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COROMANDEL LIFE LATE SPRING / HOLIDAY 2018

Left: 150 million-year-old Petrified Wood

logs in the Heaven & Earth gallery. Many

customers mistake them for real timber.

The rich brown shades of this polished piece

of petrified wood from Mill Creek in Whitianga

earned it the nickname ‘pumpkin rock’.

Of all the amazing stones of the Coromandel

Peninsula, petrified wood stands out as one

which bridges the gulf between the world of

living organisms and the mineral realm.

The formation of the Coromandel land

mass was almost completely volcanic, and

the many beautiful mineral and gemstone

treasures found here – quartz crystals,

carnelian, jasper, spherulitic rhyolite, andesite

and others – were all created through

volcanic activity.

FORMED BY PREHISTORIC ERUPTIONS

One of the most fascinating of these is

petrified wood, derived from the Greek root

‘petro’ meaning rock or stone – so literally

“wood turned into stone”. It is basically a

type of fossil in which the form of a tree

trunk or branch has evolved to stone in

a long, gradual process initiated by

violent volcanic action.

Uprooted by great flows of lava

or volcanic ash, trees were then

washed down from the highlands

and buried under cooling lava,

volcanic ash, and/or silt. This

sealed the wood in an oxygen-

free environment that prevented

normal decay. Groundwater, rich

in dissolved solids, gradually

seeped through the wood over

centuries, replacing the decaying

plant material cell by cell with silica

(quartz), calcite, pyrite, or other

inorganic materials such as opal.

Because the process is incredibly slow –

taking place literally one molecule at a time

– the rock formed often carries recognisable

features of the original tree or branch such as

bark, wood grain and cellular structures (such

as growth rings). Some specimens are such

accurate preservations that people do not

realise they are fossils until they pick them

up and are shocked by their weight. While its

rare to find these near-perfect preservations,

specimens that exhibit recognisable bark

and woody structures are common.

Recorded age may vary greatly universally,

with some pieces dating as far back as 385

million years. The famous Arizona Petrified

Forest in the USA is estimated at 225 million

years old. In specimens from Arizona, as well

as those from Madagascar, the silica often

appears in a vivid array of colours (see photo

below right).

Some NZ petrified wood has been verified

to be 6-18 million years old, with some

examples showing black edging, indicating

that the wood was charred by volcanic ash

or lava.

Right: Petrified Wood from Arizona like

this colourful piece, is estimated to be

over 225 million years old.

– Photo by Jon Sullivan Public Domain

By Robert Simmons

from Heaven & Earth Gallery

Petrified Wood