Category Archives: Disasters

Rena oil spill – update on bird mortality

The team of Te Papa bird specialists is continuing to help at the wildlife recovery centre in Tauranga as both live and dead oiled birds continue to come ashore 3 weeks after the grounding of the M.V. Rena.

Our job is primarily to make sure that dead birds are correctly identified and, working with Massey University vets, to make an assessment about whether or not they are victims of the oil spill.

Alan Tennyson holding an oiled penguin. Photograph by A. Tennyson, Te Papa

A dead little penguin covered in oil. Photograph by A. Tennyson, Te Papa

The biggest surprise during the last week was finding a dead Chatham Island albatross – a rare species confined to nesting on a single island in the Chatham group. After careful examination, we determined that it was a breeding female but it was not oiled, so its death was probably a natural event unrelated to the grounding of the Rena.

A Chatham Island albatross that apparently died of natural causes being dissected by Massey vet Stuart Hunter. Photograph by A. Tennyson, Te Papa

A Chatham Island albatross that apparently died of natural causes being dissected by Massey vet Stuart Hunter. Photograph by A. Tennyson, Te Papa

While more than a thousand dead birds were recovered in the first 2 weeks after the grounding, the number found during the last week has now, fortunately, dropped to about 20 per day. While nearly all the live oiled birds found have been little penguins, the most common dead birds (of the approximately 1,300 examined) continue to be petrels – in particular diving petrels, which make up about half of those found. The next most common victims are two species that only breed in New Zealand: fluttering shearwater (about 20%) and Buller’s shearwater (about 10%).

These little penguins are recuperating in a purpose-built swimming pool. Filmed by A. Tennyson, Te Papa

The most common victims of the oil spill: hundreds of diving petrels have died. Photograph by A. Tennyson, Te Papa

The most common victims of the oil spill: hundreds of diving petrels have died. Photograph by A. Tennyson, Te Papa

We also examined a dead northern giant petrel that had eaten a lot of milk powder, which we suspect caused its death. Giant petrels are the size of small albatrosses and are well known for their scavenging habits. Many of the containers onboard the Rena contain milk powder, so this may be another unexpected danger for birds resulting from the grounding.

Shane Baylis with a giant petrel that appeared to have died from eating milk powder that spilled from one of the Rena's containers. Photograph by A. Tennyson, Te Papa

Shane Baylis with a giant petrel that appeared to have died from eating milk powder that spilled from one of the Rena's containers. Photograph by A. Tennyson, Te Papa

As salvors continue to battle to remove the remaining oil and stabilise the wrecked Rena, we don’t know how much more oil (and milk powder) is going to end up in the sea. It will be difficult to determine the impacts on seabird populations but the information that we are gathering will be a crucial part of this.

A little blue penguin covered in oil. Photograph by A. Tennyson, Te Papa

Alan Tennyson holding a dead little penguin covered in oil. Photograph by A. Tennyson, Te Papa

By Alan Tennyson, Curator Natural Environment

Oilspill update

Dead oiled wildlife continues to be collected from Bay of Plenty beaches, and the Te Papa Natural Environment team has been assisting with the Wildlife Recovery Centres activities of documenting and recovering species affected by the oil. The species found oiled include the many birds which nest in the Bay of Plenty: most birds returned are from locally common seabird species – Common Diving Petrel and Fluttering Shearwater – the latter a New Zealand endemic species. Aside from these local birds, there are species which breed far further afield, such as the Buller’s Shearwater (from Poor Knights Islands in Northland); the giant petrels from sub-Antarctic sites (some breed in New Zealand but also found around the Southern Ocean), and Blue Petrels likely to be from the Kerguelen Islands in the Indian Ocean. The one Wandering Albatross recovered last week has been identified as coming from a population outside of the New Zealand region, as its body measurements match Indian Ocean or Atlantic Ocean populations, and not those of the smaller-sized southern New Zealand (Antipodes and Auckland Islands) populations.

