Geothermal energy discovered right under Franz Josef glacier

supplied, via RNZ


Researchers working on the Westland Deep Fault Drilling Project have drilled nearly 900 metres down into the alpine fault at Whataroa in Westland, looking at how the fault looks and sounds before an earthquake.

The research, lead by Victoria University, GNS and the University of Otago, was published today in the international journal Nature.

Victoria University researcher John Townend, one of the lead scientists on the project, told Nine to Noon 40°C temperatures would be normal at 800 metres below the surface, but the team recorded temperatures three times that – about 120°C.

Similar geothermal temperatures were normally found at depths greater than three kilometres.

“It’s a very, very warm environment – it’s comparable to what you might see in the Taupō volcanic zone for example… but that is a volcanic area, that has got magma sitting close to the earth’s surface… and this is really totally non-volcanic,” Dr Townend said.

Dr Townend said the heat was caused by the Alpine Fault was a completely different process to the volcanic areas.

“It’s the faulting that is producing earthquakes intermittently, that jacks up the Southern Alps and that means it’s bringing up this hot rock from depth.”

Another of the lead scientists, Victoria University researcher Rupert Sutherland, told Nine to Noon no one on the team predicted it would be that hot so close to the surface.

“This geothermal activity may sound alarming but it is a wonderful scientific finding that could be commercially very significant for New Zealand.”

Dr Townend said there could be commercial opportunities from the geothermal resource.

“The potential economic benefits of this remain to be fully explored … but if you think about some of the big commercial benefits or economic activities on the West Coast – tourism, dairy – these are operations that could benefit from having a source of renewable, sustainable energy produced locally.

“So we would like to do further work to establish what the quality and extent … of that resource is.”

The Alpine Fault is known to rupture in magnitude 8 earthquakes approximately every 300 years.

The borehole that was drilled will be used for further research, including to monitor changes over the years.

That just confirms New Zealand is just a tiny  hardened crust on a big ball of molten rock.  In places, it gets very near the surface.

This also begs the question:  if it is 120 degrees near the surface, could that be creating enough radiant heat to be melting the glaciers?  You know, instead of that global warming thingy.




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