1. oceanic-continental 2. oceanic-oceanic 3. continental-continental
There are four types of plate tectonics, namely major plates, minor plates, ancient plates and plates within orogens.
Earthquakes typically occur on a any fault because the most common earthquake is the tectonic earthquake and it occurs on all the faults, though usually has the most effect on strike-slip faults (like the San Andreas fault).
The lithosphere displaces the asthenoshpere. Thick tectonic plates, such as those made of continental crust, displace more asthenosphere than do thin plates, such as those made of oceanic lithosphere. The lithosphere displaces the asthenoshpere. Thick tectonic plates, such as those made of continental crust, displace more asthenosphere than do thin plates, such as those made of oceanic lithosphere.
There are three types of plate collisions. They are classified by the type of crust involved in the collision. Plate collisions fall into these three types: 1. Both plates have an oceanic leading edge, 2. One plate has a continental leading edge and the other has an oceanic leading edge, and 3. both plates have a continental leading edge
The two main types of plates are continental plates and oceanic plates. Continental plates are larger, thicker and less dense compared to oceanic plates.
Convergence, divergence and strike slip.
Indo-Austrailan and the Eurasian Plates Stay in School Kids
The interaction areas between tectonic plates are called boundaries. There are three types of boundaries:Transform--where plates essentially grind past each other with no subduction.Convergent--where plates collide. Oceanic plate to oceanic plate convergence will result in the more dense plate subducting under the less dense plate.Divergent--where plates move apart. The major diverging plates are located at the mid-ocean ridge system where melting material from the asthenosphere fills in the separating plate zone, creating new crust.
Convergence
divergent, transform and convergent divergent plate boundaries move away from each other, convergent plate boundaries move toward each other, and transform plate bounties slide past each other.
volcanic lava
The interaction areas between tectonic plates are called boundaries. There are three types of boundaries:Transform--where plates essentially grind past each other with no subduction.Convergent--where plates collide. Oceanic plate to oceanic plate convergence will result in the more dense plate subducting under the less dense plate.Divergent--where plates move apart. The major diverging plates are located at the mid-ocean ridge system where melting material from the asthenosphere fills in the separating plate zone, creating new crust.
Trasform(plates sliding past each other.) Converging(plates colliding.) Divergent(plates moving away.) These are 3 different types of plate boundries
It is along the boundary between tectonic plates that most earthquakes occur. These plate boundaries are zones of differential movement between the plates. The tectonic plates, great masses of shifting crust, move into, along or away from each other at their boundaries. Forces of almost unimaginable magnitude build up pressures that cannot possibly be measured. And this occurs between masses of rock and earth that do not want to shift. When they "let go" in response to the pressure, a quake can occur.
Convergent boundaries can form between two oceanic plates, between one oceanic plate and one continental plate, or between two continental plates.
At a convergence boundary during collision of two plates there could either be Subduction or Outcropping. Subduction occurs when the collision involves plates of different types and densities while the other happens when it involves similar plate types. Mountain ranges are formed, also Subduction Zones gives rise to Trenches.
Oceanic-Continental Convergence - Andean-Type - the Andes MountainsOceanic-Oceanic Convergence - Aleutian-Type - island arcsContinental-Continental Convergence - the Appalachian Mountains