continental and the oceanic.
Our Tectonic plates shifting and moving around.
The places where tectonic plates meet are called plate boundaries. There are three main types of plate boundaries: convergent boundaries (plates moving towards each other), divergent boundaries (plates moving away from each other), and transform boundaries (plates sliding past each other).
There are 3 main types of boundaries between plates: Convergent- when two plates are coming together (mostly form mountains) Divergent- when two plates are moving apart (mostly form rift valleys) Transform- when two plates slide past one another (also called strike-slip)
The edges of moving crustal plates are often defined by tectonic plate boundaries. There are three main types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where plates collide, and transform boundaries where plates slide past each other. These boundaries are important in understanding the processes of earthquakes, volcanic activity, and mountain building.
The earth is broken into fourteen plates: Pacific, Juan de Fuca, North American, Cocos, Caribbean, Nazca, Scotia, South American, Antarctic, African, Arabian, Eurasian, Australian-Indian, and Philippine. These are considered the main plates and are larger than minor plates.
Is this the film? If yes you can type in your question on google and it will give a the list of the main characters.
botany and zoology
The main mineral type in Oceanic plates are made of basalt
i dont know you need to give people the anwsers and a picture with it
c plates- bedrock and granite o plates- bastlic
seven main plates and about 13 smaller ones
The rising and falling of the molten lava underneath the plates. The magma is always moving in a circular motion. Since the center of the earth is the hottest when the lava rises it cools off as it gets further away from the center then it becomes cool and dense and falls back down towards the center then it heats back up and rises. That circular motion moves the plates