Aoraki Mount Cook

Beneath New Zealand 1 Documentary

Making Movies is an Auckland based film company that creates adventure and nature documentaries. I was asked to help with the script editing and presentation on a movie about the mountains of New Zealand. This involved spending time with the film team in the Southern Alps, amongst some of the most spectacular landscapes in New Zealand. We spent several days in the Aoraki Mount Cook massif. In this photo we are arriving on the Grand Plateau. The environment required full mountaineering security due to the massive drop offs and crevasse hazard The light changed constantly to pick out the landscape features in a way that I found continually fascinating to watch. We also spent some time on the Tasman Glacier and in some of the surrounding peaks: Team photo on the Tasman Saddle, with Aoraki Mount Cook in the distance Click here to see the trailer of the doco Beneath New Zealand on the Making Movies website https://www.makingmovies.co.nz/portfolio/beneath-new-zealand/

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Mount Cook Rockfall

Hooker Valley rockfall. – Simon Cox / GNS Science On the evening of Monday 14th July there was a large rockfall from the western slopes of Mount Cook into the Hooker Valley.   Staff from the Department of Conservation and GNS Scientist Simon Cox flew over the area  to make assessments of the  impact. The first photo shows the view towards Mount Cook with the dark shadow of the rockfall splaying out onto the Hooker Glacier on the left. Photo J Spencer / DoC Approaching the area, the scale of the rockfall starts to become apparent. As well as the debris fan there is a wide expanse of dust that settled on the opposite wall of the valley. Photo Simon Cox / GNS Science The devastated area of mountainside that was swept by the avalanche is well over a kilometre across. Photo Simon Cox / GNS Science Because of a prominent ridge in the path of the rockfall, the debris divided into two separate lobes as it poured down the mountain. This photo shows the smaller, upper branch and the white ridge (known as Pudding Rock) that obstructed the torrent of rock and ice debris. In the foreground is the dust covered icefall. Photo Simon Cox / GNS Science This is a view of the area from higher up, looking down the valley. Simon estimated that roughly 900 000 cubic metres of rock debris are scattered on the valley floor, having travelled  up to 3.9 kilometres and fallen a vertical distance of 1600 metres. On its journey down the mountain, the avalanche scooped up possibly three times as much snow and ice which mixed with the rock material. Photo Simon Cox / GNS Science A view upwards towards the low peak of Mount Cook, showing the source area and path of the rock avalanche Photo: DoC / J Spencer  Amazingly, the Gardiner Hut just avoided obliteration due to its favourable location on the tip of Pudding Rock. However it was badly damaged.   Photo: DoC / J Spencer The toilet block was crushed and the hut pushed off its foundations. Luckily no-one was inside. Photo DoC / D Dittmer Clinging to the mountain amongst a sea of debris. The Gardiner Hut was in the best possible position to (almost) avoid destruction in this rockfall event. Photo DoC / D Dittmer Finally here is a view of the headscarp with the 300 metre high x 100 – 150 metre wide grey rockfall scar on the cliff face, the source of all the devastation. You can visit the end of the Hooker Glacier, one of the spectacular day walks at Mount Cook: Here is the GeoTrips link: www.geotrips.org.nz/trip.html?id=685

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The growth of Tasman Glacier Lake

