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What are the different boundaries and faults?

Updated: 8/19/2019
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13y ago

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divergent-pullling apart

convergent-pushing together

transform-sliding past 1 another

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Q: What are the different boundaries and faults?
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Related questions

Why are strike faults common at transform boundaries?

Strike-slips are common at transform boundaries because of Shear stress which pushes different parts of rock in different directions.


What are the three types of fault lines?

There are three types of fault lines in the crust. There are divergent boundaries, convergent boundaries, and transform boundaries.


Where do most present day faults occur?

Most present-day faults occur along boundaries. The three types of geologic boundaries are transform boundaries, divergent boundaries and convergent boundaries.


Why are strike-slip faults common at transform boundaries?

Strike-slips are common at transform boundaries because of Shear stress which pushes different parts of rock in different directions.


Why are strikes-slip faults common at transform boundaries?

Strike-slips are common at transform boundaries because of Shear stress which pushes different parts of rock in different directions.


Where do the majority faults occur?

The majority of faults occur in the plate boundaries.


Where do majority of faults occurs?

The majority of faults occur in the plate boundaries.


Why are strik-slip faults common at transform boundaries?

They are common at transform boundaries because strike-slip faults move up and down like transform boundaries.


Are all faults located on tectonic plate boundaries?

No. Many faults, especially minor ones, are located far from plate boundaries.


Do earthquakes mostly occur at faults that are away from plate boundaries?

False. Earthquakes mostly occur along faults that are at or very near to plate boundaries.


Why do most earthquakesoccur at plate boundaries?

Because most plates boundaries are also faults


Where do most transform faults occur?

Most present-day faults occur along boundaries. The three types of geologic boundaries are transform boundaries, divergent boundaries and convergent boundaries.