Red-billed gull oiled at Maketu. Photograph by and reproduced courtesy of Dominique Filippi

Red-billed gull oiled at Maketu. Photograph by and reproduced courtesy of Dominique Filippi

The grim job of sorting through the 1250 or so dead oiled birds returned to the centre by last weekend has to be put into perspective within the very positive atmosphere at the Wildlife Recovery Centre in Tauranga. It has been an amazing operation to be part of. Each hour throughout the day, volunteers, who’d been searching beaches under the wildlife recovery scheme being run by Maritime NZ, arrive with bags and boxes of animals, alive and dead. The Centre is incredibly well run and the spirit of cooperation is very strong. The purpose of ensuring good outcomes for the wildlife affected reigns on the site. The area houses many marquees and structures to enable the washing, feeding, and monitoring the penguins, shags and shore birds which are being recovered to health.

Volunteers preparing for cleanup at Papamoa Beach. Photograph by and reproduced courtesy of Dominique Filippi

Volunteers preparing for cleanup at Papamoa Beach. Photograph by and reproduced courtesy of Dominique Filippi

We worked mainly in the Post-Mortem tent, alongside Veterinary Scientists from Massey University, to identify, and categorise dead wildlife into groups by species and breeding status, and to ascertain how the birds had died. It is a sort of grim zoological forensic study, but done with the intention of finding out as much about the species’ origins (type of bird and population of origin) as possible, to track potential population impacts later on. When the Post-Mortem tent got too much for us, it was a welcome respite to poke our heads into the “Penguin Tent” and witness the fiesty little fellows in their blue tuxedos getting ready for their sardine smoothies. Even more entertaining was seeing the penguins go for their rostered swims in the exercise pools, watched over by their wardens, some of whom had heavily taped fingers as a preventative measure against the damage than can be inflicted by little penguin beaks.

Dead oiled birds being examined by Te Papa scientists. Photograph by and reproduced courtesy of Dominique Filippi

Dead oiled birds being examined by Te Papa scientists. Photograph by and reproduced courtesy of Dominique Filippi

I was very touched by the generosity of the Tauranga locals, when stopping for a much needed cuppa in the Mess Tent, to see piles of plated muffins and other tempting morsels, with messages of support sticky-labeled on the food-wrap encouraging us “Keep up the good work” and “For all those hard working wildlife volunteers”. The centre even had recycling facilities for the waste.

Te Papa has supplied some critical expertise to help a diverse group of professionals and volunteers in the Wildllife Recovery Centre, as our most expert scientists in bird identification are needed to work out which species are which among the oiled dead birds. Our retired curator of birds, Sandy Bartle, along with current curators Colin Miskelly and Alan Tennyson have all played important roles. We will continue to work alongside Massey University vets to cover the wildlife identification activity.

Susan Waugh, Senior Curator Natural Environment.

What bird is that? The grim task of identifying seabirds killed by the M.V. Rena oil spill

Fluttering shearwaters coated in oil from the M.V. Rena. Photo: Colin Miskelly, Te Papa

Te Papa bird staff are providing expert assistance to Maritime New Zealand and Massey University veterinary staff in the form of identifying birds affected by the oil spill. Three current and one former staff member have been a ‘tag team’ since 12 October, identifying the hundreds of corpses recovered by the teams patrolling the beaches, plus any picked up at sea. There are many seabird species potentially present in the Bay of Plenty at this time of year. Making sure that each bird is correctly identified is essential for understanding the impacts of the spill. This information will be crucial if there is any potential for environmental mitigation after the clean-up is complete.

Colin Miskelly (Te Papa's Curator Terrestrial Vertebrates) with a heavily oiled northern giant petrel. Photo: Colin Miskelly, Te Papa

Identifying heavily oiled birds is a challenge, especially when the oil is thick and tar-like. Not only are all plumage markings, bill and leg colour concealed, but it can even be difficult to determine the shape of the bill, which is otherwise diagnostic for many species. For some birds it is necessary to use body structure – the relative length of the tail separates the similarly-sized Buller’s and sooty shearwaters. For others, knowing the one crucial identification character to check (e.g. leg colour) to separate species pairs means that a bird can be identified more rapidly.

