Times Colonist

What we can learn from the Christchur­ch earthquake

A similar temblor here would level downtown and likely kill hundreds

- Bob Plecas of Victoria retired after a career as a senior civil servant with the provincial government, where he was deputy minister for 25 ministers in 10 different portfolios. BOB PLECAS

Imagine a child’s jigsaw puzzle, about 20 large pieces. Take five and put them back in the box. Put the puzzle together. Look at it. This is Christchur­ch from the air today, seven years after the earthquake.

Let me recap from down under, where Pauline and I are travelling.

At 4:35 a.m., Sept. 4, 2010, a 7.1-magnitude earthquake, with the epicentre 40 kilometres away and 12 kilometres below the surface, rattled Christchur­ch. Limited damage, but infrastruc­ture cracked and weakened.

On Feb. 21, 2011, during lunch hour, a 6.3-level quake occurred, but only eight km away, and importantl­y, only three km deep. Only 10 seconds, followed by a roller-coaster ride of relief and terror as within 10 minutes there were 10 aftershock­s of magnitude 4.0 or more.

There were 185 killed and 164 seriously injured. One six-storey building — housing the local television headquarte­rs, a medical clinic and an Englishlan­guage school — pancaked, with 115 killed.

About 100,000 houses were damaged, and 10,000 demolished. The central business district closed for two years because 1,240 buildings — one in three — collapsed or were damaged beyond repair. The city’s symbol, the Anglican Cathedral, was uninhabita­ble. Miles of sewer and water systems were destroyed.

Liquefacti­on describes the process during an earthquake where sand, silt and water are combined under incredible pressure. The water/soil/sand mixture boils, volcanoes through cracks to the surface, and begins to move like ocean waves, tilting, sinking and tossing buildings, roads and pipes like flotsam.

The Avon River meanders through the broad plain where Christchur­ch was built, mainly swampland and river silt. The whole downtown and suburbs along the fault line experience­d liquefacti­on. The damage discrimina­tes — one neighbour loses everything, the other across the road, nothing.

The financial costs are astronomic­al. To date, about $32 billion has been spent out of an estimated $45 billion to $50 billion, with reconstruc­tion to be completed by 2026. Expenditur­es have been split between private insurance ($20 billion) and public monies ($12 billion). A government corporatio­n pays benefits to everyone with private fire insurance, but it is capped at $100,000 for home replacemen­t.

Instead of swampland, the area around Victoria’s harbour is built on pilings driven into the ocean. The legislativ­e precinct, the Royal B.C. Museum, the Empress and the Inner Harbour downtown core would be gone. The Saanich Peninsula, if caught along a fault line, would have liquefacti­on destructio­n.

Too dramatic? Come and see Christchur­ch.

Could Victoria handle this type of catastroph­e?

First, this type of disaster planning, both reaction and reconstruc­tion, does not have the top-of-mind priority compared to our collective perception of global warming issues, or the immediacy of the Kinder Morgan project.

Global warming issues come along gradually, like death by a thousand cuts. Earthquake­s are nature’s randomly selected future date for the collective guillotine.

Second, the performanc­e of local government in minding taxpayer monies has not been demonstrat­ed, and any discussion of public monies for capital projects has been terribly jaded by the mishandlin­g of the Blue Bridge replacemen­t and sewerproje­ct implementa­tion.

Third, there is no confidence that under the current regional government system, a disaster that will discrimina­te between municipali­ties will generate a timely, effective and unified response.

Remember Esquimalt versus the NIMBY-other-municipali­ties over the sewer project.

Immediate disasterpr­eparedness planning for protection of citizens when an earthquake or tsunami strikes is already well handled. But, as Christchur­ch shows, that is only half the issue.

The other side of the coin is how we plan for the capital replacemen­t financial issues.

Greater Victoria is the same size as Christchur­ch, and imagine $50 billion required capital for reconstruc­tion. This requires public expenditur­es of about $20 billion. How would we manage that?

New Zealand had proactivel­y built local capacity to deal with an earthquake’s ramificati­ons through amalgamati­on. But this would involve the dreaded ‘A’ word, and my grandchild­ren’s grandchild­ren will be gone before Greater Victoria municipali­ties agree. And, since there is only downside politics for a provincial government to act, it might never happen.

Therefore, if Victoria can’t amalgamate, and the province will not act, where do we go?

The system cries out for new political ideas. Amalgamati­on is a dead horse. Regional government in Greater Victoria has financial accountabi­lity and co-ordination problems among 13 municipali­ties. We are vulnerable.

One idea is found in London, England. It recognizes local government­s are essential for locally delivered services — leave them alone. Instead, they elect a regional government and mayor to be responsibl­e and accountabl­e for a narrow list of responsibi­lities with the concomitan­t tax authority.

Get rid of the current regional system. After all, below the Malahat, our earthquake is when, not if.

 ?? MARK MITCHELL, NEW ZEALAND HERALD VIA AP ?? Rescue workers block off a collapsed building in central Christchur­ch, New Zealand, on Feb. 22, 2011, following a magnitude-6.3 earthquake.
MARK MITCHELL, NEW ZEALAND HERALD VIA AP Rescue workers block off a collapsed building in central Christchur­ch, New Zealand, on Feb. 22, 2011, following a magnitude-6.3 earthquake.
 ?? SCHWEDE66 VIA WIKIPEDIA ?? The process of liquefacti­on loosened hillsides outside Christchur­ch and created flows of silt and mud that swamped city streets.
SCHWEDE66 VIA WIKIPEDIA The process of liquefacti­on loosened hillsides outside Christchur­ch and created flows of silt and mud that swamped city streets.
 ?? GABRIEL VIA WIKIPEDIA ?? The Pyne Gould Building in Christchur­ch following the 2011 earthquake.
GABRIEL VIA WIKIPEDIA The Pyne Gould Building in Christchur­ch following the 2011 earthquake.
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