Egmont EarthCache

Egmont National Park cover 33,534 hectares. Here the volcano Taranaki (or Mt Egmont as it is also known) stands above the surrounding landscape.There are beside it two volcanoes of an earlier era: Kaitake and Pouakai.

First European to climb Mt Taranaki was Dieffenbach at the end of December 1839. Captain Cook sighted the peak in January 1770 and named it after the Earl of Egmont.

The area around Mts. Egmont, Pouakai, and Kaitake is reserved as the Egmont National Park. Areas, on the north slope of Pouakai and in the west and south of Egmont are popular ski grounds. Ski tows are established on the north side of the Manganui River and the west flank of Fantham Peak. Puketi, a small volcano between Kaitake and Pouakai, is being established as a rhododendron garden by the New Zealand Rhododendron Trust. A small tributary of the Waiwakaiho River in the north-east of Egmont was a very important source of kokowai or red ochre used as a paint by the Maori.

Mt. Egmont is the latest of a series of three large volcanoes on a single volcanic line. The three in order of age and from the north to the south are Kaitake, Pouakai, and Egmont. The first two are much eroded remnants now only 683m (2,240) and 1400m (4,590 ft). The upper 1372m (4,500 ft) of Egmont is composed of lava flows and, although a few flows do descend to 762m (2,500 ft), the lower part out to the coast in the north-west and south and to the base of the East Taranaki highlands was built of vast mudflows during the Pleistocene glaciation. A prominent feature of Egmont is a small subsidiary cone, Fantham Peak 1962m (6,438 ft), on the flank of the main cone and one mile south of the main crater.

A series of eruptions of Mt. Egmont about 350 years ago gave rise to the Burrell vesicular lapilli and the Puniho ash. A tholoid of porphorytic andesite occupied the centre of the crater and was partly destroyed in an eruption which gave rise to the Puniho ash and breached the crater in its north-west quadrant. Because of this history of recent activity Egmont is regarded as dormant and not extinct.

This info is from http://www.teara.govt.nz/1966/E/EgmontMount/EgmontMount/en.

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 Wanganui River as he went and, upon reaching the ocean, turned north. While he slumbered overnight, the Pouakai Ranges thrust out a spur and trapped Taranaki in the place he now rests.

Today the majestic mountain, known as either Mount Egmont or Mount Taranaki, is surrounded by lush, green countryside, blue sea and skies, and protects the fertile region of Taranaki. It also provides unique recreational and educational opportunities for the region's residents and visitors. Dominating our weather and everyday life with its ever changing moods, the mountain provides excellent climbing (with care and planning), skiing, tramping and photography.

The mountain is the source of more than 50 rivers and streams, and is a botanically unique area containing a wide variety of vegetation from sub-tropical semi-coastal forests in the Kaitake Ranges through to sub-alpine herb fields at 1800 metres on the main cone. Many bird species can also be found in the forests surrounding the mountain.

Remember this important information:

Mt Taranaki can be a dangerous place for climbers. Weather conditions can deterioriate very quickly and many ill-prepared climbers have met their death on the slopes of the mountain. If you are going to be using the track system in Egmont National Park for overnight trips, make sure you are properly equipped and well prepared. Make sure you group has a capable leader and that everyone is carrying a sleeping bag, cooking utensils, sufficient high energy food (with some extra for emergencies), a waterproof raincoat and overtrousers, gloves, a hat, and several layers of warm (wool or fleece) clothing. For mountain climbing, specialist equipment is essential. Please check any of the Department of Conservation offices for up-to-date information on appropriate equipment, and weather and track conditions. Fill in an intention form at the office and remember to let them know when you have completed your trip.

Questions

At the above GZ you will find the following answers to the below questions. Please email the answers only. Any logs that give the answers away will be deleted, Also you must post a photo of proof with you log that you have being there this must include your GPS

Once you have emailed me your answers, you can go ahead and log your find, along your photograph (Optional). You don't have to wait for me to reply. Please do not post any answers or spoiler photos in your online log.

Mount Taranaki Statistics

Volcanic activity began in Taranaki some 1.7 million years ago. Mount Taranaki (2518m) and Fanthams Peak (1692m) comprise the volcano, the youngest of four Taranaki volcanic centres. Paritutu and Sugar Loaf Islands/Nga Motu are a spine of lava pushed up from a volcano and have been dated to 1.75 million years. The Kaitake Range was the next volcano to form and volcanic activity began 500,000 years ago. The Pouakai Range volcanic activity began about 250,000 years ago, and 120,000 years ago the volcano was formed and is where nearly all volcanic activity in Taranaki has occurred since.

The last evidence of volcanic activity on the mountain occurred around 1755AD, some 230 years ago. To ensure adequate and early warning of any volcanic activity, the Taranaki Regional Civil Defence organisation has installed the Egmont Volcanic Seismic Monitoring Network, a group of five seismometers designed to gather accurate information about earthquake activity. From this information it can be determined if it is a volcanic earthquake. The seismometers have been installed at five sites at various altitudes. This monitoring may provide weeks or even months warning that something is starting to happen under the mountain.

According to some versions of Maori history, one day Taranaki will return to Pihanga and that 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 Egmont/Taranaki may some day provide a spectacular challenge.

Above info from

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