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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Deep Cove in Fiordland

Last week I went to Fiordland to meet up with some of the Trustees of the Deep Cove Education Trust. The drive across from Dunedin lead towards some interesting cloud formations, presaging bad weather ahead. Accessed via a 50 minute ferry trip across Lake Manapouri, and then about 20kms of unsealed road, Deep Cove is in the heart of the dramatic forested mountains of Fiordland.  The Deep Cove Education Trust runs an extremely popular outdoor centre catering for school groups throughout the year. Bruce Smart (left) is a long term member of the Trust. Along with Malcolm Walker, he has a passion for introducing Fiordland’s wilderness to young people. Fiordland is made up largely of rocks that have been formed deep in the earth’s crust and then uplifted by plate collision. Millions of years of erosion have removed the overlying rock, to leave a dramatic topography of ice and water sculpted peaks, valleys and fiords. The landslide visible on this photo occurred as a result of the magnitude 7.8 earthquake in 2009. During our stay, the rain teemed down –  I liked the comment from the bus driver who said – “if you have ever wondered what the inside of a cloud looks like – just look out the window…” When the cloud cleared, we got a good view of many spectacular waterfalls thundering down the mountain slopes. Water, water, everywhere. During our short stay, there wasn’t much chance for doing a lot of geological investigation. Still, GNS Science researcher Rose Turnbull, managed to have a look for interesting samples in some rock debris not far from the Hostel. You can read about the Deep Cove Educational Facility on their website here.  Bruce also has a blog at deepcovehostel.blogspot.co.nz.

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A dynamic landscape in Hawkes Bay

Last week I was in Hawkes Bay with geologist Kyle Bland, who led a field trip for teachers, students and parents of Crownthorpe School. Hawkes Bay geology is a story of uplift along fault lines, combined with rapid erosion and deposition by rivers flowing from the inland mountain ranges. This story is etched into the geomorphology of the landscape. The Mohaka fault last ruptured between AD 1600 and 1850, and forms an amazingly straight scar across the landscape. Like many faults in New Zealand, it is an oblique strike slip fault, including both sideways and vertical movement.  If you click on the image to enlarge it you can see how streams crossing the fault have been offset by sideways movement from the last rupture. Combined sedimentation, uplift and erosion have produced stepped terraces alongside the Ngaruroro river flowing from the Ruahine range out towards the coast. There are many fossils to be found in the sedimentary rocks that have been uplifted and exposed. Fossil hunting Hawkes Bay style involves using a digger to get access to your specimens! Ancient greywacke sediments are exposed in the Ruahine Range, having been uplifted by tectonic movements of the North Island fault system (Mohaka and Ruahine faults). These rocks were deposited in a trough at the edge of Gondwanaland, long before New Zealand ever existed. In the video below, Kyle gives us a Hawkes Bay case study of landscape evolution.

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Fossil Whale

Last week I visited Palliser Bay in the Wairarapa. Along the coastline there are many exposures of mudstone from the Hurupi Formation, about 11 to 8 million years old. These mudstones contain abundant marine shell fossils, but are also known for occasional whale bones.  After some time searching, as luck would have it, I found a large piece of bone sticking out of the mud near the base of one of the cliffs. The bone was embedded in soft sediment and was easy to remove with a bit of digging. Nearby I found two other large pieces. Back at GNS, Craig Jones identified them as fragments of mandible (jawbone) from a large baleen whale species. Two of the pieces matched together to give a combined length of 75 cms. Initially we thought that these are part of the left mandible, whilst the other single piece is part of the right mandible.    John Simes is the manager of the fossil collection at GNS Science. He  helped me to give them an initial clean to remove some of the mud that coated the bones. Here you can see the typical mottled texture and brown colour of fossil bone. This is the largest  piece, half a metre long and about 25 cms across. There is an epifauna of bivalve and barnacle fossils attached to the bones. This tells us that they would have been lying in calm, relatively shallow water before they were buried by sediment. There are also several wood fragments in the surrounding clay, which suggests that the whale died not far from land. After many hours of cleaning, some interesting grooves appeared in the bones. These show where blood vessels were embedded alongside the bone. For an update on additional whale bone discoveries from this locality check out this blog post.

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NZ ShakeOut – why all New Zealanders should participate

GNS Science is very proud to support the NZ ShakeOut earthquake drill on September 26th. Watch the video if you don’t already realise why being aware and prepared for an earthquake is a good idea. The event, which will run right across the country at 9.26am, will prompt all of us to check our plans and  preparations against the possibility of a damaging earthquake. New Zealand ShakeOut has been created to help people and organisations get better prepared for major earthquakes, and practice how to be protected when they happen. Everyone will practice “Drop, Cover and Hold”—the right action to take in an earthquake. If you haven’t already registered, help the ShakeOut reach over 1 000 000 participants by clicking here

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Artificial Earthquakes on an Active Volcano