Karen and Lucy with oiled seabirds inside the pathology tent. Photo: Colin Miskelly, Te Papa

The work is dirty, smelly, frustrating, and deeply saddening for anyone who knows the beauty of these birds in their prime. Over 20 species of seabird have been identified dead and coated with oil so far, ranging in size from tiny white-faced storm petrels to an enormous wandering albatross. The three main species affected (common diving petrel, fluttering shearwater and Buller’s shearwater) are not threatened species, but their populations will take decades to recover from a mortality event of this scale. All lay a maximum of one egg per pair each year, and the two shearwaters do not start to breed until they are about 5 years old.

 

Bay of Plenty oilspill – Potential for impacts on seabird populations

New Zealand marine areas are home to a wide variety of wildlife, with many unique and threatened species inhabiting our waters. New Zealand’s title as World Seabird Capital is unchallenged, with 1/3 of the worlds’ 346 species present in the New Zealand Exclusive Economic Zone, including ½ of the 22 albatross species of the world. A high proportion (40%) of the worlds albatrosses and their smaller cousins, the petrels and shearwaters breed in New Zealand. Nineteen of these species breed only in New Zealand, and 18 of these are threatened with extinction. The Bay of Plenty is a rich environment for feeding for these species, and many of its small islands are refuges for vulnerable species.

The endemic Black Petrel Procellaria parkinsoni is one example, listed as Vulnerable by the IUCN. The breeding population is estimated at around 1750 pairs of nesting birds. Nesting only on Great and Little Barrier Island, the Black Petrel is active around the Bay of Plenty where the Rena oil spill has occurred. Black Petrels begin to return to their breeding colonies in early October, and feed extensively at this time of year around eastern New Zealand in preparation for egg-laying in November.

Black Petrel (Procellaria parkinsoni)

Black Petrel (Procellaria parkinsoni). Reproduced courtesy of Wikimedia under a CC-BY-3.0 licence

The Black Petrel species is subject to threats from predation at the breeding sites by cats and other introduced predators, and are killed in longline fisheries in New Zealand northern waters.  Any mortality of Black Petrels in the oil spill will be to adding to other deleterious influences on the population and may have very serious impacts on the population as a whole.

Research into the ability of seabird populations to cope with additional mortality has been conducted by the Ministry of Fisheries and has shown that only a small number of additional deaths can be sustained for adult seabirds of many species in the Bay of Plenty area. Additional deaths above the expected ‘natural’ deaths have potential to result in population declines for rare species such as the endemic Black Petrel. Cumulatively, deaths from fishing, and oiling add to unusual climatic incidents like this year’s very strong La Nina weather conditions, and can put a great deal of stress on fragile populations. Reduced numbers of adults of long lived species such as shearwaters and petrels has potential to have a very great effect on the sustainability of their populations, as adults killed in events such as oil spills leave young to die in the nest, and partners to the dead birds may take many years to re-mate.

Another threatened seabird species breeding in the Bay of Plenty is the Pycroft’s petrel, with its major breeding centre on the Mercury Islands. Some populations of seabirds, significant at a national level, breed in the Bay of Plenty – Coromandel area and depend on resources in the Bay of Plenty for food. These include large populations of Flesh-footed Shearwaters (Alderman Islands, Karewa Island, Ohinau Island), Common Diving Petrels (Mercury Islands) and Australasian Gannets (Whale Island).

