
Franz Josef Glacier
Interesting facts
- Geologist Julius von Haast named the glacier in 1865 after Emperor Franz Joseph I of Austria.
- At the close of the last ice age, around 18,000 years ago, the glacier reached the present coastline and possibly ran out beyond it.
- In December 1965 a flood burst out of the glacier carrying ice blocks that were still up to half a metre across after travelling 20 km to the Tasman Sea.
- A 1946 postage stamp showed the glacier framed by the altar window of St James Church; by 1954 the ice had vanished from that view, returning briefly in 1997.
- When Haast first reached it, the glacier was far longer than today and its ice surface stood about 300 metres higher.
- The Waiho Loop, an 80-metre-high arc of moraine left by the glacier thousands of years ago, was too rugged to farm and is still cloaked in native forest.
- Ground uncovered by the retreating ice can be dated by its plant cover, with forest succession recording surfaces exposed around 1600, 1750, 1830 and 1951.
- A change in snowfall on the névé takes roughly five to six years to show up as an advance or retreat at the glacier's terminus.
- The first European description of a West Coast glacier, believed to be this one, appears in the 1859 log of the ship Mary Louisa.
- Under mid-range warming projections the glacier could retreat about five kilometres and lose around 38 percent of its mass by 2100.
Why it is worth it
Few glaciers anywhere come down as far or as fast as Franz Josef. It begins in a snowfield of about twenty square kilometres, more than 2,500 metres up in the Southern Alps and over 300 metres deep, and in just eleven kilometres it drops to about 300 metres above sea level, into a valley lined with temperate rainforest. That is the strange picture it offers: blue-white ice between green walls of rainforest, its snout less than twenty kilometres from the Tasman Sea. The glacier is about twelve kilometres long and up to 300 metres thick, and the Waiho River pours grey with rock flour from its snout.
The reason is the sheer amount of snow and rain: up to fifteen metres of precipitation a year falls on the névé, and that fast supply of ice pushes the glacier far below the snowline. It also makes Franz Josef unusually quick to respond to climate. It advanced several times in the twentieth century, most strongly between 1983 and 1999, when it gained more than 1.4 km, but it had already lost about three kilometres between 1893 and 1983, and between 2008 and 2017 it pulled back another 1.5 km. Every few decades meltwater trapped in the ice breaks out in a sudden flood down the valley.
Ngāi Tahu tradition calls the glacier Kā Roimata o Hine Hukatere, the tears of Hine Hukatere. In the story her lover Tuawe was killed by an avalanche on the mountain, and her tears were frozen by Rangi, the Sky Father, into a river of ice. Since the Ngāi Tahu Claims Settlement Act of 1998 the glacier officially bears both names. The European name was given in 1865 by the German geologist Julius von Haast, after the Austrian emperor Franz Joseph I. The glacier lies in Westland Tai Poutini National Park, part of the Te Wāhipounamu World Heritage Area of south-western New Zealand.
Getting there
The township of Franz Josef (Waiau) lies on State Highway 6, about 5 km from the glacier; a sealed road leads from the highway to the valley car park, and the valley walk ends at a lookout well short of the ice. The larger town listed nearby, Timaru, is 132.8 km away in a straight line but on the far side of the Alps. The nearest airport is Hokitika (HKK), 106.0 km up the coast. Walks on the ice itself are made with guides who fly in by helicopter from the township's heliport.
Plan your visit
We have no confirmed visit data yet. Once it is confirmed, this block also carries the date it was checked.
Nearby places
- Aoraki / Mount Cook 14.1 km · summit
- Westland Tai Poutini National Park 13.9 km · national-park
- Lake Matheson 19.6 km · lake
On these lists
From the encyclopaedia
The Franz Josef Glacier is a 12-kilometre-long (7.5 mi) temperate maritime glacier in Westland Tai Poutini National Park on the West Coast of New Zealand's South Island. Together with the Fox Glacier 20 kilometres (12 mi) to the south, and a third glacier, it descends from the Southern Alps to less than 300 metres (980 ft) above sea level.
Wikipedia · CC BY-SA 4.0
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