Tongariro

NASA comes to Rotorua

Last week I was involved in a NASA Spaceward Bound meeting in Te Takinga Marae in Rotorua. The purpose of the meeting was to promote interest in Planetary Geology and  Astrobiology, and it was attended by about 50 scientists, educators, undergraduates and school students  from New Zealand, Australia, the USA, Romania, the UK and Kazakhstan.  Image:  NASA / JPL A large focus for NASA at present is the Curiosity Rover that has been exploring the surface of Mars for the last couple of years. One of the questions for the scientists is whether there are any traces of simple life forms in rocks on the surface. If found, these would show that whilst there may be no life at present on the red planet, it did manage to evolve there in the past under previous conditions. Image:  NASA / JPL In order to understand some of the geological features that are being observed using Curiosity’s various probes, it is useful to get to know comparable geological sites on the Earth’s surface that can be investigated and understood at close quarters. During the Spaceward Bound week we made several field trips to visit hot springs and volcanic landscapes in the Taupo Volcanic Zone. The focus of these trips was to see how microbial life can take hold in extreme physical environments such as very hot,  acidic geothermal springs, and to see how these living communities leave physical and chemical evidence of their existence (biomarkers) in the mineral formations that build up at these locations. This image shows a silica terrace at Waimangu volcanic valley. The colours are created by different species of microbes that thrive in these harsh conditions. The colour distribution shows the tolerance of particular species to different water temperatures.  For more about extremophiles in New Zealand find out about  the 1000 Springs Project. Extremophile microbes inhabit the hot mineral rich water that creates the rock formations at Pariki Stream, Rotokawa. The bacteria leave visible biomarkers in the sinter left behind as the mineral laden water evaporates. Parag Vaishampayan, a research scientist at NASA, took a close look. Quadcopter meets Rover at Rotokawa This small radio controlled rover was designed by Steve Hobbs at the University of New South Wales. It is adapted for remotely investigating hot springs, and includes a number of sensors such as spectrometers, a camera and a non contact thermometer. the quadcopter that you can also see in the picture has been adapted by Matthew Reyes, (a technologist at NASA) to scoop up water samples that can’t otherwise be easily accessed. Part of the field investigations included a study of plant colonisation of lava flows in the Mangatepopo Valley in Tongariro National Park. This photo shows a young lava flow on the slopes of Ngauruhoe volcano at the head of the valley. We also went on an excursion over the bare volcanic landscape of the Tongariro complex. Mars, as seen by Curiosity.            Image:  NASA / JPL For more information about astrobiology have a look at the New Zealand Astrobiology Initiative website, and to find out about Spaceward Bound New Zealand have a look here. Finally here is a news clip from TVNZ about Spaceward Bound, and an interview with AUT scientist Steve Pointing on National Radio.

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Tongariro North Crater

Earlier this week I decided to spend the night camping up on the North Crater of Tongariro. This is the large flat crater that is off to the north and west of the main track of the Tongariro Crossing. For access information have a look at the GeoTrip page here: www.geotrips.org.nz/trip.html?id=279Here is a view across to it from near to the Red Crater: The crater is about 1 km across, and is believed to have once been a lava lake several thousand years ago. In the distance you can see the crater rim to the right of the cone of Ngauruhoe. The surface of the ground is uniformly covered with scattered blocks of lava. This windswept area feels isolated and rarely visited, even though it is so near to the Tongariro Crossing track. There is a spectacular explosion crater within the North Crater itself, over 300 metres across and about 50 or more metres deep. It has broken through and partly obliterated the surface of the solidified lava lake. A low angle valley cutting across the main crater represents the line of a fault. Debris from the explosion crater to the left of the image has partly filled the valley. This photo taken by Lloyd Homer in 1984 shows two more faults (dark lines) crossing the slopes on the western flank of Tongariro. They are normal faults, indicating extension of the crust that is associated with the volcanism in the North Island. They have been active since the Taupo eruption 1800 years ago The Tongariro Crossing passes just below and east of North Crater. There is a barrier prohibiting closer access to the Te Maari Crater / Ketetahi area  . This is the 2 km exclusion zone due to continued volcanic eruption hazard. From the edge of North Crater, there is a view down to Ketetahi Hut and across to Upper Te Maari. It is sobering to think that the hut was damaged by large flying rocks erupted from Te Maari about 2 km away during the August eruption. If you click on the image to enlarge it you can see the hut near the left side of the photo. This was the view at sunrise, looking down on to the steam plume coming from Upper Te Maari.Crater.

