Blue Creek Canyon Nov 30


Lara was quite eager to check out Blue Creek Canyon, a narrow marble defile notable as the only dry canyon in New Zealand in typical conditions; the water disappears underground into a cave system above the start of the canyoning section and appears at Blue Creek Resurgence at the canyon's very end. I had been through it once before and a return was not at the top of my list but it was nice enough and I was willing to give a concession as I knew there would be some other new-to-me things we would get to check out over the coming days. 

We had a late start on the long drive after packing up, handling errands, grabbing food, and a lengthy attempt to rehabilitate a headlamp. It was typical endless Canterbury Plains driving, alternating drivers through the small towns up until we finally reached Lewis Pass. We stopped briefly to sniff out our way to Sylvia Flat Hot Springs, which I was surprised to find completely missing apart from the sulphur smell (I later found out they were buried in slips around 2017 or so). We ended the day quite late at the Marble Flat Campground. I found a nice spot in the beech forest that kept me nearly free of dew in the morning. What neither of us were prepared for was a loud night of noisy truck traffic and then a random ute driving fast through the campground yelling obscenities at 3am. Well I did have my earplugs so I was partially prepared I suppose. I vowed to not camp there again.

We awoke and got moving fairly early to continue driving. I voted for a stop at the roadside Maruia Falls near Murchison, a hard feature to drive past without a stop. I knew it was abruptly formed in the 1929 Murchison earthquake but I finally got a clearer explanation since it couldn't have been as a fault scarp; a It is frequently kayaked; a landslide to the east pushed the river out of its channel and forced it to the west. Every time I look at the falls I think it is right at the limit of what I would potentially consider packrafting over.


We both were caught a little off guard at just how far it is to the north side of Mt Owen (a full 2 hour drive past the southern access) as we had to drive almost to Motueka before turning to go up the Wangapeka valley to its road end. Sandflies immediately swarmed as we tried to get our gear organized and down a snack before hiking. We had a good track to start off on alongside a noisy Blue Creek. Past some mining relics the track begin to climb with a couple steep root-clinging sections and the noise of the creek disappeared. I was dripping sweat with the humid heat that was probably record breaking for this time of year. We struggled for a few minutes finding the canyon trail turnoff, ultimately stumbling around below a bluff rather than further up. The side trail was fairly easy to follow once we found its start but it dragged on a lot longer than I thought it would as we paralleled the creekbed for quite a while before dropping down to it. Eventually we arrived at the dry creekbed below a massive overhanging wall of marble with our first drop right below us. We put on our harnesses and I ended up rigging the first drop for Lara and downclimbing after to save some rope wear.



The canyon had a nice mix of dark narrows with water-carved marble surrounded by the ever present greenery of moss and ferns. There were a few nice pothole features and a particularly nice rappel into a grotto (frontispiece). We took our time, taking turns trading off rigging the rappels, working through downclimbs, and trying different descender combinations. There were a few nice dark hallway sections and a few logjams to surmount. Occasionally we would get hints of some nice reflected golden light in the canyon. Generally the drops were straightforward and minimally awkward other than the occasional slippery rock.






Towards the end of the canyon (rappel #12?) we encountered our first clear cold pool of water at the base of the rappel. I went for a descent in my boxers and managed to swing out to hit the thigh depth part of the pool, missing the part that was well past waist depth. I attempted to give Lara a guided rappel with mixed results, mostly getting her past the deep part but hitting the water in a seated position rather than on foot. Beyond this was one more thigh depth pool to cross, the final extent of the water we would see in the canyon. 



As we neared the end of the canyon we noticed some wonderful veining and deformation patterns in the marble and after the last rappel (#17 or so) we spotted some of the cave entrances shooting out cold air and then a short distance further the end of the canyon and the crystal waters of the resurgence. 


Harnesses off and some crisp spring water downed, we briefly check out the resurgence and carried on down the track back to the car. Along the way we passed a nicely restored 4-battery stamp mill. Undoubtedly more money was spent on getting it here and restoring it than it ever produced in gold. 


