This article is republished courtesy of our NZME partner, NZ Herald
Scientists are keeping the official alert level of New Zealand’s best-known super-volcano slightly raised, as another earthquake beneath Taupō signals an unrest period still rumbling on.
It’s now been nearly one year since scientists first noticed an increase in earthquakes and ground movement at the enormous caldera system that Lake Taupō partly covers – and around six months since GeoNet nudged its Volcanic Alert Level (VAL) from zero to one for the first time in the programme’s 20-year existence.
By early 2023, scientists had already recorded more than 1600 quakes: notably a 4.2 event in September and a 5.7 event on November 30 that triggered a small lake tsunami.
Then, at 4.13pm on Sunday, came another 4.4 quake centred around the same area – near Horomatangi Reef, just southwest of Taupō, where researchers recently pin-pointed a 250 cubic km magma chamber.
The latest event, the result of a fault rupture within 10km of the surface, caused shaking felt mostly along the lake shore, along with more than 20 aftershocks so far.
While the overall pattern of seismicity over the 10-month unrest sequence pointed to magma and fluid moving about within the system, the precise driver of the latest quake was unclear.
“The recent unrest is very likely driven by magma movements and the related movement of fluids, and they can trigger earthquakes – but [they] can also be triggered by long-term plate motion in this area,” GeoNet duty volcanologist Dr Yannik Behr said.
“So, it’s difficult to attribute one particular cause for an earthquake, but we think it’s probably related [to the unrest].”
Although there’d been a noticeable decline in earthquake activity since November – with between 10 and 50 recorded each week – Sunday’s event was preceded by a slight uptick.
“We also noticed a small signal on our newly installed tsunami sensors in the lake at the time of the earthquake, but more analysis is required to find out its cause.”
Overall, Behr said the number and size of observed quakes was within expectations for a volcano at “minor” volcanic unrest.