Glaciers 6: To Hokitika - Floods and Mountains

Mt Elie de Beaumont (3117m)) from the main West Coast highway
Mt Elie de Beaumont (3117m)) from the main West Coast highway

The Road to Hokitika

The next day was the crispest, most beautiful morning. We packed our ridiculous amount of gear and in blazing sunshine hit the road for Hokitika. After a blazing row about something so inconsequential. Eh?

 

We followed the snaking route around bluffs and spurs jutting out into the coastal plain. We darted through deep shadows cast by a sun still low in the sky, pressaging a distant but tangible winter.

 

The road to Hokitika was an absolute joy to drive along. Traffic was light, the country was delightful with one river crossing after another and stunning views up to the snowfields of the Southern Alps.

Parcel and mail box on the road to Whataroa from Fox Glacier.
Parcel and mail box on the road to Whataroa from Fox Glacier.

On the other side we had long views over the outwash plains laid down by millions of years of glaciers and rivers transporting unimaginable amounts of debris and sediment from the mountains to the sea.

 

It was not quite how I'd painted the West Coast in my head. I had visions of a sort of wilder Californian Big Sur with a road snaking over promontories above pounding surf and barking seals. That was to come but this was different.

 

The sky clear and the traffic sparse: State Highway 6 heading to Whataroa and Hokitika.
The sky clear and the traffic sparse: State Highway 6 heading to Whataroa and Hokitika.

The contrast between the dazzling blue sky, the glittering glaciers and snowfields, the dark sombre forested hills and the shimmering paddocks of pumped-up green was invigorating.

 

Of all the places this seemed to be the place for me. It seemed to sing with possibility after the harshness of the road from Haast to Fox.

Mt Elie de Beaumont from the coastal flats near the Franz Josef Glacier on State Highway 6 on the west coast of the South Island of New Zealand.
Mt Elie de Beaumont from the coastal flats near the Franz Josef Glacier on State Highway 6 on the west coast of the South Island of New Zealand.

What a difference a few houses and a friendly smile make. The weather could not have been better and the morning had a Laurie-Lee-like spring in its step.

 

Pick-ups drove along the roads with their farm supplies and dogs standing in the back. Drivers raised a friendly finger off the steering wheel, an acknowledgement of our common bonds and purpose. Or so it seemed.

The stunning blue sky of a late summer West-Coast-of-New-Zealand-morning at the turn-off to the Franz Josef Glacier.
The stunning blue sky of a late summer West-Coast-of-New-Zealand-morning at the turn-off to the Franz Josef Glacier. The Sugar Loaf is centre photo

Nothing was too big or ostentatious. Indeed, modesty ruled the roost. No brash houses hogged the view and no giant farm or logging scars broke the ever changing beauty of the road.

 

Bridges steered the road over one after another river, the sun glinting off the worn tarmac surface.

The road to the Franz Josef Glacier running on the right side of the Waiho River with Mts Roon (2233m) and Anderegg (2362m) behind
The road to the Franz Josef Glacier running on the right side of the Waiho River with Mts Roon (2233m) and Anderegg (2362m) behind

The lakes were stunning.

 

Mapourika almost completely still with Mt Tasman towering above and reflected in it. Ianthe/Matahi with its beautiful kahikatea forest rising up from the far end, the ramrod straight trunks of the rare and endangered trees parched white in the sun.

 

And the peaks of the mountains just soared and soared up from the coastal plain, their mountain top glaciers crystal clear in the brilliant light.

Permanent snow and ice on Mt Anderegg
The Andermatten Glacier on Mt Anderegg

Mt Tasman at 3,498 metres. Elie de Beaumont at 3117m. Mt Anderegg (2,362m) with its tumbling Andermatten Glacier and Mt Fletcher (2,467m) rising up above the deeply incised Butler Range.

 

At Whataroa we stopped for petrol on a tight right hand bend. A sign pointed down 'Scally Road' towards the distant sea and heron colonies. 

The single track bridge crossing the Waiho River on Highway 6 Hokitika bound.
The single track bridge crossing the Waiho River on Highway 6 Hokitika bound.

As I filled the tank a most elegant dog regarded us from his battered armchair on the balcony of a tin-roofed hut. He wandered over to say hello.

 

I paid the woman serving in the dark interior of the garage and made some small talk about the winter and the quiet. But it seemed to hold no terrors for her. 

The mountain top glacier on Mt Anderegg
The mountain top glaciers on Mt Anderegg - the Blumenthal (left) and the Croz (right)

We pressed on, always aware of the clock ticking and the miles to go.

 

But the Whataroa River demanded I stop with its staggering backdrop of mountains. And then a huge beautiful Matai tree had to be photographed.

