1888 North Canterbury Earthquake
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The 1888 North Canterbury earthquake occurred at on 1 September following a sequence of
foreshock A foreshock is an earthquake that occurs before a larger seismic event (the mainshock) and is related to it in both time and space. The designation of an earthquake as ''foreshock'', ''mainshock'' or aftershock is only possible after the full sequ ...
s that started the previous evening, and whose
epicentre The epicenter, epicentre () or epicentrum in seismology is the point on the Earth's surface directly above a hypocenter or focus, the point where an earthquake or an underground explosion originates. Surface damage Before the instrumental pe ...
was in the
North Canterbury Canterbury ( mi, Waitaha) is a region of New Zealand, located in the central-eastern South Island. The region covers an area of , making it the largest region in the country by area. It is home to a population of The region in its current fo ...
region of the South Island of New Zealand. The epicentre was approximately west of Hanmer. In
Christchurch Christchurch ( ; mi, Ōtautahi) is the largest city in the South Island of New Zealand and the seat of the Canterbury Region. Christchurch lies on the South Island's east coast, just north of Banks Peninsula on Pegasus Bay. The Avon River / ...
, about southeast of the epicentre, shaking lasted for 40 to 50 seconds. The
magnitude Magnitude may refer to: Mathematics *Euclidean vector, a quantity defined by both its magnitude and its direction *Magnitude (mathematics), the relative size of an object *Norm (mathematics), a term for the size or length of a vector *Order of ...
of the earthquake is estimated to be in the range 7.0–7.3. Severe damage to farm buildings in the epicentral region was reported and the top of the spire of
ChristChurch Cathedral ChristChurch Cathedral, also called Christ Church Cathedral and (rarely) Cathedral Church of Christ, is a deconsecrated Anglican cathedral in the city of Christchurch, New Zealand. It was built between 1864 and 1904 in the centre of the city, ...
collapsed. It was the first earthquake observed to be associated with mainly horizontal fault displacement.


Tectonic setting

New Zealand lies along the boundary between the
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and
Pacific Plate The Pacific Plate is an oceanic tectonic plate that lies beneath the Pacific Ocean. At , it is the largest tectonic plate. The plate first came into existence 190 million years ago, at the triple junction between the Farallon, Phoenix, and Iza ...
s. In the
South Island The South Island, also officially named , is the larger of the two major islands of New Zealand in surface area, the other being the smaller but more populous North Island. It is bordered to the north by Cook Strait, to the west by the Tasman ...
, most of the relative displacement between these plates is taken up along a single dextral (right lateral)
strike-slip fault In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic ...
with a major
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component, the
Alpine Fault The Alpine Fault is a geological fault that runs almost the entire length of New Zealand's South Island (c. 480 km) and forms the boundary between the Pacific Plate and the Indo-Australian Plate. The Southern Alps have been uplifted on the fa ...
. In the
North Island The North Island, also officially named Te Ika-a-Māui, is one of the two main islands of New Zealand, separated from the larger but much less populous South Island by the Cook Strait. The island's area is , making it the world's 14th-largest ...
, displacement is mainly taken up along the
Kermadec-Tonga subduction zone The Kermadec-Tonga subduction zone is a convergent plate boundary that stretches from the North Island of New Zealand northward. The formation of the Kermadec and Tonga Plates started about 4–5 million years ago. Today, the eastern boundary ...
, although the remaining dextral strike-slip component is accommodated by the
North Island Fault System The North Island Fault System (also known as North Island Dextral Fault Belt or NIFS) is a set of southwest–northeast trending seismically-active faults in the North Island of New Zealand that carry most of the dextral (right lateral) strike- ...
.


Earthquake

The earthquake occurred on the
Hope Fault The Hope Fault is an active dextral (right lateral) strike-slip fault in the northeastern part of South Island, New Zealand. It forms part of the Marlborough Fault System, which accommodates the transfer of displacement along the oblique convergen ...
, one of the group of dextral strike-slip structures known as the
Marlborough Fault System The Marlborough Fault System is a set of four large dextral strike-slip faults and other related structures in the northern part of South Island, New Zealand, which transfer displacement between the mainly transform plate boundary of the Alpine ...
that transfer displacement between the mainly
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and convergent type plate boundaries in a complex zone at the northern end of South Island. Alexander McKay, a geologist working for the geological survey, observed horizontal offsets in farm fences between along the fault. He was the first to associate a strike-slip displacement with an earthquake.


