sheer wall
A sharp cliff caused by sudden movements along dip-slip faults is called an earthquake. It causes the ground to shake for several seconds.
Normal faults are characterized by the hanging wall moving down relative to the footwall, while reverse faults are characterized by the hanging wall moving up relative to the footwall. Both faults are caused by compressional forces in the Earth's crust, but their movements are opposite in direction.
A seismometer is the instrument used to measure horizontal movements along faults. It records the seismic waves generated by these movements.
Three types of faults include: Strike-slip fault: horizontal movements along the fault line Normal fault: caused by tensional forces, with the hanging wall moving down relative to the footwall Reverse fault: caused by compressional forces, with the hanging wall moving up relative to the footwall
Cracks in the moon's bedrock are called "faults" or "fractures." These features are caused by stress and movement within the lunar surface, much like on Earth.
A sharp cliff caused by sudden movements along dip-slip faults is called an earthquake. It causes the ground to shake for several seconds.
A sharp cliff caused by sudden movements along dip-slip faults is called an earthquake. It causes the ground to shake for several seconds.
sheer wall
sheer wall
Vibrations in the Earth caused by sudden movements of rock are called earthquakes. These movements typically occur along geological faults, where stress builds up until it is released, resulting in seismic waves that propagate through the Earth. The intensity and duration of these vibrations can vary, depending on the magnitude of the earthquake and the geological conditions.
Normal faults are characterized by the hanging wall moving down relative to the footwall, while reverse faults are characterized by the hanging wall moving up relative to the footwall. Both faults are caused by compressional forces in the Earth's crust, but their movements are opposite in direction.
A seismometer is the instrument used to measure horizontal movements along faults. It records the seismic waves generated by these movements.
faults are caused by the plates under neath earth crashing together and/or parting
earthquakes
Reverse failts are caused by compression. Normal faults however are formed by tension.
Earthquake
Stress and faults are both caused by tectonic plates.