, at between ca. 5 km depth and ca. 20–25 km depth (which is the approximate depth of subducted Pacific plate at that location).[6]

Damage and effects

[edit]
Comparison map of the extent of Ahuriri Lagoon before (left) and after (right) the earthquake

Nearly all buildings in the central areas of Napier and Hastings were levelled (The Dominion noted that "Napier as a town has been wiped off the map").[7] At the time New Zealand's most damaging earthquake to buildings since European settlement began around 1840.[8]

The local landscape changed dramatically, with the coastal areas around Napier being lifted by around two metres.[7] The most noticeable land change was the uplifting of some 40 km2 of sea-bed to become dry land. This included Ahuriri Lagoon, which was lifted more than 2.7 metres[7] and resulted in draining 3,600 hectares (9,000 acres) of the lagoon.[9] Today, this area is the location of Hawke's Bay Airport,[10] housing and industrial developments and farmland.[citation needed]

The material damage of the earthquake was estimated at $823 million.[11]

Fires

[edit]

Within minutes fires broke out in a few chemist shops in Hastings Street, Napier.[12][13] The fire brigade almost had the first fire under control when the second broke out in a shop at the back of the Masonic Hotel.[citation needed] The fire continued to spread through adjoined wooden buildings, which led to the entire town being engulfed in flames by the afternoon.[12] The wind at this point also picked up strength and began blowing from the east, pushing the fires back over the city.[citation needed] The day was hot and dry which increased the fire's ability to spread. With water mains broken, the brigade was unable to save many buildings. Attempts were made at pumping water from the sea, but these failed.[12] Fire engines at Napier's central fire station were covered in debris from the earthquake which made them unavailable for use.[13] Pumping water from Clive Square, they were able to stop the fires spreading south. Only a few buildings in the central Napier area survived. Some withstood the earthquake only to be gutted by fire. Trapped people had to be left to burn as people were unable to free them in time.[citation needed] It took until the following afternoon for the main fires to go out,[12] but the ruins still smouldered for several days.[citation needed]

In Hastings, the fires were quickly brought under control.[citation needed]

Utilities

[edit]

The entire east coast of the North Island lost electricity during the quake, although power was restored to Masterton, Pahiatua, Dannevirke and Waipukurau within two hours, and to Gisborne within ten hours. At Napier substation, the transformers were tipped over by the force of the quake and the high-voltage switchgear damaged, while the Napier to Tuai transmission line was taken out of service after a landslide caused a tower to collapse. A limited supply was restored to Napier and Hastings on 4 February; due to the damage at Napier substation, the Waipukurau to Napier transmission line was jumpered to the low-voltage switchgear at both ends. The Napier to Tuai line was repaired and put back into service on 12 February, while full supply to Napier substation was restored on 29 March.[14]

There was also severe damage to sewerage systems, gas supply and telegraph systems.[15]

Transport

[edit]

The earthquake caused great damage to Napier's roads, railways,[9] bridges and wharves. Rails were badly twisted.[16] The city's tram tracks were also twisted, and were never restored.[17]

New Zealand's first commercial air disaster occurred six days after the quake, when a Dominion Airlines Desoutter monoplane crashed near Wairoa. The small airline had been making three return trips a day between Hastings and Gisborne, carrying passengers and supplies. All three on board were killed.[18]

Et cetera

[edit]

A group of prisoners working at Bluff Hill in Napier had four of their number buried in a landslip by the quake. The remaining prisoners dug them out, but two had been killed. The prisoners re-assembled without any attempt to escape and were locked up in the Napier Jail. In Taradale, Mission Estate missionaries' accommodation block had been built and opened in February 1931. The next day the Hawke's Bay earthquake struck, causing serious damage to the entire Mission. Two priests and seven students were killed when the stone chapel was destroyed. In Havelock North, St Luke's church was damaged (but not destroyed) just before a wedding was due to take place. The couple got married later in the day, but outdoors.[citation needed]

The Napier Daily Telegraph newspaper office was destroyed by the quake.[citation needed] The Hawke's Bay Herald's printing facility in Hastings were also destroyed.[19]