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Volcano Gas Flights Video

If you had to work out the daily quantities of different gases coming out of a volcano and spreading across the sky in a huge, mostly invisible plume, where would you begin? This video gives a brief introduction to how New Zealand’s GeoNet scientists go about it: The information is combined with other evidence such as seismic monitoring to judge the risk of future volcanic eruptions.

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Flight over Tongariro and Ruapehu

My next experience of a GeoNet gas monitoring flight was over Tongariro and Ruapehu. This time Karen Britten and I were joined by Fiona Atkinson (left in photo) who is part of the GeoNet volcano monitoring team. As we approached the volcanoes from over Lake Taupo, the small gas plume from Te Maari was visible. Because the plume is quite low against the mountain side, GeoNet cannot always monitor it by plane. They sometimes use a road vehicle instead, traversing under the plume along a nearby road.Our flight took us past the Red Crater (left) and the Emerald Lakes, where I had been tramping a few days before. North Crater on the right skyline is a solidified lava lake, whilst the dark lava flow in the middle distance on the right originated out of Red Crater. We circled Ngauruhoe several times just in case there was some evidence of gas emission, although non could be determined. If you click on the photo to enlarge it you can just see some people on the left hand side of the inner crater rim. The crater lake of Ruapehu was a uniform pale blue colour, with no visible upwellings. Our gas measurements showed about 670 tonnes per day of CO2 , a little H2S (0.5 t/day) and about 28 tonnes per day of SO2. These figures are in a similar range to those from the end of January, but somewhat elevated compared to December. On the way back we decided to take a closer look at the Upper Te Maari crater area. There is still a lot of grey ash covering the area from the November 21st eruption, and yellow sulphur deposits around the fumeroles. Having landed back in Taupo, I drove down to Whakapapa Village, and was able to look at the Te Maari area from the road on the way. The area affected by ash can be seen extending across the mountain side.I decided that I just had time at the end of the day to walk up Te Heuheu peak on Ruapehu. It is on  the north edge of the summit plateau.  The crater lake is just beyond the sunlit snow in the centre of the photo, out of sight behind the ridgeIn case you haven’t seen in yet, here is a video of the Te Maari eruption made from the webcam shots on November 21st:

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Ngauruhoe’s Far Side

Climbing Ngauruhoe from the South is well off the tourist route, and involves scrambling up unstable blocks of lava for about 700 vertical metres up the face of the cone. I chose to go up more or less up the centre of the view you can see here, and it took me about an hour and a half of steady plodding to the top. The crater of Ngauruhoe was last erupting from 1973 to 1975, during which time it occasionally threw out blocks of lava to a distance of about 3 kilometres. If you click on the image to enlarge it you will see people on the crater rim that give an idea of the scale of the image. Ngauruhoe’s crater rim provides what to me is one of New Zealand’s finest landscape views. On the far left is Tongariro peak, then the flat top of North Crater and the Blue Lake (with steam from Te Maari just behind it). Just below the Blue Lake is the top of Red Crater and on the right side are old lava flows in the Oturere Valley. The Tongariro crossing track passes through South Crater as a white line in the centre of the photo. Descending the northern slope of Ngauruhoe, I then climbed a rocky ridge up to Tongariro peak, seen running from the centre to the right side of this photo: Next on my route was Red Crater, followed by a swift run down grey coloured soft scree just visible on the right of the photo. This took me into the Oturere Valley from where I turned back in the direction of my campsite. In the area to the east of Ngauruhoe I cut across country around the base of the volcano. This is a relatively rarely explored area. It took me a few more hours tramping across a variety of moraine ridges and blocky lava flows to reach my tent after a very satisfying day.

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Tama Lakes

Last weekend I went to camp and tramp in the Tama Lakes area on the saddle between Ruapehu and Ngauruhoe. These lakes were created by several explosion craters within the last ten thousand years  giving them a circular or crescent form. The landscape is covered with blocks of lava and scoria as well as some fine ash  remaining from Ruapehu’s 1995 – 1996 eruptions. There are also some layers of pumice from the huge Taupo eruption about 1800 years ago. This photo shows some charcoal fragments – remains of some of the vegetation that was scorched during the most violent eruption on earth in the last 5000 years. The lower Tama lake is being slowly filled up by a river bringing in eroded ash and other volcanic debris from the surrounding area. You can see this delta on the far side of the lake in the image. Beyond it is a similar adjacent (sediment filled) crater of about the same size. The water is very clean and drinkable, and yes – it really was that blue! I set up my tent in a little hollow, sheltered from the wind and on a nice flat spot. The view north from my campsite shows the Upper Tama lake and the south face of Ngauruhoe, my planned hike for the next day.

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