Damage

In the North Canterbury region many buildings were severely damaged, particularly in the Hope Valley and Hanmer areas.
Landslide Landslides, also known as landslips, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, deep-seated grade (slope), slope failures, mudflows, and debris flows. Landslides occur in a variety of ...
s occurred in unconsolidated
sediment Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand an ...
and fissures up to wide were observed. In
Christchurch Christchurch ( ; mi, Ōtautahi) is the largest city in the South Island of New Zealand and the seat of the Canterbury Region. Christchurch lies on the South Island's east coast, just north of Banks Peninsula on Pegasus Bay. The Avon River / ...
, the top of the
Cathedral A cathedral is a church that contains the '' cathedra'' () of a bishop, thus serving as the central church of a diocese, conference, or episcopate. Churches with the function of "cathedral" are usually specific to those Christian denomination ...
spire fell down and minor damage, such as broken chimneys, affected many houses. The
Durham Street Methodist Church The Durham Street Methodist Church in Christchurch was the earliest stone church constructed in the Canterbury region of New Zealand. It is registered as a "Historic Place – Category I" by Heritage New Zealand. The church was severely damaged ...
, Christchurch's first church build with permanent materials, suffered some damage to its stonework. Another building affected was the
Christchurch Normal School Cranmer Court, the former Christchurch Normal School, was one of the most significant heritage buildings in Christchurch, New Zealand. Its demolition, due to some damage in the 2011 Christchurch earthquake, was controversial. History The Canter ...
, where chimneys fell down and ceilings were cracked. Damage was greatest in the northern and northwestern suburbs, probably due to the
peat Peat (), also known as turf (), is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. The peatland ecosystem covers and is the most efficien ...
y sub-soil. One person died of a heart attack during the earthquake.


See also

*
1848 Marlborough earthquake The 1848 Marlborough earthquake was a 7.5 () earthquake that occurred at 1:40 a.m. on 16 October 1848 and whose epicentre was in the Marlborough region of the South Island of New Zealand. In Wellington, the shaking lasted for about two min ...
*
1901 Cheviot earthquake The 1901 Cheviot earthquake occurred at 07:47 NZT on 16 November 1901 (20:15 15 November UTC) with an estimated magnitude of 6.9, centred near the township of Cheviot in the Canterbury region of New Zealand. Damage and casualties A baby was ...
*
2013 Lake Grassmere earthquake The 2013 Lake Grassmere earthquake was a magnitude 6.6 earthquake that occurred at 2:31:05  pm (NZST) on Friday 16 August 2013. The epicentre was located about 10 km south-east of Seddon, under Lake Grassmere, with a focal depth of 8 ...
*
2013 Seddon earthquake The 2013 Seddon earthquake measured 6.5 on the scale and was centred in New Zealand's Cook Strait, around east of the town of Seddon in Marlborough. The earthquake struck at 5:09:30 pm on Sunday 21 July 2013 (05:09 UTC) at a depth of , ...
*
2016 Kaikōura earthquake The 2016 Kaikoura earthquake was a magnitude 7.8 (Mw) earthquake in the South Island of New Zealand that occurred two minutes after midnight on 14 November 2016 NZDT (11:02 on 13 November UTC). Ruptures occurred on multiple faults and the e ...
*
List of earthquakes in New Zealand This is a list of large earthquakes that have occurred in New Zealand. Only earthquakes with a magnitude of 6.0 or greater are listed, except for a few that had a moderate impact. Aftershocks are not included, unless they were of great signifi ...
*
List of historical earthquakes Historical earthquakes is a list of significant earthquakes known to have occurred prior to the beginning of the 20th century. As the events listed here occurred before routine Seismometer, instrumental recordings, they rely mainly on the analys ...


References

{{DEFAULTSORT:1888 North Canterbury Earthquake Earthquakes in New Zealand North Canterbury Earthquake, 1888 North Canterbury, New Zealand History of Canterbury, New Zealand September 1888 events 1888 disasters in New Zealand