New Zealand Birds: Gannets, Cape Kidnappers, 1960 s - 1980 s, Hawke's Bay. Brake, Brian. Gift of Mr Raymond Wai-Man Lau, 2001. Te Papa

New Zealand Birds: Gannets, Cape Kidnappers, 1960 s - 1980 s, Hawke's Bay. Brake, Brian. Gift of Mr Raymond Wai-Man Lau, 2001. Te Papa

 
Reef structures can operate like oases in the otherwise sparse feeding environment of the offshore marine systems of New Zealand. Their physical structure catches the current and planktonic larvae settle, out so they support many marine life-forms. Around the reef predatory fish, and other top predators such as whales and seabirds congregate to snatch fish.

Astrolabe Reef is a really well known diving and fishing spot, removed from the effects of coastal sedimentation so has very clear water. This results in a rich algal and invertebrates (sponges, tubeworms, and the like) assemblage and with this comes a very diverse fish community. If the oil and dispersant impact on the algae and invertebrates then the reef community will be significantly degraded. Recreational species like rock lobster, snapper and kingfish are all targeted and obvious, but there also the smaller ‘hidden’ ones like pink cusks and triplefins. These, like the algae kina, paua and sponges, are permanent inhabitants of a reef and incapable of moving on when the habitat is adversely effected by something as toxic as an oil spill and dispersant. The Bay of Plenty is the southern limit for some fish species and the off-shore islands and reefs are the best place to observe them.

Common triplefin, Forsterygion lapillum Hardy, 1989, collected 13 Aug 1991, 750 m South of Tuingara Point, Pourerere, Hawke's Bay, New Zealand. Te Papa

Common triplefin, Forsterygion lapillum Hardy, 1989, collected 13 Aug 1991, 750 m South of Tuingara Point, Pourerere, Hawke's Bay, New Zealand. Te Papa

Oil impacts marine life in a variety of ways, physically coating surfaces and through toxic effects which can affect vital elements such as organs functions and respiration. Recovery of oiled wildlife can be a tenuous process, with many oiled birds suffering damage to their feathers, but also their internal organs as they injest oil when they preen their feathers to clean them. Recovery of oiled birds is possible, but very resource intensive. A large facility to cope with oiled wildlife at Phillip Island, near Melbourne has capacity to cope with 1500 penguins at a time, and is Australia’s answer to dealing with this problem. New Zealand has no centre of comparable capacity at this time.

Auction for Christchurch now on

The auction is up and running!

Te Papa Picture Library and the Brian Brake Estate, with the support of Image Lab and Trade Me have organised an online charity auction to raise funds for the Red Cross Canterbury Earthquake Appeal Fund

Twelve Brian Brake gallery-quality prints will be auctioned starting 5 September, 2011 and closing 14 September, 2011.

Sydney: Bondi beach, Brake, Brian (1927–1988), New South Wales. Gift of Mr Raymond Wai-Man Lau, 2001. Te Papa

Sydney: Bondi beach, Brake, Brian (1927–1988), New South Wales. Gift of Mr Raymond Wai-Man Lau, 2001. Te Papa

Prints usually range in price from $1955 to $2806. Starting bids in the auction range from $1173 -$1683. The reserve…..well that is a surprise, so get bidding to find out!

Each auction includes a copy of the book Brian Brake: Lens on the world (RRP $99.99) printed by Te Papa Press and nominated in the illustrated non-fiction category of the 2011 New Zealand Post Book Awards.

100% of the proceeds of this auction will go to the Red Cross Canterbury Earthquake Appeal Fund to help the rebuilding of this beautiful city.

View the auctions

Auction for Christchurch

Te Papa Picture Library is the authorised agent for the Brian Brake Estate, and for over 2 years I have had the great pleasure of working closely with the Brian Brake Estate, most recently on the project team for the exhibition Brian Brake: Lens on the world, soon to open in Christchurch.

Te Papa Picture Library and the Brian Brake Estate, with the support of Image Lab and Trade Me, are organising an online charity auction to raise funds for the Red Cross Canterbury Earthquake Appeal Fund.

