A large and shallow earthquake registered by New Zealand's GeoNet as M5.7 hit 15 km east of Christchurch, New Zealand at 00:13 UTC (13:13 local time) on February 14, 2016. The agency is reporting a depth of 15 km (9.3 miles). USGS is reporting M5.8 at a depth of 8.2 km (5.1 miles). Numerous aftershocks are hitting the region.
According to the USGS, the epicenter was located 17 km (11 miles) ENE of Christchurch, 21 km (13 miles) SE of Kaiapoi, 162 km (101 miles) NE of Timaru, 229 km (142 miles) NE of Oamaru, and 293 km (182 miles) SSW of Wellington, New Zealand.
USGS issued a green alert level for shaking-related fatalities. There is a low likelihood of casualties.
Orange alert level was issued for economic losses. Significant damage is likely and the disaster is potentially widespread. Estimated economic losses are less than 1% of GDP of New Zealand. Past events with this alert level have required a regional or national level response.
Overall, the population in this region resides in structures that are resistant to earthquake shaking, though some vulnerable structures exist.
There are about 479 634 people living within 100 km (62 miles) radius.
The quake was too small to have caused a tsunami, GeoNet reported.
"So far we have received 2 974 felt reports from Hawke's Bay to Invercargill as at 18:30 NZT. The highest level of impact from our felt reports so far has been MMI 8 in central and Christchurch. This is also shown in the coloured Shake Map below – which models shaking intensity in Modified Mercalli Intensity."
'Shake Map' image: Shaking intensities measured and modeled from the 5.7 quake. Intensities are related to the Modified Mercalli Intensity Scale. Credit: GeoNet
According to media reports, a cliff has collapsed in Sumner. Shelves have fallen in homes, shops and libraries. Police say at least 450 homes are without power.
Video credit: ECN Australia
Video credit: Breaking Disaster
According to GeoNet, the highest recorded peak ground acceleration (PGA) from this quake was 0.4g (PGA is a good measure of the intensity of the shaking). For contrast, the highest recorded PGA from the February 2011 M6.3 quake was 2.2g.
"Liquefaction in Christchurch often occurs when PGA is above 0.1g and we've had many stations in northern, central, and eastern Christchurch recorded PGAs above this level. This matches the reports that have been coming in of liquefaction around the city."
Liquefaction in Linwood North, courtesy of Andrea Cummings.
GeoNet said that the last time Christchurch experienced a quake this large was nearly 4 years ago, with the magnitude 5.2 quake 20 km (12.4 miles) east of Christchurch.
"There have been aftershocks generated from this earthquake. By 18:30 NZT, there have been 53 aftershocks, the largest is a magnitude 4 quake, 10 km east of Christchurch."
Aftershocks as at 16:15 NZT on February 14, 2016. The mainshock is in peach, and aftershocks are orange. Credit: GeoNet
Aftershock probabilities for the Canterbury region in the next year (source: GeoNet):
- It is likely (63%) that an earthquake of magnitude 5.0-5.9 will occur.
- It is very unlikely (8%) that an earthquake of magnitude 6.0-6.9 will occur.
- It is extremely unlikely (less than 1%) that an earthquake of magnitude greater than 7.0 will occur in the next year.
The aftershock forecast table below covers the coming week, month, and year:
Canterbury region aftershock probabilities
|M5.0 – 5.9||M6.0 – 6.9||M ≥7.0|
|Within a week||0.2||0 – 1||19%||0.02||0 – 1||2%||0.002||0 – 1||<1%|
|Within a month||0.24||0 – 1||21%||0.022||0 -1||2%||0.002||0 – 1||<1%|
Within 1 year
|1.0||0 – 3||
|0.09||0 – 1||
|0.006||0 – 1||<1%|
Issued on February 14, 2016 for the coming year.
This table shows an updated forecast based on a model from international expert elicitation. All forecasts starts from February 14, 2016 and is for the region from 171.6-173.2 degrees east and 43.3-43.9 degrees south.
Within the next year, there is a 63% probability of one or more earthquakes of magnitude 5.0 to 5.9 occurring in the Canterbury region. It is expected that there will be between zero and three events of this magnitude during the coming year.
As can be seen from the table, we expect the greatest concentration of earthquakes to be in the first week. The February 14 magnitude 5.7 earthquake has increased the 1-year probability of an earthquake in the magnitude range 5.0-5.9 from to 49% to 63%.