Lara seemed to really enjoy the canyon, removing the moving water from the usual equation. Back at the car we debated our options among camping at Courthouse Flat (a bit early but a nice quiet spot), dayhiking the following day up to Granity Pass, or retracing the last 2 hours of our drive to try to camp at the south side of Mt Owen to set us up for a multi-day hike. Between the weather forecast and the time of day we ultimately decided we would be better off getting the driving over to the Owen River behind us. On arriving at the carpark we only saw one other vehicle; a quick snooping glance into the car suggested cavers and I wondered if it was anyone I knew. We were a little nervous about camping just beyond the trailhead paddock, but as we made dinner the farmer strolled past, said hello, and was quite friendly and relaxed about it which alleviated all our fears. He seemed quite proud of his "magic" spot with mysterious alpine karst mountain beyond. I was only slightly embarrassed to be wearing a bug net for the persistent sandflies. I slept well under the beech with a decidedly much quieter camping spot!

Seaview Beach Nov 28


Presenting at the 2024 Geoscience Society of New Zealand Annual Conference offered me a delightful opportunity to catch up with friends and colleagues in Dunedin, my other side of the world home. It was a grand nostalgia tour overall with lots of long missed faces. A quiet morning in the conference schedule aligned with a low tide, giving an opportunity for a morning hike to a very rarely visited beach with Alan, one of my former PhD advisors. This Caversham Sandstone cliff-lined beach is only possible to visit by a steep grass-covered slope accessible through the active seaside Blackhead Quarry. I managed to get in touch with the quarry manager to secure us permission and the weather held out to a merciful intermittent spitting. My hope was to visit the interesting sea cave chamber at the far side of the beach past the first headland, which I mapped and last visited...in 2010! When we showed up at the quarry office it turned out the manager was quite eager to show us a few interesting outcrops and so we actually started with a quarry tour. We checked out the exposure of the Blackhead Fault which juxtaposes the Caversham Sandstone against the thick pile of basaltic lava that is being quarried. We then drove down towards the bottom of the quarry to check out a few interesting breccia outcrops and the fantastic columnar basalt that makes up the remaining headland of Blackhead. 


After the quarry tour we parted with the manager and drove up to the edge of the quarry nearest our slope to the beach. I brought my trekking poles which came in handy for both of us to descend the steep wet grass slope. We made our way slowly, soon reaching the basalt cobble beach, atypical for Dunedin. Awkwardly we clambered over the shifting cobbles towards the far end of the beach as seagulls swirled above us. 


Occasionally we came across pieces of kelp washed up on the shore that were completely coated in gastropods jockeying for a prime eating position which made an unusual sight. We dodged the occasional wave as we made our way along. When we got to the headland that splits the beach in half I was quite disappointed to see that for even this current low tide there was no way on without swimming. The headland had a sea cave tunnel through it in the past but we found this filled up to the ceiling with large cobbles we weren't going to be moving and less sand on the beach meant that it was not feasible to round the headland (which I had also done in the past). I shrugged and apologized to Alan; I wish I got to show him the cave beyond but oh well.



For our return we decided to walk across the top of the beach cobbles instead of along the foreshore slope. This also had some animal surprises as we encountered no fewer than twenty seagull nests built directly on the cobble beach, most with one to three just born chicks or eggs with beak pecks that would likely hatch by the end of the day. It was quite surprising to see them out in the open and apparently was a predator free beach.



We went back up the slope, out the quarry and drove on to the conference in time for morning tea and the rest of the day's events. I was thrilled to get to spend the time with Alan. The day ended quite nicely with a run through Ross Creek and reservoir with Genevieve and my old officemate Tammo, and then a nice catch up with my friend Lara over dinner as we worked to plan our next week of travel. The weather forecast made a very clear case for us to head north and not south! Many thanks to all those mentioned.