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CHRISTCHURCH, NEW ZEALAND – NOVEMBER 15:  Tourists trapped by the Kaikoura earthquakes arrive by military helicopters at Woodend School grounds on November 15, 2016 in Christchurch, New Zealand. Aftershocks have rocked regions of New Zealand following a 7.8-magnitude earthquake that killed two people yesterday.  (Photo by Martin Hunter/Getty Images)
CHRISTCHURCH, NEW ZEALAND – NOVEMBER 15: Tourists trapped by the Kaikoura earthquakes arrive by military helicopters at Woodend School grounds on November 15, 2016 in Christchurch, New Zealand. Aftershocks have rocked regions of New Zealand following a 7.8-magnitude earthquake that killed two people yesterday. (Photo by Martin Hunter/Getty Images)

SocietyNovember 15, 2016

Kaikoura aftershocks: the latest probability of another big shake

CHRISTCHURCH, NEW ZEALAND – NOVEMBER 15:  Tourists trapped by the Kaikoura earthquakes arrive by military helicopters at Woodend School grounds on November 15, 2016 in Christchurch, New Zealand. Aftershocks have rocked regions of New Zealand following a 7.8-magnitude earthquake that killed two people yesterday.  (Photo by Martin Hunter/Getty Images)
CHRISTCHURCH, NEW ZEALAND – NOVEMBER 15: Tourists trapped by the Kaikoura earthquakes arrive by military helicopters at Woodend School grounds on November 15, 2016 in Christchurch, New Zealand. Aftershocks have rocked regions of New Zealand following a 7.8-magnitude earthquake that killed two people yesterday. (Photo by Martin Hunter/Getty Images)

Geonet has released newly calculated aftershock probabilities that put the chance of one or more M6-6.9 quake in the next day at 37%.

Rapid field reconnaissance indicates that multiple faults have ruptured:

  • Kekerengu Fault at the coast – appears to have had up to 10m of slip
  • Newly identified fault at Waipapa Bay
  • Hope Fault – seaward segment – minor movement
  • Hundalee Fault

In the simplest case an earthquake is a rupture on a single fault plane.

What we are finding in New Zealand is that quite a few of our larger earthquakes involve jumping from rupture on one plane to another in a complex sequence. We first saw that with the Darfield September 2010 quake where multiple segments ruptured together as a single earthquake. We appear to have seen this again.

CHRISTCHURCH, NEW ZEALAND - NOVEMBER 15: Tourists trapped by the Kaikoura earthquakes arrive by military helicopters at Woodend School grounds on November 15, 2016 in Christchurch, New Zealand. Aftershocks have rocked regions of New Zealand following a 7.8-magnitude earthquake that killed two people yesterday. (Photo by Martin Hunter/Getty Images)
Tourists evacuated from Kaikoura arrive in Christchurch earlier today. Photo by Martin Hunter/Getty Images

In terms of what might happen next: The scenarios below provide an overview of how we see this earthquake sequence evolving over the next few days to one month, based on the best information that we have to hand at the moment. As our science information flows in over the next few days we expect that information may evolve.

Scenarios and probabilities

Most earthquake aftershock sequences decay over time, with spikes of activity and occasional larger earthquakes. We have updated our probabilities of larger or similar sized earthquakes; we use probabilities as we cannot predict earthquakes. The probabilities in the table below describe the likely progression of the sequence within the next day, week and month. The scenarios specifically address what we expect within the next 30 days, however, we expect aftershocks to continue for months to years.

Most earthquake aftershock sequences decay over time, with spikes of activity and occasional larger earthquakes. We have updated our probabilities of larger or similar sized earthquakes; we use probabilities as we cannot predict earthquakes. The probabilities in the table below describe the likely progression of the sequence within the next day, week and month. The scenarios specifically address what we expect within the next 30 days, however, we expect aftershocks to continue for months to years.

The scenarios: There are very different probabilities for each scenario; some of these are more concerning than others. We recognise that while these scenarios may increase anxiety the best thing is to be prepared. Remember: If you feel a long or strong earthquake and you are on the coast, evacuate immediately.

We’ve developed three scenarios based on what we know so far but be aware that our understanding is evolving as we do more analysis and receive more data.

Scenario One: Extremely likely (>99% within the next 30 days)

The most likely scenario is that aftershocks will continue to decrease in frequency (and in line with forecasts) over the next 30 days. Felt aftershocks (e.g. over M5) would occur from the M7.5 epicentre near Culverden, right up along the Kaikoura coastline to the Cape Palliser/Wellington area. This includes the potential for aftershocks of between 6.0 and 6.9 (91% within the next 30 days). Scenario one will continue to play out, even if either scenario two or three also occurs.

