The Cascadia
Subduction Zone generates a large earthquake roughly every 200 to 530 years.
Not exact matches
«This ocean drilling expedition will for the first time drill scientific boreholes within the sediments entering this
subduction zone, including the layer of sediment that eventually develops into the earthquake -
generating fault,» Professor Henstock explained.
Scientists have long wondered what accounts for that precipitous dive, and why the massive earthquakes that
generate long - ranging tsunamis at other
subduction zones have not been recorded in the trench.
This
subduction has created a collision
zone with the potential to
generate huge earthquakes and accompanying tsunamis, which happen when faulted rock abruptly shoves the ocean out of its way.
In the past few centuries, the
subduction zone off the coast of Sendai has
generated earthquakes of up to magnitude 8 or so, but nothing as powerful as a 9, which releases 30 times more energy.
The
subduction zone along the western edge of South America, where the Nazca plate slides eastward beneath the South American plate at an average rate of about 6.5 centimeters per year, can indeed
generate massive quakes.
The study site, Stardust Bay, faces a creeping part of the eastern Aleutian
Subduction Zone, which is sandwiched between the rupture areas of historical earthquakes in 1946 and 1957 that
generated tsunamis with devastating consequences to coastal communities around the Pacific Ocean.
Megathrust earthquakes can
generate destructive tsunamis and are a serious hazard facing communities located near
subduction zones.
However, an offshore
subduction zone earthquake or an earthquake
generated somewhere else around the Pacific Ocean will
generate a tsunami, which is actually a series of waves.
In contrast to more common shallow and deep earthquakes, a
subduction zone quake will
generate a destructive tsunami, a series of waves up to 30 feet (10 m) high that will hit the Cascadia coast and travel across the Pacific Ocean toward Alaska, Hawaii and Asia.
The research programme will investigate the geological processes that occur at
subduction zones - regions of the Earth's crust where one tectonic plate descends beneath another,
generating volcanoes and earthquakes.