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The 1968 Inangahua earthquake struck west of Murchison, New Zealand, near the small town of
Inangahua Junction Inangahua is a small settlement in the northwest of New Zealand's South Island. It consists of three settled areas: Inangahua Junction at the confluence of the Inangahua and Buller Rivers, north of Reefton and southeast of Westport; Inagahua L ...
at 5:24 am NZDT on 24 May 1968. The earthquake had a moment magnitude of 7.1, a local magnitude of 6.7, a
surface wave magnitude The surface wave magnitude (M_s) scale is one of the magnitude scales used in seismology to describe the size of an earthquake. It is based on measurements of Rayleigh surface waves that travel along the uppermost layers of the Earth. This ma ...
of 7.4 and a maximum Mercalli intensity of X (''Exreme''). It occurred at a depth of , being extremely shallow for an earthquake of its size. It resulted in the deaths of three people, with a further 14 people injured, making it the fifth deadliest earthquake in New Zealand's recorded history (tied with the
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 mi ...
). Numerous aftershocks followed the quake, including 15 that were magnitude 5 or greater and occurred within a month.


Tectonic setting

New Zealand New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 List of islands of New Zealand, smaller islands. It is the ...
lies along the boundary between the Indo-Australian 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 I ...
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 Tasma ...
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 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 ...
. The 1968 Inangahua earthquake occurred along the Northern section of the Alpine Fault, and was considered quite average for what the fault can produce.


Damage

The earthquake ruined many years of expensive work improving in the Inangahua and Buller Gorge areas. In a section of , the road through Buller Gorge was blocked in more than 50 places, either buried under landslides or where the road itself had collapsed into the gorge. The earthquake also damaged or destroyed more than 50 bridges. It also derailed two goods trains, and over of damaged railway track had to be replaced. All roads in and out of Inangahua were blocked by
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 slope failures, mudflows, and debris flows. Landslides occur in a variety of environments, ...
s. The electricity and phone networks were out, and many water pipes in Inangahua were damaged beyond repair. Other West Coast towns were heavily shaken; more than two-thirds of the chimneys in
Greymouth Greymouth () ( Māori: ''Māwhera'') is the largest town in the West Coast region in the South Island of New Zealand, and the seat of the Grey District Council. The population of the whole Grey District is , which accounts for % of the West Coas ...
, Westport, and
Reefton Reefton is a small town in the West Coast region of New Zealand, some 80 km northeast of Greymouth, in the Inangahua River valley. Ahaura is 44 km south-west of Reefton, Inangahua Junction is 34 km to the north, Maruia is 63&n ...
were damaged.


Casualties

At Whitecliffs, a limestone bluff collapsed onto a farmhouse owned by Mr Fred J. Jackson and pushed it downhill, killing Mrs Jackson instantly and fatally injuring her visiting mother, Mrs F.E. Blackmore of Christchurch. Shortly after the earthquake, one man died near
Greymouth Greymouth () ( Māori: ''Māwhera'') is the largest town in the West Coast region in the South Island of New Zealand, and the seat of the Grey District Council. The population of the whole Grey District is , which accounts for % of the West Coas ...
when his car hit a subsided section of road on the run-up to a bridge. An additional three men were killed on 29 May when a Bell 47G-2A helicopter, piloted by Gordon Hutchings, carrying two Post Office linesmen, Robert Pedder and Edwin Steer, from Murchison to Lyell, hit power lines and crashed shortly after take-off.


Landslides

The earthquake and its many aftershocks triggered numerous landslides in the surrounding mountains. A huge landslide dammed the Buller River upstream of Inangahua. The rising water backed up for , raising the river to 30 metres above its normal level. If the landslide dam had burst, the river would have flooded not only Inangahua, but the much larger town of Westport, located downstream at the river mouth. As a precaution, about 10,000 people were evacuated. The dammed river eventually overflowed the landslide debris and gradually eroded it down, without causing serious flooding.


Response

Shortly after the earthquake, a relief centre was set up in the Ministry of Works yard in Inangahua. People gathering there were concerned to hear that radio broadcasts only mentioned minor earthquake activity—the rest of New Zealand seemed unaware of what had happened to their town. The people of Inangahua remained alone in the disaster for several hours, until a driver managed to contact Gisborne on his truck radio. By noon, commercial and
RNZAF The Royal New Zealand Air Force (RNZAF) ( mi, Te Tauaarangi o Aotearoa, "The Warriors of the Sky of New Zealand"; previously ', "War Party of the Blue") is the aerial service branch of the New Zealand Defence Force. It was formed from New Zeal ...
Bell UH-1H The Bell UH-1 Iroquois (nicknamed "Huey") is a utility military helicopter designed and produced by the American aerospace company Bell Helicopter. It is the first member of the prolific Huey family, as well as the first turbine-powered helico ...
helicopters were coming into the area with aid and to survey damage. Help was also needed in isolated areas. Four people, including a constable and a doctor carrying a pack of medical supplies, walked to Inangahua Junction from Reefton. There the doctor treated most patients outdoors because aftershocks were still jolting the area. Meanwhile, one group of about 50 people started walking from Inangahua towards Reefton, a walk of roughly 7 hours. The group of 50 made it safely to Reefton.
RNZAF The Royal New Zealand Air Force (RNZAF) ( mi, Te Tauaarangi o Aotearoa, "The Warriors of the Sky of New Zealand"; previously ', "War Party of the Blue") is the aerial service branch of the New Zealand Defence Force. It was formed from New Zeal ...
UH-1H helicopters and commercial helicopters began flying people to Rotokohu, where they could board buses to Reefton, helicopters checked all outlying farmhouses. In all, 235 people were airlifted out of Inangahua.


Aftermath

Inangahua never fully recovered. Many of the town's residents never went back to their homes, either staying in nearby towns such as Reefton, or deciding to move out of the area entirely. Damaged and collapsed buildings took months—in some cases, years—to be fully restored. The railway line was, however, fully restored, as it forms a key part of the Stillwater–Westport Line. After the earthquake, the area declined. People moved because they feared aftershocks. Employment decreased and school rolls dropped. Shops had fewer customers and more and more ‘Help Wanted' signs were seen in windows. The area later experienced an economic downfall. The quake had a strong effect on the local people. Children were upset and unsettled by the dramatic change in their lives. Many had to move to Reefton School for a period after the quake as the Inangahua School was damaged beyond repair. One school teacher reportedly got his students to draw pictures of their experience. One boy drew a broken house with rain falling on it. A caption read ‘After the earthquake it rained'. Rainfall made the recovery and rescue efforts of the town much more complicated. Many families in the area were left with nothing. They were given supplies by social services such as Red Cross, and in some cases came out of it much better off than when they went in.


See also

* List of earthquakes in 1968 * List of earthquakes in New Zealand


References


External links

*
Experiencing the 1968 Inangahua Earthquake
GNS Science * {{Authority control Inangahua Earthquakes in New Zealand Inangahua History of the West Coast, New Zealand History of the Tasman District