Density current
shakes
it forms from an earthquake under water pushing the water upward.
Density's role is to push the cloudy turbid water under the less dense surrounding water to start the turbidity currents
Well, the less dense plate thing dunks under the more dense one. Eventually (over millions of years) the stuff pops, going into volcanic activity. Hope this helps! Email me if you need more info @ ghambelton@verizon.bet
The collision of plates commonly includes "subduction", where one plate is forced under the other, down into the mantle. These plates are melted and rise again, adding to the magma under the overlying plate. This creates heated rock that can later emerge through the surface in volcanoes. Oceanic plates are thinner and denser than continental plates, so are the ones forced down, either under a continental plate or another oceanic plate.
density current
riptide
In the Mediterranean Sea the cool dense water sinks under less dense water which is called density current.
In the Mediterranean Sea the cool dense water sinks under less dense water which is called density current.
In the Mediterranean Sea the cool dense water sinks under less dense water which is called density current.
No, the denser plate sinks under the less dense plate in a process called subduction.
parts of the crust and upper mantle
This is called a destructive plate boundary. It occurs due to the fact that the oceanic crust is far denser than the continental crust. As a result it subducts into the mantle and is incenerated. Hope it helped:)
Because magma rises through hot spots( holes in the ground on the ocean floor) and cools forming new crust which repeats over hundreds of years making the oceanic crust more dense than continental crust. Since the oceanic crust is more dense, it sinks faster causing it to slide under the continental crust
The heavier cold air sinks and slides under the warm air and forces it upward. This causes cumulus and cumulonimbus clouds to form. This brings in the rainstorms and thunderstorms.
The older denser plate sinks under a deep ocean trench into the mantle. Some rock above the subducting plate melts and forms magma. Since the magma is less dense than the surrounding rock, it rises toward the surface. Eventually, the magma breaks through the ocean floor, making a volcanoe.
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