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Egmont National Park - Mount Taranaki

 

Egmont Nationalpark

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

 

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Mount Taranaki

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

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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last updated:  11.12.2008