But another study by researchers in the United States and Taiwan found a similar association
between slow earthquakes — which take places over hours or even days — and tropical cyclones in Taiwan.
Not exact matches
The rumbling upheaval in relationships
between the sexes is much like a
slow - motion
earthquake.
Unlike
slow slips events,
earthquakes — or stick - slip events — occur when surfaces quickly alternate
between sticking to each other and sliding over each other.
Fault creep is the slip and
slow release of strain in the uppermost part of the Earth's crust that occurs on some faults
between large
earthquakes, when much greater stress is released in only seconds.
Earth's mantle, the large zone of
slow - flowing rock that lies
between the crust and the planet's core, powers every
earthquake and volcanic eruption on the planet's surface.
But the CWU team points out that many
slow temblors may take place in the 500 or so years
between great quakes; this makes it unlikely that any single
slow earthquake is going to be a meaningful precursor.
Slow slip events are similar to
earthquakes, as they involve more rapid than normal movement
between two pieces of Earth's crust along a fault.
A GPS network operated by GeoNet, a partnership
between GNS Science and the New Zealand
Earthquake Commission, detected
slow slip events hundreds of miles away beneath the North Island.
Although scientists are still in the early stages of trying to understand the relationships
between slow slip events and
earthquakes, Wallace said that the study results highlight additional linkages
between these processes.