Slow earthquakes such as slow slips are drawing the attention of researchers due to their potential connection to tsunami earthquakes.
An international team of seismologists recorded a slow slip event in a shallow area of plate boundary at the Hikurangi margin off the northeast shore of New Zealand, showing for the first time that such slippage can occur near troughs. This implies that subduction plates may be accumulating much more stress and strain than previously believed --before they bounce back to set off tsunami earthquakes.