Hollyford Valley Nov 23-27


It was some of the most logistically intense, high risk, strangest, and surprisingly most enjoyable fieldwork I have done to date. Back in the late 1970s a triangulation network of 6 stations was set up across the Alpine Fault at Lake McKerrow in the Lower Hollyford Valley. Each station consisted a stainless steel survey pin and galvanized angle iron set into a large slug of concrete. By measuring the position of each point relative to each other using angles and distances, and then later resurveying the network, the surveyors would be able to determine whether the fault was locked and building for the next earthquake, or exhibited a component of fault creep. The last of these surveys ended in 1984, possibly not enough time to measure a component of creep above the uncertainty. The discovery of saponite-rich gouge with identical physical properties as the creeping portion of the San Andreas Fault at the nearby Hokuri Creek prompted a heightened interest in trying to conclusively prove whether is or is not, actively creeping. The chance to collect over 30 years of fault data is a rare opportunity which could yield some important results. And so started the great Fiordland high-risk scavenger hunt....

        The first (and easiest) monument we found

All I had to do was find these six 30cm x 30cm monuments, occupy them with a high precision GPS (mm accuracy) for 18hrs each and then later compare the data to the original surveys. Problem is I had hand drawn sketches pointing me to the station locations with descriptions like "~15 m from the shore and 10 m from a prominent tree"...Fiordland is not known for being one of the more static places in New Zealand, let alone the world, so it would certainly take some persistence and luck. Nevertheless I was confident I could narrow the area down to less than 50m in most cases and hoped a metal detector could aid us from there. In order for success we needed to find five or six of the monuments. The monuments were also on both sides of a 2km wide lake, which would have discouraged most. I was confident that in most wind swell conditions Jeff and I could comfortably use our Alpackas to traverse back and forth as needed (but I was also aware of the abrupt and dramatic changes this lake could undergo). We also would have to design our campaign to make the most of the limited time and 2 GPS units. This meant initially occupying the easiest to find stations, then searching for the harder to find ones while data was being recorded.


We were able to get a helicopter backflight into Hokuri Hut where we had a frantic hovering landing due to the lack of beach from the high lake level. We quickly unloaded at the hut and set off to make the most of the remainder of the day. We inflated our packrafts on the beach and carefully loaded the heavy GPS equipment (5lb GPS unit, cables, antennae, spike mount tripod, level, etc.) into our slightly precarious boats. We quickly and easily found monument Z and carefully leveled the GPS above it. We then paddled the long 3km crossing over to the other side of the lake. Despite the wind chop we made it ok and promptly found and occupied monument C. Those first two monuments were of course the easy ones. We still had several hours of daylight so we set off along the coast to look for B. We landed at the logical location indicated by our sketch and set off narrowing the location down. Before long we identified the likely beach ridge and I tried to find it visually while Jeff used the metal detector. He got a strong hit in one location and I found an old plastic mug to dig with. Amazingly, buried 0.5m beneath modern beach gravel, we found monument B! Carrying on we had a quick look for A before crossing the lake back to the hut just before dark. It was clear A was going to be the tricky one- the "lone beech tree" and "rock pile" indicated as key landmarks were nowhere to be seen 30 years later! We did meet a couple friendly builders working on a private hut who would later be of great help.
        Metal detector says dig here

        Monument B, buried beneath 0.5 m of modern beach gravels!

Day 2. Greyer with intermittent rain. Found monument Y buried immediately beneath the path to Hokuri Hut! Found battery on Z to have been dead! I had a terrifying solo paddle across the lake with a large swell and gusts of wind that would blow me backwards. Fortunately they relented, I made it across, and wind conditions generally did not get too much worse. Occupied B, then looked for A again- still no luck! We found X relatively easily, then decided to run up to the fault core outcrop in Hokuri Creek for samples and real geology.


