Despite a somewhat gloomy forecast and some light rain in
the morning, Hilary and I planned to spend the morning doing a hike that would
bring us to a viewpoint overlooking the Franz Josef glacier. We had packed our bags the night before
so that, theoretically, we could make an early start of it in the morning. We rousted B from her loft and bundled
her next door to M and Deen’s camper – they had their own plans for the morning
– and drove off.
The light is the Franz Josef Glacier itself. They also had a pretty impressive demonstration of just how much rain (and snow) this area on the side of the mountains receives.
That tall bar is Franz Josef, which receives 4000 mm of
rainfall annually! Everyone else
is around 1000-1500 mm.
It’s a good thing we stopped by! The Roberts Point Track was, in fact, closed due to flood
damage. Bummer. The alternatives were the much shorter (1
hr round trip) Glacier View walk, which heads up the bottom of the valley to
the snout of the glacier, and the much longer (8 hrs round trip) Alex Knob
Track, which was more than we had time for today. So, OK, off to the Glacier View.
We locked up and set Bunny on guard duty:
The hit the trail:
The first half of the trail goes through young forest. This part of the valley was under ice
just a century ago.
The trail then breaks out of the forest and into the open glacier valley.
The glacier is, obviously, at the head of the valley. However, due to climate change, it has been rapidly retreating and is not visible from this point. Where I stood to take the previous image was once the end point of the trail, where the glacier ended decades before. The signs next to where I stood had another illustration from just the past few years.
We walked up the valley over the glacial moraine. What a rubbish heap (of rock and gravel)! Through the middle, the river flowed - swift and cold – a battleship grey color. On either side numerous waterfalls cascaded down the valley walls. These are not glacier-fed, but rather come from the copious rain. The streams they make are clear, rather than choked with sediment. Being rain-fed rather than glacier melt, these waterfalls and streams are nominally warmer than the main river, and some of our information indicated they’d be a fun place for an impromptu shower. They were still quite cold on this day, though.
We saw some neat effects of water and ice on the rocks.
As we got closer, we started to encounter a fierce wind rushing down the
valley off the glacier. This was
flowing in the direction opposite the prevailing winds from the coast, which
drive all the weather inland. The
rain had, however, mostly let up by this point, and the clouds were gradually
lifting enough for us to see our goal.
Because the glacier is retreating so quickly, the condition of the end of the trail varies almost daily. Rangers make daily walks up to the snout of the glacier to check conditions. There are large areas cordoned off with yellow rope, and informative signs warning of the dangers on the other side:
Danger of ice and rocks falling on your head! Missing were two other signs we’d seen in a pamphlet
Hilary was hoping to see the “Ice Falls on your head and then you drown” sign. Oh well.
At the end of the track
there is a big pile of moraine, with a
bit of ice still in it, and a prominent barrier that tells you to go no
further.
You! Shall not! Pass! |
And newspaper clippings of what has happened to people who didn’t heed
the warnings:
In the upper right corner you can see a picture of a backhoe
being used to move ice blocks to recover the body of some dead tourist. Cripes!
The icefall of the glacier
itself is quite lovely:
The glacier extends higher and for several miles further up
the valley. Goodness only knows
for how much longer, though.
Deen and B had been visiting another local attraction: the Kiwi House,
where they rear and work to protect the endangered Rowi Kiwi.
B also got to play inside a fake glacier
Because the walk to see the glacier was so easy, we brought the whole
crew back to have a look. By this
point it was raining again (more rain on the moraine, right?):
The rain began to let up as we came out from the forest. B worked to earn her Kiwi Ranger badge
for this park too. One activity
was to rub some stones together to create the “rock flour” that gives the river
its opaque color:
And also to draw and describe different rocks from the valley floor:
We did not make it all the way up to the end of the trail, in part
because the low clouds would not have made for a great view. But we came close enough for B to have
a decent look:
Then back to the visitor center for B to receive her Kiwi Ranger badge!
Our next planned stop had been less than an hour further
down the way: the Fox Glacier. Apparently,
the walking track there has been moved a bit since the glacier has retreated,
and provides a stunning and up close view. However, when we were at the visitor center, we noticed a
bulletin about the road further on, between Haast and our destination for the
night: Wanaka. Due to rock fall
and flooding, part of that road has been reduced to alternate one-way, and
sections of it are closed from 6 pm to 8 am. In order to make it over the Haast Pass and on to Wanaka
tonight, we would have to skip the Fox Glacier (rain and clouds made that a
dubious stop, anyway), and really book it to Haast, where there is a checkpoint
that closes to pass-bound traffic at 6 pm.
Then on and into the Southern Alps!
Very nice!
Unfortunately, we could go no further from here. Not mentioned anywhere was the fact that there is a second checkpoint at Timber Creek. It had been gated and locked for the night not long before we arrived.
You! Shall not! Pass! |
Had we driven straight from Haast we may have made it, but
even that timing seemed doubtful. We
felt deeply misled.
With nothing else to do, we made dinner (a quinoa salad with beans,
corn, and cilantro) and settled in for a quiet sleep. That is not to say that we did any better tonight getting B
to bed early – it was still 10 PM before lights out. Bad parents!
No comments:
Post a Comment