Marios Gavalas
Author And Researcher
I'm Marios, delivering the best of Aotearoa's nature walks to your device.
I've personally walked hundreds of New Zealand's tracks and spent months in libraries uncovering interesting information on New Zealand/Aotearoa. And you'll find a slice of that research on this page - enjoy!
5.4 km return | 1 hour 30 minutes return
Like its twin, Fox Glacier, this is one of the few glaciers which dips to such low altitude. And it’s a short walk from a carpark close to a road close to a town where you can buy a latte. That’s why lots of people visit. And it’s impressive.
A glacier descending into a rainforest makes for quite a sight - as traveller feedback shows. Although some people say you get better views if you walk beyond the warning signs - don't be tempted. Many people have died when getting too close to the ice. Keep your distance, be happy and wowed!
NOTE - Google Maps doesn't show the access road - but there is one to the pointer on the map.
The track is closed by DoC when there has been rain, or if is raining hard. Pay attention to those warning signs. Don’t be a dick and risk someone else’s life to save yours.
Read https://dcon01mstr0c21winte.dxcloud.episerver.net/visittheglacierssafely
This track is periodically closed due to rain and risk of rockfalls. The signs at the beginning of the track are updated daily and warn of conditions. The final section to the glacier viewpoint is steeper. Do not cross the barriers.
In high summer this can be a bit of a highway.
From Franz Josef township head south on SH6 over the Waihou River and then immediately left. The narrow road is 4 km to the parking area at the road end, from where the tracks are signposted.
From the carpark, head through the regenerating forest. Take the short detour to Sentinel Rock and return to the main track.
The Forest Walk to where the valley opens up is on a good surface, but from here to the terminal face the going gets rougher.
You are now following the river bed and the detritus left by the retreating glacier. Follow the marker poles and cairns, use structures over the streams and be vigilant for rock falls. This is a raw mountain environment.
At the conclusion, there is an incline past some outcrops of schist and around some massive boulders. The viewpoint at the end is around 400 m from the terminal face.
Do not cross the barriers.
Why does Franz Josef Glacier descend so low? It’s a combination of factors.
The West Coast receives a prodigious rainfall due to being a high mountain barrier in the path of moisture laden air circumnavigating the globe in the belt of winds known as the Roaring Forties. Translated to snow, the upper accumulation area, known in geology speak as a nevée, receives around 40 m of snow per year. That’s not a typo. As the layers build up, the weight of overlying snow compacts the flakes to hard ice, which due to gravity starts to flow. Just like a river. The valley then funnels this ice into a steep descent, penetrating the rainforest.
Apparently due to some phenomenon called ‘Climate Change’, the glaciers are retreating. If you visit over a number of years you can see this with your own eyes. Mind you, 17,000 years ago, all the West Coast glaciers were 11 km off shore from the present coastline, 20 km distant.
Julius von Haast was employed as the Provincial Geologist for Canterbury to undertake surveys of the West Coast region. He named the glacier after Emperor Franz Josef of Austria in 1865.
Feature | Value | Info |
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Organisation |
DOC West CoastCentral government organisation |
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Location |
South Island ▷ West Coast ▷ Cron street |
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Directions To Coordinates |
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Coordinates |