GNS Science volcanologists recently set up an experiment to test the seismic velocity of the rocks that make up White Island. Over the last few decades it has been New Zealand’s most active volcano and has produced minor eruptions in recent weeks. (For its present activity status click here.) Velocities of seismic waves through the Earth can vary considerably because of variations in the density and layout of different rock types. It is important for scientists to know these subsurface seismic velocities as they are used to calculate the locations of earthquakes under the volcano. These might indicate rising magma and therefore an impending eruption. It is for this reason that volcanic earthquakes are carefully monitored. For an explanation of how earthquakes can be located see this video, and for a look at White Island’s activity status, including the seismic drum, click here. There are various ways to generate seismic waves in order to measure velocities, such as by using explosives or air guns. These traditional methods can have environmental, safety or cost drawbacks. So in this case, a GNS Science team, led by volcano seismologist Art Jolly, used a novel method: First of all, The team set up 17 temporary seismometers around White Island, with six of those set up in a line across the volcano crater floor to record the shock waves, their travel times (hence velocity) and their intensities. Three large sacks were then filled up with about 700 kgs each of  beach sand… …whilst some of the team laid out large white crosses, held down by rocks or gravel to indicate the target zones for two of the drops. (The third target was the centre of the crater lake). A helicopter was then used to drop the bags of sand from about 400m onto the three target areas. The impacts when they hit the ground (or water) created the seismic waves required. They were also heard from a safe distance as  a very loud thwack!   The last image shows the seismic wave traces produced by the three impacts as recorded by the nearest seismometer to each impact. The drops were successfully recorded on the temporary stations giving scientists a new velocity model for White Island earthquake locations. Future tests might include heavier weights, greater drop heights and different seismometer locations to add more depth and breadth to the velocity model. (All images GNS Science)

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Filming on Ruapehu

Last week I spent some time on Ruapehu with Bruno Cedat, a french documentary maker who is making a film about the geology and landscapes of New Zealand in collaboration with GNS Science. During the making of his film he has participated in challenging outdoor adventures such as climbing, caving and kayaking in a variety of wild places across New Zealand, Here he is climbing the Pinnacles next to Whakapapa ski field. We also tramped up the mountain to the summit plateau, with great views across to Ngauruhoe volcano further north. In this next picture you can see Bruno approaching the Dome, along the edge of the summit plateau.   The Dome Shelter was covered in rime ice. Inside the shelter there is a seismometer that is used to monitor volcanic earthquakes. Here is the GeoTrip page for you to climb up to the Dome: www.geotrips.org.nz/trip.html?id=646 Here is a view of the crater lake, surrounded by a winter blanket of snow. It is currently at Alert Level 1 as you can see on the GeoNet website. For  lots more information on Ruapehu have a look at our website here Here is a preview of Bruno’s Film: New Zealand, Land of Adventure:

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Whakataki

Whakataki is a spectacular spot on the Wairarapa coast just north of Castlepoint. It features as one of the localities on our GeoTrips websiteThe shoreline is a large area of tilted rock strata that have been eroded into a broad, flat platform extending for hundreds of metres along the coast.  The rock layers are alternating sandstone and mudstone layers that stand out as distinct lines. It is believed that they formed as cyclically repeated turbulent flows of sand and mud that avalanched down and over the sides of an underwater channel about 500 to 1000 metres below the ocean surface. These sorts of deposits are know as turbidites. Here they are of early Miocene age (roughly 20 million years old) As the sediment laden water surged across the sea floor it laid down a deposit of sand and mud with several distinct layers. The base layer typically has very flat laminations, followed by a more convoluted and rippled layer above it. Above that the particles get finer as the remaining cloud of mud slowly settled on top of the coarser sandy layers below. It is interesting to look at the different structures and imagine how they formed in the dark depths of the sea so long ago. Here I am pointing at some climbing ripples in the upper sandstone layer, above a more regularly laminated base layer of the flow. They show that the current was moving from the left (south). Exploring the area shows up many interesting geological features. Here you can see that the beds are not only tilted up, but they have been dislocated by faults.   In this image you can see joints cutting across the beds at a right angle. They develop as the pressure on the sequence decreases due to erosion of overlying material. You can see how the spacing between the joints is wider for the thicker beds, and closer together on the thinner ones.   The rock layers are of interest to geologists because similar thin bedded fine grained deep sea sediments are often found to be important reservoirs for hydrocarbons which penetrate into the tiny pore spaces between the individual grains of sand.  By studying these beds where they are exposed at ground level, we can gain important information about similar but more inaccessible  sequences deep below the surface that may actually contain trapped oil or gas. During our visit, Garth Archibald was making a laser scan of the surface of the shore platform. This will be translated into a 3 dimensional computer image of the platform which can then be used for detailed analysis of the different layers in the sequence. Garth has used his laser scanner in a wide variety of settings, including a number of Christchurch cliffs that were seriously shattered by recent earthquakes, as you can see in this video.