Scenario Two: Unlikely (15% within the next 30 days)

An earthquake smaller than Monday’s mainshock and between M7.0 to M7.5. There are numerous mapped faults in the Marlborough or Cook Strait areas capable of such an earthquake. It may also occur on an unmapped fault. This earthquake may be onshore or offshore but close enough to cause severe shaking on land. This scenario includes the possibility of an earthquake in the Hikurangi Subduction Zone. Such earthquakes have the potential to generate tsunami.

Scenario Three: Very unlikely (7% within the next 30 days)

A much less likely scenario than the previous two scenarios is that recent earthquake activity will trigger an earthquake larger than Monday’s M7.5 mainshock. This includes the possibility for an earthquake of greater than M8.0, which could be on the ‘plate interface’ (where the Pacific Plate meets the Australian Plate). Although it is still very unlikely, the chances of this occurring have increased since the M7.5 earthquake.

Within this sequence, aftershocks will most likely occur anywhere in the box on the map (see image). It is this geographical region for which the modelling is done. It is important to understand that earthquakes can and do happen outside this box but the box represents the most likely area related to this sequence.

Aftershock Probabilities for the area outlined in the map below

aftershock-probability-map

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For example there is a 37% chance of one or more M6.0-6.9 earthquakes occurring within the next day. We estimate there will be between 0 and 2 earthquakes in this magnitude range within the next day.

Forecast for rectangular box with the coordinates -40.7, 171.7, -43.5, 171.7, -43.5, 175.5, -40.7, 175.5 at 12 noon, Tuesday 15 November.

* 95% confidence bounds.

Tsunami

Our earliest reports are that there is only a little bit of tsunami damage on the coast. Happily, it is not as much as we were expecting.  However, further impact assessments need to be performed before we can conclusively say this for the whole East Coast.

Landslides

We are roughly estimating from yesterday’s reconnaissance flights that there may have been from 80,0000 to 100,000 landslides. Much of the area affected by landslides is in the remote and rugged areas of the Inland and Seaward Kaikoura Ranges. Satellite imagery from both before and after the earthquake is currently being sourced. This will allow a change model to be developed telling us where the landslides have occurred. This will likely take at least two weeks, if not longer because acquiring cloud-free imagery after the earthquake takes time.

The reports of landslide dams points to a potential developing hazard. Landslide dams can last thousands of years, they can fail slowly or they can fail very quickly. When they fail very quickly they can release large volumes of water and sediment into river systems as a flood wave (flash flood). These floods can be hazardous to river users and we would ask people to stay away from the all rivers on the east coast of the South Island from the Hurunui to the Awatere until inspections have been completed and more precise information can be provided.

The landslides that have occurred as a result of the earthquake remain dangerous. Material can move at any time. Please exercise caution when in the vicinity of landslides and cracks in the ground on slopes. If it is raining the threat rises as the water can remobilise the debris as debris flows and debris floods (flash floods). Please avoid landslides in wet weather.

earthquakes-3

For more on the above animation, see here.

A word about other theories

We understand that a “super moon” is going to happen tomorrow night. However, we only report on information and correlations that can be verified through our instruments and backed up by our friends at the USGS.

The above is based on the latest Geonet post from Sara McBride; it updates earlier information summarised here.

Keep going!
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PoliticsNovember 15, 2016

UK, USA… NZ? Why the Greens’ surrender to the dark side of immigration should scare us all

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During last week’s election madness, many of us comforted ourselves with the belief that it couldn’t happen here. But how true is that? Thomas Coughlan sees ominous signs in the New Zealand left’s embrace of anti-immigrant rhetoric.

The youngest voters to participate in last week’s US election would have been only ten years old when Bush Jr. limped out of office, mocked and derided, with one of the lowest approval ratings (25%) of any post-war American president. They may remember, faintly — the curious can remind themselves with a cursory YouTube search — his gaffes, his lapses of leadership, his blank, bovine gaze as he idly leafed through pages of My Pet Goat while his country literally burned. That youngest generation, with only Bush, Obama, and now perhaps Trump in mind, may not even be aware of the magnitude of political disintegration now playing out before them.

We live, as the Chinese curse goes, in interesting times. It is impossible to discern what is acceptable in our ever-shifting political discourse. In the United States and Europe this is particularly pronounced. Trump and Brexit have shown the power of anti-establishment, fringe movements to become part of the mainstream political conversation.

Photo: Aaron P. Bernstein/Getty Images
Photo: Aaron P. Bernstein/Getty Images

For New Zealanders, whose political culture (and political system) reflects Britain’s in so many ways, the politics that enabled the Brexit vote should be particularly alarming. Our recent lurch towards anti-immigrant politics bears strange resemblance to the birth of this latest spate of nativism in Britain. In his most recent volume of memoirs, Alastair Campbell, former spin doctor to Tony Blair, hazarded a guess as to the genesis of the nationalist politics that led to Brexit.