 

And a herd of cows curious in the corner of the field by the road begged to have its picture taken.

Lake Mapourika looking SSW towards Mt Tasman (3498m)
Lake Mapourika looking SSW towards Mt Tasman (3498m)

And then when things seemed to be calming down after Lake Ianthe/Matahi we passed a sign that said, 'Fergusons Bush Development' and later another that said 'Ferguson Farms'.

 

It was as if God Almighty himself had stepped down off a drifting white cloud and had spoken directly to me.

 

(For the significance of this go to my page 'Fergusons Farms: a names a name for that').

Red roof, picket fence and pick-ups, Whataroa.
Red roof, picket fence and pick-ups, Whataroa.
The woman in the filling station in Whataroa.
The woman in the filling station in Whataroa.
The rocky snow free peak of Mt Fletcher in the Southern Alps with Butler range in foreground
The rocky snow free peak of Mt Fletcher (2,467m) in the Southern Alps with Butler range in foreground
A magnificent remnant Matai trees on the Whataroa Flats.
A magnificent remnant Matai trees on the Whataroa Flats.
An Angus and Jersey herd on the road to Hokitika.
An Angus and Jersey herd on the road to Hokitika.
The Kahikatea Swamp Forest at the end if Lake Ianthe/Matahi.
The Kahikatea Swamp Forest at the end if Lake Ianthe/Matahi.
Truck on State Highway 6 heading for Whataroa.
Truck on State Highway 6 heading for Whataroa.

The Waiho River: a catastrophe waiting to happen?

So as not to get too carreid away here I later read about the problem with the short Waiho River that drains the Franz Josef Glacier. It is aggrading (that is dropping more debris than it can carry) at a rate of 300mm/year and the riverbed now stands some two metres above the surrounding land.

The main highway bridge across the Waiho River at Franz Josef Glacier April 2014. See the same bridge under flood conditions belowThe main highway bridge across the Waiho River at Franz Josef Glacier
The main highway bridge across the Waiho River at Franz Josef Glacier April 2014. See the same bridge under flood conditions below in January 2013.

Current flood defences are 'unlikely to provide protection today from a 1-in-10-year event' and the township is 'very vulnerable to a failure in the current flood protection systems'. A large loss of life could occur with an early morning flood in the tourist season when 2000 tourists can be staying in the village (MFE.og.nz)

 

The breaking of ice dams in the glacier adds to the flood risk. There is also a 1-2% chance per annum that a landslip could block the Callery Gorge upriver and then subsequently break releasing a deluge of water onto Franz Josef  Township (NZ CivilDefence).

The Waiho river running towards the sea with floood defence to left - a stopwall - for the vulnerable Franz Josef Township (pop. 270). Aggrading debris can be clearly seen in the river bed.
The Waiho river running seawards with flood defences to left - a stopwall - for the vulnerable Franz Josef Township (pop. 270). Aggrading debris can be clearly seen in the river bed. Rivers in Westland have among the highest sediment loads in the world.

This sounds like a catastrophic disaster waiting to happen. The Westland District Council's Waiho River Severe Flood Hazard Policy Unit says,

 

the only secure solution to the problem is to remove the risk by not populating the area. The Waiho Flood Management Committee has consulted with the community and affected parties and plans are underway for relocation or vacation of existing residences and businesses

 

It seems that earlier attempts at flood defence through the building of control or stop-banks have restricted the spread of the alluvial flan of the river and this has caused it to build up on the river bed. (Davies, RH et al. 2003 Anthropic aggradation of the Waiho River, Westland, New Zealand: microscale modelling, Earth Surface Processes and Landforms,Vol 28, Issue 2).

 

The video below is of the river in flood on 2 January 2013.

Rates of erosion in the Southern Alps of New Zealand are phenomenal and amongst the highest in the world. The combined action of glaciers, earthquakes and rainfall that defies description carve out and carry millions of tons of relatively soft schist and greywacke downhill each year (for rates see comparisons in my Milford Sound: Geology and Glaciation page).


The stone and dust has to go somewhere and as the raging mountain torrents hit the flat coastal plains built up from the Alps over two and half million years of glaciation they slow down and start to drop their loads, so to speak. Flooding and river course changes are an ever-present danger and were at one time the great killer in New Zealand.


On a sunny day it is all very peachy and perfect. We were lucky not to have to battle through the torrential downpours that can turn the West Coast into a death trap for the unwary.

The Waiho River which drains the Franz Josef Glacier and the mouth to the Callery Gorge, a tributary that presents a dam-burst flood hazard with a 2% annual probability.
The Waiho River which drains the Franz Josef Glacier and the mouth to the Callery Gorge, a tributary that presents a dam-burst flood hazard with a 2% annual probability.