Scientists have uncovered a key piece of the puzzle behind the unusual “slow earthquakes” occurring off the east coast of New Zealand’s North Island.

A new international study, published in Science Advances, identifies hidden fault structures called polygonal fault systems (PFSs) as a major influence on the behavior of the northern Hikurangi subduction zone.

These shallow geological features, found in sediments entering the subduction zone, appear to play a critical role in where and how slow slip earthquakes occur.

A team of international researchers from the Helmholtz-Zentrum Dresden-Rossendorf (HZDR), Johns Hopkins University and Duke University has discovered that a century-old theory describing turbulence in fluids also applies to a very bubbly problem: how rising bubbles stir the water around them.

The Electric Viking

FutureAzA

The Nasdaq-listed Faraday Future has pivoted to crypto with plans for a basket index, crypto treasury and possibly a crypto-tracking ETF.

Thailand aims to boost tourism through a crypto-to-baht payment plan set to be trialed for foreign visitors.

In a first, scientists have recreated the formation of the first ever molecules in the universe to learn more about early star formation.

Untethered acoustic levitation device enables frictionless, high-speed movement of delicate components in industrial applications.