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!
10 km return | 4 hours return
Rob Roy track is a beaut. A highly accessible track enabling you to experience glaciers and alpine environments in half a day. Great reward for little work.
A spectacular drive up the Matukituki Valley, crossing fords and admiring the classic U-shaped glaciated valleys of Mount Aspiring National Park is only a prelude to this walk. After crossing the milky waters of the Matukituki River West Branch on a swingbridge, beech forest alongside a gorge ends at a bowl with high schist peaks and remnant glaciers encrusting the precipitous faces. And there’s some massive waterfalls if that wasn’t enough. Find a sunny rock for a picnic.
This is a late spring/summer/autumn only walk.
The track crosses known avalanche paths. Check with DoC before embarking on this walk.
From Wanaka follow Wanaka Mount Aspiring Road past Glendu Bay and the entrance to Treble Cone Ski Field. The road becomes unsealed as it passes the working high country stations. Watch for stock on the road, as the farms graze large cattle beasts on the roadside verges. Shepherds and dogs often muster mobs of sheep between paddocks. This is the real New Zealand.
Several fords, some of which will graze the air conditioning units of low ground-clearance vehicles, some slippery patches and narrow sections close to bluffs are obstacles that require careful negotiation. Slow down and pull over. High schist peaks encircle the branch left into the Matukituki West Branch and the carpark at Raspberry Creek. There’s a toilet and shelter here, with the start of the track signposted along a 4WD drive farm road.
Orange triangles mark the initial section through farmland before a crossing of the Matukituki West Branch via a sturdy swing bridge. Entering the shady beech forest the track starts to climb, past a viewpoint up the valley towards Cascade Saddle. Gushing waters of the Rob Roy Stream have incised a deep gorge in the schist with strata of quartz evident in the rock. A milky opalescence in the water due to glacial silt gives clues to the water’s origins.
Cross a slip, with huge boulders perched precariously above, before a section climbs up and over a spur to the Lower Lookout. These first views are surpassed when the track exits the forest (with a toilet thunder box close by) to a viewing area under Rob Roy Glacier, Glengyle Peak, Rob Roy Peak and the seracs of the remnant Rob Roy Glacier. Plumes of spray peel off the massive waterfalls and occasional rock falls pierce the soothing sounds of running water.
It is dangerous to go much further than the rocks at the track end.
Like most of the area, the Haast Schist is a metamorphosed sedimentary rock, laid down as thick layers of mud and marine sand on the Pacific Ocean bed around 250 million years ago. As the weight of overlying layers accumulated the rocks were depressed into areas of great depth, where increased pressure and heat metamorphosed the layers to the mica-schists of today. These blocks of rock were later upthrust and levelled by erosional processes during Mesozoic times. As the rock reformed it was inter-bedded with layers of quartz. These veins not only provide the mesmerising linear patters, but contained the gold on which later exploration of the land was grounded.
The mountain ranges we tramp through today had their genesis around 5 million years ago. River systems developed along lines of weakness in the rock and have since been exaggerated by a series of glacial advances.
In later spring, look for the beech strawberries on the lower sections of track. These resemble golf balls, and are the fruiting bodies of a fungus which has had association with the roots of beech trees since Gondwanaland times over 80 million years ago. The same species is found in Chile.
Listen for the screech of kea.
Long before European exploration, South Island Maori had settled at the mouth of the nearby Dart Valley, using the strategic location as a stopping off point in their search for pounamu. Archaeological remains from the 1300s at the mouth of the Dart River include a series of preserved mounds, accurately portraying the structure of the early dwellings. Slab paved pathways connected the rudimentary ‘houses’ and drainage ditches controlled the water flows. The site is also significant, as examples of flaked hammer dressed Routeburn greenstone were found, along with middens containing moa bones.
Settlement of inland Otago took place from the late 1700s, spurred on by the search for moa. Nearby areas were likely inhabited in the early 1800s by Ngai Tahu, who had displaced Ngati Mamoe and Waitaha from the region.
Feature | Value | Info |
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Organisation |
DOC OtagoCentral government organisation |
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Location |
South Island ▷ Wanaka Region ▷ Wanaka Township |
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Coordinates |