Twelve Brian Brake gallery-quality prints will be auctioned starting 5 September, 2011

’Offerings to the unknown dead, Kyoto’ (Toshi Satow offering a candle). Taken for a series on Japan for ’Life’, 1964, Brake, Brian (1927–1988), Kyoto. Gift of Wai Man Lau, 2010. Te Papa

’Offerings to the unknown dead, Kyoto’ (Toshi Satow offering a candle). Taken for a series on Japan for ’Life’, 1964, Brake, Brian (1927–1988), Kyoto. Gift of Wai Man Lau, 2010. Te Papa

Prints usually range in price from $1955 to $2806.  Starting bids in the auction range from $1173 -$1683, 40% below normal retail price. Reserve price….well that is a surprise, so you will have to get bidding to find out!

100% of the proceeds of this auction will be going to Red Cross Canterbury Earthquake Appeal Fund to help the rebuilding of this beautiful city.

So watch this space people and spread the word!  The links to the auction will be posted soon.

By Becky Masters, Picture Library Manager

Canterbury Earthquake anniversary: send us your photos

“Your humanity is more powerful than any act of nature.” – John Key

On 4 September a year will have passed since the first large earthquake rocked Canterbury and the nation. To mark this event and the significant effect it has had on New Zealanders’ lives we would like to invite you to contribute photos and films to OurSpace that reflect the resilience, innovation and kindness of Cantabrians in the wake of this disaster. We will profile the photos in the OurSpace site in Te Papa from 2 – 9 September.

Since the September 2010 and February 2011 earthquakes in the Canterbury region there has been an immense amount of heartbreak, stress, frustration and anger residents try to rebuild their lives in a city that is physically, systemically and emotionally broken.  However, the earthquake has also brought out the extraordinary in many.

Extraordinary strength – remember Ahsei ‘Ace’ Sopoaga, the ‘awesome Maori guy’ who was really Samoan, who tossed concrete slabs aside ‘like Lego’ to rescue two strangers?

Extraordinary inventiveness and creativity, from  longdrops to Gap Filler, a creative  urban regeneration initiative, to the transformation of Christchurch into a giant skate park.

And thousands of selfless acts of kindness.

We would love you to share your experiences of the good times and moments of inspiration within the hard times with Te Papa, the nation and our visitors through OurSpace. In the meantime, I will leave you with an inspirational short film by James Muir called Love in a Little Town. Its speaks of everything we are after as we mark the anniversary of the September 4 Canterbury Quake: 

‘When everything is stripped back by disaster it reveals what is at the heart of a resilient neighbourhood… Its the love, time and energy of its people… This film tells a little of the healing power of arts and the connected nature of the community in Lyttelton’.

Still from Love in a Little Town

Riders of the storm – thousands of seabirds perish on New Zealand shores

It started as a trickle and soon developed into a flood of devastating proportions. On 11 July 2011 I received an email enquiry from a family at Waikanae seeking help with identifying an unusual seabird that they had found dead on their driveway. It was a Salvin’s prion, a not-too-unexpected discovery near the coast during a winter storm. But the next day a Department of Conservation colleague phoned from Masterton reporting a dozen live prions found scattered inland in the Wairarapa, on the sheltered (eastern) side of the Tararua Range. If that number had reached the leeside, what was happening of the exposed western coast? It didn’t take long to find out.

By 14 July over a thousand live prions had been handed in to wildlife care centres in Wellington and Manawatu, an alarming number given that during prion ‘wrecks’, only a tiny fraction of the birds are still alive by the time they reach land. But what is a prion? and why do they wreck?

Fig. 1. Some of the 660+ stranded prions delivered to Wellington Zoo. These are all broad-billed prions. Photo: Colin Miskelly. Copyright Te Papa

Prions (the singular is pronounced ‘pry-on’) are a group of six small closely-related seabirds that are hugely abundant in southern oceans. They are petrels, and like most petrels, typically breed in enormous colonies on remote islands free of introduced predators. They should not be confused with the other use of the word (in this case pronounced ‘pree-on’) used for a particularly nasty group of infectious proteins that cause the brain-wasting Creutzfeldt–Jakob disease in humans, plus mad-cow disease, and scrapie in sheep.

