This process is known as subduction and occurs at convergent plate boundaries because oceanic crust is denser than continental crust.
Depends on the type of tectonic plate. If it is two continental plates, usually a mountain range will be formed and the plates will 'lock' together due to their thickness. The Indian sub-continent colliding with the eurasian plate is one example. If an oceanic plate is subducting under a continental plate an island arc can be formed or mountain range such as Japan and the Andies mountains respectively. This type is also where volcanoes will be commonly found unlike the collision of two continental plates, due to the magma formed from the subduction of the oceanic plate. If two oceanic plates collide, usually form an oceanic mountain range and lock together similar to the continental plates.
They dive for pearl oysters or other objects.
dive drove devine draught draft
emperor penguin
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this is because the oceanic plate is much denser than the continental plate so when they collide the oceanic plate will sink easily
Oceanic crust is more dense than continental crust. All that water weight compresses the heck out of the material in the plate and also the oceanic crust contains larger percentages of denser elements such as magnesium and iron than the continental crust which also contributes to it's higher density. This sets the conditions for what happens. The more dense oceanic crust will "dive under" continental crust because it is more dense, and all because of the difference in densities.
The ocean crust dives below the continental crust due to a collision. This collision involves the two types of crust and since the oceanic crust is denser, it sinks to the bottom while the less dense continental crust rises to the top.
One theory states that upon convergence of continental plates one will dive below the other, or subduct. This process, however is physically impossible since oceanic crusts that are many miles thick cannot dive down below continental, granitic rock that is much more dense. If anything, the oceanic crust must move onto the top of the continental plates. A more reasonable theory that has emerged lately is that the earth grows and all tectonic plates are expanding and constantly moving away from each other.
When an oceanic plate subducts below another continental or oceanic plate, the cold, wet, dense rock and sediments slowly dive into the asthenosphere, where, due to the volume of water contained in the subducting plate, the melting point of the subducting plate is lower than the surrounding rock. Volcanoes may result from the rising of molten material created by the subduction.
When an oceanic plate subducts below another continental or oceanic plate, the cold, wet, dense rock and sediments slowly dive into the asthenosphere, where, due to the volume of water contained in the subducting plate, the melting point of the subducting plate is lower than the surrounding rock. Volcanoes may result from the rising of molten material created by the subduction.
OCeanic... Look the top of the mask.. and find the brand name.. but there is nothing simillar with it on oceanic m.m..
you don't EVER turn off ANY dive computer.... they will turn themselves off when they have completed their calculations (ie: 24 hours to fly after last dive).
A convergent boundary. In the case of the Andes, the oceanic Nazca Plate and part of the oceanic Antarctic Plate slide towards the continental South American Plate. Because the former are heavier, they subduct (dive) under the lighter South American Plate causing orogenesis (the Andes) and corresponding volcanism (e.g. the Lascar Volcano).
You click the darker water underneath the statue of Poseidon on the seahorse.
It is not possible because land goes down to the bottom of the ocean.
Depends on the type of tectonic plate. If it is two continental plates, usually a mountain range will be formed and the plates will 'lock' together due to their thickness. The Indian sub-continent colliding with the eurasian plate is one example. If an oceanic plate is subducting under a continental plate an island arc can be formed or mountain range such as Japan and the Andies mountains respectively. This type is also where volcanoes will be commonly found unlike the collision of two continental plates, due to the magma formed from the subduction of the oceanic plate. If two oceanic plates collide, usually form an oceanic mountain range and lock together similar to the continental plates.