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NZ’s First Reptile Discoverer returns to Mangahouanga

In 1958, Petroleum Geologist Don Haw was mapping the rocks in the Mohaka river catchment of Western Hawkes Bay. The project was part of a wide ranging exercise to evaluate the hydrocarbon potential of the East Coast basin at that time for BP, Shell and Todd.  His discovery of reptile bones in the Cretaceous sediments was recorded on Company maps which subsequently caught the eye of Joan Wiffen in the early seventies. She ventured into the region to take a closer look. Remarkably this led to her eventual unearthing of New Zealand’s first dinosaur fossils, as well as many other new species of exciting Cretaceous reptiles. For her significant effort Joan became known as the “Dinosaur Lady”.  For his essential initial work, Don was awarded the Wellman Prize in 2001. On March 24th 2012, 54 years after his initial explorations,  Don returned to Mangahouanga along with the teachers and school children who were participants of our GNS Science “Dinosaurs and Disasters Geocamp“. This was a historic day as it was his first return to the valley in all that time. In the photo, Don (centre) is with Robyn Adams, one of Joan Wiffen’s long term fossil hunting assistants who still leads trips into the valley. In the following transcript, Don describes his experiences from all that time ago:   “We were mapping outcropping sediments in the Upper Mohaka river tributaries, observing for the first time, what might be there. Nobody had really mapped that steep isolated terrain before. We were keen to find what was present between the greywacke basement rocks and the overlapping Upper Tertiary sandstone section. Perhaps nothing – we just didn’t know – maybe the Upper Tertiary rested directly on basement.   Was there any Cretaceous section exposed?  This was so important to the assessment of the hydrocarbon prospectivity of the region.”   “It was high summer, February 1958 I think, and we were scrambling up this really difficult stream bed, huge boulders, and totally bush covered. We recognised we were stepping on boulders and outcrops of massive concretionary sandstones which we had not seen before. These appeared to be of marine origin, and had fine shell debris in them which was triggering off alert signals to me – There might be other important fossils here!  We should look carefully! I was with field assistant Ken Fink Jensen to whom I owe much for his support and encouragement in those days, Together we began to examine some odd protuberances on the surface of certain boulders, which I quickly recognised, because of their shape and texture, had to be organic and which were almost certainly bone remains from some marine creature.  I think my initial reaction was that they were fish remains. The rock was hard, very hard, and we extracted several and brought them back to Gisborne.“ “They were sent off to Jack Marwick, a retired NZGS chief palaeotologist,  who identified them as reptilean bones. Eventually they were recognised to be Mosasaur fossils, a type of  marine Plesiosaur.  It was a first for New Zealand.”   “This region became the hunting ground of Mrs Joan Wiffen who followed up our fossil discovery, with many years of hard work there, excavating numerous other finds from the same stream bed.  She, with her husband and family team, found many new fossils, some really exciting, including some terrestrial dinosaur remains which must have been washed into those early primeval seas. It has now become one of the most prolific fossil sites in New Zealand.”The final image shows a mosasaur skull that was found by Joan and her team and is now kept at GNS Science in Lower Hutt.

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Cape Kidnappers

Cape Kidnappers and the Clifton Cliffs make for a spectacular geological site in Hawkes Bay. The cliffs extend for several kilometres southwards from Clifton, on the coast near Hastings. They  are very high and consist of quite loose rocks, so it is important not to go too close where possible. It is also important to start your visit on a falling tide which will give enough time for a return trip without being cut off by high water. At the start, near Clifton, the cliffs are made up of thick river gravels, with thin layers of white pumice (volcanic ash) and occasional dark layers of plant material.  Initially the beds are about 300 000 years old. Because they are dipping gently down to the north, you will pass further and further down the sequence as you walk along the beach to the south.and east. Here you can see the fluted erosion of the unconsolidated gravels caused by rainwater. In this photo, a layer of light coloured volcanic ash separates overlying river gravels from marine mudstones below. Just above the ash is a very thin dark organic layer with plant remains in it. There are many pale coloured ash layers in the sequence. They have been erupted from the Taupo Volcanic Zone in  the Central North Island, at least 150 kms away. The thickness of the layers even at this distance, testifies to the magnitude and violence of these past rhyolitic eruptions. In this photo you can also see how a fault has dislocated the beds by several metres. Further along the beach, towards Black Reef, there is a distinct change in the bedding, seen in this image about half way up the cliff. The lower gently dipping beds have been eroded flat with much younger beds deposited on top of them. This unconformity represents a time gap of about two and a half million years. The lower unit is three and a half million years old – the upper one starts at about 1 million. An exciting find on our visit was this fossil whalebone. It extended through the boulder for about one metre. Out on the reef itself were some well preserved shell fossils as well as another orange coloured whalebone fossil slowly being eroded away. Last but not least I should mention the gannets, for which Cape Kidnappers is most famous. The young birds here will take their first flight soon, and without looking back or touching down will travel all the way to Australia. Cape Kidnappers features on our GeoTrips website where you can also find lots of other locations to explore geology and landforms: www.geotrips.org.nz/trip.html?id=182

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