Track description

Hiking time and distance

Mangatepopo Valley and Taranaki in distance.
Mangatepopo Valley and Taranaki in distance

The Tongariro Alpine Crossing is a challenging hike over active volcanoes, rugged and sometimes steep rocky terrain; you need a reasonable level of fitness.

Time: 5 hr 30 min - 8 hr one way
Distance: 19.4 km one way

Your hiking time is relative to your hiking pace, the weather conditions, and how often you stop for rest and sightseeing. Times given for each track section are approximate, as everyone walks at a different pace. Allow longer in winter conditions.

You can walk the track in either direction, although there is less climbing involved if you walk from Mangatepopo (1120 m) to Ketetahi (760 m). Shuttle buses operate for hiking in this direction, with services to Mangatepopo in the morning and back from Ketetahi in the afternoon. Allow an extra hour to walk the track in reverse from Ketetahi to Mangatepopo.

Shorter walking options

You can walk part of the Crossing and still enjoy the fabulous volcanic environment, without doing the whole hike. Drive to either end of the track, walk part way and return the same way to your vehicle.

Mangatepopo Valley to Soda Springs

Time: 1 - 1 hr 30 min

Beginning at the Mangatepopo Road parking area (7 km off of SH 47), the track makes its way up the Mangatepopo Valley. The Mangatepopo hut and campsite is along a short side track 20 minutes from the parking area. Continuing at a gentle gradient the main track climbs alongside a stream and around the edges of old lava flows.

It is generally believed that the Mangatepopo Valley was glacially carved out during the last ice age and subsequently partially in-filled by lava flows from Ngauruhoe.

The water in Mangatepopo stream contains significant levels of dissolved minerals from the volcanic rock the water passes through on the way to the surface. It is not suitable for drinking.

Mangatepopo Valley.
Mangatepopo Valley

Note the different colours on the lava flows as you walk up the valley. The surface colour of younger lava is darker and absorbs much of the sun's heat - this is a harsh environment for plants to grow and the reason why the youngest flows only have a few plants, lichens and moss. The older flows have progressively more species and large plants, which take advantage of the slow build up of precious soil. The vegetation has also been modified by fire and farming.

Mountain buttercups (Ranunculus insignis).
Mountain buttercups
(Ranunculus insignis)

Near the head of the valley a short side track leads to Soda Springs. The springs are an oasis for the moisture loving yellow buttercups and white foxgloves. Read more about the Soda Springs side trip

Soda Springs to South Crater

Time: 1 hr

The track climbs steadily, gaining 340 m from Soda Springs to South Crater. You cross over two lava flows from eruptions in 1870 and two pyroclastic flows from 1975. On a clear day there are magnificent views from this section of track, as far as Mount Taranaki on the west coast.

At the top of the climb the Tongariro Alpine Crossing track continues east across South Crater, and the sign indicates access to Ngauruhoe summit for keen and fit hikers! Read more about the Ngauruhoe summit side trip

South Crater to Red Crater

Time: 45 min - 1 hr

Hikers at Red Crater.
Hikers at Red Crater

Follow the poled route across South Crater to a ridge leading up Red Crater. South Crater is not a real crater but a basin that may have been glacially carved, and has since filled with sediment from the surrounding ridges. An explosion pit in the southeast part of the crater formed around 14,000 years ago. The lava seen from Ngauruhoe dates back to the 1870 eruption.

As you walk up the ridge to Red Crater you can smell sulphur, evidence that Red Crater is still active. Enjoy the spectacular view to the east over the Kaimanawa Forest Park and Desert Road.

Looking into Red Crater notice the unusual formation within, known as a 'dike'. This feature was formed as molten magma moved to the surface through a vertical channel in the crater wall. Having solidified at its outer surface, the dike was later left partially hollow when the magma drained from below. Being more resistant than the surrounding scoria, erosion by wind and rain has now left this structure exposed.

The red colour is from high temperature oxidation of iron in the rock. You can see old lava flows from Red Crater extending into Oturere Valley, South and Central Craters.

From near the top of Red Crater you can take a side trip along a poled route to the summit of Mount Tongariro. Read more about the Tongariro summit side trip

Red Crater to Emerald Lakes

Lower Emerald Lake and Red Crater.
Lower Emerald Lake and Red Crater

Time: 10 - 20 min

The summit of Red Crater (1886 m) is the highest point on the Tongariro Alpine Crossing. From here the track descends steeply to Emerald Lakes and you can see across to the Blue Lake past the Central Crater.

The Emerald Lakes' brilliant colour is caused by minerals leaching from the adjoining thermal area. You can see thermal steaming around the Red Crater and Emerald Lakes.

The Maori name for the lakes is Ngarotopounamu meaning greenstone-hued lakes. The water is cold and acidic, and they freeze in winter.

Take care on the steep descent on loose stony terrain (scree).

The next two sections of the track go through the active volcanic zone, near Te Maari craters - the site of the 2012 volcanic eruptions. Observe the warning signs, and keep your stops to a minimum. Know about the volcanic risks and what to do in an eruption.

Blue Lake (Te Wai-whakaata-o-te-Rangihiroa).
Blue Lake
(Te Wai-whakaata-o-te-Rangihiroa)

Emerald Lakes to Ketetahi shelter

Time: 1 hr - 1 hr 30 min

The Tongariro Northern Circuit Great Walk track to Oturere Hut branches off to the right at the lowest lake, while the Tongariro Alpine Crossing continues over Central Crater, a drainage basic rather than a true crater.

After a short climb out of Central Crater you can see Te Wai-whakaata-o-te-Rangihiroa / Blue Lake - this translates as Rangihiroa's mirror. Te Rangihiroa was the son of local chief Pakaurangi, and Te Maari (after whom the crater is named) was his sister. Te Rangihiroa is said to have explored the Tongariro volcanoes about AD 1750.

The Blue Lake is tapu (sacred) - do not swim in or eat food around the lake. From Blue Lake the track sidles around the flanks of North Crater (a cooled lava lake) and descends to Ketetahi shelter. 

An impact crater and Te Maari steam vents in the distance.
An impact crater and the
Te Maari steam vents in the distance

You can see evidence from the volcanic eruptions in 2012 - excellent views of the new steaming vents at Te Maari craters, impact craters near the track, and damage to the Ketetahi hut.

To protect the fragile soil and plants it's important that you stay on the formed track.

Ketetahi Springs are on private land and hiking the Tongariro Alpine Crossing does not convey any right of access to the springs. Keep to the track.

Ketetahi shelter to Ketetahi parking area

Time: 1 hr 30 min - 2 hr

The track continues to descend through golden tussock-covered slopes to the forest section. The tree line is the end of the Active Volcanic Hazard Zone. There are fantastic views of lakes Rotoaira and Taupo to the north. The cool podocarp-hardwood forest and its bird life provides a final contrast on the long descent to the roadend.

At two points the track passes over the tongue of a lava flow from Te Maari Crater and for a distance follows alongside the Manga-a-te-tipua Stream (polluted with minerals from the Ketetahi Springs). Toward the end of the track you can take a short side track to see a waterfall.

Flax flowers and Lake Rotoraira from Ketetahi track.
Flax flowers and Lake Rotoraira from Ketetahi track


Find out more


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Follow the Outdoor Safety Code:
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2. Tell someone
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4. Know your limits
5. Take sufficient supplies

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Tongariro National Park Visitor Centre
Phone:      +64 7 892 3729
Address:   Whakapapa Village
State Highway 48
Mount Ruapehu
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