All prion (bird) species are very similar in size and plumage markings, with the most obvious difference being bill shape, which varies from broad through to narrow or chunky. Within this continuum of variation, some pairs of species are very difficult to distinguish from each other. 

Fig. 2. Bill shapes of four species of prions. Left to right: broad-billed prion, Salvin’s prion, Antarctic prion and fairy prion. Photo: Colin Miskelly. Copyright Te Papa.

The three species with the widest bills have prominent lamellae (comb-like structures) along the edge of the upper mandible, used to filter tiny crustaceans and other small animals and their eggs from sea-water. When combined with a muscular tongue and an extendible pouch below the bill, these adaptations recall those of baleen whales, which feed in a similar way. Perhaps this is why prions are sometimes referred to as ‘whale-birds’. 

Fig. 3. Lamellae (comb-like filters on the edge of the upper mandible) on a broad-billed prion. Photo: Colin Miskelly. Copyright Te Papa.

Prions are well known to New Zealand birdwatchers, even if they are frustratingly difficult to distinguish at sea. Members of the Ornithological Society of New Zealand have for many years patrolled the New Zealand coastline recording the numbers and identities of birds cast ashore. For many, this is the only way to become familiar with prions, particularly in those years when large multi-species wrecks occur. The results of these ‘beach patrols’ are occasionally published in the OSNZ’s journal Notornis. Between 1960 and 1996, over 86,000 prions were found dead on New Zealand beaches; large wrecks occurred in 1961, 1970, 1974, 1975, 1984-86 and 2002, with over 10,000 birds cast ashore in 1974, 1985 and 2002. Earlier wrecks occurred in 1878, 1918 and 1932.

Like all petrels, prions are true seabirds, spending their entire lives at sea apart from the 4 months when they are tied to a nesting burrow and the care of their single egg and resultant chick. At other times they are constantly on the move, often in vast flocks, skimming the waves of the southern oceans in search of productive upwellings. Although frail-looking, they thrive in a part of the globe renown for strong winds. Until they encounter land… 

Fig. 4. A flock of Antarctic prions near South Georgia in the South Atlantic Ocean. Photo: Colin Miskelly. Copyright Colin Miskelly.

Prions move with the wind, using the varying airspeeds on the windward and leeward sides of waves to fly long distances with great energetic efficiency. There are few land masses in the southern ocean, and it is usually easy for flocks of prions to slide around the few obstacles that present. Except, that is, for the 1500 km coast of New Zealand. For ten consecutive days in July 2011, persistent westerly gales in the Tasman Sea pushed prions against New Zealand’s western shores. To start with, the birds moved effortlessly with the wind. Then as land loomed, they started to fight the wind, trying to stay offshore. But the relentless gale continued, consuming the birds’ energy until they were exhausted and driven ashore in tens of thousands.

Although there is a long history of prion wrecks on New Zealand beaches, the scale of the 2011 wreck is unprecedented. Far more prions have been killed in this single event than the 37-year total recorded by the OSNZ. Details are still being collected and collated, but large numbers have been found from at least Dargaville to Okarito, 900 km apart. In places they have stranded at rates over 400 birds per kilometre of coast. And that ignores the birds blown inland.

Even more alarming is that nearly all the birds are broad-billed prions (91% estimated), a locally-breeding species. The two previous largest wrecks of broad-billed prions were between 1100 and 1400 birds. It will be difficult to estimate the full extent of the 2011 wreck, but it is likely to be up to 250 times larger than either the 1961 or 1974 events. 

Fig. 5. Beach-wrecked broad-billed prions, Paekakariki (Wellington west coast), 16 July 2011. Photo: Colin Miskelly. Copyright Te Papa.