The Tasman Glacier is the largest glacier in New Zealand. Its upper section is mostly white as you would expect of a river of ice. However, the lower half is covered with a layer of rock debris about a metre thick. This forms an insulating layer that slows down surface melting and allows the glacier to descend a long way down the valley to warmer elevations. This photo, taken from the location of the the top of the moraine wall near the old Ball Shelter in 2007, shows what the debris covered surface of the lower Tasman Glacier looks like.The moraine walls show how much the glacier surface has lowered in the last century. Before about 1912 the glacier surface was higher than the lateral moraine. New Zealand’s other large valley glaciers have all been suffering a similar loss of ice. Tasman Moraine Wall.      Julian Thomson GNS Science This is what the moraine wall of the Tasman Glacier looks like close up. The unstable terrain is very hard to travel over, especially when you are carrying heavy gear like this group of glaciologists. For more information about fascinating processes of glaciation check out this GNS Science web page. On our flight up to the Grand Plateau for the height survey of Mount Cook recently, it was interesting to see the state of the terminal lake of the Tasman Glacier. This has been expanding rapidly in recent years.  Once the lake became well established, the water could undermine and erode the ice much more quickly. This photo illustrates the process of melting of the ice. The surface water cuts away into the ice face to create a notch at water level. Once this notch is several metres deep, the overhanging ice collapses, leaving buoyant ice underwater that eventually breaks off in big pieces to float up to the surface as a new iceberg. The icebergs will continue to be eroded by the water in the same way. As they get lighter, they rise up in the water, lifting the ice notch up to give a mushroom like profile. The bergs often get top heavy by this process and can unexpectedly roll over. This video that we made several years ago gives a dramatic illustration of this process seen from a boat at close quarters: Here is some information on our GeoTrips website if you want to visit the lower reaches of the Glacier for a closer look: www.geotrips.org.nz/trip.html?id=147 I have flown up the Tasman Glacier several times on various glacier field expeditions in recent years. This is a photo of the lower section in 2002, looking down valley. The glacier itself is about 2 kilometres wide and the lake is already extending up the east side of the glacier by about 5 kilometres. Two years later (November 2004) you can see that the lake has continued to expand. The large ponds that can be seen near to the lake have grown and started to join together as more and more of the ice melts. November 2007, after a large break out of ice bergs, the lake has greatly increased in size. November 2013 from our recent flight up to the Grand Plateau on Mount Cook. It is inevitable that the lake will continue to expand. Due to the overdeepening effect of the glacier on its bed, the deepest point of the lake will be some distance up from the terminus, probably below the  area in the foreground of the image. After expanding past the deepest point, the lake will get shallower and shallower as it progresses up the valley, potentially to the point where the bed of the glacier meets the lake surface. It has a long way still to go. This image (added as an update in early March 2015) shows that the basic shape of the lake hasn’t changed substantially since the previous photo was taken over a year ago. However, if you look at the position of scree slopes on the right of the photo you can see that the glacier’s retreat is continuing. In this last photo you can see that as the lake erodes further up the glacier, the terminal ice cliff at the edge of the lake is getting higher due to the increasing surface elevation of the ice. There is a very good view of the lateral moraine wall in the background, that used to be below the level of the glacier surface back in the nineteenth century.  The glacier ice in this area has thinned vertically by roughly 200 metres since that time.

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The Changing Height of Mount Cook

Mount Cook  rock avalanche 1991. Lloyd Homer, GNS Science On 14th  December 1991 a massive rock avalanche occurred from the East Face of Aoraki /Mount Cook, sending an estimated 14 million cubic metres of rock in a 1.5 kilometre wide cascade across the grand plateau and down onto the Tasman Glacier. It is thought that the avalanche travelled at speeds of 400 to 600 km per hour, and the resulting seismic recording at Twizel, 75 km away, lasted well over a minute, registering the equivalent of a magnitude 3.9 earthquake. Mt Cook Dec. 1991.  M. McSaveney, GNS Science Prior to the avalanche the surveyed height of New Zealand’s highest peak was 3764m. The Department of Survey and Land Information (now LINZ) calculated that this was reduced by 10 metres after the summit fell off with the rock fall. As you can see from the photo, the peak became extremely narrow and unstable. In the image taken by GNS geomorphologist Mauri McSaveney a few days after the event. A lone climber that can be seen as a tiny dot inside the red circle  gives some idea of the scale. The “new” summit was obviously highly unstable, and would be subject to quite rapid erosion following the rockfall. Since 1991, there has been no re-calculation of the revised elevation of 3754m until recently. At the end of November 2013, I flew up to Plateau Hut with a climbing team who planned to take direct GPS measurements of the summit ridge of the mountain, a short distance from and a few metres below the highest point. The measurement would then be used to validate a computer model made from recent aerial photos to give a precise calculation of the present height of the peak itself. The team was made up of (left to right): Geoff Wayatt, mountain guide; Nicolas Cullen from Otago University; Brian Weedon, mountain guide; Pascal Sirguey (project leader) from the National School of Surveying at the University of Otago; Jim Anderson from Survey Waitaki and myself. Geoff, Brian, Nicolas and Jim made up the climbing team. GNS Science provided support in terms of the helicopter flights.  I was able to accompany the team to Plateau Hut where I spent two days gathering a visual record whilst they were involved in their climb. Mount Cook East Face   Julian Thomson, GNS Science The plateau of Mount Cook is arguably the most spectacular alpine setting in New Zealand. This image shows the 1500m high East Face of Mount Cook in the early morning light seen from Plateau Hut. The normal route up the mountain follows the Linda Glacier, starting on the right hand side of the image and following into the shadow behind the long low angled rock ridge (Bowie Ridge) up to the summit rocks. As well as Mount Cook itself, the Grand Plateau has views of many other summits along the main divide, including Silberhorn, Tasman and Dixon. This image shows the top section of Syme Ridge on Mount Tasman. There are three climbers just visible on the ridge just above the centre of the photo, about 10 hours into their climb from the hut. This image shows the patterns of crevasses on the grand plateau, just above the Hochstetter Icefall. Plateau Hut at night.  Julian Thomson, GNS Science The climbing party left Plateau Hut just after midnight with clear, cold weather conditions that were perfect for the climb. Mt Cook Summit Rocks, Photo Geoff Wayatt Aoraki / Mount Cook is a challenging peak to climb, with very dynamic glaciers and steep rock and ice faces to negotiate. In this photo, the climbers are in the ice gullies that run through the summit rocks. Photo Nicolas Cullen View from the summit, with Mount Tasman in the background Photo Nicolas Cullen Looking along the summit ridge of Aoraki / Mount Cook, with the two GPS units in place. The very highest point is about 45 metres distant. The GPS units measured a height of 3719 metres at their position. This measurement was consistent with the height from the computer model which then allowed the height of the high peak to be calculated as 3724 metres above mean sea level. This means that Aoraki / Mount Cook is a full 30 metres lower than the 1991 estimate of its height, showing that the mountain peak has continued to erode significantly during the last 22 years. There is more information about the project at the Otago University School of Surveying website. Here is our video of the expedition : Mountaineers staying at Plateau Hut can get an incredible 360 view of the surroundings from nearby glacier dome. We have even created a GeoTrip for the location:  www.geotrips.org.nz/trip.html?id=450