        Alpine Fault fault core at Hokuri Creek

        Endlessly fascinating saponite gouge textures

Day 3. With a great deal of luck (first rock I overturned!) I found A, the last of our 6 lost monuments. We occupied A (thanks to the digger battery the builders lent us!), then setup X with the other GPS. The rain began at 11am and continued through the day. With spare time while we were waiting on the GPS, and too much rain for productive fieldwork, we decided to try packrafting down Hokuri Creek. The approach was surprisingly easy along the true left bank, which also gave us a view of all the major obstacles including several significant drops and holes. This was going to be an interesting run!
We didn't have wetsuits, only rain gear, so I was pretty motivated to avoid a full drenching and stay upright. We hiked up to just above the main confluence, the logical place to put-in. The run was surprisingly fast and fun with some excellent features and little flat water! There were three particular obstacles of note: (1) a series of rapidfire drops in a long and sustained stretch of river, (2) a steep and messy chute-like rapid near the Alpine Fault outcrops, and (3) a sustained wave-train immediately under the three-wire bridge. We both had a clean and enjoyable ride straight through (Class II-III+) and slid right into the lake, where we paddled back to Hokuri Hut.


        Gearing up for the first descent of Hokuri Creek (Class II to IV-)

 Day 4. More rain today. We removed the GPS from A and had a cup of tea with the builders before moving on. We arrived at X a little early so took a walk along the beach to the old Jamestown site, where an ill-conceived idea to put in a settlement was master planned by folks in England with little founding in reality. We moved the GPS down to reoccupy Z (this time with a functional battery) and then retreated to Hokuri Hut. It was raining very hard by the afternoon! We had some visitors to Hokuri Hut. I was pretty content to stay dry and read my book but Jeff had other ideas. Eventually he succeeded in convincing me to have another run down Hokuri Creek (this time it would be at much higher flow). What a fast run this time! It was probably Class III- to IV- at this flow. The drops on the upper portion of the run were all probably a bit more straightforward this time and the wave trains were much more fun at this flow. Once we got to the bend in the river near the Alpine Fault things got crazy. Here we wanted to stay hard right but I was slow with my positioning and ended up too far left to make the main channel. Jeff stayed right and had a wild ride down some messy holes which eventually flipped him. Over to the left in no man's land I was having a bit of a panic- the river on this side dropped over large boulders and past grabby logs in flow about twice the width of my packraft. I pretty much could only anticipate clearing one obstacle at a time- reaction, reaction, repeat, action, reaction, repeat. To my great surprise I managed to clear the rapid unscathed (looking back at it I have no idea how). I was feeling a little shaken up but glad to still be upright and intact as I waited for Jeff. I was soon to get my turn though. The wire bridge rapids were looking considerably beefier. I chose a line right of center clipped the edge of a hole and flipped instantly. I executed a pretty effective self-rescue considering it was my first kayak flip ever, managing to herd my packraft, paddle, and hat through several more wave trains until I got to shallows and could right myself. Thoroughly drenched in water and adrenaline, I was remarkably warm. We floated the last cruisy stretch to the lake, and onward for a peaceful paddle back to the hut just before dark. The trampers (some of which went to extraordinary lengths to keep their feet dry) thought us rather peculiar showing up to the hut like wet dogs.


        A calm crossing for a change

        Walking towards Jamestown

        Hokuri Creek ?first descent?


        The aftermath

The last day we picked up the last GPS from station Z (this time still recording) and packed up. The whirlibird dropped out of the sky more-or-less on time and off we went. Amazingly we managed to find all six needles in the haystack that is the thick bush of Fiordland. Now its only qa matter of processing the data to see what the results are. Preliminary results suggested the GPS had poor signal due to the thick bush overhead, but more careful attempts are forthcoming. I would love to have a convincing answer one way or the other.

Photos of me by Jeff. Thanks to him! Thanks also due to the fine people at Hollyford Track Ltd. who have always been friendly towards research in the valley.

Caversham Caves Nov 2014


Thanks to a National Geographic-Waitt grant I was able to return to the ever fascinating Caversham sea caves to do some more survey and science work. I had an exhaustive list of goals, and while a great deal was accomplished, we were also very limited by the unseasonably poor swell conditions brought on by this year's atypical weather. There was not a single day appropriate to visit the rugged South Coast and the conditions were never appropriate for SCUBA diving. Surveying was a struggle and we often

We did managed to map 4 of the 10 longest sea caves in the world, surveying over 2 km of passage which is a monumental accomplishment given the survey conditions. I also collected shell samples for amino acid racemization dating and sand for OSL dating to provide age constraint on the +4m marine terraces, and thus the rate of cave formation, speleogenesis, and tectonic stability of the coast. I also employed the high-precision GPS I brought to determine the exact elevation of the +4m terraces. We surveyed and explored the first definitive karst formed cave in the Caversham Sandstone. We took extensive photos of the Cave of a Hundred Names to enable a 3D structure from motion (SfM) model to be created of the entire cave. We also made attempts to document the sea life present (including some rather interesting sponges and bryozoa) and took some good photos of the more interesting features of the caves. Ongoing work includes a kayak-mounted shallow bathymetry survey, cutting and polishing a large stalagmite (half for the Waikouaiti Museum and half for paleoclimate study), sending off samples for analysis, and drafting the cave surveys into proper maps.

