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The three types of faults are normal, reverse, and strike-slip faults. Normal faults are associated with divergent plate boundaries, reverse faults with convergent plate boundaries, and strike-slip faults with transform plate boundaries.
Yes, It is convergent
The three types of plate boundaries are divergent, convergent, and transform boundaries. Divergent boundaries have normal faults, convergent boundaries have thrust faults, and transform boundaries have strike-slip faults.
The boundary between plates is called a plate boundary, which is where tectonic plates meet. These boundaries can be divergent, convergent, or transform faults, and are characterized by various geological activities such as earthquakes, volcanic eruptions, and mountain building. Plate boundaries are dynamic regions where the Earth's lithosphere is constantly changing.
Earthquakes occur at all three types of plate boundary.
There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.
The three types of faults are normal, reverse, and strike-slip faults. Normal faults are associated with divergent plate boundaries, reverse faults with convergent plate boundaries, and strike-slip faults with transform plate boundaries.
There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.
The normal fault, the thrust fault, the transcurrent fault , and the reverse fault.
Yes, It is convergent
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
The three types of convergent plate boundaries are oceanic-continental, oceanic-oceanic, and continental-continental boundaries. Oceanic-continental boundaries occur when an oceanic plate subducts beneath a continental plate. Oceanic-oceanic boundaries happen when one oceanic plate subducts beneath another oceanic plate. Continental-continental boundaries involve the collision of two continental plates.
Conteinent-Conteinent boundery
Convergent boundary.
A convergent boundary causes compressional stress.
Normal faults are associated with divergent plate boundaries, where two tectonic plates are moving away from each other. This type of boundary results in tensional stress that leads to the hanging wall moving down relative to the footwall, creating a normal fault.