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Our Changing World radio broadcast

For those of you interested in the follow up of our ice core drilling expedition, here is the National Radio broadcast of the story as told on “Our Changing World” on Thursday 20th August. The broadcast is about 13 minutes long. http://podcast.radionz.co.nz/ocw/ocw-20090820-2120-Southern_Alps_Ice_Cores_Drilling-048.mp3

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Baker Glacier

Out of our original top 3 favourite glaciers to check for ice cores there was still one left to go. This was the Baker Glacier, visible clearly from our previous site on Mount Hutton, almost directly across on the other side of the Murchison Glacier Valley. Baker Glacier is relatively low altitude at 2360 metres. None the less, because it is also east of the Main Divide, it will have relatively low accumulation rates and, with a depth of about 70m, potential for a longer core than we got on Mount Hutton. However the radar images showed a very strong reflector at about 30 – 40 metres, possibly due to the presence of water or rock debris about half way down, a potential indicator of trouble ahead. By now we had our gear preparation down to a tee, and were set for another blitz approach to get in and out before impending bad weather trapped us in. We flew in to the upper part of the Baker Glacier, directly opposite the imposing cliffs of the East Face of Malte Brun. Almost immediately an ice avalanche rumbled down the face, I guess as some sort of greeting to us.Within a couple of hours the drill was set to go and the tents were in place. After getting past the initial surface snow, we were soon pulling up nice quality ice cores, full of air bubbles trapped within a matrix of ice. As usual, Uwe helped Xinsheng at the drill control box and I worked with Dan bagging, labelling and packing the cores. Evening fell whilst we continued working, expecting to go on until the early hours, all being well with the ice. However at about 8.30pm, with 30 metres of core recovered, we suddenly started getting wet ice again. The strong reflector layer in the radar images was explained. One further drill section confirmed that the ice was getting wetter and Xinsheng again called a halt to the drilling. We were to get some sleep after all. In the photo, Dan is holding the final section of ice core that we drilled. We decided to pack up as much as possible in order to make a swift departure in the morning. Once the net load was more or less organised, we got out the dice and played a game of Zilch, sitting on ice core boxes with our head torched on. During the night occasional avalanches roared down the cliffs in the dark. A beautiful sunrise lit up the scene as we got ready for our final helicopter ride down to the valley floor.

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Top of the World

 Just for the hell of it, I bivouacked out for the night, with the intention of watching shooting stars. Despite the cold (about -12 deg C) I was reasonably comfortable in my warm sleeping bag. I quickly fell asleep and overslept – waking at 9am. We spent the morning packing up the drill gear and piling it all in the net ready for the heli to carry it away. The chopper had a hard time lifting the weight, as there was a down draft of wind coming over the ridge above. Slowly it pulled away and left us in silence again. We got the rest of our gear back to the safe landing site, admired the spectacular views of Mount Cook and the other major peaks, and enjoyed our last moments ‘on top of the world’. The helicopter could be heard approaching from a long way off. Once all aboard, we had the delicious sensation of dropping off the precipice as we left our peak for the last time. For once I decided to leave my camera in its case and just to watch the beautiful cliffs and glaciers passing underneath as we headed back to our base in Aoraki / Mount Cook Village.