Desperate efforts are being made to save some of the birds, including a combined total of over 1000 being hand-fed at Wellington Zoo and Massey University. As the birds are exhausted and emaciated from their struggle against the gale, it is terribly difficult to revive them, and hundreds of those delivered have since died.  

Fig. 6. A rescued broad-billed prion being fed at Wellington Zoo. Photo: Colin Miskelly. Copyright Te Papa.

The 2011 prion wreck will have wreaked a terrible toll on the New Zealand broad-billed prion population. The species also occurs in the South Atlantic, but the birds in New Zealand waters are thought to come from the breeding populations on the Chatham Islands, Snares Islands, and islands around Stewart Island and off the Fiordland coast. Apart from the 330,000 pairs estimated on Rangatira Island in the Chatham Islands, none of these other populations are thought to number more than a few thousand pairs. The total New Zealand population is likely to be little more than a million birds, and so the tragic deaths of (probably) several hundred thousand of them will have a huge impact, especially if the birds in the Tasman Sea were mainly from the less numerous southern (non-Chatham) populations. 

Fig. 7. The calm before the storm – healthy broad-billed prions on Kundy Island, off Stewart Island, March 2011. Photo: Colin Miskelly. Copyright Te Papa.
Other blogs on this topic:
 

Te Papa expresses its sympathy for the people of Christchurch

Tīkoki ana te waka o Aoraki!
Ko Rūaumoko e ngunguru nei!
He parekura! He parekura! He parekura e!

Ko te motu whānui tonu kua pani.
Kei te hunga kua riro ki te pō, moe mai rā.
Kei ngā makorea, he aha rā he kōrero mō koutou?

Ko te Atua hei whakawhirinakitanga atu mō koutou
hei aupehi i te mamae, ā ngākau, ā wairua.
Kia piki te ora, piki te kaha ki a koutou katoa.

The canoe of Aoraki rocks!
It is Rūaumoko, earth shaker, rumbling!
Causing great calamity! 

The nation mourns.
To those who’ve breathed their last breath,
Rest in peace.

To the survivors, what words can we possibly say?
Let the Creator be your support in this time of pain.
Be strong, get well soon.

Like many others throughout New Zealand, staff at Te Papa have close connections through family, friends and colleagues in Christchurch. We have all watched in horror at the devastation that has taken place because of the earthquake on 22 February.

Christchurch Memorial Display, Wellington Foyer, Te Papa

Christchurch Memorial Display in the Wellington Foyer, Te Papa

In the Wellington Foyer, Level 2 of the Museum there is now a place for staff and members of the public to express their condolences. On display is a small boulder of pounamu, symbolising aroha – love and support – for the earthquake victims, their families and friends. It has a tangible connection with the South Island – Te Wai Pounamu – as it was sourced from the Arahura River, Westland. This variety of pounamu is known as kawakawa – as are the leaves of mourning placed on the case in which it sits.

If you would like to help with the Christchurch Quake Appeal, you can do so through the Red Cross, Mayoral Fund and Salvation Army to name a few. There is also a donations box at Te Papa. All donations will be passed on to the emergency services.

Earthquake update from Dr Hamish Campbell, GNS

Kia ora kotou

Dr Hamish Campell has just sent through an article he has written for the NZ Herald. The text is reproduced in full below. Hamish is Senior Scientist at GNS Science and is Te Papa’s geological advisor.

Bill Fry, GNS Science Seismologist, also explains Tuesday’s catastrophic events in this excellent video.

“The 22 February Aftershock

by Dr Hamish Campbell

Some 24 hours have passed since the magnitude 6.3 earthquake that struck the Christchurch area shortly after 1:00pm on Tuesday 22 February. A more precise picture of what is going on beneath Christchurch is beginning to emerge from the pattern of aftershocks and this will improve as time passes.

