The findings might apply to other
oceanic plates as well.
This olivine structure is then «frozen» into
the oceanic plate as it travels across the Earth's surface.
Not exact matches
The Andes were formed by tectonic activity whereby earth is uplifted
as one
plate (
oceanic crust) subducts under another
plate (continental crust).
Three basic forces are believed to drive
oceanic plate movement:
plates are «pushed» away from mid-ocean ridges
as new sea floor forms;
plates are «pulled»
as the oldest parts of the
plate dive back into the earth at subduction zones; and convection within the asthenosphere helps ferry the
plates along.
«When crust from an
oceanic tectonic
plate plunges beneath a continental tectonic
plate,
as it does beneath the Andean Plateau, it brings water with it and partially melts the mantle, the layer below Earth's crust,» said Rice University's Jonathan Delph, co-author of the new study published online this week in Scientific Reports.
«Orogenic
oceanic - continental subduction zones have been common
as long
as modern
plate tectonics have been active,» Delph said.
Its strength resulted from the abrupt release of
plate tectonic forces, a process known
as subduction, centered on an area beneath Honshu where it slides over the top of
oceanic crust.
The Sea of Okhotsk earthquake may have involved re-rupture of a fault in the
plate produced when the
oceanic plate bent down into the Kuril - Kamchatka subduction zone
as it began to sink.
Beghein and her research team advanced our understanding of how
oceanic plates form and evolve
as they age by using and comparing two sets of seismic data; the study revealed the presence of a compositional boundary inside the
plate that appears to be linked to the formation of the
plate itself.
At subduction zones such
as these, an
oceanic tectonic
plate sinks (subducts) into the Earth's interior, the mantle.
At certain subduction zones, such
as those in Cascadia, Sumatra and eastern Alaska, a thick sediment layer overlies the subducting
oceanic plate.
Although a few of Earth's largest islands, such
as Greenland, are composed of the same continental crust
as the mainland, most islands are made of a denser, chemically distinct
oceanic crust, created midocean by magma welling up beneath separating tectonic
plates.
With the
oceanic plate, water enters the earth
as it is trapped in minerals of the
oceanic crust or overlaying sediments.
So yes, Rapa Nui sits way out in the ass end of nowhere, atop a seamount that has formed via the Easter hotspot, an upwelling of magma below the
oceanic crust that has generated a range of undersea mountains (the Nazca Ridge)
as the Nazca
Plate drifted above it....
The consensus is that several factors are important: atmospheric composition (the concentrations of carbon dioxide, methane); changes in the Earth's orbit around the Sun known
as Milankovitch cycles (and possibly the Sun's orbit around the galaxy); the motion of tectonic
plates resulting in changes in the relative location and amount of continental and
oceanic crust on the Earth's surface, which could affect wind and ocean currents; variations in solar output; the orbital dynamics of the Earth - Moon system; and the impact of relatively large meteorites, and volcanism including eruptions of supervolcanoes.
Deep earthquakes, also called intraplate quakes, take place within the
oceanic Juan de Fuca
plate (beneath Oregon and Washington) and the Gorda
plate (beneath northwestern California)
as they subduct beneath the North America
plate.
Washington, D.C. — Seawater circulation pumps hydrogen and boron into the
oceanic plates that make up the seafloor, and some of this seawater remains trapped
as the
plates descend into the mantle at...
«Water, absorbed into the
oceanic crust
as hydrous minerals, follows the
plate into the mantle.
As the accreting (being added to)
oceanic plates move away from the spreading ridge, they start to cool, and thus become more dense.