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Bedrock

After yet another day of sorting out and preparing our gear, the weather forecast looked quite promising for a few days. We decided to fly back up to Mount Hutton and drill non stop until we either came to bedrock of had to stop for other reasons, such as water in the ice. The four of us -Xinsheng, Dan, Uwe and myself, again flew up to the peak. It is a spectacular location with steep drop offs falling hundreds of metres down on all sides. Once up there you are committed! A sky of whispy clouds stretched above Mount Cook . Our heli put us safely on the landing spot, with our emergency survival gear (tents, food and extra warm clothing). This is standard procedure just in case something prevents the second load from being delivered – a sudden change in the weather or problems with the heli. Whilst the other three went up to the drill site (the same place that we had drilled our 10 metres core already), I walked across to a beautiful horizontal scoop in the snow that we had chosen for a campsite. Although the weather was sunny and calm, I made sure that the tents were well attached to the ground with snow stakes and shovel loads of snow on their snow flaps. We wanted to be able to go to bed very late without worrying about a change in the weather. By about lunchtime I could hear the humming of the generator at the site about 200 metres away telling me that the drilling had started. Once finished with the campsite I walked up to the others, feeling the effort more than usual due to the altitude. The drill site was now top notch. We had an upgraded snow wall to keep the wind off us, the drill pit was enlarged and the hot plate was on, melting snow for hot drinks and food. Uwe had decided to start a new core right next to the previous one to see if we could get a better quality first 10 metres that was less broken into sections than the first had been. Progress was very good, with no technical problems. The ice was mostly very bubbly glacier ice, immediately below this year’s winter snow. At the top there was a distinct layer of small pebbles and grit, but below that we saw little evidence of summer dirt layers. Sometimes there were clear areas in the ice, suggesting melting and re-freezing, but we found it difficult to interpret the age of the ice or what its features were telling us. Is it a remnant of old ice or all quite recent? Only the later analysis will tell. Uwe was measuring the ice temperature in the cores, which stayed consistently below freezing at about – 3 deg C. This was very promising! We had never drilled ice below 0 deg before. At last we had found some accessible cold ice in the Southern Alps! Once the routine of drilling and bagging the cores was established, there was time to look around, take pictures and chat. As the drill gets deeper, it takes longer and longer to winch up the core each time.  I took advantage of the opportunity to take an ice axe and climb the short distance up to the summit for a view from the top.Taking care not to slip I peered down the East face – a very long way down! After a few minutes I carefully cut steps back down off the summit to rejoin the others. The photo shows my tracks from near the top and you can see the drill site and our tents in the distance Just around 9pm we started to find bits of gravel in the ice cores at about 33 metres depth. Then suddenly Xinsheng said “Is finished!” – We could hear the drill clunking against rock down below in the hole. The first ever New Zealand ice core drilled to bedrock had just been drilled, a humble 35 metres from the surface.

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Mount Hutton

Today we flew up to our highest planned drill site on Mount Hutton. Yulan stayed behind, and with us instead were Tom McRae and Ron Madden from TV1. Because of the prospect of poor weather forecasted for tomorrow, we had decided to do a rapid reconnaissance drill only. If the results proved to be good we would come back with a better weather window to drill deeper. Mount Hutton is relatively remote – on the eastern side of the Park in the Liebig Range. We hoped that with the higher elevation and the location some distance away from the main divide, we would get a better preserved and longer climate record. Our radar survey showed a depth of only 50 metres of ice, but perhaps 50 metres of thinner layers would be as good as 100 metres of thicker ice further to the West (such as on Annette Plateau). The flight up was spectacular the icy clouds producing a nice sundog spectrum . Mount Hutton has a small glacier on top. It has a ridge running straight up the middle, and our drill site was about 3/4 of the way up the ridge from our landing site at the bottom. I went a head with Uwe to find our spot and start digging in. The winter snow was only 1.5 metres deep here (as opposed to 4 metres on Annette Plateau)Tom and Ron were interested in what we were attempting, asked lots of questions and interviewed us for their news programme. When they left at about 1pm, Dan went down with them, leaving Uwe, Xinsheng and myself. By 4pm we finished drilling having got down to 10 metres, with very nice, bubbly glacier ice immediately below the top surface snow. The heli arrived and flew away with the net load of gear, then returned half an hour later to pick us up. The evening light was beautiful across the big peaks of the Southern Alps.

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Down from Annette

Dan and I got up early and each went of for a walk around the glacier. I climbed up Mount Annette and then returned through the wind scoop. The plane arrived and by the time it was fully packed there was no room to fit both of us in! I decided I would be happy to walk down to the village. I set out with a pair of bamboo poles and snow shoes. The way down involved crossing some steep slopes, with wonderful views across the Mueller glacier and I was happy when I reached the valley floor where Uwe had come to pick me up. The photo shows the tracks I followed across the mountainside.

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