February 14, 2016 M5.7 quake and aftershocks in relation to December 23, 2011 to January 2012 quakes. Credit: GeoNet
Seismotectonics of the Eastern Margin of the Australia Plate
The eastern margin of the Australia plate is one of the most seismically active areas of the world due to high rates of convergence between the Australia and Pacific plates. In the region of New Zealand, the 3000 km long Australia-Pacific plate boundary extends from south of Macquarie Island to the southern Kermadec Island chain. It includes an oceanic transform (the Macquarie Ridge), two oppositely verging subduction zones (Puysegur and Hikurangi), and a transpressive continental transform, the Alpine Fault through South Island, New Zealand.
Since 1900 there have been 15 M7.5+ earthquakes recorded near New Zealand. Nine of these, and the four largest, occurred along or near the Macquarie Ridge, including the 1989 M8.2 event on the ridge itself, and the 2004 M8.1 event 200 km to the west of the plate boundary, reflecting intraplate deformation. The largest recorded earthquake in New Zealand itself was the 1931 M7.8 Hawke's Bay earthquake, which killed 256 people. The last M7.5+ earthquake along the Alpine Fault was 170 years ago; studies of the faults' strain accumulation suggest that similar events are likely to occur again.
North of New Zealand, the Australia-Pacific boundary stretches east of Tonga and Fiji to 250 km south of Samoa. For 2,200 km the trench is approximately linear, and includes two segments where old (>120 Myr) Pacific oceanic lithosphere rapidly subducts westward (Kermadec and Tonga). At the northern end of the Tonga trench, the boundary curves sharply westward and changes along a 700 km-long segment from trench-normal subduction, to oblique subduction, to a left lateral transform-like structure.
Australia-Pacific convergence rates increase northward from 60 mm/yr at the southern Kermadec trench to 90 mm/yr at the northern Tonga trench; however, significant back arc extension (or equivalently, slab rollback) causes the consumption rate of subducting Pacific lithosphere to be much faster. The spreading rate in the Havre trough, west of the Kermadec trench, increases northward from 8 to 20 mm/yr. The southern tip of this spreading center is propagating into the North Island of New Zealand, rifting it apart. In the southern Lau Basin, west of the Tonga trench, the spreading rate increases northward from 60 to 90 mm/yr, and in the northern Lau Basin, multiple spreading centers result in an extension rate as high as 160 mm/yr. The overall subduction velocity of the Pacific plate is the vector sum of Australia-Pacific velocity and back arc spreading velocity: thus it increases northward along the Kermadec trench from 70 to 100 mm/yr, and along the Tonga trench from 150 to 240 mm/yr.
The Kermadec-Tonga subduction zone generates many large earthquakes on the interface between the descending Pacific and overriding Australia plates, within the two plates themselves and, less frequently, near the outer rise of the Pacific plate east of the trench. Since 1900, 40 M7.5+ earthquakes have been recorded, mostly north of 30°S. However, it is unclear whether any of the few historic M8+ events that have occurred close to the plate boundary were underthrusting events on the plate interface, or were intraplate earthquakes. On September 29, 2009, one of the largest normal fault (outer rise) earthquakes ever recorded (M8.1) occurred south of Samoa, 40 km east of the Tonga trench, generating a tsunami that killed at least 180 people.
Across the North Fiji Basin and to the west of the Vanuatu Islands, the Australia plate again subducts eastwards beneath the Pacific, at the North New Hebrides trench. At the southern end of this trench, east of the Loyalty Islands, the plate boundary curves east into an oceanic transform-like structure analogous to the one north of Tonga.
Australia-Pacific convergence rates increase northward from 80 to 90 mm/yr along the North New Hebrides trench, but the Australia plate consumption rate is increased by extension in the back arc and in the North Fiji Basin. Back arc spreading occurs at a rate of 50 mm/yr along most of the subduction zone, except near ~15°S, where the D'Entrecasteaux ridge intersects the trench and causes localized compression of 50 mm/yr in the back arc. Therefore, the Australia plate subduction velocity ranges from 120 mm/yr at the southern end of the North New Hebrides trench, to 40 mm/yr at the D'Entrecasteaux ridge-trench intersection, to 170 mm/yr at the northern end of the trench.
Large earthquakes are common along the North New Hebrides trench and have mechanisms associated with subduction tectonics, though occasional strike slip earthquakes occur near the subduction of the D'Entrecasteaux ridge. Within the subduction zone 34 M7.5+ earthquakes have been recorded since 1900. On October 7, 2009, a large interplate thrust fault earthquake (M7.6) in the northern North New Hebrides subduction zone was followed 15 minutes later by an even larger interplate event (M7.8) 60 km to the north. It is likely that the first event triggered the second of the so-called earthquake "doublet". (USGS) More information on regional seismicity and tectonics
Featured image credit: USGS
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