Napier Technical College was destroyed in the earthquakes, which caused it to be disestablished and amalgamated into Napier Girls' High School and Napier Boys' High School.[20]

About 10 per cent of homes on soft ground in Napier experienced ground damage, such as liquefaction.[8] There was a large amount of damage to buildings, mainly ones made of brick; the earthquake occurred at a time before an earthquake building code was introduced.[21]

Casualties

[edit]

The official death toll was 256 although the Napier earthquake memorial lists 258 names.[22] Of these, 161 people were in Napier, 93 in Hastings, and two in Wairoa.[3] Thousands more were injured, with over 400 hospitalised.[12] Places with several deaths include 17 deaths due to Roach's department store collapsing, 15 in an old men's home,[22] nine students in Napier Technical College,[23] eight from Grand Hotel, and seven at the Greenmeadows seminary.[22]

Response

[edit]

Shortly after the earthquake, people escaped to the Marine Parade Beach. After noticing that the shoreline had receded, they ran away in panic under the expectation that a tsunami was on its way. There was, however, no tidal wave; the receded shoreline was caused by the land moving upwards.[24][13]

Telegram from King George V to Governor-General of New Zealand, 3 February 1931

On 4 February over 5,000 people evacuated Napier,[13] mainly women and children. Men were expected to stay to help out with the recovery. The army and navy also arrived in Napier to help with the recovery. Nelson Park served as Napier's "evacuation centre" which was the site of many tents and was able to cater for over 1,000 people from a field kitchen. Many people also lived in tents in Marine Parade and other places. There were several places that gave out free food in Napier and Hawke's Bay, such as in several schools. Water barrels were also kept full to allow for people to take from them, after losing water access from their homes.[12]

Within four days of the quake, cinemas around New Zealand offered news specials about the disaster.[citation needed]

HMS Veronica

[edit]

The death toll might have been much higher had the Royal Navy ship HMS Veronica not been in port at the time. Within minutes of the shock the Veronica had sent radio messages asking for help. The sailors joined survivors to fight the fires, rescue trapped people and help give them medical treatment. The Veronica's radio was used to transmit news of the disaster to the outside world and to seek assistance. The crew from two cargo ships, the Northumberland and Taranaki, also joined the rescue works, while two cruisers, HMS Diomede and HMS Dunedin, were dispatched from Auckland that afternoon with food, tents, medicine, blankets, and a team of doctors and nurses. The cruisers sailed at high speed overnight, arrived on 4 February and provided valuable assistance in all areas until their departure on 11 February.[citation needed]

Aftershocks

[edit]

On 13 February, Hawke's Bay was struck by a 7.3 Ms  aftershock. At the time, this was New Zealand's fourth strongest recorded earthquake. Author Matthew Wright reported that "the power failed three seconds before the earthquake was felt in Napier. People from Napier to Dannevirke ran for their lives as previously damaged buildings cracked and fell".[25] He added "Some inland parts of Hawke's Bay felt this aftershock more strongly than 3 February quake ... but 'there was no damage of any moment'. People rushed into the streets in Dannevirke and Masterton. In Wellington all but one of the clocks stopped working in the Dominion Observatory, and ceiling lights in the Evening Post offices swayed 'more vigorously' than they had the week before".[25] The earthquake of 13 February 1931 is widely regarded as an aftershock of the larger event ten days earlier. But Messrs Adams, Barnett and Hayes commenting on the rapid decline in the frequency of aftershocks in the Journal of Science & Technology stated, "The fresh outbreak on the 13th February, due to the severe shock on that date, may almost be regarded as a separate disturbance, although it probably arose from conditions produced by the original shock on the 3rd".[citation needed]

Aftershocks continued to shake Hawke's Bay frequently until July 1931, where the average aftershock occurrence dropped to less than one daily. Aftershocks continued for several years, with the last major jolt shaking the Bay in April 1934.[citation needed]

Below is a list of all recorded aftershocks following the main event.

