A couple of days before the New Year, I made a quick trip to Bobs Cove, a beauty spot some 14 km west of Queenstown along the road to Glenorchy. Bobs Cove is at the bottom left of this aerial view: a small, sheltered bay across which the words ‘Bob’s Cove Track’ are printed.
Officially spelled without an apostrophe, Bobs Cove is on the western end of a promontory that’s full of other attractions as well. These include a Lord of the Rings filming site at Twelve Mile Delta, where you can also pan for gold.
Twelve Mile Delta isn’t twelve miles from Queenstown: it is the delta of Twelve Mile Creek, which originates up in the hills and curves toward Queenstown before entering the lake.
A lakefront track called the Bobs Cove Track runs between Twelve Mile Delta and Bobs Cove.
Here’s a photo of the entrance to the Bobs Cove Track at Twelve Mile. There’s also a track that goes up to Mount Crighton.
There’s lots of native bush, which is unusual for the Queenstown area.
Halfway along the track, I came to a lovely bay with a Southern Rātā, a relative of the famous Christmas-blooming Pōhutukawa tree of the North Island, in crimson blooms of its own.
Here is a video I made at that spot, showing the Rātā and the peaks on the other side of the lake.
At around the same spot, I came across old lime workings. Local limestone was burned to make quicklime in kilns, which was then used to make cement and mortar for the expanding settlement of Queenstown.
Finally, I got to Bob’s Cove and to a spot named Picnic Point, a hill on the end of a peninsula that guards the cove.
The cove was a beautiful blue colour. The water was crystal clear, but shallow. It was the blue of a tropical lagoon, or of the Blue Pools of Haast and the Hokitika Gorge.
Bobs Cove is named after Bob Fortune, who commanded a lakeboat for William G. Rees, the founder of Queenstown. That’s why the maps call it ‘Fortune or Bobs Cove’. Though, I’ve never heard it called anything other than Bobs Cove, just like the nearby mountain that’s called Bobs Peak.
Captain Bob would often take shelter from local storms in the cove, which is how it got its name.
Here’s a photo of an old-time lake steamer, Mountaineer (1879–1932), in the cove. It doesn’t look like Mountaineer is sheltering from a storm. More likely, it’s tied up at a jetty, either letting tourists off or loading up with lime which was being mined from the hill.
Before Bob’s day, the cove was known as te Puna-tapu or the sacred pool in Māori, the hills as ka Puke-tapu or the sacred hills. Maybe that was because the spot really is a magical-looking one.
Maybe: because it’s likely that nobody really knows, now, what the locality was sacred for. Māori were never very numerous in the South Island. And so their folkways died out more completely in the face of European colonisation — in Māori the coming of the Pākehā, a word that’s also used in New Zealand English — than in the North Island.
For instance, twenty or so Māori placenames from around Lake Wakatipu, Puna-tapu and Puke-tapu included, come down to us through the recollection of just one individual, Henare te Maire, who passed them on to an Otago Museum researcher named Herries Beattie. If it wasn’t for Te Maire and Beattie, they would have been lost entirely. In Beattie’s words,
As sacred as the cove and its surrounding hills might have been, that didn’t keep the miners out. For the hills were made out of a mundane but vital mineral: limestone.
Local colonists preferred to build in stone wherever possible in order to keep out the winter cold, which is harsh by the standards of the rest of New Zealand. And while some little cottages and walls could be built just by piling the stones up — the ‘drystone’ technique — for proper, respectable buildings, they needed some kind of cement to stick the stones together.
The most practical solution, in the absence of any cement factories as yet, was to burn limestone to make lime mortar. Heating limestone, which is mostly calcium carbonate, drives off carbon dioxide to leave calcium oxide, a chemical traditionally known as quicklime.
The syllable quick means ‘alive’ or chemically reactive. If quicklime comes in contact with water it gets hot, indeed to the point of boiling and splattering everywhere unless the amount of water used is copious.
Mixed with sand as well as water the quicklime gives rise to an initially hot paste — lime mortar — which absorbs carbon dioxide from the air and slowly turns back into something resembling the original limestone. The only drawback is that absorbing carbon dioxide to turn back into limestone takes weeks and weeks whereas modern cement, which doesn’t need to absorb carbon dioxide to go hard, sets more quickly.
Making lime mortar is an old-fashioned, do-it-yourself approach to dealing with a lack of ‘proper’ cement. As you can imagine, the early colonists of the Queenstown area did have to do quite a lot of things themselves!