His account exonerates the usual suspects: he does not lay blame at the feet of Enoch Powell, whose ‘Rivers of Blood’ speech ignobly languishes alongside Donald Trump’s ‘Murderers and Rapists’ in the annals of Anglo-American nativist rhetoric, nor does he give credit to bumbling Nigel Farage, Brexit’s (somehow) affable salesman. Instead, Campbell lays the responsibility squarely on the shoulders of the Tory party leadership, who, desperate for a line of attack on the still-popular Tony Blair, tried to weaponise Polish migration during the 2005 election.

“We were more and more aware of the problem politically but there was always a tension between knowing that the economy and public services needed immigration but knowing the issue was causing real concerns,” Campbell told The Guardian, “I think the fact that we won two elections in 2001 and 2005 despite the Tories campaigning on immigration may also have made us complacent.” Labour refused to push back against the anti-immigrant rhetoric of the right, allowing it to mutate, cancer-like into the nation’s single political issue.

From that point, immigration, specifically European immigration, became part of the acceptable political discourse. Incubated by an intellectually and ideologically impoverished Tory leadership, anti-immigrant sentiment reentered the political mainstream. Eventually, Labour countered, not wanting to look weak. From then, legitimated by policy from the two leading parties, immigration became a political football.

The 1922 Committee of hardline Tory backbenchers, many of whom had scarcely uttered a word about immigration, now used it to fuel fresh invective against the European Union. Their chief gripe, that the EU restricted national sovereignty, had never gained much traction since the first European referendum in 1975. In immigration they found the political Trojan horse with which to advance their agenda.

Over the past year, the discussion of immigration in New Zealand has raised echoes of Britain’s anguishing experience. In Winston Peters, we have our own Nigel Farage, a likeable enough nativist hitherto confined to the political fringe. But with Labour, National and finally the Greens all pledging to cut immigration — in the Greens’ case, radically – New Zealand’s three largest parties have allowed this toxic issue to enter the political mainstream, the very thing our MMP system was designed to prevent.

With its focus on issues of nationality and citizenship, immigration is by definition political. To be clear, it does have an effect on house prices and wages if not managed correctly. In the UK, mass migration has uprooted communities and put strain on already underfunded schools and hospitals — it is therefore our right to discuss it. However, it’s disheartening to watch the gatekeepers of established political discourse so spinelessly kowtow to some relatively marginal anxiety over a brief uptick in migration in a pathetic vote-grabbing exercise.

Politicians pretend exploiting anti-immigrant sentiment energises voters at the minor expense of immigrants yet to arrive; that their bluster will encourage Pacific Islanders or Chinese to think twice about emigrating, and stay in their own countries. The recent spilling of Polish blood in the streets of Britain grimly disproves this calculation. The immigrants already arrived pay the heavy price for politicians’ cheaply won electoral gains — there are rivers of blood alright.

The new low in establishment politics was struck at this year’s Tory party conference, where both Prime Minister Theresa May and Home Secretary Amber Rudd articulated, to the braying party faithful, their vision of grateful, supplicant immigrants, ever-conscious of their difference and their debt, and mindful always of their rapacious drain on public finances. These immigrants, if they could learn to tolerate themselves, would be tolerated by Britain. When a radio host read a page of Mein Kampf on air, initially claiming it to be an excerpt from Rudd’s speech, few were surprised.

New Zealanders should look at this in fear. When even the apparently far-sighted Greens look at weaponising high house prices and low wage growth via anti-immigrant sentiment, we know our political discourse has truly jumped the shark. Lurking in the shadows of the nativist madness gripping Britain is the hubris of her politicians who recklessly thought they could open the Pandora’s Box of immigration and tame the horrific nationalism inside. There is only one end to that kind of anti-immigration debate, and it is an end that Britain and America are fast approaching: outright fascism. It is not too much to say that, if conducted incorrectly, the debate on immigration which will inevitably play out at next year’s election may win thousands of votes, but come at the cost of our democracy. As New Zealanders, we must ponder where we would like our own political discourse to be in ten years.

As a student, it took me a long time to work out a definition for politics that reconciled my disparate views on human rights, economics and the provision of social services. For me, ideal politics is not about the ‘what’ or the ‘whether’, but the ‘how’. One of the simplest examples of this is the role of feminism in our democracy. Politics is not the space to question the place of women in our society – we do (or should) know what that place is: absolute liberty. Rather, politics is the place to debate how we might better achieve that place — the how. The same is true of all human rights movements and the same is definitely true of immigration. People move. We always have. It is therefore incumbent upon our political system to deliver us solutions that will facilitate the movement of people to our country, reconciling their needs with those already here.