Year Month Date Number of aftershocks Largest shock
1931 February 597
3 February 151 5.5 Ms
4 February 55
5 February 50
6 February 29
7 February 24
8 February <20 6.4 Ms
9 February <20
10 February <20
11 February <20
12 February <20
13 February 81 7.3 Ms
14 February 23
15 February 18
16 February 19
1931 March 75
1931 April 52 5.5 Ms
1931 May 40 6.0 Ms
1931 June 40
1931 July 26
1931 August 17
1931 September 20
1931 October 16
1931 November 19
1931 December 14
1932 May 5.9 Ms
1932 September 6.9 Ms
1934 March 6.3 Ms
1934 April 5.6 Ms

In all, 597 earthquakes were recorded at Hastings in February 1931, and more than 900 by the end of December 1931.[25][26]

Recovery

[edit]

The government quickly realised that the Napier borough council would be overwhelmed with organising the rebuild and appointed two commissioners for this task, John Barton and Lachlan Bain Campbell.[27][28] When the commissioners were due to leave in May 1933, they were petitioned to stay, and Barton was invited to stand for the mayoralty, which he declined.[29]

The temporary shopping centre known as "Tin Town"

Several temporary structures were built following the earthquake, including the shopping centre commonly referred to as Tin Town in Clive Square.[12][30] It remained for about two years,[31] housed over 50 businesses, and was created with a £10,000 loan[12] which did not have to be paid back. According to The Press, it was the world's first "pop-up mall".[31]

The earthquake prompted a thorough review of New Zealand building codes,[32] which were found to be totally inadequate.[33] The first earthquake building code was created in 1935.[8] Many buildings built during the 1930s and 1940s are heavily reinforced, although more recent research has developed other strengthening techniques. Building regulations established as a result of this event mean that to this day, there are only four buildings in Hawke's Bay taller than five storeys, and as most of the region's rebuilding took place in the 1930s when Art Deco was fashionable, Hawke's Bay architecture is regarded today as being one of the finest collections of Art Deco in the world.[34]

At the time of the earthquake, there were no national emergency response organisations or legal provisions in case of such disaster, which was a hindrance to recovery. As a result, new legislation had to be passed quickly,[35] such as the Hawke's Bay Earthquake Act 1931 which received assent on 28 April to give out loans for the rebuild. The Great Depression caused difficulty gathering funds however, so a large portion came from charity.[36]

On the tenth anniversary of the earthquake, the New Zealand Listener reported that Napier had risen from the ashes like a phoenix. It quoted the 1931 principal of Napier Girls' High School as saying "Napier today is a far lovelier city than it was before".[citation needed]

The New Napier Carnival was held in January 1933 to celebrate the rebuild of the town,[12][37] which officially declared it reborn.[30]

Memorials

[edit]
The Hastings Clock Tower was built in 1935 to symbolise the recovery of the earthquake.

A common grave was created on 5 February 1931 to bury 101 of the earthquake's victims. Architect J. A. Louis Hay started designing a memorial for the site in 1932, which consists of an obelisk, a garden, the text "Their sun is gone down while it is yet day", and a written list of the victims known to be buried there.[38] A clock tower memorial was built in Hastings in 1935, which serves the purpose of symbolising recovery rather than being a memorial.[39]

Hastings holds a commemoration every year on 3 February for the earthquake, which starts at 10.30am and has clock towers ring at 10.47, which was the same time the earthquake struck.[40]

The HMS Veronica Sunbay memorial is located on Marine Parade, which remembers the crew of the ship Veronica. It was built in 1934 and named in 1937 after the ship was decommissioned. The ship's bell is used for community services. The council decided in 2024 that the memorial will be restored again after it was deemed potentially unsafe.[41]

[edit]

See also

[edit]

