Mount Ruapehu

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Mount Ruapehu

From Wikipedia, the free encyclopaedia

Mount Ruapehu
Elevation: 2,797 metres (9,175 feet)
Latitude: 39º 18′ S
Longitude: 175º 35′ E
Location: North Island, New Zealand
First ascent: 1879 by G. Beetham & J. P. Maxwell
Easiest route: hike

Mount Ruapehu, or just Ruapehu, is an active stratovolcano, situated at the southern end of the Taupo Volcanic Zone. It is 23 kilometres northeast of the town of Ohakune and 40 kilometres southwest of the southern shore of Lake Taupo.

Ruapehu is the highest point on the North Island of New Zealand. Ruapehu contains three major peaks: Tahurangi (2,797m), Te Heuheu (2,755m) and Paretetaitonga (2,751m). Ruapehu is frequently active, and is one of the largest active volcanoes in New Zealand. It is part of Tongariro National Park.

The name Ruapehu is Maori for pit of noise or exploding pit.

Volcanic Activity

The volcano has erupted in 1861, 1895, 1903, 1945, 1969, 1971, 1975, 1988, 1995 and 1996.

Between eruptions, a crater lake forms from melting snow. Where an eruption has deposited a tephra dam across the lake's outlet, the dam may collapse after the lake has risen above the level of its normal outlet, causing a mud flow known as a lahar.

A lahar on December 24, 1953 caused the Tangiwai disaster, with the loss of 151 lives, when the Tangiwai railway bridge, across the Whangaehu river, collapsed just before an express train crossed the bridge while the lahar was in full flood. It was already known that the river had partially undermined one of the bridge piers and it is believed that the lahar finished the job, causing the bridge to collapse. Although warned of the collapsed bridge, the train driver was unable to stop the train in time.

Spectacular eruptions occurred during 1995 and 1996. Ruapehu had been showing signs of increased activity since late November 1994, with elevated Crater Lake temperatures and a series of eruptions that increased in intensity over about 9 months. Several lahar were observed, both in the Whangaehu river and other areas of the mountain between September 18 and September 25 1995, indicating the Crater lake was being emptied by the eruptions. The Department of Conservation immediately issued hazard warnings and advised all people to keep off the mountain. This eruption also ended the ski season on the mountain. The eruption cloud also disrupted air travel, occasionally closing airports and the central north island airspace. Episodic eruptions continued until the end of November 1995.

Within hours of a major eruption during the night being reported on September 25 1995, news media were trying to get live video of the eruption and amateur photographers had published eruption images on the World Wide Web. A webcamera, dubbed the world's first "VolcanoCam", was also set up. Since then Ruapehu has been monitored by at least one and sometimes several volcanocams.

Another, smaller, eruption phase began on the morning of June 17, 1996, again the mountain was closed to visitors and the ski fields were closed for the season, this time before they even opened.

After the 1996 eruption, it was recognised that a catastrophic lahar could again occur when the crater lake burst the volcanic ash dam blocking the lake outlet. This is the same mechanism that caused the 1953 lahar. The lake has been gradually filling with snowmelt since 1996 and by January 2005 the lake had reached the level of the hard rock rim. As the water level continues to rise, so does the likelihood of the lahar being triggered. The lahar is unlikely to occur prior to the 2005/06 summer. Authorities are currently planning for managing this event safely when it occurs.

Ski Fields

Ruapehu has two commercial skifields, Whakapapa on the northern side and Turoa on the southern slope. The private Tukino field is located on the east of the mountain. The season is generally from July to October but depends on snow and weather conditions. Both skifields are accessible by car and chairlifts, with beginners to advanced skiing slopes. Limited accommodation and refreshments are available at Top O'the Bruce - the car park at the top of Bruce Road - and at the entry to Whakapapa, as well as elsewhere on the mountain. Alpine huts are also provided for trampers and climbers.


Weather conditions can be changeable over the day, and mountain visitors are advised to be prepared and carry basic survival equipment. Although severe weather is unusual and generally forecast, it has claimed several lives over the years, including a party of soldiers undergoing winter survival training. During the same storm a Japanese tourist was trapped in a snow cave for several days after he made the shelter when the weather unexpectedly closed in on him. On July 5, 2003 about 350 skiers and 70 skifield staff were trapped on the mountain overnight at Top O'the Bruce when a sudden snow storm blew up and within a few minutes made the access road too dangerous to descend. They spent the night in relative comfort and all safely descended the next morning. Such rapidly changing conditions are typical of the weather on New Zealand mountains.

Mt. Ruapehu, New Zealand

From NASA Earth Observatory

Satellite Image of Mount Ruapehu

All around the world, people live in places where the threat of natural disaster is high. On the North Island of New Zealand, the Mount Ruapehu volcano is just such a threat. A towering, active stratovolcano (the classic cone-shaped volcano), snow-capped Ruapehu Volcano is pictured in this enhanced-color image. The image is made from topography data collected by the Shuttle Radar Topography Mission aboard the Space Shuttle Endeavour, launched on February 11, 2000, and imagery collected by the Landsat satellite on October 23, 2002.

Ruapehu is one of New Zealand's most active volcanoes, with ten eruptions since 1861. The eruptions aren't the only threat from the volcano, however. Among the most serious threats is a volcanic mudflow called a lahar. In between eruptions, a lake forms in the volcano's caldera from melting snow. If a previous eruption has deposited a dam of ash, rocks and mud in the lake's natural overflow point, then the lake becomes dangerously full, held back only by the temporary dam. In this scene, the lake is nestled among the ridges at the top of the volcano.

Eventually, the dam gives way and a massive flow of mud and debris churns down the mountain toward farmland and towns below. Scientists estimate that Ruapehu has experienced 60 lahars in the last 150 years. A devastating lahar in 1953 killed more than 150 people, who died when a passenger train plunged into a ravine when a railroad bridge was taken out by the lahar. The flank of the volcano below the lake is deeply carved by the path of previous lahars; the gouge can be seen just left of image centre.

Currently scientists in the region are predicting that the lake will overflow in a lahar sometime in the next year. There is great controversy about how to deal with the threat. News reports from the region indicate that the government is planning to invest in a high-tech warning system that will alert those who might be affected well in advance of any catastrophic release. Others feel that the government should combat the threat through engineering at the top of the mountain, for example, by undertaking a controlled release of the lake.

Landsat data provided courtesy of the University of Maryland Global Land Cover Facility Landsat processing by Laura Rocchio, Landsat Project Science Office SRTM 3-arcsecond elevation data courtesy of SRTM Team NASA/JPL/NIMA Visualization created by Earth Observatory staff.

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