About 10 days ago, drilling was stopped at the Alpine Fault drill site so that geophysical measurements could be made down the borehole, and the bit could be replaced. This involved lifting all of the drill rods out one by one and stacking them next to the rig. Next to come up was the bottom […]
Bottom Hole Assembly Read More »
Announcing our new Google Map that shows the locations of blog posts, videos and some of our website information within New Zealand. Zoom in and out to find a location and click on any icon to go straight to the online content. If you enable full screen (by clicking on the square icon at the
Geolocating GNS Science Outreach Read More »
A visit to Fox Glacier shows that changes over the last 5 years are similar to those at the Franz Josef Glacier. Here is a view of the Fox Glacier front in 2009: And this year (March 2014): The terminal face from another angle in 2009… …and as it was recently in 2014. The grass
Franz Josef Glacier 2009 – Julian Thomson GNS Science Recently I visited the West Coast Glaciers and was interested to see their condition after my last visit 5 years ago in 2009. Franz Josef 2009- Photo Eric Burger These photos give and immediate comparison of Franz Josef Glacier over the last 5 years: In 2009 the
Franz Josef Ice on the Retreat Read More »
Simon Cox GNS Science M. McSaveney GNS Science Slip Stream is a tributary to the Dart River in the South Island of New Zealand. There has been an active landslide here for several thousand years, periodically sending down lobes of debris to gradually build up a large fan in the Dart Valley. There was
The Dart Landslide Read More »
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
The growth of Tasman Glacier Lake Read More »
K-Pg boundary layer – when the Earth changed forever The K-Pg Boundary (or Cretaceous Paleogene boundary, or K-T boundary as it is still sometimes called) is a layer in the Earth’s crust that marks a very dramatic moment in the history of life on earth about 65 million years ago. There is a huge change
Global Catastophe in a thin rock layer Read More »
Along with Waipatiki, another excellent Hawkes Bay locality for looking at rocks laid down over a cycle of sea level change is Darkeys Spur, about twenty minutes by car west of Lake Tutira. The road is very narrow and care should be exercised to park safely and watch out for vehicles. Fortunately the road is
Darkeys Spur’s rock record of sea level change Read More »
Over the last two weeks, GNS Science, with support from the Todd Foundation, The Royal Society and the National Aquarium in Napier, has been running a ‘Dinosaurs and Disasters Geocamp’ for a group of Hawkes Bay Intermediate level students and teachers. The participants investigated many landforms and cliff sections around Hawkes Bay. GNS Science geologists
Dinosaurs and Disasters Geocamp 2012 Read More »
Along with biological specimens, the sled brings a lot of rock off the sea floor. Christian Timm sorts through all the samples, cuts some of them up with a rock saw, and packs and labels them to be studied in detail back at GNS Science. The different minerals present in the samples will be analysed