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Convergence, divergence and strike slip.
bobobobobo
No, all motion along the faults can also occur in the form of a tsunami
along the the boundarys between 2 or more tectonic plates
Strike-slip faults Fault rupture of the ground generates vibrations-or waves-in the rock that we feel as the ground is shaking. Faults are weaknesses in the rock and therefore earthquakes tend to occur over and over along the same faults. Most major faults in the United States, particularly in California, are what are known as strike-slip faults. For strike-slip faults, the rupture is nearly vertical and during an earthquake one side slides past the other. The San Andreas fault is a strike-slip fault formed where two parts of the earth's crust (plates) slide past each other.
Convergence, divergence and strike slip.
bobobobobo
No, all motion along the faults can also occur in the form of a tsunami
Slip-strike faults always occur at transform boundaries. The San Andreas Fault is a famous transform boundary in located in southern California.
False. Earthquakes mostly occur along faults that are at or very near to plate boundaries.
along the the boundarys between 2 or more tectonic plates
plates of the earth crash into each other along faults causing an earthquake
because that's where the edges of the plates are and that's where it shifts
Strike-slip faults Fault rupture of the ground generates vibrations-or waves-in the rock that we feel as the ground is shaking. Faults are weaknesses in the rock and therefore earthquakes tend to occur over and over along the same faults. Most major faults in the United States, particularly in California, are what are known as strike-slip faults. For strike-slip faults, the rupture is nearly vertical and during an earthquake one side slides past the other. The San Andreas fault is a strike-slip fault formed where two parts of the earth's crust (plates) slide past each other.
Earthquake is the result of a sudden release of energy in the Earth's crust that creates seismic waves.Tectonic earthquakes will occur anywhere within the earth where there is sufficient stored elastic strain energy to drive fracture propagation along a fault plane.There are three main types of fault that may cause an earthquake: normal, reverse (thrust) and strike-slip. Normal and reverse faulting are examples of dip-slip, where the displacement along the fault is in the direction of dip and movement on them involves a vertical component. Normal faults occur mainly in areas where the crust is being extended such as a divergent boundary. Reverse faults occur in areas where the crust is being shortened such as at a convergent boundary. Strike-slip faults are steep structures where the two sides of the fault slip horizontally past each other ; transform boundaries are a particular type of strike-slip fault. Many earthquakes are caused by movement on faults that have components of both dip-slip and strike-slip; this is known as oblique slip.Earthquakes often occur in volcanic regions and are caused there, both by tectonic faults and the movement of magma in volcanoes. Such earthquakes can serve as an early warning of volcanic eruptions.
Most present-day faults occur along boundaries. The three types of geologic boundaries are transform boundaries, divergent boundaries and convergent boundaries.
fault