Seismologists at GNS Science regard this earthquake, large though it is, as an aftershock relating to the magnitude 7.1 Darfield Earthquake that struck Canterbury on 4 September 2010. The technical reason for this is that the epicentre is adjacent to the existing aftershock zone.

As a general rule of thumb, earthquakes that follow a major earthquake are significantly smaller but can attain magnitudes that are about one order of magnitude less than the original. For this reason, GNS Science and its surveillance arm, GeoNet, has been anticipating an aftershock of about magnitude 6, so in that sense this is no surprise.

This devastating event has nevertheless taken us all by surprise because of its violence. The hypocentre was shallow, somewhere between 3 and 5 kilometres deep, and located some 9-10 kilometres southeast of the city centre, more or less half-way between Lyttelton and Sumner on the northern edge of the Port Hills.

The energy involved in this explosive earthquake generated unprecedented ground acceleration both horizontally and vertically. Accelerations in excess of 1.8 times the acceleration due to gravity were recorded by GeoNet ‘strong motion instruments’ deployed in the Christchurch area. This far exceeds the peak ground acceleration recorded in the Darfield Earthquake on 4 September 2010 which was 1.26g, and is the strongest ground acceleration ever recorded in a New Zealand earthquake.

No wonder so many stone buildings, including Christchurch Cathedral, were brought to their knees. Such structures are simply not designed to be thrown sideways or up into the air and left to go into free-fall, even though the fall is all over in a matter of milliseconds to seconds.

The pattern of aftershocks following Tuesday’s big jolt has revealed yet another previously unidentified active fault. This is the culprit that has ruptured within the earth’s crust and which has given rise to the intense seismic shaking in the Christchurch region. However, it may also be thought of as a valve that has enabled pent-up energy to be released. In many ways, faults actually focus and channel energy.

It has ruptured over a length of some 17km on a near vertical plane, slightly inclined to the south, and between 3 and 12 kilometres in depth. It is more or less parallel to the east-west trending Greendale Fault that ruptured in the Darfield Earthquake. It may be thought of as an eastward extension but it is clearly dislocated from the trend of the Greendale Fault and and stepped to the south. The eastern end terminates right on the coast in Sumner. The actual movement was a displacement that is largely sideways (strike-slip) rather than vertical.

Aftershocks are thick and fast at present but should drop off fairly rapidly, more so than after the 7.1 Darfield Earthquake. Nevertheless, they will continue to torment Christchurch for the weeks and months to come.

And why is this happening to Christchurch in the first place? The answer relates in part to the nature of the plate collision in the Canterbury region and in part to its ancient geological history.

The current rate of collision between the Pacific Plate and the Australian Plate is 4 to 5 centimetres per year. This may not seem much but given enough time, it is considerable. Geologists estimate that about 80% of the deformation associated with this plate motion is ‘accommodated’ by uplift of the Southern Alps and movement on the Alpine Fault about 90 kilometres to the west of Christchurch. The remaining 20% of deformation (faulting and folding) is accommodated over a broad zone eastwards across Canterbury.

East–west trending faults in Canterbury are relatively unfamiliar to geologists. Most active faults in New Zealand are roughly parallel to the plate boundary. That is, they trend northeast-southwest. However, if you take away Banks Peninsula (extinct Miocene volcanos that erupted between 10 and 6 million years ago) and the gravels of the Canterbury Plains, the underlying geology is essentially that of the western end of the Chatham Rise. And the Chatham Rise is riddled with old east-west oriented faults. Many seismologists suspect the current plate motion in the South Island is exploiting old faults within the earth’s crust, causing them to fail.

Let us hope there are no other major surprises in the near future. Geological evidence suggests that thee has not been a Darfield Earthquake event near Christchurch city for thousands of years, and no movement on the Greendale Fault for at least 16,000 years. However, this is small consolation for those people who have suffered in this tragic event. If only we could predict such events…but we can’t, not with the precision that we humans need to get by with our daily lives.”




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