Old, slow techniques like lime mortar are having a bit of a revival these days, because they are often more carbon-neutral than their industrial equivalents. Carbon dioxide is emitted when lime is burned and also when modern cement is made, but then it gets re-absorbed if you go the old-fashioned route.
Indeed, the process at Bob’s Cove was 100% carbon-neutral because the lime-kilns, in which the lime was heated, were fired by eucalyptus trees planted for the purpose. Though I doubt that the workers thought about that issue very much at the time!
The descendants of the lime-burners’ eucalypts are still there, growing amid native New Zealand rainforest. The curiously mixed ecology makes the Bobs Cove area look as if you were in the Snowy Mountains, or Tasmania, and not in New Zealand at all.
What was once the Sacred Pool of the southern Māori has thus turned into a sort of Jindabyne, the nearby forest dominated by the eucalypts towering over the native bush, which is otherwise little more than underbrush by comparison.
There are tall trees that are native to New Zealand: kauri, rimu, totara, pūriri and kahikatea to name five of the biggest. But none of these include Lake Wakatipu in their natural range. Surprisingly enough, eucalypts brought over from the sunburnt continent thrive in such a chilly region, while the forest giants of New Zealand don’t.
There are two preserved lime kilns at Bobs Cove, fired by abundant eucalyptus back in the day, and the ruins of a few more. There were seven in operation at the peak of the local lime-burning industry.
Here’s a video tour around the kiln in the photo above.
As this signboard explains, the reason that there’s limestone at Bobs Cove is because the whole area was once at the bottom of the romantically-named Moonlight Sea.
Though, again, I’m sure the prehistoric animals that inhabited the Moonlight Sea didn’t think of it in those terms. The name was coined much later, of course. It honours another early colonist, George Moonlight, a cousin of a late-1870s Governor of Wyoming named Thomas Moonlight.
After having learned the mining trade in the Wild West and California, cousin George migrated to southern New Zealand and discovered many of the goldfields nearly Lake Wakatipu. He’s also honoured in the name of the now-defunct township of Moonlight northwest of Queenstown, and by the name of the still-popular, overland, Moonlight Track that runs thorough both localities and ends up at another pretty picnic spot quite close to Bobs Cove called Moke Lake: a Māori word meaning lonesome, properly pronounced Mokeh and not Moak.
George eventually moved to the much warmer Nelson region further north, an area normally thought of as a pleasantly sunny retirement haven and fruit-bowl. But as was his wont, he went looking for gold in the hills around Nelson and eventually froze to death up there in the winter of 1884, his eighteen-year-old daughter Tottie riding down into the town to get a search party going and then back up with the searchers, but to no avail.
Walking from the carpark around the ‘sacred pool’ to the nearest limestone peak on the peninsula called Picnic Point, you pass the lime kiln that’s shown above and then a jetty, lately rebuilt. That’s surely the one the Mountaineer was tied up at in the old photo also shown above. The jetty’s where the burnt lime, or quicklime, was loaded for Queenstown and for all those not prepared to settle for drystone walls.
The track around the cove and up the hill is mostly quite good, but it’s a bit of a hike to the top, 77 metres or 253 feet above the usual level of the lake.
And when you get to the top, you discover why this part of the promontory is called Picnic Point.
This is actually one of the most ‘Instagrammable’ spots in New Zealand.
Here’s another video:
The best results are gained on a sunny day in summer, with the sun high in the sky and not reflecting off the water. This brings out the full, rich, turquoise of the waters on either side of the peninsula.
There are fantails, or pīwakawaka, in the forest at the top of the hill. These are small, insect-eating forest birds with a fan-like tail for maneouverability, which flitter about in dim light like bats. Most are brown with a white tail and face markings, though some are black nearly all over.
Fantails often flit close to people to see if they have stirred up any insects. Or they may sit on a branch and tweet at you, just feet away. If you tweet back, it fascinates them. They may even do a little dance for you, hopping excitedly from one leg to the other.
Dogs, like the one that barks excitedly at the end of the video above, will chase the fantails and scare them away (it did). If you want to share a moment with these magical fairies of the forest that come out on a dim afternoon, or at dusk, don’t bring a dog.
The track continues downhill by way of a rapid and equally scenic descent.
A sign warns of the need to keep kids under control.
There is one spot that is rather ‘exposed’ as we say in New Zealand.
But that’s only a short bit. The rest is fine!
Note: all the colour photos and video that appear after the first mention of Bob Fortune’s full name were taken by Chris Harris on an earlier trip, in 2020.
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