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Volcanoes - Ministry of Civil Defence and Emergency Management

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oes<br />

This article outlines how the ‘Contingency Plan<br />

for the Auckl<strong>and</strong> Volcanic Field’ <strong>and</strong> other preparedness<br />

measures provide a framework to manage these unique<br />

circumstances, <strong>and</strong> minimise the risk to Auckl<strong>and</strong><br />

communities.<br />

THE AUCKLAND VOLCANIC FIELD<br />

The earliest eruptions <strong>of</strong> the monogenetic<br />

Auckl<strong>and</strong> Volcanic Field (AVF) are estimated to have<br />

occurred 150,000 years ago. Since this time, another 49<br />

basaltic volcanoes have been created. During the last<br />

20,000 years eruptions have been more frequent with<br />

events occurring, on average, once every 1000 years.<br />

Therefore there is a 5% probability <strong>of</strong> an eruption from<br />

the AVF within the next 50 years. The most recent<br />

<strong>and</strong> largest eruption occurred approximately 750 years<br />

ago. It created Rangitoto Isl<strong>and</strong>, a volcano that erupted<br />

approximately 1/3 <strong>of</strong> the total magma extruded from the<br />

Auckl<strong>and</strong> Volcanic Field.<br />

There are no written or scientific records <strong>of</strong><br />

an eruption from the Auckl<strong>and</strong> Volcanic Field, <strong>and</strong><br />

therefore limited knowledge <strong>of</strong> the length <strong>of</strong> warning<br />

that eruption precursors (eg. volcanic earthquakes) will<br />

give. Geological evidence indicates that volcanic activity<br />

will give rise to a number <strong>of</strong> hazards which will have<br />

minor to severe impacts both in terms <strong>of</strong> damage <strong>and</strong><br />

geographic extent.<br />

VOLCANIC HAZARDS<br />

The areal extent <strong>of</strong> the AVF Volcanic hazards,<br />

described in Table 1, may be greater should there be<br />

more than one eruption vent active at a time. Vents in a<br />

multi-vent episode are expected to develop within a few<br />

kilometres <strong>of</strong> one another.<br />

The highly developed nature <strong>of</strong> metropolitan<br />

Auckl<strong>and</strong>, <strong>and</strong> the reliance <strong>of</strong> its residents on<br />

continuance <strong>of</strong> infrastructural services, makes this city<br />

vulnerable to eruptive events.<br />

A number <strong>of</strong> preparedness measures have been<br />

established to reduce the risk to Auckl<strong>and</strong> communities<br />

from an Auckl<strong>and</strong> Volcanic Field Eruption.<br />

READINESS MECHANISMS<br />

Preparedness mechanisms established to<br />

minimise risk from an AVF eruption include:<br />

• Seismic Monitoring: Monitoring <strong>of</strong> the Auckl<strong>and</strong><br />

Volcanic Field using a network <strong>of</strong> permanent<br />

seismometers.<br />

• Volcanic Contingency Plan: Establishes a framework<br />

to enable a coordinated civil defence emergency<br />

management response <strong>and</strong> identifies roles,<br />

responsibilities <strong>and</strong> actions for organisations that<br />

will contribute to response to, <strong>and</strong> recovery from, an<br />

eruption.<br />

Auckl<strong>and</strong>, with the Auckl<strong>and</strong> Harbour Bridge in the foreground is home to about 1.3 million people. Photo: GNS Lloyd Homer.<br />

33<br />

TEPHRA<br />

June 2004

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