        Exiting at high tide

        Crux climb back up the cliff from Skull Head Cave

        In the Perfect Squeeze passage




        A very narrow passage that will likely never be revisited...

        The ever interesting Peephole Cave



        Precisely measuring the elevation of abandoned marine terraces


Easily one of the main highlights of the sea cave work was the last day of surveying in Skull Head Cave. Jeff and I just had a little bit of tie-up survey to do. The last passage left to survey, well into the cave, took off towards the sea from a four-way junction. It was a modest passage about a kayak in width, with surging flow and slight ledges on the side (one of those extreme low tide only passages). Usually these passages go 5-10m in and then end abruptly. Not this one! Jeff led the survey. Many tens of meters onward we reached a narrow bedrock passage (another sign of a typical passage end). Here however we had a faint glow of light in the distance and a slight draft. It headed out to an entrance! I was a bit perplexed where we were headed but we surveyed on, passing through increasingly nice (and very long) passage. Our 10 m of survey turned into hundreds of meters, cleanly pushing the length of Skull Head past the magic one kilometer mark (the second cave in the world to do this, its neighbor Matainaka being the first). To my surprise we ended up connecting into the Hall of Whispers Cave which features one of the nicest chambers on this coast. Rocks block the entrance at low tide so I had only been in this passage during higher tides when the key connecting passage would have been flooded. I was ecstatic that there was still more to discover on the Caversham caves.


World's Longest Sea Caves   (as of November 2014)

1  Matainaka Cave                 Otago            New Zealand    1540m
2  Skull Head Cave                 Otago            New Zealand    1120m *
3  Erangi Point Cave                Waitakere       New Zealand       850m (est.)
4  Noisy Cave                          Otago             New Zealand      563m *
5  Kotau Point Cave                 Waitakere       New Zealand        485m (est.)
6  Mercer Bay Cave                 Waitakere       New Zealand        470m
7  Gemma's Cave                    Otago            New Zealand       421m *
8  Lamb of the Lost Cave       Otago            New Zealand       407m *
9  Pink Cathedral Cave          Otago            New Zealand       404m
10 Sea Lion Cave                     Oregon           United States        401m
* surveyed November 2014          BOLD- Caversham cave (Barth et al. survey)



A lot more scientific work is on its way for the Caversham caves in the coming months. Photos of me by Jeff. Big thanks to Jeff Creamer for field assistance and National Geographic for funding.

Nichol Creek Nov 16

Wanting to take a break from the cold sea caves for a day, I decided to have a lazier day showing my visitors a local canyon (and their first canyon). Although far from being a high quality canyon as far as the rest of New Zealand is concerned, it's a good couple hour jaunt which packs a good variety of beautiful terrain and up to five rappels. Even better, the trailhead was less than 5 minutes drive from the place I was renting in Dunedin!

I think it took us longer to find the drop in than it did on my first descent years ago because we ended up trying to drop in too early. Eventually we figured it out and strolled down the creek to the first waterfall. Though not the tallest, this waterfall is probably the most scenic, dropping into a nice water sculpted flute. Between having two harnesses for four of us and the pull being rather difficult, we had plenty of time to enjoy this beautiful, if cold, spot.


We soon arrived at the Cup & Saucers, an odd in-faulted sliver of Caversham Sandstone exposed amongst the Dunedin Volcanics. The hard volcanic boulders effectively sculpt the sandstone into a chain of perfect little potholes. Unfortunately this stretch is over almost as soon as it starts and it is back to volcanics. A few other short drops and downclimbs lead to the top of Nichol Falls (frontispiece), which trampers hike up to from below.




After a good soaking in Nichol Falls, we carried on down the creek which still offers a pretty spectacular narrows with wall-clinging ferns before we finally get kicked out at a weir. Despite being my second descent, I still enjoyed it quite a bit. The new canyoners seemed to have a good time as well.