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Egmont National Park - Mount Taranaki
Egmont Nationalpark
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Egmont National Park cover 33,534
hectares. Here the volcano Taranaki (or Mt Egmont as it is also known) rules
supreme standing tall above the surrounding landscape. Beside it are two
volcanoes of an earlier era: Kaitake and Pouakai.
In good weather it is a challenging climb for the fit and well prepared. For
those wanting a more relaxing experience there are beautiful walks through
verdant forest to waterfalls, wetlands and excellent viewpoints. Standing as
it does in isolation from other mountains it is one of the best parks from
which to get an elevated view of another New Zealand - the rural heartland.
It was established as a national park in 1900, the second in New Zealand
after its not too distant neighbour, Tongariro.
Egmont National Park can be found on the western coast of New Zealand's
North Island. The nearest towns are New Plymouth, Inglewood, Stratford and
Opunake.
Source: Departement of Conservation |
Mount Taranaki
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Mount Taranaki or Mount Egmont is
a dormant stratovolcano in the Taranaki region on the west coast of New
Zealand's North Island. The 2518-metre-high mountain is one of the most
symmetrical volcanic cones in the world. There is a secondary cone, Fanthams
Peak, on the south side. Because of its resemblance to Mount Fuji, Taranaki
provided the backdrop for the movie The Last Samurai.
Taranaki is geologically young, having commenced activity approximately
135,000 years ago. The most recent volcanic activity was a moderate ash
eruption, of the size of Ruapehu's activity in 1995/1996, that occurred
about 1755 and possibly in the early 1800s, and the last major eruption
occurred around 1655. Recent research has shown that over the last 9000
years minor eruptions have occurred roughly every 90 years on average, with
major eruptions every 500 years.
Hazards
Taranaki is considered unusual in
that it has experienced at least five of its major eruptions by the method
of cone collapse. Few volcanoes have undergone more than one cone collapse.
The vast volume of material involved in these collapses is reflected in the
extensive ringplain surrounding the volcano. There is also evidence of
lahars being a common result of eruption.
Much of the region is at risk from lahars, which have reached as far as the
coast. A volcanic event is unnecessary: even earthquakes combined with heavy
rain or snow could dislodge vast quantities of unstable layers resting on
steep slopes. Many farmers live in the paths of such possible destructive
events.
Although volcanic eruptions are notoriously chaotic in their frequency, some
scientists warn that a large eruption is "overdue". Research from Massey
University indicates that significant seismic activity is likely again in
the next 50 years. Prevailing winds would probably blow ash east, covering
much of the North Island, and disrupting air routes, power transmission
lines and local water supplies.
The mountain's name
For many centuries the mountain
was called Taranaki by Māori. Captain Cook named it Mount Egmont after John
Perceval, 2nd Earl of Egmont, the First Lord of the Admiralty who promoted
Cook's first voyage. It appeared as Mt Egmont on maps until the 1980s, when
it was ruled that the official name is Mount Taranaki or Mount Egmont,
although most regard the two names as interchangeable. The Egmont name still
applies to the national park that surrounds the peak. The name Mount
Taranaki is linguistically redundant, since the word tara means mountain
peak. Naki is thought to come from ngaki, meaning shining, a reference to
the snow-clad winter nature of the upper slopes. Geologists refer to it as
the Egmont Volcano.
Source: Wikipedia |
Maori History
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One version of Maori history
recalls how Te Maunga o Taranaki (Mount Taranaki) once lived in the centre
of New Zealand's North Island with other mountain gods: Tongariro, Ruapehu
and Ngauruhoe. Nearby stood the lovely maid Pihanga with her cloak of deep
green bush, and all the mountain gods were in love with her.
What had been a long, peaceful existence for the mountain gods was disturbed
when Taranaki could no longer keep his feelings in control and dared to make
advances to Pihanga. A mighty conflict between Tongariro and Taranaki
ensued, which shook the foundations of the earth. The mountains belched
forth their anger and darkness clouded the sky.
When peace finally came to the land, Tongariro, considerably lowered in
height, stood close by Pihanga's side. Taranaki, wild with grief and anger,
tore himself from his roots with a mighty wrench and left his homeland.
Weeping, he plunged recklessly towards the setting sun, gouging out the
Whanganui River as he went and, upon reaching the ocean, turned north. While
he slumbered overnight, the Pouakai Range thrust out a spur and trapped
Taranaki in the place he now rests.
According to some versions of Maori history, one day Taranaki will return to
Pihanga and so it is unwise to live along the path between the two
mountains.
When covered with a veil of mist and rain, Taranaki is said to be weeping
for his lost Pihanga. But for now the mountain stands amid its own cloak of
deep green bush, a majestic icon for the region. Already well known for its
unpredictability, Mount Taranakimay some day provide a spectacular
challenge.
Source: New
Plymouth District Council |
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