There are two types of lithosphere: the oceanic lithosphere and the continental lithosphere. The oceanic lithosphere exists in the ocean basins while the continental lithosphere exists in the continental crust.
Oceanic plates are denser and thinner, found beneath the oceans, while continental plates are thicker and less dense, making up the Earth's landmasses. These two types of tectonic plates interact at boundaries, influencing processes like earthquakes and volcanic eruptions.
The Plate Boundaries. It could be called the plate boundary, plate edge, or continental divide. With tectonic plates, they meet at the fault line.
False. A rift valley forms when continental plates diverge or pull apart. When two continental plates collide the result is a mountain range.
When two continental plates collide, they can form mountain ranges due to the intense compression and uplift of the Earth's crust. This collision can also lead to the formation of earthquakes as the plates grind against each other. Over time, the collision can result in the merging of the two continental plates into a single larger landmass.
There are two types of lithosphere: the oceanic lithosphere and the continental lithosphere. The oceanic lithosphere exists in the ocean basins while the continental lithosphere exists in the continental crust.
The area where two tectonic plates meet is called a plate boundary. At plate boundaries, interactions between the plates can result in processes like subduction, seafloor spreading, or continental collision.
Oceanic plates are denser and thinner, found beneath the oceans, while continental plates are thicker and less dense, making up the Earth's landmasses. These two types of tectonic plates interact at boundaries, influencing processes like earthquakes and volcanic eruptions.
Places, where plates meet, are called plate boundaries. There are seven significant plates along with countless minor plates. You can see that a plate can be made of both oceanic crust and continental crust. Interactions between the plates change our planet.
When two continental plates collide,fold mountains are formed.
The two types of tectonic plates are continental and oceanic.
The Plate Boundaries. It could be called the plate boundary, plate edge, or continental divide. With tectonic plates, they meet at the fault line.
If the plates are moving toward each other, the more dense oceanic plate will subduct underneath the less dense continental plate. Mountain ranges and volcanism may result as the water saturated subducting oceanic crust creates molten rock which attempts to rise to the surface.
Continental Plates
The two continental plates that meet at the San Andreas Fault are the North American Plate and the Pacific Plate. These plates are moving horizontally past each other, which causes a lot of seismic activity along the fault line. The movement has led to numerous earthquakes in California, making the San Andreas Fault one of the most well-known geological features in the world.
The two main types of plates that make up the Earth's lithosphere are oceanic plates, which are denser and thinner, and continental plates, which are less dense and thicker. These plates interact with each other at their boundaries, causing movements such as subduction, spreading, and collisions that shape the Earth's surface.
earthquake!!!!!!