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AnswerThe continental plates are made up of largely granitic rock, while the oceanic plates are largely basaltic rock. Certainly some other types of rock are included, but these are the largest contributors to the material or composition. A link is provided below for more information.
The two types are Dna, and fossils
Slab pull occurs when two plates stick together.
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mathematical model and physical model
The two types of tectonic plates are continental and oceanic.
The two types of tectonic plates are continental and oceanic.
Two types of divergent plates are Eurasian and Nazca
The three types of Earth's plates are convergent plates, where two plates move towards each other; divergent plates, where two plates move away from each other; and transform plates, where two plates slide past each other horizontally.
There are 3 types of plate boundaries, but only one in of them do the plates "connect". There is a convergent boundary, in which two plates come together (or "connect"), a divergent boundary, where two plates move a apart, and a transform boundary, which is when two plates slide next to each other.
two seafloor plates and a seafloor plate and continental plate
When two continental plates collide,fold mountains are formed.
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.
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.
There are two types of crust on Earth: oceanic and continental. A convergent plate boundary can involve two plates of oceanic crust, two of continental crust, or one of each.
The Earth's crust is primarily made up of two types of plates: oceanic plates, which are denser and thinner, and continental plates, which are less dense and thicker. These plates interact at plate boundaries, where tectonic forces drive movements such as subduction, spreading, and collision.
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