The Earth's rocky outer crust solidified billions of years ago, soon after the Earth formed. This crust is not a solid shell; it is broken up into huge, thick plates that drift atop the soft, underlying mantle.
The plates are made of rock and drift all over the globe; they move both horizontally (sideways) and vertically (up and down). Over long periods of time, the plates also change in size as their margins are added to, crushed together, or pushed back into the Earth's mantle. These plates are from 50 to 250 miles (80 to 400 km) thick.
Oh and if you want to know how to make things huge: go to power point and copy down what you want then copy and paste.
Its when the oceanic crust and the continental crsut colide together.
The African Plate is primarily a continental tectonic plate. It includes much of the African continent and extends into the Atlantic Ocean and the Indian Ocean. While it contains oceanic crust along its western and eastern boundaries, the main portion of the plate consists of continental crust.
not nescessarily. It could be two plates of any kind rubbing against each other. Sometimes it is two continental plates or one of each.
When an oceanic plate converges with a continental plate at a convergent boundary, the denser oceanic plate typically subducts beneath the lighter continental plate. This process can lead to the formation of a trench in the ocean where the oceanic plate sinks, and it can also result in volcanic activity on the continental plate, creating a volcanic arc. Additionally, intense pressure and friction from the subduction process can cause earthquakes in the region.
When the ocean floor comes into contact with a continental plate, subduction often occurs if the oceanic plate is denser. The oceanic plate may slide beneath the continental plate, leading to the formation of deep ocean trenches and volcanic activity. This subduction process can result in geological phenomena such as earthquakes and the creation of mountain ranges on the continent. Over time, sediment and material from the ocean floor can also accumulate at the boundary, influencing the geology of the continental plate.
a BIG earthquake
When an ocean plate collides with a continental plate, a subduction zone occurs and forms a deep trench. An ocean plate is more dense while a continental plate is less dense which causes the ocean plate to go under the continental plate and pull the land and water down, forming a trench.
Deep ocean trenches are associated with subduction zones where an ocean plate descends into the asthenosphere. The Ocean plate is heavier than a Continental plate which causes the Ocean plate to slide beneath the Continental plate. As the Ocean plate descends, a deep ocean trench is formed.
When an ocean plate collides with a continental plate, a subduction zone occurs and forms a deep trench. An ocean plate is more dense while a continental plate is less dense which causes the ocean plate to go under the continental plate and pull the land and water down, forming a trench.
When an ocean plate collides with a continental plate, a subduction zone occurs and forms a deep trench. An ocean plate is more dense while a continental plate is less dense which causes the ocean plate to go under the continental plate and pull the land and water down, forming a trench.
No. It subducts under the continental plate.
Its when the oceanic crust and the continental crsut colide together.
When an oceanic plate collides with a continental plate, the denser oceanic plate is subducted beneath the continental plate due to its weight. This subduction can lead to the formation of deep ocean trenches, volcanic arcs, and seismic activity.
As the oceanic plate pushes against the continental plate, it forms a subduction zone where it sinks beneath the continental plate due to its greater density. This process can create deep ocean trenches, earthquakes, and volcanic activity as the sinking plate melts and interacts with the mantle.
The oceanic plate goes under the continental plate and into the mantle in a process known as subduction. This results in the formation of mountains and volcanoes on the continental plate.
The Himalayas and the Tibetan Plateau are formed by a continental-continental boundary where the Indian continental plate is moving north against the Eurasian continental plate.
The African Plate is primarily a continental tectonic plate. It includes much of the African continent and extends into the Atlantic Ocean and the Indian Ocean. While it contains oceanic crust along its western and eastern boundaries, the main portion of the plate consists of continental crust.