Notes

[edit]
  1. ^ a b Webb, T.H.; Anderson, H. (1998). "Focal mechanisms of large earthquakes in the North Island of New Zealand: slip partitioning at an oblique active margin". Geophysical Journal International. 134 (1): 40–86. Bibcode:1998GeoJI.134...40W. doi:10.1046/j.1365-246x.1998.00531.x.
  2. ^ National Geophysical Data Center / World Data Service (NGDC/WDS) (1972). "Significant Earthquake Information". NOAA National Centers for Environmental Information. doi:10.7289/V5TD9V7K.
  3. ^ a b The exact number of deaths varies according to different sources; the New Zealand Listener article cited below gives 258 deaths, but the Bateman New Zealand Encyclopedia gives 256. The difference is due to two people "missing" and presumed dead. Some articles add these two to the death toll, while others do not.
  4. ^ "M 7.4 Hawke's Bay Tue, Feb 3 1931". GeoNet.
  5. ^ Mouslopoulou, V; Nicol, A; Little, T. A; Walsh, J. J (2007), "Terminations of large strike-slip faults: An alternative model from New Zealand", Geological Society, London, Special Publications, 290 (1): 387–415, Bibcode:2007GSLSP.290..387M, doi:10.1144/SP290.15, S2CID 129003001
  6. ^ "Bay quake highlights NZ's vulnerability". gns.cri.nz. GNS Science. Archived from the original on 18 February 2013. Retrieved 23 June 2011.
  7. ^ a b c New Zealand Historical Atlas – McKinnon, Malcolm (Editor); David Bateman, 1997, Plate 87
  8. ^ a b c Dowrick 1998, p. 141.
  9. ^ a b "The Hawke's Bay Earthquake, 1931". An Encyclopaedia of New Zealand. 1966. Retrieved 12 May 2024.
  10. ^ Morton, Jamie (4 December 2023). "Why next major Hawke's Bay earthquake could cause opposite effect of 1931 disaster". The New Zealand Herald. Retrieved 11 May 2024.
  11. ^ Dowrick 1998, p. 140.
  12. ^ a b c d e f g h i "The 1931 Earthquake | Napier City Council". napier.govt.nz. Retrieved 11 May 2024.
  13. ^ a b c d "Hawke's Bay earthquake". my.christchurchcitylibraries.com. Retrieved 15 May 2024.
  14. ^ "AtoJs Online – Appendix to the Journals of the House of Representatives – 1931 Session I-II – D-01 PUBLIC WORKS STATEMENT (BY THE RIGHT HON. J. G. COATES, MINISTER OF PUBLIC WORKS)". atojs.natlib.govt.nz. 1931. Retrieved 26 February 2021.
  15. ^ Dowrick 1998, p. 145.
  16. ^ Dowrick 1998, p. 142-143.
  17. ^ "Napier Earthquake". Christchurch City Libraries. Archived from the original on 16 February 2008. Retrieved 13 February 2008.
  18. ^ "First fatal accident on a scheduled air service in New Zealand". nzhistory.govt.nz. Retrieved 15 April 2024.
  19. ^ "The Hawke's Bay Tribune". PapersPast. Retrieved 11 May 2024.
  20. ^ "H B Heritage News" (PDF). historicplacesaotearoa.govt.nz. 1 May 2014. Retrieved 12 April 2024.
  21. ^ Dowrick 1998, p. 146.
  22. ^ a b c "Deadly Hawke's Bay earthquake". nzhistory.govt.nz. Retrieved 11 May 2024.
  23. ^ "H B Heritage News" (PDF). historicplacesaotearoa.govt.nz. 1 May 2014. Retrieved 11 May 2024.
  24. ^ Fowler, Michael (27 November 2016). "1931 quake sparked tidal-wave fear". Hawke's Bay Today. The New Zealand Herald. Retrieved 16 May 2024.
  25. ^ a b c "Hawke's Bay Earthquakes 1931 « Wild Land". Wildland.owdjim.gen.nz. 13 February 2006. Retrieved 18 June 2015.
  26. ^ Alan G. Hull (1990) Tectonics of the 1931 Hawke's Bay earthquake, New Zealand Journal of Geology and Geophysics, 33:2, 309–320, doi:10.1080/00288306.1990.10425689
  27. ^ McSaveney, Eileen (13 July 2012). "Historic earthquakes – Rebuilding Napier". Te Ara: The Encyclopedia of New Zealand. Retrieved 15 June 2015.
  28. ^ Astwood, Karen (24–26 November 2014). Learning from experience: three case studies of New Zealand natural disasters and engineers' responses, 1878–1953 (PDF). 4th Australasian Engineering Heritage Conference. Lincoln University, New Zealand. Archived from the original (PDF) on 18 January 2015.
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References

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